The IB Physics THERMAL PHYSICS

Wednesday May 28, 2008

3. THERMAL PHYSICS

3.1. From mechanics to thermal physics

Many concepts in thermal physics are based on mechanical concepts - for example temperature which is a measure of average kinetic energy. When mechanics is applied on millions and millions of atoms or molecules moving and colliding, it is often not possible to study every one in detail, but they are represented by “collective”, more easily measurable quantities.

3.2. Temperature, internal energy and heat

Temperature

This is ususally measured in degrees Celsius or oC where the freezing point of water is 0 oC and the boiling point is + 100 oC. We have taken observable physical phenomena for the substance water, and comibined with something that changes in the interval between them (the height of a pillar of a liquid in a thermometer) a temperature scale could be defined. Though we have negative values on the Celsius scale temperature is a scalar - the negative sign does not give information about any direction, only about what value the “temperature” has compared to that of a chosen phenomenon (freezing or melting water).

In the Kelvin scale the size of a “degree” is the same as in Celsius, but the scale has been shifted to avoid negative numbers. The lowest possible temperature in the universe (more about why it is that later), about - 273 oC is 0 Kelvin = 0 K (not called ‘degrees’) and 0 oC is 273 K.

ex. 25 oC = (25 + 273) K = 298 K and 400 K = (400 - 273) oC = 127 oC

The higher the temperature, the more do the atoms or molecules move. A more exact definition of temperature is that

temperature is proportional to average kinetic energy

[or (not necessary in IB) Ek,average = ½mv2average = 3kT/2 where m = the mass of the atom or molecule, T = the temperature in Kelvins, k = the Boltzmann constant = 1.38 x 10-23 JK-1 ]

Thermal energy (= energy in the form of kinetic energy of the atoms in a material) can be transferred from one object to another in several ways, which means that one loses average kinetic energy (the temperature decreases, it cools) and another gains it (the temperature increases):

Thermal energy flows from an object with a higher temperature to one with a lower

“Zeroth law of thermodynamics”

If two objects have the same temperature, then there is no flow of thermal energy between them and vice versa - if there is no flow of thermal energy, they must be at the same temperature. They are then in thermal equilibrium. That these (no flow of thermal energy and same temperature) are equivalent is somtimes called the 0th law of thermodynamics.

Internal energy

The temperature is proportional to average kinetic energy of the atoms. But there are millions of them, and their total kinetic energy combined with their total potential energy (which they may have because there are forces between the atoms or molecules) is the total internal energy U.

Read the rest of this entry »



Scientfic Advancements due to Relativity

Monday May 19, 2008

The scientific world of the late nineteenth and early twentieth century believed they discovered all of the laws and equations of the natural world. Those scientists based their works and studies on the rules of classical physics. Only a few humans remained as revolutionary thinkers and physicists within the community of that time period. Albert Einstein fell into the rare revolutionary group of imaginative scientists. Einstein discovered many revolutionary equations and theories during his lifetime. Although one of the half respectable theorists of the twentieth century, he did not perform well in grade school or college. He spent most of his career researching and studying in Europe, starting in the Swiss Patent Office. With the ample and serene conditions at the Patent Office, Einstein could ponder on his theories and thoughts (Motz and Weaver 243-7). At the Patent Office, he discovered the Special Theory of Relativity and the Photoelectric Effect (Motz and Weaver 244; ‘Quantum Theory’ 4). Then in 1910, Einstein moved to the University of Prague for a full professorship. Mr. Einstein developed the basis of the General Theory of Relativity in Prague. The Annalen der Physik, a German science publication, published his General Theory of Relativity, which shows that ’space is not merely a backdrop against which the events of the universe unfold, but that space itself has a fundamental structure that is affected by the energy and masses of the bodies it contains.’ This curvature of space propelled him to include the newly-formed positively curved geometry of Georg Riemann. The positively curved geometry contained curved lines and planes replacing the old Euclid straight lines and planes. After the discovery of the General Theory of Relativity, he began to ‘formulate mathematical framework that would unite both electromagnetism and gravitation,’ which is now called the unified field theory. When the Nazis overran Germany in 1932, Einstein fled to the United States of America where he continued his work at Princeton. He was a professor in the Institute for Advanced Study at Princeton where he died during practice in 1955 (Motz and Weaver 247-50). The two theories of relativity were the most recognized theories of Einstein’s works. Likewise, they produced the most significant effects onto the scientific world. Einstein’s composition of the theories of relativity impacted the scientific community by spurring the intellectual growth of quantum theory and mechanics, by theorizing and discovery of black holes, and by the beginning of formulating new theories and experiments in the area of time travel.

Read the rest of this entry »



Albert Einstein

Monday May 19, 2008

Albert Einstein

Einstein was born on March 14, 1879, in Ulm Germany. He lived there with his parents,

Herman and Pauline. Einstein attended a Catholic School near his home. But, at age 10, Einstein

was transferred to the ‘Luitpold Gymnasium’, where he learned Latin, Greek, History, and

Geography. Einstein’s father wanted him to attend a university but he could not because he did not

have a diploma from the Gymnasium. But there was a solution to this problem over the Alps, in

Zurich. There was The Swiss Federal Institute of Technology which did not require a diploma to

attend. The one thing it did require was applicant to pass an entrance exam. But then yet another

problem arose most scholars were 18 when they entered the institute, and Einstein was only 16.

In Berne, on January 6, 1903; Einstein married Mileva Maric. The twowitnesses at the

small, quiet wedding, were Maurice Solovine and Conard Habicht. After the wedding, there was a

meal to celebrate at a local restaurant. But no honeymoon. After the meal, the newlyweds returned

to their new home. It was a small flat, about 100 yards away from Bere’s famous clock tower.

Upon returning home, a small incident occured, that was to occur many times throughout Einstern’s

life; he had forgotten his key. A year later, in 1904 they had a child, Hans Albert. In that same

year, he recieved a job at the swiss patent office.

Read the rest of this entry »



Nuclear Energy

Monday May 19, 2008

Nuclear energy, also called atomic energy, is the powerful energy released by changes in the nucleus (core) of atoms. The heat and light of the sun result from nuclear energy. Scientists and engineers have found many uses for this energy, including the production of electric energy and the explosion of nuclear weapons. Scientists knew nothing about nuclear energy until the early 1900’s, though they knew that all matter consists of atoms. Scientists then further learned that a nucleus makes up most of the mass of every atom and that this nucleus is held together by an extremely strong force. A huge amount of energy is concentrated in the nucleus because of this force. The next step was to make nuclei let go of much of that energy. Scientists first released nuclear energy on a large scale at the University of Chicago in 1942, three years after World War II began. This achievement led to the development of the atomic bomb. The first atomic bomb was exploded in the desert near Alamogordo, New Mexico, on July 16, 1945. In August, United States planes dropped bombs on Hiroshima and Nagasaki, Japan. The bombs largely destroyed both cities and helped end World War II. Since 1945, peaceful uses of nuclear energy have been developed. The energy released by nuclei creates large amounts of heat. This heat can be used to make steam, and the steam can be used to generate electric energy. Engineers have built devices called nuclear reactors to produce and control nuclear energy. A nuclear reactor operates somewhat like a furnace. But instead of using such fuels as coal or oil, almost all reactors use uranium. And instead of burning in the reactor, the uranium fiss power production is by far the most important peaceful use of nuclear energy. Nuclear energy also powers some submarines and other ships. In addition, the fission that produces nuclear energy is valuable because it releases particles and rays called nuclear radiation that have uses in medicine, industry, and science. However, nuclear radiation can be extremely dangerous. Exposure to too much radiation can result in a condition called radiation sickness. Almost all the world’s electric energy is produced by hydroelectric and thermal power plants. Hydroelectric plants use the force of rushing water from a dam or waterfall to generate electricity. Thermal plants use the force of steam from boiling water. The great majority of thermal plants burn fossil fuels–coal, oil, and natural gas–to produce heat to boil water. The remaining thermal plants fission uranium. Few countries have enough water power to generate large amounts of hydroelectricity. Most countries depend mainly on fossil fuels. But fossil fuels are a non-renewable resource. Therefore, many experts predict that nuclear power will become increasingly important. Worldwide distribution of nuclear energy. In the mid-1990’s, about 425 nuclear power reactors operated in about 30 countries. Nuclear power plants produced less than 20 percent of the world’s electric energy. The United States had about 110 nuclear reactors and was the world’s largest producer of nuclear energy. Reactors produced about 20 percent of the country’s electricity. Canada had 22 reactors, which produced about 15 percent of Canada’s electricity. Other countries, notably France and Japan, have a large nuclear power generating capacity. Advantages and disadvantages of nuclear energy. Nuclear power plants have two main advantages over fossil-fuel plants. (1) Once built, a nuclear plant can be less expensive to operate than a fossil-fuel plant, mainly because a nuclear plant uses a much smaller volume of fuel. (2) Uranium, unlike fossil fuels, releases no chemical or solid pollutants into the air during use. However, nuclear power plants have three major disadvantages. These drawbacks have slowed the development of nuclear energy in the United States. (1) Nuclear plants cost more to build than fossil-fuel plants. (2) Because of the need to assure that hazardous amounts of radioactive materials are not released, nuclear plants must meet certain government regulations that fossil-fuel plants do not have to meet. For example, a nuclear plant must satisfy the government that it can quickly and automatically deal with any kind of emergency. (3) Used nuclear fuel produces dangerous radiation long after it has been removed from the reactor. The full development of nuclear energy. Many experts believe that the benefits of nuclear energy outweigh any problems involved in its production. According to these experts, oil may be so scarce by the mid-2000’s that it will be too expensive to drill. Canada, Germany, Russia, the United States, and some other countries have enough coal to meet their energy requirements for hundreds of years at present rates of use. However, coal releases large amounts of sulfur and other pollutants into the air when it is burned. If nuclear energy were fully developed, it could completely replace oil and coal as a source of electric power. But a number of problems must be solved before nuclear energy can be fully developed. For example, almost all today’s power reactors use a scarce type of uranium known as U-235. If U-235 continues to be used at its present rate, the world’s supply of it will become so small that it will be too expensive to mine and process by about 2050. Therefore, for nuclear energy to replace other energy sources, it must be based on fuel that is much more plentiful than U-235. NUCLEAR ENERGY/The science of nuclear energy The process by which a nucleus releases energy is called a nuclear reaction. To understand the various types of nuclear reactions, a person must know something about the nature of matter. The composition of matter All the matter that makes up all solids, liquids, and gases is composed of chemical elements. The chemical elements, in turn, are composed of atoms. A chemical element consists of a substance that cannot be broken down chemically into simpler substances. There are 112 known chemical elements. Ninety-one of them are found on or in the earth. The other 21 elements are artificially created. Scientists rank the elements according to mass, a measure of the quantity of matter in an object. An object’s mass is proportional to its weight. Hydrogen is the lightest natural element, and uranium is the heaviest. Most of the artificially created elements are heavier than uranium. Atoms and nuclei. An atom consists of a positively charged nucleus and one or more electrons, which are negatively charged. The nucleus makes up almost all of an atom’s mass. The electrons, which are almost massless, revolve about the nucleus. Electrons determine the various chemical combinations that an atom enters into with other kinds of atoms . However, electrons do not play an active part in nuclear reactions. The nuclei of every chemical element except hydrogen consist of particles called protons and neutrons. An ordinary nucleus of hydrogen, the lightest element, has one proton and no neutrons. The heaviest elements, such as uranium and thorium, have the largest number of protons and neutrons. Protons carry a positive charge. Neutrons have no net charge. Extremely strong forces, called nuclear forces, hold the protons and neutrons together in the nucleus. The nuclear forces of each type of nucleus determine the amount of energy that would be required to release its neutrons and protons. Isotopes. Most chemical elements have more than one form. These different forms are called the isotopes of an element. The atoms that make up each of the different forms have different masses and are also called isotopes. Scientists identify an isotope by its mass number–that is, the total number of protons and neutrons in each of its nuclei. All the isotopes of a given element have the same number of protons in every nucleus. Every hydrogen nucleus, for example, has just 1 proton. Every uranium nucleus has 92 protons. However, each isotope of an element has a different number of neutrons in its nuclei and so has a different mass number. For example, the most plentiful isotope of uranium has 146 neutrons. Its mass number is therefore 238 (the sum of 92 and 146). Scientists call this isotope uranium 238 or U-238. The uranium isotope that almost all nuclear reactors use as fuel has 143 neutrons, and so its mass number is 235. This isotope is called uranium 235 or U-235. No two elements have the same number of protons in their atoms. However, if an atom gains or loses one or more protons, it becomes an atom of a different element. However, if an atom gains or loses one or more neutrons, it becomes another isotope of the same element. Nuclear reactions A nuclear reaction changes the structure of a nucleus. The nucleus gains or loses one or more neutrons or protons. It thus changes into the nucleus of a different isotope or element. If the nucleus changes into the nucleus of a different element, the change is called a transmutation . Three types of nuclear reactions release useful amounts of energy. These reactions are (1) radioactive decay, (2) nuclear fission, and (3) nuclear fusion. During each reaction, the matter involved loses mass. The mass is lost because it changes into energy. Radioactive decay, or radioactivity, is the process by which a nucleus changes into the nucleus of another isotope or element. The process releases energy chiefly in the form of particles and rays called nuclear radiation. Uranium, thorium, and several other elements decay naturally and so contribute to the natural, or background, radiation that is always present on the earth. Nuclear reactors produce radioactive isotopes artificially. Nuclear radiation accounts for about 10 percent of the energy produced in a reactor. Nuclear radiation consists largely of alpha and beta particles and gamma rays. An alpha particle, which is made up of two protons and two neutrons, is identical with a helium nucleus. A beta particle is identical with an electron. It results from the breakdown of a neutron in a radioactive nucleus. The breakdown also produces a proton, which remains in the nucleus. Gamma rays are electromagnetic waves similar to X rays. Scientists measure the rate of radioactive decay in units of time called half-lives. A half-life equals the time required for half the atoms of a particular radioactive element or isotope to decay. Half-lives range from a fraction of a second to billions of years. Nuclear fission is the splitting of heavy nuclei to release energy. All commercial nuclear reactors produce energy in this way. To produce fission, a reactor requires a bombarding particle, such as a neutron, and a target material, such as U-235. Nuclear fission occurs when the bombarding particle splits a nucleus in the target material into two parts called fission fragments. Each fragment consists of a nucleus with about half the neutrons and protons of the original nucleus. The energy is released in many forms. But most of the energy released by fission eventually takes the form of heat. The bombarding particle must first be captured by a nucleus for fission to occur. Reactors use neutrons as bombarding particles because they are the only atomic particles that are both easily captured and able to cause fission. Neutrons can also pass through most kinds of matter, including uranium. The target material. Commercial power reactors use uranium as their target material, or fuel. A uranium nucleus is the easiest of all natural nuclei to split because it has a large number of protons. Protons naturally repel one another, and so a nucleus with many protons has a tendency to “fly apart” and can be split with little difficulty. Uranium also makes a good nuclear reactor fuel because it can sustain a continuous series of fission reactions. As a result, uranium can produce a steady supply of energy. To create a series of reactions, each fissioned nucleus must give off neutrons. Each of these neutrons can split still another uranium nucleus, thus releasing still more neutrons. As this process is repeated over and over, it becomes a self-sustaining chain reaction. Chain reactions can produce an enormous amount of energy. Only nuclei that have many more neutrons than protons, such as uranium nuclei, can produce a nuclear chain reaction. The scarce uranium isotope U-235 is the only natural material that nuclear reactors can use to produce a chain reaction. Nuclei of the much more abundant U-238 isotope usually absorb neutrons without fissioning. An absorbed neutron simply becomes part of the U-238 nucleus. Neutrons released in fission travel too rapidly to be absorbed by U-235 nuclei in numbers large enough to sustain a chain reaction. Reactors can use U-235 as a fuel because they utilize other materials called moderators to slow the neutrons down. Some reactors use water as a moderator, while others use graphite. The slowed neutrons travel at a velocity of about 2.2 kilometers per second and are known as thermal neutrons. Reactors that use moderators are called thermal reactors. Most of today’s reactors are thermal reactors. Thermal neutrons are highly effective in causing fission in U-235. Therefore, the uranium in a thermal reactor can have a low percentage of U-235 content. Depending on their design, today’s power reactors use a U-235 content ranging from 0.71 percent–the percentage in natural uranium–to about 4 percent. Special purpose reactors may use fuel with a higher percentage of U-235. Scientists have also developed fast reactors, in which high-velocity neutrons cause the fissions. These reactors use plutonium or uranium 233 fuel. Fast breeder reactors produce more fuel material than they consume. A fast breeder reactor that converts U-238 to plutonium can greatly extend the use of uranium as an energy resource. In addition, a fast reactor can be designed to consume certain radioactive elements that have long-lives and are present in used fuel. Such a reactor would reduce the amount of certain radioactive wastes that must be disposed of. The section Research on new types of reactors in this article discusses fast reactors in more detail. Nuclear fusion occurs when two lightweight nuclei fuse (combine) and form a nucleus of a heavier element. The products of the fusion have less mass than the original nuclei had. The lost mass has therefore been changed into energy. Fusion reactions that produce large amounts of energy can be created by means of extremely intense heat. Such reactions are called thermonuclear reactions. Thermonuclear reactions produce the energy of both the sun and the hydrogen bomb. A thermonuclear reaction can occur in only a form of matter called plasma. Plasma is a gaslike substance made up of free electrons and free nuclei (nuclei that have no electrons revolving about them). Normally, nuclei repel one another because of the positive charges of their protons. However, if a plasma containing lightweight atomic nuclei is heated many millions of degrees, the nuclei begin moving so fast that they overcome the force of repulsion and fuse. Problems of controlling fusion. Scientists have not yet succeeded in harnessing the energy of fusion to produce electric energy. In their fusion experiments, scientists generally work with plasmas that are made from isotopes of hydrogen. Hydrogen has three isotopes. A mixture of deuterium and tritium is an excellent thermonuclear fuel because ordinary seawater contains plentiful stocks of deuterium and lithium. One barrel of seawater contains enough of these substances to produce as much energy as the burning of about one-fifth of a barrel of oil. To produce a controlled thermonuclear reaction, a plasma of one or more hydrogen isotopes must be heated many millions of degrees. But scientists have yet to develop a container that can hold plasma this hot. The plasma expands quickly. In addition, the walls of the container must be kept at low temperatures to prevent them from melting. But if the plasma touches the walls, it becomes too cool to produce fusion. The plasma must therefore be kept away from the walls of the container long enough for its nuclei to fuse and produce usable amounts of energy. Fusion devices. Most experimental fusion reactors are designed to contain hot plasma in “magnetic bottles” twisted into various shapes. The walls of the bottles are made of copper or some other metal and are surrounded by electromagnets. An electric current is passed through the electromagnets, creating a magnetic field on the inside of the walls. The magnetism pushes the plasma away from the walls. All the fusion devices thus far developed, however, use much more energy than they create. The section Research on new types of reactors discusses experimental fusion reactors in greater detail. NUCLEAR ENERGY/How nuclear energy is produced All large commercial nuclear power plants produce energy by fissioning U-235. But U-235 makes up about 0.71 percent of the uranium found in nature. About 99.28 percent of all natural uranium is U-238. The two types occur together in uranium ores, such as carnotite and pitchblende. Separating the U-235 from the U-238 in these ores is difficult and costly. For this reason, the fuel used in reactors consists largely of U-238. But the fuel has enough U-235 to produce a chain reaction. Nuclear fuel requires special processing before and after it is used. The processing begins with the mining of uranium ore and ends with the disposal of fuel wastes. This section deals chiefly with the methods used in the U.S. nuclear power industry. These methods resemble those used in other countries. Power plant design. Most nuclear power plants cover 200 to 300 acres (80 to 120 hectares). The majority are built near a large river or lake because nuclear plants require enormous quantities of water for cooling purposes. A nuclear plant consists of several main buildings, one of which houses the reactor and its related parts. Another main building houses the plant’s turbines and electric generators. Every plant also has facilities for storing unused and used fuel. Many plants are largely automated. Each of these plants has a main control room, which may be in a separate building or in one of the main buildings. The reactor building, or containment building, has a thick concrete floor and thick walls of steel or of concrete lined with steel. The concrete and steel guard against the escape of radioactive material from an accidental leak in the nuclear reactor. Power reactors that are used in nuclear power plants in the United States consist of three main parts: (1) a reactor, or pressure, vessel; (2) a core; and (3) a set of control rods. In addition, reactor operations depend upon two substances–moderators and coolants. The reactor, or pressure, vessel is a tanklike structure that encloses the other main parts of the reactor. The vessel has steel walls that are typically up to least 6 inches (15 centimeters) thick and capable of containing the high pressure exerted in a reactor. The core contains the nuclear fuel, in which the fission chain reaction occurs. The core sits in the lower half of the reactor vessel. A great many fuel assemblies stand upright in the core between an upper and lower support plate. Each fuel assembly contains a bundle of fuel rods. A fuel rod consists of pellets of fuel inside a metal tube. The pellet material is usually a powder called uranium dioxide. The tubing material is typically zircalloy, a mixture of the metal zirconium and one or more other metals. Neutrons can pass from the fuel through the tube walls, but most other nuclear particles cannot. The control rods are long metal rods that are used to regulate fission in the fuel. The control rods contain such neutron-absorbing materials as boron or cadmium. A mechanism outside the reactor vessel is attached to the rods. This mechanism inserts the rods into the core and withdraws them when necessary. When inserted fully into the core, the control rods absorb many neutrons and so prevent a fission chain reaction from occurring. To begin operation of the reactor, the control rods are partially withdrawn until a chain reaction occurs at a constant rate. To increase power in the reactor, the rods are withdrawn slightly more. Thus, fewer neutrons are absorbed, and more are available to cause fission. To stop the chain reaction, the rods are inserted all the way into the core to absorb most of the neutrons. The moderator is a substance that slows down neutrons as they pass through it. Slow neutrons are needed for fission. The moderator fills the space between the fuel rods in the fuel assemblies. It slows down neutrons as they pass from one fuel rod to another. The coolant is a liquid or gas that carries off the heat created by the fission chain reaction. The coolant circulates throughout the core. It carries the heat from the reactor to an energy conversion system. Thus, the coolant keeps the fuel and cladding from getting too hot, and it transfers energy to a place where electricity can be generated. All commercial power reactors in the United States are light water reactors. In these devices, light (ordinary) water serves as the moderator and the coolant. Canadian reactors are heavy water reactors. They use heavy water as the moderator and the coolant. Heavy water contains deuterium in place of ordinary hydrogen. For more information on reactors, see the section Research on new types of reactors in this article. Fuel preparation. After uranium ore has been mined, it goes through a long milling and refining process to separate the uranium from other elements in the ore. Light water absorbs more neutrons than do other types of moderators. The uranium used in light water reactors must therefore be enriched–that is, the percentage of U-235 must be increased. Neutrons then have a better chance of striking a U-235 nucleus. In the United States, uranium that has been separated from the ore is sent to an enrichment plant. Enrichment plants increase the proportion of U-235 in the uranium, depending on the intended use of the uranium. Most light water reactors use fuel with about 2 to 4 percent U-235. Each tube measures about 1/2 inch (13 millimeters) in diameter and 10 to 14 feet (3 to 5 meters) long. After a tube has been filled with uranium dioxide pellets, its ends are welded shut. These fuel rods are then fastened together into bundles of 30 to 300 each. Each bundle, or fuel assembly, weighs 300 to 1,500 pounds (140 to 680 kilograms). Commercial power reactors need 50 to 150 short tons (45 to 136 metric tons) of uranium dioxide. The amount depends on the size of the reactor Chain reactions. A reactor requires a certain minimum amount of fuel to keep up a chain reaction. This amount, called the critical mass, varies according to the design and size of the reactor. Reactors are designed to hold more than a critical mass of fuel to allow for fuel use during operation. The position of the control rods determines the effective mass of the fuel, the amount of fuel taking part in the chain reaction. If the effective mass is decreased below the critical mass, the chain reaction will die out and reactor power will decrease. If the effective mass is increased above the critical mass, the chain reaction will become more rapid and reactor power will increase. In an emergency, if the chain reaction became too rapid, the reactor could overheat. However, the control rods are available to slow down the chain reaction if it becomes too rapid. To prepare a reactor for operation, the fuel assemblies are loaded into the core with the control rods completely inserted. In a light water reactor, the water used as a moderator to slow down the neutrons fills the spaces between the fuel assemblies. The control rods are then slowly withdrawn, and a chain reaction begins. The farther the rods are withdrawn, the greater the rate of the reaction because fewer neutrons are absorbed. More neutrons thus are available to cause fission. When the desired power is reached, the control rods are positioned so that the effective mass is equal to the critical mass. The water in the core carries off the heat created by the chain reaction. To stop the reaction, the rods are again inserted all the way into the core to absorb most neutrons. Steam production. The light water reactors used by almost all U.S. nuclear plants are of two main types. One type, the pressurized water reactor, produces steam outside the reactor vessel. The other type, the boiling water reactor, makes steam inside the vessel. Most nuclear plants in the United States use pressurized water reactors. These reactors heat the moderator water in the core under extremely high pressure. The pressure allows the water to heat past its normal boiling point of 212 °F (100 °C) without actually boiling. The chain reaction heats the water to about 600 °F (316 °C). Pipes carry this extremely hot, though not boiling, water to steam generators outside the reactor. The steam generators transfer heat from the pressurized water to a separate supply of water that boils and so produces steam. In a boiling water reactor, the chain reaction boils the moderator-water in the core. Steam is therefore produced inside the reactor vessel. Pipes carry the steam from the reactor to the plant’s turbines. In producing electric energy, a nuclear plant’s steam turbines and electric generators work like those in a fossil-fuel plant. The steam produced by a reactor spins the blades of the plant’s turbines, which drive the generators. Many plants have combination turbines and generators called turbo generators. After steam has passed through a plant’s turbines, it is piped to a condenser. The condenser changes the steam back into water. A reactor can thus use the same water over and over. But a condenser requires a constant supply of fresh water to cool the steam. Most plants pump this water from a nearby river or lake. The water, which becomes warm as it passes through the condenser, is then pumped back into the river or lake. This warm wastewater may heat the water in the river or lake enough to endanger plants and animals that live there. For this reason, the discharge of the wastewater is sometimes called thermal pollution. To help solve the problem of thermal pollution, most new nuclear plants have cooling towers. Hot water from the steam condensers is moved through the towers in such a way that the heat passes into the atmosphere. The cooled water is returned to the steam condenser for reuse. Hazards and safeguards. An ordinary power reactor cannot explode like an atomic bomb. Only a greatly supercritical mass of plutonium 239 or of highly enriched uranium 235 can explode in this way. A supercritical mass contains more than the amount of plutonium or uranium required to sustain a chain reaction. The chief hazards of nuclear power production result from the great quantities of radioactive material that a reactor produces. These materials give off radiation in the form of alpha and beta particles and gamma rays. The reactor vessel is surrounded by thick concrete blocks called a shield, which normally prevents almost all radiation from escaping. Federal regulations limit the amount of radiation allowed from U.S. nuclear plants. Every plant has instruments that continually measure the radioactivity in and around the plant. They automatically set off an alarm if the radioactivity rises above a predetermined level. If necessary, the reactor is shut down. A plant’s routine safety measures greatly reduce the possibility of a serious accident. Nevertheless, every plant has emergency safety systems. Possible emergencies range from a break in a reactor water pipe to a leak of radiation from the reactor vessel. Any such emergency automatically activates a system that instantly shuts down the reactor, a process called scramming. The usual method of scramming is to insert the control rods rapidly into the core. A leak or break in a reactor water pipe could have dangerous consequences if it results in a loss of coolant. Even after a reactor has been shut down, the radioactive materials remaining in the reactor core can become so hot without sufficient coolant that the core melts. This condition, called a meltdown, could result in the release of dangerous amounts of radiation. In most cases, the large containment structure that houses a reactor would prevent radioactive material from escaping into the atmosphere. To prevent such an accident from occurring, all reactors are equipped with an emergency core cooling system, which automatically floods the core with water in case of a loss of coolant. Wastes and waste disposal. The fissioning of U-235 produces more neutrons than are needed to continue a chain reaction. Some of them combine with U-238 nuclei, which far outnumber U-235 nuclei in the reactor fuel. When U-238 captures a neutron, it is changed into U-239. The U-239 then decays into neptunium 239 (Np-239), which decays into plutonium 239 (Pu-239). This same process forms Pu-239 in a breeder reactor. Slow neutrons can fission Pu-239, as well as U-235. Some of the newly formed Pu-239 is thus fissioned during the fissioning of U-235. Even in small amounts, plutonium can cause cancer or genetic damage in human beings. Larger amounts can cause radiation sickness and death. Safe disposal of these wastes is one of the most difficult problems involved in nuclear power. Most nuclear plants need to replace their fuel assemblies only about once a year. The radioactive wastes generate heat, and so used fuel assemblies must be cooled after removal from a reactor. Nuclear plants cool the assemblies by storing them underwater in specially designed storage pools. In the United States, the federal government is working on guidelines for the safe and permanent disposal of nuclear wastes. The current U.S. plan calls for isolating long-lived radioactive waste from the environment in underground storage sites. A law passed by Congress in 1982 required the federal government to build two sites for nuclear wastes from commercial power plants. In 1987, the law was changed to require a single site. A storage site for nuclear waste must lie in a highly stable area that is free of earthquakes, faulting, and other geologic activity. The site must be dry so that the waste containers cannot be corroded and water supplies cannot be contaminated. The site also must be constructed so that future generations do not dig into it and release radioactivity. The government is studying the suitability of a location in Nevada. In the meantime, commercial nuclear power plants in the United States continue to store used fuel assemblies and other wastes in pools of water on the plant grounds. Other countries, including Japan, Russia, and the United Kingdom, are pursuing a reprocessing plan. Under this plan, nuclear plants would ship their used fuel assemblies to the reprocessing plants for removal of Pu-239 and unused U-235. These radioactive isotopes would then be recycled into fuel for nuclear reactors. However, this method would leave radioactive isotopes in the chemical solutions used for reprocessing. These solutions would have to be changed into a solid form that could be safely stored. In every country that has a nuclear energy industry, the government plays a role in the industry. But the government’s role varies greatly among countries. This section deals mainly with the U.S. and Canadian nuclear energy industries. Organization of the industry. Private utility companies own most of the nuclear power plants in the United States. The rest are publicly owned. Private companies also manufacture reactors, mine uranium, and handle most other aspects of U.S. nuclear power production. Canada’s nuclear power plants are all publicly owned. Atomic Energy of Canada Limited (AECL), a government corporation, has overall responsibility for the country’s nuclear research and development program. AECL also designs the CANDU (CANada Deuterium oxide-Uranium) heavy water reactors used by all Canadian nuclear plants. Private companies make the various reactor parts and mine and process the country’s uranium. Canada has no uranium enrichment plants because CANDU reactors operate with unenriched uranium fuel. The industry and the economy. The main economic advantage of nuclear power plants is that this fuel is less expensive than fossil fuels. But nuclear plants cost somewhat more to build than do fossil-fuel plants. Under normal economic conditions, a nuclear plant’s savings in fuel eventually make up for its higher construction expenses. At first, these expenses add to the cost of producing electricity. But after some years, a plant will have paid off its construction costs. It can then produce electricity more cheaply than a fossil-fuel plant can. But two main problems–sharply higher costs and equipment failures–have somewhat lessened this long-run economic advantage of nuclear power plants. Many nuclear plants in the United States have had to shut down for months at a time because of equipment failures. Such losses of operating time further add to the cost of producing electricity. The industry and the environment. Unlike fossil-fuel plants, nuclear plants do not release solid or chemical pollutants into the atmosphere. A nuclear plant releases small amounts of radioactive gas into the air. In addition, the cooling water used in pressurized water plants picks up a small amount of radioactive tritium in the steam condenser. The tritium remains in this water when it is returned to a river or lake. But these small amounts of radiation released into the environment are not believed to be harmful. Thermal pollution remains a problem at some nuclear plants. But cooling towers help correct this problem. In a small number of nuclear accidents, hazardous amounts of radiation have been released into the atmosphere. Accidental releases of radioactive substances have occurred in Russia, the United States, and the United Kingdom; and an especially serious accident occurred in 1986 at the Chernobyl nuclear power plant in Ukraine (then part of the Soviet Union). The subsection Hazards and safeguards that appears earlier in this article discusses the main methods of guarding against accidents. Critics of nuclear power also fear another danger to the environment. As power production increases, the creation of high-level radioactive wastes also increases. The United States has no permanent storage place for such wastes. The problem of storing radioactive wastes is discussed in the subsection Wastes and waste disposal. Government regulation. The Nuclear Regulatory Commission (NRC), an agency of the federal government, regulates nonmilitary nuclear power production in the United States. One of the NRC’s main duties is to ensure that nuclear power plants operate safely, and it makes and enforces a variety of safety standards. Every nuclear reactor and power plant must be inspected and licensed by the NRC before it may begin operations. The NRC also supervises the manufacture and distribution of nuclear fuels, and controls the disposal of radioactive wastes from commercial production. The Atomic Energy Control Board, a Canadian government agency, regulates Canada’s nuclear energy industry. The board’s duties resemble those of the Nuclear Regulatory Commission. Careers in nuclear energy cover a wide range of occupations and require widely varying amounts of training. A high percentage of the jobs require a college degree or extensive technical education. Many of these jobs are in large research laboratories, which work to improve nuclear processes and to lessen their hazards. Other careers requiring advanced training are in such areas as uranium mining and processing, reactor manufacturing and inspection, power plant operation, and government regulation. In 1972, scientists discovered that a natural chain reaction had released nuclear energy nearly 2 billion years ago in a uranium deposit in west-central Africa. Two billion years ago, there had been so little radioactive decay that the ore contained enough U-235 for a chain reaction. An accumulation of ground water acted as a moderator to begin the reaction. As heat from the reaction changed the water into steam, less and less water was available to serve as a moderator and the reaction died out. Except for such rare natural occurrences, nuclear energy was not released on a large scale on the earth until 1942. That year, scientists produced the first artificially created chain reaction. Scientific discoveries that took place within the last 100 years led to the large-scale release of nuclear energy. Early developments Before the late 1800’s, scientists did not suspect that atoms could release nuclear energy. Then in 1896, the French physicist Antoine Henri Becquerel found that uranium constantly gives off energy in the form of invisible rays. He thus became the discoverer of radioactivity. Other scientists soon began experiments to learn more about this mysterious phenomenon. The beginning of nuclear physics. In 1898, the great British physicist Ernest Rutherford identified two kinds of radioactive “rays,” which he called alpha rays and beta rays. He and other researchers later showed that these rays are actually high-energy particles, which became known as alpha and beta particles. Experiments with these particles then led Rutherford to discover the atom’s nucleus. This achievement, which Rutherford announced in 1911, marked the beginning of a new science–nuclear physics. About 1914, scientists began doing experiments to see what happens when nuclear particles collide. The experimenters used alpha particles from naturally radioactive materials to bombard the nuclei of light atoms. Light nuclei do not repel positively charged particles, such as alpha particles, as strongly as heavy nuclei do. Rutherford used this method to produce the first artificial transmutations in a series of experiments from 1917 to 1919. He bombarded nitrogen atoms with alpha particles. In rare collisions, a nitrogen 14 nucleus absorbed an alpha particle (a helium 4 nucleus). At the same time, the alpha particle pushed a proton out of the nitrogen nucleus. The nucleus thereby became an oxygen 17 nucleus. Artificial fission. To produce nuclear reactions in heavy nuclei, scientists needed a particle that heavy nuclei would not repel. In 1932, the British physicist James Chadwick discovered such a particle–the neutron. In 1938, two German radiochemists, Otto Hahn and Fritz Strassmann, reported they had produced the element barium by bombarding uranium with neutrons. At first, scientists could not explain how uranium had produced barium, which is much lighter than uranium. All previous transmutations had resulted in an element about as heavy as the original one. Then in 1939, the Austrian physicist Lise Meitner and her nephew Otto Frisch showed that Hahn and Strassman had in fact produced the first known artificial fission reaction. A uranium nucleus had split into two nearly equal fragments, one of which consisted of a barium nucleus. Two neutrons were also emitted. The other fragment consisted of a nucleus of krypton, a somewhat lighter element than barium. These two nuclei, together with the emitted neutrons, are lighter than a uranium nucleus and a neutron. The reaction had therefore produced more energy than it consumed. Scientists soon realized that if many uranium nuclei could be made to fission, a tremendous amount of energy would be released. The amount of energy could be calculated from a theory developed by the great German-born physicist Albert Einstein in 1905. The theory shows that matter can change into energy and that matter and energy are related by the equation E equals m times c-squared. This equation states that the energy (E) into which a given amount of matter can change equals the mass (m) of that matter multiplied by the speed of light squared (c-squared). The speed of light squared is obtained by multiplying the speed of light by itself. Using this equation, scientists determined that the fissioning of 1 pound (0.45 kilogram) of uranium would release as much energy as 8,000 short tons (7,300 metric tons) of TNT. Uranium could therefore be used to make a powerful bomb. The beginning of the nuclear age The development of nuclear weapons. World War II broke out in Europe in September 1939. The month before, Einstein had written to U.S. President Franklin D. Roosevelt urging him to commit the United States to developing an atomic bomb. Einstein had fled to the United States from Germany to escape Nazi persecution. He warned Roosevelt that German scientists might already be working on a nuclear bomb. Roosevelt acted on Einstein’s urging, and early in 1940 scientists received the first funds for uranium research in the United States. The United States entered World War II in 1941. The government then ordered an all-out effort to build an atomic bomb and in 1942 established the top-secret Manhattan Project to achieve this goal. A group of scientists at the University of Chicago had charge of producing plutonium for the Manhattan Project. The group included such noted physicists as Enrico Fermi, Leo Szilard, and Eugene Wigner, all of whom had been born in Europe and had settled in the United States. Fermi headed the group. Under the scientists’ direction, workers built an atomic pile, or reactor, beneath the stands of the university athletic field. The pile consisted of 50 short tons (45 metric tons) of natural uranium oxide and uranium embedded in 500 short tons (450 metric tons) of graphite. The graphite served as a moderator. The pile was designed to demonstrate a controlled nuclear chain reaction in the uranium. Cadmium rods controlled the reaction. On Dec. 2, 1942, this reactor produced the first artificial chain reaction. The success of the University of Chicago project led the U.S. government to build a plutonium-producing plant in Hanford, Wash. The government also built a uranium enrichment plant in Oak Ridge, Tenn. Plutonium and greatly enriched uranium from these plants were used in the two atomic bombs that the United States dropped on Japan in August 1945. After World War II, scientists began work on developing a hydrogen bomb. The United States exploded the first hydrogen bomb in 1952 and so achieved the world’s first large-scale thermonuclear reaction But the AEC became responsible for regulating the nuclear energy industry. It also kept control in such areas as uranium enrichment and waste disposal. The United States made the world’s first full-scale use of controlled nuclear energy in 1954. That year, the U.S. Navy launched the first nuclear-powered vessel, the submarine Nautilus. The world’s first full-scale nuclear power plant began operations in 1956 at Calder Hall in northwestern England. In 1957, the first large-scale nuclear plant in the United States opened in Shippingport, Pa. It supplied electricity to the Pittsburgh area until 1982, when the plant was closed. Canada opened its first full-scale plant in 1962 at Rolphton, Ont. The successful start of the nuclear power industry convinced world leaders of the need for international cooperation in the field. In 1957, the United Nations (UN) established the International Atomic Energy Agency to promote the peaceful uses of nuclear energy. Also in 1957, Belgium, France, Italy, Luxembourg, the Netherlands, and West Germany formed the European Atomic Energy Community (Euratom). The organization encourages the development of nuclear power among its member countries. Denmark, the United Kingdom, and Ireland joined Euratom in 1973. The spread of nuclear capability During the 1960’s and early 1970’s, a number of countries acquired reactors and used them to start nuclear power development. Progress was also made during this period toward limiting nuclear weapons tests and stopping the spread of nuclear weapons. In 1970, for example, a nuclear nonproliferation treaty went into effect. The treaty prohibits the nuclear powers that have agreed to abide by the document from giving nuclear weapons to nations that do not already have them. The nonproliferation treaty also prohibits nations without nuclear weapons from acquiring them. But the nonproliferation treaty does not prohibit nations from selling or buying nuclear reactors. A reactor can be used not only for peaceful purposes but also to produce plutonium for nuclear weapons. India used a research reactor for this purpose and in 1974 exploded its first atomic bomb. Canada had supplied the reactor to India with the understanding it would be used for peaceful purposes only. Canada has signed the nonproliferation treaty, but India has not. Critics of India’s action question the wisdom of supplying reactors to countries that do not already have them. Meanwhile, the United States had been greatly increasing its nuclear power capacity. But opposition to nuclear power development also increased in the United States during the late 1960’s and early 1970’s. Critics began to question nearly every aspect of nuclear power production, from the cost of uranium enrichment to the problems of waste disposal. Many critics of the United States nuclear program charged that the government overlooked various safety risks at nuclear plants to promote nuclear power development. Partly as a result of such criticism, Congress disbanded the Atomic Energy Commission (AEC) in 1974 and divided its functions between two newly formed agencies. The Energy Research and Development Administration (ERDA) took over the AEC’s development programs. The Nuclear Regulatory Commission (NRC) took over its regulatory duties. The NRC, it was believed, could better regulate the industry if it was not also responsible for the industry’s growth and development. In 1977, Congress abolished ERDA and transferred its responsibilities to the newly created Department of Energy. Safety concerns There have been a number of accidents at nuclear power plants. Most of them have not been serious. However, in 1957, a fire at the Windscale plutonium production plant in northern England resulted in the release of a large quantity of radioactivity. The British government banned the sale of milk from cows in that part of England for more than a month after the fire. In the United States, concerns about the safety of nuclear reactors increased after a serious accident in 1979 at the Three Mile Island nuclear power plant near Harrisburg, Pennsylvania. Mechanical and human failures resulted in a breakdown of the reactor’s cooling system and the destruction of the reactor core. Scientists and technicians prevented a failure of the reactor vessel that might have released large amounts of radioactive isotopes into the reactor containment building. Cleanup of the plant was completed in the early 1990’s. The worst nuclear accident in history occurred in 1986 at the Chernobyl nuclear power plant near Kiev in Ukraine, which was then part of the Soviet Union. An explosion and fire ripped apart the reactor and released large amounts of radioactive isotopes into the atmosphere. Unlike most Western reactors, the Chernobyl reactors lacked an enclosure to prevent radioactive isotopes from escaping. Soviet officials reported that 31 people died from radiation sickness or burns and more than 200 others were seriously injured. The radioactive substances spread over parts of what are now Ukraine, Russia, and Belarus, and were carried by wind into northern and central Europe. Experts expected a significant increase in the number of cancer deaths among those near the reactor. But they predicted that the health effects outside the Chernobyl area would be slight. As a result of the accidents at Three Mile Island and Chernobyl, opposition to nuclear power increased in many countries during the late 1980’s. In the United States, the NRC tightened its control of nuclear plants. Experts have expressed particular concern over the safety of older Soviet-designed reactors now operating in Russia, Ukraine, and several countries of the former Soviet bloc. Western scientists and engineers are helping to remedy some of the most urgent safety problems in these reactors. As the nuclear power industry has continued to develop, many improvements in plant equipment and operation have increased safety. Nonetheless, some experts insist that the next generation of reactors should take greater advantage of design features that rely less–or not at all–on mechanical equipment such as pumps and valves to remove heat if an accident occurs. Some of these reactors are known as passively safe reactors.



The Physics of Scuba Diving

Monday May 19, 2008

Swimming with the Fish….

Have you ever wondered what it would be like to swim with the fish and explore the underwater jungle that covers two-thirds of the earth’s surface? I have always been interested in water activities; swimming, diving and skiing, and I felt that scuba was for me. My first dive took place while on a family vacation. I came across a dive shop offering introductory dives, which immediately caught my interest. After much convincing (my parents), with my solemn assurance that I would be careful, I was allowed to participate in a dive. I was ready, or so I thought. The slim basics such as breathing were explained and I was literally tossed in. Sounds easy enough, right!, well WRONG!!. From the moment I hit the water, my experience was much less than fun. I quickly sank to the bottom into a new world, with unfamiliar dangers. I really wasn’t ready for this experience. I was disorientated, causing me to panic, which shortened the length of my dive, not to mention my air supply. Let’s just say I would not do that again.

To start exploring the underwater world, one must first master a few skills. Certification is the first step of learning to dive. From qualified professionals one must learn how to use the equipment, safety precautions, and the best places to dive. This paper is designed to help give a general understanding of the sport and the importance that physics plays in it.

Self-contained Underwater Breathing Apparatus, or SCUBA for short, is a hell of a lot of fun. However, there is considerably more to Diving than just putting on a wetsuit and strapping some compressed air onto ones back. As I quickly learned, diving safely requires quite a bit more in terms of time, effort, and preparation. When one goes underwater, a diver is introduced to a new and unfamiliar world, where many dangers exist, but can be avoided with proper lessons and understanding. With this knowledge the water is ours to discover.

The Evolution of Scuba Diving

Divers have penetrated the oceans through the centuries for the purpose of acquiring food, searching for treasure, carrying out military operations, performing scientific research and exploration, and enjoying the aquatic environment. Bachrach (1982) identified the following five principal periods in the history of diving which are currently in use. Free (or breath-hold) diving, bell diving, surface support or helmet (hard hat) diving, scuba diving, and, saturation diving or atmospheric diving (Ketels, 4)

SCUBA DIVING

The development of self-contained underwater breathing apparatus provided the free moving diver with a portable air supply which, although finite in comparison with the unlimited air supply available to the helmet diver, allowed for mobility. Scuba diving is the most frequently used mode in recreational diving and, in various forms, is also widely used to perform underwater work for military, scientific, and commercial purposes.

There were many steps in the development of a successful self-contained underwater system. In 1808, Freiderich yon Drieberg invented a bellows-in-a-box device that was worn on the diver’s back and delivered compressed air from the surface. This device, named Triton, did not actually work but served to suggest that compressed air could be used in diving, an idea initially conceived of by Halley in 1716. (Ketels, 9)

In 1865, two French inventors, Rouquayrol and Denayrouse, developed a suit that

they described as ’self-contained.’ In fact, their suit was not self contained but consisted of a helmet-using surface-supported system that had an air reservoir that was carried on the diver’s back and was sufficient to provide one breathing cycle on demand. The demand valve regulator was used with surface supply largely because tanks of adequate strength were not yet available to handle air at high pressure. This system’s demand valve, which was automatically controlled, represented a major breakthrough because it permitted the diver to have a breath of air when needed.

The Rouquayrol and Denayrouse apparatus was described with remarkable accuracy in Jules Verne’s classic, Twenty Thousand Leagues Under The Sea, which was written in 1869, only 4 years after the inventors had made their device public (Ketels, 10).

Semi-Self-Contained Diving Suit

The demand valve played a critical part in the later development of one form of scuba apparatus. In the 1920’s, a French naval officer, Captain Yves Le Prieur, began work on a self-contained air diving apparatus that resulted in 1926 in the award of a patent, shared with his countryman Fernez. This device was a steel cylinder containing compressed air that was worn on the diver’s back and had an air hose connected to a mouthpiece. The diver wore a nose clip and air-tight goggles that undoubtedly were protective and an aid to vision but did not permit pressure equalization.

The major problem with Le Prieur’s apparatus was the lack of a demand valve, which necessitated a continuous flow (and thus waste) of gas. In 1943, almost 20 years after Fernez and Le Prieur patented their apparatus, two other French inventors, Emile Gagnan and Captain Jacques-Yves Cousteau, demonstrated their ‘Aqua Lung.’

This apparatus used a demand intake valve drawing from two or three cylinders, each containing over 2500 psig. Thus it was that the demand regulator, invented over 70 years earlier by Rouquayrol and Denayrouse and extensively used in aviation, came into use in a self-contained breathing apparatus which did not emit a wasteful flow of air during inhalation (although it continued to lose exhaled gas into the water). This application made possible the development of modern open-circuit air scuba gear (Ketels,11).

In 1939, Dr. Christian Lambertsen began the development of a series of three patented forms of oxygen rebreathing equipment for neutral buoyancy underwater swimming. This became the first self-contained underwater breathing apparatus successfully used by a large number of divers. The Lambertsen Amphibious Respiratory Unit (LARU) formed the basis for the establishment of U.S. military self-contained diving. This apparatus was designated scuba (for self-contained underwater breathing apparatus) by its users. Equivalent self-contained apparatus was used by the military forces of Italy, the United States, and Great Britain during World War II and continues in active use today. (Ketels, 12).

A major development in regard to mobility in diving occurred in France during the 1930’s: Commander de Carlieu developed a set of swim fins, the first to be produced since Borelli designed a pair of claw-like fins in 1680. When used with Le Prieur’s tanks, goggles, and nose clip, de Carlieu’s fins enabled divers to move horizontally through the water like true swimmers, instead of being lowered vertically in a diving bell or in hard-hat gear. The later use of a single-lens face mask, which allowed better visibility as well as pressure equalization, also increased the comfort and depth range of diving equipment (Tillman, 27).

Thus the development of scuba added a major working tool to the systems available to divers. The new mode allowed divers greater freedom of movement and access to greater depths for extended times and required much less burdensome support equipment. Scuba also enriched the world of sport diving by permitting recreational divers to go beyond goggles and breath-hold diving to more extended dives at greater depths.

The physics of Scuba Diving

Upon entering the underwater world, one notices new and different sensations as one ventures into a realm where everything looks, sounds and feels different than it does above the water. These sensations are part of what makes diving so special.

Understanding why the underwater world is different helps you adapt and become accustomed to the changes. In the following pages I will attempt to explain two factors that greatly affect a diver under water: buoyancy and pressure.

Have you ever wondered why a large steel ocean liner floats, but a small steel nail sinks? The answer is surprisingly simple. The steel hull of the ship is formed in a shape that displaces much water. If the steel used to manufacture the ocean liner were placed in the sea without being shaped into a large hull, it would sink like the nail. The ocean liner demonstrates that whether an object floats depends not only on its weight, but on how much water it displaces (Ascher, 51).

The principle of buoyancy can be simplified this way: An object placed in water is buoyed up by the force equal to the weight of the quantity of water it displaces. The principle of buoyancy is that if an object displaces an amount of water weighing more than its own weight, it will float. If an object displaces an amount of water weighing less than its own weight then it will sink. If an object displaces an amount of water equal to its own weight it will neither float nor sink, but remain suspended. If an object floats, it is said to be positively buoyant; if it sinks, it is negatively buoyant; and if it neither floats nor sinks, it is neutrally buoyant (Kolezer, 16).

It is important for a diver to learn to use these principles of buoyancy so that the diver can effortlessly maintain his/her position in the water. One must control buoyancy carefully. When you are at the surface, you will want to be positively buoyant so that you could conserve energy while resting or swimming. Under water, you will want to be neutrally buoyant so that you are weightless and can stay off the bottom and avoid crushing or damaging delicate corals and other aquatic life. Neutral buoyancy permits a diver to move freely in all directions (Kolezer, 17).

Buoyancy control is one of the most important skills that a diver could master, but it is also one of the easiest. A diver, controls his/her buoyancy using lead weight and a buoyancy control device (BCD). The lead weight, which is incorporated into a weight system, such as a weight belt is negatively buoyant. The BCD is a device that can be partially inflated or deflated to control buoyancy (Kolezer, 19).

Another factor that affects the buoyancy of an object is the density of water. The denser the water, the greater the buoyancy. Salt water (due to its dissolved salts) is more dense than fresh water, so you’ll be more buoyant in salt water than in fresh water - in fact, when floating motionless at the surface, most divers need to exhale air from their lungs to sink. By exhaling, the volume of the lungs is decreased, and less water is displaced, resulting in less buoyancy (Kolezer, 19).

Thus, we can see, that changing the volume of an object changes its buoyancy. Divers primarily control buoyancy by changing the volume of air in their BCD’s.

Body air spaces and water pressure

Although usually not noticeable, air is constantly exerting pressure on us. An example being as simplified as when walking against a strong wind, what is actually felt its force pushing against our body. This demonstrates that air can exert pressure, or weight. One doesn’t usually feel the air’s pressure because our body is primarily liquid, distributing the pressure equally throughout our entire body. The few air spaces in our body are- in the ears, sinuses and lungs- These are filled with air equal in pressure to the external air. However, when the surrounding air pressure changes, such as when you change altitude by flying or driving through mountains, some of us can feel the change as a popping sensation in our ears (Tillman, 40).

Just as air exerts pressure on us at the surface, water exerts pressure when a person is submerged. Because water is much denser than air, pressure changes under water occur more rapidly, making one more aware of them.

The weight of the water above a person greatly compounds the amount of pressure one (ears, lungs, and the air in ones lungs) is under. While it takes the entire height of the atmosphere to contain a weight of air enough to give 1 atmosphere (1 ATM) of pressure (the pressure one is used to be under as one walks around daily), it only takes 33 ft. of water to make up an additional ATM of pressure. Of course, the air is still there too, so at a depth of 33 feet, a diver is subjected to two Atmospheres of pressure, fully twice what one is subjected to at the surface! (Resneck, 53)

A diver would have to go really, really deep before being in any danger of actually being crushed by pressure. It’s what the pressure does to the gases in your body that can be dangerous. Physics teaches us Boyle’s Law of gases, which suggests that the volume of a gas is proportional to its pressure. Thus, when one goes to a depth of, say, 33 feet (1 extra ATM) and fills ones lungs with a breath of air from a tank and then ascend to the surface without exhaling, the air in the lungs would expand to twice its volume, causing massive trauma to the lungs. Other more subtle problems occur with gas under pressure, such as the accumulation of residual nitrogen in the body’s tissues which can result in Decompression Sickness (DCS), commonly known as the bends (Tillman, 44).

As with air pressure, one doesn’t feel water pressure on most of ones body, but we can feel it in our body’s air spaces. When water pressure changes corresponding with a change in depth, it creates a pressure sensation one can feel. Through training and experience a diver will learn to avoid the problems associated with water pressure and the air spaces in our bodies.

As previously mentioned, pressure increases at a rate of one atmosphere (ATM) for each additional 33 feet of depth underwater. The total pressure is twice as great at 33 feet than at the surface, three times as great at 66 feet, and so on. This pressure pushes in on flexible air spaces, compressing them and reducing their volume. The reduction of the volume of the air spaces is proportional to the amount of pressure placed upon it.

When the total pressure doubles, the air volume is halved. When the pressure triples, the volume is reduced to one third, and so on (Tillman, 40).

The density of air in the air spaces is also affected by pressure. As the volume of the air spaces is reduced due to compression, the density of the air increases as it is squeezed into a smaller place. No air is lost; it is simply compressed. Air density is also proportional to pressure, so that when the total pressure is doubled, the air density is doubled. When the pressure is tripled the air density triples and so on.

To maintain an air space as its original volume when pressure is increased, more air must be added to the space. This is the concept of pressure equalization, and the amount of air that must be added is proportional to the pressure increased.

Air within an airspace expands as pressure is reduced. If no air has been added to the air space, the air will simply expand to fill the original volume of the air space upon reaching the surface (Ketels, 76).

If air has been added to an air space to equalize the pressure, this air will expand as pressure is reduced during ascent. The amount of expansion is again proportional to the pressure. In an open container, such as the bucket, the expanding air will simply bubble out of the opening, maintaining it original volume during ascent. In a closed flexible container, however, the volume will increase as the pressure is reduced. If the volume exceeds the capacity of the container, the container may be ruptured by the expanding air (Cramer, 51).

Now let’s take a look at how the relationship between pressure volume and density affect a diver while diving. Previously it has been mentioned that air spaces are effected by changes in pressure. The air spaces that a diver is concerned about are both the natural ones in your body and those artificially created by wearing diving equipment.

The air spaces within a diver’s body that are most obviously affected by increasing pressure are found in the ears and sinuses. The artificial air spaces most affected by increasing pressure is the one created by a divers mask.

During descent, water pressure increases and pushes in your body’s air spaces, compressing them. If pressure within these air spaces is not kept in balance with this increasing water pressure, the sensation of pressure builds, becoming uncomfortable and possibly even painful as the diver continues to descend. This sensation is the result of a squeeze on the air spaces. A squeeze is not only a scuba phenomena but may also be experienced in a swimmers ears when diving to the bottom of a swimming pool. A squeeze, then is a pressure imbalance resulting in a pain or discomfort in a bodies air space. In this situation, the imbalance is such that the pressure outside the air space is greater than the pressure inside (Ketels, 76-77).

Squeezes are possible in several places: ears, sinuses, teeth, lungs and ones mask. Fortunately, divers can easily avoid all these squeezes.

To avoid discomfort, pressure inside an air space must always equal the water pressure outside the air spaces. This is accomplished by adding air to the air spaces during descent, before discomfort occurs. This is called equalization.

Compared to the ear and sinus air spaces, the lungs are large and flexible. As a scuba diver, one automatically equalizes the pressure in the lungs by continuously breathing from the scuba equipment. When you skin dive, holding ones breath, the lungs can be compressed with no consequence as long as they are filled with air when one begins to descent. The lungs will be reduced in volume during decent and will re-expand during ascent to nearly the original volume when one reaches the surface (some of the air from the lungs is used to equalize the other body air spaces) (Ketels, 78).

In a healthy diver, blocking the nose and attempting to gently blow through it with the mouth closed will direct air into the ear and sinus air spaces. Swallowing and wiggling the jaw from side to side may be an effective equalization technique. Some divers even attempt a combination of the previous two methods.

As mentioned previously along with squeezes, the lungs experience no harmful effects from the changes in pressure when holding ones breath while skin diving. At the start of the skin dive, one takes a breath and descends; the increasing water pressure compresses the air in the lungs. During ascent, the air re-expands so that when reaching the surface, the lungs return to their original volume (Ketels, 78).

When scuba diving, however, the situation is different. Scuba equipment allows one to breathe under water by automatically delivering the air at a pressure equal to the surrounding water pressure. This means the lungs will be at their normal volume while at depth, full of air that will expand on ascent (Cramer, 51).

If a diver breaths normally, keeping the airway to you lungs open, the expanding air escapes during ascent and your lungs remain at their normal volume. But, by holding ones breath and then blocking the airway while ascending the lungs would over expand, much like the sealed bag. Expanding air can cause lung over-pressurization (lung rupture), the most serious injury that can occur to a diver. The most important rule in scuba diving is to breath continuously and never hold your Breath. Lung rupture will occur unless pressure is continuously equalized by breathing normally at all times (Cramer, 52).

Other physical Phenomena’s

As an air-breathing creature, we have evolved to live on land. Above the water, we see, hear and move about in a familiar and comfortable manner that seems normal because we have adapted to an air environment.

Under water, though, one enters a new world, where seeing, hearing, staying warm and moving are different. This is because water is 800 times more dense than air, affecting light, sound and heat in ways that we aren’t used to.

Sight seeing is a big part of what diving is all about. One dives for numerous reasons. A primary purpose is to see new environments, aquatic life and natural phenomena. Since underwater sight seeing is important, like buying a new camera, one must learn, how. Therefor when diving, one must know how the liquid environment affects vision.

To see clearly under water, a mask is needed because the human eye cannot focus without any air space in front of it. A mask provides the air space. Without the mask, you can see large objects, but they will be blurred and indistinct because your eyes cannot bring the rays of light into sharp focus. Only by wearing a mask can you see sharply (Ascher, 9).

Light travels at a different speed in water than in air. When light enters the air in your mask from the water, the change in speed causes its angle of travel to shift slightly. This causes a magnificent effect that makes objects under water appear 25% larger and closer (Ascher, 52).

Water has other effects on light. As you descend, there is less light. This is due to several facts: some light reflects off the water’s surface, some is scattered by particles in the water, and some is absorbed by the water itself. However, water does not absorb light uniformly.

White light, such as sunlight, is actually composed of various colors mixed together. The colors are absorbed one by one as depth increases: First red, followed by orange and yellow. Since each color is part of the total light entering the water, less light remains as depth increases and each color is absorbed. For these reason, deeper water is darker and less colorful. To see true colors, divers sometimes carry underwater lights with them (Resneck, 151).

Underwater Hearing

The underwater world is not a silent world. One can hear many new and interesting sounds, like snapping shrimp, grunting fish, and boat engines passing in the distance. Since sound travels farther in water than in air, one is able to hear things over much longer distances.

Sound also travels about four times faster in water than in air and because of this, one may have trouble determining the direction a sound is coming from (Cramer, 95).

Speech is virtually impossible under water because ones vocal cords do not work in a liquid environment, not to mention the addition of the tube in ones mouth. Communication by sound is usually limited to attracting the attention of another diver by rapping on the tank with a solid object, such as a knife. The diver will hear the rapping, but may not be able to tell where the sound is coming from.

Heat loss in water.

Diving stops being enjoyable when the diver gets cold. In fact, even a small loss of body heat has the potential to be a serious health threat. For these reasons, understanding about heat loss is important.

In air, body heat is lost as it rises from the skin into the air, as it is carried away by air currents, or as perspiration cools the skin through evaporation. Water conducts heat away from your body twenty times faster than air does, meaning that for a given temperature, water has a far greater cooling effect. Even seemingly warm 86F water can become chilly after a while (Cramer, 91).

The loss of body heat in water can quickly lead to a serious condition unless you use insulation to reduce the heat loss. Insulation through the use of exposure suits is recommended for diving in water 75F or colder. Just as one dresses according to the temperature and conditions to go outdoors, one must dress appropriately for diving.

Motion in water

One of the best aspects of diving is that it can be so relaxing. There’s little reason for hurrying. By learning how to move without breathlessness, cramping or fatigue, you learn to relax during a dive.

Due to the greater density of water, resistance to movement in water is much greater than in air. If you’ve ever tried to run waist-deep water, you’ve experienced this. In overcoming this increased resistance while diving, the best way to conserve energy is to move slowly and steadily. Avoid rapid and jerky movements that waste energy. Simply take your time. After all this is a sport to enjoy.

Conclusion

Several months after my vacation, I decided to give scuba diving a second chance. However, this time I decided to do it right. I signed up to take a P.A.D.I. certification, which is one of the many internationally recognized scuba associations. It was here, in a properly structured course, consisting of both theoretical and practical (in water) sessions where I was properly re-introduced to the sport.

Since my introductory dive from hell, I have had the chance to become quite the scuba enthusiast. Partaking in numerous dives not only in warmer climates (preferably) but in the colder Montreal waters as well, scuba diving has become part of my lifestyle. I participate in and enjoy every opportunity to re-visit the underwater world that once scared me away.

In this paper, I included some history of the evolution of the sport in order to point out that there is more to this particular sport than jumping into the water. Scuba is a complex sport and can not be enjoyed without some scientific knowledge. Scuba diving did not simply evolve, but it is the result of numerous inventions and physical properties. One could only imagine the difficulty that those historic divers (scientists) had in creating this sport.

My objective in writing this paper was not to deter people away from the sport, but to stress the importance of the knowledge that is required to properly and safely partake in it. Like everything else in life, one must work towards a goal, and this is no different. One will quickly see that the payoff is far greater than anything else ever experienced. Recreational scuba is meant to be a very enjoyable and relaxing sport. The scenery is magnificent and the sensations are truly indescribable.

Today, scuba diving is quickly becoming one of the expanding trades. Whether for military, research, business, or recreation, hundreds of thousands of people are heading for the depths, to experience the unknown. My advice for a new diver is to do it right. Get the proper certification and make each dive a safe one.

When a diver is fully trained, and in good mental and physical condition, safe diving can be one of the most enjoyable of experiences. The true beauty of the underwater world, coupled with the marvelous almost-weightlessness of floating with neutral buoyancy is an indescribable experience.

Bibliography/Further Reading

Ascher, Scott M. Scuba Handbook for Humans. Iowa : Kendall/Hunt Publishing Company. 1975.

Cramer, John L. Ph.D. Skin and Scuba Diving: Scientific Principles and Techniques. N.Y.: Bergwall Productions, Inc. 1975.

Ketels, Henry & McDowell, Jack. Safe Skin and Scuba Diving, adventure in the underwater world. Canada : Little, Brown and Company (Canada) Ltd. 1975.

Koelzer, William. Scuba Diving, How to get started. Pennsylvania :Chilton Book Company. 1976.

Resneck, John Jr. Scuba, Safe and Simple. New Jersey : Prentice-Hall, Inc. 1975.

Tillman, Albert A. Skin and Scuba Diving. Iowa : Wm. C. Brown Company Publishers. 1966.