EExplainingxplaining CCryogenicsryogenics Cryogenics Cryogenics is the science of producing and studying low-temperature conditions. Th e word cryogenics comes from the Greek word cryos, meaning “cold,” combined with a shortened form of the English verb “to generate.” It has come to mean the generation of temperatures well below those of normal human experience. More specifi cally, a low-temperature environment is termed a cryogenic environment when the temperature range is below the point at which permanent gases begin to liquefy. Permanent gases are elements that normally exist in the gaseous state and were once believed impossible to liquefy. Among others, they include oxygen, nitrogen, hydrogen, and helium. Th e origin of cryogenics as a scientifi c discipline coincided with the discovery by nineteenth-century scientists that the permanent gases can be liquefi ed at exceedingly low temperatures. Consequently, the term “cryogenic” applies to temperatures from approximately −100°C (−148°F) down to absolute zero (the coldest point a material could reach). Th e temperature of any material—solid, liquid, or gas—is a measure of the energy it contains. Th at energy is due to various forms of motion among the atoms or molecules of which the material is made. A gas that consists of very rapidly moving molecules, for example, has a higher temperature than one with molecules that are moving more slowly. In 1848, English physicist William Th omson (later known as Lord Kelvin; 1824–1907) pointed out the possibility of having a material in which particles had ceased all forms of motion. Th e absence of all forms of motion would result in a complete absence of heat and temperature. Th omson defi ned that condition as absolute zero. Words to Know Absolute zero = Th e lowest temperature possible at which all molecular motion ceases. It is equal to −273°C (−459°F). Cryogenics = the science which involves very low temperatures, usually regarded as below -150F (-100C). Liquid Nitrogen, Oxygen, Argon, Helium and Hydrogen are all cryogenic. Cryo-Treating = the treatment of metals and other materials at very low (-300F) temperatures, resulting in certain property changes Cryonics = Th e practice of freezing humans who are not curable by current medical technology, in the hope that ways may be found to bring them back to life at some future time when ways of repairing the damage caused by the freezing process have been developed, as well as cures for the diseases or other causes of death which necessitated their cryonics suspension. Dew Point = the temperature at which liquid fi rst condenses when a vapor is cooled Kelvin temperature scale = A temperature scale based on absolute zero with a unit, called the kelvin, having the same size as a Celsius degree. Liquefi ed Gases = the liquid form of a gas which under normal (atmospheric pressure and ambient temperature) conditions of pressure and temperature are found only as a gas. Liquid Nitrogen and Liquid Oxygen are good examples. LNG = liquefi ed natural gas, a fuel. Liquefi ed by cooling below the normal boiling point, approximately -260F (-160C) Nitrogen = a naturally occurring atmospheric gas, 78% of air by volume, inert, boiling point is -320F (-196C) Normal Boiling Point = the temperature at which a liquid boils when under a total pressure of one atmosphere Superconductivity = Th e ability of a material to conduct electricity without resistance. An electrical current in a superconductive ring will fl ow indefi nitely if a low temperature (about −260°C) is maintained. Th omson’s discovery became the basis of a temperature scale based on absolute zero as the lowest possible point. VALVESV ALV ES CYLINDERS CRYOGENIC HOSES & PAIN TS ACCESSORIES Evergreen Midwest Co 8976 Osborne Drive Mentor, OH 44060 www.Ever GreenMidwest.c om Toll: 800.659.3358 Phone: 440.255.5540 Fax: 440.255.6434 Email: [email protected] EExplainingxplaining CCryogenicsryogenics Th at scale has units the same size as the Celsius temperature scale but called kelvin units (abbreviation K). Absolute zero is represented as 0 K, where the term degree is omitted and is read as zero kelvin. Th e Celsius equivalent of 0 K is −273°C, and the Fahrenheit equivalent is −459°F. One can convert between Celsius and Kelvin scales by one of the following equations: °C = K − 273 or K = °C + 273 Cryogenics, then, deals with producing and maintaining environments at temperatures below about 173 K. One aspect of cryogenics involves the development of methods for producing and maintaining very low temperatures. Another aspect includes the study of the properties of materials at cryogenic temperatures. Th e mechanical and electrical properties of many materials change very dramatically when cooled to 100 K or lower. For example, rubber, most plastics, and some metals become exceedingly brittle. Also many metals and ceramics lose all resistance to the fl ow of electricity, a phenomenon called superconductivity. In addition, helium that is cooled to very nearly absolute zero (2.2 K) changes to a state known as superfl uidity. In this state, helium can fl ow through exceedingly narrow passages with no friction. Methods of producing cryogenic temperatures Cryogenic conditions are produced by one of four basic techniques: heat conduction, evaporative cooling, cooling by rapid expansion (the Joule-Th omson eff ect), and adiabatic demagnetization. Th e fi rst two are well known in terms of everyday experience. Th e third is less well known but is commonly used in ordinary refrigeration and air conditioning units, as well as in cryogenic applications. Th e fourth process is used primarily in cryogenic applications and provides a means of approaching absolute zero. Heat conduction is a relatively simple concept to understand. When two bodies are in contact, heat fl ows from the body with the higher temperature to the body with a lower temperature. Conduction can occur between any and all forms of matter, whether gas, liquid, or solid. It is essential in the production of cryogenic temperatures and environments. For example, samples may be cooled to cryogenic temperatures by immersing them directly in a cryogenic liquid or by placing them in an atmosphere cooled by cryogenic refrigeration. In either case, the sample cools by conduction (or transfer) of heat to its colder surroundings. Th e second process for producing cryogenic conditions is evaporative cooling. Humans are familiar with this process because it is a mechanism by which our bodies lose heat. Atoms and molecules in the gaseous state are moving faster than atoms and molecules in the liquid state. Add heat energy to the particles in a liquid and they will become gaseous. Liquid perspiration on human skin behaves in this way. Perspiration absorbs body heat, becomes a gas, and evaporates from the skin. As a result of that heat loss, the body cools down. Cryogens and Th eir Boiling Points EExplainingxplaining CCryogenicsryogenics In cryogenics, a container of liquid is allowed to evaporate. Heat from within the liquid is used to convert particles at the surface of the liquid to gas. Th e gas is then pumped away. More heat from the liquid converts another surface layer of particles to the gaseous state, which is also pumped away. Th e longer this process continues, the more heat is removed from the liquid and the lower its temperature drops. Once some given temperature is reached, pumping continues at a reduced level in order to maintain the lower temperature. Th is method can be used to reduced the temperature of any liquid. For example, it can be used to reduce the temperature of liquid nitrogen to its freezing point or to lower the temperature of liquid helium to approximately 1 K. A third process makes use of the Joule-Th omson eff ect, which was discovered by English physicist James Prescott Joule (1818–1889) and William Th omson, Lord Kelvin, in 1852. Th e Joule-Th omson eff ect depends on the relationship of volume (bulk or mass), pressure, and temperature in a gas. Change any one of these three variables, and at least one of the other two (or both) will also change. Joule and Th omson found, for example, that allowing a gas to expand very rapidly causes its temperature to drop dramatically. Reducing the pressure on a gas accomplishes the same eff ect. To cool a gas using the Joule-Th omson eff ect, the gas is fi rst pumped into a container under high pressure. Th e container is fi tted with a valve with a very small opening. When the valve is opened, the gas escapes from the container and expands quickly. At the same time, its temperature drops. Th e fi rst great success for the Joule-Th omson eff ect in cryogenics was achieved by Kamerlingh Onnes in 1908 when he liquefi ed helium. Th e Joule-Th omson eff ect is an important part of our lives today, even though we may not be aware of it. Ordinary household refrigerators and air conditioners operate on this principle. First, a gas is pressurized and cooled to an intermediate temperature by contact with a colder gas or liquid. Th en, the gas is expanded, and its temperature drops still further. Th e heat needed to keep this cycle operating comes from the inside of the refrigerator or the interior of a room, producing the desired cooling eff ect. Th e fourth process for producing cryogenic temperatures uses a phenomenon known as adiabatic demagnetization. Adiabatic demagnetization makes use of special substances known as paramagnetic salts. A paramagnetic salt consists of a very large collection of particles that act like tiny (atom-sized) magnets. Normally these magnetic particles are spread out in all possible directions.