Mikkel Frandsen

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Mikkel Frandsen
Born1892
Died1981
Alma mater University of California
Scientific career
Institutions National Bureau of Standards,

Mikkel Frandsen (1892–1981) was a Danish American physical chemist noted for experiments involving chemical thermodynamics, oil, and heavy water. Also known as deuterium oxide (D2O), heavy water is used to produce nuclear power and is used in other nuclear applications such as nuclear magnetic resonance spectroscopy.

Contents

Early years

Frandsen was born in the parish of Sønder Lem in the town of Ringkøbing in Ringkøbing-Skjern, Midtjylland, Denmark. He emigrated from Denmark to the United States in 1921. Frandsen earned his Ph.D. in Physical Chemistry from the University of California in 1926.

In 1928, Frandsen invented the Liquid Phase Cracking Process, discovering that when oil is heated to a point at which cracking (chemistry) takes place, the heat consumed causes the oil temperature to decrease. This results in an increased yield of gasoline and a decreased knocking tendency of gasoline.

Heavy Water

In 1931 while at the National Bureau of Standards (NBS), Frandsen began a study with Edward W. Washburn (1881-1934), chief of the NBS and his assistant Edgar R. Smith, the results of which were published in "The Isotopic Fractionation of Water" (1933). [1] [2] In Frandsen et al.'s experiment, the scientists subjected water to electrolysis, and an isotope fractionation took place. The heavy water produced displayed a higher density than regular water. Heavy water has a higher freezing point, higher boiling point, and lower refractive index than regular water.

Heavy water differs from regular water in that the two atoms of hydrogen have been substituted with two atoms of deuterium, which is an isotope of hydrogen. The mass of heavy water is about 10% more than that of regular water due to the extra neutron in deuterium. Heavy water was discovered by Gilbert N. Lewis in 1933.

In 1934, Frandsen, along with Washburn and Smith, also published "On Change in Density, Index of Refraction, Boiling Point, and Freezing Point of Water after Electrolysis."[ citation needed ]

National Bureau of Standards

From 1931 to 1934, Frandsen authored or co-authored a series of experiments while at the National Bureau of Standards, the first of which was entitled, Cryoscopic Constant Heat of Fusion, and Heat Capacity of Camphor (1931). In 1932, Frederick Rossini, Washburn, and Frandsen authored "The Calorimetric Determination of the Intrinsic Energy of Gases as a Function of the Pressure." This experiment resulted in the development of the Washburn Correction for bomb calorimetry, a decrease or correction of the results of a calorimetric procedure to normal states.

Frandsen also co-authored two articles with Merle Randall in 1932, The Standard Electrode Potential of Iron and the Activity Coefficient of Ferrous Chloride [3] and Determination of the Free Energy of Ferrous Hydroxide from Measurements of Electromotive Force. [4] Randall, along with Lewis, wrote one of the most influential books in chemical thermodynamics, Thermodynamics and the Free Energy of Chemical Substances (1923). In 1933, Frandsen conducted research on the Heat Capacity of Phosphorus Pentoxide. Another of Frandsen's experiments in 1933 was entitled, A Method of Determining Solvent Properties of Volatile Thinners in Varnishes. [5] [ permanent dead link ]

Later years

In 1952, working at the U.S. Naval Gun Factory, Frandsen conducted chemical and spectrographic analyses of steels and copper alloys that led to a more effective testing procedure, the Quantometric Method. His research led to an article entitled, "Preparation of Vanadium Monoxide (1952)." [ permanent dead link ]

Related Research Articles

Cold fusion Hypothetical type of nuclear reaction

Cold fusion is a hypothesized type of nuclear reaction that would occur at, or near, room temperature. It would contrast starkly with the "hot" fusion that is known to take place naturally within stars and artificially in hydrogen bombs and prototype fusion reactors under immense pressure and at temperatures of millions of degrees, and be distinguished from muon-catalyzed fusion. There is currently no accepted theoretical model that would allow cold fusion to occur.

Deuterium Isotope of hydrogen with 1 neutron

Deuterium is one of two stable isotopes of hydrogen. The nucleus of a deuterium atom, called a deuteron, contains one proton and one neutron, whereas the far more common protium has no neutrons in the nucleus. Deuterium has a natural abundance in Earth's oceans of about one atom in 6420 of hydrogen. Thus deuterium accounts for approximately 0.02% of all the naturally occurring hydrogen in the oceans, while protium accounts for more than 99.98%. The abundance of deuterium changes slightly from one kind of natural water to another.

Exothermic process Thermodynamic reaction

In thermodynamics, the term exothermic process describes a process or reaction that releases energy from the system to its surroundings, usually in the form of heat, but also in a form of light, electricity, or sound. Its etymology stems from the Greek prefix έξω and the Greek word θερμικός. The term exothermic was first coined by Marcellin Berthelot.

Gilbert N. Lewis American physical chemist

Gilbert Newton Lewis or was an American physical chemist and a Dean of the College of Chemistry at University of California, Berkeley. Lewis was best known for his discovery of the covalent bond and his concept of electron pairs; his Lewis dot structures and other contributions to valence bond theory have shaped modern theories of chemical bonding. Lewis successfully contributed to chemical thermodynamics, photochemistry, and isotope separation, and is also known for his concept of acids and bases. Lewis also researched on relativity and quantum physics, and in 1926 he coined the term "photon" for the smallest unit of radiant energy.

Hydrogen Chemical element with atomic number 1

Hydrogen is the chemical element with the symbol H and atomic number 1. With a standard atomic weight of 1.008, hydrogen is the lightest element in the periodic table. Hydrogen is the most abundant chemical substance in the universe, constituting roughly 75% of all baryonic mass. Non-remnant stars are mainly composed of hydrogen in the plasma state. The most common isotope of hydrogen, termed protium, has one proton and no neutrons.

Heavy water Form of water

Heavy water is a form of water that contains only deuterium rather than the common hydrogen-1 isotope that makes up most of the hydrogen in normal water. The presence of the heavier hydrogen isotope gives the water different nuclear properties, and the increase of mass gives it slightly different physical and chemical properties when compared to normal water.

Nuclear fission Nuclear reaction splitting an atom into multiple parts

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Electrolysis Technique in chemistry and manufacturing

In chemistry and manufacturing, electrolysis is a technique that uses direct electric current (DC) to drive an otherwise non-spontaneous chemical reaction. Electrolysis is commercially important as a stage in the separation of elements from naturally occurring sources such as ores using an electrolytic cell. The voltage that is needed for electrolysis to occur is called the decomposition potential. The word "lysis" means to separate or break, so in terms, electrolysis would mean either "breakdown of electricity" or "breakdown via electricity".

Ringkøbing

Ringkøbing is a town in Ringkøbing-Skjern municipality in Region Midtjylland on the west coast of the Jutland peninsula in west Denmark. It has a population of 9,923..

Harold Urey American physical chemist

Harold Clayton Urey was an American physical chemist whose pioneering work on isotopes earned him the Nobel Prize in Chemistry in 1934 for the discovery of deuterium. He played a significant role in the development of the atom bomb, as well as contributing to theories on the development of organic life from non-living matter.

In physical organic chemistry, a kinetic isotope effect (KIE) is the change in the reaction rate of a chemical reaction when one of the atoms in the reactants is replaced by one of its isotopes. Formally, it is the ratio of rate constants for the reactions involving the light (kL) and the heavy (kH) isotopically substituted reactants (isotopologues):

Isotopes of hydrogen hydrogen with different numbers of neutrons

Hydrogen (1H) has three naturally occurring isotopes, sometimes denoted 1H, 2H, and 3H. The first two of these are stable, while 3H has a half-life of 12.32 years. There are also heavier isotopes, which are all synthetic and have a half-life less than one zeptosecond. Of these, 5H is the most stable, and 7H is the least.

In electrochemistry, overpotential is the potential difference (voltage) between a half-reaction's thermodynamically determined reduction potential and the potential at which the redox event is experimentally observed. The term is directly related to a cell's voltage efficiency. In an electrolytic cell the existence of overpotential implies the cell requires more energy than thermodynamically expected to drive a reaction. In a galvanic cell the existence of overpotential means less energy is recovered than thermodynamics predicts. In each case the extra/missing energy is lost as heat. The quantity of overpotential is specific to each cell design and varies across cells and operational conditions, even for the same reaction. Overpotential is experimentally determined by measuring the potential at which a given current density is achieved.

Merle Randall was an American physical chemist famous for his work with Gilbert N. Lewis, over a period of 25 years, in measuring reaction heat of chemical compounds and determining their corresponding free energy. Together, their 1923 textbook "Thermodynamics and the Free Energy of Chemical Substances" became a classic work in the field of chemical thermodynamics.

Frederick Dominic Rossini was an American thermodynamicist noted for his work in chemical thermodynamics.

Faraday efficiency describes the efficiency with which charge (electrons) is transferred in a system facilitating an electrochemical reaction. The word "Faraday" in this term has two interrelated aspects. First, the historic unit for charge is the faraday, but has since been replaced by the coulomb. Secondly, the related Faraday's constant correlates charge with moles of matter and electrons. This phenomenon was originally understood through Michael Faraday's work and expressed in his laws of electrolysis.

Deuterium-depleted water (DDW) is water which has a lower concentration of deuterium than occurs naturally on Earth. DDW is also known as light water, although, that term is also used in reference to normal water as well.

The isotopic resonance hypothesis(IsoRes) postulates that certain isotopic compositions of chemical elements affect kinetics of chemical reactions involving molecules built of these elements. The isotopic compositions for which this effect is predicted are called resonance isotopic compositions.

Hydrogen isotope biogeochemistry is the scientific study of biological, geological, and chemical processes in the environment using the distribution and relative abundance of hydrogen isotopes. There are two stable isotopes of hydrogen, protium 1H and deuterium 2H, which vary in relative abundance on the order of hundreds of permil. The ratio between these two species can be considered the hydrogen isotopic fingerprint of a substance. Understanding isotopic fingerprints and the sources of fractionation that lead to variation between them can be applied to address a diverse array of questions ranging from ecology and hydrology to geochemistry and paleoclimate reconstructions. Since specialized techniques are required to measure natural hydrogen isotope abundance ratios, the field of hydrogen isotope biogeochemistry provides uniquely specialized tools to more traditional fields like ecology and geochemistry.

Isotopic reference materials are compounds with well-defined isotopic compositions and are the ultimate sources of accuracy in mass spectrometric measurements of isotope ratios. Isotopic references are used because mass spectrometers are highly fractionating. As a result, the isotopic ratio that the instrument measures can be very different from that in the sample's measurement. Moreover, the degree of instrument fractionation changes during measurement, often on a timescale shorter than the measurement's duration, and can depend on the characteristics of the sample itself. By measuring a material of known isotopic composition, fractionation within the mass spectrometer can be removed during post-measurement data processing. Without isotope references, measurements by mass spectrometry would be much less accurate and could not be used in comparisons across different analytical facilities. Due to their critical role in measuring isotope ratios, and in part, due to historical legacy, isotopic reference materials define the scales on which isotope ratios are reported in the peer-reviewed scientific literature.

References

  1. William Albert Noyes. "Biographical Memoir of Edward Wight Washburn" (PDF). National Academy Of Sciences. Retrieved December 20, 2015.CS1 maint: discouraged parameter (link)
  2. Edward W. Washburn; Edgar R. Smith & Mikkel Frandsen (1933). "The Isotopic Fractionation of Water". J. Chem. Phys. 1 (4): 288. Bibcode:1933JChPh...1..288W. doi:10.1063/1.1749290.
  3. Randall, M.; Frandsen, M. (1932). "The Standard Electrode Potential of Iron and the Activity Coefficient of Ferrous Chloride". Journal of the American Chemical Society. 54: 47–54. doi:10.1021/ja01340a006.
  4. Randall, M.; Frandsen, M. (1932). "Determination of the Free Energy of Ferrous Hydroxide from Measurements of Electromotive Force". Journal of the American Chemical Society. 54: 40–46. doi:10.1021/ja01340a005.
  5. Frandsen, M. (1933). "A Method of Determining Solvent Properties of Volatile Thinners in Varnishes". Industrial & Engineering Chemistry Analytical Edition. 5 (3): 184–185. doi:10.1021/ac50083a014.