Nuclear chemistry

Nuclear chemistry is a subfield of chemistry dealing with radioactivity, nuclear processes and nuclear properties. Within this area of chemistry the chemistry of radioactive elements such as the actinides, radium and radon is considered as is the chemistry associated with equipment (such as nuclear reactors) which are designed to perfrom nuclear processes, this includes the corrosion of surfaces and the behaviour under both conditions of normal operation and abnormal operation (such as during an accident). Another area which is important is the behaviour of the objects and materials after they have been placed into a waste store or otherwise disposed of.

In addition to the study of radioactive objects and materials, nuclear chemistry includes the study and use of nuclear processes and properties within non-radioactive areas of human activity, for instance NMR spectrscopy is commonly used within synthetic organic chemistry.

It can be divided into several main categories:

Early history

After the discovery of X-rays by Wilhelm Röntgen, many scientists began to work on ionizing radiation. One of these was Henri Becquerel, who investigated the relationship between phosphorescence and the blackening of photographic plates. When Becquerel (working in France) discovered that, with no external source of energy, the uranium generated rays which could blacken (or fog) the photographic plate, radioactivity was discovered. Marie Curie (working in Paris) and her husband Pierre Curie isolated two new radioactive elements from uranium ore. They used radiometric methods to identify which stream the radioactivity was in after each each chemical separation; they separated the uranium ore into each of the different chemical elements that were known at the time, and measured the radioactivity of each fraction. They then attempted to separate these radioactive fractions further, to isolate a smaller fraction with a higher specific activity (radioactivity divided by mass). In this way, they isolated polonium and radium. Their daughter Irène Joliot-Curie and her husband were the first to 'create' radioactivity: they bombarded boron with alpha particles to make a proton-rich isotope of nitrogen; this isotope emitted positrons.[5] In addition, they bombarded aluminium and magnesium with neutrons to make new radioisotopes.

Ernest Rutherford, working in Canada and England, discovered that radioactivity decays according to first order kinetics (half life); he coined the terms alpha, beta and gamma rays. He also converted nitrogen into oxygen, and most importantly he supervised the students who did the Geiger-Marsden experiment (gold leaf experiment) which showed that the 'plum pudding model' of the atom was wrong. In the plum pudding model, proposed by J. J. Thomson in 1904, the atom is composed of electrons surrounded by a 'cloud' of positive charge to balance the electrons' negative charge. To Rutherford, the gold foil experiment implied that the positive charge was confined to a very small nucleus leading first to the Rutherford model, and eventually to the Bohr model of the atom.

Main areas

Radiochemistry

Radiochemistry is the chemistry of radioactive materials. In radiochemistry, radioactive isotopes of elements are used to study the properties and chemical reactions of ordinary non-radioactive isotopes (often within radiochemistry the absence of radioactivity leads to a substance being described as being inactive as the isotopes are stable). An example of a biological use of radiochemistry is the study of DNA using radioactive phosphorus-32.

Radiation chemistry

Radiation chemistry is the study of the chemical effects of radiation on matter; this is very different to radiochemistry as no radioactivity needs to be present in the material which is being chemically changed by the radiation. An example is the conversion of water into hydrogen gas and hydrogen peroxide.

Study of nuclear reactions

see also nuclear physics A combination of radiochemistry and radiation chemistry is used to study nuclear reactions such as fission and fusion. Some early evidence for nuclear fission was the formation of a shortlived radioisotope of barium which was isolated from neutron irradated uranium (¹³⁹Ba, with a half-life of 83 minutes and ¹⁴⁰Ba, with a half-life of 12.8 days, are major fission products of uranium). At the time, it was thought that this was a new radium isotope, as it was then standard radiochemical practise to use a barium sulphate carrier percipitate as a means of assisting in the isolation of radium.[6]. More recently, a combination of radiochemical methods and nuclear physics has been used to try to make new 'superheavy' elements; it is thought that islands of relative stability exist where the nuclides have half-lives of years, thus enabling weighable amounts of the new elements to be isolated. For more details of the original discovery of nuclear fission see the work of Otto Hahn..

Radioisotope production

The processes forming new isotopes (often radioactive) involves several areas of nuclear chemistry.

Processes

Neutrons

By neutron irradiation with slow neutrons it is possible to form neutron-rich isotopes which tends to decay by beta decay (i.e. by electron emission from the nuclei). For instance, irradiating ⁵⁹Co with neutrons forms an excited state of ⁶⁰Co (best written as ^60mCo) which decays by emitting a gamma ray to the ground state of ⁶⁰Co, which in turn decays by emitting an electron to form ^60mNi. The excited state of the ^60mNi then decays with the emission of two gamma photons to the ground state of ⁶⁰Ni.

As the neutron energy increases, the simple capture reactions become less important, while other reactions such as the (n,p) reaction become more important. An example is the production of phosphorus-32 by neutron irradiation of ³²S. The sulphur nucleus captures a neutron and emits a proton to form the radioactive phosphorus isotope. Carbon-14 is obtained in a similar manner by irradiating ¹⁴N with neutrons.

Fast protons, deuterons and other positive projectiles

Using a cyclotron or a linear accelerator (linac) it is possible to obtain a beam of fast moving positive particles (up to 30 MeV protons and deuterons can be obtained). The energies of these particles are so high that they can overcome the electrostatic barrier which opposes the entry of positive particles into the nucleus. An example of the use of the (p,n) reaction is the conversion of ¹⁰³Rh into ¹⁰³Pd, this can be performed by irradiating rhodium foil with protons to form the radioactive palladium isotope.

The reaction of beryllium with alpha particles is another example of this type of reaction. While the reaction of ⁹Be with ⁴He²⁺ generates ¹²C, its most important aspect is that it generates neutrons.

Formation by the decay of parent isotopes

Many isotopes can be made from a parent isotope which decays to form the wanted isotope. If the parent and the product element can be chemically separated, then it is possible to create an "isotope cow". The classic isotope cow is the technetium cow, many others work by the same principle. The technetium cow uses molybdum-99 absorbed on alumina, and it is "milked" by passing saline solution through it to give a solution of technetium. In the following diagram the technetium is represented in red, in picture two the cow is milked to make a product solution. The technetium then builds up again to allow the cow to return to the technetium loaded state where it can be milked again.

A diagram explaining the operation of a technetium cow, the technetium is represented by the colour red. It is milked off the alumina column and then builds up again

Using this general method, aqueous solutions of the following isotopes can be made from parent isotopes (shown in brackets)

• ⁶⁸Ga (⁶⁸Ge)
• ⁸²Rb (⁸²Sr)
• ^99mTc (⁹⁹Mo)
• ^113mIn (¹¹³Sn)
• ¹⁸⁸Re (¹⁸⁸W)
• ⁶²Cu (⁶²Zn)

When the product isotope is a gas, then the cow can be milked by allowing the product to diffuse out of a solid. An early method of forming radiography sources was to milk radon from a radium source; this method was used by Marie Curie during the first World War (WWI). The same method was used for making Brachytherapy sources in the USA. Using this general method, the following isotopes can be obtained from parent isotopes (shown in brackets)

• ^81mKr (⁸¹Rb)
• ²²²Rn (²²⁶Ra)

Within some nuclear materials, new isotopes will be formed by the decay of a parent isotope. For instance, the beta decay of ²⁴¹Pu will form ²⁴¹Am, thus if a sample of plutonium which has been allowed to stand for several years is subjected to a new chemical purification then it is possible to harvest the americium.

• ²⁴¹Am (²⁴¹Pu)

Uses

Radioactive sources are used for many different purposes, a short review of the use of radioactivity in industry can be read online[7]. A sealed source is sealed within a container so that, in normal use, no radioactive material can be lost from the source. In many sealed sources, the radioactive filling is surrounded by one or more layers of a corrosion-resistant material (such as stainless steel or gold). Alternatively, it is possible to form a source using material which holds the radioactivity in a chemically resistant and strong form without needing a metal cover. In designing sealed sources, it is common to choose a chemically stable form of the radioactive element, but for cesium radiotherapy sources it is common to use the water soluble chloride, because it is impossible to obtain the required density of cesium in another compound.

Sealed sources

Sealed sources are used for radiotherapy (both brachytherapy and teletherapy), food irradation, industrial radiography, nuclear gauges and many other applications.

Open sources

Open sources are used for a range of applications which include the use of tracers to study the physical operation of industrial processes, to trace the chemical mechanism by which a product forms or for some forms of radiotherapy.

For instance krypton has been used to study the underground combustion of fuels such as oil and coal.[8][9]

The nuclear fuel cycle

The chemistry associated with any part of the nuclear fuel cycle which includes nuclear reprocessing. The fuel cycle includes all the operations involved with the production of fuel from mining, ore processing, enrichment and fuel production (Front end of the cycle). Also it includes the 'in-pile' behaviour (use of the fuel in a reactor) before the back end of the cycle. The back end includes the management of the used nuclear fuel in either a cooling pond or dry storage, before it is either disposed of directly into an underground waste store or it is reprocessed.

The study of used fuel

Used nuclear fuel is studied in post irradation examination, where used fuel is examined to know more about the processes that occur in fuel during use, and how these might alter the outcome of an accident. For example, during normal use, the fuel expands due to thermal expansion. This causes cracking, and in extreme cases, such as during the power surge which destroyed the Chernobyl nuclear reactor in April, 1986, the fuel can shatter into very small fragments. The majority of nuclear fuel is uranium dioxide which is a cubic solid which has a structure similar to that of calcium flouride, in used fuel the solid state structure of the majority of the solid remains the same as that of pure cubic uranium dioxide.

The solid state structure of uranium dioxide, the oxygen atoms are in red while the uranium atoms are in green

Uranium dioxide is very insoluble in water, but after oxidation it can be converted to uranium trioxide or another uranium(VI) compound which is much more soluble in water. It is important to understand that uranium dioxide (UO₂) can be oxidised to an oxygen rich hyperstoichiometric oxide (UO_2+x) which can be further oxidised to U₄O₉, U₃O₇, U₃O₈ and UO₃.2H₂O.

Because used fuel contains alpha emitters (plutonium and the minor actinides) the effect of adding an alpha emitter (²³⁸Pu) to uranium dioxide on the leaching rate of the oxide has been investigated. It was found that for the crushed oxide the addition of ²³⁸Pu did tend to increase the rate of uranium leaching, but the difference in the leaching rate between between 0.1 and 10% ²³⁸Pu was very small. For further detail read V.V. Rondinella, Hj. Matzke, J. Cobos and T. Wiss, Radiochimica Acta, 2000, 88, 527-531.

The concentration of carbonate in the water which is in contact with the used fuel has a great effect upon the rate of corrosion, this is because uranium(VI) forms soluble anionic carbonate complexes such as [UO₂(CO₃)₂]^2- and [UO₂(CO₃)₃]^4-. When carbonate ions are absent, and the water is not strongly acidic, the hexavalent uranium compounds which form on oxidation of the uranium dioxide oftein form insoluble hydrated uranium trioxide phases. For further detail see D.W. Shoesmith, Journal of Nuclear Materials, 2000, 282, 1-31.

By sputtering using uranium metal and an argon/oxygen gas mixture thin films of uranium dioxide can be deposited upon gold surfaces. These gold surfaces which are modified with uranium dioxide have been used for both cyclic voltammetry and AC impedance experiments which offer an insight into the likely leaching behaviour of uranium dioxide. For details please see F. Miserque, T. Gouder, D.H. Wegen and P.D.W. Bottomley, Journal of Nuclear Materials, 2001, 298, 280-290. A review of the topic of the corrosion of uranium dioxide in a waste store was written by D.W. Shoesmith (Journal of Nuclear Materials, 2000, 282, 1-31) in which he explains much of the chemistry.

Fuel cladding interactions

The study of the nuclear fuel cycle includes both the study of the behaviour of nuclear materials both under normal conditions and under accident conditions. For example a large amount of work has been done on the interaction between uranium dioxide based fuel and the zirconium alloy tubing used to cover the fuel. In short using use the fuel swells due to thermal expansion and then starts to react with the surface of the zirconium alloy, to form a new layer which contains both fuel and zirconium (from the cladding). Then, on the fuel side of this mixed layer, is a layer of fuel which is a cesium rich layer which has a higher cesium to uranium ratio than most of the fuel. This is because xenon isotopes are formed as fission products and these diffuse out of the lattice of the fuel into voids such as the narrow gap between fuel and the cladding, after diffusing to these voids it decays to cesium isotopes. Because of the thermal gradient which exists in the fuel during use, the volatile fission products tend to be driven from the centre of the pellet to the rim area.. Below can be seen a graph of the temperture of uranium metal, uranium nitride and uranium dioxide as a function of the distance from the centre of a 20 mm dimeter pellet which has a rim temperture of 200 ^oC, it is important to note that the uranium dioxide (due to its poor thermal conductivity) will overheat at the centre of the pellet under these conditions while the more thermally conductive other forms of uranium will remain below their melting points.

Temperature profile for a 20 mm diameter fuel pellet with a power density of 1000 W per cubic meter. The fuels other than uranium dioxide are not compromised.

Absorption of fission products on surfaces

Another important area of nuclear chemistry is the study of the interaction of fission products with surfaces. This is thought to control the rate of release and migration of fission products both from waste containers under normal conditions and from power reactors under accident conditions.

It is interesting to note that, like chromate and molybdate, the ⁹⁹TcO₄ anion can react with steel surfaces to form a corrosion resistant layer. In this way, these metaloxo anions act as anodic corrosion inhibitors. The formation of ⁹⁹TcO₂ on steel surfaces is one effect which will retard the release of ⁹⁹Tc from nuclear waste drums and nuclear equipment which has become lost before decontamination (eg submarine reactors lost at sea). This ⁹⁹TcO₂ layer renders the steel surface passive, it inhibits the anodic corrosion reaction. It has also been shown that ⁹⁹TcO₄ anions react to form a layer on the surface of activated carbon (charcoal).

Formation of a TcO2 layer on a steel surface.

In a similar way, the release of iodine-131 in a serious power reactor accident could be retarded by absorption on metal surfaces within the nuclear plant.

Spinout areas

Some methods which were first developed within nuclear chemistry and physics have become so widely used within chemistry and other physical sciences that they may be best thought of as not being part of normal nuclear chemistry. For example, Isotopic chemistry could be included in this subtopic, but due to the use of the isotope effect to investigate chemical mechanisms and the use of cosmogenic isotopes and long-lived unstable isotopes in geology it is best to consider much of isotopic chemistry as separate from nuclear chemistry.

Kinetics (use within mechanistic chemistry)

The mechanisms of chemical reactions can be investigated by observing the effect upon the kinetics of making an isotopic modification of a substrate in a reaction. This is now a standard method in organic chemistry. Briefly, the replacement of normal hydrogens (protons) within a chemical compound with deuterium causes the rate of molecular vibration (C-H, N-H and O-H bonds show this) to decrease, this then can lead to a decrease in the reaction rate if the rate determining step involves the breaking of a bond between hydrogen and another atom, hence if upon replacement of protons for deuteriums the reaction changes in rate it is reasonable to assume that the breaking of the bond to hydrogen is part of the step which determines the rate.

Uses within geology, biology and forensic science

Cosmogenic isotopes are formed by the interaction of cosmic rays with the nucleus of an atom. These can be used for dating purposes and for use as natural tracers. In addition, by careful measurement of some ratios of stable isotopes it is possible to obtain new insights into the origin of bullets, ages of ice samples, ages of rocks, and the diet of a person can be identified from a hair or other tissue sample. (See Isotope geochemistry and Isotopic signature for further details).

Nuclear magnetic resonance (NMR)

NMR spectroscopy uses the net spin of nuclei in a substances upon energy absorption, and is used to identify molecules. This has now become a standard spectrscopic tool within synthetic chemistry One of the main uses of NMR is to determine the bond connectivity within an organic molecule.

NMR imaging also uses the net spin of nuclei (commonly protons) for imaging. This is widely used in medicine, and can provide detailed images of the inside of a person without inflicting any radiation upon them. In a medical setting, NMR is often known simply as "Magnetic resonance" imaging, as the word 'nuclear' has negative connotations for many people.

Text books

Radiochemistry and Nuclear Chemistry

• Choppin, Liljenenzin and Rydberg
• ISBN -0750674636, Butterworth-Heinemann, 2002

Description: Comprehensive textbook.

Radioactivity, Ionizing radiation and Nuclear Energy

• Hála and Navratil
• ISBN -807302053-X, Konvoj, 2003

Description: Basic textbook for undergraduates.

The Radiochemical Manual

• Edited by BJ Wilson
• Written by RJ Bayly, JR Catch, JC Charlton, CC Evans, TT Gorsuch, JC Maynard, LC Myerscough, GR Newbery, H Sheard, CBG Taylor and BJ Wilson.
• No ISBN number (too old for the ISBN system), The radiochemical centre (Amersham) was sold via HMSO, 1966 (second edition)

Description: Overview of the production and uses of sources, both open and sealed.