Elements nuclides

International Atomic Energy Agency and United Nations Environment Programme (1996) Survey of Reference Materials, Volume 2 Environmentally Related Reference Materials for Trace Elements, Nuclides and Micro-contaminants. IAEA-TECDOC-880, IAEA, Vieima. 

IAEA (1990) [Cortes Toro E, Parr RM, Clements SA] Biological and environmental reference materials for trace elements, nuclides and organic microcontaminants. Report lAEA/RI./ i28(Rcv.i), International Atomic Energy Agency, Vienna, Austria. 

The atoms of all isotopes of an element have the same number of protons, the atomic number, Z. The nuclei of different isotopes differ, however, in the number of neutrons and therefore in the total number of nucleons per nucleus. The total number of nucleons is 4, the mass number. Atoms of different isotopic forms of an element, nuclides, are distinguished by using the mass number as a left superscript on the symbol of the element, e.g., 15N refers to the isotope of N with mass number 15. 

Element Nuclide Gamma Ray Energy (keV) Cone, in Standard SRM 1633a CounP3 Analytical Precision SRM 679 RNL to SI Conversion Factors... 

Forms of an element (nuclide) where the numbers of neutrons are different leading to different atomic weights, for example and C. 

Iodine reacts easily with other chemicals, and isotopes of iodine are found as compounds rather than as a pure elemental nuclide. Thus, iodine-129 and -131 found in nuclear facilities and waste treatment plants quickly form compounds with the mixture of chemicals present. However, iodine released to the environment from nuclear power plants is usually a gas. 

Isotope l-s3- top [is- + Gk topos place] (1913) n. In chemistry, one of two or more forms of an element ( nuclides ) having the same number of protons in the nucleus but differing in mass number because of different numbers of neutrons. Natural elements are usually mixtures of isotopes thus the observed atomic weights are average values weighted by isotopic relative abundance. Serway RA, Faugh JS, Bennett CV (2005) College physics. Thomas, New York. 

A nuclide is an atomic species as determined by its atomic number (proton number) Z and mass number (nucleon number) A = Z+N, where N is the number of neutrons in its nucleus. Atomic species with the same nuclear composition but different nuclear energy states with measurable lifetime are considered independent nuclides in their own right. Nuclides can be classified in different ways. Nuclides having the same atomic number Z (but different mass number A) represent the same chemical element and are called the isotopes of that element. Nuclides with the same mass number A (but different atomic number Z) are called isobars. Nuclides of the same number of neutrons N (but different atomic number Z) are called isotones. Nuclides of the same nuclear composition but different nuclear states are referred to as (nuclear) isomers. The terms isotope, isotopic, isobar, isobaric, isotone, isotonic, isomer, and isomeric can also be applied to nuclei, but the terms nuclide and nuclidic can only be applied to atoms. 

In hot-fusion reactions, the cross section for producing heavy-element nuclides is determined by the probability that the highly excited compound nucleus will avoid fission in the deexcitation process. Cold fusion near the reaction barrier is qualitatively different the formation of the compound nucleus comes about in two separate steps [105, 107]. The reacting nuclei come into contact, captured into a dinuclear configuration, which is separated from an equilibrated compound nucleus by a potential-energy barrier which is not reproduced by the one-dimensional Coulomb-barrier model [94, 95, 210, 219, 220]. This extra barrier diverts the trajectory of the reaction through multidimensional deformation space toward quasifission, making reseparation much more likely than complete fusion. 

Nuclide. Each nuclide is identified by element name and the mass number A, equal to the sum of the numbers of protons Z and neutrons N in the nucleus. The m following the mass number (for example, Zn) indicates a metastable isotope. An asterisk preceding the mass number indicates that the radionuclide occurs in nature. Half-life. The following abbreviations for time units are employed y = years, d = days, h = hours, min = minutes, s = seconds, ms = milliseconds, and ns = nanoseconds. 

Natural abundance. The natural abundances listed are on an atom percent basis for the stable nuclides present in naturally occurring elements in the earth s crust. 

Several portions of Section 4, Properties of Atoms, Radicals, and Bonds, have been significantly enlarged. For example, the entries under Ionization Energy of Molecular and Radical Species now number 740 and have an additional column with the enthalpy of formation of the ions. Likewise, the table on Electron Affinities of the Elements, Molecules, and Radicals now contains about 225 entries. The Table of Nuclides has material on additional radionuclides, their radiations, and the neutron capture cross sections. 

Nuclear-physical methods ai e the basic ones in controlling environmental pollution which results from nucleai -power complexes and power plants work. Oil and gas production leads to the extraction of radio nuclides of natural origin in considerable amounts, which later spread from oil-slimes and water wastes in the neighborhoods of oil and gas producing entei prises. Similaidy, toxic and radioactive elements can pollute environment in case of mineral deposits extraction. 

Because of the long time scale involved in the s-process, unstable nuclides formed by (n.y) reactions have time to decay subsequently by decay (electron emission). The crucial factor in determining the relative abundance of elements... 

Elements with radioactive nuclides amongst their naturally occurring isotopes have a built-in time variation of the relative concentration of their isotopes and hence a continually... 

Our present views on the electronic structure of atoms are based on a variety of experimental results and theoretical models which are fully discussed in many elementary texts. In summary, an atom comprises a central, massive, positively charged nucleus surrounded by a more tenuous envelope of negative electrons. The nucleus is composed of neutrons ( n) and protons ([p, i.e. H ) of approximately equal mass tightly bound by the force field of mesons. The number of protons (2) is called the atomic number and this, together with the number of neutrons (A ), gives the atomic mass number of the nuclide (A = N + Z). An element consists of atoms all of which have the same number of protons (2) and this number determines the position of the element in the periodic table (H. G. J. Moseley, 191.3). Isotopes of an element all have the same value of 2 but differ in the number of neutrons in their nuclei. The charge on the electron (e ) is equal in size but opposite in sign to that of the proton and the ratio of their masses is 1/1836.1527. 

It will be recalled that is 100% abundant and is the heaviest stable nuclide of any element (p. 550), but it is essential to use very high purity Bi to prevent unwanted nuclear side-reactions which would contaminate the product Po in particular Sc, Ag, As, Sb and Te must be <0.1 ppm and Fe <10ppm. Polonium can be obtained directly in milligram amounts by fractional vacuum distillation from the metallic bismuth. Alternatively, it can be deposited spontaneously by electrochemical replacement onto the surface of a less electropositive metal... 

Since the radioactive half-lives of the known transuranium elements and their resistance to spontaneous fission decrease with increase in atomic number, the outlook for the synthesis of further elements might appear increasingly bleak. However, theoretical calculations of nuclear stabilities, based on the concept of closed nucleon shells (p. 13) suggest the existence of an island of stability around Z= 114 and N= 184. Attention has therefore been directed towards the synthesis of element 114 (a congenor of Pb in Group 14 and adjacent superheavy elements, by bombardment of heavy nuclides with a wide range of heavy ions, but so far without success. 

Element has no stable nuclides the value given in parentheses is the atomic mass number of the isotope of longest known half-life. However, three such elements (Th, Pa and U) do have a characteristic terrestrial isotopic composition, and for these an atomic weight is tabulated. 

Element Abundance Cross Section, barns Nuclide Half-Life y-photopeak, MeV... 

In general, three basic kinds of sorption mechanisms for trace elements in geologic aqueous systems can be distinguished (56). Due to non-specific forces of attraction between sorbent and the solute, a physical adsorption may occur. This sorption mechanism results in the binding of species from the solution in several consecutive layers on exposed solid surfaces. This would be a rapid non-selec-tive and reversible process, fairly independent of nuclide concentration and only little dependent on ion exchange capacity of the solid. 

The discoveries of Becquerel, Curie, and Rutherford and Rutherford s later development of the nuclear model of the atom (Section B) showed that radioactivity is produced by nuclear decay, the partial breakup of a nucleus. The change in the composition of a nucleus is called a nuclear reaction. Recall from Section B that nuclei are composed of protons and neutrons that are collectively called nucleons a specific nucleus with a given atomic number and mass number is called a nuclide. Thus, H, 2H, and lhO are three different nuclides the first two being isotopes of the same element. Nuclei that change their structure spontaneously and emit radiation are called radioactive. Often the result is a different nuclide. 

Nucleosynthesis is the formation of elements. Hydrogen and helium were produced in the Big Bang all other elements are descended from these two, as a result of nuclear reactions taking place either in stars or in space. Some elements—among them technetium and promethium—are found in only trace amounts on Earth. Although these elements were made in stars, their short lifetimes did not allow them to survive long enough to contribute to the formation of our planet. However, nuclides that are too unstable to be found on Earth can be made by artificial techniques, and scientists have added about 2200 different nuclides to the 300 or so that occur naturally. 

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