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beryllium Geostandards Newsletter has continued its annual bibliography on geochemical reference samples (B13, B14). Roelandts also cataloged over 170 geochemical standards and provided references to compiled data (B15). SAMPLE PREPARATION AND DISSOLUTIONThe sample preparation step is frequently the most time consuming and a major potential source of error in any geochemical analysis. Numerous approaches have been used to automate this step such as using robots to grind samples (Cl) or to perform acid digestions. The use of microwave ovens to speed up the digestion process is becoming commonplace.
beryllium Geostandards Newsletter has continued its annual bibliography on geochemical reference samples (B13, B14). Roelandts also cataloged over 170 geochemical standards and provided references to compiled data (B15). SAMPLE PREPARATION AND DISSOLUTIONThe sample preparation step is frequently the most time consuming and a major potential source of error in any geochemical analysis. Numerous approaches have been used to automate this step such as using robots to grind samples (Cl) or to perform acid digestions. The use of microwave ovens to speed up the digestion process is becoming commonplace.
The article contains sections titled: 1. Introduction 1.1. Definition and Purpose 1.2. History 1.3. General Features 1.4. Importance and Trends 2. Requirements for Analytical Use of Radionuclides 2.1. Safety and Operational Aspects 2.2. The Labeled Substance 2.3. Activity Measurements 2.4. Choice of Radionuclide 2.5. Appraisal of Radionuclide Use in Analysis 2.5.1. Advantages 2.5.2. Disadvantages 2.5.3. Sources of Error 3. Radiotracers in Methodological Studies 3.1. Principles and Importance 3.2. Control of Sampling 3.3. Control of Contamination and Loss 3.4. Separation Procedures 3.5. Control of the Determination Stage 4. IsotopeDilution Analysis 4.1. Direct Isotope Dilution Analysis 4.2. Reverse Isotope Dilution Analysis 4.3. Derivative Isotope Dilution Analysis 4.4. Substoichiometric Isotope Dilution Analysis 4.4.1. Substoichiometric Separation by Liquid ‐ Liquid Distribution 4.4.2. Redox Substoichiometry 4.4.3. Displacement Substoichiometry 4.4.4. Applications 4.5. Sub‐ and Superequivalence Method 5. Radioreagent Methods 5.1. Simple Radioreagent Methods 5.1.1. Determination with Labeled Reagents 5.1.2. Determination with Labeled Analyte 5.1.3. Determination with Labeled Competing Substances 5.2. Method of Concentration‐Dependent Distribution 5.3. Isotope Exchange Methods 5.4. Radioimmunoassay 5.5. Radiorelease Methods 5.5.1. Radioactive Kryptonates 5.5.2. Radioactive Metals 5.5.3. Radioactive Salts and other Radioactive Substances 5.6. Radiometric Titration
After a brief historical survey of the role of neutron activation analysis (NAA) in environmental analysis there follows a section on the main types of NAA and their application to environmental problems and a table of ideal sensitivities is given. The rest of the article deals with NAA as it is applied to the main divisions of the environment. Each of these sections includes a short summary of the sampling requirements suitable for NAA. Section 3 deals with its application to biological samples and includes a brief discussion on standard reference materials (SRMs) in NAA. Applications to various types of biological material are discussed, ending with a survey of biomonitoring using NAA. The next section (the longest) is the analysis of water by NAA. This is mainly based on the preconcentration and postirradiation procedures currently used for the major types of water (seawater, surface water and underground water). A table of element concentrations in seawater and surface water illustrates the low limits of detection required to determine many trace elements by instrumental neutron activation analysis (INAA). Applications are discussed in the main body of the text. There then follows a section on the use of NAA in air particulate analysis for trace elements. The importance of PM10s (particles with aerodynamic diameter less than 10 µm) to human health and the reasons for concentrating on the analysis of these particles by NAA is discussed. Having discussed the main areas of NAA used there follows an application section. Large‐scale biomonitoring procedures are outlined, particularly those involving plant materials. The final section on major environmental divisions covers the use of NAA in analysis of soils and sediments together with the analysis of coal. This latter topic also includes on‐line analysis of coal using isotope sources. Finally, there is a discussion of speciation and the function of NAA in environmental speciation, particularly atmospheric and aqueous speciation analysis.
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