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10. Label vial with the sample identification shown on the field container. <br /> 11. Mix sample thoroughly by tumbling the vial end-over-end before <br /> subsampling for laboratory procedures (primarily chemical analyses). <br /> 3.2 CHEMICAL METHODS <br /> 3.2.1 S <br /> Chemical methods for characterizing overburdens and minesoils are given. <br /> For a particular parameter, more than one method may be listed. This will <br /> allow the user of the manual some freedom of choice. <br /> The determination of toxic or nontoxic materials due to acidity is over- <br /> riding in importance in the Appalachian and Eastern and Western Interior <br /> Coal Provinces. The methods for determining toxic or potentially toxic <br /> materials are given high priority and are listed at the very front of the <br /> chapter. Methods 3.2.2, 3.2.3, 3.2.4, and 3.2.6 are used to determine the <br /> acid-base balance of minesoils and overburdens. <br /> Next in importance is the nutrient status of the overburden materials. <br /> Nutrient status can be measured by using methods 3.2.5, 3.2.6, and 3.2.15. <br /> These methods give a measure of plant nutrients such as phosphorus, <br /> potassium, calcium, magnesium, and nitrogen. A knowledge of what plant <br /> UV nutrients are contained in an overburden material enables the mine operator <br /> to efficiently plan the mining operation so that full advantage can be <br /> taken of these nutrients in the resulting minesoil. <br /> For more intensive study of minesoils and overburden materials, procedures <br /> for determining the cation exchange capacity (3.2.16 and 3.2.17) are given. <br /> Ways of estimating the lime requirement in minesols are presented in <br /> _ methods 3.2.7 through 3.2.10. Also, methods applicable to anid-and-semi <br /> and regions have been included. <br /> -- -3.2.2 -Paste PH - <br />-r 3.2.2.1 Principle-- <br /> Perhaps the most commonly measured soil characteristic is pH. Soil pH was <br /> defined by Sorensen (1909) as the negative logarithm of the hydrogen--ion <br /> concentration. However, in actuality, hydrogen-ion activity is measured <br /> instead of hydrogen-ion concentration. <br /> Soil pH is measured by a glass electrode incorporated with a pH meter for <br /> - this-procedure." Water is 6 ed_ta_the sample Forming a paste. The electrode ____ <br /> is placed in the paste with pH being read directly from the meter. <br /> 3.2.2.2 Comments-- - <br /> Six factors affecting the measurement of pH are: (1) drying the soil sample <br /> during preparation; (2) soil:water ratio used; (3) soluble salts content; <br /> 45 i <br />