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The international standards to determine A in water quality and soil quality are both B methods. The Chinese standard to determine A in water quality now is still adopt C method which was abolished by ISO. However, the C method provides unstable testing results and has certain toxicity by using large amounts of D. What¡¯s more, it also has some disadvantages of more reagents, complex operation, and determination of one element at one time. And that in soil is E method. Compared to B method which is adopted by ISO, the main advantage of the E method is the improved limit of detection, typically 10 to 20 times. However, the B method has the most serious disadvantage of poor resistance against atomization interferences and often unsatisfactory linearity of calibration curves. The US EPA has proposed a method of F for the analysis of A in water. It requires few reagents and instruments, but more interference is obtained.
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B method is the international standards to measure A in both water and soil. The Chinese standard still adopts expired ISO method C to analyze A in water. However, the C method provides inconsistent test results and requires/consumes a large amount of D with high toxicity. Furthermore, it also has some disadvantages including demand of many reagents, complexity and low efficiency (1 element per test). E method is adapted in the chinese standard as of now. Compared to ISO B method, the E method shows an improved detection limit, typically by a factor of 10 to 20. Moreover, the B method has poor resistance against atomization interference and often displays NONLINEAR calibration curves. The US EPA SUGGESTS TO USE METHODE F for the analysis of A in water. It requires LESS reagents and instruments, but more interference CAN BE OBSERVED.

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