Isotopic (13C) fractionation during plan
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Marina Schweizer; John Fear; Georg Cadisch
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Article
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1999
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John Wiley and Sons
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English
โ 88 KB
Carbon isotopic fractionations in plant materials and those occurring during decomposition have direct implications in studies of short-and longer-term soil organic matter dynamics. Thus the products of decomposition, the evolved CO 2 and the newly formed soil organic matter, may vary in their 13 C