Plant effects on soil N mineralization are mediated by the composition of multiple soil organic fractions

Dario A. Fornara, Richard Bardgett, Sibylle Steinbeiss, Donald R. Zak, Gerd Gleixner, David Tilman

    Research output: Contribution to journalArticlepeer-review

    Abstract

    Despite the topic of soil nitrogen (N) mineralization being well-studied, very few studies have addressed the relative contribution of different plant and soil variables in influencing soil N mineralization rates, and thus the supply of inorganic N to plants. Here, we used data from a well-studied N-limited grassland to address the relative effects of six plant and soil variables on net and on gross rates of soil N mineralization. We also addressed whether plant effects on soil N mineralization were mediated by changes in C and N concentrations of multiple soil organic matter (SOM) fractions. Regression analyses show that key plant traits (i.e., plant C:N ratios and total root mass) were more important than total C and N concentrations of bulk soil in influencing N mineralization. This was mainly because plant traits influenced the C and N concentration (and C:N ratios) of different SOM fractions, which in turn were significantly associated with changes in net and gross N mineralization. In particular, C:N ratios of a labile soil fraction were negatively related to net soil N mineralization rates, whereas total soil C and N concentrations of more recalcitrant fractions were positively related to gross N mineralization. Our study suggests that changes in belowground N-cycling can be better predicted by simultaneously addressing how plant C:N ratios and root mass affect the composition and distribution of different SOM pools in N-limited grassland systems. © 2010 The Ecological Society of Japan.
    Original languageEnglish
    Pages (from-to)201-208
    Number of pages7
    JournalEcological Research
    Volume26
    Issue number1
    DOIs
    Publication statusPublished - 2011

    Keywords

    • Ecosystem process
    • Nitrogen cycling
    • Soil density fractionation
    • Soil organic matter

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