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Contrasting effects of organic and mineral nitrogen challenge the N-Mining Hypothesis for soil organic matter priming

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dc.contributor.author Mason-Jones K.
dc.contributor.author Schmücker N.
dc.contributor.author Kuzyakov Y.
dc.date.accessioned 2019-01-22T20:34:26Z
dc.date.available 2019-01-22T20:34:26Z
dc.date.issued 2018
dc.identifier.issn 0038-0717
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/147771
dc.description.abstract © 2018 Elsevier Ltd Addition of easily available organic substances to soil often increases the CO2 efflux from pre-existing soil carbon (C). This phenomenon is often explained in terms of the Nitrogen (N)-Mining Hypothesis. According to this proposed – but never conclusively proven – mechanism, increased C availability induces N limitation in microbes, which then access N by degrading soil organic matter (SOM) – a priming effect. This is supported by some experiments demonstrating reduced CO2 efflux after mineral N addition. However, amino acids cause priming, despite their very low C:N ratios and rapid deamination to mineral N. To explore this contradiction, we applied 14C- and 15N-labelled C and N sources (glucose, alanine and ammonium sulfate) to rigorously test two key predictions of the N-Mining Hypothesis: (i) an amino acid should stimulate much less priming than glucose, and (ii) priming should be similarly suppressed for an amino acid or a stoichiometrically equivalent addition of glucose plus mineral N. Both of these key predictions of the N-Mining Hypothesis failed. Efflux of CO2 from native C was essentially determined by the type and amount of C added, with alanine stimulating more priming than glucose (16–50% cumulative increase relative to control, versus 0–25%, respectively). Higher C additions caused more priming than low additions. Mineral N reduced native-C-derived CO2 efflux when added alone or with organic substrates, but this effect was independent of the organic C additions and did not influence C-induced priming. These results were inconsistent with the hypothesized role of N mining in priming. We conclude that the N-Mining Hypothesis, at least in its current form, is not a universal explanation for observed priming phenomena. Instead, we observed a strong correlation between the rates of priming and the mineralization of the added substrates, especially during the first 8 days. This indicated that priming was best explained by energy-induced synthesis of SOM-degrading exoenzymes, possibly in combination with apparent priming from accelerated turnover of microbial biomass.
dc.relation.ispartofseries Soil Biology and Biochemistry
dc.subject Alanine
dc.subject Amino acids
dc.subject Carbon and nitrogen interactions
dc.subject Low molecular weight organic substances
dc.subject Priming effect
dc.subject Sugars
dc.title Contrasting effects of organic and mineral nitrogen challenge the N-Mining Hypothesis for soil organic matter priming
dc.type Article
dc.relation.ispartofseries-volume 124
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 38
dc.source.id SCOPUS00380717-2018-124-SID85047880769


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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