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Review and synthesis of the effects of elevated atmospheric CO<inf>2</inf> on soil processes: No changes in pools, but increased fluxes and accelerated cycles

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dc.contributor.author Kuzyakov Y.
dc.contributor.author Horwath W.
dc.contributor.author Dorodnikov M.
dc.contributor.author Blagodatskaya E.
dc.date.accessioned 2020-01-21T20:33:31Z
dc.date.available 2020-01-21T20:33:31Z
dc.date.issued 2019
dc.identifier.issn 0038-0717
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/157430
dc.description.abstract © 2018 Elsevier Ltd Atmospheric change encompassing a rising carbon dioxide (CO2) concentration is one component of Global Change that affects various ecosystem processes and functions. The effects of elevated CO2 (eCO2) on belowground processes are incompletely understood due to complex interactions among various ecosystem fluxes and components such as net primary productivity, carbon (C) inputs to soil, and the living and dead soil C and nutrient pools. Here we summarize the literature on the impacts of eCO2 on 1) cycling of C and nitrogen (N), 2) microbial growth and enzyme activities, 3) turnover of soil organic matter (SOM) and induced priming effects including N mobilization/immobilization processes, and 4) associated nutrient mobilization from organic sources, 5) water budget with consequences for soil moisture, 6) formation and leaching of pedogenic carbonates, as well as 7) mobilization of nutrients and nonessential elements through accelerated weathering. We show that all effects in soil are indirect: they are mediated by plants through increased net primary production and C inputs by roots that foster intensive competition between plants and microorganisms for nutrients. Higher belowground C input from plants under eCO2 is compensated by faster C turnover due to accelerated microbial growth, metabolism and respiration, higher enzymatic activities, and priming of soil C, N and P pools. We compare the effects of eCO2 on pool size and associated fluxes in: soil C stocks vs. belowground C input, microbial biomass vs. CO2 soil efflux vs. various microbial activities and functions, dissolved organic matter content vs. its production, nutrient stocks vs. fluxes etc. Based on these comparisons, we generalize that eCO2 will have little impacts on pool size but will strongly accelerate the fluxes in biologically active and stable pools and consequently will accelerates biogeochemical cycles of C, nutrients and nonessential elements.
dc.relation.ispartofseries Soil Biology and Biochemistry
dc.subject Belowground processes
dc.subject Biochemical weathering
dc.subject Carbon and nitrogen cycling
dc.subject Elevated atmospheric CO 2
dc.subject Enzyme activities
dc.subject Microbial growth
dc.subject Plant-microbial interactions
dc.subject Rhizodeposition
dc.title Review and synthesis of the effects of elevated atmospheric CO<inf>2</inf> on soil processes: No changes in pools, but increased fluxes and accelerated cycles
dc.type Review
dc.relation.ispartofseries-volume 128
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 66
dc.source.id SCOPUS00380717-2019-128-SID85055979742


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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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