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    <identifier>10.11922/sciencedb.00912</identifier>
    <datestamp>2021-07-15T16:17:31Z</datestamp>
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<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:date>2021-07-15</dc:date>
  <dc:title>Topography modulates effects of nitrogen deposition on soil nitrous oxide emission in a subtropical forest</dc:title>
  <dc:identifier>doi:10.11922/sciencedb.00912</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>Forests are increasingly recognized as a significant source of atmospheric nitrous oxide (N2O) under elevated atmospheric nitrogen (N) deposition. Nevertheless, it is still unclear whether topography modulates the responses of soil N2O emission to elevated N deposition. Here, N was applied as NH4NO3 in three levels, i.e., 0 (Control), 50 (moderate N) and 100 (high N) kg N ha&amp;ndash;1 yr&amp;ndash;1 in the valley and on the slope of a subtropical forest in southwest China. Soil N2O emission along with microbial functional gene abundances (ammonia&amp;ndash;oxidizing bacteria (AOB) and archaea (AOA) amoA, nirK, nirS, fungal nirK, nosZI and nosZII) and soil properties were measured in responses to three years of N addition. The cumulative N2O fluxes were 1.15 &amp;plusmn; 0.25 kg N ha&amp;ndash;1 in the valley and 1.25 &amp;plusmn; 0.35 kg N ha&amp;ndash;1 on the slope under the control. Nitrogen addition increased cumulative soil N2O emission by 87&amp;ndash;176% in the valley and 27&amp;ndash;143% on the slope. In the valley, the stimulation of N2O emission by N addition was mainly due to increase of ammonium availability and AOB amoA abundances but decrease of AOA:AOB amoA ratio. On the slope, the stimulation was mainly explained by increase of nitrate availability, AOB amoA and nirK abundances. Furthermore, the stimulation of N2O emission by moderate N addition was significantly greater in the valley than on the slope largely owing to the lower N status in the valley. This work highlights the importance of topography in regulating the responses of soil N2O emission to elevated N deposition.&amp;nbsp;</dc:description>
  <dc:subject>Subtropical forest; Nitrogen deposition; Topography; Nitrous oxide; Functional genes</dc:subject>
  <dc:creator>Pengpeng Duan</dc:creator>
  <dc:creator>Daobo Wang</dc:creator>
  <dc:creator>Kongcao Xiao</dc:creator>
  <dc:creator>Liang Zheng</dc:creator>
  <dc:creator>Hao Chen</dc:creator>
  <dc:creator>Kelin Wang</dc:creator>
  <dc:creator>Dejun Li</dc:creator>
  <dc:rights>PUBLIC</dc:rights>
  <dc:rights>https://creativecommons.org/licenses/by/4.0/</dc:rights>
  <dc:type>dataset</dc:type>
  <dc:publisher>Science Data Bank</dc:publisher>
</oai_dc:dc>

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