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	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>7</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bg-7-409-2010</doi>
	<article_url>http://www.biogeosciences.net/7/409/2010/</article_url>
	<abstract_html>http://www.biogeosciences.net/7/409/2010/bg-7-409-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/7/409/2010/bg-7-409-2010.pdf</fulltext_pdf>
	<start_page>409</start_page>
	<end_page>425</end_page>
	<publication_date>2010-02-02</publication_date>
	<article_title content_type="html">Soil organic carbon dynamics under long-term fertilizations in arable land of northern China</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. J. Zhang</name>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>X. J. Wang</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. G. Xu</name>
			<email>mgxu@caas.ac.cn</email>
		</author>
		<author numeration="4" affiliations="4">
			<name>S. M. Huang</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>H. Liu</name>
		</author>
		<author numeration="6" affiliations="6">
			<name>C. Peng</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Ministry of Agriculture Key Laboratory of Crop Nutrition and Fertilization, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China</affiliation>
		<affiliation numeration="2" content_type="html">Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, 830000, China</affiliation>
		<affiliation numeration="3" content_type="html">Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740, USA</affiliation>
		<affiliation numeration="4" content_type="html">Inst. of Soil and Fertilizer, Henan Academy of Agricultural Sciences, Zhengzhou, Henan 450002, China</affiliation>
		<affiliation numeration="5" content_type="html">Inst. of Soil and Fertilizer &amp; Agricultural sparing water, Xinjiang Academy of Agricultural Sciences, Urumqi 830091, China</affiliation>
		<affiliation numeration="6" content_type="html">Inst. of Soil and Fertilizer, Jilin Academy of Agricultural Sciences, ChangChun, 130001, China</affiliation>
	</affiliations>
	<abstract content_type="html">Soil carbon sequestration is a complex process influenced by agricultural
practices, climate and soil conditions. This paper reports a study of
long-term fertilization impacts on soil organic carbon (SOC) dynamic from
six long-term experiments. The experiment sites are located from
warm-temperate zone with a double-cropping system of corn (&lt;i&gt;Zea mays&lt;/i&gt; L.) – wheat
(&lt;i&gt;Triticum Aestivium&lt;/i&gt; L.) rotation, to mild-temperate zones with mono-cropping systems of
continuous corn, or a three-year rotation of corn-wheat-wheat. Mineral
fertilizer applications result in an increasing trend in SOC except in the
arid and semi-arid areas with the mono-cropping systems.
Additional manure application is important to maintain SOC level in the arid
and semi-arid areas. Carbon conversion rate is significant lower in the
warm-temperate zone with double cropping system (6.8%–7.7%) than that
in the mild-temperate areas with mono-cropping systems (15.8%–31.0%).
The conversion rate is significantly correlated with annual precipitation
and active accumulative temperature, i.e., higher conversion rate under
lower precipitation and/or temperature conditions. Moreover, soil high in
clay content has higher conversion rate than soils low in clay content. Soil
carbon sequestration rate ranges from 0.07 to 1.461 t ha&lt;sup&gt;&amp;minus;1&lt;/sup&gt; year&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
in the upland of northern China. There is significantly linear correlation
between soil carbon sequestration and carbon input at most sites, indicating
that these soils are not carbon-saturated thus have potential to migrate
more CO&lt;sub&gt;2&lt;/sub&gt; from atmosphere.</abstract>
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</article>

