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Long-term Changes of Nitrogen, Carbon and Phosphor Fluxes of a Typical Agricultural Landscape in North China Plain

机译:华北平原典型农业景观氮,碳和磷通量的长期变化

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Biogeochemical cycles of carbon, nitrogen, phosphor and sulfur are the most important processes in agricultural landscape, which more or less contributes to global changes. Based on the resource data got from household surveys combined with land use data derived from remote sensing imagery, this article studied on the long-term changes of main life elements (C, N and P) fluxes in a typical agricultural landscape of North China Plain. The results show that C and N balances of large-scale irrigated land changed from deficits (-865kg/hm2 C and -9kg/hm2 N) in 1945 into great surpluses (1761kg/hm2 C and 213kg/hm2 N) in 2002, respectively, and P surpluses also doubled in 2002. However, C and N fluxes showed deficit during both periods with more significantly in 2002. C, N and P fluxes in whole arable landscape showed significant surpluses despite of 18.75% total arable area decrease in 2002 than that in 1945. Contrarily, C and N fluxes of arable landscape in 1945 showed overall deficits. Nutrient flux changes of arable landscape are impacted mainly by the changes of fertilizer input, land productivity, crop residue utility and arable land types.
机译:碳,氮,磷和硫的生物地球化学循环是农业景观中最重要的过程,或多或少地有助于全球变化。基于家庭调查获得的资源数据,结合遥感影像获得的土地利用数据,研究了华北平原典型农业景观中主要生命元素(碳,氮和磷)通量的长期变化。 。结果表明,大型灌溉土地的碳和氮平衡从1945年的赤字(-865kg / hm2 C和-9kg / hm2 N)变为2002年的大量盈余(1761kg / hm2 C和213kg / hm2 N)。 ;和P盈余在2002年也翻了一番。但是,C和N的通量在两个时期都显示出赤字,在2002年更为明显。尽管2002年的耕地总面积减少了18.75%,但整个耕地中的C,N和P的通量显示出了显着的盈余。相反,1945年耕地中的碳和氮通量却显示出总体赤字。耕地景观养分通量变化主要受到肥料投入,土地生产力,农作物残渣利用度和耕地类型变化的影响。

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