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Estimating net anthropogenic nitrogen inputs (NANI) in the Lake Dianchi basin of China

机译:估算中国滇池流域的人为氮净输入量(NANI)

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Net anthropogenic nitrogen inputs (NANI) with components of atmospheric Ndeposition, synthetic N fertilizer, agricultural N fixation and N in net foodand feed imports from 15 catchments in the Lake Dianchi basin were determinedover an 11-year period (2000–2010). The 15 catchments range in size from44 km2 to 316 km2 with an average of 175 km2. To reduceuncertainty from scale change methodology, results from data extraction byarea-weighting and land use-weighting methods were compared. Results showthat the methodology for extrapolating data from the county scale towatersheds has a great influence on NANI computation for catchments in theLake Dianchi basin, and that estimates of NANI between the two methods havean average difference of 30% on a catchment basis, while a smallerdifference (15%) was observed on the whole Lake Dianchi basin basis. Theriverine N export has a stronger linear relationship with NANI computed bythe land use-weighting method, which we believe is more reliable. Overall,nitrogen inputs assessed by the NANI approach for the Lake Dianchi basin are9900 kg N km?2 yr?1, ranging from 6600 to28 000 kg N km?2 yr?1 among the 15 catchments. Synthetic Nfertilizer is the largest component of NANI in most subwatersheds. Onaverage, riverine flux of nitrogen in catchments of the Lake Dianchi basinaverages 83% of NANI, far higher than generally observed in NorthAmerica and Europe. Saturated N sinks and a limited capacity fordenitrification in rivers may be responsible for this high percentage ofriverine N export. Overall, the NANI methodology should be applicable insmall watersheds when sufficiently detailed data are available to estimateits components.
机译:在过去的11年中(2000-2010年)确定了人为净氮输入量(NANI),包括大气N沉积,合成氮肥,农业固氮和净食物中的氮以及从滇池流域15个集水区进口的饲料。 15个集水区的大小从44 km 2 到316 km 2 ,平均175 km 2 。为了降低尺度变化方法的不确定性,比较了面积加权和土地利用加权方法提取数据的结果。结果表明,从县级尺度向流域外推数据的方法对滇池流域的NANI计算有很大影响,并且两种方法之间的NANI估算值在流域的基础上平均相差30%,而差异较小(在整个滇池盆地基础上观察到了15%的水。氮素出口量与土地利用加权法计算得出的NANI有更强的线性关系,我们认为这更可靠。总体而言,通过NANI方法评估的滇池流域的氮输入量为9900 kg N km 2 yr ?1 ,范围为6600至28000 kg N km ? 15个流域中有2 yr ?1 。在大多数流域中,合成肥料是NANI的最大组成部分。平均而言,滇池盆地集水区的河流氮通量平均为NANI的83%,远高于北美和欧洲的普遍水平。河流中氮含量高的原因可能是饱和的氮汇和河流中有限的脱氮能力。总体而言,如果有足够详细的数据来估算其组成部分,则NANI方法应适用于小流域。

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