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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 N deposition, synthetic N fertilizer, agricultural N fixation and N in net food and feed imports from 15 catchments in the Lake Dianchi basin were determined over an 11-year period (2000-2010). The 15 catchments range in size from 44 km~2 to 316 km~2 with an average of 175 km~2. To reduce uncertainty from scale change methodology, results from data extraction by area-weighting and land use-weighting methods were compared. Results show that the methodology for extrapolating data from the county scale to watersheds has a great influence on NANI computation for catchments in the Lake Dianchi basin, and that estimates of NANI between the two methods have an average difference of 30% on a catchment basis, while a smaller difference (15 %) was observed on the whole Lake Dianchi basin basis. The riverine N export has a stronger linear relationship with NANI computed by the land useweighting method, which we believe is more reliable. Overall, nitrogen inputs assessed by the NANI approach for the Lake Dianchi basin are 9900 kgNkm~(-2) yr~(-1), ranging from 6600 to 28 000 kgNkm~(-2) yr~(-1) among the 15 catchments. Synthetic N fertilizer is the largest component of NANI in most subwatersheds. On average, riverine flux of nitrogen in catchments of the Lake Dianchi basin averages 83 % of NANI, far higher than generally observed in North America and Europe. Saturated N sinks and a limited capacity for denitrification in rivers may be responsible for this high percentage of riverine N export. Overall, the NANI methodology should be applicable in small watersheds when sufficiently detailed data are available to estimate its components.
机译:在11年期间(2000-2010年)确定了人为净氮输入量(NANI),包括大气氮沉降,合成氮肥,农业固氮和净食物和饲料中氮的含量,这些元素来自滇池盆地15个流域。 。 15个流域的规模从44 km〜2到316 km〜2,平均为175 km〜2。为了减少尺度变化方法的不确定性,比较了通过面积加权和土地使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,两种方法之间的NANI估算值在流域的基础上平均相差30%,而整个滇池流域的差异较小(15%)。用土地利用权重法计算得出的河流氮素与NANI的线性关系更强,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为9900 kgNkm〜(-2)yr〜(-1),在15个国家中为6600至28000 kgNkm〜(-2)yr〜(-1)。流域。在大多数流域中,合成氮肥是NANI的最大组成部分。平均而言,滇池盆地流域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。饱和氮汇和河流中反硝化能力有限可能是造成河流氮高比例出口的原因。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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