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首页> 外文期刊>Journal of Hydrology >Modeling and forecasting riverine dissolved inorganic nitrogen export using anthropogenic nitrogen inputs, hydroclimate, and land-use change
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Modeling and forecasting riverine dissolved inorganic nitrogen export using anthropogenic nitrogen inputs, hydroclimate, and land-use change

机译:利用人为氮输入,水文气候变化和土地利用变化对河流溶解性无机氮出口进行建模和预测

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A quantitative understanding of riverine nitrogen (N) export in response to human activities and climate change is critical for developing effective watershed N pollution control measures. This study quantified net anthropogenic N inputs (NANI) and riverine dissolved inorganic N (DIN = NO_3-N + NH_4-N + NO_2-N) export for the upper Jiaojiang River catchment in eastern China over the 1980-2010 time period and examined how NANI, hydroclimate, and land-use practices influenced riverine DIN export. Over the 31-yr study period, riverine DIN yield increased by 1.6-fold, which mainly results from a ~77% increase in NANI and increasing fractional delivery of NANI due to a -55% increase in developed land area. An empirical model that utilizes an exponential function of NANI and a power function of combining annual water discharge and developed land area percentage could account for 89% of the variation in annual riverine DIN yields in 1980-2010. Applying this model, annual NANI, catchment storage, and natural background sources were estimated to contribute 57%, 22%, and 21%, respectively, of annual riverine DIN exports on average. Forecasting based on a likely future climate change scenario predicted a 19.6% increase in riverine DIN yield by 2030 due to a 4% increase in annual discharge with no changes in NANI and land-use compared to the 2000-2010 baseline condition. Anthropogenic activities have increased both the N inputs available for export and the fractional export of N inputs, while climate change can further enhance riverine N export. An integrated N management strategy that considers the influence of anthropogenic N inputs, land-use and climate change is required to effectively control N inputs to coastal areas.
机译:对响应人类活动和气候变化的河流氮(N)出口的定量了解对于制定有效的流域氮污染控制措施至关重要。这项研究量化了1980-2010年期间中国东部椒江上游流域的人为净氮输入(NANI)和河流溶解无机氮(DIN = NO_3-N + NH_4-N + NO_2-N)出口,并研究了如何NANI,水气候和土地利用方式影响了DIN河的出口。在31年的研究期内,河道DIN的产量增加了1.6倍,这主要是由于NANI的增加了约77%,以及由于发达土地面积增加了-55%所致的NANI的分批交付量增加。一个利用NANI的指数函数和将年排水量与已开发土地面积百分比相结合的幂函数的经验模型可以解释1980-2010年河道DIN年产量变化的89%。应用该模型,估计每年的NANI,集水区存储和自然本底源分别分别占河流DIN年度年出口量的57%,22%和21%。根据未来可能发生的气候变化情景进行的预测预测,到2030年,由于2000年至2010年基线条件下年排放量增加4%,而NANI和土地利用均未发生变化,河流DIN的产量将增加19.6%。人为活动增加了可用于出口的氮投入和氮投入的部分出口,而气候变化可进一步促进河流氮的出口。需要一种综合的氮管理战略,考虑人为氮输入,土地利用和气候变化的影响,以有效地控制向沿海地区的氮输入。

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