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A DRAINMOD-based method to estimate effects of drainage water management on annual nitrogen loss to surface water.

机译:一种基于DRAINMOD的方法,用于估算排水管理对地表水年氮损失的影响。

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Effects of drainage water management (DWM) on nitrogen (N) losses to surface waters can be estimated by multiplying the change in subsurface drainage and surface runoff, as predicted by DRAINMOD, by long-term mean nitrogen (N) concentration, which is a function of local site conditions (climate, soil, cropping system, farming practices, and drainage system). Consistent with experimental observations from several sources, this approximate method assumes that the effect of DWM on N losses is proportional to its effect on drainage and surface runoff volumes. The reliability of the method was evaluated by comparing estimated annual N losses for two sites (one in North Carolina and one in Illinois) to those predicted by the process-based nitrogen model DRAINMOD-NII. The long-term N concentrations used in the approximate method were based on DRAINMOD-NII predictions. DRAINMOD-NII simulations predicted that DWM would reduce long-term average N losses to surface waters by 35% for continuous corn (CC) and 33% for a corn-wheat-soybean (CWS) rotation in North Carolina and by 31% and 26% for CC and a corn-soybean (CS) rotation in Illinois. The approximate method estimated the annual effect of DWM on N losses within 3 kg ha-1 of that predicted by DRAINMOD-NII in over 68% of the years for the CWS and CS rotations at both sites and in over 51% of the years for CC. Overestimated effects in some years were balanced by underestimated effects in others. However, relatively large errors occurred in about 25% of the years when N concentrations in the drainage water varied significantly from the long-term average. These errors typically occurred following periods when crop yields deviated significantly from the average. When these outliers were excluded from the analyses, the goodness of fit between annual N losses predicted by DRAINMOD-NII and annual losses estimated by the approximate method was substantially improved (Nash-Sutcliffe EF values ranging from 0.54 to 0.79). Although more research is needed to improve the approximate method when concentrations vary significantly from the long-term average, the results presented herein indicate that the method provides a reliable means of assessing impacts of DWM under normal conditions.
机译:可以通过将DRAINMOD预测的地下排水和地表径流的变化乘以长期平均氮(N)浓度来估算排水管理(DWM)对地表水氮(N)损失的影响。当地条件的功能(气候,土壤,耕作系统,耕作方式和排水系统)。与来自多个来源的实验观察结果一致,该近似方法假设DWM对N损失的影响与其对排水和地表径流量的影响成正比。通过将两个地点(北卡罗来纳州一个地点和伊利诺伊州一个地点)的估计年度氮损失与基于过程的氮模型DRAINMOD-NII预测的氮损失进行比较,评估了该方法的可靠性。近似方法中使用的长期N浓度基于DRAINMOD-NII预测。 DRAINMOD-NII模拟预测,在北卡罗莱纳州,连续玉米(CC)连续施用玉米(CC)可使地表水长期长期平均氮损失减少35%,玉米-小麦-大豆(CWS)减少33%,长期减少26 CC和伊利诺伊州玉米-玉米(CS)轮换的百分比。近似方法估计DWM对DRAINMOD-NII预测的在超过68%的年内两个站点和CWS轮换的NWS的年度损失在3 kg ha -1 之内的年度影响。 CC超过51%的年份。在某些年份,高估的效果与在另一些年份的低估的效果相抵消。但是,当排水中的氮浓度与长期平均值相比有显着差异时,大约25%的年份中会发生相对较大的误差。这些错误通常发生在作物单产大大偏离平均水平的时期之后。当将这些离群值排除在分析范围之外时,DRAINMOD-NII预测的年度N损失与近似方法估计的年度N损失之间的拟合优度大大提高了(Nash-Sutcliffe EF值介于0.54至0.79之间)。尽管当浓度与长期平均值相比有显着差异时,需要进行更多的研究来改善近似方法,但此处显示的结果表明,该方法提供了一种评估正常条件下DWM影响的可靠方法。

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