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量化气候和管理措施对华北平原区域作物产量和氮淋失的影响。

Quantifying climate and management effects on regional crop yield and nitrogen leaching in the north china plain.

出版信息

J Environ Qual. 2013 Sep;42(5):1466-79. doi: 10.2134/jeq2013.03.0086.

DOI:10.2134/jeq2013.03.0086
PMID:24216424
Abstract

Better water and nitrogen (N) management requires better understanding of soil water and N balances and their effects on crop yield under various climate and soil conditions. In this study, the calibrated Root Zone Water Quality Model (RZWQM2) was used to assess crop yield and N leaching under current and alternative management practices in a double-cropped wheat ( L.) and maize ( L.) system under long-term weather conditions (1970-2009) for dominant soil types at 15 locations in the North China Plain. The results provided quantitative long-term variation of deep seepage and N leaching at these locations, which strengthened the existing qualitative knowledge for site-specific management of water and N. In general, the current management practices showed high residual soil N and N leaching in the region, with the amounts varying between crops and from location to location and from year to year. Seasonal rainfall explained 39 to 84% of the variability in N leaching (1970-2009) in maize across locations, while for wheat, its relationship with N leaching was significant ( < 0.01) only at five locations. When N and/or irrigation inputs were reduced to 40 to 80% of their current levels, N leaching generally responded more to N rate than to irrigation, while the reverse was true for crop yield at most locations. Matching N input with crop requirements under limited water conditions helped achieve lower N leaching without considerable soil N accumulation. Based on the long-term simulation results and water resources availability in the region, it is recommended to irrigate at 60 to 80% of the current water levels and fertilize only at 40 to 60% of the current N rate to minimizing N leaching without compromising crop yield.

摘要

更好的水和氮(N)管理需要更好地了解土壤水分和 N 平衡及其在不同气候和土壤条件下对作物产量的影响。本研究利用校准后的根区水质模型(RZWQM2),在华北平原 15 个地点的主要土壤类型上,评估了长期气象条件(1970-2009 年)下现行和替代管理措施下小麦(Triticum aestivum L.)和玉米(Zea mays L.)双季作物系统下的作物产量和 N 淋失。结果提供了这些地点长期深层渗漏和 N 淋失的定量变化,加强了针对特定地点的水和 N 管理的现有定性知识。总的来说,现行管理措施在该地区表现出高残留土壤 N 和 N 淋失,其数量因作物、地点和年份而异。在各个地点,季节降雨量解释了玉米 N 淋失(1970-2009 年)变化的 39%至 84%,而对于小麦,其与 N 淋失的关系仅在五个地点显著(<0.01)。当 N 和/或灌溉投入减少到当前水平的 40%至 80%时,N 淋失通常对 N 率的响应比对灌溉的响应更敏感,而在大多数地点,作物产量的情况则相反。在有限的水资源条件下,根据长期模拟结果和该地区的水资源可用性,建议将灌溉水平降低到当前水平的 60%至 80%,施肥水平降低到当前 N 率的 40%至 60%,以在不影响作物产量的情况下最大限度地减少 N 淋失。

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