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首页> 外文期刊>Journal of Environmental Quality >Quantifying climate and management effects on regional crop yield and nitrogen leaching in the North China Plain.
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Quantifying climate and management effects on regional crop yield and nitrogen leaching in the North China Plain.

机译:量化气候和管理对华北平原地区作物产量和氮素淋失的影响。

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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 (Triticum aestivum L.) and maize (Zea mays 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 (P<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.
机译:更好的水和氮(N)管理要求更好地了解土壤水和氮的平衡及其在各种气候和土壤条件下对作物产量的影响。在这项研究中,使用校准的根区水质模型(RZWQM2)来评估双季小麦(Triticum aestivum L.)和玉米(Zea mays L.)系统下当前和其他管理方式下的作物产量和氮淋失。在华北平原15个地区的长期天气条件(1970-2009)下主要土壤类型。结果提供了这些位置深层渗漏和N淋失的定量长期变化,从而加强了针对水和N的特定地点管理的现有定性知识。总体而言,当前的管理实践表明,土壤中氮和N的残留量很高。该地区的产量因作物而异,各地之间以及每年之间都有所不同。季节性降雨解释了不同地区玉米氮素淋失(1970-2009年)的39%至84%的变化,而对于小麦,其与氮素淋溶的关系仅在五个地点显着(P <0.01)。当氮和/或灌溉投入减少到当前水平的40%到80%时,氮淋失对氮素的反应通常比对灌溉的响应更大,而在大多数地方,农作物的产量却相反。在有限的水分条件下使氮素输入量与作物需求相匹配,有助于减少氮素的淋失,而不会大量累积土壤氮素。根据长期的模拟结果和该地区的水资源可用性,建议以当前水位的60%至80%进行灌溉,仅以当前氮素水平的40%至60%施肥,以最大程度地减少氮素的淋失而不损害土壤作物产量。

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