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Modelling the effects of climate variability and water management on crop water productivity and water balance in the North China Plain. (Special Issue: Crop water use efficiency at multiple scales.)

机译:对华北平原气候变化和水资源管理对作物水分生产率和水分平衡的影响进行建模。 (特刊:多种尺度的作物水分利用效率。)

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In the North China Plain (NCP), while irrigation using groundwater has maintained a high-level crop productivity of the wheat-maize double cropping systems, it has resulted in rapid depletion of groundwater table. For more efficient and sustainable utilization of the limited water resources, improved understanding of how crop productivity and water balance components respond to climate variations and irrigation is essential. This paper investigates such responses using a modelling approach. The farming systems model APSIM (Agricultural Production Systems Simulator) was first calibrated and validated using 3 years of experimental data. The validated model was then applied to simulate crop yield and field water balance of the wheat-maize rotation in the NCP. Simulated dryland crop yield ranged from 0 to 4.5 t ha-1 for wheat and 0 to 5.0 t ha-1 for maize. Increasing irrigation amount led to increased crop yield, but irrigation required to obtain maximum water productivity (WP) was much less than that required to obtain maximum crop yield. To meet crop water demand, a wide range of irrigation water supply would be needed due to the inter-annual climate variations. The range was simulated to be 140-420 mm for wheat, and 0-170 mm for maize. Such levels of irrigation applications could potentially lead to about 1.5 m year-1 decline in groundwater table when other sources of groundwater recharge were not considered. To achieve maximum WP, one, two and three irrigations (i.e., 70, 150 and 200 mm season-1) were recommended for wheat in wet, medium and dry seasons, respectively. For maize, one irrigation and two irrigations (i.e., 60 and 110 mm season-1) were recommended in medium and dry seasons, while no irrigation was needed in wet season.
机译:在华北平原,使用地下水灌溉保持了小麦-玉米双作系统的高水平作物生产力,但导致地下水位快速枯竭。为了更有效和可持续地利用有限的水资源,必须更好地了解作物生产力和水平衡要素如何应对气候变化和灌溉。本文使用建模方法研究了此类响应。首先使用3年的实验数据对农业系统模型APSIM(农业生产系统模拟器)进行了校准和验证。然后,将经过验证的模型用于模拟NCP中小麦-玉米轮作的作物产量和田间水分平衡。小麦的旱地作物模拟产量为0-4.5 t ha -1 ,玉米为0-5.0 t ha -1 。灌溉量的增加导致农作物产量的增加,但是获得最大水分生产率(WP)所需的灌溉量远远少于获得最大作物产量所需的灌溉量。为了满足农作物的水需求,由于年际气候变化,将需要大量的灌溉水供应。模拟范围为小麦为140-420毫米,玉米为0-170毫米。如果不考虑其他地下水补给源,这样的灌溉水平可能导致地下水位下降约150万年 -1 。为了获得最大的WP,建议在湿季,中季和旱季分别对小麦进行一,二和三次灌溉(即70、150和200 mm季节 -1 )。对于玉米,建议在旱季和旱季进行一次灌溉和两次灌溉(即60和110 mm季节 -1 ),而在潮湿季节则不需要灌溉。

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