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首页> 外文期刊>Agricultural and Forest Meteorology >Enhancing soil drought induced by climate change and agricultural practices: Observational and experimental evidence from the semiarid area of northern China
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Enhancing soil drought induced by climate change and agricultural practices: Observational and experimental evidence from the semiarid area of northern China

机译:增强气候变化和农业实践引起的土壤干旱:来自中国北方半干旱地区的观察和实验证据

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Increased water scarcity has led to a decade-long soil drought in the semiarid area of northern China, which caused food insecurity in this region. However, there is a lack of sufficient observational evidence about how climate change and agricultural practices have interactively affected this soil drought. Long-term in situ soil moisture measurements collected in agricultural experimental plots indicate that the mean temperature and precipitation during the growing season have reduced soil moisture by 11.2%, and agricultural practices have aggravated the soil drying trend in the 0-100 mm soil layer over the past three decades. Our results also show that planting water-expensive crops (e.g., potato and maize) may aggravate soil drought. Crop rotation increases soil water consumption by 8.9-12.6% over continuous cropping. Excessive fertilizer use increases water consumption by 25.4-46.9% and decreases the water use efficiency (WUE) by 14.6-35.3%, while tillage accounts for the consumption of 10.3% more soil moisture than no-tillage. Our results indicate that agricultural practices, including crop rotation, a high fertilizer input, and tillage, may increase water consumption and aggravate soil drying. Our findings call for effective strategies for mitigating soil drought in semiarid regions, such as an adjustment of the cropping system, reduced fertilizer use, and improved conservation tillage.
机译:增加的水资源稀缺导致了中国北方半干旱地区的十多年的土壤干旱,导致该地区的食物不安全。然而,缺乏足够的观察证据,了解气候变化和农业实践如何交互地影响这种土壤干旱。在农业实验局部收集的长期原位土壤水分测量表明,生长季节的平均温度和降水量降低了土壤水分,减少了11.2%,农业实践加剧了0-100毫米土层的土壤干燥趋势过去三十年。我们的结果还表明,种植水昂贵的作物(例如,马铃薯和玉米)可能会加重土壤干旱。作物旋转在连续种植中将土壤耗水量增加了8.9-12.6%。过度肥料使用将耗水量增加25.4-46.9%,并将水利用效率(WUE)降低14.6-35.3%,而耕作占土壤水分的消耗量比无耕作量增加10.3%。我们的结果表明,农业实践,包括作物旋转,高肥料投入和耕作,可能会增加耗水量和加剧土壤干燥。我们的调查结果呼吁有效策略用于修复半干旱地区的土壤干旱,例如调整种植系统,减少肥料使用和改进的保护耕作。

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