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Impact of temporal change of land use and cropping system on some soil properties in northwestern parts of Indo-Gangetic Plain

机译:印岗西北土地利用和种植制度的时间变化对土壤性质的影响。

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Soil series representing different physiographic units were studied to know the impact of temporal change in land use and cropping system on some soil properties in the northwestern parts of the Indo-Gangetic Plain. The dynamics in land use and cropping system for the period 1983-84, 1996-97 and 2007-2008 and change in soil properties for the period 1983 and 2008 were studied. In Singhpur soil series developed on Shiwalik hills, the soil organic carbon (SOC) content decreased from 0.69% in 1983 to 0.40% in 2008 on account of increased deforestation and soil erosion. However, no significant changes were observed in soil pH and electrical conductivity (EC). In Manjuwal (upper piedmont plain) and Mandiani series (lower piedmonts) slight changes in SOC, pH, EC and calcium carbonate were found. In Naura series (normal soils), occurring in the old flood plain, SOC content of surface soils increased to > 1.0% in 2008 compared to 0.41% in 1983 because of shifting of cropping system of maize-wheat to high biomass-producing cropping system (rice-wheat, rice-potato/mustard/peas/sunflower) and addition of fertilizers under high management practices. The soil pH and EC decreased slightly during 1983 to 2008. Similar results were also observed in Bhaura series (salt-affected soils) and Bairsal series in recent flood plains. Thus, the land use and cropping system in less-intensive cultivated areas of Shiwalik hills and piedmonts do not have much influence on the soil properties. However, in intensively cultivated areas of old and recent flood plains, where high biomass-producing rice-wheat system replaced wheat-maize system, the soil properties had changed to a large extent.
机译:研究了代表不同生理单位的土壤序列,以了解土地利用和耕作制度的时间变化对印度恒河西北部某些土壤性质的影响。研究了1983-84年,1996-97年和2007-2008年期间土地利用和耕作制度的动态以及1983年和2008年期间土壤性质的变化。在Shiwalik丘陵上开发的Singhpur土壤系列中,由于森林砍伐和土壤侵蚀增加,土壤有机碳(SOC)含量从1983年的0.69%降至2008年的0.40%。然而,在土壤pH和电导率(EC)方面未观察到显着变化。在Manjuwal(上山前平原)和Mandiani系列(下山前)中,SOC,pH,EC和碳酸钙略有变化。在Naura系列(正常土壤)中,发生在旧的洪泛平原上,由于玉米小麦的种植系统向高生物量生产的种植系统转变,表层土壤的SOC含量从1983年的0.41%增加到2008年的> 1.0% (大米,马铃薯,芥末,豌豆,向日葵等),并在严格的管理规范下添加化肥。在1983年至2008年期间,土壤的pH值和EC略有下降。在最近的洪泛平原中,Bhaura系列(受盐影响的土壤)和Bairsal系列中也观察到了类似的结果。因此,Shiwalik丘陵和山前丘陵耕种程度较低的耕种区的土地利用和耕作制度对土壤特性的影响不大。但是,在老旧的平原平原的集约化耕种地区,高生物量生产的稻麦系统取代了小麦玉米系统,土壤性质发生了很大变化。

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