首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effect of vegetation restoration on soil and water erosion and nutrient losses of a severely eroded clayey Plinthudult in southeastern China
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Effect of vegetation restoration on soil and water erosion and nutrient losses of a severely eroded clayey Plinthudult in southeastern China

机译:植被恢复对严重侵蚀的黏土Plinthudult水土流失和养分流失的影响

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The clayey Ultisols in low hilly area in southeastern China were called for agricultural reclamation to meet the increasing food demand. However, little attention was given to soil erosion during land use planning due to lack of information on the amount of soil erosion and how to restore the severely eroded bare soils. The objectives were to estimate the long-term influences of reforestation on soil and water erosion and nutrient losses on a severely eroded bare land derived from Quaternary red clay. The results indicated that reforestation using integrative measures decreased surface runoff and soil erosion on the severely eroded land. On the severely eroded bare land. annual runoff varied from 303 to 1056 mm and annual total soil loss from 53 to 256 tons ha(-1). After reforestation, soil erosion dramatically reduced to 2-43 tons ha(-1) year(-1) from 1988 to 1990 and became negligible since then. The high level of soil erosion was attributed to high rainfall erosivity, readily transportable particles due to the presence of pseudo sand on the bared soil surface formed in the dry season and due to clay dispersion occurring in the long rainy season, and the gully landform. Depositional soil loss accounted for the high proportion of soil loss, while enrichment ratios (ER) of soil nutrients in the suspensional sediment were greater than 1. The results suggest that soil erosion has to be taken into account when planning to convert the clayey soils in the low hilly area for agricultural use, and integrative treasures to reforest are key to prevent soil erosion on the severely eroded bared land
机译:中国东南部低丘地区的黏土Ultisols被要求进行农垦,以满足不断增长的粮食需求。但是,由于缺乏有关土壤侵蚀量以及如何修复严重侵蚀的裸露土壤的信息,在土地使用规划期间很少关注土壤侵蚀。目的是评估在第四纪红粘土衍生的严重侵蚀的裸地上,重新造林对水土流失和养分流失的长期影响。结果表明,采用综合措施进行的造林减少了严重侵蚀土地上的地表径流和土壤侵蚀。在严重侵蚀的光秃秃的土地上。年径流量从303到1056 mm不等,年土壤总损失从53到256吨ha(-1)。植树造林后,从1988年到1990年,土壤侵蚀急剧减少到2-43吨ha(-1)year(-1),从那时起就可以忽略不计了。高水平的土壤侵蚀归因于高降雨侵蚀力,由于在干旱季节形成的裸露土壤表面上存在假砂,在漫长的雨季出现了粘土分散以及沟壑地貌而易于运输的颗粒。沉积物的土壤流失占土壤流失的比例很高,而悬浮沉积物中土壤养分的富集比(ER)大于1。结果表明,在计划中转换黏性土壤时必须考虑土壤侵蚀。低丘陵地区的农业用地以及综合造林的宝藏是防止严重侵蚀的裸露土地上水土流失的关键

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