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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Soil erosion characteristics of ditch banks during reclamation of a saline/sodic soil in a coastal region of China: Field investigation and rainfall simulation
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Soil erosion characteristics of ditch banks during reclamation of a saline/sodic soil in a coastal region of China: Field investigation and rainfall simulation

机译:中国沿海地区盐碱水复垦过程中沟岸的土壤侵蚀特征:田间调查与降雨模拟

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摘要

Understanding soil erosion processes is essential for assessing the extent and causes of soil erosion and for planning soil conservation including those on the banks of excavated ditches. Based on a field investigation and laboratory rainfall simulation experiments, the soil erosion characteristics of a saline/sodic soil undergoing reclamation that was exposed on irrigation/drainage ditch banks in a coastal region of China were investigated. Preliminary analyses of the data indicated that the soil erosion was more severe from the ditch banks in the coastal region than from those in other areas of China. The annual erosion loss from ditch banks in the most recently reclaimed farmland (2007) was 140 kg/m(2), but the erosion modulus decreased significantly (p < 0.05) with increasing reclamation time. Increasing rainfall intensity and/or slope gradient increased runoff and sediment yield rates. However, there was a critical slope gradient of about 25 degrees, above which no further increases occurred. As rainfall intensity and/or slope gradient increased, the overland flow velocity and the Froude number (Fr) increased notably. The Reynolds number (Re) increased with increasing rainfall intensity, but decreased and was more affected by increases in slope gradient. Positive parabolic relationships were found between sediment yield rates and Re. The resistance to flow decreased with increasing rainfall intensity and slope gradient Negative correlations were found between the sediment yield rate and the resistance force (f and n). Covering the soil surface greatly decreased runoff and soil erosion by increasing the surface roughness and decreasing the runoff velocity. Compared with covers of stones or netting, and with no cover, the slope runoff coefficient and sediment yield rate of soil under straw mulch were the lowest with values of 0.043 and 0.14 kg/m2 min, respectively. Therefore, using straw mulch would be a way to control erosion until salt-tolerant plants colonized and protected the ditches
机译:了解土壤侵蚀过程对于评估土壤侵蚀的程度和原因以及规划土壤保护(包括在开挖沟渠岸边的土壤保护)至关重要。基于野外调查和实验室降雨模拟实验,研究了在中国沿海地区灌溉/排水沟岸暴露的复垦盐碱土壤的土壤侵蚀特征。对数据的初步分析表明,沿海沟渠的土壤侵蚀比中国其他地区的严重。最近开垦的农田中,沟渠的年侵蚀损失为140 kg / m(2),但随着开垦时间的增加,侵蚀模数显着降低(p <0.05)。降雨强度和/或坡度的增加会增加径流和沉积物的产率。但是,存在大约25度的临界坡度,在该坡度以上没有进一步的增加。随着降雨强度和/或坡度的增加,陆上流速和弗洛德数(Fr)显着增加。雷诺数(Re)随着降雨强度的增加而增加,但下降,并且受坡度梯度的增加的影响更大。沉积物产率与Re之间存在正抛物线关系。流动阻力随着降雨强度和坡度梯度的增加而减小。在沉积物产水率与阻力(f和n)之间存在负相关关系。通过增加表面粗糙度和降低径流速度,覆盖土壤表面大大减少了径流和土壤侵蚀。与不覆盖的石头或网罩相比,秸秆覆盖下的坡面径流系数和沉积物产率最低,分别为0.043和0.14 kg / m2 min。因此,使用秸秆覆盖是控制侵蚀的一种方法,直到耐盐植物定居并保护了沟渠。

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