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踩踏干扰对生物结皮土壤渗透性的影响 被引量:19

Effect of trampling disturbance on soil infiltration of biological soil crusts
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摘要 采用人工模拟降雨试验,研究了踩踏干扰对生物结皮土壤渗透性的影响.结果表明:踩踏干扰显著增加了土壤表面粗糙度,增加幅度与干扰强度有关,50%干扰度下表面粗糙度指数较不干扰增加91%.踩踏干扰延长了坡面产流时间,20%~50%干扰度范围内,随着干扰强度的增加,初始产流时间呈线性增加趋势,50%干扰度的初始产流时间较不干扰增加了169.7%.踩踏干扰增加了土壤渗透性,降低径流系数.50%干扰度的土壤累积入渗量较不干扰增加12.6%;去除生物结皮,土壤渗透性降低,累积入渗量较不干扰降低30.2%.50%以下的干扰度未显著增加土壤侵蚀模数.去除生物结皮,土壤侵蚀模数较不干扰增加10倍.生物结皮破碎度低于50%的干扰在不明显增加土壤流失量的前提下,可增加降水入渗,减小径流风险,改善土壤水分状况. The effect of trampling disturbance on soil infiltration of biological soil crusts was investigated by using simulated rainfall. The results showed that the trampling disturbance significantly increased soil surface roughness. The increasing extent depended on the disturbance intensity. Soil surface roughness values at 50% disturbance increased by 91% compared with the undisturbed treatment. The runoff was delayed by trampling disturbance. A linear increase in the time of runoff yield was observed along with the increasing disturbance intensity within 20%-50%. The time of runoff yield at 50% disturbance increased by 169. 7% compared with the undisturbed treatment.Trampling disturbance increased soil infiltration and consequently decreased the runoff coefficient.The cumulative infiltration amount at 50% disturbance increased by 12.6% compared with the undisturbed treatment. Soil infiltration significant decreased when biocrusts were removed. The cumulative infiltration of the treatment of biocrusts removal decreased by 30.2% compared with the undisturbed treatment. Trampling disturbance did not significantly increase the soil loss when the disturbance intensity was lower than 50%,while the biocrusts removal resulted in 10 times higher in soil erosion modulus. The trampling disturbance of lower than 50% on biocrusts might improve soil infiltration and reduce the risk of runoff,thus might improve the soil moisture without obviously increasing the soil loss.
作者 石亚芳 赵允格 李晨辉 王闪闪 杨巧云 谢申琦 SHI Ya-fang ZHAO Yun-ge LI Chen-hui WANG Shan-shan YANG Qiao-yun XIE Shen-qi(College of Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resource, Yangling 712100, Shaanxi, China).)
出处 《应用生态学报》 CAS CSCD 北大核心 2017年第10期3227-3234,共8页 Chinese Journal of Applied Ecology
基金 国家自然科学基金项目(41571268 41271298)资助~~
关键词 退耕地 生物结皮 入渗 表面粗糙度 径流 revegetated grassland biological soil crust infiltration surface roughness runoff
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