首页|降雨入渗-地表径流下延安卸荷黄土边坡侵蚀演化特征

降雨入渗-地表径流下延安卸荷黄土边坡侵蚀演化特征

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明确卸荷黄土边坡降雨侵蚀规律对地质灾害防治和流域生态治理具有重要意义.以延安卸荷黄土边坡降雨侵蚀灾害为研究背景,利用自行开发的降雨入渗-地表径流黄土边坡试验平台,研究降雨强度、降雨历时对卸荷黄土边坡入渗量、径流量、土壤流失量以及坡体含水率的影响,揭示降雨作用下卸荷黄土边坡侵蚀演化规律.研究结果表明:1)降雨初期坡面雨水以入渗为主,入渗量约为地表径流量的2~8倍;随着降雨历时增加,地表径流量呈增加趋势,雨水入渗量呈减少趋势;短历时强降雨条件下地表径流量小于入渗量,而持续强降雨条件下地表径流量大于入渗量.2)坡面侵蚀产沙量与降雨强度呈正相关关系,持续强降雨条件下的土壤流失量约为短历时强降雨的10.81倍.3)地表土体含水率随降雨次数增加呈现快速增长到缓慢增长再到平稳状态的发展过程,随降雨强度降低呈减小趋势;相同雨强下,持续强降雨下的地表土体含水率较短历时强降雨增长了9.62%;坡面中、底部浅层土体含水率增长速率高于坡面顶部.4)持续强降雨下边坡侵蚀灾变演化过程为雨水入渗→浅表层土体增湿→坡面密集溅蚀坑→地表径流→浅、细、短的侵蚀沟槽→深、宽、长的侵蚀沟槽→坡体浅层滑塌,坡面侵蚀破坏范围表现为由坡脚向坡顶逐渐后退.
Characteristics of erosion evolution of unloaded loess slope in Yan'an under rainfall infiltration and surface runoff
It is of great significance to determine the regularity of rainfall erosion of unloading loess slope for geological disaster prevention and watershed ecological management.Taking the rainfall erosion disaster of the unloaded loess slope in Yan'an as the background,the effects of rainfall intensity and rainfall duration on the infiltration,runoff,soil loss and moisture content of loess slope were studied by using the self-developed rainfall infiltration and surface runoff test platform,and the erosion evolution law of loess slope under the action of rainfall was revealed.The results showed that:1)In the early stage of rainfall,the slope rainwater was mainly infiltration,and the infiltration amount was about 2~8 times of the surface runoff.With the increase of rainfall duration,the surface runoff showed an increasing trend and the rainwater infiltration showed a decreasing trend.The surface runoff was less than the infiltration under the condition of short duration heavy rainfall,while the condition of sustained heavy rainfall was the opposite.2)The erosion mud yield of slope surface was positively correlated with the rainfall intensity,and the soil loss quantity under the condition of continuous strong rainfall was about 10.81 times that of short duration heavy rainfall.3)The development process of moisture content of slope surface soil suc-cessively transformed from rapid growth,slow growth and then to steady state with rain fall frequency,and it was decreased with the decrease of rainfall intensity.Under the same rainfall intensity,the soil moisture content under continuous heavy rainfall increased by 9.62%compared with short duration heavy rainfall.The soil moisture content in the middle bottom of slope increased faster than that at the top of slope.4)The evolutionary process of slope ero-sion catastrophe under continuous heavy rainfall was rainwater infiltration,shallow surface soil wetting,intensive splash pits on the slope surface,surface runoff,shallow,thin and short erosion trench deep,wide and long erosion trench and shallow landslides,and the erosion damage range of slope surface was manifested as the gradual retreat from the slope foot to the top.

unloaded loess sloperainfall infiltrationsurface runoffmodel testerosion evolution

邱明明、杨玉欣、王磊、孙杰龙、杨红霞、赵海峰

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延安大学 建筑工程学院,陕西 延安 716000

卸荷黄土边坡 降雨入渗 地表径流 模型试验 侵蚀演化

陕西省教育厅服务地方专项延安市科技计划延安大学科研项目延安大学科研项目国家级大学生创新创业训练计划

21JC0352022SLSFGG-0042021ZCQ011YDY2020-36202210719004

2024

延安大学学报(自然科学版)
延安大学

延安大学学报(自然科学版)

影响因子:0.238
ISSN:1004-602X
年,卷(期):2024.43(1)
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