自然科学版
陕西师范大学学报(自然科学版)
水土资源高效利用专题
室内模拟降雨情形下黄土坡面沉降程度的试验研究
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权鑫1,史红伟1,3,蔡强国2,和继军1*,郑明国2,孙莉英2,方海燕2
(1 首都师范大学 城市环境过程和数字模拟国家重点试验室培育基地,北京资源环境与GIS重点试验室,北京 100048; 2 中国科学院 地理科学与资源研究所,中国科学院大学 资源与环境学院,北京 100101;3 水利部建设管理与质量安全中心,水利工程管理处,北京 100038)
和继军,男,教授,博士,主要从事土壤侵蚀、水土保持及区域水文学等方面研究工作。Email:hejiun_200018@163.com
摘要:
针对降雨过程中如果土体发生沉降将会严重影响三维激光扫描仪的土壤侵蚀监测精度,从而影响试验结果的问题,采用室内人工模拟降雨试验,在试验土体内插入细钢钎,通过对降雨前后钢钎出露于坡面的高度数据进行统计分析,来判断试验过程中是否发生了土体沉降。试验土壤为分别取自安塞和绥德的黄绵土,试验土层厚度30 cm,试验条件包括2种雨强、2个坡长和5个坡度等处理。结果表明:大部分试验条件下两个取样点的黄土降雨前后钢钎出露于坡面的长度无显著性差异(P<0.05),没有充分证据表明降雨前后坡面土体发生了沉降,由坡面沉降引起的测量精度可以忽略。因此,在本试验研究中可以使用三维激光扫描技术对坡面侵蚀沉积进行监测,并可为类似室内土壤侵蚀试验研究提供借鉴。
关键词:
人工模拟降雨;土体沉降;统计检验;三维激光扫描;黄土坡面
收稿日期:
2020-11-30
中图分类号:
S157.1
文献标识码:
A
文章编号:
16724291(2021)02009809
基金项目:
国家自然科学基金(41771314,41401302)
Doi:
Experimental study on the settlement of loess slope under indoor simulated rainfall
QUAN Xin1,SHI Hongwei1,3,CAI Qiangguo2,HE Jijun1*,ZHENG Mingguo2,SUN Liying2,FANG Haiyan2
(1 State Key Laboratory of Urban Environmental Processes and Numerical Simulation,Capital Normal University Resources Environment and GIS Key Lab of Beijing,Beijing 100048,China;2 Institute of Geographical Sciences and Natural Resources Research,Chinese Academy of Sciences,College of Resources and Environment,University Chinese Academy of Sciences,Beijing 100101,China;3 Ministry of Water Resources Construction Management and Quality and Safety Center, Water Conservancy Engineering Management Department,Beijing 100038,China)
Abstract:
With the development of science and the progress of monitoring technology, many studies have applied 3D laser scanning technology to study soil erosion, it can quantitatively monitor soil erosion deposition. However, if the soil settlement occurs in the process of rainfall, it will seriously affect the monitoring accuracy of the 3D laser scanner, thus affecting the experimental results. Aiming at this problem, this study adopts the indoor artificial simulated rainfall test, inserts the fine steel chisel into the test soil body, through carrying on the statistical analysis to the height data of steel chisel exposed to the slope surface before and after the rainfall, to determine whether the soil settlement occurred in the test process. The test soil was loess taken from Ansai county and Suide county respectively. The thickness of the test soil was 30 cm. The test conditions included 2 kinds of rain intensity, 2 slope lengths and 5 slope gradients. The results show that there is no significant difference in the length of the steel chisel exposed to the slope surface before and after rainfall in most of the test conditions (P
KeyWords:
artificial simulated rainfall;soil settlement;statistical test;3D laser scanning;loess slope