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全风化花岗岩管沟回填土坡面侵蚀影响因素及交互作用
引用本文:张凯,孔志岗,李燕清,周剑,贾福聚,张垚.全风化花岗岩管沟回填土坡面侵蚀影响因素及交互作用[J].水土保持学报,2023,37(1):52-58.
作者姓名:张凯  孔志岗  李燕清  周剑  贾福聚  张垚
作者单位:1. 昆明理工大学国土资源工程学院, 昆明 650093;2. 昆明理工大学自然资源部高原山地地质灾害预报预警与生态保护修复重点实验室, 昆明 650093;3. 云南省交通运输厅, 云南省交通安全统筹中心, 昆明 650031;4. 北京工业大学城市建设学部, 北京 100124;5. 中国有色金属工业昆明勘察设计研究院有限公司, 昆明 650093
基金项目:国家管网集团西南管道有限责任公司科技开发项目(2018016);云南省重点研发计划项目(202203AC100003)
摘    要:为了查明全风化花岗岩地区输油气管道作业边坡坡面水土流失问题,通过野外典型边坡边界条件测量、坡面侵蚀特征冲沟沟深、冲沟截面积数据采集、岩土体取样测试,并结合室内模型降雨试验等方法。结果表明:降雨、坡长、坡度、汇水面积、岩土体特性5种因素均影响全风化花岗岩管沟回填土坡面侵蚀。产沙率和产流率随着降雨强度的增大而增大。坡长、坡度、汇水面积与冲沟沟深和冲沟截面积呈正相关关系,且随着坡长、坡度、汇水面积的增大,冲沟沟深和冲沟截面积也在增大。通过取样测试发现,原状土与回填土的颗粒组成相对含量具有较大差异,初始回填土粒度级配为良好土。降雨冲刷初期回填土坡面径流主要携带粉粒和黏粒。5年回填土相对于原状土,孔隙率增加到原来的1.13倍,土体渗透系数增大1个数量级,饱和状态下黏聚力降低为原状土的67.6%,内摩擦角降低为原状土的87.5%。通过查明全风化花岗岩管沟回填土坡面侵蚀影响因素及其作用,为后续的边坡治理提供依据。

关 键 词:管沟回填土  边界条件  岩土体特性  坡面侵蚀  交互作用
收稿时间:2022/6/19 0:00:00

Influence Factors and Interaction of Slope Erosion of Completely Weathered Granite Pipe Trench Backfill
ZHANG Kai,KONG Zhigang,LI Yanqing,ZHOU Jian,JIA Fuju,ZHANG Yao.Influence Factors and Interaction of Slope Erosion of Completely Weathered Granite Pipe Trench Backfill[J].Journal of Soil and Water Conservation,2023,37(1):52-58.
Authors:ZHANG Kai  KONG Zhigang  LI Yanqing  ZHOU Jian  JIA Fuju  ZHANG Yao
Institution:1. Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093;2. MNR Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, Kunming University of Science and Technology, Kunming 650093;3. Yunnan Provincial Traffic Safety Coordination Center, Department of Transport of Yunnan Province, Kunming 650031;4. Faculty of Urban Construction, Beijing University of Technology, Beijing 100124;5. Kunming Survey, Design and Research Institute of China Nonferrous Metals Industry Co., LTD., Kunming 650093
Abstract:In order to find out the problem of soil and water loss on the slope side of oil and gas pipeline operation in fully weathered granite area, this paper adopted the methods of measuring the boundary conditions of typical slopes in the field, collecting the data of gully depth and gully sectional area of slope erosion characteristics, sampling and testing rock and soil mass, and the indoor model rainfall test. The results showed that rainfall, slope length, slope, catchment area and geotechnical characteristics all affected the slope erosion of backfill soil in fully weathered granite pipe trench. Sediment yield and flow yield increased with the increase of rainfall intensity. The slope length, slope and catchment area were positively correlated with gully depth and gully cross-sectional area, and the gully depth and gully cross-sectional area increased with the increase of slope length, slope and catchment area. Through sampling, it was found that the relative content of particle composition of undisturbed soil was different from that of backfill soil, and the particle size distribution of the initial backfill soil was good. At the initial stage of rainfall scouring, the runoff of backfill slope mainly carried away silt and clay particles. Compared with the original soil, the porosity of the backfill soil in five years increased to 1.13 times, the soil permeability coefficient increased by one order of magnitude, and the cohesion in saturated state and internal friction angle decreased to 67.6% and 87.5% of that of the original soil, respectively. By finding out the influencing factors and their effects on slope erosion of backfill soil in fully weathered granite pipe trench, it could provide a basis for the subsequent slope treatment.
Keywords:pipe trench backfill soil  boundary conditions  geotechnical characteristics  slope erosion  interaction
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