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作 者:丰佳 潘明九 顾晨临 余智芳 赵满 赵晓红 李健 FENG Jia;PAN Mingjiu;GU Chenlin;YU Zhifang;ZHAO Man;ZHAO Xiaohong;LI Jian(State Grid Zhejiang Electric Power Corporation,Hangzhou 310007,Zhejiang,China;Economic and Technical Research Institute of State Grid Zhejiang Electric Power Corporation,Hangzhou 310020,Zhejiang,China;HydroChina Huadong Engineering Corporation Limited,Hangzhou 311122,Zhejiang,China;State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau,Institute of Soil and Water Conservation,Northwest A&F University,Yangling 712100,Shaanxi,China)
机构地区:[1]国网浙江省电力有限公司,浙江杭州310007 [2]国网浙江省电力有限公司经济技术研究院,浙江杭州310020 [3]中国电建集团华东勘测设计研究院有限公司,浙江杭州311122 [4]西北农林科技大学水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100
出 处:《水利水电技术(中英文)》2021年第S02期496-502,共7页Water Resources and Hydropower Engineering
基 金:国家电网公司总部科技项目“山丘区架空输电线路工程水土保持设计施工关键技术研究”(8100-202019156A-0-0-00)
摘 要:为明确红壤山地丘陵区输电线路工程水土流失特征,以雅中~江西±800 kV特高压工程为研究对象,通过实地调查,对不同土地利用塔基部位侵蚀沟断面形态进行了研究。结果表明:(1)裸地、稀疏灌木地侵蚀沟沟深在0.05~0.25 m范围内的累积频率分别为82.76%、92.86%;横断面积在0.0025~0.01 m^(2)内的占比分别为37.9%和42.9%。(2)裸地侵蚀沟的平均长度和深度较草地、稀疏灌木地高出68.8%、30.9%和59.8%、18.8%;平均横断面积和体积从大到小依次为裸地>稀疏灌木地>草地;裸地、稀疏灌木地侵蚀沟断面特征表现为“窄且深”,而草地表现为“宽且浅”。(3)土地利用为裸地、稀疏灌木地的塔基部位侵蚀沟体积可通过宽深比进行估算。本研究可为该区同类项目水土流失量估算以及水土流失治理提供一定的理论依据。In order to clarify the soil and water erosion characteristics of the transmission line project in the red soil hilly area,the Ya zhong~Jiang xi±800 kV UHV project was taken as the research object,and the cross-sectional morphology characteristics of the erosion grooves of the tower foundations of different land use were studied through field investigations.The results shows that:(1)The cumulative frequency of erosion of bare land and sparse shrubland within the range of 0.05~0.25m is 82.76%and 92.86%,respectively;the proportion of cross-sectional area within 0.0025~0.01 m^(2)is 37.9%and 42.9%,respectively.(2)The average length and depth of the bare slope erosion ditch is 68.8%,30.9%,59.8%,18.8%higher than that of grassland and sparse shrubland;the average cross-sectional area and volume from large to small are bare land>sparse shrubland>grassland.;the cross-section characteristics of the erosion gullies on bare land and sparse shrubland are"narrow and deep",while grassland is"wide and shallow".(3)The volume of the erosion ditch at the base of the tower where the land is used as bare land and sparse shrubland can be estimated by the ratio of width to depth of the erosion ditch.This study can provide a certain theoretical basis for the estimation of soil erosion amount and soil erosion control of similar projects in this area.
分 类 号:S157.1[农业科学—土壤学] TM75[农业科学—农业基础科学]
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