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作 者:张婉璐 袁再健 李定强 郑明国 廖义善 蔡强国[3,4] 黄炎和 蔡崇法[6] 牛德奎[7] 王治国[8] ZHANG Wanlu;YUAN Zaijian;LI Dingqiang;ZHENG Mingguo;LIAO Yishan;CAI Qiangguo;HUANG Yanhe;CAI Chongfa;NIU Dekui;WANG Zhiguo(Guangdong Engineering Research Center for Non-point Source Pollution Control, Guangdong Key Laboratory of Integrated Agro-environmental Pollution Control and Management, National-Regional Joint Engineering Research Center for Soil Pollution Control and Remediation in South China, Institute of Eco-environmental and Soil Science, Guangdong Academy of Sciences, 510650, Guangzhou, China;International Institute of Soil and Water Conservation, 514000, Meizhou, Guangdong,China;Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, 100101, Beijing, China;College of Resource and Environment, University of Chinese Academy of Sciences, 100049, Beijing, China;Fujian Agriculture and Forestry University, 350002, Fuzhou, China;Research Center of Water and Soil Conservation, Huazhong Agricultural University, 30070, Wuhan, China;College of Forestry, Jiangxi Agricultural University, 330045, Nanchang, China;China Renewable Energy Engineering Institute, 100120, Beijing, China)
机构地区:[1]广东省科学院生态环境与土壤研究所华南土壤污染控制与修复国家地方联合工程研究中心广东省农业环境综合治理重点实验室广东省面源污染防治工程技术研究中心,广州510650 [2]梅州市国际水土保持研究院,广东梅州514000 [3]中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室,北京100101 [4]中国科学院大学资源环境学院,北京100049 [5]福建农林大学,福州350002 [6]华中农业大学水土保持研究中心,武汉430070 [7]江西农业大学林学院,南昌330045 [8]水利部水利水电规划设计总院,北京100120
出 处:《中国水土保持科学》2020年第5期136-143,共8页Science of Soil and Water Conservation
基 金:国家重点研发计划课题“生态防护型水土流失治理技术集成与示范”(2017YFC0505404);广东省省级科技计划项目“南岭森林生态系统野外科学观测研究站”(2018B030324001);广东省重点领域研发计划“练江水体综合治理与生态修复关键技术集成及示范”(2019B110205003);广东省科学院专项资金项目(2019GDASYL-0502004)。
摘 要:崩岗是我国南方丘陵区特殊的地质灾害类型,是坡面土体在多种外营力作用下,沿沟壁处不断崩坍破坏,最终形成巨大创口的侵蚀地貌现象。崩岗侵蚀通常伴随着大量的水土流失,对生态环境造成严重威胁。目前,国家对南方崩岗侵蚀治理工作日益重视,崩岗已从小众的地貌学词汇逐渐趋向大众化;且随着水土保持领域国际交流合作日益加强,关于崩岗的研究成果已逐渐引起国际关注。首先对崩岗的概念及其涵义进行介绍分析,进而探讨了崩岗的英文译法。为了更好地体现崩岗独特的文化特色与内涵,崩岗这一具有中国特色的侵蚀地貌,采用译音Benggang的方法,有助于深化国内外学者对我国崩岗侵蚀独特性的认识,进一步推进我国水土保持研究的国际化进程。[Background]Benggang is a typical geo-hazard in the tropical and subtropical areas of South China with the greatest scale of water and soil erosion and serious ecological damage.It is an erosional geomorphology that the soil in the red soil hilly of south China collapses continuously along the gully wall,under the action of hydraulic and gravity,and finally forms a huge wound.With the urgent attention of the country to the management of Benggang erosion in South China,this niche geomorphology vocabulary now gradually tends popular.In addition,with the exchange and cooperation of soil and water erosion globally,the research achievement for Benggang has attracted international attention.[Methods]In this paper,the concept and connotation of Benggang were discussed,based on the comprehensive summary of the development,morphology and destination of Benggang.On the other hand,the English translation for Benggang was analyzed by comparing the domestic and international erosional landforms,and by discussing the present translations for Benggang.[Results]1)Benggang is usually developed in tropical and subtropical granite areas with 20-50 m weathering crust,and exists in a small amount in glutenite,argillaceous shale,phyllite and other rock areas.There are about 239,100 Benggangs in China and the average annual sediment yield by Benggang erosion is about 67,239,000 t in recent decades.2)A Benggang system can be divided into five parts:upper catchment area,collapsing wall,colluvial deposit,scour channel,and alluvial fan.Typical Benggang landforms are characterized by arc-shaped,linear-shaped,ladle-shaped,composite-shaped,and claw-shaped.3)According to the development conditions,mechanism,and region of Benggang,it is different from the erosion landforms in foreign countries.Therefore,there is no appropriate native English word that can be used as the translation of Benggang.In addition,Benggang is also significantly different from the soil erosion landforms in China,such as landslide and debris flow,which are dominated by gr
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