1) ephemeral gully erosion
浅沟侵蚀
1.
Seasonal discrepancy of ephemeral gully erosion in Northeast China with black soils;
典型黑土区小流域浅沟侵蚀季节差异分析
2.
The correlation between catchment topography and ephemeral gully erosion in northeastern China with black soils was discussed.
浅沟侵蚀是坡耕地上重要的产沙方式之一,地形是控制其发生及发展的关键因素。
3.
A field survey in the spring 2005 in the two small watersheds was conducted to investigate ephemeral gully erosion in freeze-thawing period in this area.
浅沟侵蚀是东北漫岗黑土区农耕地上常见的水蚀类型,往往对坡耕地造成严重的破坏。
2) intercolparis erosion
沟间侵蚀
1.
In order to made a study of law of development of side slope gully erosion of highway spoil ground,upgrowth characteristic and law of development of gully erosion and realation between intercolparis erosion and gully erosion had been studied in the spoil ground of constructing Hurongxi expressway of Hubei province.
为探讨公路弃土场边坡沟蚀发生发展规律,以湖北沪蓉西高速公路(宜长段)为例,从弃土场沟蚀发育特征、发生发展规律和与沟间侵蚀的关系3方面对弃土场沟蚀规律进行探讨。
3) erosion gully
侵蚀沟
1.
Administing soil erosion and improving ecology environment are the main measures to solve farmer agriculture and countryside problem at mountainous area and make some good tries and studies,and accumutate some experience for administing erosion gully.
13×104hm2,大型侵蚀沟就有6 300余条、沟壑密度达0。
4) erosion ditch
侵蚀沟
1.
Brief discussion on the formation reason and prevention measure of erosion ditch in plain area;
平原区侵蚀沟的成因及防治措施初探
2.
The causes of forming erosion ditch and main harm to the economic and social development are analyzed in this paper,and the ways and measures of comprehensive prevention and treatment for erosion ditch are put forword in construction projects.
分析了侵蚀沟对经济社会发展的主要危害和形成原因,针对侵蚀沟防治工程建设中存在的主要问题,提出了侵蚀沟综合防治的途径与对策。
6) rill erosion
细沟侵蚀
1.
Simulation study on the dynamic rill erosion processes: model validation with laboratory experiments;
细沟侵蚀动态过程模拟室内试验和模型验证研究
2.
Simulation study on dynamic rill erosion processes: mathematical models and FEM formulation;
细沟侵蚀动态过程模拟数学模型和有限元计算方法
3.
Study on spatial and temporal characters of rill erosion on slope;
坡面细沟侵蚀产沙时空分布规律试验研究
补充资料：侵蚀沟
侵蚀沟
为线形伸展的槽形凹地。是暂时性流水形成的侵蚀地貌，主要发育在半干旱气候带的松散沉积层上，在植被稀疏的缓坡地区，侵蚀沟可以发展得很快，使地形遭受强烈的分割，蚕食耕地，破坏道路，造成大量的水土流失。
侵蚀沟的形成与发展可分为以下几个阶段，细沟阶段；水流在斜坡上由片流逐渐汇集成细小的股流，在地表形成大致平行的细沟（宽0.5米，深0.1～0.4米，长数米）。由细沟进一步下切加深形成了切沟；切沟已有了明显的沟缘，沟口形成小陡坎，宽和深可达1～2米。切沟再进一步下蚀，形成了冲沟；冲沟的沟头有了明显的陡坎，沟边经常发生崩塌、滑坡、使沟槽不断加宽，冲沟深约几米至几十米，长约几百米，冲沟在我国的黄土高原特别发育。冲沟进一步发展，沟坡由崩塌逐渐变得平缓，沟底填充碎屑物，形成宽而浅的干谷称为拗谷。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条