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溯源侵蚀的英文

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"溯源侵蚀"怎么读用"溯源侵蚀"造句

英文翻译手机手机版

  • head erosion
  • headerosion
  • headward erosion
  • headward-migrating erosion
  • headwater erosion

例句与用法

  • So , river capture can be taken as the time and space scale of geomorphologic evolution in quaternary in csmasr it can represent the process of river head wards erosion , expand of lincheng period denudation surface and the broken of yangping period denudation surface
    认为河流袭夺是判断地貌演进,即临城期(第四纪)溯源侵蚀与仰平期剥夷面解体破碎的时空标尺,并据此探讨了临城期河流溯源侵蚀的时空格局。
  • This kind of instability bulk movement is induced by wave cyclic loading , as a result the slope of bottom bed decrease , water depth increase , and instability bulk movement has the character of subregion , regularity and head erosion , thus it will influence evolvement of region of interest landform , and change flow field and bottom stratum condition continually , so will lead to dynamic influence on structure foundation soil
    这种不稳定块体运动由波浪循环荷载诱发,其结果使底床整体坡度减缓,水深加大,而且不稳定的块体运动具有小区域、多发性和溯源侵蚀的特点,将继续影响着海域以后的水深地形的发展演化,并不断改变着该区的流场与底床地层条件,对构筑物地基土的稳定性产生着动态的影响。
  • There are four characteristics of the evolution of tidal creek as follows : ( 1 ) in the initial stages , tidal creek develops by continuous eroding trace to the source and depriving of the top of other tidal creeks . ( 2 ) the transverse moving of tidal creek occur mostly in the lower part , the middle part and the outlet take second place , and the upper part is more stability . ( 3 ) the different level branches of tidal creek transform into each other in the whole evolution course
    潮沟的演变具有以下特点: ( 1 )潮沟在形成初期,不断进行溯源侵蚀和袭夺以扩大集水面积而发展壮大, ( 2 )潮沟的侧向移动主要发生在潮沟的下段,中段和口门次之,上段最为稳定( 3 )不同级别的支潮沟之间处在不断地相互转化过程之中。
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