沟蚀

gōu shí
  • Gully erosion;liner erosion
沟蚀沟蚀
沟蚀[gōu shí]
  1. GPS和GIS进行短期沟蚀研究初探&以东北漫川漫岗黑土区为例

    Preliminary Research on Short-term Channel Erosion Using GPS and GIS

  2. 利用高精度GPS动态监测沟蚀发育过程

    Application of High-Precision GPS to Dynamic Monitoring Gully Erosion Processes

  3. GPS技术正在成为一种快速高效研究沟蚀发生演变的手段。

    GPS-survey technology is becoming an effective tool for determining topographic-related parameters .

  4. 然而,目前国内沟蚀的研究主要集中于黄土高原地区和东北黑土区,而且主要是在较小的空间尺度内,采用实地调查或GPS测量等方法研究沟蚀的发生演变规律。

    However , the recent studies on soil erosion are mainly concerned on the gullies in the Loess Plateau and Black soil area in Northeast China in the small scale , there is a lack of study on gully erosion in the Upper Yangtze River Basin .

  5. 中国水土流失地区土壤沟蚀的研究进展

    Research progresses in gully erosion of water and soil erosion region in China

  6. 南部沟蚀、滑坡严重;

    The South has gully erosion and serious slip .

  7. 作为面蚀向沟蚀转化的特殊阶段,细沟侵蚀在坡面侵蚀机理的研究中有着重要的意义。

    Rill erosion plays a very important role in the study of slope erosion .

  8. 集中股流造成坡面强烈冲刷,引发沟蚀。

    Gathered stream flow can washed out sloping farmland and cause gully erosion . 6 .

  9. 青海省黄土丘陵沟壑区沟蚀影响因子的贡献率

    Contributing ratio of impact factor on gully erosion in Loess hilly and gully area of Qinghai province

  10. 东北黑土区沟蚀机理及防治模式的研究

    Study on Dynamics of Gully Erosion and Its Controlling in the Black Soil Region , Northeast China

  11. 黄土高原的土壤侵蚀情况比较复杂,以各种类型的沟蚀为主,并具有垂直分带性。

    Soil erosion on the loess plateau is very complicated with various types of gully erosion in the main characterized with vertical belt erosion .

  12. 含有介壳的凝缩段、下超面及沟蚀面是划分玛托组体系域的关键界面。

    It is condensed section with shells , downlap surface and ravinement surface that constitute the critical boundaries in dividing the system tracts of Matuo Formation .

  13. 桦树沟蚀变岩型铜矿床属一种破碎带蚀变岩型铜矿床,区域上具有明显的层控性,但在矿田和矿区范围,矿体明显受构造破碎蚀变带控制。

    Huashugou copper deposits belong to a kind of altered rock-type copper deposit with the regional stratabound property , ore body is controlled by the fracture zone within mine district .

  14. 这些方法虽能描述小流域沟蚀现状,但不能为沟壑治理的工程设计提供前期资料。

    Although these methods mentioned above can describe the existing condition of the gully erosion in a small watershed , it can not provide the antecedent information for the design of gully harnessing engineering .

  15. 裸露的路堤边坡水力侵蚀发生发展规律一般为:沟蚀→边坡滑坍;

    The development regularities of water erosion on bare road embankment slope and bare cutting slope are gully erosion → shallow slip of slope and splash erosion → surface erosion → gully erosion → collapse respectively .

  16. 在以沟壑密度作为主要评价因子的沟蚀研究中,航片判读方法较其它两种方法更适合本区域内的沟蚀研究。

    Comparing three above methods , the method for deriving gully system parameters using aerial photo interpretation is the optimal method to assess gully erosion , as the gully density were taken as the key assessment factor .

  17. 结果表明,研究区内面蚀侵蚀量最大,沟蚀次之,重力侵蚀最小,分别占总量的46.8%,35.1%和18.1%。

    Using the model conclusion might be gotten in the studied watershed , that is , erosion amount by surface erosion is the greatest ( 46.8 % ), gully erosion the greater ( 35.1 % ) and gravity erosion Lhe least ( 18.1 % ) .

  18. 计算结果表明,流域内坡面侵蚀只占流域侵蚀模数的7.1%~11.7%,流域侵蚀物质主要来源于沟蚀、部分重力侵蚀。

    The calculative products of the models manifest that slope erosion is small and equated to 7.1 % ~ 11.7 % of watershed erosion . It suggests that the erosion matter of the small watershed mainly comes from channel erosion and gravitation erosion , instead of slope erosion .

  19. 论林木的固沟减蚀作用

    The Effects of Forest in Controlling Gully Erosion

  20. 在植被破坏15年的裸露休闲地浅沟集水区,侵蚀蚀强度随坡长的增加而增加,且浅沟槽侵蚀量大于浅沟间,切沟沟槽侵蚀量大于切沟间。

    As slope length increased on hill-slope in a shallow gully catchment that has been destroyed for 15 years , soil erosion intensity tended to increase ;

  21. 平沟造田技术在沟蚀治理中的应用

    The application of filling ditch to reclamation technique in gullying control