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1)  overland flow erosion
坡面流侵蚀
2)  hill-slop soil erosion module
坡面流侵蚀模型
3)  slope erosion
坡面侵蚀
1.
The slope erosion is the original zone of water and soil loss and water and soil on slope must be treated quickly.
坡面侵蚀是水土流失的源区 ,有必要加快坡面水土治理。
2.
According to observation data and the outcomes of artificial rainfall in Wangjiaqiao basin, based on erosion mechanics mechanism, two concepts of slope erosion and basin erosion are distinguished grimly and soil erosion models of slope and small watershed have been established.
根据王家桥流域观测资料及人工降雨实验成果,从侵蚀力学机制出发,严格区分了坡面侵蚀与流域侵蚀两个不同的概念,建立了坡面侵蚀模数和流域侵蚀模数。
3.
There is serious slope erosion when the railway or road is constructed in granite region in southern China where ecological environment and engineering conditions is weak area in.
南方花岗岩地区是生态环境和工程条件脆弱区之一,铁路公路穿过时,常常存在较为严重的坡面侵蚀问题。
4)  slope surface erosion
坡面侵蚀
1.
It is considered that the slope surface erosion is the inducing and promoting factor of the gradual destruction of the loess slope in long-term rainfall wash and infiltration,whose surface is exposed and within which is the slippage interface.
分析了斜坡坡面遭受天然降水与人类活动的侵蚀破坏对坡体稳定性的影响,认为坡面裸露的黄土边坡在长期的雨水冲刷与入渗情况下,坡面侵蚀破坏成为滑动面位于土层中的黄土边坡渐进破坏的诱发与促进因素。
2.
From the following four aspects: drag forces, velocity, energy and sediment carrying capability of slope surface flow, the threshold gradient of slope surface erosion in the granite area in the south of china is discussed, and it is obtained the critical slope gradient is from 35 to 43 degree.
从坡面流拖曳力、流速、能量及挟沙力4 个方面,分析了南方花岗岩地区坡面侵蚀临界坡度,得出其临界坡度为35~43
5)  Soil erosion
坡面侵蚀
1.
However, soil erosion and seasonal drought are major constraint for sustainable agriculture due to improper land use and uneven distribution of .
研究结果有助于深入了解坡面侵蚀机理,为泥沙输移模型开发提供必要的土壤参数。
6)  runoff generation and soil erosion
坡面降雨侵蚀产流产沙
补充资料:坡流液桥涂布
分子式:
CAS号:

性质:系胶片生产中一种常用的挤压涂布方式。涂液进入挤压嘴的腔体,经阻流间隙形成均匀液膜,沿倾斜坡流面流至唇边。在涂布过程中,由于润湿作用,液膜片与片基表面之间形成悬空弯月面(即液桥)从而达到涂布的目的。液桥的形态和稳定状况直接影响涂层厚度和质量,它适合一次多层(一般6~8层)快速涂布。

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