1) Infiltration type basin
渗入型盆地
2) surface infiltration
地表入渗
1.
The landslide mechanism of rock slope under the influence of surface infiltration is discussed.
采用延伸的摩尔-库仑破坏准则以考虑基质吸力对岩体抗剪强度的贡献,对地表入渗影响下的岩坡失稳机制进行了探讨。
2.
Water flow in fractured rockmass due to surface infiltration is a saturated unsaturated seepage process.
有地表入渗的裂隙岩体渗流是一饱和非饱和渗流过程。
3.
In the doctoral dissertation, thorough studies on determination of unsaturated hydraulic parameters of fracture through experiment and numerical simulation, mechanisms of unsaturated seepage flow in fracture, analysis of saturated-unsaturated seepage flow in fractured rock mass due to surface infiltration and influence of surface infiltration to the stability of rock slope are made.
本文就单裂隙非饱和水力参数的试验测定和数值模拟确定、单裂隙非饱和渗流的机理、有地表入渗的裂隙岩体饱和非饱和渗流分析以及地表入渗对岩坡稳定性的影响等方面展开了较为深入的研究，并将上述研究成果应用于实际大型工程问题的分析中。
3) infiltration
[英][,infil'treiʃən] [美][,ɪnfɪl'treʃən]
渗入(地)
4) surface infiltration
地面入渗
5) penetrating pattern
渗入型式
1.
For a full well excavated down to the impervious stratum, the penetrating pattern could be considered as a model of ca.
完整井情况下的锥探灌浆,其渗入型式可按单向渠道网络模型下的竖向渗流形式来考虑。
6) infiltration model
入渗模型
1.
Thereby two single point source infiltration models including the side infiltration .
通过室内膜孔单点源入渗试验,分析了膜孔灌单点源入渗单位面积侧渗量与一维垂直入渗量的变化规律,研究了膜孔灌单点源入渗单位面积侧渗量与入渗时间、膜孔直径之间的关系,建立了包含垂直一维入渗量和侧渗量的两个具有明确物理意义的膜孔单点源入渗模型,只需知道垂直一维入渗参数、膜孔直径和入渗时间,即可用于膜孔单点源入渗量的计算。
2.
In this paper, infiltration model, formula of soil water movement and interflow in forestland were introduced and analyzed contrastively, and the advantages and shortcomings were pointed out.
介绍国内外林地土壤水分入渗模型、林地土壤水分运动方程、森林流域壤中流模型及其验证和应用 ,并对这些模型做对比分析 ,指出各自的优点和不足 ,阐述深入研究林地土壤水分运动的重要意义。
3.
The aims of the experimental study on multi-factors film hole infiltration are studying film hole infiltration law and setting up a infiltration model which is including pa- rameters of soil dry density(r),soil water content(θ),film hole area(s),on the basis of Kostiakov model,The model provides convenience for the design of film hole irrigation.
多因子膜孔入渗试验研究的目的,就是通过试验研究,探明膜孔入渗规律,建立以 Kostiakov 模型为基础,包含变量 r(土壤干容重)、θ(土壤含水率)、s(膜孔面积)在内的入渗模型,为膜孔灌的设计提供方便。
补充资料：渗入
分子式：
CAS号：
性质：土壤从降水中或流过地面的河流中吸收水的过程。在给定条件下，土壤能够吸收雨水或融雪的最大速率称为渗入量。
CAS号：
性质：土壤从降水中或流过地面的河流中吸收水的过程。在给定条件下，土壤能够吸收雨水或融雪的最大速率称为渗入量。
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