3) non-sufficient water supplied condition
非充分供水
1.
On the basis of indoor test of disturbed homogenized soil water infiltration,the influence of water supply intensity on soil water infiltration was analyzed under non-sufficient water supplied condition.
基于室内扰动均质土壤水分入渗试验,分析讨论了非充分供水条件下供水强度对土壤水分入渗的影响规律。
4) adequate water supply
充分供水
1.
This paper studies the behaviors of water flow advance process based on field experimental data, and suggests the film hole infiltration model based on the Kostiakov infiltration equation, and presents a new method of determining single point source infiltration parameters under adequate water supply in film hole irrigation.
根据膜孔畦灌大田灌水试验实测资料，研究了膜上水流推进规律，并对膜孔入渗采用Ｋｏｓｔｉａｋｏｖ入渗模型，提出利用膜孔畦灌田面水流推进和观测断面水深资料推求充分供水条件下点源入渗参数的新方法。
2.
Film hole infiltration characteristics under adequate water supply are analyzed based on indoor experimental data of vertical infiltration and film hole infiltration, and a Philip model of film hole infiltration under adequate water supply is development.
通过室内垂直入渗和膜孔入渗试验 ,研究了充分供水条件下膜孔入渗特性 ,建立了充分供水条件下膜孔入渗的 Philip模型 ,分析了膜孔入渗与一维垂直入渗之间的关系 ,可以由一维垂直入渗资料确定充分供水条件下膜孔入渗模型。
5) infiltration
[英][,infil'treiʃən] [美][,ɪnfɪl'treʃən]
水分入渗
1.
HJ4/9] A field rainfall simulation experiment was carried out to assess the impacts of conservation tillage on runoff and infiltration, and the effects of surface tillage, residue cover and wheel traffic compaction were also studied.
采用人工模拟降雨试验研究了保护性耕作控制农田地表径流的效果 ,重点探讨了表土耕作、秸秆覆盖及土壤压实 3种因素对地表径流和水分入渗的影响。
2.
In arid areas,the percentage of interception loss may be small,but the role in redirecting water and nutrients in the root zone by stem flow is very significant,infiltration rate increase under the shrubs with higher litter and org.
干旱区严重缺水,土地荒漠化的部分原因是对现有水资源的不合理管理和利用,本文从提高水分利用效率(WUE)的角度,就干旱区降雨截留、水分入渗和土壤蒸发等若干水文过程的影响因素及其机理的研究进展进行评述。
6) water infiltration
水分入渗
1.
Based on soil water infiltration testing and related parameters measured in field,tillage soil water infiltration capacity attenuation process was analyzed and the mechanism was discussed.
基于大田土壤水分入渗试验与相关参数的测定,分析了耕作土壤入渗能力衰减过程,探讨了耕作土壤入渗能力衰减机理。
2.
By using the basic principle of soil hydrodynamics,this paper designs the indoor experiment of soil water infiltration under surge furrow irrigation,and in the light of the influence of the different water-supplying times,circulating ratios and periods on the soil water infiltration process,determines some parameters related to the soil water movement.
应用土壤水动力学的基本原理,设计了波涌沟灌条件下水分入渗的室内试验,针对不同供水时间、循环率及周期对土壤水分入渗过程的影响,测定土壤水分运动有关参数。
3.
A new method of irrigation was designed and tested for its water infiltration and crop water use in the field where maize were grown.
以玉米为试验材料 ,通过大田灌水技术和灌溉制度试验对交替隔沟灌溉水分入渗规律及其对作物水分利用的影响进行了研究。
补充资料：灌溉入渗补给系数
灌溉入渗补给系数
coefficient of irrigation recharge into ground water
guan’gai rushen buji xishu灌溉入渗补给系数(eoeffieient of irriga-tion reeharge into ground water)灌溉水补给地下水的数量指标，是灌溉入渗补给地下水的量与灌溉水量之比。影响因素主要有灌溉定额，土壤含水量、土壤质地、地下水埋深、植被情况和气候条件等。 灌溉水入渗，只有在土壤含水量超过田间持水量时，多余的水才能补给地下水。一般在相同的条件下，灌溉定额小、土壤质地粘重与植被差时，灌溉入渗补给系数小(如果灌溉定额很小，可能无入渗补给);反之则大。田间的地下水埋深大(即非饱和带上壤的厚度较大)，故灌溉入渗补给系数小;反之亦然。当引外区的河水或井水时，由灌溉入渗补给系数算得补给地下水量，作为本区的地下水补给量。引河水灌溉，一般灌水定额较大，灌溉入渗补给系数大;引井水灌溉，灌水定额较小，此系数亦小。(金光炎)
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