1) infiltration ponding time
入渗积水时间
1.
In order to study the effects of water supply intensity,soil bulk density,initial soil moisture and soil texture on infiltration ponding time under the condition of non-sufficient water supply,and build mathematical relation on infiltration ponding time and each factor,infiltration experiments with eight kinds of homogenized soils under non-sufficient water supply condition were conducted indoors.
为了研究供水强度、土壤容重、初始含水率、土壤质地等因素对非充分供水入渗积水时间的影响,建立入渗积水时间与单一因素的数学关系,在室内进行了8种均质土壤的非充分供水入渗试验。
2) ponding infiltration
积水入渗
1.
The insitu ponding infiltration test was conducted with the doublering infiltration device and the soil water content profile was measured with the γray in Qinwangchuan irrigatedarea.
在秦王川灌区利用双环入渗仪在现场进行了积水入渗试验，同时利用γ射线测定土壤水分剖面，进而根据室内外所测定的土壤水分特征曲线，推求了该灌区非饱和土壤水分运动参数，并对室内外所确定的结果进行了对比分析。
3) catchment distribution curve
积水时间
4) In water time
入水时间
5) ponding water infiltration characteristics
积水入渗特征
6) one-dimensional ponded water infiltration
一维积水入渗
1.
Experimental research on the effect of entrapped air on one-dimensional ponded water infiltration
封闭气泡对一维积水入渗影响的试验研究
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)
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