2) the soil stable infiltration rate
土壤稳定入渗率
3) vegetation restoration
土壤稳定入渗
1.
The effect of vegetation restoration on soil stable infiltration rates in small watershed of loess gully region;
黄土丘陵沟壑区小流域植被恢复对土壤稳定入渗的影响
4) soil steady infiltration rate
土壤稳渗速率
1.
The results show runoff time has a negative relationship with soil bulk, antecedent soil moisture, slope gradient, rainfall intensity, and different tillage measures; soil steady infiltration rates have a positive relationship with rainfall intensity and tillage measures, and have a negative relationship with soil bulk, antecedent soil moisture, and slope gradient.
发现坡面产流历时与土壤容重、初始含水率、坡度、降雨强度、耕作管理措施呈负相关;土壤稳渗速率与降雨强度、耕作管理措施呈正相关,与土壤容重、初始含水率、坡度呈负相关。
5) soil infiltration rate
土壤入渗速率
1.
The results indicated that the soil infiltration rate in forest watershed is obviously higher than that in rangeland watershed.
结果表明 :森林小流域林地土壤入渗速率显著高于荒坡草灌小流域。
6) steady water infiltration rates
稳定入渗速率
1.
This study mainly discuss the spatial interpolation uncertainty of soil steady water infiltration rates in Ji river basin which located in the third vice-area of loess hilly and gully region.
以黄土丘陵沟壑第三副区的藉河流域为研究区,根据65个实测点数据,采用普通克里格法、反距离权重法、样条函数法等插值方法,分析了测点数量变化、栅格像元尺寸变化及插值方法的差异对土壤稳定入渗速率空间插值结果的影响,剖析了空间插值中的不确定性。
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