1) furrow interference infiltration
沟灌交汇入渗
1.
In order to understand the patterns of water infiltration in furrow irrigation,based on lab experiment under furrow infiltration,a two stage infiltration model of furrow interference infiltration was founded and the reduced infiltration characteristics of furrow interference infiltration to furrow free infiltration was researched.
为进一步探明沟灌灌水沟的水分入渗规律,通过室内沟灌入渗试验,分析了沟灌交汇入渗的入渗规律,建立了沟灌交汇入渗的二阶段入渗模型,研究了沟灌交汇入渗相对与沟灌自由入渗的减渗特性。
2) interference infiltration
交汇入渗
1.
The shape of wetting soil, the wetting front movement law, the soil moisture content and redistribution law under the film hole multi point sources interference infiltration are studied via a great number of the tests of film hole multi point sources interference infiltration.
通过大量膜孔多点源交汇入渗试验 ,研究了膜孔多点源交汇入渗湿润体形状、湿润锋运移规律、湿润体内土壤含水量和土壤水分的再分布规律。
2.
Through test, characteristic and influential factors of multiple point sources interference infiltration are analyzed.
通过大量膜孔多点源交汇入渗试验资料 ,分析了膜孔多点源交汇入渗特性和影响因素 ,研究了膜孔直径、膜孔间距、土壤质地、土壤容重和土壤初始含水率等因素对多点源膜孔交汇入渗的影响 ,提出了各影响因素与膜孔交汇入渗量和交汇时间的关系 ,并分析了膜孔交汇入渗机理。
3) bilateral interference infiltration
多向交汇入渗
1.
Infiltration reduction effect and mathematical model of bilateral interference infiltration in film hole irrigation;
膜孔灌多向交汇入渗减渗特性和数学模型研究
4) single-line interference infiltration
单向交汇入渗
1.
Influence of fertilizer solution concentration on water transport characteristics under film hole single-line interference infiltration
肥液浓度对膜孔单向交汇入渗水分运移特性的影响
5) penetration through ditch irrigation
沟灌渗透
1.
The irrigation methods included conventional flooding irrigation and penetration through ditch irrigation with different farmland width as 90cm, 130cm and 170cm.
研究了不同畦宽(90cm、130cm、170cm)沟灌渗透栽培与常规淹水栽培对直播水稻根、茎、叶生长发育特性、机能及其产量的影响。
2.
Three kinds of farmland with different width (90 cm, 130 cm and 170 cm) for penetration through ditch irrigation have been studied, as comparison with the irrigation by conventional inundation, to see their influences on the growth characteristics, functions of the roots and leaves of direct- seeding rice and its yield.
研究了90、130、170cm3种畦宽沟灌渗透灌溉与常规淹水灌溉对直播水稻根、叶生长特征、机能及其产量性状的影响。
6) infiltration irrigation through shallow furrow
浅沟渗灌
1.
Study on yield increasing mechanism of the infiltration irrigation through shallow furrow to the southern direct sowing rice;
南方直播水稻浅沟渗灌节水增产机理研究
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