Chinese translation for "壤中流"

prompt subsurface flow

Related Translations:

真理之川从它的错误之沟渠中流过:  the stream of truth flows through its channels of mistakes

壤:  名词1.(土壤) soil 短语和例子粘[砂] 壤 clayey [sandy] soil; 沃壤 fertile [rich] soil2.(地) earth 短语和例子天壤之别 be as far removed as heaven from earth; be vastly different; 有霄壤之别。 there is a world of differenc

壤质:  loamy texture

壤粘土:  loam clay

棕壤:  brown forest soil;braunerde; [俄语]burozem;[农业] brown earth; brunisolic soil

云壤:  phsar reamream

壤驷:  a surname 短语和例子壤驷赤 rangsi chi

壤丘:  rang qiu

富水土壤:  water ground

班梅壤:  ban me giamg

Example Sentences:

	1.	Effect of pipe flow on interflow on granite slope in three gorges area of yangtze river 长江三峡花岗岩坡面管流在壤中流中的作用
	2.	On the development process , the rills were influenced by rainfall runoff on slope , but the sockets were the result of the long - term repetitious action of rainfall and runoff and subsurface flow 在发展过程上，前者受降雨径流侵蚀作用时间集中；后者是在长期多次降雨形成地面径流和壤中流侵蚀的共同作用下，逐渐发展起来。
	3.	On the formation mechanism , the rills were mainly formed by the concentrated action of the runoff on dyke slope , while the formation of socket mainly depended on surface runoff , subsurface flow and the existing defects within the dykes such as crack , mouse hole , fox and brocks dens 在成因上，前者主要是降雨形成超渗地面径流的集中对戗坡的侵蚀作用而形成；后者主要与坡面径流、壤中流，以及土堤的薄弱点(如裂缝、鼠洞、狐1一灌洞等）有关。
	4.	When soil antecedent condition is dry and the initial rainfall intensity is high , peak surface runoff also considerably lag behind that of rainfall , because of the formation of temporary relative impermeable top layer ; b ) surface runoff is controlled primarily by infiltration - excess runoff mechanism under unsaturated condition ; the major fraction of surface runoff are dominated by saturated infiltration - excess runoff response , only a small fraction by return flow mechanism when soil is saturated ; c ) subsurface flow is dominated by saturated runoff mechanism , and the duration of subsurface post the rainfall end is dependent upon rather the soil properties than the rainfall characteristics ; d ) subsurface flow intensity in cultivated soil layer ( 0 ~ 20cm ) is high up to 35mm / h when rainfall intensity is up to 120mm / h , indicating the existing of macropores and pipe flow in cultivated layer 2 )耕作制下紫色土的产流主要机制是： 1 )当雨前土壤含水量未达到饱和状态时，表面产流起始时间有明显滞后现象，这与紫色土的快吸水性和较多非毛管孔隙密切相关；当雨前土壤较干燥，降雨初期雨强较大时，易形成临时相对不透水表层，表面产流峰也有明显滞后现象。 2 )表面径流的产流方式主要是超渗产流，当土壤达到饱和状态后，有四川大学博士学位论文小部分回归流发生，但主要是饱和超渗产流发生，因为紫色土的相对不透水层和其它透水障碍层不明显。 3 ）壤中流主要是饱和产流，与降雨过程有明显的滞后，而且雨停后的壤中流产流历时与降雨特征无关。
	5.	For the soil infiltration , generally , the order of the original and stable infiltration speed from big to small is the inner , the outer space and the paludal trace , as well as layer a b . in the view of the rainfall balance of the wildwood , the canopy interception is averagely 61 . 10 % of the rainfall , the trunk runoff 0 . 80 % , the inner 38 . 10 % , the surface and the litter evapotranspiration 18 . 00 % , the surface runoff does n ' t appear in the forest , and the interflow is also very small , which is 0 . 30 % of the total rainfall ; the conflux is 21 . 10 % 原始森林的水量平衡中，林冠截留量平均占降雨的58 . 27 ，树干径流量占降雨的0 . 80 ，林内降雨占降雨的40 . 93 ，地表蒸发及地被物蒸散量占总降雨的20 . 13 ，林内很少发生地表径流，壤中流量也极少，只占总降雨的0 . 07 ；汇流量占总降雨的21 . 43 。

Similar Words：

"壤质细砂土" Chinese translation, "壤质细土" Chinese translation, "壤质粘土" Chinese translation, "壤中冰" Chinese translation, "壤中空气" Chinese translation, "壤中流土内水流" Chinese translation, "壤中气" Chinese translation, "壤中气探头" Chinese translation, "壤中水相对活动性" Chinese translation, "壤中蒸气测量" Chinese translation