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Home > chinese-english > "storage equation" in English

English translation for "storage equation"

储量方程
蓄量方程
蓄水量方程


Related Translations:
unification equations:  合一方程
rigorous equation:  精确方程式
breguet equation:  布列盖航程公式
terpolymer equation:  三元共聚体等式
helmholtz equation:  亥姆霍兹方程式;黑目合兹方程式黑目合兹方程式
colour equation:  色方程
equation budget:  equation平均到期日
resistance equation:  阻力方程
deformation equation:  变形方程
consistent equation:  相容方程
Example Sentences:
1.In this paper , a physics - based subsurface runoff parameterization with water storage and recharge based on the boussi - nesq - storage equation is presented . this paper is or - ganized as follows
1基于boussinesq - storage方程的地下径流机制下面主要是以潜水面上的boussinesq方程为基础来建立地下径流模型
2.It can be seen from the temporal behavior of the three aquifers that hillslopes with a larger inclination react significantly quicker to the re - charge input and tend tend to drain faster than nearly hori - zontal aquifers . this is caused by the increasing it can therefore be estimated using a finite differ - ence approximation , ststttntlqsnt where t is a discrete change in time . so the subsurface runoff parameterization with wa - ter storage and recharge based on the boussinesq - storage equation is founded
很显然对于同样的入渗强度,地下径流深随着坡度的增大而变化明显,这里面关science in china ser . d earth sciences第4期? ?田向军等:基于boussinesq - storage方程同时考虑水分储存和入渗的地下径流机制379图2模型参数的敏感性键的原因在于随着坡度的增大,重力的因素起到了更大的作用
3.11 can be a subsurface runoff parameterization with water storage and recharge based on the boussinesq - storage equation 625 written as 11 ee sineee sine . nnnnktaxbtnnuxktbtnsknnktbtaxnnuxktbtnsknnhxtwfnxhkbwfnxhkb letting t tend to infinity , one can get the steady aquifer function hs 13 : 1 sinee . uxaxnsksnnnfnhxxhkb multiplying through by the specific yield , f , and in - tegrating with respect to x between 0 and l gives the drainable storage associated with this steady - state free surface
下面考虑整个潜水面的一种稳定状态,也就是是对于任意一个恒定的入渗,当时间时潜水面将达到稳定的状态不再发生变化,这个时候显然有, 0 , . sntnt t , ssqnl也就是入渗补充量等于地下径流量
4.This model is validated by a subsurface flow separation algorithm for an ex - ample river basin , which shows that the new model can simulate the subsurface flow reasonably . keywords : subsurface runoff parameterization , boussinesq - storage equation , water storage and re - charge . hydrological processes including surface runoff , subsurface runoff , and soil water movement play a great role in land surface processes
文中基于boussinesq - storage方程建立了同时考虑潜水面水分储存和非饱和层水分入渗两方面影响的地下径流机制,并利用流域水文资料以及地下径流分离算法验证了所建立模型的可靠性,结果表明该模型能够比较合理地模拟地下径流的变化情况
5.5 summary a subsurface runoff model with water storage and recharge is developed in this paper based on the bous - sinesq - storage equation . the sensitivity of the model parameters is also tested . the subsurface runoff model is applied to a river basin with observed precipitation , observed air temperature data , observed runoff data , and a base flow separation algorithm in order to vali - date the model application
5结论与讨论基于boussinesq - storage方程发展了同时考虑水分储存和入渗的地下径流机制,分析了模型参数的敏感性,并针对淮河流域的的息县控制站所控制的区域,利用降水径流资料及通用的基流分离算法进行了验证
6.Yang and xie 9 developed a numeri - cal model for the moving boundary problem through reducing it to a fixed boundary problem by a coordi - nate transformation . it is necessary to reduce the a subsurface runoff parameterization with water storage and recharge based on the boussinesq - storage equation 623 computational cost of the groundwater model so that it can be applied to a land surface model for climate studies
文献9通过一个坐标变换将运动边界问题转化为一个固定边界问题,进一步改进了该土壤水模型的数值计算方法,使其减少计算量,达到能在一般通用的模式中实际应用
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