补充量 meaning in Chinese
magnitude of recruitment
Examples
- The supplement had about the amount of caffeine found in two cups of coffee
关于咖啡因的补充量是2杯咖啡的所含的量。 - 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 - The results show that after reaching relative stableness , the dam system located in the region is able to supply 1 . 6 - 2 . 9 billion m3 of water for agriculture . most annual runoff in approximately half of years can be stored and utilized , and the replenished soil moisture is 5 . 2 billion m3 above in more than half of years
结果表明：河龙区间在坝系达到相对稳定后，通过坝系的拦蓄作用，每年可提供16 29亿m ~ 3农业用水；有47的年份年径流大部分可被拦蓄利用；有53的年份坝系土壤水分补充量可达52亿m ~ 3以上。 - Traditionally , the saturated zone is modeled as a simple lumped continuity equation : , dsitqsdt where t is time , s is the total storage in the reservoir , i is the spatially integrated volume of incoming wa - ter , and q is the discharge subsurface runoff which only depends on the total storage s . this kind of subsurface runoff model has many different parame - terizations 10 12 , however it has a very common char - acteristic that the subsurface runoff is just a sin - gle - valued storage - discharge function
对于大尺度水文模型而言,目前常常采用的是集总式的地下径流机制,其连续性方程一般可表示为d , dsitqst ? 1这里t是时间, s表示整个流域潜水面土壤层的饱和区域总的水分储存量, i t表示t时刻土壤的非饱和区域向整个潜水面的水分补充量, q s表示仅依赖于水分储存量s的地下径流量量