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

English translation for "total storage"

总蓄水量
Example Sentences:
1.Total storage capacity is limited by number of songs
总储存量受限于歌曲数目。
2.Plan for total storage capacity of 4 times amount of raw data
计划总存储容量为原始数据的四倍。
3.This phase cost the government more than $ 9 , 500 , 000 and the extended reservoir had a total storage capacity of 3 billion gallons
水塘全期耗资950多万元,总容量达30亿加仑。
4.When you add dimensions to an array , the total storage needed by the array increases considerably , so use multidimensional arrays with care
增加一个数组的维数时,该数组所需的总存储空间会急剧增大,因此应慎用多维数组。
5.In 1959 , with the completion of the tai lam chung reservoir , hong kong s total storage capacity rose to 10 billion gallons . on average every person would have a daily supply of 9 . 1 gallons
1959年大榄涌水塘建成后,全港的存水量提升到100亿加仑,平均每人每日供水量约为9
6.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
7.Ultimately , the function derived here is in - tended for use with the lumped continuity equation in which the only variable describing the internal state of the aquifer is the total storage ; so suppose the storage in the aquifer is known to be s , then 0100221 dsineed11ecos esin 1e . nlsullxsaxknnnalnsnnnnnnalnnulksfhxxfnfxdxhfxkbfnflkbaaluhfk by defining 0 lshhxdxl it is easy to see that is h h greater than or equal to by and fig
因为新的入渗所造成的潜水面的变化与原来稳定状态下的潜水面有下面的差异1 , , sin , saxnnnnsnhxthxthxfsttxekbs ? ? ? ? ? ? ? ? ? 21而这里的稳定状态显然是根据潜水面的逐次稳定的理论把任何一个时候的潜水面都看作是某一恒定的入渗在时间趋于无穷大时得到的一种理想状况
8.Subsurface runoff is obviously closely related with soil water movement in the unsaturated soil zone and dynamic change of the groundwater table . there - fore , it is necessary to develop the subsurface runoff model with a physical base associated with recharge on the aquifer and total storage in the reservoir . also a soil model with a dynamic representation of the groundwater table makes it possible and reasonable to represent a more logical subsurface runoff parame - terization
地下径流显然与非饱和土壤层中的水分运动以及地下水位的动态变化密切相关,因而有必要发展考虑土壤含水量与潜水面science in china ser . d earth sciences 376中国科学d辑地球科学第36卷水分通量以及地下水位动态变化的土壤水模型相适应且具有物理意义的地下径流模型;同时地下水位动态表示的土壤水模型也为发展更为合理的地下径流模型创造了很好的条件
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