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径流计算的英文

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"径流计算"怎么读用"径流计算"造句

英文翻译手机手机版

  • runoff computation

例句与用法

  • Study on runoff calculation method in beijing mountainous
    北京地区坡面径流计算模型的比较研究
  • The operation chart of individual and associated operation of new and old units are plotted by using series of multiyears flows
    通过长系列径流计算,绘制了新老机组单独运行和联合运行的调度图。
  • Calculation of quantity of soil evaporation takes an important part in moisture content prediction , rainfall surface flow calculation and evaluation of water resources
    摘要土壤蒸散发量的计算,在墒情预报、降雨径流计算及水资源评价中都占有重要的地位。
  • The results show that the precision of the model is well , but the influence to the precision of the model in the prediction of field runoff can ' t be ignored
    分析结果表明,该模型应用于小面积径流计算时精度很高,但在进行野外坡面径流量的预测时,不能忽略控制面积的大幅扩大对模型预测精度的影响。
  • Considering that the infiltration capacity curve can ' t express the actual infiltration capacity , the authors develop the surface runoff yield models that combine with the infiltration capacity curve , unstable raining process and antecedent soil moisture in each rainfall or over a duration time
    考虑到流域实际的下渗能力,建立了将下渗能力曲线、不稳定降雨过程和前期土壤含水量有机联系起来的流域场(时段)暴雨地表径流计算模式。
  • Regard - ing the surface runoff mechanism , liang and xie 1 , 2 presented a new surface runoff parameterization which dynamically represents both the horton and dunne runoff generation mechanisms within within a model grid cell together with a consideration of the subgrid - scale het - erogeneity , which can be applied to not only humid regions but also droughty regions as well 3 , 4 . regard - ing the soil water movement , xie et al . 5 developed an unsaturated flow numerical model based on the finite element method , and xie et al . 6 presented another numerical model to compute soil moisture and water flow flux together by means of a mixed finite element method
    在地表径流方面,文献1 3发展了一种同时考虑蓄满超渗产流机制及次网格非均匀性的新的径流机制模型,并用其改进了陆面模式vic variable infiltration capacity中的径流计算,该模型既适用于湿润地区也适用于干旱地区4 .在土壤水模型方面,文献5采用有限元质量集中法发展了非饱和土壤水流的数值模型,文献6则采用混合有限元法建立了非饱和土壤水分含量和通量计算的数值模型
  • By the test of the imitated rain , the article researches some rainfall runoff features of the plain area which the slope is less than 3 , the changing regulation of runoff coefficient under the steady rainfall condition , puts forward the calculation principle of the rainfall runoff this area by using the maximum runoff coefficient method and makes a calculation of the runoff for the process of rainstorm under the unsteady or natural condition
    利用仿雨试验,研究地面坡度小于3的平原区降雨产流的特征,稳定降雨条件下径流系数的变化规律,提出了“最大径流系数法”对平原降雨产流的计算原理,对非稳定及天然条件下的暴雨过程进行了径流计算
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