片语

preferential flow coefficient优先流系数

Preferential Flow Paths优先路径

fieldwide preferential flow direction油田主流向

preferential solution flow显微组织

KDM preferential flow modelKDM优先流模型

KDW preferential flow modelKDW优先流模型

preferential flow s types优先流类型

preferential flow path优先流槽

英汉例句

• to analyze the influence of rainfall on preferential flow, the preferential flow process was observed when the rainfalls were recorded.

  在降雨过程中观察优先流过程，分析降雨对优先流的影响。

• soil preferential flow is the non-equilibrium channeling flow.

  土壤优先水流是非平衡管道流。

• the problem of wetting front infiltration theory is the neglect of the affection of preferential flow in soil.

  湿润锋面入渗理论没有考虑土壤水优势流的影响。

• preferential flow paths「 means the soil pores formed by plant roots, burrowing animals, cracks and fissures caused by soil shrinkage and soil swell and finger channels made by unsteady wet front.」

  「优先路径」是指土壤中植物根系穿插而产生的根孔、动物的运动通道和居穴、由于土壤膨胀收缩形成的裂隙，以及因湿润锋不稳定所形成的指状渗透通道等。

• based on that, the preferential flow model was modified.

  在此基础上，修正了优先流模型。

• the preferential flow of heavy metals(cu2+ and zn2+)was evaluated by equilibrium and non-equilibrium convective-dispersion equation(cde).

  运用平衡和非平衡对流-弥散模型对溴离子和铜、锌离子在不同土柱中的穿透曲线进行拟合。

• the main factor influencing the peak of preferential flow is the amount of rainfall, which is evidently positively related to the peak of preferential flow.

  影响优先流峰值流量的主要降雨因子是降雨总量，两者为显着正相关关系。

• in both conditions, the peak of preferential flow appeared earlier than that of infiltrated soil water flow.

  在两种情况下，优先流的峰值都先于土壤渗流。

• in this paper, the lower boundary flow of considered upper soil stratum was expressed into linear relation with infiltration ratio and saturated degree by introducing preferential flow coefficient.

  率先采用线性简化式，并引入优先流系数来表示计算土层下边界渗漏水流通量；

• the general research method were reviewed. some problems in research on the root system and preferential flow were presented.

  介绍了根系及优势流的一般研究方法，以及有关根系和优势流关系的研究中的一些问题。

• there are some special issues that cause difference to predict fluid flow in fractured vadose zone, including capillary flow, film flow, preferential flow and fracture-matrix interaction.

  非饱和带裂隙巖体中的渗流和饱和带相比有其不同的特点，包括毛细管流、薄膜流、优先流和裂隙-基质相互作用等。