在水文地质勘探试验中发现，各类不同设备抽水产生的水跃值各不相同。
From investigating and testing the hydrogeology, this paper discusses that different pump equipments make different water_leap values.
结果表明无论对稳定内部水跃还是移动内部水跃计算所得的水量掺混系数均比试验值约小10%，初步验证了本文所提出的理论计算方法。
The water entrainment coefficients calculated from theoretical formula both for stable hydraulic jump and movable hydraulic jump in density flow are less than the experimental values by 10%.
结果表明无论对稳定内部水跃还是移动内部水跃计算所得的水量掺混系数均比试验值约小10%，初步验证了本文所提出的理论计算方法。
The water entrainment coefficients calculated from theoretical formula both for stable hydraulic jump and movable hydraulic jump in density flow are less than the experimental values by 10%.
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