0.49 The hydraulic conductivity (K) of an isotropic aquifer is 10 m/day. If the hydraulic head within the aquifer drops 4 m at a distance of 750 m, the groundwater flow velocity within the aquifer is m/day. (up to the third decimal place)
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If the hydraulic head within the aquifer drops 4 m at a distance of 750 m, the groundwater flow velocity within the aquifer is
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