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\frac{d Q_{WAQ}}{dt} = \frac{4 \pi \sigma}{ \ln \frac{1.781 \cdot A_e^2}{ 4 \pi \chi t} } \cdot ( p_i - p(t)) |
where
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| initial formation pressure | ||||||||
| field-average formation pressure at time moment
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| aquifer transmissibility | ||||||||
| aquifer diffusivity |
This model is based on assumption of:
- Infinite Acting Radial Flow Aquifer
- Slow variation of aquifer influx water influx
in timeLaTeX Math Inline body Q_{WAQ}(t)
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