Construct · 1 fields · 1 citations

Thiem equation: a standalone construct

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Hydrogeology

the steady-state relation between pumping rate, transmissivity and drawdown at two distances from a well in a confined aquifer.

In hydrogeology, Thiem equation refers to the steady-state relation between pumping rate, transmissivity and drawdown at two distances from a well in a confined aquifer. This meaning comes from Thiem (1906) in Hydrologische Methoden.[1]

Unit
Recovery means
Measured by

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Nearby constructs

drawdown2 fields · 2 citationsjingle · one word, two constructs relation4 fields · 4 citationsjingle · one word, four constructs transmissivity2 fields · 2 citationsjingle · one word, two constructs

References

Thiem, G. (1906). Hydrologische Methoden. J.M. Gebhardt's Verlag. Open Library record

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