Analytical Solutions of Vertical Airflow in an Unconfined Aquifer with Rising or Falling Water Table
The rise and fall of the groundwater level can drive air flow in the vadose zone. In turn, the air flow can interact with the water flow. When the unconfined aquifer is covered by a low-permeability media, the coupling of the water flow and the air flow is more obvious. In this study, a conceptual m...
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Veröffentlicht in: | Water (Basel) 2021-03, Vol.13 (5), p.625 |
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