| 1. | Flowstones are formed via the degassing of vadose percolation waters.
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| 2. | During this vadose, or air filled state, abundant speleothem deposits formed.
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| 3. | Therefore, the resulting finite water-content vadose zone flow equation is:
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| 4. | But until now scientists believed that waste was securely trapped in the vadose zone.
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| 5. | Many cave passages are formed by a combination of phreatic followed by vadose action.
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| 6. | If the vadose zone envelops soil, the water contained therein is termed soil moisture.
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| 7. | Krubera Cave has an extremely steep profile and reveals a huge thickness of the vadose zone.
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| 8. | Hence, the vadose zone extends from the top of the ground surface to the water table.
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| 9. | The vadose zone is often the main factor controlling water movement from the land surface to the aquifer.
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| 10. | Surface and subsurface stores are linked though the vadose zone using a number of different optional numerical methods.
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