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Moisture could be easily controlled by wet air feeding and leachate recirculation.
The relationship between residual Rs (or Rh) based on soil temperature and observed Rs (or Rh) and soil moisture could be well fitted in a quadratic model.
Furthermore, the results show that simulation of soil moisture could be improved if the errors in these important parameter combinations are reduced.
Even in the most arid places on Earth, there is some moisture in the air, and a practical way to extract that moisture could be a key to survival in such bone-dry locations.
Our results demonstrated that spatial means and variability of soil moisture could be reliably estimated using measurements from nearby uplands provided previous soil moisture datasets for gullies and upland locations are simultaneously available.
On the other hand, on the terrestrial ecosystem side, some of this decrease in soil moisture could be offset by CO2 fertilization the extent to which is not known (and very controversial–I've had people in both camps tell me that it is KNOWN what the right answer is and given me a completely different answers!).
Similar(42)
Un-ventilated attics prevent snow accumulation but do not allow for effective removal of moisture, which could be risky and prone to moisture damages.
In spite of some computational and practical limitations, image analysis of apparent soil moisture patterns could be used in connection with traditional soil moisture sampling, which always renders punctual estimates.
No differences in soil moisture content could be found between gap and understory microsites.
The moisture absorption could be reduced five folds compared to that of normal clay aerogels depending on the exposure relative humidity.
In addition, the reduction in moisture content could be remarkably enhanced by using a vacuum pump to remove the evaporated water vapor from the inside of the dryer.
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