The soil will cool faster because it has a lower specific heat than water (even if it is wet).
The specific heat is a thermodynamic property. It is the quantity of energy required to raise a temperature by one degree Celcius (or Kelvin). By this property, you can measure how much energy a material need to raise its temperature (or how much energy it needs to lose by decreasing the temperature).
The specific heat of water is 1.001 Btu(IT)/(lbm °F).
The specific heat of a dry soil is 0.19 Btu(IT)/(lbm °F).
The specific heat of a wet soil is 0.35 Btu(IT)/(lbm °F).
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Land restoration can include the process of cleaning up and rehabilitating a site that has sustained environmental degradation, such as those by natural cause (desertification) and those caused by human activity (strip mining), to restore that area back to its natural state as a wildlife home and balanced habitat.
Explanation:
- setting up reliable water provisioning (e.g. by digging wells or placing long-distance water pipes)
- stabilizing and fixating the soil