The Effect of Temperature
Pore suctions have the effect of “pulling” the saturated zone nearer the ground surface than it would otherwise have been from where evaporation becomes possible. When evaporation is significant then upward water flow takes place to replace the water being evaporated. Evapotranspiration by vegetation also introduces an upward water flow towards roots in a similar manner. In hot climates, evaporation can lead to upward moving water tens of metres above the phreatic surface and it can also lead to salts being lifted to the surface where they precipitate out in the soil pores forming calcretes and silcretes (Sabkha soils are an example of this).
Another cause of suction is seasonal ground freezing in high latitudes or at high altitudes...
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