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The movement of heat embodied in water vapour as it leaves vegetation is not well understood given the complexity of the dynamics. [11] While the movement of water into the atmosphere through evapotranspiration and consequent cooling is broadly accepted, the movement of water further into the atmosphere is more contentious. [12]
Hydraulic redistribution is a passive mechanism where water is transported from moist to dry soils via subterranean networks. [1] It occurs in vascular plants that commonly have roots in both wet and dry soils, especially plants with both taproots that grow vertically down to the water table, and lateral roots that sit close to the surface.
Transpiration cools plants, as the evaporating water carries away heat energy due to its large latent heat of vaporization of 2260 kJ per liter. This section is an excerpt from Transpirational cooling (biological) .
The specific heat of pure water is ~ 1 calorie per gram, the specific heat of dry soil is ~ 0.2 calories per gram, hence, the specific heat of wet soil is ~ 0.2 to 1 calories per gram (0.8 to 4.2 kJ per kilogram). [90] Also, a tremendous energy (~584 cal/g or 2442 kJ/kg at 25 °C) is required to evaporate water (known as the heat of ...
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The growth of trees is another source of disturbance, creating a micro-scale heterogeneity which is still visible in soil horizons once trees have died. [190] By passing from a horizon to another, from the top to the bottom of the soil profile, one goes back in time, with past events registered in soil horizons like in sediment layers.
“We saw damage to plants this summer that had never showed heat stress before,” Schilling said. Sunburned leaves of a mock orange shrub on Aug. 23. Brown patches show where the tissue was damaged.
With heat, we get humidity, and the moisture in the air allows the water in the soil to evaporate more slowly. This is why you should always check the soil before watering. Only water when the ...