Abstract
We are concerned with radiation and the microclimate above the soil because they have such large influences on:
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1)
Evaporation of water from soil.
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2)
Transpiration of water from plants.
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3)
Soil and air temperature.
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4)
Plant growth (plant growth is closely related to transpiration and to soil and air temperatures).
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References
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Hanks, R.J., Ashcroft, G.L. (1980). Soil—Plant—Atmosphere Relations. In: Applied Soil Physics. Advanced Series in Agricultural Sciences, vol 8. Springer, New York, NY. https://doi.org/10.1007/978-1-4684-0184-4_4
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DOI: https://doi.org/10.1007/978-1-4684-0184-4_4
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