Titlebook: Climate Under Cover; Tadashi Takakura,Wei Fang Book 2002Latest edition Kluwer Academic Publishers 2002 agriculture.carbon dioxide.climate.

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Heat Balance of Bare Ground,yers, neglecting water movement in the soil. At the surface, not only sensible but also latent heat transfer occurs. These heat flows from the surface to the ambient air are by convection. Therefore, three types of heat transfer are at work in a soil-air system, as shown in Fig. 4.1

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Solar Radiation Environment,he earth. Therefore, for cultivation in controlled environments, it is very important to calculate how much of the solar radiation we can utilize at a given place on the earth at a given time of the year.

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https://doi.org/10.1007/978-3-030-88670-7ren Bereich Wärme, wo sie bei hohen Temperaturen zur Verfügung steht. Hier aber müßte nur dem Feststoff Wärme übertragen werden, der innerhalb des Fließbettes die relativ höchste Temperatur hat und kurz vor dem Austritt steht.