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Titlebook: Water Requirements for Irrigation and the Environment; Marinus G. Bos,Rob A. L. Kselik,David J. Molden Book 2009 Springer Science+Business

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Effective Precipitation,tural precipitation. Hence, precipitation needs to be measured (Fig. 3.1). Not all precipitation infiltrates into the soil; a part may evaporate; another part may become surface runoff. Of the precipitation that infiltrates, only a part will be stored in the root zone and the remainder will recharge
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Capillary Rise,ted effective precipitation, .), through irrigation, and through capillary rise. If the depth to the groundwater table is shallow (less than about 3 m) and the soil is fine-textured, capillary rise can contribute a significant volume of water to the rootzone of the crop. However, in order for the gr
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Capillary Rise,ted effective precipitation, .), through irrigation, and through capillary rise. If the depth to the groundwater table is shallow (less than about 3 m) and the soil is fine-textured, capillary rise can contribute a significant volume of water to the rootzone of the crop. However, in order for the gr
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Using the CRIWAR Software,ory and calculation procedures to estimate the potential evapotranspiration of agricultural crops. Chapter 3 presents three methods to estimate the contribution of precipitation to crop water requirements while Chapter 4 presents the water contribution to the effective root zone from capillary rise.
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Using the CRIWAR Software,ory and calculation procedures to estimate the potential evapotranspiration of agricultural crops. Chapter 3 presents three methods to estimate the contribution of precipitation to crop water requirements while Chapter 4 presents the water contribution to the effective root zone from capillary rise.
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Capillary Rise,. This chapter illustrates the case of when capillary rise is a potential source of water. In which case, the calculated crop water requirements should be corrected for the contribution from groundwater (see Section 4.6)
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