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Determination of Actual Evapotranspiration and Crop Coefficient for Hot Pepper ( Capsicum annum L.) Inside Plastic Houses
Naem Mazahrih, INCARTT
Abstract
The limited water resources in arid and semi-arid regions, such as Jordan, are considered the greatest challenge facing agricultural development in the country. In addition, high population growth rate in Jordan increases pressure on the available water resources.
About 68% of the available water resources in Jordan is allocated for irrigated agriculture. Decision-makers have to look for methods to reduce water consumption in this sector through developing appropriate management to improve water-use efficiency. For these purposes, information about actual and potential plant water requirement under specified condition is necessary. Irrigation scheduling aiming for maximum crop yield production is determined based on crop transpiration in the field with soil moisture maintained at an optimal condition. The subject of evapotranspiration and crop water needs has been widely investigated by many researchers such as Doorenbos and Pruitt (1975), Jensen et. al., (1990), and Allen et. al. (1994). The accuracy of ET estimates depends primarily on the ability of the equations being used to describe the physical laws governing the processes and the accuracy of the meteorological and cropping data. (Jensen et al., 1990).
Evapotranspiration is a necessary parameter for proper irrigation
scheduling and for establishing the duties and the dimension of the
irrigation system. It allows better water management, by adjusting
the volume and frequency of irrigation to meet crop requirements
depending on the soil characteristics. Furthermore, it is a crucial
factor on which irrigation management decisions are based. Managing
limited water supplies as well as designing and evaluating
irrigation systems, are all dependent on ET data. Studies concerning
ET for alfalfa and grass have special importance since alfalfa and
grass are being used as reference crops for reference
evapotranspiration estimation (Allen et. al.,1994). Reference crop
ET is the rate at which water will be evaporated from given plant
and soil surfaces, with the surface specified, if water is readily
available within the plant root zone. (Wright, 1996). |