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Crop yield response to water - Cra

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Maximum Yield (Y x )The FAO I&D No. 33 recommended procedures for estimating maximum <strong>yield</strong> either fromavailable local data for maximum crop <strong>yield</strong>s or based on the calculation of maximum biomassand a corresponding harvest index, following two different procedures:I. Wageningen procedure (De Wit, 1968; Slabbers, 1978)II. Ecological zone approach (Kassam, 1977)These procedures for <strong>yield</strong> estimation were developed in the late sixties and seventies. Theconsiderable advances in agronomy and crop physiology, though, allow for the use of moreprecise methods <strong>to</strong> estimate maximum <strong>yield</strong>s.Maximum <strong>Crop</strong> EvAPOTRANSPIRATION (ET x )Procedures for determining ET x were based on FAO guidelines for crop-<strong>water</strong> requirements(ET c ), and the ET x component of Equation 1, which is equal <strong>to</strong> ET c , was determined throughthe product of the reference-crop evapotranspiration (ET o ) times the crop coefficient (K c ), i.e.(2) ET x = K c ET oOriginal procedures for determining ET o are described in FAO I&D No. 24 (Doorenbos andPruitt, 1977), offering different equations for its calculation according <strong>to</strong> the availableclimate data. K c values were provided for a large number of crops and procedures <strong>to</strong>determine ET c over the growing season. Subsequently, revised procedures for calculatingET o were introduced in FAO I&D No. 56 (Allen et al., 1998), according <strong>to</strong> the FAO Penman-Monteith equation, which has now become the standard for estimating reference cropevapotranspiration.Actual <strong>Crop</strong> EvAPOTRANSPIRATION (ET a )It is very difficult <strong>to</strong> estimate the actual crop evapotranspiration with precision. FAO I&D No. 33provided tables from which ET a could be estimated from data on evapotranspiration rate,available soil <strong>water</strong> and wetting intervals. The tables however proved cumbersome and laterwere replaced by more accurate ET a calculations based on daily <strong>water</strong> balance calculations anddigital computation methods.Water balance calculations allow the level of available soil <strong>water</strong> in the root zone <strong>to</strong> bedetermined on a daily basis. As long as soil <strong>water</strong> is readily available for the crop, then ET a =ET x . When a critical soil moisture level is reached, defined as a fraction of the <strong>to</strong>tal availablesoil <strong>water</strong> content (p), transpiration is reduced because the s<strong>to</strong>mata close and thus ET a < ET x ,until the level of soil <strong>water</strong> in the root zone reaches the permanent wilting point, when ET ais assumed <strong>to</strong> be zero. This critical soil-<strong>water</strong> content is estimated from soil, crop and rootingcharacteristics and from the ET o rate. Depletion of soil-<strong>water</strong> content between p and thepermanent wilting point will result in a proportional reduction of ET a .Yield Response <strong>to</strong> Water of All <strong>Crop</strong> Types 9

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