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crop growth and, therefore, yield. This is because the path- <br />way for transpiration water losses in plants is the same one <br />that allows for plant uptake of carbon dioxide, which is the <br />raw material for photosynthesis. Both exchange processes <br />occur through pores called stomates on the leaf surface. <br />When soil water is not limiting, which is usually the case <br />under irrigated conditions, stomates are fully open. When <br />this condition exists, both transpiration and photosynthesis <br />are occurring at maximum rates allowed by current condi- <br />tions both internal and external to the plant. If soil water <br />becomes limiting, stomates begin to close, limiting both <br />transpiration water losses and photosynthesis. <br />A key ingredient of irrigation water management is the <br />ability to estimate the magnitude of ET losses for any given <br />set of conditions. The most important factors that have to <br />be accounted for are: 1.) the local weather conditions; and <br />2.) the cropping system for which estimates are needed <br />(type of crop, planting date, etc.). Local weather conditions <br />are important, because ET is driven by weather factors that <br />determine the drying power of the air. A branch of sci- <br />ence known as agricultural meteorology has provided good <br />insight into the variables that drive evaporation of water <br />from soil and crop surfaces. We can accurately predict <br />ET losses in a given area from measurements of four local <br />weather variables; solar radiation, temperature, humidity, <br />and wind. To be useful, these measurements have to be <br />made under a standardized set of conditions. By conven- <br />tion, the variables are measured using instrumentation of <br />specific design located within large areas devoted to stands <br />of irrigated grass or alfalfa. The data from these measure- <br />ments are then used in specially calibrated equations that <br />accurately predict the daily rate of ET for these standard- <br />ized conditions. The values obtained from this process <br />provide standardized measurements of ET that are referred <br />to as reference ET. The term, reference, refers to stan- <br />dardization of the entire process including type of crop used <br />under the weather- monitoring instrumentation, the weather <br />variables measured, and the calculations performed. When <br />all these factors are accounted for, the ET of the reference <br />crop, which is designated as reference ET, can be estimated <br />with great accuracy. In most cases, reference ET values are <br />generated on a daily basis. The specific calculations used <br />are from a set of calculations known as combination equa- <br />tions. The common name of Penman is often used to refer <br />to these equations. <br />Crop /Soil ET Coefficients -- Reference ET values ap- <br />ply to a specific reference crop grown under a set of local <br />weather conditions. To be useful for other crops within the <br />area in which the reference values were obtained, reference <br />ET values have to be adapted to fit these other crops. This <br />is accomplished by adjusting the reference ET values by <br />use of a crop coefficient. As a general rule, crop coeffi- <br />cients must account for factors such as type of crop, stage <br />of development, and all other aspects of culture that might <br />contribute to variability in the extent and distribution of <br />canopy cover. Variation in available soil water also can be <br />used to adjust crop coefficients for any period of the grow- <br />ing season. Locally adapted crop coefficients are available <br />for most kinds of crops that are likely to be grown in a <br />given area. These coefficients provide daily adjustments <br />to the reference ET values generated each day throughout <br />the growing season. In practice, the coefficient is used as a <br />multiplier, such that the actual daily ET for a given crop on <br />a specific day of the season is the product of the reference <br />ET obtained for that date times the crop coefficient for that <br />same date. The procedures described here are for use under <br />conditions where soil moisture is not limiting. If moisture <br />does become limiting, an additional adjustment factor, <br />called the soil coefficient, can be applied in addition to the <br />crop coefficient. <br />Concentrated Animal Feeding Operations <br />EPA has developed the "Producers Guide" to help concentrated animal <br />feeding operation (CAFO) owners and operators understand how to comply <br />with federal CAFO regulations. The guide is intended for large or medium <br />facilities, or those which have been designated by a state permitting author- <br />ity as a CAFO. The guide provides background and other information on: <br />CAFO regulations; determining what facilities are affected; how to apply for <br />a National Pollution Discharge Elimination System ( NPDES) permit; require- <br />ments that would be contained in a permit; the compliance assurance process; <br />and contact information for each state's NPDES program. The guide will <br />soon be available from EPA regional offices, and is now available online at <br />Western States Water, November 28, 2003 <br />S <br />