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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />'~~~~~r <br />UL~;~;l) <br /> <br />Conveyance System - all those structures, facilities and operations needed <br />to convey irrigation waters from water source (well, reservoir, stream, <br />etc.) to field of application. <br /> <br />Cubic foot per second (cfs) - a common measurement of rate of flow in <br />irrigation, equals 448.831 gallons per minute or 28.32 liters per <br />second. <br /> <br />Deficit (Stress) irrigation - optimizing the relationship of water applied <br />with respect to crop yield by scheduling the time and amount of water <br />application in accordance with the minimum water requirements at the <br />several stages of plant growth. Some crops can be stressed during cer- <br />tain stages of growth with minimal effects on yield. Simple reductions <br />in water application rates or frequencies without corresponding con- <br />sideration of plant growth and yield effects do not meet the criteria <br />for planned deficit irrigation. Other definitions of deficit <br />irrigation--e.g. keeping the evapotranspiration requirements of plants <br />(ETp) below the total ET losses from applied waters (ETa < ETp) are also <br />commonly used. <br /> <br />Evaporation (E) - the physical transformation and movement of water from <br />a liquid state to a gaseous (vapor) state in the atmosphere. Evaporation <br />from water surfaces (Ew) and evaporation from wetted soil surfaces (Es) <br />make up the major portions of water losses to evaporation, though evap- <br />oration from plant surfaces (Ep) and from spray droplets in the air also <br />contribute to total E losses. At some stages of plant growth, the evap- <br />oration loss from plant surfaces (Ep) can exceed all other evaporative <br />losses. Temperature (solar radiation), relative humidity and wind <br />velocity all play direct roles in the rate of evaporation. Evaporation, <br />along with plant transpiration, make up the two principal sources of <br />nonrecoverable water losses (see below). <br /> <br />Evapotranspiration (ET) - a combined measure of water evaporated from the <br />soil (Es) and plant surfaces (Ep) plus that water transpired (T) by <br />growing plants. Irrigation water requirements for crops are commonly <br />expressed in units of ET per unit of time (day, month, growing season). <br /> <br />xi <br />