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How much water does rice need? - adron.sr

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<strong>How</strong> <strong>much</strong> <strong>water</strong><strong>does</strong> <strong>rice</strong> use?by Bas BoumanRice Today examines this often-asked(and often poorly answered) questionJose Raymond PanaliganMany people ask thequestion, “<strong>How</strong> <strong>much</strong><strong>water</strong> <strong>does</strong> it take toproduce 1 kg of <strong>rice</strong>?”The answer to this question lies inthe definition of “<strong>water</strong> use” and of“<strong>rice</strong>.” We can identify three types of<strong>water</strong> “use”—through transpiration,evaporation, and a combinationof seepage and percolation—at,respectively, three scales of <strong>rice</strong>—theplant, the crop, and the field.The <strong>rice</strong> plant “uses” <strong>water</strong>through the process of transpiration,which cools the plant and drivesthe upward sap flow—which carriesessentialnutrients—fromroots to leaves.This is a “real”<strong>water</strong> use, sinceonce the plant hastaken up <strong>water</strong>and released it tothe atmospherethroughtranspiration,that amountof <strong>water</strong> is nolonger availablefor reuse by thatsame plant inthe same growthcycle. Transpired<strong>water</strong> enters theSOglobal <strong>water</strong> cycle and will eventuallyreturn to the earth as rain or snow.The <strong>rice</strong> crop comprisesthe plants and underlying soil.Besides transpiration from theplants, <strong>water</strong> leaves the cropfrom the soil underneath throughevaporation. Like transpiration,evaporated <strong>water</strong> is “lost” andcannot be used again by that samecrop in the same growth cycle. Thiscombined <strong>water</strong> use by a <strong>rice</strong> cropis called “evapotranspiration.”In <strong>rice</strong> fields, <strong>water</strong> is oftenponded to ensure there is plentyfor the crop to take up. BesidesPlow layerI R TPuddledsoilSubsurface soilevapotranspiration, outflows of<strong>water</strong> from a field occur throughseepage and percolation: sidewardand downward <strong>water</strong> flows throughthe soil and bunds out of the field.For an individual farmer, these arereal losses as well, and she considersthe total combined outflows byevapotranspiration, seepage, andpercolation as <strong>water</strong> use by her <strong>rice</strong>field (see figure). The farmer <strong>need</strong>sto ensure sufficient irrigation (tocomplement rain<strong>water</strong> if rainfallis insufficient) to match all theseoutflows. At a larger spatial scale,however, seepage and percolationFlood<strong>water</strong>CPEBundSOGround<strong>water</strong>Water balance of a puddled <strong>rice</strong> field: C = capillary rise; E = evaporation; I = irrigation; O = over-bund flow; P = percolation; R = rainfall;S = seepage; T = transpiration.28 Rice Today January-March 2009

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