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Water management in irrigated rice - Rice Knowledge Bank ...

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Irrigation systems55.1 <strong>Water</strong> flows <strong>in</strong> irrigation systemsIrrigated <strong>rice</strong> fields are characterized by large volumesof outflows by surface dra<strong>in</strong>age, seepage, andpercolation (Chapter 1.3). Although these outflowsare losses from an <strong>in</strong>dividual field, there is greatscope for reuse of these flows with<strong>in</strong> a landscapethat consists of many <strong>in</strong>terconnected fields (Fig.5.1). Surface dra<strong>in</strong>age and seepage water usuallyflow <strong>in</strong>to downstream fields and the loss of onefield is the ga<strong>in</strong> of another. At the bottom of atoposequence, these flows enter dra<strong>in</strong>s or ditches.However, farmers can use small pumps to lift waterfrom dra<strong>in</strong>s to irrigate fields that are <strong>in</strong>adequately,or not, serviced by irrigation canals. In many irrigationsystems <strong>in</strong> low-ly<strong>in</strong>g deltas or flood pla<strong>in</strong>swith impeded dra<strong>in</strong>age, the cont<strong>in</strong>uous percolationof water (from fields, but also from canals) has createdshallow groundwater tables close to the surfacethat may directly provide the <strong>rice</strong> crop with water(Chapter 1.4). Aga<strong>in</strong>, farmers can either directlypump water up from the shallow groundwater orpump groundwater when it becomes surface wateras it flows <strong>in</strong>to creeks or dra<strong>in</strong>s.Irrigation channelSDDDDra<strong>in</strong>age channelPPPSPSPSGroundwater<strong>in</strong>flowPumpPumpGroundwateroutflowFig. 5.1. Surface and subsurface water flows across a toposequence of <strong>rice</strong> fields. D = dra<strong>in</strong>age (overbund flow), I = irrigation,P = percolation, S = seepage.39

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