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Effect of Conjunctive Use of Water for Paddy Field Irrigation onGroundwater Budget in an Alluvial Fan

机译:稻田联合灌溉用水对冲积扇地下水平衡的影响

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Conjunctive use of surface water and groundwater for irrigation plays an important role inthe hydrology of alluvial fans, both as a source of recharge to the groundwater and as a cause ofdischarge by pumping. Therefore, reliable estimates of distributed groundwater recharge anddischarge are critical in analyzing groundwater budgets in alluvial fans. Nasunogahara basin, TochigiPrefecture, Japan, is an alluvial fan with abundant shallow groundwater, which is extracted and used forirrigation. In this study an integrated surface water- groundwater model, which combined a modifiedtank model with a finite difference model, was used to evaluate quantitatively groundwater recharge anddischarge capacities of each recharge source and discharge route and to assess the effect of conjunctiveuse of surface water and groundwater for paddy field irrigation on the water balance of the shallow aquiferof Nasunogahara. The tank model calculated recharge by different recharge sources to the shallowaquifer and also calculated the amount of groundwater pumped for irrigation. Distributed groundwaterrecharge and discharge were estimated at each node in the groundwater flow model based on thepaddy field area around the node. Results of the model indicate that the calculated water tableelevations were able to describe the actual behavior of the shallow aquifer adequately. From the modelsimulation runs, it was found that although paddy fields are big users of groundwater by pumping, theirrigation water applied is used in a cyclic manner to recharge the shallow aquifer. The percentage of therecharge from paddy fields to the total net recharge is 21 %, which is mainly provided from paddy fieldsirrigated by canal water. These facts indicate the importance of the conjunctive use of surface water andgroundwater for irrigation in maintaining the hydrologic system of the basin.
机译:地表水和地下水的联合使用在灌溉中起着重要作用。 冲积扇的水文状况,既是补给地下水的资源,又是造成地下水流的原因 抽水排放。因此,可靠的估计分布的地下水补给和 排放对于分析冲积扇中的地下水预算至关重要。 To木县Nasunogahara盆地 日本的县府是一种冲积扇,其地下水很浅,被提取并用于 灌溉。在这项研究中,综合了地表水-地下水模型 带有有限差分模型的水箱模型用于定量评估地下水补给量和 每个充电源和放电路径的放电容量,并评估合取的效果 利用地表水和地下水在浅层含水层水平衡上进行稻田灌溉 Nasunogahara的储罐模型通过不同的补给源来计算浅层补给 含水层,还计算了用于灌溉的地下水量。分布的地下水 地下水流模型中每个节点的补给量和排放量基于 节点周围的稻田面积。模型的结果表明计算出的地下水位 高程能够充分描述浅层含水层的实际行为。从模型 模拟运行发现,尽管稻田是抽水对地下水的大用户,但是 循环使用灌溉水来补充浅层含水层。的百分比 稻田补给量占总净补给量的21%,主要由稻田提供 用运河水灌溉。这些事实表明,联合使用地表水和水的重要性。 地下水用于维持流域水文系统。

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