首页> 外文期刊>Irrigation and Drainage >SIMULATING GROUNDWATER DYNAMICS USING FEFLOW-3D GROUNDWATER MODEL UNDER COMPLEX IRRIGATION AND DRAINAGE NETWORK OF DRYLAND ECOSYSTEMS OF CENTRAL ASIA
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SIMULATING GROUNDWATER DYNAMICS USING FEFLOW-3D GROUNDWATER MODEL UNDER COMPLEX IRRIGATION AND DRAINAGE NETWORK OF DRYLAND ECOSYSTEMS OF CENTRAL ASIA

机译:中亚旱地生态系统复杂灌溉排水网络下的FLOWLOW-3D地下水模型模拟地下水动态。

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Surface and groundwater resources are often conjunctively used to cope with water scarcity in irrigated agriculture. Farmers in the dryland ecosystems of central Asia also utilize shallow groundwater in addition to surface water withdrawn from rivers. This study modelled groundwater dynamics in an irrigation and drainage network in Khorezm region, Uzbekistan. The system, characterized by a vast, unlined channel network used to convey water mainly for flood irrigation and an open drainage system, is typical of Central Asian irrigated areas. Groundwater levels in the region are shallowthis contributes to crop water requirements but threatens crop production through secondary salinization. High losses during irrigation in fields and through the irrigation network are the main causes of these shallow groundwater levels. The main objective of this study was thus to simulate groundwater levels under improved irrigation efficiency scenarios. The FEFLOW-3D model, applied in a case study to the water users' association (WUA) of Shomakhulum in south-west Khorezm, was used to quantify the impact of improved irrigation efficiency scenarios on groundwater dynamics. The modelled scenarios were: current irrigation efficiency (S-A, our baseline), improved conveyance efficiency (S-B), increased field application efficiency (S-C), and improved conveyance and application efficiency (S-D). Recharge rates were separately determined for six hydrological response units (differing in groundwater level and soil type) and introduced into the FEFLOW-3D model. After successful model calibration (R-2=0.94) and validation (R-2=0.93), the simulations showed that improving irrigation efficiency under existing agro-hydroclimatic conditions would lower groundwater levels from the baseline scenario (S-A) in August (the peak irrigation period) on average by 12cm in S-B, 38cm in S-C and 44cm in S-D. Any interventions which would improve irrigation efficiency will lower the groundwater levels and hence policy makers should consider them and formulate the policy accordingly. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:在灌溉农业中,地表和地下水资源常常被用来应对水资源短缺问题。中亚干旱地区生态系统中的农民除了利用从河流中抽取的地表水以外,还利用浅层地下水。这项研究对乌兹别克斯坦Khorezm地区的灌溉和排水网络中的地下水动力学进行了建模。该系统的特点是广阔的,无衬里的河道网络,主要用于洪水灌溉和开放式排水系统,是中亚灌溉地区的典型代表。该地区的地下水位很浅,这有助于增加作物的需水量,但会通过二次盐碱化威胁作物的生产。田间灌溉过程中以及通过灌溉网络造成的大量损失是造成这些浅层地下水位的主要原因。因此,本研究的主要目的是在提高灌溉效率的情况下模拟地下水位。 FEFLOW-3D模型应用于案例研究中,该模型应用于Khorezm西南部Shomakhulum的用水户协会(WUA),用于量化改善的灌溉效率情景对地下水动力学的影响。建模的方案是:当前的灌溉效率(S-A,我们的基准),提高的输送效率(S-B),提高的田间施用效率(S-C)以及改进的输送和施用效率(S-D)。分别确定了六个水文响应单位(地下水位和土壤类型的不同)的补给率,并将其引入FEFLOW-3D模型。在成功进行模型校准(R-2 = 0.94)和验证(R-2 = 0.93)之后,模拟表明,在现有农业-水文气候条件下提高灌溉效率将降低8月基线情景(SA)的地下水位。灌溉期),SB平均增加12cm,SC增加38cm,SD增加44cm。任何可以提高灌溉效率的干预措施都会降低地下水位,因此政策制定者应予以考虑并制定相应的政策。版权所有(c)2015 John Wiley&Sons,Ltd.

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