首页> 外文期刊>International Journal of Agricultural and Biological Engineering >Transformation of surface water and groundwater and water balance in the agricultural irrigation area of the Manas River Basin, China
【24h】

Transformation of surface water and groundwater and water balance in the agricultural irrigation area of the Manas River Basin, China

机译:玛纳斯河流域农业灌溉区地表水与地下水的转化及水平衡

获取原文
           

摘要

Calculation of the water balance is very important to relieve the pressure on water resources in arid agricultural irrigation areas. This research focused on irrigation water balance calculations in the Manas River Basin of the southern margin of the Junggar Basin of China, and aimed to analyze the groundwater level dynamic trend and response characteristics of the basin water cycle under water-saving irrigation measures. The surface water and groundwater coupling model of MIKE 11-Visual MODFLOW was used to simulate rainfall runoff in mountainous areas, and quantify the contribution of water balance components in the plain irrigation area. Convergence of the delayed watershed in the mountain area was obvious, and when the river runoff exceeded 200 m3/s, the error in the runoff simulation was large. The water balance in the plain agricultural irrigation area was in a negative equilibrium state, and the difference between recharge and discharge was ?2.65 billion m3. The evapotranspiration was 24.49 billion m3 under drip irrigation, accounting for only approximately 51% of the total discharge. The lateral discharge of the unsaturated and saturated aquifers was 15.38 billion m3, accounting for approximately 32% of the total discharge. The main reason for the groundwater decline in the irrigation area was closely related to the extraction of groundwater, because the amount of recharge and discharge in the natural state was approximately identical. The MIKE 11-Visual MODFLOW model produced accurate results, and the research method provided a new exploration technique to quantify the effect of water supply mode on the groundwater table. The model is suitable for the management of water resources in arid areas. Keywords: water balance, coupling model, surface water and groundwater, water saving irrigation, Manas River Basin DOI: 10.25165/j.ijabe.20171004.3461 Citation: Yang G, He X L, Li X L, Long A H, Xue L Q. Transformation of surface water and groundwater and water balance in the agricultural irrigation area of the Manas River Basin, China. Int J Agric & Biol Eng, 2017; 10(4): 107–118.
机译:水平衡的计算对于减轻干旱农业灌溉地区的水资源压力非常重要。本研究重点研究了准southern尔盆地南缘玛纳斯河流域的灌溉水平衡计算,旨在分析节水灌溉措施下地下水位的动态趋势和流域水循环的响应特征。利用MIKE 11-Visual MODFLOW的地表水与地下水的耦合模型模拟了山区的降雨径流,并量化了平原灌溉区水平衡成分的贡献。山区延迟流域的收敛性明显,当河流径流量超过200 m3 / s时,径流模拟误差较大。平原农业灌溉区的水平衡处于负平衡状态,补给和排放之间的差额为26.5亿立方米。滴灌条件下的蒸散量为244.9亿立方米,仅占总排放量的51%。非饱和含水层和饱和含水层的侧向排放量为153.8亿立方米,约占总排放量的32%。灌溉区地下水减少的主要原因与地下水的抽取密切相关,因为自然状态下的补给量和排放量大致相同。 MIKE 11-Visual MODFLOW模型产生了准确的结果,该研究方法为量化供水方式对地下水位的影响提供了一种新的勘探技术。该模型适用于干旱地区的水资源管理。关键词:水平衡,耦合模型,地表水与地下水,节水灌溉,玛纳斯河流域DOI:10.25165 / j.ijabe.20171004.3461引用:杨广,何XL,李XL,Long AH,薛LQ。玛纳斯河流域农业灌溉区的地下水,地下水和水平衡。国际农业与生物工程杂志,2017; 10(4):107-118。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号