河套灌区典型区土壤水-地下水动态与转化关系研究
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国家自然科学基金项目(51769024、51879132)和人才引进优秀博士科研项目(NDYB2017-34)


Dynamic and Transformation Relationship between Soil Water and Groundwater in Typical Areas of Hetao Irrigation District
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    摘要:

    为确定限制引水背景下河套灌区土壤水-地下水动态及其转化关系,为优化农田水管理策略提供理论依据,选取河套灌区典型斗渠区域,基于2年土壤水、地下水的监测数据,分析在不同作物种植区、不同灌溉期的农田土壤水、地下水的动态变化规律。运用水量平衡法对地下水浅埋区农田土壤水与地下水的转化关系进行定量研究,结果表明:生育期内农田土壤水分变化属于“灌溉降水入渗补充-腾发消耗型”;受灌溉影响,不同时期地下水埋深动态具有显著的灌溉型特征,土壤水渗漏补给地下水明显抬升地下水位,地下水排水和潜水蒸发又降低地下水位;在作物生育期内,土壤水与地下水进行双向补给,且不同时期具有不同的转化特征;研究区2年生育期内灌溉降水补给土壤水分别为544.56mm和541.85mm,平均腾发量为465.5mm和434.8mm,土壤储水量减少61.96mm和63.1mm,土壤水补给地下水为207.73mm和236.94mm。研究可为当地及相近地区农业节水灌溉提供科学依据。

    Abstract:

    Aiming to determine the soil water-groundwater dynamics and their transformation relationship in the Hetao Irrigation District under the background of restricted water diversion, so as to provide a theoretical basis for optimizing farmland water management strategies, a typical bucket canal area in Hetao Irrigation District was selected, and the dynamic changes of farmland soil water in different crop planting areas and groundwater in different irrigation periods were analyzed based on the monitoring data of soil water and groundwater in two years. Using soil water balance to quantitatively study the transformation relationship between farmland soil water and groundwater in shallow groundwater areas, the results showed that the change of farmland soil moisture during the growth period belonged to the “irrigation precipitation infiltration supplement-evapotranspiration type”; it was different due to irrigation. The dynamics of groundwater depth during the period had significant characteristics, and the groundwater depth fluctuated drastically with the leakage of soil moisture in the farmland; during the growth period of crops, soil water and groundwater were recharged in both directions, and different periods had different transformation characteristics; the internal irrigation and precipitation replenish soil water were 544.56mm and 541.85mm in 2a growth periods, respectively. The average evapotranspiration in the study area was 465.5mm and 434.8mm, respectively, the soil water storage was reduced by 61.96mm and 63.1mm, respectively, and the soil water replenishing groundwater was 207.73mm and 236.94mm, respectively. The research results can provide a scientific basis for agricultural water-saving irrigation in the local and similar areas.

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张文聪,史海滨,李仙岳,李祯,周慧,王维刚.河套灌区典型区土壤水-地下水动态与转化关系研究[J].农业机械学报,2022,53(10):352-362. ZHANG Wencong, SHI Haibin, LI Xianyue, LI Zhen, ZHOU Hui, WANG Weigang. Dynamic and Transformation Relationship between Soil Water and Groundwater in Typical Areas of Hetao Irrigation District[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(10):352-362.

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  • 收稿日期:2021-11-16
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  • 在线发布日期: 2021-12-10
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