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典型引黄灌区包气带与地下水动态响应试验

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[目的]开展银川平原引黄灌溉引起的包气带和地下水的动态响应试验,研究"灌溉水-包气带水-地下水"的转换过程和规律。[方法]以典型引黄灌区水田为研究对象,运用水文地质学、土壤水动力学等学科理论对原位试验观测资料数值分析,借助Origin、SPSS等统计分析软件进行数据处理,利用Hydrus-1D、Surfer等数值模拟软件进行拟合和插值分析。[结果]结果得出,灌溉过程中包气带各埋深层位的水分和负压变化呈显著相关性,相关系数达0。9以上;运用Hydrus-1D拟合田间土壤水分特征曲线,发现叠加各埋深层位可得到较连续的拟合曲线;在多次灌溉入渗试验中,第 1次灌溉入渗引起的地下水动态响应最快,灌溉后响应时间为388。8 min;运用地下水灌溉响应法定量测算灌溉入渗能力,算得田间灌溉入渗系数均值为0。202;对地下水位动态进行插值分析,发现回灌逐步形成"水丘"中心,地下水流场也随之发生变化;通过地下水补给源项分析,引黄灌区内灌溉水对地下水的年灌溉补给贡献率达79%。[结论]通过原位田间试验,进一步厘清引黄灌区的包气带特性和地下水响应过程,发现引黄灌溉对灌区地下水的补给和流场特征有着决定性的作用,为提高引黄水量利用率和包气带-地下水资源评估、管理及调控提供一定科学支撑。
Dynamic response test of vadose zone and groundwater in typical Yellow River irrigation area
[Objective]The dynamic response test is carried out to study the conversion process and rule of"irrigation water-va-dose zone water-groundwater"caused by irrigation recharge in Yinchuan Plain.[Methods]The paddy field in typical irrigated area of Yellow River diversion is taken as the research object,and the observation data of in-situ test is analyzed by using the the-ories of hydrogeology and soil hydrodynamics.Statistical analysis softwares such as Origin and SPSS is used for data processing,and numerical simulation software such as Hydrus-1D and Surfer is used for fitting and interpolation analysis.[Results]In analy-sis result,there is a certain correlation between water and negative pressure at each buried depth in the process of irrigation,and the correlation coefficient is more than 0.9;The soil-water characteristic curve in the field is fitted with Hydrus-1D,and it is found that continuous fitting curve can be obtained only by superposing each buried deep level;In multiple irrigation infiltration tests,the dynamic response of groundwater caused by the first infiltration is the fastest,the response time is 388.8 min after irri-gation;The groundwater irrigation response method is used to quantitatively measure the field irrigation infiltration capacity,and the average field infiltration coefficient is calculated to be 0.202.By interpolation analysis of groundwater level dynamics,it is found that recharge gradually forms a"water hill"center,and the groundwater flow field changes accordingly.Through the sta-tistical analysis of groundwater recharge sources,the annual contribution rate to groundwater recharge is 79%by irrigation water in the Yellow River irrigation area.[Conclusion]The situ field experiments are carried out to further clarify the characteristics of the vadose zone and the response process of groundwater.The Yellow River irrigation has a decisive role in the groundwater re-charge and flow field characteristics in the irrigation area.It is provided some scientific support for improving the utilization rate of the Yellow River diversion water and the assessment,management and control of vadose zone and groundwater resources.

in-situ soil testirrigation rechargevadose zoneinfiltration ratedynamic response

王成文、方磊、李英、黄小琴、张勃、徐兆祥、马波

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宁夏回族自治区水文环境地质调查院,宁夏银川 750011

中国地质大学(北京)水资源与环境学院,北京 100083

宁夏回族自治区地质局,宁夏银川 750021

原位试验 地下水 包气带 灌溉入渗系数 动态响应

宁夏地下水与生态环境效应研究人才小高地项目宁夏自然科学基金宁夏自然科学基金宁夏自然科学基金宁夏地质局宁夏生态地质调查示范项目

2021AAC034492023AAC037852023AAC02081NXCZ20220201

2024

水利水电技术(中英文)
水利部发展研究中心

水利水电技术(中英文)

CSTPCD北大核心
影响因子:0.456
ISSN:1000-0860
年,卷(期):2024.55(7)