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Variability Characteristics of Groundwater Chemical Under Condition of Yellow River Diversion and Recharge
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Cheng-wen WANG1, Lei FANG1, Li-hu YANG2, Ying LI3, 4, Bo MA1, Zhao-xiang XU1, Hong-bo LI1
Water Resources and Power | 2023, 41(11) : 43 - 47
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Water Resources and Power | 2023, 41(11): 43-47
HYDROLOGY, WATER RESOURCES AND ENVIRONMENT
Variability Characteristics of Groundwater Chemical Under Condition of Yellow River Diversion and Recharge
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Cheng-wen WANG1, Lei FANG1, Li-hu YANG2, Ying LI3, 4, Bo MA1, Zhao-xiang XU1, Hong-bo LI1
Affiliations
  • 1.Institute of Hydrogeology and Environmental Geology of Ningxia Hui Autonomous Region, Yinchuan 750011, China
  • 2.Key Laboratory of Land Water Cycle and Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
  • 3.School of Water Resources & Environment, China University of Geosciences, Beijing 100083, China
  • 4.Geological Bureau of Ningxia Hui Autonomous Region, Yinchuan 750021, China
Published: 2023-11-25 doi: 10.20040/j.cnki.1000-7709.2023.20231043
Outline
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The study of groundwater chemical varieties has a positive indicator effect on the regulation and improvement of regional groundwater quality caused by infiltration in the Yellow River Irrigation Area. The field in-situ infiltration test was carried out to monitor and analyze the recharge water-groundwater during the recharge process of paddy field and dry field, and the groundwater chemical evolution law was revealed by AquaChem hydrochemical analysis and SPSS mathematical statistics. Under the condition of infiltration, the characteristics of groundwater chemical change show four evolution processes: "rapid change and active zone in the early stage, gradual transition zone in the middle stage, gentle and stable zone in the late stage, and potential recovery zone after stopping irrigation". It can be seen from the experiment that the groundwater is mainly affected by the physical mixing of recharge water, accompanied by the water-rock physical adsorption ion exchange, chemical dissolution and leaching, etc. especially, the amount of recharge water in paddy field was large, and the water quality of recharge determined the direction of groundwater chemical evolution. At the same time, the concentrations of Na+、Cl- of groundwater chemical components showed a good linear change, and the correlation coefficient was above 0.93, and the concentrations of Ca2+、Mg2+ showed a certain linear correlation with SO42-、HCO3-. After stopping irrigation, the evaporation and concentration of groundwater was strong, and the ions of groundwater showed an increasing trend. Especially for Na+、Cl-, the drainage and precipitation are timely needed after the irrigation. The research shows that the water supply of groundwater not only enriched groundwater sources, but also improved groundwater quality.

Yellow River Diversion Irrigation Area  /  in situ test  /  hydrochemical characteristics  /  water-rock interaction  /  correlation
Cheng-wen WANG, Lei FANG, Li-hu YANG, Ying LI, Bo MA, Zhao-xiang XU, Hong-bo LI. Variability Characteristics of Groundwater Chemical Under Condition of Yellow River Diversion and Recharge[J]. Water Resources and Power, 2023 , 41 (11) : 43 -47 . DOI: 10.20040/j.cnki.1000-7709.2023.20231043
Year 2023 volume 41 Issue 11
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Article Info
doi: 10.20040/j.cnki.1000-7709.2023.20231043
  • Receive Date:2023-06-26
  • Online Date:2026-01-27
  • Published:2023-11-25
Article Data
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History
  • Received:2023-06-26
  • Revised:2023-08-02
Funding
Affiliations
    1.Institute of Hydrogeology and Environmental Geology of Ningxia Hui Autonomous Region, Yinchuan 750011, China
    2.Key Laboratory of Land Water Cycle and Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    3.School of Water Resources & Environment, China University of Geosciences, Beijing 100083, China
    4.Geological Bureau of Ningxia Hui Autonomous Region, Yinchuan 750021, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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