汉江下游河水-地下水侧向交互带中溶解态锰的分布特征

马奥兰; 刘慧; 毛胜军; 朱子超; 李民敬

doi:10.3799/dqkx.2021.038

Volume 47 Issue 2

Feb. 2022

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Ma Aolan, Liu Hui, Mao Shengjun, Zhu Zichao, Li Minjing, 2022. Distribution Characteristics of Dissolved Manganese in the Lateral Hyporheic Zone between River and Groundwater in the Lower Reaches of the Han River. Earth Science, 47(2): 729-741. doi: 10.3799/dqkx.2021.038

Citation:

Ma Aolan, Liu Hui, Mao Shengjun, Zhu Zichao, Li Minjing, 2022. Distribution Characteristics of Dissolved Manganese in the Lateral Hyporheic Zone between River and Groundwater in the Lower Reaches of the Han River. Earth Science, 47(2): 729-741. doi: 10.3799/dqkx.2021.038

Citation:

Ma Aolan, Liu Hui, Mao Shengjun, Zhu Zichao, Li Minjing, 2022. Distribution Characteristics of Dissolved Manganese in the Lateral Hyporheic Zone between River and Groundwater in the Lower Reaches of the Han River. Earth Science, 47(2): 729-741. doi: 10.3799/dqkx.2021.038

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Distribution Characteristics of Dissolved Manganese in the Lateral Hyporheic Zone between River and Groundwater in the Lower Reaches of the Han River

doi: 10.3799/dqkx.2021.038

Ma Aolan^{1
,
,},
Liu Hui^{1, 2
,
,
,},
Mao Shengjun¹,
Zhu Zichao¹,
Li Minjing¹

1.
School of Environment Studies, China University of Geosciences, Wuhan 430078, China
2.
State Key Laboratory of Biogeology and Environmental Geology, Wuhan 430078, China

Received Date: 2021-09-13
Publish Date: 2022-02-25

Abstract

Abstract

The content of manganese in shallow groundwater in Jianghan Plain is generally high. Studying the distribution characteristics of manganese in the hyporheic zone helps to understand manganese's biogeochemical process in the hyporheic zone. It is of great significance for guiding the protection of river and groundwater quality. This study takes the lateral hyporheic zone in the Han River's lower reaches as the research object. The temporal and spatial distribution of dissolved manganese under different interaction directions between river and groundwater in the lateral hyporheic zone is studied and discussed by detecting manganese concentration and its related parameters in the river and groundwater. The results showed that the dissolved manganese is enriched in the river-groundwater lateral interaction zone near the riparian zone, and the manganese content is higher in the place where there is local reverse flow; The phenomenon of local enrichment is more obvious in the interactive zone where river water supplies groundwater. After flooding for 1-3 months, the enrichment area migrates with the direction of water flow; The dissolved manganese concentration in the groundwater of the study area has a very significant positive correlation with HCO₃^-, Mg²⁺, Ca²⁺, and has a remarkably substantial negative correlation with NO₃^-. It is also negatively correlated with Fe²⁺. However, it is not related to the Eh and pH of groundwater in the hyporheic zone.In a word, the spatial and temporal distribution of dissolved manganese in the hyporheic zone is influenced by topographic conditions, hydrodynamics and hydrochemistry.
- hyporheic zone,
- dissolved manganese,
- spatial and temporal distribution,
- the han river,
- water chemistry,
- hydrogeology

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Distribution Characteristics of Dissolved Manganese in the Lateral Hyporheic Zone between River and Groundwater in the Lower Reaches of the Han River

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