河水-地下水侧向交互带微生物群落分布特征及其主控因子

朱子超; 刘慧; 毛胜军; 马奥兰; 李民敬

doi:10.3799/dqkx.2021.217

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3832-3843

Zhu Zichao, Liu Hui, Mao Shengjun, Ma Aolan, Li Minjing, 2023. Distribution Characteristics of Microbial Communities in River-Groundwater Interaction Zone and Main Environmental Factors. Earth Science, 48(10): 3832-3843. doi: 10.3799/dqkx.2021.217

Citation:

Zhu Zichao, Liu Hui, Mao Shengjun, Ma Aolan, Li Minjing, 2023. Distribution Characteristics of Microbial Communities in River-Groundwater Interaction Zone and Main Environmental Factors. Earth Science, 48(10): 3832-3843. doi: 10.3799/dqkx.2021.217

Citation:

Zhu Zichao, Liu Hui, Mao Shengjun, Ma Aolan, Li Minjing, 2023. Distribution Characteristics of Microbial Communities in River-Groundwater Interaction Zone and Main Environmental Factors. Earth Science, 48(10): 3832-3843. doi: 10.3799/dqkx.2021.217

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Distribution Characteristics of Microbial Communities in River-Groundwater Interaction Zone and Main Environmental Factors

doi: 10.3799/dqkx.2021.217

Zhu Zichao^{1
,
,},
Liu Hui^{1, 2
,
,},
Mao Shengjun¹,
Ma Aolan¹,
Li Minjing¹

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

Received Date: 2021-08-24
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

The unique hydrogeochemical process of the river-groundwater interaction zone can seriously affect microbial community distribution. Studying the microbial distribution characteristic can provide a new understanding of a series of biogeochemical cycles. In this paper, the microbial community diversity, species composition and relationship with environmental factors in the two-dimensional sediment profiles of the interactive zone are analyzed by high-throughput sequencing of 16SrRNA gene. The results show that the microbial community distribution is more heterogeneous in the profile where river water recharge is the main water flow direction. Microbial diversity in the hyporheic zone has a remarkably substantial negative correlation with NH₄⁺, As, and has a negatively correlation with TOC, Mn. Below the water level near the river distributed an area with high microbial diversity where the oxidative NO₃^-, Fe(III), and SO₄^2- were accumulated, the abundance of a large number of chemoheterotrophic microbes decreased, and that of microorganisms related to phosphorus-accumulating, ammonia oxidation and methyl-phage increased. The marginal areas of the interaction zone show less biodiversity, with relatively high TOCs, NH₄⁺, Mn and As. In conclusion, the interaction of river and groundwater determines the distribution of DO and TOC in the interaction zone sediments, thus regulating the changes of the microbial community and the biochemical processes of various elements.
- river-groundwater interaction zone,
- high-throughput sequencing of 16SrRNA gene,
- microbial community,
- environmental factor,
- redundancy analysis,
- biogeochemistry,
- environmental geology

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