Conversion relationship between surface water and groundwater based on stable isotopes of D and <sup>18</sup>O of new town in the northern Wuhan, Hubei

YANG Yanlin; JING Jing; ZHAO Yongbo; HE Jun; DU Xiaofeng

doi:10.12029/gc20220303

GEOLOGY IN CHINA > 2022 > 49(3): 706-715. > DOI: 10.12029/gc20220303

YANG Yanlin, JING Jing, ZHAO Yongbo, HE Jun, DU Xiaofeng. Conversion relationship between surface water and groundwater based on stable isotopes of D and ¹⁸O of new town in the northern Wuhan, Hubei[J]. GEOLOGY IN CHINA, 2022, 49(3): 706-715. DOI: 10.12029/gc20220303

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Conversion relationship between surface water and groundwater based on stable isotopes of D and ¹⁸O of new town in the northern Wuhan, Hubei

1.
Wuhan Center, China Geological Survey, Wuhan 430205, Hubei, China
2.
School of City and Environmental, Hubei Normal University, Huangshi 435002, Hubei, China
3.
Institute of Hubei Geological Survey, Wuhan 430034, Hubei, China

Funds:

the project of China Geological Survey DD20190282

the project of China Geological Survey DD20221743

More Information

Author Bio:
YANG Yanlin, male, born in 1984, senior engineer, engaged in hydro-environmental geological survey; E-mail: yangyanlinjida@gmail.com
Corresponding author:
HE Jun, male, born in 1984, senior engineer, engaged in hydro-environmental geological survey; E-mail: 176041779@qq.com
Received Date: January 17, 2021
Revised Date: May 08, 2022
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

This paper is the result of hydrogeological survey engineering.
Object
Reveal the characteristics and interaction of D and ¹⁸O between surface water and groundwater in the northern new town of Wuhan,
Methods
7 precipitation samples, 6 river samples, 14 reservoir samples, 98 minjing samples, 3 spring samples and 11 borehole samples were collected and measured in 2019, what' s more, 50 monitoring data of Wuhan station from 1986 to 1998 were collected. The research methods of D and ¹⁸O spatial analysis and watershed analysis are carried out in this paper.
Results
(1) The D and ¹⁸O isotopes of precipitation in Wuhan vary with seasons, and the negative correlation between isotopic value and precipitation indicates "rainfall effect", but the no correlation between isotopic value and temperature indicates "no temperature effect". (2) Due to strong evapotransporation, the surface water shows the certain correlation between isotopic value and geomorphic types, and the main stream is enriched in stable isotopic, while the tributaries is depleted; (3) Groundwater such as wells, springs and boreholes are all derived from atmospheric precipitation, and the stable isotopes value of groundwater is related to the buried depth and geomorphic type; (4) During the dry season, the Jiehe River is recharged by upstream reservoir and underground water in the Jiehe basin, and the XiaJiasi reservoir is recharged by underground water in the XiaJiasi reservoir basin.
Conclusion
D and ¹⁸O can significantly improve the understanding of the conversion relationship between surface water and groundwater in the northern new town of Wuhan.
- groundwater,
- river,
- reservoir,
- stable isotopes D and ¹⁸O,
- hydrogeological survey engineering,
- New Town,
- Wuhan,
- Hubei Province

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References (31)

References

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Conversion relationship between surface water and groundwater based on stable isotopes of D and 18O of new town in the northern Wuhan, Hubei

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Conversion relationship between surface water and groundwater based on stable isotopes of D and ¹⁸O of new town in the northern Wuhan, Hubei