Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China

Li Jinzhen; Sun Tianhe; Jiang Zhenguo; Wang Jilin; Jin Lijie; Yu Chunnan

doi:doi:10.11648/j.sd.20221004.13

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Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China

Li Jinzhen, Sun Tianhe, Jiang Zhenguo, Wang Jilin, Jin Lijie, Yu Chunnan

Published in Science Discovery (Volume 10, Issue 4)

Received: 15 July 2022 Accepted: 6 August 2022 Published: 9 August 2022

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Abstract

Hongfanchi spring area is one of the most important areas of Jinan spring group, and the hydrochemical characteristics and material source mechanism are of great significance for the reasonable development and protection of the spring area. In this study, the water sampling sites were arranged in the typical spring water and the confluent surface water, and the contents of major ion geochemistry were analyzed. The research methods of such as: statistical analysis, Piper diagram, correlation analysis, cluster analysis, Gibbs diagram and mass conservation calculation were used to study the hydrochemical characteristics, and the source mechanism of major ion geochemistry in Hongfanchi spring area has been proposed for the first time. The results show that: the water in the Hongfanchi spring area were mainly with the hydrochemical type of HCO₃·SO₄-Ca; and the contents of K⁺, Na⁺, Mg²⁺, Cl^-, F^- in the spring water were much lower than that in the surface water, while the contents of Ca²⁺, SO₄^2-, HCO₃^-, NO₃^- and TDS were obviously higher. The spring water was mainly affected by the carbonate weathering (62.91% - 73.10%) and the anthropogenic inputs (12.79% - 23.97%); while the surface water was affected by the carbonate weathering (36.03% - 60.91%), the evaporite dissolution (15.74% - 22.00%), the silicate weathering (11.28% - 16.81%) and the anthropogenic inputs (10.12% - 15.70%). The proportion of atmospheric inputs in both were very small.

Published in	Science Discovery (Volume 10, Issue 4)
DOI	10.11648/j.sd.20221004.13
Page(s)	217-223
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Hongfanchi, Spring, Hydro-Geochemical Characteristics, Ion, Source Mechanism

References

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APA Style

Li Jinzhen, Sun Tianhe, Jiang Zhenguo, Wang Jilin, Jin Lijie, et al. (2022). Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Science Discovery, 10(4), 217-223. https://doi.org/10.11648/j.sd.20221004.13

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ACS Style

Li Jinzhen; Sun Tianhe; Jiang Zhenguo; Wang Jilin; Jin Lijie, et al. Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Sci. Discov. 2022, 10(4), 217-223. doi: 10.11648/j.sd.20221004.13

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AMA Style

Li Jinzhen, Sun Tianhe, Jiang Zhenguo, Wang Jilin, Jin Lijie, et al. Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Sci Discov. 2022;10(4):217-223. doi: 10.11648/j.sd.20221004.13

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@article{10.11648/j.sd.20221004.13,
  author = {Li Jinzhen and Sun Tianhe and Jiang Zhenguo and Wang Jilin and Jin Lijie and Yu Chunnan},
  title = {Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China},
  journal = {Science Discovery},
  volume = {10},
  number = {4},
  pages = {217-223},
  doi = {10.11648/j.sd.20221004.13},
  url = {https://doi.org/10.11648/j.sd.20221004.13},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sd.20221004.13},
  abstract = {Hongfanchi spring area is one of the most important areas of Jinan spring group, and the hydrochemical characteristics and material source mechanism are of great significance for the reasonable development and protection of the spring area. In this study, the water sampling sites were arranged in the typical spring water and the confluent surface water, and the contents of major ion geochemistry were analyzed. The research methods of such as: statistical analysis, Piper diagram, correlation analysis, cluster analysis, Gibbs diagram and mass conservation calculation were used to study the hydrochemical characteristics, and the source mechanism of major ion geochemistry in Hongfanchi spring area has been proposed for the first time. The results show that: the water in the Hongfanchi spring area were mainly with the hydrochemical type of HCO3·SO4-Ca; and the contents of K+, Na+, Mg2+, Cl-, F- in the spring water were much lower than that in the surface water, while the contents of Ca2+, SO42-, HCO3-, NO3- and TDS were obviously higher. The spring water was mainly affected by the carbonate weathering (62.91% - 73.10%) and the anthropogenic inputs (12.79% - 23.97%); while the surface water was affected by the carbonate weathering (36.03% - 60.91%), the evaporite dissolution (15.74% - 22.00%), the silicate weathering (11.28% - 16.81%) and the anthropogenic inputs (10.12% - 15.70%). The proportion of atmospheric inputs in both were very small.},
 year = {2022}
}

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TY  - JOUR
T1  - Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China
AU  - Li Jinzhen
AU  - Sun Tianhe
AU  - Jiang Zhenguo
AU  - Wang Jilin
AU  - Jin Lijie
AU  - Yu Chunnan
Y1  - 2022/08/09
PY  - 2022
N1  - https://doi.org/10.11648/j.sd.20221004.13
DO  - 10.11648/j.sd.20221004.13
T2  - Science Discovery
JF  - Science Discovery
JO  - Science Discovery
SP  - 217
EP  - 223
PB  - Science Publishing Group
SN  - 2331-0650
UR  - https://doi.org/10.11648/j.sd.20221004.13
AB  - Hongfanchi spring area is one of the most important areas of Jinan spring group, and the hydrochemical characteristics and material source mechanism are of great significance for the reasonable development and protection of the spring area. In this study, the water sampling sites were arranged in the typical spring water and the confluent surface water, and the contents of major ion geochemistry were analyzed. The research methods of such as: statistical analysis, Piper diagram, correlation analysis, cluster analysis, Gibbs diagram and mass conservation calculation were used to study the hydrochemical characteristics, and the source mechanism of major ion geochemistry in Hongfanchi spring area has been proposed for the first time. The results show that: the water in the Hongfanchi spring area were mainly with the hydrochemical type of HCO3·SO4-Ca; and the contents of K+, Na+, Mg2+, Cl-, F- in the spring water were much lower than that in the surface water, while the contents of Ca2+, SO42-, HCO3-, NO3- and TDS were obviously higher. The spring water was mainly affected by the carbonate weathering (62.91% - 73.10%) and the anthropogenic inputs (12.79% - 23.97%); while the surface water was affected by the carbonate weathering (36.03% - 60.91%), the evaporite dissolution (15.74% - 22.00%), the silicate weathering (11.28% - 16.81%) and the anthropogenic inputs (10.12% - 15.70%). The proportion of atmospheric inputs in both were very small.
VL  - 10
IS  - 4
ER  -

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Author Information

Li Jinzhen

No. 1 Institute of Geology and Mineral Resources of Shandong Province, Jinan, China
Sun Tianhe

No. 1 Institute of Geology and Mineral Resources of Shandong Province, Jinan, China
Jiang Zhenguo

No. 1 Institute of Geology and Mineral Resources of Shandong Province, Jinan, China
Wang Jilin

Shandong Bureau Testing Center of China Metallurgical Geology Bureau, Jinan, China
Jin Lijie

No. 1 Institute of Geology and Mineral Resources of Shandong Province, Jinan, China
Yu Chunnan

No. 1 Institute of Geology and Mineral Resources of Shandong Province, Jinan, China

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APA Style

Li Jinzhen, Sun Tianhe, Jiang Zhenguo, Wang Jilin, Jin Lijie, et al. (2022). Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Science Discovery, 10(4), 217-223. https://doi.org/10.11648/j.sd.20221004.13

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ACS Style

Li Jinzhen; Sun Tianhe; Jiang Zhenguo; Wang Jilin; Jin Lijie, et al. Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Sci. Discov. 2022, 10(4), 217-223. doi: 10.11648/j.sd.20221004.13

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AMA Style

Li Jinzhen, Sun Tianhe, Jiang Zhenguo, Wang Jilin, Jin Lijie, et al. Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China. Sci Discov. 2022;10(4):217-223. doi: 10.11648/j.sd.20221004.13

Copy | Download

@article{10.11648/j.sd.20221004.13,
  author = {Li Jinzhen and Sun Tianhe and Jiang Zhenguo and Wang Jilin and Jin Lijie and Yu Chunnan},
  title = {Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China},
  journal = {Science Discovery},
  volume = {10},
  number = {4},
  pages = {217-223},
  doi = {10.11648/j.sd.20221004.13},
  url = {https://doi.org/10.11648/j.sd.20221004.13},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sd.20221004.13},
  abstract = {Hongfanchi spring area is one of the most important areas of Jinan spring group, and the hydrochemical characteristics and material source mechanism are of great significance for the reasonable development and protection of the spring area. In this study, the water sampling sites were arranged in the typical spring water and the confluent surface water, and the contents of major ion geochemistry were analyzed. The research methods of such as: statistical analysis, Piper diagram, correlation analysis, cluster analysis, Gibbs diagram and mass conservation calculation were used to study the hydrochemical characteristics, and the source mechanism of major ion geochemistry in Hongfanchi spring area has been proposed for the first time. The results show that: the water in the Hongfanchi spring area were mainly with the hydrochemical type of HCO3·SO4-Ca; and the contents of K+, Na+, Mg2+, Cl-, F- in the spring water were much lower than that in the surface water, while the contents of Ca2+, SO42-, HCO3-, NO3- and TDS were obviously higher. The spring water was mainly affected by the carbonate weathering (62.91% - 73.10%) and the anthropogenic inputs (12.79% - 23.97%); while the surface water was affected by the carbonate weathering (36.03% - 60.91%), the evaporite dissolution (15.74% - 22.00%), the silicate weathering (11.28% - 16.81%) and the anthropogenic inputs (10.12% - 15.70%). The proportion of atmospheric inputs in both were very small.},
 year = {2022}
}

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TY  - JOUR
T1  - Major Ion Geochemistry and Source Mechanism of the Hongfanchi Spring Area, Jinan, China
AU  - Li Jinzhen
AU  - Sun Tianhe
AU  - Jiang Zhenguo
AU  - Wang Jilin
AU  - Jin Lijie
AU  - Yu Chunnan
Y1  - 2022/08/09
PY  - 2022
N1  - https://doi.org/10.11648/j.sd.20221004.13
DO  - 10.11648/j.sd.20221004.13
T2  - Science Discovery
JF  - Science Discovery
JO  - Science Discovery
SP  - 217
EP  - 223
PB  - Science Publishing Group
SN  - 2331-0650
UR  - https://doi.org/10.11648/j.sd.20221004.13
AB  - Hongfanchi spring area is one of the most important areas of Jinan spring group, and the hydrochemical characteristics and material source mechanism are of great significance for the reasonable development and protection of the spring area. In this study, the water sampling sites were arranged in the typical spring water and the confluent surface water, and the contents of major ion geochemistry were analyzed. The research methods of such as: statistical analysis, Piper diagram, correlation analysis, cluster analysis, Gibbs diagram and mass conservation calculation were used to study the hydrochemical characteristics, and the source mechanism of major ion geochemistry in Hongfanchi spring area has been proposed for the first time. The results show that: the water in the Hongfanchi spring area were mainly with the hydrochemical type of HCO3·SO4-Ca; and the contents of K+, Na+, Mg2+, Cl-, F- in the spring water were much lower than that in the surface water, while the contents of Ca2+, SO42-, HCO3-, NO3- and TDS were obviously higher. The spring water was mainly affected by the carbonate weathering (62.91% - 73.10%) and the anthropogenic inputs (12.79% - 23.97%); while the surface water was affected by the carbonate weathering (36.03% - 60.91%), the evaporite dissolution (15.74% - 22.00%), the silicate weathering (11.28% - 16.81%) and the anthropogenic inputs (10.12% - 15.70%). The proportion of atmospheric inputs in both were very small.
VL  - 10
IS  - 4
ER  -

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