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), 2022. Published by Science Publishing Group

Keywords

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

References

[1]	孟庆斌，邢立亭，滕朝霞. 济南泉域“三水”转化与泉水恢复关系探讨[J]. 山东大学学报（工学版）, 2008, 38 (5): 82-87。
[2]	邢立亭，武强，徐军祥，等. 地下水环境容量初探：以济南泉域为例[J]．地质通报, 2009, 28 (1): 124-129。
[3]	XING LT, WU Q, YE C H, et al. Groundwater environmental capacity and its evaluation index [J]. Environmental Monitoring and Assessment. 2010, 169 (1-4): 217-227.
[4]	张建芝，邢立亭. 回归分析法在地下水动态分析中的应用[J]. 地下水, 2010, 32 (4): 88-90。
[5]	祁晓凡，杨丽芝，韩晔，等. 济南泉域地下水位动态及其对降水响应的交叉小波分析[J]. 地球科学进展, 2012, 27 (9): 969-978。
[6]	ZHOU J, XING L T, ZHANG F J, et al. Chemical characteristics research on karst water in Jian spring area [J]. Advanced Materials Research. 2015, 1092-1093: 593-596.
[7]	何奔，贾超，刘新宇，等. 济南市区泉域地下水时空分布规律及污染物运移特性研究[J]. 工程地质学报, 2014, 22 (5): 981-988。
[8]	殷秀兰，王庆兵，凤蔚. 济南岩溶泉域泉群区水化学与环境同位素研究[J]. 地质学报, 2017, 91 (7): 1651-1660。
[9]	孟庆晗，王鑫，邢立亭，等. 济南四大泉群补给来源差异性研究[J]. 水文地质工程地质, 2020, 47 (1): 37-45。
[10]	邢立亭，周娟，宋广增，等. 济南四大泉群泉水补给来源混合比讨论[J]. 地学前缘, 2018, 25 (2): 260-272。
[11]	魏兴，周金龙，乃尉华，等. 新疆喀什三角洲地下水化学特征及演化规律[J]. 环境科学, 2019, 40 (9): 4042-4051。
[12]	沈扬，何江涛，王俊杰，等. 基于多元统计方法的地下水水化学特征分析：以沈阳市李官堡傍河水源地为例[J]. 现代地质, 2013, 27 (2): 440-447。
[13]	林永生，裴建国，杜毓超，等. 基于多元统计方法的岩溶地下水化学特征及影响因素分析[J]. 环境化学. 2016, 35 (11): 2394-2401。
[14]	秦松柏，欧阳正平，程天舜. 分层聚类分析在水文地球化学分类中的应用[J]. 地下水, 2008, 30 (1): 21-24。
[15]	LI X. P, FENG L N. Multivariate and geostatistical analyzes of metals in urban soil of Weinan industrial areas, Northwest of China [J]. Atmospheric Environment. 2012, 47: 58-65.
[16]	杨安，王艺涵，胡健，等. 青藏高原表土重金属污染评价与来源解析[J]. 环境科学, 2020, 41 (2): 886-894。
[17]	李笑，于奭，李亮，等. 石期河流域地下水化学特征及物质来源分析[J]. 环境科学, 2020, 41 (9): 4021-4029。
[18]	黄奇波，覃小群，刘朋雨，等. 乌江中上游段河水主要离子化学特征及控制因素[J]. 环境科学, 2016, 37 (5): 1779-1787。
[19]	孙平安，于奭，莫付珍，等. 不同地质背景下河流水化学特征及影响因素研究：以广西大溶江、灵渠流域为例[J]. 环境科学, 2016, 37 (1): 123-131。
[20]	刘江涛，袁五，曹月婷，等. 沁河冲洪积扇地下水水化学特征及成因分析[J]. 环境科学, 2018, 39 (12): 5428-5439。
[21]	安乐生，赵全升，叶思源，等. 黄河三角洲浅层地下水化学特征及形成作用 [J]. 环境科学. 2012, 33 (2): 370-378。
[22]	孙英，周金龙，魏兴，等. 巴楚县平原区地下水水化学特征及成因分析 [J].环境化学. 2019, 38 (11): 2601-2609。
[23]	刘伟江，袁祥美，张雅，等. 贵阳市岩溶地下水水化学特征及演化过程分析 [J].地质科技情报. 2018, 37 (6): 245-251。
[24]	LONG X, SUN Z Y, ZHOU A G, et al. Hydrogeochemical and Isotopic Evidence for Flow Paths of Karst Waters Collected in the Heshang Cave, Central China [J]. Journal of Earth Science. 2015, 26 (1): 149-156.
[25]	李洲，李晨曦，华琨，等. 黄土区洛川塬地下水化学特征及影响因素分析 [J]. 环境科学. 2019, 40 (8): 3559-3567。
[26]	GALY A, FRANCELANORD C. Weathering processes in the Ganges-Brahmaputra basin and the riverine alkalinity budget [J]. Chemical Geology. 1999, 159 (1-4): 31-60.
[27]	刘杰云，邱虎森，汤宏，等. 生物质炭对双季稻水稻土微生物生物量碳、氮及可溶性有机碳氮的影响[J]. 环境科学. 2019, 40 (8): 3799-3807。
[28]	GIBBS R J. Mechanisms Controlling Word Water Chemistry [J]. Science. 1970, 170: 1088-1090.
[29]	GIBBS R J. Water chemistry of the Amazon River [J]. Geochemica et Cosmochimica Acta. 1972, 36 (9): 1061-1066.
[30]	NOH H, HUH Y, QIN J H, et al. Chemical weathering in the Three Rivers region of Eastern Tibet [J]. Geochimica et Cosmochimica Acta. 2009, 73 (7): 1857-1877.
[31]	RAI S K, SINGH S K, KRISHNASWAMI S. Chemical weathering in the plain and peninsular sub-basins of the Ganga: impact on major ion chemistry and elemental fluxes [J]. Geochimica et Cosmochimica Acta. 2010, 74 (8): 2340-2355.
[32]	LI J, YUAN G L, DENG X R, et al. Major ion geochemistry of the Nansihu Lake basin rivers, North China: chemical weathering and anthropogenic load under intensive industrialization [J]. Environmental Earth Sciences. 2016, 75 (6): 453.
[33]	CHETELAT B, LIU C Q, ZHAO Z Q, et al. Geochemistry of the dissolved load of the Changjiang Basin rivers: Anthropogenic impacts and chemical weathering [J]. Geochimica et Cosmochimica Acta. 2008, 72 (17): 4254-4277.

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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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