Evolution characteristics of total dissolved solids in the groundwater level funnel area in the Hufu piedmont plain

ZHANG Xiyu; ZHANG Guanghui; YAN Mingjiang

doi:10.16030/j.cnki.issn.1000-3665.202009047

Volume 48 Issue 3

May 2021

Turn off MathJax

Article Contents

Abstract

References

Hydrogeology & Engineering Geology > 2021 > 48(3): 72-81. > DOI: 10.16030/j.cnki.issn.1000-3665.202009047

ZHANG Xiyu, ZHANG Guanghui, YAN Mingjiang. Evolution characteristics of total dissolved solids in the groundwater level funnel area in the Hufu piedmont plain[J]. Hydrogeology & Engineering Geology, 2021, 48(3): 72-81. DOI: 10.16030/j.cnki.issn.1000-3665.202009047

Citation:

PDF (5733 KB)

Evolution characteristics of total dissolved solids in the groundwater level funnel area in the Hufu piedmont plain

1.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei　050061, China
2.
China University of Geosciences(Beijing), Beijing　100083, China
3.
School of Water Resources and Environment, Hebei Center for Ecological and Environmental Geology Research, Hebei Province Collaborative Innovation Center for Sustainable Utilization of Water Resources and Optimization of Industrial Structure, Hebei Province Key Laboratory of Sustained Utilization and Development of Water Resources, Hebei GEO University, Shijiazhuang, Hebei　050031, China

More Information

Received Date: August 09, 2020
Revised Date: October 14, 2020
Available Online: May 12, 2021
Published Date: May 12, 2021

Graphical Abstract

Abstract

Abstract

In order to reveal the response characteristics of total dissolved solids (TDS) increase to groundwater level decline and the main chemical components that drive TDS to increase in the core area of the groundwater level funnel in the Hufu piedmont plain, geological statistical analysis, time series variation analysis and GIS spatial feature analysis technology are applied to analyze the variation characteristics of groundwater level depth, TDS and chemical compositions in the study area in the past 50 years (1972-2017). The results show that (1) the increase of TDS is characterized by stages along with the decrease of groundwater levels. In the initial stage of the funnel formation (1972-1980), the annual decrease of groundwater levels was the largest, and the annual increase of groundwater TDS was also the largest. In the middle period (1981-2000), the average annual decrease of groundwater level was the lowest, and the average annual increase of groundwater TDS was also the lowest. At the end of the period (2001-2017), the average annual decline of groundwater level was in the middle, and the average annual increase of groundwater TDS was also in the middle. (2) The influence of groundwater level on the increasing TDS presents a decreasing effect with the increase of the depth of groundwater level. For each increase of groundwater level of 1.0 m, the average growth rate of groundwater TDS increased by 21.96 mg/L at the initial stage of the funnel formation (the groundwater level buried depth ranged from 9.10 m to 23.20 m), the average growth rate of groundwater TDS increased by 13.54 mg/L at the middle stage (the groundwater level buried depth ranged from 13.40 m to 42.28 m), and the average growth rate of groundwater TDS increased by 12.32 mg/L at the end stage (the groundwater level buried depth ranged from 21.41 m to 50.29 m). (3) The increase of concentrations of Na⁺ and ${\rm{SO}}_4^{2-}$ in groundwater is the main reason for the increase of TDS in the funnel core area. From the initial stage to the final stage of the funnel formation, with the increasing depth of groundwater level and TDS, the ratio of the increment of Na⁺ and ${\rm{SO}}_4^{2-}$ in groundwater to the increment of TDS in each stage shows an increasing characteristic. However, the total ratio of the increment of Ca²⁺, Mg²⁺, ${\rm{HCO}}_3^-$ and Cl⁻ contents in the final stage to the increment of TDS is still 65.88%, which still plays a crucial role in the increasing of groundwater TDS in the funnel core area.
- piedmont plain,
- shallow groundwater,
- funnel forming process,
- decline of the water table,
- total dissolved solids,
- Hufu piedmont plain

FullText(HTML)

References (29)

References

[1]	李凤林, 杨先铎, 杨天申, 等. 石家庄城市供水水文地质勘测报告[R]. 石家庄: 河北省地质局水文地质观测总站, 1965. LI Fenglin, YANG Xianduo, YANG Tianshen, et al. Hydrogeological survey report of Shijiazhuang City water Supply[R]. Shijiazhuang: Hydrogeological Observation Station of Hebei Geology Bureau, 1965. (in Chinese)
[2]	张光辉, 费宇红, 张行南, 等. 滹沱河流域平原区地下水流场异常变化与原因[J]. 水利学报,2008,39(6):747 − 752. [ZHANG Guanghui, FEI Yuhong, ZHANG Xingnan, et al. Abnormal variation of groundwater flow field in plain area of Hutuo River basin and analysis on its cause[J]. Journal of Hydraulic Engineering,2008,39(6):747 − 752. (in Chinese with English abstract) DOI: 10.3321/j.issn:0559-9350.2008.06.017
[3]	王金哲, 张光辉, 母海东, 等. 人类活动对浅层地下水干扰程度定量评价及验证[J]. 水利学报,2011,42(12):1445 − 1451. [WANG Jinzhe, ZHANG Guanghui, MU Haidong, et al. Quantitative valuation and validation of the influence degree of human activities on shallow groundwater[J]. Journal of Hydraulic Engineering,2011,42(12):1445 − 1451. (in Chinese with English abstract)
[4]	冯慧敏, 张光辉, 王电龙, 等. 近50年来石家庄地区地下水流场演变驱动力分析[J]. 水利学报,2014,45(2):180 − 186. [FENG Huimin, ZHANG Guanghui, WANG Dianlong, et al. Analysis on driving force for groundwater flow field evolution in Shijiazhuang Area in recent 50 years[J]. Journal of Hydraulic Engineering,2014,45(2):180 − 186. (in Chinese with English abstract)
[5]	冯慧敏. 石家庄平原区地下水流场演变特征与尺度效应[D]. 北京: 中国地质科学院, 2015. FENG Huimin. Groundwater flow field evolution characteristic and size effect of Shijiazhuang plain[D]. Beijing: Chinese Academy of Geological Sciences, 2015. (in Chinese with English abstract)
[6]	张光辉, 田言亮, 王电龙, 等. 冀中山前农业区地下水位强降弱升特征与机制[J]. 水科学进展,2015,26(2):227 − 232. [ZHANG Guanghui, TIAN Yanliang, WANG Dianlong, et al. Sharp decline and sluggish rise of shallow groundwater level in the Central Hebei piedmont agricultural region[J]. Advances in Water Science,2015,26(2):227 − 232. (in Chinese with English abstract)
[7]	张千千, 王慧玮, 王龙, 等. 滹沱河冲洪积扇地区地下水硬度升高的机理研究[J]. 环境科学与技术,2018,41(增刊2):62 − 68. [ZHANG Qianqian, WANG Huiwei, WANG Long, et al. Increasing mechanism of groundwater total hardness (TH) in the hutuo river alluvial-pluvial fan[J]. Environmental Science & Technology,2018,41(Sup2):62 − 68. (in Chinese with English abstract)
[8]	张小文, 何江涛, 刘丹丹, 等. 滹沱河冲洪积扇浅层地下水水质外界胁迫作用分析[J]. 水文地质工程地质,2018,45(5):48 − 56. [ZHANG Xiaowen, HE Jiangtao, LIU Dandan, et al. An analysis of the stress effects and methods of the shallow groundwater quality in the Hutuo River alluvial fan[J]. Hydrogeology & Engineering Geology,2018,45(5):48 − 56. (in Chinese with English abstract)
[9]	王磊, 何江涛, 张振国, 等. 基于信息筛选和拉依达准则识别地下水主要组分水化学异常的方法研究[J]. 环境科学学报,2018,38(3):919 − 929. [WANG Lei, HE Jiangtao, ZHANG Zhenguo, et al. Research on the method to identify the outliers of the main components of groundwater based on the information screening coupled with PauTa criterion[J]. Acta Scientiae Circumstantiae,2018,38(3):919 − 929. (in Chinese with English abstract)
[10]	单晓杰, 何江涛, 张小文, 等. 基于人为活动影响识别的区域地下水水质演化预测: 以石家庄地区为例[J]. 现代地质,2020,34(1):189 − 198. [SHAN Xiaojie, HE Jiangtao, ZHANG Xiaowen, et al. Prediction of regional groundwater quality evolution affected by human activities: A case study of Shijiazhuang area[J]. Geoscience,2020,34(1):189 − 198. (in Chinese with English abstract)
[11]	李亚松, 张兆吉, 费宇红, 等. 河北省滹沱河冲积平原地下水质量及污染特征研究[J]. 地球学报,2014,35(2):169 − 176. [LI Yasong, ZHANG Zhaoji, FEI Yuhong, et al. Groundwater quality and contamination characteristics in the hutuo river plain area, Hebei Province[J]. Acta Geoscientica Sinica,2014,35(2):169 − 176. (in Chinese with English abstract) DOI: 10.3975/cagsb.2014.02.07
[12]	程中双. 强烈开采含水层的水化学和同位素响应及其水文地质指示: 以石家庄山前平原为例[D]. 北京: 中国地质科学院, 2015. CHENG Zhongshuang. Chemical and isotopic response to intensive groundwater exploitation and its implications: A case study in the piedmont plain, Shijiazhuang[D]. Beijing: Chinese Academy of Geological Sciences, 2015. (in Chinese with English abstract)
[13]	田夏. 滹沱河超采区地下水水化学演变特征与模拟[D]. 北京: 中国地质大学(北京), 2016. TIAN Xia. Study on the chemical characteristics and simulation of groundwater in overdrafted zone of the Hutuo River Basin[D]. Beijing: China University of Geosciences (Beijing), 2016. (in Chinese with English abstract)
[14]	YAN M J, WANG Q, TIAN Y L, et al. The dynamics and origin of groundwater salinity in the northeast Hufu Plain[J]. Environmental Earth Sciences,2016,75(16):1 − 15.
[15]	RINA K, SINGH C K, DATTA P S, et al. Erratum to: Geochemical modelling, ionic ratio and GIS based mapping of groundwater salinity and assessment of governing processes in Northern Gujarat, India[J]. Environmental Earth Sciences,2013,70(5):2421 − 2422. DOI: 10.1007/s12665-013-2821-1
[16]	费宇红, 陈树娥, 刘克岩. 滹沱河断流区水环境劣变特征与地下调蓄潜力[J]. 水利学报,2001(11):41 − 44. [FEI Yuhong, CHEN Shue, LIU Keyan. characteristics of inferior variation of water environment in Hutuohe River dried-up area[J]. Journal of Hydraulic Engineering,2001(11):41 − 44. (in Chinese with English abstract) DOI: 10.3321/j.issn:0559-9350.2001.11.007
[17]	李婉珠. 石家庄市地下水环境演化规律研究[D]. 石家庄: 石家庄经济学院, 2009. LI Wanzhu. Research of environmental evolution of groundwater of Shijiazhuang City[D]. Shijiazhuang: Shijiazhuang University of Economics, 2009. (in Chinese with English abstract)
[18]	张学礼. 滹沱河流域水环境变迁与区域社会发展研究(1949-2009)[D]. 石家庄: 河北师范大学, 2018. ZHANG Xueli. Research on water environmental transition and regional social development in Hutuo River basin(1949-2009)[D]. Shijiazhuang: Hebei Normal University, 2018. (in Chinese with English abstract)
[19]	王晓玮, 邵景力, 王卓然, 等. 西北地区地下水水量-水位双控指标确定研究: 以民勤盆地为例[J]. 水文地质工程地质,2020,47(2):17 − 24. [WANG Xiaowei, SHAO Jingli, WANG Zhuoran, et al. A study of the determination of indicators of dual control of groundwater abstraction amount and water table in northwest China: a case study of the Minqin Basin[J]. Hydrogeology & Engineering Geology,2020,47(2):17 − 24. (in Chinese with English abstract)
[20]	田夏, 李亚松, 费宇红, 等. 滹沱河超采区地下水硫酸盐来源识别及迁移转化[J]. 科学技术与工程,2020,20(7):2583 − 2589. [TIAN Xia, LI Yasong, FEI Yuhong, et al. Sulfate source identification, migration and transformation in the groundwater over-exploited area of the hutuo river basin[J]. Science Technology and Engineering,2020,20(7):2583 − 2589. (in Chinese with English abstract) DOI: 10.3969/j.issn.1671-1815.2020.07.008
[21]	张小文, 何江涛, 彭聪, 等. 地下水主要组分水化学异常识别方法对比: 以柳江盆地为例[J]. 环境科学,2017,38(8):3225 − 3234. [ZHANG Xiaowen, HE Jiangtao, PENG Cong, et al. Comparison of identification methods of main component hydrochemical anomalies in groundwater: a case study of Liujiang basin[J]. Environmental Science,2017,38(8):3225 − 3234. (in Chinese with English abstract)
[22]	王水献, 王云智, 董新光. 焉耆盆地浅层地下水埋深与TDS时空变异及水化学的演化特征[J]. 灌溉排水学报,2007,26(5):90 − 93. [WANG Shuixian, WANG Yunzhi, DONG Xinguang. The spatio-temporal variation of shallow groundwater TDS, depth and it's evolvement characteristic of water chemistry in Yanqi basin[J]. Journal of Irrigation and Drainage,2007,26(5):90 − 93. (in Chinese with English abstract)
[23]	赵江涛, 周金龙, 高业新, 等. 新疆焉耆盆地平原区地下水溶解性总固体时空演化[J]. 农业工程学报,2016,32(5):120 − 125. [ZHAO Jiangtao, ZHOU Jinlong, GAO Yexin, et al. Spatial-temporal evolution of total dissolved solids of groundwater in plain area of Yanqi Basin, Xinjiang[J]. Transactions of the Chinese Society of Agricultural Engineering,2016,32(5):120 − 125. (in Chinese with English abstract) DOI: 10.11975/j.issn.1002-6819.2016.05.017
[24]	王雨山, 李戍, 李海学, 等. 海原盆地地下水咸化特征和控制因素[J]. 水文地质工程地质,2019,46(4):10 − 17. [WANG Yushan, LI Shu, LI Haixue, et al. Groundwater salinization characteristics and controlling factors in the Haiyuan Basin[J]. Hydrogeology & Engineering Geology,2019,46(4):10 − 17. (in Chinese with English abstract)
[25]	章旭, 郝红兵, 刘康林, 等. 西藏加查象牙泉水文地球化学特征及成因[J]. 水文地质工程地质,2019,46(4):1 − 9. [ZHANG Xu, HAO Hongbing, LIU Kanglin, et al. Hydrogeochemical characteristics and formation of the Ivory spring in Jiacha County of Tibet[J]. Hydrogeology & Engineering Geology,2019,46(4):1 − 9. (in Chinese with English abstract)
[26]	张千千, 王慧玮, 翟天伦, 等. 滹沱河冲洪积扇地下水硝酸盐的污染特征及污染源解析[J]. 水文地质工程地质,2017,44(6):110 − 117. [ZHANG Qianqian, WANG Huiwei, ZHAI Tianlun, et al. Characteristics and source apportionment of groundwater nitrate contamination in the Hutuo River alluvial-pluvial fan regions[J]. Hydrogeology & Engineering Geology,2017,44(6):110 − 117. (in Chinese with English abstract)
[27]	YI Q, STEWART M. Prediction of groundwater quality trends resulting from anthropogenic changes in southeast Florida[J]. Ground Water,2018,56(1):46 − 61. DOI: 10.1111/gwat.12544
[28]	张光辉, 刘中培, 连英立, 等. 河北平原地下水质变及农药化肥施用量变化影响[J]. 南水北调与水利科技,2009,7(2):50 − 54. [ZHANG Guanghui, LIU Zhongpei, LIAN Yingli, et al. Variation of groundwater quality and influence of pesticide and fertilizer on Hebei plain[J]. South-to-North Water Transfers and Water Science & Technology,2009,7(2):50 − 54. (in Chinese with English abstract)
[29]	张英, 刘春燕, 王金翠, 等. 快速城镇化进程中典型冲洪积扇地下水化学演变特征及影响因素解析[J]. 南水北调与水利科技,2019,17(5):172 − 179. [ZHANG Ying, LIU Chunyan, WANG Jincui, et al. Analysis of characteristics and influencing factors of groundwater chemical evolution of typical alluvial fans of rapid urbanization[J]. South-to-North Water Transfers and Water Science & Technology,2019,17(5):172 − 179. (in Chinese with English abstract)

Cited By

Get Citation

PDF

XML

Article views (376) PDF downloads (248)

Evolution characteristics of total dissolved solids in the groundwater level funnel area in the Hufu piedmont plain

Abstract

References

Catalog

Export File

Citation

Format

Content