Chemical and Isotopic Responses to Intensive Groundwater Abstraction and Its Implications on Aquifer Sustainability in Shijiazhuang, China

Zhongshuang Cheng; Yongbo Zhang; Chen Su; Zongyu Chen

doi:10.1007/s12583-017-0729-5

Volume 28 Issue 3

Jun 2017

Turn off MathJax

Article Contents

Journal of Earth Science > 2017 > 28(3): 523-534.

Zhongshuang Cheng, Yongbo Zhang, Chen Su, Zongyu Chen. Chemical and Isotopic Responses to Intensive Groundwater Abstraction and Its Implications on Aquifer Sustainability in Shijiazhuang, China. Journal of Earth Science, 2017, 28(3): 523-534. doi: 10.1007/s12583-017-0729-5

Citation:

Zhongshuang Cheng, Yongbo Zhang, Chen Su, Zongyu Chen. Chemical and Isotopic Responses to Intensive Groundwater Abstraction and Its Implications on Aquifer Sustainability in Shijiazhuang, China. Journal of Earth Science, 2017, 28(3): 523-534. doi: 10.1007/s12583-017-0729-5

Citation:

Zhongshuang Cheng, Yongbo Zhang, Chen Su, Zongyu Chen. Chemical and Isotopic Responses to Intensive Groundwater Abstraction and Its Implications on Aquifer Sustainability in Shijiazhuang, China. Journal of Earth Science, 2017, 28(3): 523-534. doi: 10.1007/s12583-017-0729-5

PDF( 2038 KB)

Chemical and Isotopic Responses to Intensive Groundwater Abstraction and Its Implications on Aquifer Sustainability in Shijiazhuang, China

doi: 10.1007/s12583-017-0729-5

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China

More Information

Author Bio:
Zhongshuang Cheng: http://orcid.org/0000-0002-0983-4971

Zongyu Chen: http://orcid.org/0000-0001-7320-0204
Corresponding author: Zongyu Chen, chenzongyu_iheg@126.com
Received Date: 01 Nov 2014
Accepted Date: 30 Mar 2015
Publish Date: 01 Jun 2017

Abstract

Abstract

The stress imposed on groundwater resources due to intensively exploited aquifer has resulted in groundwater depletion in the North China Plain (NCP). Management of groundwater resources needs to understand the changes or dynamic responses due to the exploitation. The response of groundwater systems to intensive exploitation and groundwater availability were assessed by the combined use of conventional hydrochemical data and environmental isotopes in Shijiazhuang, NCP. The generally increased concentration of total dissolved solids (TDS), major cation and anion of groundwater in the past 40 years indicated high vulnerability of aquifer system but a short turn over time by intensive groundwater exploitation, which also was proved by changes of groundwater renewal rate estimated by tritium. The vertical distribution of tritium in aquifers showed that the active groundwater recharge zone has been extended from the depth of 100 to ~150 m since 1985, indicating an enhancement of active groundwater flushing of local groundwater system due to intensive groundwater abstraction. The enrichment trend of δ¹⁸O and δ²H value with groundwater abstraction, suggested the impacts of local recharge from irrigation return. The increase concentrations of nitrate with time indicated high aquifer vulnerability. A comprehensive effort should be developed for effective management strategies that ensure long-term, stable, and flexible water supplies to meet water demands in the NCP.
- isotope,
- renewal rate,
- North China Plain,
- groundwater

FullText(HTML)

References(44)

References

Bicalho, C. C., Batiot-Guilhe, C., Seidel, J. L., et al., 2012. Hydrodynamical Changes and Their Consequences on Groundwater Hydrochemistry Induced by Three Decades of Intense Exploitation in a Mediterranean Karst System. Environmental Earth Sciences, 65(8): 2311-2319. doi: 10.1007/s12665-011-1384-2

Bruce, D. L., Yechieli, Y., Zilberbrand, M., et al., 2007. Delineation of the Coastal Aquifer of Israel Based on Repetitive Analysis of ¹⁴C and Tritium. Journal of Hydrology, 343(1): 56-70. doi: 10.1007/s12665-011-1384-2

Chen, W. H., 1999. Ground Water in Hebei. Seismological Press, Beijing. 539 (in Chinese)

Chen, Z. Y., Chen, J. S., Fei, Y. H., et al., 2006. Estimation of Groundwater Renewal Rate by Tritium in the Piedmont Plain of the Taihang Mountains. Nuclear Techniques, 29(6): 426-431 (in Chinese with English Abstract) https://www.researchgate.net/publication/285778438_Estimation_of_groundwater_renewal_rate_by_tritium_in_the_piedmont_plain_of_the_Taihang_Mountains

Chen, Z. Y., Nie, Z. L., Zhang, Z. J., et al., 2005. Isotopes and Sustainability of Ground Water Resources, North China Plain. Groundwater, 43(4): 485-493. doi: 10.1111/j.1745-6584.2005.0038.x

Chen, Z. Y., Qi, J. X., Xu, J. M., et al., 2003. Paleoclimatic Interpretation of the Past 30 Ka from Isotopic Studies of the Deep Confined Aquifer of the North China Plain. Applied Geochemistry, 18(7): 997-1009. doi: 10.1016/s0883-2927(02)00206-8

Cheng, R. N. , 1988. Groundwater Replenishment Analysis through Isotope Composition of Water in the Nature. In: Liu, C. M. , Ren, H. , eds. , Air, Surface, Soil and Ground Water Interaction. Science Press, Beijing. 275-286 (in Chinese)

Clark, I. D., Fritz, P., 1997. Environmental Isotopes in Hydrogeology. CRC Press, Florida. 352

Currell, M. J., Cartwright, I., Bradley, D. C., et al., 2010. Recharge History and Controls on Groundwater Quality in the Yuncheng Basin, North China. Journal of Hydrology, 385(1-4): 216-229. doi: 10.1016/j.jhydrol.2010.02.022

Deng, Y. M., Wang, Y. X., Li, H. J., et al., 2015. Seasonal Variation of Arsenic Speciation in Shallow Groundwater from Endemic Arsenicosis Area in Jianghan Plain. Earth Science--Journal of China University of Geosciences, 40(11): 1876-1886 (in Chinese with English Abstract) doi: 10.3799/dqkx.2015.168

Doney, S. C., Glover, D. M., Jenkins, W. J., 1992. A Model Function of the Global Bomb Tritium Distribution in Precipitation, 1960-1986. Journal of Geophysical Research, 97(C4): 5481-5492. doi: 10.1029/92jc00015

El-Naqa, A., Al-Momani, M., Kilani, S., et al., 2007. Groundwater Deterioration of Shallow Groundwater Aquifers due to Overexploitation in Northeast Jordan. CLEAN-Soil, Air, Water, 35(2): 156-166. doi: 10.1002/clen.200700012

Fritz, S. J., Drimmie, R. J., Fritz, P., 1991. Characterizing Shallow Aquifers Using Tritium and ¹⁴C: Periodic Sampling Based on Tritium Half-Life. Applied Geochemistry, 6(1): 17-33. doi: 10.1016/0883-2927(91)90060-3

Guendouz, A., Moulla, A. S., Edmunds, W. M., et al., 2003. Hydrogeochemical and Isotopic Evolution of Water in the Complexe Terminal Aquifer in the Algerian Sahara. Hydrogeology Journal, 11(4): 483-495. doi: 10.1007/s10040-003-0263-7

Hu, Y. K., Moiwo, J. P., Yang, Y. H., et al., 2010. Agricultural Water-Saving and Sustainable Groundwater Management in Shijiazhuang Irrigation District, North China Plain. Journal of Hydrology, 393(3-4): 219-232. doi: 10.1016/j.jhydrol.2010.08.017

IAEA (International Atomic Energy Agency), 2006. Isotopic Assessment of Long Term Groundwater Exploitation. International Atomic Energy Agency, Vienna. 286

IAEA/WMO, 2012. Water Isotope System for Data Analysis, Visualization and Electronic Retrieval. The GNIP Database. [2017-04-01]. http://www.univie.ac.at/cartography/project/wiser/

Kamel, S., Dassi, L., Zouari, K., et al., 2005. Geochemical and Isotopic Investigation of the Aquifer System in the Djerid-Nefzaoua Basin, Southern Tunisia. Environmental Geology, 49(1): 159-170. doi: 10.1007/s00254-005-0076-1

Kendy, E., Zhang, Y. Q., Liu, C. M., et al., 2004. Groundwater Recharge from Irrigated Cropland in the North China Plain: Case Study of Luancheng County, Hebei Province, 1949-2000. Hydrological Processes, 18(12): 2289-2302. doi: 10.1002/hyp.5529

Kreuzer, A. M., von Rohden, C. V., Friedrich, R., et al., 2009. A Record of Temperature and Monsoon Intensity over the Past 40 kyr from Groundwater in the North China Plain. Chemical Geology, 259(3/4): 168-180. doi: 10.1016/j.chemgeo.2008.11.001

Lang, X. J., Lin, W. J., Liu, Z. M., et al., 2016. Hydrochemical Characteristics of Geothermal Water in Guide Basin. Earth Science--Journal of China University of Geosciences, 41(10): 1723-1734 (in Chinese with English Abstract) https://www.researchgate.net/publication/309769549_Hydrochemical_characteristics_of_geothermal_water_in_guide_basin

Le Gal La Salle, C., Marlin, C., Leduc, C., et al., 2001. Renewal Rate Estimation of Groundwater Based on Radioactive Tracers (³H, ¹⁴C) in an Unconfined Aquifer in a Semi-Arid Area, Iullemeden Basin, Niger. Journal of Hydrology, 254(1): 145-156. doi: 10.1016/s0022-1694(01)00491-7

Liang, X., Liu, Y., Jin, M. G., et al., 2010. Direct Observation of Complex Tóthian Groundwater Flow Systems in the Laboratory. Hydrological Processes, 24(24): 3568-3573. doi: 10.1002/hyp.7758

Lin, X. Y., Jiao, Y., 1987. Scientific Management of Groundwater Resources in Shijiazhuang. Xinhua Press, Changchun. 220 (in Chinese)

Liu, J., Chen, Z. Y., Wei, W., et al., 2014. Using Chlorofluorocarbons (CFCs) and Tritium (³H) to Estimate Groundwater Age and Flow Velocity in Hohhot Basin, China. Hydrological Processes, 28(3): 1372-1382. doi: 10.1002/hyp.9659

Liu, J., Zheng, C. M., Zheng, L., et al., 2008. Ground Water Sustainability: Methodology and Application to the North China Plain. Groundwater, 46(6): 897-909. doi: 10.1111/j.1745-6584.2008.00486.x

Long, X., Sun, Z. Y., Zhou, A. G., et al., 2015. Hydrogeochemical and Isotopic Evidence for Flow Paths of Karst Waters Collected in the Heshang Cave, Central China. Journal of Earth Science, 26(1): 149-156. doi: 10.1007/s12583-015-0522-2

Madioune, D. H., Faye, S., Orban, P., et al., 2014. Application of Isotopic Tracers as a Tool for Understanding Hydrodynamic Behavior of the Highly Exploited Diass Aquifer System (Senegal). Journal of Hydrology, 511(7): 443-459. doi: 10.1016/j.jhydrol.2014.01.037

Meng, S. H., Liu, J., Zhang, Z. J., et al., 2015. Spatiotemporal Evolution Characteristics Study on the Precipitation Infiltration Recharge over the Past 50 Years in the North China Plain. Journal of Earth Science, 26(3): 416-424. doi: 10.1007/s12583-014-0494-7

Shi, X. F., Dong, W. H., Li, M. Z., et al., 2012. Evaluation of Groundwater Renewability in the Henan Plains, China. Geochemical Journal, 46(2):107-115. doi: 10.2343/geochemj.1.0154

Shu, Y. Q., Villholth, K. G., Jensen, K. H., et al., 2012. Integrated Hydrological Modeling of the North China Plain: Options for Sustainable Groundwater Use in the Alluvial Plain of Mt. Taihang. Journal of Hydrology, 464/465: 79-93. doi: 10.1016/j.jhydrol.2012.06.048

Su, X. S., Xu, W., Du, S. H., 2014. In Situ Infiltration Test Using a Reclaimed Abandoned River Bed: Managed Aquifer Recharge in Shijiazhuang City, China. Environmental Earth Sciences, 71(12): 5017-5025. doi: 10.1007/s12665-013-2893-y

Trabelsi, R., Kacem, A., Zouari, K., et al., 2009. Quantifying Regional Groundwater Flow between Continental Intercalaire and Djeffara Aquifers in Southern Tunisia Using Isotope Methods. Environmental Geology, 58(1): 171-183. doi: 10.1007/s00254-008-1503-x

von Rohden, C., Kreuzer, A., Chen, Z. Y., et al., 2010. Characterizing the Recharge Regime of the Strongly Exploited Aquifers of the North China Plain by Environmental Tracers. Water Resources Research, 46: 1-14. doi: 10.1029/2008wr007660

Wan, J. W., Liu, C. F., Chao, N. Y., et al., 2003. Principle and Application of Isotope Hydrology. China University of Geosciences Press, Wuhan. 431 (in Chinese)

Wang, J. Z., Zhang, G. H., Mu, H. D., et al., 2010. The Shallow Groundwater Recharging Characteristics Responding to Human Activities. Acta Geoscientica Sinica, 31(4): 557-562 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB201004009.htm

Yu, K. N., Hao, A. B., Li, D., et al., 2001. Distribution of Groundwater Salt Pollution and the Polluting Mechanism in Shijiazhuang. Earth Science Frontiers, 8(1): 151-154 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200101031.htm

Zha, Y. Y., Shi, L. S, Ye, M., et al., 2013. A Generalized Ross Method for Two-and Three-Dimensional Variably Saturated Flow. Advances in Water Resources, 54: 67-77. doi: 10.1016/j.advwatres.2013.01.002

Zhan, Y. H., Guo, H. M., Wang. Y., et al., 2014. Evolution of Groundwater Major Components in the Hebei Plain: Evidences from 30-Year Monitoring Data. Journal of Earth Science, 25(3): 563-574. doi: 10.1007/s12583-014-0445-3

Zhang, Y. H., Ye, S. J., Wu, J. C., 2011. A Modified Global Model for Predicting the Tritium Distribution in Precipitation, 1960-2005. Hydrological Processes, 25(15): 2379-2392. doi: 10.1002/hyp.8001

Zhang, Z. G., Zhang, H. P., Sun, J. C. et al., 1987. Environmental Isotope Study Related to Ground Water Age, Flow System and Saline Water Origin in Quaternary Aquifer of Hebei Plain. Hydrogeology and Engineering Geology, 96(4): 1-6 https://www.researchgate.net/publication/284299387_Environmental_isotope_study_related_to_groundwater_age_flow_system_and_saline_water_origin_in_Quaternary_aquifer_of_Hebei_plain

Zhang, Z. J., Fei, Y. H., 2009. Atlas of Groundwater Sustainable Utilization in North China Plain. Sinomaps Press, Beijing. 185 (in Chinese)

Zhang, Z. J., Fei, Y. H., Chen, Z. Y., et al., 2009. Investigation and Assessment of Sustainable Utilization of Groundwater Resources in the North China Plain. Geological Publishing House, Beijing. 471 (in Chinese with English Abstract)

Zhou, L., Liu, C. F., Jiang, S., et al., 2001. A Study of ³⁶Cl Age in Quaternary Groundwater of Hebei Plain, China. Science in China Series E: Technological Sciences, 44(S1): 11-15. doi: 10.1007/bf02916783

Relative Articles

Supplements(0)

Cited By

Proportional views