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Groundwater recharge and evolution in the Wuwei Basin, northwestern China

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Abstract

Understanding the mechanisms and processes of groundwater recharge and evolution is critical for sustainable water resources management to meet human and agriculture needs under climate change, because groundwater is the primary water source in semiarid and arid regions, where the surface water resources are usually highly unstable and scarce. However, few studies investigated the recharge and evolution processes of groundwater combining with isotopic geochemistry and radiocarbon data, especially focused on the interactions among precipitation, surface water, groundwater, and rock. This study examined the recharge and evolution processes of groundwater in the Wuwei Basin based on stable isotopes, chemical indicators, and radiocarbon data. Our results showed that the Na+ (sodium ion) and K+ (potassium ion) concentrations of the groundwater were controlled by the dissolution of sylvite and halite origin from sediments, whereas the increase of Na+ and Cl (chloride ion) concentrations were not in accordance with a ratio of 1:1, indicating that the Na+ and K+ concentrations in groundwater were barely affected by the dissolution of halite and sylvite. Meanwhile, we also found that bicarbonate ion (HCO3) was the dominant ion with a decreased ratio in the groundwater. The SO42−/Cl (sulfate ion/chloride ion) ratio decreased with the sample profile from Southwest to Northeast due mainly to the increases of Cl concentration. The Ca2+/Cl (calcium ion/chloride ion) ratio decreased with the enhancement of Cl in the hydrodynamic sluggish belt. In addition, the δ18O (oxygen isotope) and δ2H (hydrogen isotope) values of groundwater gradually increased from Southwest to Northeast along the flow path. The heavy isotopic values were more strongly depleted than the isotopic values of precipitation in the ground water samples, suggesting that the recharge of ground water in the plain region was very limited from precipitation. Moreover, the groundwater in the phreatic aquifer was younger water with 3H (tritium isotope) values from 47 to 71 a.BP (before present), while the groundwater age in the confined aquifer was 1000–5800 BP evidenced by the 14C (carbon isotope) values between 48 and 88 pmc (percentage modern carbon content). Overall, these results suggested that the unconfined groundwater enriched along the overall groundwater flow path from the southwest to northeast of the Wuwei Basin and the melt water from the Qilian Mountains may determine the water isotopic composition and contributed to the steady long-term runoff of the Shiyang River. Our findings may have important implications for inter-basin water allocation programmes and groundwater management in the Wuwei Basin.

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References

  1. Chen XY, Chau KW (2016) A hybrid double feedforward neural network for suspended sediment load estimation. Water Resour Manage 30(7):2179–2194

  2. Chen ZY, Nie ZL, Zhang GH (2006) Environmental isotopic study on the recharge and residence time of groundwater in the Heihe River Basin, northwestern China. Hydrogeol J 14:1635–1651

  3. Chen YN, Chen YP, Xu CC (2010) Effects of ecological water conveyance on groundwater dynamics and riparian vegetation in the lower reaches of Tarim River, China. Hydrol Process 24:170–177

  4. Conan C, Bouraoui F, Turpin N, de Marsily G, Bidoglio G (2003) Mofelling flow and nitrate fate at catchment scale in Brittany (France). J Environ Qual 32:2026–2032

  5. Ding H, Zhao C, Huang X (2001) The ecological environment and desertification in the Shule River basin. Arid Zone Res 18:5–10

  6. Feng Q, Wei L, Su YH (2005) Distribution and evolution of water chemistry in Heihe River Basin. Environ Geol 45:947–956

  7. Fotovatikhah FH, Chau KW (2018) Survey of computational intelligence as basis to big flood management: challenges, research directions and future work. Eng Appl Comput Fluid Mech 12(1):411–437

  8. Hu LT, Chen CX, Jiao JJ (2007) Simulated groundwater interaction with rivers and springs in the Heihe river basin. Hydrol Process 21:2794–2806

  9. Huang TM, Pang ZH (2010) Changes in groundwater induced by water diversion in the Lower Tarim River, Xinjiang Uygur, NW China: evidence from environmental isotopes and water chemistry. J Hydrol 387:188–201

  10. Jin L, Edmunds WM, Lu ZL, Ma JZ (2015) Geochemistry of sediment moisture in the Badain Jaran desert: implications of recent environmental changes and water–rock interaction. Appl Geochem 63:235–247

  11. Li J (2010) Water shortages loom as northern China’s aquifers are sucked dry. Nature 328:1462–1463

  12. Li ZX, Feng Q, Yong S, Wang QJ, Yang J, Li YG, Li JG, Guo XY (2016) Stable isotope composition of precipitation in the south and north slopes of Wushaoling Mountain, northwestern China. Atmos Res 182:87–101

  13. Ma JZ, Wang XS, Edmunds WM (2005) The characteristics of ground-water resources and their changes under the impacts of human activity in the arid northwest China—a case study of the Shiyang River Basin. J Arid Environ 61:277–295

  14. Ma JZ, Ding ZY, Gates JB, Su YH (2008) Chloride and the environmental isotopes as the indicators of the groundwater recharge in the Gobi Desert, Northwest China. Environ Geol 55:1407–1419

  15. Ma JZ, Pan F, Chen LH, Edmunds WM, Ding ZY, He JH, Zhou KP, Huang TM (2010) Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China. Appl Geochem 25:996–1007

  16. Ma JZ, Zhang P, Zhu GF, Wang YQ, Edmunds WM, Ding ZY, He JH (2012) The composition and distribution of chemicals and isotopes in precipitation in the Shiyang River system, northwestern China. J Hydrol 436–437:92–101

  17. Ma ZY, Wu M, Zheng HJ, Xu Y, Meng Y, Dang SS (2018) A re-recognition of the main controlling factors for δ18O enrichment in deep geothermal water of Guanzhong Basin. Geol Bull China 37(2/3):487–495

  18. Nabavi PA, Bayat R, Hosseinzadeh BH, Afrasyabi H, Chau KW (2017) Modeling of energy consumption and environmental life cycle assessment for incineration and landfill systems of municipal solid waste management—a case study in Tehran Metropolis of Iran. J Clean Prod 148:427–440

  19. Narula KK, Gosain AK (2013) Modeling hydrology, groundwater recharge and non-point nitrate loadings in the Himalayan Upper Yamuna basin. Sci Total Environ 468–469:S102–S116

  20. Olyaie E, Banejad H, Chau KW, Melesse AM (2015) A comparison of various artificial intelligence approaches performance for estimating suspended sediment load of river systems: a case study in United States. Environ Monit Assess 187(4):189

  21. Ren W, Yao TD, Xie SY, He Y (2017) Controls on the stable isotopes in precipitation and surface waters across the southeastern Tibetan Plateau. J Hydrol 545:276–287

  22. Saeko I, Takeshi O, Shiro H (2014) Paleoceanographic changes of surface and deep water based on oxygen and carbon isotope records during the last 130 kyr identified in MD179 cores, off Joetsu, Japan Sea. J Asian Earth Sci 290:254–265

  23. Scanlon BR, Keese KE, Flint AL, Flint LE, Gaye CB, Edmunds WM, Simmers I (2006) Global synthesis of groundwater recharge in semiarid and arid regions. Hydrol Process 20:3335–3370

  24. Shi SE, Wei W, Yang D, Hu X, Zhou JJ, Zhang Q (2018) Spatial-temporal evolution of eco-environmental quality in the oasis of Shiyang river basin based on RSEDI. Chin J Ecol. https://doi.org/10.13292/j.1000-4890.201804.034

  25. Tang ZG, Ma JH, Li CK, Peng HH, Liang J (2016) Spatiotemporal changes of vegetation and the responses to temperature and precipitation in upper Shiyang River Basin. Geogr Geo Inf Sci 32(3):116–120

  26. Taormina R, Chau KW, Sivakumar B (2015) Neural network river forecasting through baseflow separation and binary-coded swarm optimization. J Hydrol 529(3):1788–1797

  27. Vairavamoorthy K, Gorantiwar SD, Pathirana A (2008) Managing urban water supplies in developing countries-climate change and water scarcity scenarios. Phys Chem Earth 33:330–339

  28. Vörösmarty CJ, McIntyre PB, Gessner MO, Dudgeon D, Prusevich A, Green P, Glidden S, Bunn SE, Sullivan C, Reidy LC, Davies PM (2010) Global threats to human water security and river biodiversity. Nature 467:555–561

  29. Wang LC, Chen F (2018) Change in water-use efficiency of irrigated areas before and after integrated management in Shiyang River Basin. Acta Ecol Sin. https://doi.org/10.5846/stxb201704060588

  30. Wang WC, Xu DM, Chau KW (2014) Assessment of river water quality based on theory of variable fuzzy sets and fuzzy binary comparison method. Water Resour Manag 28(12):4183–4200

  31. Wang ZT, Chen TY, Liu SW, Lai ZP (2016) Aeolian origin of interdune lakes in the Badain Jaran Desert, China. Arab J Geosci 9:190

  32. Wu YQ, Wen X, Zhang Y (2004) Analysis of the exchange of groundwater and river water by using Radon-222 in the middle Heihe Basin of northwestern China. Environ Geol 45:647–653

  33. Zhang HS (2005) A brief introduction of the changes in groundwater resources in the Hexi Corridor. Hydrogeol Eng Geol 32:81–84

  34. Zhang YH, Wu Y, Su J (2005) Groundwater replenishment analysis by using natural isotopes in Ejina Basin, northwestern China. Environ Geol 48:6–14

  35. Zhang L, Han M, Jin YK, Liu J (2015) Analysis of hydrogen and oxygen isotope in water sample using isotope ratio mass spectrometry and laser spectroscopy. J Chin Mass Spectrom Soc 36(6):559–564

  36. Zhou SE, Zhang MJ, Wang SJ, Sun MP (2018) Assessment of vulnerability in natural-social system in Hexi, Gansu. Resour Sci 40(2):452–462

  37. Zhu GF, Su YH, Feng Q (2008) The hydrochemical characteristics and evolution of groundwater and surface water in the Heihe River Basin, northwest China. Hydrogeol J 16:167–182

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Acknowledgements

We gratefully thank the anonymous reviewers for their constructive comments and suggestions on revising the manuscript. We also thank Mr. Steven Xu (Rutgers University, USA) for their kindly help on editing and polishing the English of the manuscript. This study was supported by the Natural Science Foundation of Hebei Province (nos. E2015402128, E2016402098, C2016402088, 31400418), Science and Technology Research Project of Hebei Colleges and Universities (QN2015253), and the Henan Key Laboratory of Water-Saving Agriculture (FIRI2019-01-01).

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Correspondence to Yunpu Zheng.

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This article is a part of a Topical Collection in Environmental Earth Sciences on Water Resources and Hydraulic Engineering, guest edited by Drs. Yanqing Lian, Walton Kelly, and Fulin Li.

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Wu, H., Wang, L., Liu, L. et al. Groundwater recharge and evolution in the Wuwei Basin, northwestern China. Environ Earth Sci 78, 366 (2019). https://doi.org/10.1007/s12665-019-8362-5

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Keywords

  • Environmental isotopes
  • Hydrochemistry
  • Groundwater circulation
  • Stable isotopes