Abstract
The groundwater quality in the Lilou Coal Mine in Shandong Province can be divided into “three zones” based on the range of mining-induced fractures. Considering the observed Ordovician aquifer water level decline rate of 2.6 m/year, we propose that the saline mine water contained in Zones II and III can be injected into the well-developed underling karst Ordovician aquifer in Zone I. A water quality comparison of 27 factors demonstrated that only the Na+ concentration in the mine water exceeded that in the Ordovician aquifer water. The Ordovician aquifer has an average karst development thickness of 140 m, and the karst fracture rate ranges from 6 to 14%. The filter screen length of the injection well should reach 150 m to achieve zero pressure at the surface for an injection flow rate of 200 m3/h. With only the need to reduce Na+ concentrations below 319 mg/L, ≈ $2.4 million (U.S.) could be saved annually by simplifying the mine water treatment process.
摘要
根据采动裂隙的范围, 将山东**楼煤矿的地下水水质划分为“三区”。考虑到奥陶系含水层水位下降速率观测值为2.6 m/年, 我们建议将II区和III区所含的含盐矿井水注入I区发育良好的下伏奥陶系岩溶含水层。通过27个因素的水质比较表明, 矿井水中只有Na+浓度超过奥陶系含水层。奥陶系含水层岩溶的发育厚度**均为140m, 岩溶裂隙率在6-14%之间。注入井的滤网长度应达到150 m, 注入流速为200 m3/h的情况下实现地面零压力。只需将Na+浓度降低到319 mg/L以下, 通过简化矿井水处理过程, 每年可节省约240万美元。
Zusammenfassung
Die Qualität des Grundwassers in der Lilou Kohlenmine (Provinz Shandong) kann anhand des Ausmaßes bergbaubedingter Brüche in drei Zonen eingeteilt werden. In Anbetracht der beobachteten Absenkungsrate des ordovizischen Grundwasserleiters von 2,6 m/a schlagen wir vor, dass das in den Zonen II und III enthaltene, salzhaltige Grubenwasser in den gut entwickelten, darunterliegenden, ordovizischen Karstgrundwasserleiter in Zone I eingeleitet werden könnte. Ein Vergleich der Wasserqualität anhand von 27 Faktoren zeigte, dass nur die Na+-Konzentration des Grubenwassers über der des Grundwassers im ordovizischen Aquifer liegt. Der ordovizische Grundwasserleiter hat eine durchschnittliche Mächtigkeit der Karstbildung von 140 m und die Karstbruchrate liegt zwischen 6 und 14%. Die Länge des Filters der Injektionsbohrung sollte 150 m betragen, um bei einem Injektionsdurchfluss von 200 m³/h an der Oberfläche einen Druck von Null zu erreichen. Da nur eine Absenkung der Na Na+-Konzentration unter 319 mg/L erforderlich wird, könnten durch Vereinfachung der Grubenwasseraufbereitung jährlich rund 2,4 Mio. US-$ eingespart werden.
Resumen
La calidad del agua subterránea en la mina de carbón Lilou en la provincia de Shandong se puede dividir en "tres zonas" a partir del grado de fracturación inducido por la minería. Considerando la tasa de disminución del nivel del agua de 2.6 m/año observada en el acuífero Ordovícico, proponemos que el agua salina de la mina contenida en las Zonas II y III podría ser inyectada en el acuífero Ordovícico kárstico bien desarrollado en la Zona I. Una comparación de la calidad del agua a partir de 27 factores demostró que solo la concentración de Na+ en el agua de la mina superaba la del agua del acuífero Ordovícico. El acuífero Ordovícico tiene un grosor promedio de desarrollo kárstico de 140 m, mientras que la tasa de fracturación kárstica varía del 6 a 14%. La longitud de la pantalla del filtro del pozo de inyección debería alcanzar los 150 m para lograr una presión cero en la superficie con una tasa de flujo de inyección de 200 m3/h. Solo necesitando reducir las concentraciones de Na+ por debajo de 319 mg/L, se podrían ahorrar aproximadamente 2.4 millones $ anualmente, al simplificar el proceso de tratamiento del agua de la mina.
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References
Alqahtani A, Sale T, Ronayne MJ, Hemenway C (2021) Demonstration of sustainable development of groundwater through aquifer storage and recovery (ASR). Water Resour Manag 35(2):429–445. https://doi.org/10.1007/s11269-020-02721-2
Al-Shalabi EW, Sepehrnoori K (2016) A comprehensive review of low salinity/engineered water injections and their applications in sandstone and carbonate rocks. J Pet Sci Eng 139:137–161. https://doi.org/10.1016/j.petrol.2015.11.027
Babushkin VD, Böcker T, Borevsky BV, Kovalewsky VS (1975) Regime of subterranean water flows in karst regions. In: Burger A, Dubertret L (eds) Hydrogeology of karstic terrains, Int Union Geol Sci Ser B 3. IAH, Paris, pp 68–78
Cai QW, Huang BX, Zhao XL, **ng YK, Liu SL (2023) Experimental investigation on the morphology of fracture networks in hydraulic fracturing for coal mass characterized by X-ray micro-computed tomography. Rock Mech Rock Eng. https://doi.org/10.1007/s00603-022-03210-1
Cao JR, Li QH, Cheng XS, Zheng G, Ha D, Zeng CF (2022) Study on artificial recharge and well loss in confined aquifers using theoretical and back-analysis calculations of hydrogeological parameters from recharge and pum** tests. Bull Eng Geol Environ. https://doi.org/10.1007/s10064-022-02988-2
Chandra S, Medha I, Tiwari AK (2023) The role of modified biochar for the remediation of coal mining-impacted contaminated soil: a review. Sustainability. https://doi.org/10.3390/su15053973
Chen X, He SM, Falinski MM, Wang YX, Li T, Zheng SX, Sun DY, Dai JQ, Bian YH, Zhu XB, Jiang JY, Hu LB, Ren ZJ (2021) Sustainable off-grid desalination of hypersaline waters using Janus wood evaporators. Energy Environ Sci 14(10):5347–5357. https://doi.org/10.1039/d1ee01505b
Chen G, Xu Z, Sun Y, Sui W, Li X, Zhao X, Liu Q (2022) Minewater deep transfer and storage. J Clean Prod. https://doi.org/10.1016/j.jclepro.2021.129848
Cognac KE, Ronayne MJ (2020) Changes to inter-aquifer exchange resulting from long-term pum**: implications for bedrock groundwater recharge. Hydrogeol J 28(4):1359–1370. https://doi.org/10.1007/s10040-020-02141-x
Fallatah OA, Ahmed M, Cardace D, Boving T, Akanda AS (2019) Assessment of modern recharge to arid region aquifers using an integrated geophysical, geochemical, and remote sensing approach. J Hydrol 569:600–611. https://doi.org/10.1016/j.jhydrol.2018.09.061
Gong DA, Yin YC, Chen HL, Guo B, Wu P, Wang Y, Yang Y, Li ZK, He Y, Zeng GF (2021) Interfacial ions sieving for ultrafast and complete desalination through 2D nanochannel defined graphene composite membranes. ACS Nano 15(6):9871–9881. https://doi.org/10.1021/acsnano.1c00987
He M, Li Q, Li XY (2022) A new simulator for hydromechanical coupling analysis of injection-induced fault activation. Geomech Geophys Geo-Energy Geo-Resour. https://doi.org/10.1007/s40948-022-00353-x
Kang G-d, Cao Y-m (2014) Application and modification of poly(vinylidene fluoride) (PVDF) membranes - a review. J Membr Sci 463:145–165. https://doi.org/10.1016/j.memsci.2014.03.055
Kang F, Shi Q, Ma Z, Sui H (2023) Genetic mechanism of the karst geothermal reservoir in buried uplifts of basins: a case study of Heze. Acta Geol Sin 97(1):221–237. https://doi.org/10.19762/j.cnki.dizhixuebao.2022017
Khadra WM, Stuyfzand PJ (2020) Problems and promise of managed recharge in karstified aquifers: the example of Lebanon. Water Int 45(1):23–38. https://doi.org/10.1080/02508060.2019.1682910
Li J, Chen JJ, Zhan HB, Li MG, **a XH (2020a) Aquifer recharge using a partially penetrating well with clogging-induced permeability reduction. J Hydrol. https://doi.org/10.1016/j.jhydrol.2020.125391
Li LN, **e DL, Wei JC, Yin HY, Li GH, Man XQ, Zhang WJ (2020b) Analysis and control of water inrush under high-pressure and complex karstic water-filling conditions. Environ Earth Sci. https://doi.org/10.1007/s12665-020-09242-6
Li XF, Peng B, Liu Q, Liu JW, Shang LW (2023) Micro and nanobubbles technologies as a new horizon for CO2-EOR and CO2 geological storage techniques: a review. Fuel. https://doi.org/10.1016/j.fuel.2023.127661
Liu QQ, Hanati G, Danierhan S, Zhang Y, Zhang ZP (2021a) Modeling of multiyear water-table fluctuations in response to intermittent artificial recharge. Hydrogeol J 29(7):2397–2410. https://doi.org/10.1007/s10040-021-02388-y
Liu Y, Gao X, Wang ZP, Wang K, Dou XY, Zhu HG, Yuan X, Pan LK (2021b) Controlled synthesis of bismuth oxychloride-carbon nanofiber hybrid materials as highly efficient electrodes for rocking-chair capacitive deionization. Chem Eng J. https://doi.org/10.1016/j.cej.2020.126326
Lu CH, Shi WL, **n P, Wu JC, Werner AD (2017) Replenishing an unconfined coastal aquifer to control seawater intrusion: Injection or infiltration? Water Resour Res 53(6):4775–4786. https://doi.org/10.1002/2016WR019625
Manglik A, Rai SN (2015) Modeling water table fluctuations in anisotropic unconfined aquifer due to time varying recharge from multiple heterogeneous basins and pum** from multiple wells. Water Resour Manag 29(4):1019–1030. https://doi.org/10.1007/s11269-014-0857-y
Mitko K, Turek M (2021) Membrane-based solutions for the Polish coal mining industry. Membranes 11(8):638. https://doi.org/10.3390/membranes11080638
Mugova E, Wolkersdorfer C (2022) Density stratification and double-diffusive convection in mine pools of flooded underground mines—a review. Water Res. https://doi.org/10.1016/j.watres.2021.118033
Nguyen TS, Guglielmi Y, Graupner B, Rutqvist J (2019) Mathematical modelling of fault reactivation induced by water injection. Minerals 9(5):282. https://doi.org/10.3390/min9050282
Pinto PX, Al-Abed SR, Balz DA, Butler BA, Landy RB, Smith SJ (2016) Bench-scale and pilot-scale treatment technologies for the removal of total dissolved solids from coal mine water: a review. Mine Water Environ 35(1):94–112. https://doi.org/10.1007/s10230-015-0351-7
Pu L, **n P, Yu XY, Li L, Barry DA (2021) Temperature of artificial freshwater recharge significantly affects salinity distributions in coastal confined aquifers. Adv Water Resour. https://doi.org/10.1016/j.advwatres.2021.104020
Sanayei HRZ, Javdanian H, Rakhshandehroo GR (2021) Assessment of confined aquifer response to recharge variations and water inflow distributions using analytical approach. Environ Sci Pollut Res 28(36):50878–50889. https://doi.org/10.1007/s11356-021-14314-6
Sendros A, Himi M, Lovera R, Rivero L, Garcia-Artigas R, Urruela A, Casas A (2020) Geophysical characterization of hydraulic properties around a managed aquifer recharge system over the Llobregat River alluvial aquifer (Barcelona metropolitan area). Water. https://doi.org/10.3390/w12123455
Shi TW, Pan YS, Zheng WH, Wang AW (2022) Influence of water injection pressure on methane gas displacement by coal seam water injection. Geofluids. https://doi.org/10.1155/2022/6208933
Spellman P, Breithaupt C, Bremner P, Gulley J, Jenson J, Lander M (2022) Analyzing recharge dynamics and storage in a thick, karstic vadose zone. Water Resour Res. https://doi.org/10.1029/2021WR031704
Sun XL, Yang PT, Zhang ZW (2017) A study of earthquakes induced by water injection in the Changning salt mine area, SW China. J Asian Earth Sci 136:102–109. https://doi.org/10.1016/j.jseaes.2017.01.030
Sun Y, Chen G, Xu Z, Yuan H, Zhang Y, Zhou L, Wang X, Zhang C, Zheng J (2020) Research progress of water environment, treatment and utilization in coal mining areas of China. Meitan Xuebao/ J China Coal Soc 45(1):304–316. https://doi.org/10.13225/j.cnki.jccs.YG19.1654
Sun Y, Zhang L, Xu Z, Chen G, Zhao X, Li X, Gao Y, Zhang S, Zhu L (2022) Multi-field action mechanism and research progress of coal mine water quality formation and evolution. Meitan Xuebao/ J China Coal Soc 47(1):423–437. https://doi.org/10.13225/j.cnki.jccs.YG21.1937
Thiruvenkatachari R, Francis M, Cunnington M, Su S (2016) Application of integrated forward and reverse osmosis for coal mine wastewater desalination. Sep Purif Technol 163:181–188. https://doi.org/10.1016/j.seppur.2016.02.034
van Lopik JH, Hartog N, Schotting RJ (2020) Taking advantage of aquifer heterogeneity in designing construction dewatering systems with partially penetrating recharge wells. Hydrogeol J 28(8):2833–2851. https://doi.org/10.1007/s10040-020-02226-7
Wang JX, Wu YB, Zhang XS, Liu Y, Yang TL, Feng B (2012) Field experiments and numerical simulations of confined aquifer response to multi-cycle recharge-recovery process through a well. J Hydrol 464:328–343. https://doi.org/10.1016/j.jhydrol.2012.07.018
Wang JL, ** MG, Jia BJ, Kang FX (2015) Hydrochemical characteristics and geothermometry applications of thermal groundwater in northern **an, Shandong, China. Geothermics 57:185–195. https://doi.org/10.1016/j.geothermics.2015.07.002
Wang ZW, Chen HW, Li FL, Wang GX (2022) Experimental and simulation study on the impact of storage and recovery of coastal aquifer to seawater intrusion. Nat Hazards 114(1):237–259. https://doi.org/10.1007/s11069-022-05388-7
**ong RH, Chen Q, Liu J, Wei C (2017) Experimental study on seeded precipitation assisted reverse osmosis for industrial wastewater reuse. J Water Process Eng 20:78–83. https://doi.org/10.1016/j.jwpe.2017.10.002
Yajun S, Zhimin X, **n L, Li Z, Ge C, **anming Z, Yating G, Qi L, Shangguo Z, Weijun W, Lulu Z, Sheng W (2021) Mine water drainage pollution in China’s coal mining areas and the construction of prevention and control technical system. Coal Geol Explor 49(5):1–16. https://doi.org/10.3969/j.issn.1001-1986.2021.05.001
Zeng YF, Meng SH, Wu Q, Mei AS, Bu WY (2023) Ecological water security impact of large coal base development and its protection. J Hydrol. https://doi.org/10.1016/j.jhydrol.2023.129319
Zhang ZX, Wang WP (2021) Managing aquifer recharge with multi-source water to realize sustainable management of groundwater resources in **an. China Environ Sci Pollut Res 28(9):10872–10888. https://doi.org/10.1007/s11356-020-11353-3
Zhang YQ, Li MG, Wang JH, Chen JJ, Zhu YF (2017a) Field tests of pum**-recharge technology for deep confined aquifers and its application to a deep excavation. Eng Geol 228:249–259. https://doi.org/10.1016/j.enggeo.2017.08.019
Zhang YQ, Wang JH, Chen JJ, Li MG (2017b) Numerical study on the responses of groundwater and strata to pum** and recharge in a deep confined aquifer. J Hydrol 548:342–352. https://doi.org/10.1016/j.jhydrol.2017.03.018
Zhao HJ, Ma FS, Liu G, Feng XL, Guo J (2018) Analytical investigation of hydraulic fracture-induced seismicity and fault activation. Environ Earth Sci. https://doi.org/10.1007/s12665-018-7708-8
Acknowledgements
This work was funded by the National Key Research and Development Project of China (Grant 2019YFC1805400), the Shandong Energy Group Co., Ltd Key, Science and Technology Project (Grant SNKJ2022A02-R18), the National Science Foundation of Jiangsu Province (Grant BK20210524), and the National Natural Science Foundation (Grant 42202268). We thank the editors and anonymous reviewers for their valuable suggestions.
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Fig. S1.
Water level fluctuation trend in the three complete well pum** tests (DOCX 126 KB)
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Li, X., Chen, G., Wei, W. et al. Feasibility of Injecting Pretreated Mine Water into a Deep Ordovician Aquifer in the Lilou Coal Mine, China. Mine Water Environ 43, 168–182 (2024). https://doi.org/10.1007/s10230-024-00977-3
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DOI: https://doi.org/10.1007/s10230-024-00977-3