Challenges in Strip Mining of Sodium Sulfate Sedimentary Reserves in Mighan Playa, Arak: Environmental Impacts and Engineering Solutions | ||
| Journal of Mining and Environment | ||
| مقاله 12، دوره 17، شماره 3، مرداد و شهریور 2026، صفحه 993-1013 اصل مقاله (10.77 M) | ||
| نوع مقاله: Original Research Paper | ||
| شناسه دیجیتال (DOI): 10.22044/jme.2025.15633.3001 | ||
| نویسندگان | ||
| Abolfazl Shafaei؛ Abdolmotaleb Hajati؛ Feridon Ghadimi* | ||
| Department of Mining Engineering, Arak University of Technology, Arak, Iran | ||
| چکیده | ||
| This work investigates the extraction of sodium sulfate (Na2SO4) from Mighan Playa in Arak, Iran, where 163 boreholes were drilled to depths of up to 20 m revealed a heterogeneous lithology dominated by Glauberite (Na2Ca(SO4)2) and Mirabilite (Na2SO4·10H2O) with average sodium sulfate concentrations of 25% (ranging from 2–32% and peaking at 55% in localized southwestern areas). The playa’s surface is primarily clay-covered (94%) and interbedded with evaporitic facies including Gypsum, Halite, and carbonate minerals. Seasonal water inflows of 200–800 l/s from a wastewater treatment plant, together with 3.5 m-deep extraction pits and gravitational drainage, have resulted in stagnant ponds over 25% of the southern lake area and an annual reduction in surface area of 5–10%. Stratigraphic analysis further indicates pure Glauberite layers (0.5–1 m thick) at depths of 1,653–1,656 m, in contrast with thicker impure Glauberite-Mirabilite sequences (up to 9 m) present between 1,649–1,659 m. To mitigate these challenges, an integrated engineering approach is proposed that includes pumping seepage brine (with a moisture content of 40%) to solar evaporation pools, employing continuous dual-pump slurry systems for tailings management, and implementing hydraulic balancing through retaining walls and winter brine reserves—measures that enhance extraction efficiency by 30–42% in high-concentration zones. These adaptive mining practices, incorporating in-situ brine leaching and advanced wastewater treatment, are designed to meet 70% of Iran’s annual sodium sulfate demand from an 8 km² operational area while reducing environmental degradation. | ||
| کلیدواژهها | ||
| Sedimentary facies؛ Glauberite-mirablite؛ sodium sulfate؛ Extraction ponds؛ Arak Mighan saline Lake | ||
| مراجع | ||
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[1]. Vallati, M., Tomás, S., Galli, C., Winter Leitner, G., & Mutti, M. (2023). Depositional controls in an ancient, closed lake system: A high-resolution and multi-scalar case study from the Yacoraite Formation (Salta Basin, Argentina). Sedimentary Geology, 454,106456.
[2]. Jiménez-Bonilla, A., Rodríguez-Rodríguez, M., Yanes, J.L., & Gázquez, F. (2023). Hydrological modeling and evolution of lakes and playa-lakes in southern Spain constrained by geology, human management, and climate change. Science of Total Environment, 905,167183.
[3]. Sheibani, S., Ataie-Ashtiani, B., Safaie, A., & Hosseini, S.M. (2023). Coupled water and salt balance models for Lake Urmia: Salt precipitation and dissolution effects. Journal of Great Lakes Research, 49 (3), 581-595.
[4]. Kendall, A.C. (1992). Evaporites, in R. G. Walker, and N. P. James, eds., Facies Models: Responses to sea level change. Geological Association of Canada, pp 375–409.
[5]. Noble, R.R.R., Gray, D.I., & Reid, N. (2011). Regional exploration for channel and playa uranium deposits in Western Australia using groundwater. Applied Geochemistry, 26(12), 1956-1974.
[6]. Chong Oh, H., Koibuchi, Y., & Isobe, M. (2024). Changes in sedimentary environments in Shihwa Lake, Korea. Environment Advances, 16, 100544.
[7]. Ma, L., Lowenstein, T. K., Li, B., Jiang, P., Liu, C., Zhong, J., Sheng, J., Qiu, H., & Wu, H. (2010). Hydrochemical characteristics and brine evolution paths of Lop nor Basin, Xinjiang Province, Western China. Applied Geochemistry, 25 )11(, 1770-1782.
[8]. Gu, A., & Eastoe, C.J. (2021). The Origins of Sulfate in Cenozoic non-Marine evaporites in the Basin and-Range Province, Southwestern North America. Geoscience, 11, 455. https://doi.org/10.3390/geosciences11110455
[9]. Eugster, H.P., & Hardie, L.A. (1978). Saline lakes. In Lerman A (ed). Lakes Chemical Geology Physics, pp 237-239.
[10]. Kipnis, E.L., Bowen, B.B., Hutchings, S.J., Hynek, S.A.A., & Benison, C. (2020). Major ion geochemistry in Na-Ca-Mg-K-Cl-SO4 brines using portable X-ray fluorescence spectrometry. Chememistry Geology, 558, 119865.
[11]. Erfanian Kaseb, H., Torshizian, H.H., Jahani, D., Javanbakht, M., & Kohansal Ghadimvand, N. (2020). Studying evolutionary processes of petergan playa brines in south Khorasan, east of Iran. Geopersia, 10 (2), 333-349.
[12]. Raudsepp, M.J., Wilson, S., Zeyen, N., Arizaleta, M.L., & Power L.M. (2024). Formation of carbonates in the alkaline lakes and playas of the Cariboo Plateau, British Columbia, Canada. Chemical Geology, 648, 121951.
[13]. Alkhayer, M., Karimian Eghbal, M., Hamzehpour, N., & Rahnemaie, R. (2023). Brine geochemical changes and salt crust evolution of Lake Urmia in Iran. Catena, 231, 107310.
[14]. Ren, X., Yu, R., Kang, J., Wang, R., Li, X., Wang, D., & Zhang, P. (2024). Unraveling the sources of organic matter in suspended particulates and sediment in a closed inland lake using stable isotope fingerprinting. International Journal of Sediment Research, 9(3), 421-434.
[15]. Barouillet, C., Laird, K.R., Cumming, B.F., Finney, B.P., & Selbie, D.T. (2024). Assessment of anthropogenic impacts on the trophic dynamics of Babine Lake: Implications for the production of sockeye salmon. Journal of Great Lakes Research, 50 (5), 102395.
[16]. Han, L., Liu, D., Cheng, G., Zhang, G., Wang, L. (2019). Spatial distribution and genesis of salt on the saline playa at Qehan Lake, Inner Mongolia, China. Catena, 177, 23-35.
[17]. Li, R., Liu, C., Xu, H., Jiao, P., Hu, Y., Fan, L., & Sun, X. (2020). Genesis of glauberite sedimentation in Lop Nur Salt Lake - Constraints from thermodynamic simulation of the shallow groundwater in the Tarim River Basin, China. Chemical Geology, 537,119461.
[18]. Marazuela, M.A., Vázquez-Suñé, E., Ayora, C., & García-Gil, A. (2020). Toward more sustainable brine extraction in salt flats: Learning from the Salar de Atacama. Science of the Total Environment, 703, 135605.
[19]. Bhadrachari, G., Ahmad, M., Alambi, R.K., Thomas, R.K. (2023). Extraction of commercially valuable mineral salt from reverse osmosis brine using a spray dry process. Environment Engineering Research, 28(4), 220299.
[20]. Warren, K.J. (2016). Evaporates, A geological compendium, second edition, Springer Cham Heidelberg New York Dordrecht London, P. 1813. https://lib.ugent.be/catalog/ebk01:3710000000685914
[21]. Ghadimi, F., Hajati, A., & Sabzian, A. (2020). Assessment of Heavy Metal Contamination in Waters due to Mineral Salts Company from Mighan playa/lake, Arak, Iran. Journal of Mining Environment, 11 (1), 171-184.
[22]. Ghadimi, F. (2014). Assessment of the sources of chemical elements in sediment from Arak Mighan Lake. International Journal of Sediment Research, 29.159-170.
[23]. Ghadimi, F., Hajati, A., & Sabzian, A. (2021). The role of Mineral Salts Company in pollution of Mighan playa sediments with heavy metals by contamination indices and multivariate analysis methods, Arak, Iran. International Journal of mining and Geo-Engineering, 55(2), 117-124.
[24]. Ghadimi, F., & Ghomi, M. (2013). Geochemical and sedimentary changes of the Mighan playa in Arak, Iran. Iranian Journal of Earth Science, 5, 25-32.
[25]. Rahimpour-Bonab, H., & Abdi, L. (2012). Sedimentology and origin of Meyghan Lake/playa deposits in Sanandaj–Sirjan zone, Iran. Carbonates and Evaporites, 27, 375–393.
[26]. Castañeda, C., Herrero, J., & Casterad, A. M. (2005). Facies identification within the playa-lakes of the Monegros desert, Spain, from field and satellite data. Catena, 63(1), 39-63.
[27]. Vera, M.L., Torres, W.R., Galli, C.L., Chagenes, A., & Flexer, V. (2023). Environmental impact of direct lithium extraction from brines. National Review Earth Environment, 4, 149–165.
[28]. Pazand, K., Behzadinasab, A., Ghaderi, M.R., Rezvanianzadeh, M.R. (2018). The sediments of Dagh-e-Sorkh playa, Ardestan, central Iran. Carbonates and Evaporites, 33, 55-64.
[29]. Kuscu, M., Ener, S., Başpınar, E. (2017). Recharge sources and hydrogeochemical evaluations of Na2SO4 deposits in the Acıgöl Lake (Denizli, Turkey). Journal of African Earth Science.
[30]. Kumar, M., Rajesh Kumar, R., Kumar Singh, C., & Kumar, A. (2024). Identification of Playa Lakes and tracking their evolution pathways using geochemical models in the Great Indian Thar desert. Science of Total Environment, 912, 169250.
[31]. Fooladi, M., Ghadimi, F., Sheikh Zakariaee, S.J., & Rahimpour Bonab, H. (2021). Influence of Physical and Chemical Material Properties on Mining Soil Erosion Processes Around Mineral Salts Company in Mighan playa, Arak, Iran. Journal of Mining Environment, 12(3), 725-741.
[32]. Coetsiers, M., Walraevens, K. (2006). Chemical characterization of the Neogene aquifer, Belgium. Hydrogeology Journal, 14, 1556-1568.
[33]. Stober, I., Zhong, J., & Bucher, K. (2023). From freshwater inflows to salt lakes and salt deposits in the Qaidam Basin, W China. Swiss Journal of Geoscience, 116 (5).
[34]. Nasri, N., Ahmed, R., & Bouhlila, R. (2022). Hydrogeochemical characteristics and sources of mirabilite in the high saline system of Sabkha Oum El Khialate, Southern Tunisia. Applied Geochemistry, 143, 105294. https://doi.org/10.1016/j.apgeochem.2022.105294.
[35]. Krinsley, D. B. (1970). A geomorphological and paleoclimatological study of the playas of Iran. United States Geological Survey, U.S. Department of Interior, Washington D.C., p 486.
[36]. Krinsley, D.B. (1972). Dynamic processes in the morphogenesis of salt crusts within the Great Kavir, north-central Iran. In: Proceedings of 24th International Geological Congress, Montreat, 167–174.
[37]. Hajati, A., & Usefirad, M. (2019). Optimizing the method of extracting sodium sulfate by observing the balance of the hydrogeological regime and environmental considerations of Mighan Arak playa, Industrial report of Arak University of Technology and Amlah Iran Mining Company. | ||
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