Abstract
Eighty-seven groundwater samples have been collected from a mountainous region (Alvand, Iran) for hydrochemical investigations to understand the sources of dissolved ions and assess the chemical quality of the groundwater. Most water quality parameters are within World Health Organization acceptable limits set for drinking water. The least mineralized water is found closest to the main recharge zones and the salinity of water increased towards the north of the basin. The most prevalent water type is Ca–HCO3 followed by water types Ca–NO3, Ca–Cl, Ca–SO4 and Mg–HCO3. The Ca–NO3 water type is associated with high nitrate pollution. Agricultural and industrial activities were associated with elevated level of NO −3 . Mineral dissolution/weathering of evaporites dominates the major element hydrochemistry of the area. Chemical properties of groundwater in Alvand region are controlled both by natural geochemical processes and anthropogenic activities.
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Adams S, Tredoux G, Harris C, Titus R, Pietersen K (2001) Hydrochemical characteristics of aquifers near Sutherland in the Western Karoo, South Africa. J Hydrol 241:91–103
Andre L, Franceschi M, Pouchan P, Atteia O (2005) Using geochemical data and modelling to enhance the understanding of groundwater flow in a regional deep aquifer, Aquitaine Basin, south-west of France. J Hydrol 305:40–62
Appelo CAJ, Postma D (1996) Geochemistry, groundwater and pollution. Balkema, Rotterdam, 536 pp
Baharifar A, Moinevaziri H, Bellon H, Pique A (2004) The crystalline complexes of Hamadan (Sanandaj-Sirjan zone, western Iran): metasedimentary Mezoic sequences affected by Late Cretaceous tectono-metamorphic and plutonic events. C R Geosci. 336:1443–1452
Dalai TK, Krishnaswami S, Sarin MM (2002) Barium in the Yamuna River System in the Himalaya: sources, fluxes, and its behavior during weathering and transport .Geochem geophysics geosyst 3. no. 1076
Dixon W, Chiswell B (1992) The use of hydrochemical sections to identify recharge areas and saline intrusions in alluvial aquifers, southeast Queensland, Australia. J Hydrol 130:299–338
Drever JI (1997) The geochemistry of natural waters, 3nd edn. Prentice Hall, New Jersey, 436 pp
Edmunds WM, Cook JM, Darling WG, Kinniburgh DG, Miles DL, Bath AH, Morgan-jones M, Andrews JN (1987) Baseline geochemical conditions in the Chalk aquifer, Berkshire, U. K.: a basis for groundwater quality management. Appl Geochem 2:251–274
Garcia MG, Hidalgo MD, Blessa MA (2001) Geochemistry of groundwater in the alluvial plain of Tucuman province, Argentina. Hydrogeol J 9:597–610
Herczeg A (2001) Can major ion chemistry be used estimate groundwater residence time in basaltic aquifer. In: Cidu R (ed) Proceedings of the 9th international symposium on water–rock interaction. A. A. Balkema, Rotterdam, pp 529–532
Hidalgo MC, Cruz-Sanjulian J (2001) Groundwater composition, hydrochemical evolution and mass transfer in a regional detrital aquifer (Baza basin, southern Spain). Appl Geochem 16:745–758
Hidalgo MC, Cruz-Sanjulian J, Sanroma A (1995) Evolucion geoquimica de las aguas subterraneas en una cuenca sedimentaria semiarida (acuifero de Baza-Caniles, Granada, Espana) . Tierra y Tecnol 20:39–48
Jalali M (2005a) Release kinetics of non-exchangeable potassium in calcareous soils. Commun Soil Sci Plant Anal 36:1903–1917
Jalali M (2005b) Nitrates leaching from agricultural land in Hamadan, western Iran. Agric Ecosyst Environ 110:210–218
Jalali M (2005c) Major ion chemistry in the Bahar area, Hamadan, western Iran. Environ Geol 47:763–772
Jalali M (2005d) A survey on agricultural practices and their effects on the nitrate concentration of the vegetables and soil solution. In: Proceedings of international conference on human impacts on soil quality attributes. Isfahan, Iran
Magaritz M, Nadler A, Koyumdjisky H, Dan N (1981) The use of Na/Cl ratio to trace solute sources in a semiarid zone. Water Resour Res 17:602–608
Marofi S (2003a) Transmissivity estimations in the Gara Chay hydrological basin. 1st Conference on applied environmental geology. (AEG’03)
Marofi S (2003b) Groundwater dynamics in a semi arid region. 1st Conference on Applied Environmental Geology. (AEG’03)
Mathess G (1982) The properties of groundwater. Wiley, New York
McLean W, Jankowski J, Lavitt N (2000) Groundwater quality and sustainability in an alluvial aquifer, Australia. In: Sililo O et al. (eds) Groundwater, past achievements and future challenges. A Balkema, Rotterdam, pp 567–573
Merrikhpour H, Jalali M (2005) Effect of land use of wastewater on movement of some cations and anions through repacked soil columns. In: Proceedings of international conference on human impacts on soil quality attributes. Isfahan, Iran
Meybeck M (1987) Global chemical weathering of surficial rocks estimated from river dissolved loads. Am J Sci 287:401–428
Oren O, Yechieli Y, Bohlke JK, Dody A (2004) Contamination of groundwater under cultivated fields in an arid environment, central Arava Valley, Israel. J Hydrol 290:312–328
Parkhurst DL, Appelo CAJ (1999) User’s guide to PHREEQC (version 2)—a computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations: U.S. Geological Survey Water Resources Investigations Report. 99–4259, 310 p
Plummer L, Busby J, Lee R, Hanshaw B (1990) Geochemical modeling of the Madison aquifer in parts of Montana, Wyoming, and South Dakota. Water Resour Res 26:1981–2014
Rowell DL (1994) Soil science: methods and applications. Longman and Scientific Technical, Harlow 350 pp
Sabziparvar AA (2003) The analysis of aridity and meteorological drought indices in west of Iran. Research report. Bu-Ali Sina University, Hamadan
Sami K (1992) Recharge mechanisms and geochemical processes in a semi-arid sedimentary basin, Eastern cape, South Africa. J Hydrol 139:27–48
Sepahi A (1999) Petrology of the Alvand plutonic complex with special reference on granitoids, PhD thesis, Tarbiat-Moallem University, 348 pp (in Persian)
Sikdar P, Sarkar S, Palchoudhwy S (2001) Geochemical evolution of groundwater in the Quaternary aquifer of Calcutta and Howrah, India. J Asian Earth Sci 19:579–594
Smolders AJP, Hudson-Edwards KA, Van der Velde G, Roelofs JGM (2004) Controls on water chemistry of the Pilcomayo river (Bolivia, South-America). Appl Geochem 19:1745–1758
Stallard RF, Edmond JM (1987) Geochemistry of the Amazon 3. Weathering chemistry and limits to dissolved inputs. J Geophys Res 92:8293–8302
Stimson J, Frape S, Drimmie R, Rudolph D (2001) Isotopic and geochemical evidence of regional-scale anisotropy and interconnetivity of an alluvial fan system, Cochabamba Valey, Bolivia. Appl Geochem 16:1097–1114
Tesoriero AJ, Spruill TB, Eimers JL (2004) Geochemistry of shallow ground water in coastal plain environments in the southeastern United States: implications for aquifer susceptibility. Appl Geochem 19:1471–1482
Todd D (1980) Groundwater hydrology, 2nd edn. Wiley, New York
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Jalali, M. Chemical characteristics of groundwater in parts of mountainous region, Alvand, Hamadan, Iran. Environ Geol 51, 433–446 (2006). https://doi.org/10.1007/s00254-006-0338-6
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DOI: https://doi.org/10.1007/s00254-006-0338-6