HYDROGEOCHEMICAL EVIDENCE OF WATER BRACKISHNESS OF INCHEH WETLAND IN NORTH OF AGH-GHALA, GOLESTAN PROVINCE, IRAN

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RAGHIMI M.; SHAMANIAN GH.H.; SHAKERI ALI REZA; RAHIMI CHAKDEL A.; GHOLIPOUR M.

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Journal: Journal of Agricultural Sciences and Natural Resources Year:2008 | Volume:15 | Issue:2 Page(s): 193-202

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Title

HYDROGEOCHEMICAL EVIDENCE OF WATER BRACKISHNESS OF INCHEH WETLAND IN NORTH OF AGH-GHALA, GOLESTAN PROVINCE, IRAN

Author(s)

Keywords

HYDROGEOCHMISTRYQ2

SALINE WETLANDQ3

SALINE GROUNDWATERSQ3

AGH-GHALAQ2

GOLESTAN PROVINCEQ2

Abstract

Salinization is the whereby the concentration of dissolved salts in water and soil is increased due to natural or human-induced processes. Salinity has been increased in groundwater flow directions and low land area. In this study, hydrogeochemical quality of Incheh wetland in north of AGH-GHALA and certain shallow groundwater wells in western part of the incheh wetland with collection of water samples in winter (2005) have been carried out. Hydrogeochemistry results indicate that high salinity of this wetland and shallow groundwaters wells with total dissolved solids more than>1000 mg/l. According to the Gibbs and Chadha diagrams, evaporation is dominant phenomena responsible for the high ionic concentrations found in wetland and shallow ground waters. A high content of Na+ and Cl ions in SALINE WETLAND and shallow groundwater wells in comparison with those of river water, suggests a evaporitic origin of wetland and groundwaters. The high positive correlation between of K+ and Na+ indicates that the present evaporitic salts in saline soils are the main source of these ions. On the basis of Piper diagram which shows that the hydrochemical facies in SALINE WETLAND is dominated by sodic and chloride (Na+-Cl-) types. The Hydrochemical model reveals that aragonite, dolomite and calcite are saturated while evaporated mineral. Halite in this season is undersaturated.

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APA: Copy

RAGHIMI, M., SHAMANIAN, GH.H., SHAKERI, ALI REZA, RAHIMI CHAKDEL, A., & GHOLIPOUR, M.. (2008). HYDROGEOCHEMICAL EVIDENCE OF WATER BRACKISHNESS OF INCHEH WETLAND IN NORTH OF AGH-GHALA, GOLESTAN PROVINCE, IRAN. JOURNAL OF AGRICULTURAL SCIENCES AND NATURAL RESOURCES, 15(2), 193-202. SID. https://sid.ir/paper/9649/en

Vancouver: Copy

RAGHIMI M., SHAMANIAN GH.H., SHAKERI ALI REZA, RAHIMI CHAKDEL A., GHOLIPOUR M.. HYDROGEOCHEMICAL EVIDENCE OF WATER BRACKISHNESS OF INCHEH WETLAND IN NORTH OF AGH-GHALA, GOLESTAN PROVINCE, IRAN. JOURNAL OF AGRICULTURAL SCIENCES AND NATURAL RESOURCES[Internet]. 2008;15(2):193-202. Available from: https://sid.ir/paper/9649/en

IEEE: Copy

M. RAGHIMI, GH.H. SHAMANIAN, ALI REZA SHAKERI, A. RAHIMI CHAKDEL, and M. GHOLIPOUR, “HYDROGEOCHEMICAL EVIDENCE OF WATER BRACKISHNESS OF INCHEH WETLAND IN NORTH OF AGH-GHALA, GOLESTAN PROVINCE, IRAN,” JOURNAL OF AGRICULTURAL SCIENCES AND NATURAL RESOURCES, vol. 15, no. 2, pp. 193–202, 2008, [Online]. Available: https://sid.ir/paper/9649/en

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