تعداد نشریات | 161 |
تعداد شمارهها | 6,533 |
تعداد مقالات | 70,506 |
تعداد مشاهده مقاله | 124,124,998 |
تعداد دریافت فایل اصل مقاله | 97,233,502 |
Mineralogical and physico-chemical characterization of gypsiferous semi-arid soils in the north of Urmia, Iran | ||
Desert | ||
دوره 26، شماره 1، شهریور 2021، صفحه 1-15 اصل مقاله (1.15 M) | ||
نوع مقاله: Research Paper | ||
شناسه دیجیتال (DOI): 10.22059/jdesert.2019.279895.1006714 | ||
نویسندگان | ||
L. Pashei1؛ Sh. Manafi* 2 | ||
1Urmia University | ||
2Assistant Professor of Soil Science, Department of soil science, Faculty of agriculture, University of Urmia, Urmia, Iran | ||
چکیده | ||
Gypsiferous soils contain sufficient gypsum to influence soil physico-chemical, mineralogical, mechanical properties and geotechnical conditions and as a consequence, affect plant growth and crop production. So physico-chemical and mineralogical properties of 6 soil profiles located on the gypsiferous parent material with semi-arid climate in north of Urmia, West Azerbaijan province, Iran, were investigated. Based on standard methods, morphological, physico-chemical and mineralogical properties of these soils were determined. Soils with higher gypsum content had lighter color, lighter texture, lower values of organic carbon and cation exchange capacity and higher values of electrical conductivity. These parameters were reversely changed with decreasing gypsum content of soils. Semi-quantitative analysis of clay minerals indicated the presence of smectite, illite, chlorite, kaolinite and palygorskite were as major clay minerals with decreasing order from smectite to palygorskite. The origin of illite, chlorite and kaolinite were related to the inheritance from parent material. Smectite group of clay minerals has been resulted from three origins of inheritance from parent material, transformation of illite and palygorskite and neoformation, but the transformation and neoformation are the main pathways for its formation. Palygorskite has pedogenic origin and has been formed via neoformation. The comparison of clay mineralogy of soils with different gypsum values revealed the presence of higher smectites in soils with higher gypsum. Palygorskite was identified just in soils with higher gypsum. In soils with lower values of gypsum, illite and chlorite were the predominant clay minerals and palygorskite did not identified. | ||
کلیدواژهها | ||
clay mineralogy؛ gypsum؛ neoformation؛ palygorskite؛ smectite؛ transformation | ||
مراجع | ||
References Abbaslou H, Abtahi A. 2007. Origin and distribution of clay minerals in calcareous, gypsiferous, saline soils and sediments of Bakhtegan Lake Bank, Southern Iran. Iran Agricultural Research, 26(1-2): 71- 86. Ahmed KI. 2013. Effect of gypsum on the hydro-mechanical characteristics of partially saturated sandy soil. PhD thesis, College of Physical Sciences and Engineering Cardiff University, Cardiff, Australia, 302p. Al- Saoudi NKS, Al- Khafaji AN, Al- Mosawi MJ. 2013. Challenging Problems of Gypseous Soils in Iraq. In: Delage, P., J. Desrues, F. Roger, (Eds.). Challenges and innovations in geotechnics. Proceedings of the 18th International Conference on Soil Mechanics and Geotechnical Engineering, 2-6 September, Paris. France. pp. 479-482. Al-Barrak K, Rowell DL. 2006. The solubility of gypsum in calcareous soils. Geoderma, 136: 830– 837. Al-Dabbas MA, Schanz T, Yassen M.J. 2010. Comparison of gypsiferous soils in Samarra and Karbala areas, Iraq. Iraqi Bulletin of Geology and Mining, 6(2): 115- 126. Azeez SN, Rahimi I. 2017. Distribution of gypsiferous soil using geoinformatics techniques for some aridisols in garmian, Kurdistan region-Iraq. Kurdistan Journal of Applied Research, 2(1): 57-64. Azizi P, Mahmoodi Sh, Torabi H, Masihabadi M.H, Homaee M. 2011. Morphological, physico- chemical and clay mineralogy investigation on gypsiferous soils in southern of Tehran, Iran. Middle- East Journal of Scientific Research, 7 (2): 153-161. Barzanji AF. 1973. Gypsiferous soils of Iraq. Ph.D. Thesis, University of Ghent, Ghent, Belgium. Bhattacharyya T, Ray S.K, Chandran P, Karthikeyan K, Pal D.K. 2018. Soil quality and fibrous mineral in black soils of Maharashtra. Current science, 115(3): 482-492. Boettinger JL, Southard R.J. 1995. Phyllosilicate distribution and origin in Aridisols on a granitic pediment, Western Mojave Desert. Soil Science Society of American Journal, 59: 1189-1198. Borchardt G. 1989. Smectites. In: Dixon, J.B., S.B. Weed, (Eds.). 1989. Minerals in soil environment. 2nded. Number I in the SSSA book series. Published by SSSA. Madison. Wisconsin. USA. pp. 675- 729. Bouza PJ, Simon MJ, Aguilar H, Rostagno M. 2007. Fibrous clay mineral formation and soil evolution in Aridisols of northeastern Patagonia, Argentina. Geoderma, 139: 38-50. 15 Pashaei and Manafi Buringh P. 1960. Soils and soil conditions in Iraq. Ministry of Agriculture, Iraq. 322p. Chiquoine LP. 2012. Restoration of biological soil crust on disturbed gypsiferous soils in Lake Mead National Recreation area, eastern Mojave Desert. M.Sc. thesis, University of Nevada, Las Vegas, USA. Churchman GJ, Lowe DJ. 2012. Alteration, formation, and occurrence of minerals in soils. In: Huang, P.M., Y. Li, M.E. Sumner, Handbook of Soil Science: Properties and Processes. CRC Press, Boca Raton, FL, USA; p. 1–72. Farpoor MH, Khademi H, Eghbal MK. 2005. Genesis of selected gypsiferous soils in southeast Iran. In: Afyuni, M. (Ed.). Proceedings of international conference on human impacts on soil quality attributes. Sept. 12-16, 2005. Isfahan. Iran. pp. 126-131. Galan E, Singer A. 2011. Developments in palygorskite- sepiolite research. A new outlook on these nanoparticles. Developments in clay science. Elsevier. 520p. Gee GW, Bauder JW. 1986. Particle Size Analysis, Hydrometer Method. Part I. In: Klute, A. (Ed.). Methods of Soil Analysis. American Society of Agronomy, Madison, WI. pp. 404-408. Golyeva A, Khokhlova O, Lebedeva M, Shcherbakov N, Shuteleva I. 2018. Micromorphological and chemical features of soils as evidence of Bronze Age ancient anthropogenic impact (late Bronze Age muradymovo settlement, Ural Region, Russia). Geosciences, 8(9), 313: 1-12. Grobler L. 2002. The nature of precipitated gypsum in a soil irrigated with gypsiferous water. M.Sc. thesis, Department of soil science, University of Pretoria, Pretoria, South Africa. Hashemi SS, Baghernejad M, Najafi Ghiri M. 2013. Clay mineralogy of gypsiferous soils under different soil moisture regimes in Fars Province, Iran. Journal of Agricultural Science and Technology, 15: 1053-1068.Hesse, P.R., 1974. Methods of soil analysis- texture analysis of gypsic soils. The Euphrates pilot irrigation project, FAO. Report number 67, 522 p. Jackson ML. 1975. Soil Chemical Analysis. Advanced Course University of Wisconsin, College of Agriculture, Department of Soils, Madison, WI. 894 pp. Johns WD, Grim R.E, Bradley F. 1954. Quantitative estimation of clay minerals by diffraction methods. Journal of Sedimentary Petrology, 24(4): 242-251. Khademi H, Mermut AR. 1998. Source of palygorskite in gypsiferous Aridisols and associated sediments from central Iran. Clay Minerals, 33: 561-575. Khechai S, Daoud Y. 2016. Characterization and origin of gypsum rhizoliths of Ziban Oases Soil- Algeria. World Applied Sciences Journal, 34 (7): 948-955. Kijjanapanich P. 2014. Sulfate reduction for remediation of gypsiferous soils and solid wastes. Ph.D. Thesis, Erasmus Joint doctorate program in Environmental Technology for Contaminated Solids, Soils and Sediments (ETeCoS3). 150p. Kittrick JA, Hope EW. 1963. A procedure for the particle size separation of soils for X-Ray diffraction analysis. Soil Science Society of American Journal, 96: 312-325. Mahmoodi Sh. 1994. Properties and management of gypsiferous soils. In: Jalalian, A. (Ed.). Proceedings of 4th Soil Science Congress of Iran, Isfahan University of Technology, 29- 31 Aug. Isfahan, Iran. pp. 59-65. Manafi Sh. 2010. Mineralogical Evidence of Climate Change in some Semiarid Soils of Southern Urmia, Iran. Soil Science, Agrochemistry and Ecology, 4: 17-24. Mashali AM. 1996. Soil management practice for gypsiferous soils. In: Poch, M. (Ed.). Proceedings of the International Symposium on Soil with Gypsum. Lleida, Catalonia, Spain. pp. 34-52. Mehra OP, Jackson ML. 1960. Iron oxide removal from soils and clays by a dithionite citrate system with sodium bicarbonate. Clays and Clay Minerals, 7: 317-327. Omran E. 2012. A neural network model for mapping and predicting unconventional soils at a regional level. Applied Remote Sensing Journal, 2(2): 35-44. Owliaie HR, Najafi Ghiri M, Shakeri S. 2018. Soil-landscape relationship as indicated by pedogenesis data on selected soils from Southwestern, Iran. Eurasian Journal of Soil Science, 7(2): 167–180. Perkins D. 2002. Mineralogy. 2nd ed. Prentice Hall. New Jersey. 483p. DESERT2021, 26(1):1-15 16 Shahid ShA, Abdel Fattah MA. 2009. Gypsum polymorphism in the desert environment of Abu Dhabi Emirate. European Journal of Scientific Research; 29(2): 237-248. Singer A. 2002. Palygorskite and sepiolite. In: Dixon, J.B., D.G. Schulze, (Eds.). Soil Mineralogy with Environmental Applications, SSSA Book Series, Soil Science Society of America, Madison, WI, Vol. 7, pp. 555–583. Soil Survey Staff, 2012. Field Book for Describing and Sampling Soils. National Soil Survey Center. Natural Resources Conservation Service. U.S. Department of Agriculture. Version 3.0, 315p. Soil survey staff, 2014. Keys to soil taxonomy. 12th edition. USDA.NRCS. 346p. Soltani Sisi G. 2005. Geological map of Iran, 1:100000 series, sheet No, 5065. Geological survey and mineral Exploration of Iran. Stoops G, Ilaiwi M. 1981. Gypsum in arid soils morphology and genesis. In: Beinroth, F.H., A. Osman, (Eds.). Proceeding of the third international soil classification workshop. Arab Center for the studies of Arid Zones and Dry lands. Damascus, Syria. pp: 175-185. Sumner ME, Miller WP. 1996. Cation Exchange Capacity and Exchange Coefficients. In: Sparks, D.L. (Ed.), Methods of Soil Analysis Part 3: Chemical Methods, SSSA Book Series 5, Soil Science Society of America. Madison, Wisconsin. pp. 1201-1230. USDA-NRCS, 2004. Soil Survey Laboratory Methods Manual. Soil survey investigations. Report No, 42. Version 3, 693p. Van Alphen JG, Romero F. 1971. Gypsiferous soils. Notes on their characteristics and management. International Institute for Land Reclamation and Improvement. Bulletin number: 12. 44p. Verheye WH, Boyadgiev TG. 1997. Evaluating the land use potential of gypsiferous soils from field pedogenic characteristics. Soil Use and Management, 13:97-103. Wilson MJ. 1999. The origin and formation of clay minerals in soils: past, present and future perspectives. Clay Minerals, 34: 7-24. | ||
آمار تعداد مشاهده مقاله: 386 تعداد دریافت فایل اصل مقاله: 572 |