Physico-chemical , morphological and mineralogical properties of Bushehr- Borazjan’s soil

Yıl 2015, Cilt: 36 Sayı: 3, 528 - 535, 13.05.2015

Narges Khormouji Ali Abtahi

Öz

Abstract. Formation, classification, morphological, physiochemical, and mineralogical characteristics of Bushehr-Borazjan soil was evaluated. The region soil was of calcic kind. Furthermore; the humidity regime and thermal regime were of Aridic and Hyperthermic respectively. The region is associated with average yearly rain of 234.85 mm. On the other hand, the average yearly temperature is 25.2. As mentioned earlier, the main purpose of this paper is to evaluate physical, chemical, morphological, and mineralogical characteristics of the region soils so that they could be classified; Hence, first , the physiography was determined .Then, several profiles were installed in different physiography units . Next, considering the chosen profiles, the samples are brought to the laboratory for further investigation. Considering the latter sentence, six samples, in hope of mineralogical analysis, were chosen. It is noteworthy that the soil formation, because of hot and dry climate, was weak. Furthermore; the sample pedons were of cambic, calcic, and salic diagnostic horizon. The main two soil order were: Entisol and Aridisol. The known minerals were as follow: Chlorite, Illite, Smectite, Kaolinite, and Polygorskite. Finally, there was a subtle difference between the pedons’ mineral kinds..

Anahtar Kelimeler

Classification, Profile, Bushehr, Aridic, Entisols

Kaynakça

• Bagheri, M. 1387. Applied land evaluation and land use planning. Publications Pelk. First edition.
• Brady, M. N and R.R, Will.1385. Translation Shahuy . The Nature and properties of Soils. Publications University of Kurdistan, First Edition.
• Abtahi,A.1978.Soil and ground water salinity and their relation to physiography.Iran J.Agric.Res. 6:21-32.
• Abtahi,A.1980.Soil genesis as affected by topography and time in highly calcareous parent material under semiarid conditions in Iran.Soil Sci.Sco. Am.J.44:329-336.
• Ramshny, Kh.1371. Climate impact on the formation, development, morphological characteristics, Classification of mineral soil of tropical Kohgiluyeh , Master's thesis, Department of Soil Science, College of Agriculture, Shiraz University.
• Sawhney,J.S.,V.K.V.Verma,B.D.Sharma,and P.K.Sharma. 1992. Pedogenesis in relation to physography in semi-arid condition of Punjab-Indian.Arid Soil Res.6(2):93-103.
• Boul,S.W.,F.D.Hole.,and R.J.Mc Craken.1997.Soil genesis and classification.4th ed.Iowa State Unvi.press,Ames.IA.446pp.
• Miles,J.1985.The pedogenic effects of different soecies and vegetation types and the implications of successions.J.Soil Sci.36:571-584.
• Miller, D. C. and P. W. Birkland. 1992. Soil catena variation along alpine climate transect, northern Peruvian Andes, Geoderma 55: 211-223.
• Rameshni,Kh.,and A. Abtahi. 1995.Effect of climate and topography on the formation of the soils of Kuhgiluye area.4th Congrees of Soil Science.Isfahan University of Technology, (In Persian).
• Soil Survey Staff.1993.Soil Survey Manual U.S.S.A.Handbook. No.18, Washington,D.C., USA.
• Soil Survey Staff.2010.Keys to soil taxonomy.USDA.NRCS.338pp.
• FAO-UNESCO-ISRIC.1988.Soil map of the world.Revised legend reprinted with correction world soil ressources report.No 60,FAO,Rome, 119pp.
• Bouyoucos,C.J.1962.Hydrometer method improved for making particle-size analysis of soils.Agron.J.54:464-465.
• Richards,L.A.(ed).1954.Diagnosis nd improvement of saline and alkaline soils.USDA Hand Book.No .60.US.Government Printing Office, Washingtone,DC.96pp.
• Jackson,M.L.1975.Soil chemical analysis-advanced course .Univ.Wis, Collage Agric,Dept. Soils,Madison,Wiscon-sin.211 pp.
• Kittrick,J.A.,and E.W.Hoppe.1963.A procedure for x-ray diffraction analysis.Soil Sci. 96:312-325.