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Genesis and Micromorphology of Gypsum on Loess-Derived Soils in Northern Iran

机译:伊朗北部黄土源性土壤上石膏的成因与微观形态

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Gypsum is the most common sulfate mineral in soils of arid and semi-arid regions. Two hundred million hectares of the earth’s surface and about 28 million hectares of Iranian arid soils are covered by gypsiferous soils. The studied soils consist of alluvial plane and eolian plains in northern Iran. Soils were classified as Haplocambids, Aquisalids and Endoaquepts. In this study, genesis, formation and development of gypsum in soils were investigated. Study area includes different geomorphic surfaces from the upper watershed to alluvial plains. Gypsum crystals without considering their size, shape, arrangement are determined as pedogenic. In the weakly-developed horizons, in aridic moisture regimes, formation of euhedral pedogenic gypsum crystals and incomplete infilling of voids was dominant. In the well-developed soils, in xeric moisture regime, gypsum crystals are oriented and the perpendicular in arrangement of crystals along pores is dominants. Gypsum crystals occur in different shapes such as lenticular, tabular, and rosette-like and fan arrangement. Origin of gypsum in weakly-developed soils was weathered gypsiferous marls in upper Atrak basin. The source of gypsum in the soils with shallow ground water is high content of sulfate dissolved in soil solutions. In horizons affected by fluctuation of ground water contaning sulphur, euhedral tabular shape is dominant. In well-developed soils, based on Snowball morphology, gypsum is classified as stage II nodule. Results showed that there is no relationship between formation of the snowball morphology, b-fabric and kind of diagnostic horizons (A, B and C). Keywords: Micromorphology, Pedogenic gypsum, Loess, Northern Iran. Full-Text Type of Study: Research | Subject: Ggeneral Received: 2010/09/20 Related Websites Scientific Publications Commission - Health Ministry Scientific Publications Commission - Science Ministry Yektaweb Company Site Keywords ?????, Academic Journal, Scientific Article, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ?? Vote ? 2015 All Rights Reserved | JWSS - Isfahan University of Technology
机译:石膏是干旱和半干旱地区土壤中最常见的硫酸盐矿物。石膏状土壤覆盖了地球两亿公顷的表面和约2800万公顷的伊朗干旱土壤。研究的土壤包括伊朗北部的冲积层和风积平原。土壤被分类为单节生类,潮生类和内生类。在这项研究中,研究了石膏在土壤中的发生,形成和发展。研究区域包括从上流域到冲积平原的不同地貌表面。不考虑其大小,形状,排列的石膏晶体被定为成岩作用。在较弱的地层中,在干旱的水分条件下,主要是形成了浅水成土的石膏石膏晶体和空隙的不完全填充。在发达的土壤中,在干湿条件下,石膏晶体是定向的,且晶体沿孔隙的垂直排列是主要的。石膏晶体以不同的形状出现,例如透镜状,板状,玫瑰花状和扇形排列。欠发达土壤中的石膏起源是上阿特拉克盆地的风化石膏灰泥。地下水浅的土壤中石膏的来源是溶解在土壤溶液中的硫酸盐含量高。在受地下水含硫量波动影响的地层中,平整的板状形状占主导地位。在发达的土壤中,根据雪球形态,石膏被归为II期结核。结果表明,雪球形态的形成,b纤维与诊断层的种类(A,B和C)之间没有关系。关键词:微观形态,成岩石膏,黄土,伊朗北部。全文研究类型:研究|主题:一般收稿时间:2010/09/20相关网站科学出版物委员会-卫生部科学出版物委员会-科学部Yektaweb公司网站关键字??????,Academic Journal,Scientific Article,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ??投票吗? 2015版权所有| JWSS-伊斯法罕工业大学

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