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This article in SSSAJ

  1. Vol. 47 No. 1, p. 149-157
     
    Received: July 30, 1981
    Accepted: Sept 21, 1982


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doi:10.2136/sssaj1983.03615995004700010030x

Mineralogy of Saudi Arabian Soils: Central Alluvial Basins1

  1. B. E. Viani2,
  2. A. S. Al-Mashhady3 and
  3. J. B. Dixon2

Abstract

Abstract

These investigations were conducted to provide basic soil chemical, physical, and mineralogical data for an area of Saudi Arabia that had not been studied and for which greatly increased agricultural development is anticipated. Fourteen soils were collected from two arid interior basin areas of Saudi Arabia. The silt and clay mineralogy was studied using x-ray diffraction, differential thermal analysis, and electron microscopy. Quantitative estimation of clay-sized minerals was based on a combination of chemical and x-ray diffraction techniques. The calcareous soils of the central basins show minimal profile development. Particle-size classes range from sandy-skeletal to fine silty. Soils with shallow water tables are saline with large SAR values. The clay minerals in soils of the basins are primarily inherited. Soils developed in alluvium from mixed igneous rocks have clay fractions in which smectite > mica > kaolinite > chlorite, palygorskite, vermiculite. Soils formed from Permian sedimentary rocks have kaolinitic clay fractions. It is postulated that the central basins do not receive sufficient Si inputs for palygorskite neoformation and it is though that palygorskite is detrital, originating from easternregion Tertiary rocks. The soil clays of the central hasins have greater smectite contents than those of the kaolinitic western highland soils and palygorskite-rich eastern-region soils.

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