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Published bySucianty Sugiarto Modified over 6 years ago
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GES166/266, Soil Chemistry Lecture 1, Introduction
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Salt Affected Soils
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Acid Soils
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Saturated Soil (wetland)
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Parent Material ¾¾¾¾¾¾¾® Soil
primary secondary minerals minerals
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Parent Material ¾¾¾¾¾¾¾® Soil
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Entisol - rich in primary mineral relics
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Mollisol - rich in 2:1 phyllosilicate clay minerals and OM
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Vertisol - 2:1 minerals with high shrink-swell
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Alfisol (with a duripan)
- increased weathering but 2:1 minerals still dominate; 1:1 minerals are creeping in, however.
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(California State Soil)
Alfisol (California State Soil) Durixeralf
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Ultisol - 1:1 minerals and ‘oxides’ now are becoming a dominant feature
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Oxisol - Oxides of Al and Fe dominate the soil profile
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Andisol - volcanic ash
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Spodosol - evidence of the role O.M. and climate have on soil development
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Histosol
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EXPECTED ION CORRDINATION
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BOND VALENCE
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BOND VALENCE
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BUILDING BLOCKS
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APICAL TETRAHEDRAL LINKAGE
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BASAL TETRAHEDRAL LINKAGES
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ALTERNATING TETRAHEDRAL LINKAGES
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Si6O18
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Si6O18 Polyhedral View
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CORNER-SHARING OCTAHEDRA
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EDGE-SHARING OCTAHEDRA
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