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Published byClement Hampton Modified over 9 years ago
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Building Soil Minerals
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EXPECTED ION CORRDINATION
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BOND VALENCE
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Clay Minerals
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BUILDING BLOCKS
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Si 6 O 18
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Tetrahedral Sheet Side View (100) plane Top View (001) plane
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Structural Views: Anion Sheets
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Creating Octahedral Sheets - Filling of Anion Sheets Dioctahedral (trivalent ions) and Trioctahedral (divalent ions)
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(di)OCTAHEDRAL SITE FILLING Anion Sheet with Trivalent (Al 3+ ) Cations
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(di)OCTAHEDRAL SITE FILLING Dioctahedral Sheet Without Basal Hydroxyls
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Octahedral Sheets Trioctahedral (divalent cation) Dioctahedral (trivalent cation) View down [001] axis x y
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Charge Development Isomorphic substitution Terminal (unsatisfied) bonds
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Charge Development Isomorphic Substitution Tetrahedral Sites: Al 3+ for Si 4+ (-) charge Octahedral Sites: Mg 2+ + for Al 3+ (-) charge Al 3+ for Mg 2+ (+) charge
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surface Charge Development Terminal (unsatisfied) bonds - bond valence considerations
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Minerals within Soils
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Rock Entisol Inceptisol Alfisol Ultisol Oxisol Mollisol Vertisol (clay mineralogy) Ideal Weathering Series
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Rock Entisol Inceptisol Alfisol Ultisol Mollisol Oxisol
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Phyllosilicates: Clay Minerals Entisol Inceptisol Alfisol Ultisol Mollisol - Phyllosilicates dominate the clay size particles of most soils
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General Classes (layer build-up) of Phyllosilicate Minerals
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Octahedral Minerals Oct. Brucite, Mg(OH) 2 Gibbsite, Al(OH) 3
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H-bonds 1:1 Phyllosilicates tet oct Sheets } 1:1 layer Kaolinite and Serpentine
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Kaolinite: Al 2 Si 2 O 5 (OH) 4 - dioctahedral, 1:1 mineral
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Sharing of Apical Oxygens in Tetrahdral Sheet with Hydroxyls of Two Octahedral Sheets tet oct tet Talc (2:1 trioctahedral mineral)
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Phlogopite: KMg 3 (AlSi 3 O 10 )(OH) 2 Biotite: KFe 3 (AlSi 3 O 10 )(OH) 2 Muscovite: KAl 2 (AlSi 3 O 10 )(OH) 2 Micas tet oct tet oct tet K+K+ K+K+ K+K+ Unit layer of charge
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K+K+K+K+
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Si 6 O 18 Ditrigonal (hexagonal) Cavity
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Illite (hydrous mica) Vermiculite Smectite Expandable 2:1 Layer Phyllosilicates tet oct tet oct tet K+K+ H2OH2O Ca 2+ H2OH2O H2OH2O Illite: KAl 1.3 Fe 0.4 Mg 0.2 Si 3.4 Al 0.6 O 10 (OH) 2
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Vermiculite dioctahedral: Na x (Al,Fe) 2 (Si 4-x Al x )O 10 (OH) 2 n H 2 O trioctahedral: Na x (Mg,Fe) 3 (Si 4-x Al x )O 10 (OH) 2 n H 2 O Expandable 2:1 Layer Phyllosilicates tet oct tet oct tet K+K+ H2OH2O Ca 2+ H2OH2O H2OH2O
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Expandable 2:1 Layer Phyllosilicates Smectite Dioctahedral Forms: Montmorillonite Na x (Al 2-x Mg x )Si 4 O 10 (OH) 2 Beidellite: Na x (Al 2 )(Al x Si 4-x )O 10 (OH) 2 Trioctahedral Forms: Saponite: Na x-y (Mg 3-y Al y ) 3 (Si 4-x Al x )O 10 (OH) 2 Hectorite: Na x (Mg 3-x Li x ) 3 Si 4 O 10 (OH) 2
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Interlayer Expansion Two Dominant Factors: 1. Structural Charge 2. Interlayer Ion
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[Mg 2 Al 1 (OH ) 6 ]Mg 3 (Si 3 Al)O 10 (OH) 2 2:1:1 Layer Phyllosilicates
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oct (b) 2:1:1 Layer Phyllosilicates Hydroxy Interlayer Vermiculite (HIV) Hydroxy Interlayer Smectite (HIS) - pedogenic chlorites versus true chlorites tet oct tet oct tet [Mg 2 Al 1 (OH ) 6 ]Mg 3 (Si 3 Al)O 10 (OH) 2
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Iron Oxides Aluminum Oxides Manganese Oxides Accessory Minerals
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Andisol - volcanic ash Hydrous Silicates and Aluminosilicates Accessory Minerals
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Hydrous Silicates and Aluminosilicates Accessory Minerals 100 nm
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Identifying Soil Minerals X-ray Diffraction
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Useful (Common) Methods/Approaches Optical Microscopy Infrared Spectroscopy Thermal Analysis X-ray Diffraction (XRD) Physical Properties
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X-ray Diffraction Attributes Limitations
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X-ray Diffraction: Foundation Consider wave properties
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X-ray Diffraction: Foundation Constructive versus Destructive Interference
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X-ray Diffraction: Foundation Bragg’s Law: n = 2d sin d wavelength to 2.5 Å)
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General Classes (layer build-up) of Phyllosilicate Minerals
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Trioctahedral Phyllosilicate Minerals Sheets Octahedral Layer Only: Brucite, Mg(OH) 2 Oct. 1:1 Mineral: Serpentine, Mg 3 Si 2 O 5 (OH) 4 Tet. Oct. Tet. Oct. Tet. 2:1 Mineral: Talc, Mg 3 Si 4 O 10 (OH) 2 Layer Build-up: z y
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MineralMg 2+ K+K+ Glycerol550 C Kaolinite777- Mica10 Vermiculite14101410 Smectite14-1612-141810 HIV14 10-11 HIS14-16141810-11 XRD: Chemical Treatment d-spacing, Angstroms
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Octahedral Minerals Oct. Brucite, Mg(OH) 2 Gibbsite, Al(OH) 3
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Serpentine: Mg 3 Si 2 O 5 (OH) 4 - trioctahedral Kaolinite: Al 2 Si 2 O 5 (OH) 4 - dioctahedral
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Phlogopite: KMg 3 (AlSi 3 O 10 )(OH) 2 Biotite: KFe 3 (AlSi 3 O 10 )(OH) 2 Muscovite: KAl 2 (AlSi 3 O 10 )(OH) 2 Micas tet oct tet oct tet K+K+ K+K+ K+K+
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Illite Vermiculite Smectite Expandable 2:1 Layer Phyllosilicates tet oct tet oct tet K+K+ H2OH2O Ca 2+ H2OH2O H2OH2O
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oct (b) 2:1:1 Layer Phyllosilicates Hydroxy Interlayer Vermiculite (HIV) Hydroxy Interlayer Smectite (HIS) - pedogenic chlorites versus true chlorites tet oct tet oct tet [Mg 2 Al 1 (OH ) 6 ]Mg 3 (Si 3 Al)O 10 (OH) 2
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