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-
charge
-
hydration
-
bonding
作者:
Sebastian Birch Schmidt
10 月以前
77
Halides
The discussion revolves around the properties and behaviors of various minerals and their interactions with cations, particularly focusing on the differences in ion sizes such as Al+3 and Fe+.
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aluminium-oxides
Iron-Oxides
Goethite
Gibbsite
pH-levels
releasing vs apsorption of H+
OH-groups
Ph-dependent charge
CEC
resistent to hydration
octhedral in interlayergap
Expansion when heated
Presence of water and cations in interlayer gap
surface area: Fixed vs interlaygap
Effective charge
Negative permanent charge
Isomorphous sub
Divalent vs trivalent cation
Swelling from hydration
Strength of intermolecular bonding
Framework silicates (3D)
Layer silicates (Micas)
Evaporites
2:1:1 Layer
Chlorite
2:1 layer
Illite
Smectite
vermiculite
1:1 layer
Kaolinite
OH-groups(octahedral) and O^-2 group (tetrahedral)
Hydrogen vs vanderwalls
K+ in the interlayer gap
Na-feldspar
K-feldspar
Tetrahedral
Oxides
single chain (pyroxenes)
Double chain (amphiboles
single, non polymer silcate (olivines)
polymer structure
Octahedral
need for extra cations to negate the charge
Feldspar
Low-level
Low negative permanent charge
Difference in Al+3 and Fe+ ion size
Sulfides
native elements
Phosphates
Sulfates
silicates
Carbonates
-4 charge from oxygen pr. cation
Isomorphous sub Si+4 -> Al3+
Quartz
Clay
Halides