1 Carbonates and Bicarbonates GLY 4200 Lab 8 - Fall, 2012.
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Transcript of 1 Carbonates and Bicarbonates GLY 4200 Lab 8 - Fall, 2012.
![Page 1: 1 Carbonates and Bicarbonates GLY 4200 Lab 8 - Fall, 2012.](https://reader036.fdocuments.in/reader036/viewer/2022083005/56649f255503460f94c3c5f5/html5/thumbnails/1.jpg)
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Carbonates and Bicarbonates
GLY 4200
Lab 8 - Fall, 2012
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Carbonate Stability
• Carbonates are minerals consisting of metallic elements bonded to the carbonate group, CO3
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• Although anionic groups are usually stable, one exception to this is the reaction of a carbonate with acid:
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Fizz
• The carbon dioxide is a gas and bubbles (or "fizzes") off
• This provides a good qualitative test for the presence of carbonate minerals in most samples
• Most carbonate minerals will fizz when a small (!) drop of acid is placed on the mineral
• However, it may be necessary to listen for the fizz and a few minerals react so slowly that the reaction is not detectable
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Hydrous Carbonates
• Hydrous carbonates are often soluble in water
• Hydrous carbonates are frequently weathering products
• Some, like azurite and malachite, are indicator minerals for possible ore deposits
• Both are idiochromatic
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Azurite
• Azurite = Deep blue
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Malachite
• Malachite = green• Secondary mineral in
the oxidized zones of copper ore deposits
• This picture shows a botryoidal specimen
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Botryoidal
• From the Greek botrys, meaning bunch or cluster of grapes
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Banding in Malachite
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Calcite Group
• Consists of divalent cations bonded to the carbonate anionic group
• Structure is a distorted NaCl type, compressed along a three-fold axis, and CN = VI
• All members of the calcite group belong to class bar3 2/m
• Cations and carbonate anionic groups form alternate layers
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Dolomite Group
• The dolomite group is similar to calcite except that two distinct divalent cations are present in the structure
• These cations occupy separate layers• For example in dolomite itself there is a layer of
Mg2+ ions, a layer of carbonate ions, a layer of Ca2+ ions, a layer of carbonate ions, a layer of Mg2+ ions, a layer of carbonate ions, etc
• The ordering of the cations results in dolomite group minerals belonging to class bar3
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Aragonite Group
• Minerals in this group have large divalent cations and each cation is coordinated to nine oxygens
• Calcium is borderline between the ratio required for CN = VI or IX so occurs in both the calcite and aragonite structures
• Aragonite is denser and is stable at higher pressures
• The aragonite group minerals are orthorhombic, 2/m 2/m 2/m
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Bicarbonates
• Bicarbonates are minerals with the bicarbonate anion, HCO3
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• Trona is a typical saline lake deposit
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Text Reference
• See chapter 17 in the text for more information on carbonates and bicarbonates, pp. 399-403 and 407-416
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