Wikibooks: Methods Manual for Salt Lake Studies/Sequential crystallisation of brine salts
Authors PSJ Coleman = Overview = The brines in salt lakes are made up of a variety of dissolved salts derived from the environment in which the lake is located. Salt lakes even those in extremely cold places such as Antarctica are usually found in semi arid areas of the earth with low rainfall and h...
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| Language: | English |
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| Online Access: | https://en.wikibooks.org/wiki/Methods_Manual_for_Salt_Lake_Studies/Sequential_crystallisation_of_brine_salts |
| Summary: | Authors PSJ Coleman = Overview = The brines in salt lakes are made up of a variety of dissolved salts derived from the environment in which the lake is located. Salt lakes even those in extremely cold places such as Antarctica are usually found in semi arid areas of the earth with low rainfall and high evaporation. Sources of salts to salt lakes are various they may be the result of the stranding of marine areas in the geological past or they may be the result of dissolution of nearby rocks over eons into a terminal lake system. = What type of lake is it? = Marine derived brines are characterised by the presence of calcium and magnesium salts. Salt lakes formed from local dissolution may have very different salt compositions. Sodium chloride is present in all salt lakes. Most lakes fall into four major groups if you are classifying them by their salt composition Sulfate type lakes that derive their salts from surrounding rocks that contain sodium sulfate Carbonate type lakes (marl or flos ferri lakes) are alkaline lakes which contain sodium carbonate in addition to sodium chloride and sodium sulfate (gypsum and anhydrite). Bittern lakes like the Dead Sea contain more magnesium than sodium. Sodium chloride type lakes such as the Great Salt Lake of USA and most Australian salt lakes are similar in composition to sea brine of an identical density. = Crystallisation sequence in marine derived lakes = In sodium chloride type lakes the crystallisation pattern of the different salts is very similar to that of evaporating seawater brines and occurs as follows (Baseggio 1974 Venkatesh Mannar 1982) The least soluble salts are the ferric oxides which precipitate out of solution between 30g/L TDS and 70g/L TDS. Calcium carbonate (calcite or flos ferri) starts to deposit at the same salinity as ferric oxide but continues precipitating up to a salinity of about 170g/L TDS. Calcium sulfate as gypsum or selenite (CaSO 4 .2H 2 O)starts to precipitate at a salinity of about 143g/L TDS. At about 191g/L TDS the form of calcium ... |
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