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This is higher than that of calcite (2.7) or dolomite (2.85) because the barium atom is very heavy, with atomic mass 137, which is much more than magnesium at 24 and calcium at 40. Barytocalcite is soluble in dilute hydrochloric acid HCl [4] and it is not radioactive. [2]
Limestone outcrops are recognized in the field by their softness (calcite and aragonite both have a Mohs hardness of less than 4, well below common silicate minerals) and because limestone bubbles vigorously when a drop of dilute hydrochloric acid is dropped on it. Dolomite is also soft but reacts only feebly with dilute hydrochloric acid, and ...
It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. Unless it is in fine powder form, it does not rapidly dissolve or effervesce (fizz) in cold dilute hydrochloric acid as calcite does. [9] Crystal twinning is common.
Calcite, like most carbonates, dissolves in acids by the following reaction CaCO 3 + 2 H + → Ca 2+ + H 2 O + CO 2. The carbon dioxide released by this reaction produces a characteristic effervescence when a calcite sample is treated with an acid. Due to its acidity, carbon dioxide has a slight solubilizing effect on calcite. The overall ...
Calcite alabaster, harder than the gypsum variety, was used in ancient Egypt and the wider Middle East (except Assyrian palace reliefs), and also in modern times. It is found as either a stalagmitic deposit from the floor and walls of limestone caverns , or as a kind of travertine , similarly deposited in springs of calcareous water.
Calcite has several unique properties. It can polarize light, has fluorescence, phosphorescence, thermoluminescence, triboluminescence, double refraction, and fizzes with a weak acid, such as hydrochloric acid (diluted) or vinegar. Polarized light is light that has been “filtered”.
Quartz is commonly the dominant mineral component, and some mica is often present. Apart from the mineral content, rock fragments may also be a significant component. Arkose usually contains small amounts of calcite cement, which causes it to effervesce (fizz) slightly in dilute hydrochloric acid; sometimes the cement also contains iron oxide.
It is quite soft, with hardness 2.5, between gypsum and calcite, and relatively dense; its specific gravity is 3.84, close to that of topaz, and much denser than quartz (specific gravity 2.5 to 2.7). It is easily soluble in hydrochloric acid .