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Calcite is a colorless mineral that bubbles with acid due to its reaction to the acid, releasing carbon dioxide gas.
The mineral that fits this description is calcite. When hydrochloric acid is applied to calcite, it will bubble and effervesce. Calcite is commonly used in the production of cement and lime due to its abundance and chemical properties.
The mineral that is colorless and fizzes with acid is likely calcite, which is a type of carbonate mineral. When calcite comes into contact with acid, such as vinegar, it will bubble or effervesce due to the carbon dioxide gas being released.
Calcite is the most likely mineral to display effervescence when treated with dilute acid. The acid reacts with the calcium carbonate in calcite, releasing carbon dioxide gas, which causes the mineral to bubble or fizz.
Minerals that contain carbonate minerals, such as calcite or dolomite, will bubble when treated with hydrochloric acid due to the release of carbon dioxide gas from the reaction between the acid and the carbonate minerals. This bubbling effect is a simple test to identify carbonate minerals in mineral samples.
Calcite is a colorless mineral that bubbles with acid due to its reaction to the acid, releasing carbon dioxide gas.
If the acid test is positive for a mineral, the surface of the mineral may show signs of fizzing or bubbling due to a chemical reaction between the acid and the mineral. This reaction indicates that the mineral contains carbonate minerals like calcite or dolomite, which are reactive to acid.
The mineral that fits this description is calcite. When hydrochloric acid is applied to calcite, it will bubble and effervesce. Calcite is commonly used in the production of cement and lime due to its abundance and chemical properties.
The mineral that is colorless and fizzes with acid is likely calcite, which is a type of carbonate mineral. When calcite comes into contact with acid, such as vinegar, it will bubble or effervesce due to the carbon dioxide gas being released.
Calcite is the most likely mineral to display effervescence when treated with dilute acid. The acid reacts with the calcium carbonate in calcite, releasing carbon dioxide gas, which causes the mineral to bubble or fizz.
The bubbling reaction when acid is added to sandstone indicates the presence of the mineral calcite, which is sensitive to acids. Calcite is a common mineral found in sedimentary rocks like sandstone.
Minerals that contain carbonate minerals, such as calcite or dolomite, will bubble when treated with hydrochloric acid due to the release of carbon dioxide gas from the reaction between the acid and the carbonate minerals. This bubbling effect is a simple test to identify carbonate minerals in mineral samples.
Hydrochloric acid is a mineral acid, not organic. It is a strong acid produced by inorganic reactions involving hydrogen and chlorine atoms.
No. Only sedimentary rocks containing carbonate minerals will bubble with acid.
No, Pantothenic acid (Vitamin B5) is a vitamin and not a mineral.
Someone should not have placed carbonic acid in the mineral acid list. For your edification though, whether or not an acid is strong or weak has no bearing on whether or not it is a mineral acid or an organic acid. Mineral acid is any acid comprised of one or more inorganic compounds and dissociate into a hydrogen ion and conjugate base.
No