Chemical weathering
This is chemical weathering. Carbonic acid (and often sulphuric acid from SO2) destroy CaCO3 (limestone) through chemical attack.Carbonic acid is formed by reaction of H2O and CO2 to create H2CO3.
Carbonic acid reacts chemically with limestone, which is observed as weathering. As such, carbonic acid weathering is a chemical, not physical, change.
chemical weathering by acid rain.
mechanical weathering +++ I'd class it as chemical weathering because the action is dissolution by weakly-acid, and it works only in limestone, gypsum and dolomite - although dolomite deposits are not normally structurally disposed to cave development.
One reason why limestone is susceptible to chemical weathering because when acid acts on the calcium carbonate in the limestone to form calcium bicarbonate which is dissolved by water, which results in pits and holes found in the limestone. Equations to represent: CaCO3 + H2O + CO2 results in Ca(HCO3)2
This is chemical weathering. Carbonic acid (and often sulphuric acid from SO2) destroy CaCO3 (limestone) through chemical attack.Carbonic acid is formed by reaction of H2O and CO2 to create H2CO3.
Karst topography is formed by chemical weathering, and affects the underlying carbonate rock (limestone or dolomite). This occurs under specific drainage conditions. Slightly acidic water (carbonic acid in solution) is the active agent.
acid chemicals
dissolving of limestone by acid rain
The dissolution of limestone by rainwater containing carbonic acid is the perfect example of chemical weathering.
No. It dissolves limestone slowly. It may take centuries for a limestone outcrop to show visible weathering.
The acid rain causes erosion and weathering of the limestone.Acid rain attacks and dissolves Limestone .As a result of that , carbon dioxide gas is evolved
Acid does indeed cause weathering. It is a common form of chemical weathering, and is sometimes influenced by humans. It is particularly devastating to basic rocks like limestone which neutralise the acid rain, but at the expense of its own volume, as after the neutralisation, the salt is often washed away and the limestone is consequently worn away.
type of weathering represented by dissolution of lime stone in acid is known as chemical weathering and is mainly expirienced in coastal regions as rain water dissoves CO2 in the air forming a weak carbonic acid which then dissolves limestone in the area in the process of chemical weathering and it results in the formation of karst scenary.
The process that hollows out limestone in caves is called chemical weathering. This occurs when rainwater combines with carbon dioxide in the atmosphere to create a weak carbonic acid, which gradually dissolves the limestone over time, resulting in the formation of caves and caverns.
Carbonic acid reacts chemically with limestone, which is observed as weathering. As such, carbonic acid weathering is a chemical, not physical, change.
Chemical weathering processes are particularly effective on limestone landscapes forming because of carbonation. When rainwater combines with acid in the air, limestone is formed.