Errrrr..... and the question is?
Carbonic acid is a solution of carbon-dioxide in water. It can dissolve limestone (calcium carbonate), dolomite (magnesium carbonate) and gypsum (calciumm sulphate).
+++ This was flagged on "gibberish" grounds. The question is badly worded but but after gently teasing the writer about that, I answered seriously & concisely what I took to be his or her enquiry.
Carbonic acid can react with rocks containing calcium carbonate, such as limestone or marble, leading to their dissolution. This process is known as chemical weathering and can result in the formation of caves, sinkholes, and other features in the rock. Over time, this reaction can alter the physical structure of the rock and contribute to the shaping of landscapes.
Carbonic acid, formed when carbon dioxide dissolves in water, can increase the acidity of rainwater. This acidic rainwater can react with rocks containing calcium carbonate, such as limestone, leading to their dissolution over time. The carbonic acid breaks down the calcium carbonate in the rock, causing it to weather or erode.
Limestone and marble are two types of rocks that are easily weathered by carbonic acid due to their high calcium carbonate content. Over time, carbonic acid dissolves these rocks, leading to the formation of caves, sinkholes, and other karst landscapes.
Carbonic acid, formed by the dissolution of carbon dioxide in water, reacts with minerals in rocks through a process called carbonation. This chemical reaction breaks down minerals in rocks, especially those like limestone and marble containing calcium carbonate, leading to their dissolution and weathering. Over time, the rocks can erode and change in appearance due to the weathering effects of carbonic acid.
Limestone and marble are two types of rocks that can be easily weathered by carbonic acid. This is because carbonic acid reacts with the calcium carbonate in these rocks, leading to the formation of calcium bicarbonate and ultimately causing dissolution and erosion of the rock.
Carbonic acid reacts with minerals in rocks, particularly calcite and dolomite, to dissolve them through a process called carbonation. This reaction breaks down the rocks and releases calcium and magnesium ions into the surrounding water, leading to erosion and weathering of the rocks. Over time, this can result in the formation of features such as caves, sinkholes, and limestone landscapes.
carbonic acid can react with minerals in rocks, leading to the dissolution of the minerals and erosion of the rock. This process is known as carbonic acid weathering and is a key component in the chemical weathering of rocks.
Carbonic acid, formed when carbon dioxide dissolves in water, can increase the acidity of rainwater. This acidic rainwater can react with rocks containing calcium carbonate, such as limestone, leading to their dissolution over time. The carbonic acid breaks down the calcium carbonate in the rock, causing it to weather or erode.
Limestone and marble are two types of rocks that are easily weathered by carbonic acid due to their high calcium carbonate content. Over time, carbonic acid dissolves these rocks, leading to the formation of caves, sinkholes, and other karst landscapes.
Yes, it is correct; for example calcium carbonate react with carbonic acid.
Carbonic acid, formed by the dissolution of carbon dioxide in water, reacts with minerals in rocks through a process called carbonation. This chemical reaction breaks down minerals in rocks, especially those like limestone and marble containing calcium carbonate, leading to their dissolution and weathering. Over time, the rocks can erode and change in appearance due to the weathering effects of carbonic acid.
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geological
Fizz
Limestone and marble are two types of rocks that can be easily weathered by carbonic acid. This is because carbonic acid reacts with the calcium carbonate in these rocks, leading to the formation of calcium bicarbonate and ultimately causing dissolution and erosion of the rock.
Carbonic acid reacts with minerals in rocks, particularly calcite and dolomite, to dissolve them through a process called carbonation. This reaction breaks down the rocks and releases calcium and magnesium ions into the surrounding water, leading to erosion and weathering of the rocks. Over time, this can result in the formation of features such as caves, sinkholes, and limestone landscapes.
Carbonic acid reacts chemically with limestone, which is observed as weathering. As such, carbonic acid weathering is a chemical, not physical, change.
Chemical weathering is the process that forms carbonic acid in water. This occurs when carbon dioxide in the atmosphere dissolves in rainwater, forming a weak carbonic acid solution that can weather rocks over time.