Your question is somewhat odd, you use the words "chemical weathering" and "dissolution" together.
Chemical weathering is usually a process of weathering by "solution" in which case the minerals susceptible to this would be:- Carbonates and halides.
Dissolution means decomposition into fragments or parts, a disintegration or liquefaction. There are some minerals that will do this, for instance Iron Pyrites.
There are a number of things which are susceptible to chemical weathering by dissolution. Carbonates are the most susceptible as they dissolve easily.
warm and humid
acid rain probably
calcite
Dissolution occurs.
Clay minerals are the product of chemical weathering of silicate minerals, such as feldspars. Clays are silicate minerals.
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.
Chemical weathering often refers to the chemical reactions that take place between acidic rain or ground water and various rock types. It can also refer to the gradual oxidation of minerals by exposure to air and water. The chemical reaction usually results in the gradual dissolution of the rock.
We apply the term chemical weathering to the (chemical) reactions that occur and dissolve minerals in rock.
It's called dissolution, a form of chemical weathering.
Quartz is a mineral that is highly resistant to chemical weathering. Marble is a mineral that is more susceptible to chemical weathering.
Dissolution occurs.
•reaction of rock/minerals with water •The ultimate fate of all surface rocks •Contrast with physical weathering •Hydration •Hydrolysis •Dissolution •Carbonation •Biological •Redox
Clay minerals are the product of chemical weathering of silicate minerals, such as feldspars. Clays are silicate minerals.
Chemical weathering
False
Carbonation. Minerals combine chemically with H2CO3 and form a new product called...Carbonation. Which happens inside the rock :)
in chemical the minerals present in the rock dissolve in water causing chemical weathering
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.
Minerals with a simple composition and strong bonding tend to have the greatest chemical stability. For example, minerals like quartz (SiO2) and diamond (C) have extremely stable chemical structures and are resistant to chemical weathering. Other stable minerals include halite (NaCl), calcite (CaCO3), and pyrite (FeS2).
Chemical weathering often refers to the chemical reactions that take place between acidic rain or ground water and various rock types. It can also refer to the gradual oxidation of minerals by exposure to air and water. The chemical reaction usually results in the gradual dissolution of the rock.