The process of a soluble mineral receiving water through precipitation and weakening is known as chemical weathering. This process occurs when water, which contains dissolved ions and acids, seeps into the cracks and pores of a mineral. The water reacts with the mineral, causing it to break down and dissolve. This process can be accelerated by the presence of certain microorganisms, such as bacteria and fungi, which produce acids that further dissolve the mineral.

Chemical weathering can cause a variety of different effects on minerals, including:

* Dissolution: This is the most common type of chemical weathering, and it occurs when the entire mineral is dissolved in water.

* Hydrolysis: This occurs when water breaks down the chemical bonds of a mineral, causing it to break down into smaller, simpler molecules.

* Oxidation: This occurs when oxygen reacts with a mineral, causing it to change color and become more brittle.

* Reduction: This occurs when hydrogen or another reducing agent reacts with a mineral, causing it to lose oxygen and become more metallic.

Chemical weathering can have a significant impact on the landscape. It can cause rocks to break down and erode, and it can also lead to the formation of new minerals and soils.