What Is Chemical Weathering

There are three types of weathering which affect rock: physical, biological, and chemical. Chemical weathering, also known as decomposition or decay, is the breakdown of rock  by chemical mechanisms. How Chemical Weathering Happens Chemical weathering does not break rocks into smaller fragments through wind, water, and ice (thats physical weathering). Nor does it break rocks apart through the action of plants or animals (thats biological weathering). Instead, it changes the chemical composition of the rock, usually through carbonation, hydration, hydrolysis or oxidation.   Chemical weathering alters the composition of the rock material toward surface minerals, such as clays. It attacks minerals that are relatively unstable in surface conditions, such as the primary minerals of igneous rocks like basalt, granite or peridotite. It can also occur in sedimentary and metamorphic rocks and  is an element of  corrosion  or chemical erosion.   Water is especially effective at introducing chemically active agents by way of fractures and causing rocks to crumble piecemeal. Water may also loosen thin shells of material (in spheroidal weathering). Chemical weathering may include shallow, low-temperature alteration. Lets take a look at the four main types of chemical weathering that were mentioned earlier. It should be noted that these are not the only forms, just the most common. Carbonation Carbonation occurs when rain, which is naturally slightly acidic due to atmospheric carbon dioxide  (CO2), combines with a calcium carbonate (CaCO3), such as limestone or chalk. The interaction forms calcium bicarbonate, or  Ca(HCO3)2. Rain has a normal pH level of 5.0-5.5, which alone is acidic enough to cause a chemical reaction. Acid rain, which is unnaturally acidic from atmospheric pollution, has a pH level of 4 (a lower number indicates greater acidity while a higher number indicates greater basicity).   Carbonation, sometimes referred to as  dissolution,  is the driving force behind the sinkholes, caverns and underground rivers of  karst topography.   Hydration Hydration occurs when water reacts with an anhydrous mineral, creating a new mineral. The water is added to the crystalline structure of a mineral, which forms a hydrate.   Anhydrite, which means waterless stone, is a calcium sulfate (CaSO4) that is  usually found in underground settings. When exposed to water near the surface, it quickly becomes gypsum, the softest mineral on the Mohs hardness scale.  Ã‚  Ã‚   Hydrolysis Hydrolysis is the opposite of hydration; in this case, water breaks down the chemical bonds of a mineral instead of creating a new mineral. It is a decomposition reaction.   The name makes this one particularly easy to remember: The prefix hydro- means water, while the suffix -lysis means decomposition, breakdown or separation.   Oxidation Oxidation refers to the reaction of oxygen  with metal elements in a rock, forming oxides.  An easily recognizable example of this is rust.  Iron (steel) reacts easily with oxygen, turning into reddish-brown iron oxides. This reaction is responsible for the red surface of Mars and the red color of hematite and magnetite, two other common oxides.