CHEMICAL WEATHERING - Chemical weathering, also known as decomposition or decay, is the breakdown of rock by chemical mechanisms. Chemical weathering does not break rocks into smaller fragments through wind, water, and ice (that's physical weathering). 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. Water is especially effective at introducing chemically active agents by way of fractures and causing rocks to crumble piecemeal.

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Chemical Weathering

What Is Chemical Weathering?

Chemical weathering can change the composition and shape of rocks

by Andrew Alden 

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 (that's physical weathering).

Nor does it break rocks apart through the action of plants or animals (that's 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.

Let's 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.   

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.

Andrew Alden

Professional geologist, writer, photographer, and geological tour guide

Thirty-seven years of experience writing about geological subjects

Six years as a research guide with U.S. Geological Survey (USGS)

Member of Geological Society of America (GSA), and American Geophysical Union (AGU)

Experience

Andrew Alden is a former writer for ThoughtCo who contributed hundreds of articles for more than 17 years. Andrew works as a geologist, writer, editor, and photographer. He has written on geological subjects since 1981 and participates actively in his field. For example, Andrew spent six years as a research guide with the U.S. Geological Survey, leading excursions on both land land and at sea. And since 1992, he has hosted the earthquakes conference for the online discussion platform, The Well, which began as a dialogue between the writers and readers of the Whole Earth Review. 

In addition, Andrew is a longtime member of the member of the Geological Society of America — an international society that serves members in academia, government, and industry; and the American Geophysical Union — a community of earth and space scientists that advances the power of science to ensure a sustainable future.

Andrew lives in Oakland, California; and though he writes about the whole planet and beyond, Andrew finds his own city full of interest too and blogs about its geology. 

Education

Andrew Alden holds a bachelor's (B.A.) degree in Earth Science from the University of New Hampshire, College of Engineering and Physical Sciences, in Durham, N.H.

Awards and Publications

Andrew Alden on Earthquakes ​(The Well Group, Inc., 2011)

Assessment of River — Floodplain Aquifer Interactions (Environmental and Engineering Geoscience, 1997)

Andrew Alden on Hosting (The Well Group, Inc., 1995)

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