Physical weathering of rock breakdown more important than previously recognized

Physical weathering of rock breakdown more important than previously recognized
Research led by the University of Wyoming shows that physical weathering is far more important than previously recognized in the breakdown of rock in mountain landscapes. Because it is difficult to measure, physical weathering has commonly been assumed to be negligible in previous studies.


Cliff Riebe, a professor in UW s Department of Geology and Geophysics, headed a research group that discovered that climate and erosion rates strongly regulate the relative importance of subsurface physical and chemical weathering of saprolite, the zone of weathered rock that retains the relative positions of mineral grains of the parent bedrock and lies between the layer of soil and harder rock underneath. Saprolite is much like the weathered granite found on the flat areas surrounding the hard granite of Vedauwoo.

"Our work shows that physical strain can no longer be ignored in studies of subsurface weathering. It s not just a chemical process. It is physical as well," Riebe says. "What we found is that anisovolumetric weathering is much more common than previously thought, and that variations in this process can be explained by climate and erosion."

Riebe is lead author of a paper, titled "Anisovolumetric Weathering in Granitic Saprolite Controlled by Climate and Erosion Rates," which was published in the Jan. 12 issue of Geology.

The study looked at three sites -- with differing climates and elevations of granitic bedrock -- of the Sierra Nevada, a mountain range in California.

In the lingo of geochemists, weathering has long been assumed to be "isovolumetric," meaning without a change in volume caused by physical strain.


"Our work shows that, to the contrary, weathering is commonly anisovolumetric, meaning that strain caused by physical weathering is important," Riebe says.

Riebe credits some of the tools and instruments that were purchased from the Wyoming Center for Environmental Hydrology and Geophysics (WyCEHG) EPSCoR (Established Program to Stimulate Competitive Research) project that ended a few years ago as the reason his team could measure both physical and chemical weathering at several sites in California.

"The reason why weathering was difficult to measure in the past is you have to be able to access the deep subsurface and sample it without disturbing it," Riebe explains. "You need a Geoprobe push coring system, which is basically a big track-mounted drill rig, to do this.

"It s expensive work, especially if you do not happen to own a Geoprobe and have to hire someone to do the work," he continues. "Fortunately, we have access to this equipment and the expertise to operate it through Wyoming s Near Surface Geophysics facility, which is ably managed by Brad Carr, one of the study s co-authors."

The research was funded by grants from the National Science Foundation (NSF), NASA and the Natural Sciences and Engineering Research Council of Canada.

Riebe says there is a direct correlation between the research in this paper and the $5.33 million NSF grant he received last September. The grant focuses on connections among rock, water and life at Earth s surface.

"This research is partly supported by that grant and also helped inspire it," Riebe says.

Materials provided by University of Wyoming . Note: Content may be edited for style and length.

University of Wyoming. "Physical weathering of rock breakdown more important than previously recognized." ScienceDaily. ScienceDaily, 13 January 2021. .

University of Wyoming. "Physical weathering of rock breakdown more important than previously recognized." ScienceDaily. (accessed January 13, 2021).



Sep. 19, 2018 — The amount of carbon dioxide released from thawing permafrost might be greater than previously thought, according to a new study by ecologists. The research is the first to document the potential for ...

Aug. 1, 2017 — Scientists have discovered that chemical weathering, a process in which carbon dioxide breaks down rocks and then gets trapped in sediment, can happen at a much faster rate than scientists previously ...

Mar. 27, 2017 — Researchers have developed an integrated sediment, wood, and organic carbon budget for North St. Vrain Creek in the semi-arid Colorado Front Range following an extreme flooding event in September of ...

Apr. 14, 2016 — Chemical weathering can control how susceptible bedrock in river beds is to erosion, according to new research. In addition to explaining how climate can influence landscape erosion rates, the ...
News Topics :
Similar Articles :
A University of Wyoming researcher and his team discovered that weathering of subsurface rock in the Southern Sierra Nevada Mountains of California occurs due more to rocks expanding than from...
A University of Wyoming researcher and his colleagues have shown that much of the southwestern United States was once a vast high elevation plateau, similar to Tibet today. advertisement This work...
Research published this week by University of Wisconsin Madison scientists shows how bacteria can degrade solid bedrock, jump starting a long process of alteration that creates the mineral portion of soil. advertisement...
Mars mantle may be more complicated than previously thought. In a new study published in the Nature affiliated journal Scientific Reports, researchers at LSU document geochemical changes over time in...
Chemical reactions deep below ground affect water quality, but methods for seeing them are time consuming, expensive and limited in scope. A Penn State led research team found that seismic waves can...