EP004
Bedrock Breakdown: The Role of Weathering in the Evolution and Function of the Critical Zone
Bedrock Breakdown: The Role of Weathering in the Evolution and Function of the Critical Zone
Session ID#: 249030
Session Description:
The breakdown of bedrock through chemical and physical weathering processes creates fractures and pores that influence water movement and storage within hillslopes, making it vital to many hydrologic and ecological processes. Weathering also affects rock strength and hillslope sediment grain-size, which affect rates of erosion, sediment transport, and landscape evolution. In the spirit of AGU25’s theme, “Where Science Connects Us,” we seek contributions that utilize observational, experimental, and modeling techniques to quantify the fundamental controls on critical zone (CZ) weathering and the consequences of weathering for the geomorphic, hydrologic, and ecological systems that support life on Earth’s surface. Because CZ science is transdisciplinary, contributions will span diverse scales and methods, from mineral-scale measurements of fracturing and chemical alteration, to hillslope-scale geophysical measurements of CZ structure, to modeling and remote sensing of landscape-scale CZ processes. We especially encourage contributions that span disciplines and lead to a transformative understanding of CZ processes.
Co-Sponsor(s):
- H - Hydrology
- NS - Near Surface Geophysics
Index Terms:
1402 - Critical Zone [CRITICAL ZONE]
1826 Geomorphology: hillslope [HYDROLOGY]
1829 Groundwater hydrology [HYDROLOGY]
1886 Weathering [HYDROLOGY]
Primary Convener: Nancy Weinheimer, University of Wyoming, Laramie, WY, United States
Conveners: David Litwin, Temple University, Earth and Environmental Science, Philadelphia, United States and Russell Callahan, University of Connecticut, Department of Earth Sciences, Storrs, United States
See more of: Earth and Planetary Surface Processes