Critical zone (CZ) structure, including the spatial distribution of minerals, elements, and fluid-filled pores, evolves on geologic time scales resulting from both top-down climatic forcing and bottom-up geologic controls. Climate and lithology may be imprinted in subsurface structure as depth-dependent trends in geophysical, geochemical, mineralogical, and biological datasets. As the weathering profile is as much (or more) a product of past environmental conditions, development of predictive models requires understanding the relative roles of climatic forcing and the geologic template on which CZ processes evolve. Doing so in complex volcanic terrains with high initial bedrock porosity and distinct depositional and hydrothermal alteration histories is particularly challenging. To resolve CZ structure in a rhyolitic catchment in the Valles Caldera National Preserve (NM, USA), this study combined geophysics, drilling, and laboratory analyses to produce depth-resolved porosity, geochemistry, and mineralogy datasets to >40 m in depth. Quantitative X-ray diffraction analysis showed that local mineral transformations control complex chemical enrichment/depletion (τ) patterns. Using linear discriminant analysis, key variables enabled separation of complex-layered geology into discrete zones. Contemporary, matrix-dominated weathering processes and modern hydrologic fluxes occur dominantly within the top 15 m of the weathering profile. This zone is convoluted by incomplete primary mineral weathering and overprinted by post-eruption weathering and metasomatism. Matrix weathering transitions to fracture surface weathering driven by deep percolation of slower moving, longer residence time meteoric waters at depth. By altering initial conditions and weathering trajectory, geologic legacy is a critical factor in how this subsurface landscape evolved and functions.
|Original language||English (US)|
|Journal||Journal of Geophysical Research: Earth Surface|
|State||Published - Jan 1 2020|
Bibliographical noteFunding Information:
Funding for this project was provided by the Jemez River Basin-Santa Catalina Critical Zone Observatory (NSF EAR-0724958; EAR-1331408). Portions of this research were carried out at Stanford Synchrotron Radiation Laboratory, a National User Facility operated by Stanford University on behalf of the U.S. Department of Energy, Office of Basic Energy Sciences. Additional drilling, geophysical data, and core analysis and images may be accessed at http://osf.io/8fkzk. We thank Anders Noren and Ryan O'Grady from the Continental Scientific Drilling Coordination Office and LacCORE for their support on this project. We also wish to thank Mary Kay Amistadi, Rachel Burnett, Kenneth Domanik, Desiree Carillo, Kelly Orman, Casey McDuffy, Anissa McKenna, Rachel Gallery, Yalu Hu, Shawn Pedron, Nate Abramson, Michael Pohlmann, Ravindra Dwivedi, Dawson Fairbanks, and Cascade Drilling Inc. (Bothell, WA).
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- critical zone
- legacy geology
Continental Scientific Drilling Facility tags