The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
A bottom-up control on fresh-bedrock topography under landscapes
Open accessAbstract
Significance: Hilly landscapes are typically mantled with soil and underlain by a weathered bedrock zone that may extend tens of meters beneath the surface before reaching fresh bedrock. The weathered bedrock zone influences water runoff to channels, the chemistry of that water, the rates and processes of erosion, and atmospheric processes due to plant uptake of moisture and return to the atmosphere. However, the spatial pattern of the underlying fresh-bedrock surface is essentially unknown. We present a testable model that predicts hillslope form and the depth to fresh bedrock. The depth increases upslope and depends strongly on the porosity and permeability of the bedrock and the rate of channel incision at the base of the hillslope.
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Biggs, T. W., Dunne, T., & Martinelli, L. A. (2004) · Biogeochemistry · doi:10.1023/b:biog.0000025744.78309.2e · Cited by 113
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Richter, D. D., & Billings, S. A. (2015) · New Phytologist · doi:10.1111/nph.13338 · Cited by 221
Brantley, S. L. (2025) · Reviews of Geophysics · doi:10.1029/2025rg000881 · Cited by 11
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Metadata
- Authors
- Rempe, D. M., & Dietrich, W. E.
- Venue
- Proceedings of the National Academy of Sciences
- Published
- 2014-04-23
- Volume
- 111
- Issue
- 18
- Pages
- 6576-6581
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- OpenAlex
- W2085746088
- Cited by
- 302
- References
- 1
- FWCI
- 15.38
- Type
- journal article
- Language
- en
- Open access
- green
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- Rempe, D. M., & Dietrich, W. E. (2014). A bottom-up control on fresh-bedrock topography under landscapes. Proceedings of the National Academy of Sciences. https://doi.org/10.1073/pnas.1404763111
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.