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| Type: | Resource | |
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| Created: | Mar 08, 2024 at 7:16 p.m. | |
| Last updated: | Mar 08, 2024 at 7:29 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 224 |
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Abstract
Large wood (LW) is widely recognized as a significant driver of geomorphic and ecological processes in river systems, but research on LW has been focused largely on low-order streams in high-gradient catchments. By comparison, there have been relatively few studies examining the channel-scale distribution of LW in higher-order, low-gradient river systems, such as those in the Coastal Plain of the Southeast US. This dataset is based on a field survey of LW in three Coastal Plain rivers (Lumber River, North Carolina; Sipsey River, Alabama; West Fork Choctawhatchee River, Alabama). The dataset consists of locations, dimensions, and characteristics for all surveyed LW pieces.
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Content
Additional Metadata
| Name | Value |
|---|---|
| Metadata | LW surveys were completed on the Lumber and West Fork Choctawhatchee rivers in June 2022 and on the Sipsey River in October 2022. Stability codes: B = buried, P = pinned, R = attached rootwad, U = unstable Orientation codes: 1 = parallel to flow, 2 = perpendicular to flow, 3 = other angle Decay codes: 1 = minimal decay (contains leaves, branches, and all bark), 2 = low decay (no leaves, contains branches and >50% of bark), 3 = moderate decay (few remaining branches, >50% of bark), 4 = high decay (no branches, <50% of bark), 5 = extreme decay (no bark, soft wood) |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| National Science Foundation | Large wood in low-gradient floodplain rivers: Spatial distribution, physical controls, and geomorphic effects | EAR-2112642 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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