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| Type: | Resource | |
| Storage: | The size of this resource is 1.3 MB | |
| Created: | Oct 17, 2024 at 10:08 p.m. (UTC) | |
| Last updated: | Jul 09, 2025 at 9:12 p.m. (UTC) | |
| Published date: | Jul 09, 2025 at 9:12 p.m. (UTC) | |
| DOI: | 10.4211/hs.975ae49ca7c7428caa38746e5f4a7038 | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Published |
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| Views: | 43 |
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Abstract
Dissolved oxygen (DO), dissolved organic carbon (DOC), temperature (temp), boulder coordinates, and other data collected at the Center for Ecohydraulics Research, University of Idaho, Boise. Experiments were conducted to measure the impact of macroroughness elements (MRE), like boulders, and MRE-induced topographical changes on hyporheic chemistry. DO was measured using the system described in Reeder et al. (2019). The DOC was measured using a Shimadzu TOC-VCSH total organic carbon analyzer (CAT NO. 638-91062-22).
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This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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