Let
This content will become publicly available on May 1, 2025
Hypolimnetic hypoxia has become increasingly prevalent in stratified water bodies in recent decades due to climate change. One primary sink of dissolved oxygen (DO) is sediment oxygen uptake (
In this study, a computational procedure is proposed to determine the SWI and DBL objectively and automatically. The procedure was evaluated for more than 300 DO profiles in the sediment of three eutrophic water bodies spanning gradients of depth and surface area. Synthetic DO profiles were modeled based on sediment characteristics estimated by laboratory experiments. The procedure was further verified adopting the synthetic profiles.
The procedure, which was evaluated for both measured and synthetic DO profiles, determined the SWI and DBL well for both steady and non-steady state DO profiles. A negative relationship between DBL thickness and aeration rates was observed, which agrees with existing literatures.
The procedure is recommended for future studies involving characterizing DBL to improve efficiency and consistency.
- Award ID(s):
- 1753639
- PAR ID:
- 10518919
- Publisher / Repository:
- Springer
- Date Published:
- Journal Name:
- Journal of Soils and Sediments
- Volume:
- 24
- Issue:
- 5
- ISSN:
- 1439-0108
- Page Range / eLocation ID:
- 2132 to 2143
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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