Lake stability and anoxia dynamics revealed from high frequency vertical profiling in a eutrophic polymictic reservoir

• Published in: Inland waters (Print) Vol. ahead-of-print; no. ahead-of-print; pp. 1 - 15
• Main Authors: Wagner, Nicole D., Osburn, Felicia S., Robbins, Caleb J., Ernst, Mark R., Owens, Jennifer, Powers, Stephen M., Scott, J. Thad
• Format: Journal Article
• Language: English
• Published: Taylor & Francis 03.04.2023
• Subjects: hypoxia; Lake Number; Schmidt stability; water quality; wavelet coherence
• ISSN: 2044-2041; 2044-205X
• DOI: 10.1080/20442041.2022.2161264

High-frequency water quality monitoring is rapidly growing in freshwater research and management. Sensor deployments at fixed depths in naturally formed lakes dominate the current understanding of ecosystem dynamics, with comparatively few studies focusing on reservoirs. Here we examined how environmental parameters affect the water column stability and dissolved oxygen (DO) dynamics in a North Texas eutrophic reservoir. We used an autonomous water quality monitoring profiler that recorded temperature, DO, and pH as well as wind speed, wind direction, and air temperature from an on-platform mounted weather station. Data were collected every 2 h from 25 April to 29 October 2019, with each profile spanning from the surface to 10 m depth at 0.5 m steps. Throughout most of the sampling period, the lake had no distinct thermocline, but we observed an oxycline throughout most of the monitoring period, with multiple mixing events. Near the sediments, periods of anoxia lasting hours to days were first observed in May, and July through September were chronically anoxic. In August and September, DO was frequently <2.0 mg L −1 throughout the entire water column, with 2 periods of total water column anoxia. Surface DO measurements for each 2 h interval were highly synchronous with Schmidt stability. During decreasing and low Schmidt stability or Lake Number, the oxycline destabilized in association with changes in wind direction and speed. Our results indicate that DO can be highly dynamic in polymictic reservoirs, with strong implications for carbon and nitrogen biogeochemical cycles.