Interplay between ambient surface water mixing and manipulated hydraulic flushing: Implications for harmful algal bloom mitigation
•Prymnesium parvum blooms can be mitigated by deep-water hydraulic flushing of coves.•Measured water exchange rates between the open lake and targeted coves were 0.25–0.30d−1.•Water exchange rates informed a numerical model used to explore efficacy of bloom mitigation approach.•With high and continu...
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Veröffentlicht in: | Ecological engineering 2013-11, Vol.60, p.289-298 |
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Sprache: | eng |
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Zusammenfassung: | •Prymnesium parvum blooms can be mitigated by deep-water hydraulic flushing of coves.•Measured water exchange rates between the open lake and targeted coves were 0.25–0.30d−1.•Water exchange rates informed a numerical model used to explore efficacy of bloom mitigation approach.•With high and continuous deep-water flushing at 16.3×104m3d−1, P. parvum blooms in coves were reduced by 65–80%.
Creation of refugia from fish-killing algal blooms in coves of lakes represents a promising approach to bloom mitigation, especially in regards to Prymnesium parvum blooms. A way to create refugia might involve flushing of coves with deeper waters from open lake areas that are free of P. parvum. The efficacy of this mitigation approach, however, is likely influenced by the rate of water exchange between coves and surface waters of the open lake that often contain P. parvum. Conceptually, higher rates of water exchange would dilute mitigation efforts, particularly if flushing is timed to preempt harmful bloom initiation. We explored this potential limitation by conducting several dye-tracer studies in Lake Granbury (USA) that enabled direct measurement of water exchange rates between the open lake and target coves. Our measured rates of water exchange, which were typically in the range of 0.25–0.30d−1 during periods of bloom initiation, development and decline, were then used to inform a numerical model that predicted P. parvum bloom dynamics. Our simulations showed that P. parvum populations located in coves quickly returned to bloom levels when deep water flushing ceased. Nevertheless, significant benefits were predicted. For example, continuously pumping deeper waters from the open lake at rates of 16.3×104m3d−1, resulting in hydraulic residence times in the range of 0.88–1.41 days, resulted in a 65–80% predicted reduction of blooms in coves. |
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ISSN: | 0925-8574 1872-6992 |
DOI: | 10.1016/j.ecoleng.2013.07.063 |