Estimating flow rates to optimize winter habitat for centrarchid fish in Mississippi River (USA) backwaters

Barry L. Johnson,, Brent C. Knights, J. Barko, Robert F. Gaugush, D. Søballe, W. F. James
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引用次数: 23

Abstract

The backwaters of large rivers provide winter refuge for many riverine fish, but they often exhibit low dissolved oxygen levels due to high biological oxygen demand and low flows. Introducing water from the main channel can increase oxygen levels in backwaters, but can also increase current velocity and reduce temperature during winter, which may reduce habitat suitability for fish. In 1993, culverts were installed to introduce flow to the Finger Lakes, a system of six backwater lakes on the Mississippi River, about 160 km downstream from Minneapolis, Minnesota. The goal was to improve habitat for bluegills and black crappies during winter by providing dissolved oxygen concentrations >3 mg/L, current velocities 1°C. To achieve these conditions, we used data on lake volume and oxygen demand to estimate the minimum flow required to maintain 3 mg/L of dissolved oxygen in each lake. Estimated flows ranged from 0.02 to 0.14 m3/s among lakes. Data gathered in winter 1994 after the culverts were opened, indicated that the estimated flows met habitat goals, but that thermal stratification and lake morphometry can reduce the volume of optimal habitat created. This article is a U.S. Government publication and is in the public domain in the United States.
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估算流量以优化密西西比河(美国)回水中部鱼类的冬季栖息地
大型河流的回水为许多河流鱼类提供了冬季避难所,但由于高生物需氧量和低流量,它们往往表现出低溶解氧水平。从主河道引入水可以增加死水的含氧量,但也会增加水流速度,并在冬季降低温度,这可能会降低鱼类的栖息地适宜性。1993年,修建了涵洞,将水流引入芬格湖。芬格湖是密西西比河上的六个回水湖泊组成的系统,位于明尼苏达州明尼阿波利斯市下游约160公里处。目标是在冬季提供溶解氧浓度>3 mg/L,流速1°C,以改善蓝鳃鱼和黑鲷的栖息地。为了达到这些条件,我们使用湖泊体积和需氧量的数据来估计每个湖泊维持3 mg/L溶解氧所需的最小流量。湖泊间的流量估计在0.02至0.14立方米/秒之间。在涵洞开通后1994年冬季收集的数据表明,估计的流量符合生境目标,但热分层和湖泊形态测定法可能会减少所创造的最佳生境的体积。本文为美国政府出版物,在美国属于公有领域。
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