2006
DOI: 10.1080/07438140609354363
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Limnological Characterization and Flow Patterns of a Three-coupled Reservoir System and Their Influence onDreissena polymorphaPopulations and Settlement During the Stratification Period

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Cited by 34 publications
(14 citation statements)
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“…Wittmann et al (2010) also found the highest quagga mussel densities on muddy and sandy substrates at depths from 12-42 m in Lake Mead. In a reservoir in Spain, Navarro et al (2006) found the highest densities of zebra mussels in the hypolimnion, but the biomass of the individuals was much less than mussels found in the epilimnion. This study and Wacker and von Elert (2003) both found the lowest densities of mussels in the hypolimnion and the highest densities in the epilimnion.…”
Section: Comparison To Other Bodies Of Watermentioning
confidence: 91%
“…Wittmann et al (2010) also found the highest quagga mussel densities on muddy and sandy substrates at depths from 12-42 m in Lake Mead. In a reservoir in Spain, Navarro et al (2006) found the highest densities of zebra mussels in the hypolimnion, but the biomass of the individuals was much less than mussels found in the epilimnion. This study and Wacker and von Elert (2003) both found the lowest densities of mussels in the hypolimnion and the highest densities in the epilimnion.…”
Section: Comparison To Other Bodies Of Watermentioning
confidence: 91%
“…Integrated surface water samples (INAG IP 2009) were collected at each sampling site using a one-inch diameter garden hose (Navarro et al 2006;Becker et al 2010), with modifications. Garden hoses 5, 3, and 2 m in length were used when the depths of the sampling sites were greater than 10 m, between 10 and 5 m, and less than 5 m, respectively ( Table 2).…”
Section: Coordinates Measured With Utm Wgs Datum 84mentioning
confidence: 99%
“…It receives water from the Ebro, Segre and Matarraña rivers, although the latter provides only a small quantity of water and has not been taken into account in the model, although it is sufficient to transport larvae. As a preliminary approach, this reservoir presents a hydrodynamic organization (Navarro et al, 2006) with a stratification of the water column due to the interaction between colder and more mineralized water from the Ebro River located at the bottom, and less mineralized, warmer water, with a greater concentration of nutrients, coming from the Segre River, flowing near or through the surface. This arrangement allows the distinction of two clearly different layers in the water column in the reservoir throughout the year (upper, U, and lower, L), especially in summer, when the incoming waters from Segre are warmer.…”
Section: The Study Areamentioning
confidence: 99%