Abstract:In January 1990 10 m 3 of washed gravel (grain size 16-50 mm) were introduced in an impounded section of the River High-Rhine to test its potential as a spawning ground for salmonids. The process of infiltration of fine sediments into the gravel and subsequent clogging was monitored for three years. Levels of clogging of the gravel matrix were estimated and ranged from slight to moderately-heavy. The degree of clogging was lower in winter than in summer. Since no bedload transport was observed during the study… Show more
“…The few studies monitoring in situ oxygen concentrations in gravel streams report a high temporal and spatial variability of this parameter (e.g. Zeh and Dönni, 1994;Peterson and Quinn, 1996;Niepagenkemper and Meyer, 2002;Groves and Chandler, 2005). Surprisingly, even if the geomorphology at potential spawning sites seems to be suitable for reproduction of salmon, suboptimal DO concentrations in the pore water of gravel interstices may prevail (Niepagenkemper and Meyer, 2002).…”
Section: Introductionmentioning
confidence: 95%
“…Frequently occurring flood events can winnow out fine sediments and prevent an extensive microbial growth within the interstices of the gravel bed even if no bedload transport occurs (Zeh and Dönni, 1994). This results in an exchange of oxygen-rich surface water with the pore water of the hyporheic interstices, stressing the significance of a natural discharge regime for maintaining high instream-dynamics (Sear, 1993;Gibson, 2002;Mürle et al, 2003).…”
Dissolved oxygen (DO) conditions within the hyporheic zone were investigated in a gravel stream (River Sieg) in North Rhine Westphalia, Germany, populated in the spawning season by recurring migratory fish species, like Atlantic salmon (Salmo salar L.) and sea trout (Salmo trutta trutta L.). The gravel bed was cleaned at three sites in an area of approximately 150 m 2 to a depth of 50 cm, reducing the quantity of grains <2 mm to below 0.2%. DO concentrations in cleaned and uncleaned sediments were monitored in situ at 10, 20 and 30 cm sediment depth from the end of November 2001 to the end of April 2002. DO showed only minor fluctuations at the cleaned sites and steadily decreased at all uncleaned sites over time. Fine sediment accumulation over 5 months in the cleaned sites was comparable to the proportion of material within the bed prior to the experimental cleaning and probably influenced the DO concentrations of the hyporheic water. Decreasing DO concentrations at all sites coincided with increasing water temperatures towards the end of the study period. The cleaning operation significantly improved the conditions of DO in the hyporheic zone of the three study sites.
“…The few studies monitoring in situ oxygen concentrations in gravel streams report a high temporal and spatial variability of this parameter (e.g. Zeh and Dönni, 1994;Peterson and Quinn, 1996;Niepagenkemper and Meyer, 2002;Groves and Chandler, 2005). Surprisingly, even if the geomorphology at potential spawning sites seems to be suitable for reproduction of salmon, suboptimal DO concentrations in the pore water of gravel interstices may prevail (Niepagenkemper and Meyer, 2002).…”
Section: Introductionmentioning
confidence: 95%
“…Frequently occurring flood events can winnow out fine sediments and prevent an extensive microbial growth within the interstices of the gravel bed even if no bedload transport occurs (Zeh and Dönni, 1994). This results in an exchange of oxygen-rich surface water with the pore water of the hyporheic interstices, stressing the significance of a natural discharge regime for maintaining high instream-dynamics (Sear, 1993;Gibson, 2002;Mürle et al, 2003).…”
Dissolved oxygen (DO) conditions within the hyporheic zone were investigated in a gravel stream (River Sieg) in North Rhine Westphalia, Germany, populated in the spawning season by recurring migratory fish species, like Atlantic salmon (Salmo salar L.) and sea trout (Salmo trutta trutta L.). The gravel bed was cleaned at three sites in an area of approximately 150 m 2 to a depth of 50 cm, reducing the quantity of grains <2 mm to below 0.2%. DO concentrations in cleaned and uncleaned sediments were monitored in situ at 10, 20 and 30 cm sediment depth from the end of November 2001 to the end of April 2002. DO showed only minor fluctuations at the cleaned sites and steadily decreased at all uncleaned sites over time. Fine sediment accumulation over 5 months in the cleaned sites was comparable to the proportion of material within the bed prior to the experimental cleaning and probably influenced the DO concentrations of the hyporheic water. Decreasing DO concentrations at all sites coincided with increasing water temperatures towards the end of the study period. The cleaning operation significantly improved the conditions of DO in the hyporheic zone of the three study sites.
“…Spawning habitat rehabilitation (SHR) is widely performed for regulated rivers in the western United States and other semi-arid regions globally (Zeh and Donni, 1994;Wheaton et al, 2004a;Gard, 2006;Elkins et al, 2007) to mitigate the decline in anadromous fish populations associated with dam impacts and excessive fishing (Yoshiyama et al, 1998;Graf, 2001). A component of SHR involves adding washed gravel and cobble, 8-256 mm in diameter, to a stream (aka gravel augmentation) to increase the quantity and quality of spawning habitat at a placement site (Harper et al, 1998;Wheaton et al, 2004a) as well as to provide coarse sediment to transport downstream where it may form diverse habitats .…”
River restoration practices aiming to sustain wild salmonid populations have received considerable attention in the Unites States and abroad, as cumulative anthropogenic impacts have caused fish population declines. An accurate representation of local depth and velocity in designs of spatially complex riffle-pool units is paramount for evaluating such practices, because these two variables constitute key instream habitat requirements and they can be used to predict channel stability. In this study, three models for predicting channel hydraulics-1D analytical, 1D numerical and 2D numerical-were compared for two theoretical spawning habitat rehabilitation (SHR) designs at two discharges to constrain the utility of these models for use in river restoration design evaluation. Hydraulic predictions from each method were used in the same physical habitat quality and sediment transport regime equations to determine how deviations propagated through those highly nonlinear functions to influence site assessments. The results showed that riffle-pool hydraulics, sediment transport regime and physical habitat quality were very poorly estimated using the 1D analytical method. The 1D and 2D numerical models did capture characteristic longitudinal profiles in cross-sectionally averaged variables. The deviation of both 1D approaches from the spatially distributed 2D model was found to be greatest at the low discharge for an oblique riffle crest with converging cross-stream flow vectors. As decision making for river rehabilitation is dependent on methods used to evaluate designs, this analysis provides managers with an awareness of the limitations used in developing designs and recommendations using the tested methods.
“…Beyond such morphodynamic processes, Kappesser et al (2002) defined a Riffle Stability Index (RSI) which estimates the mobility of cobbles in riffles. The effects of restored riffles as spawning grounds, in accordance with the European Water Framework Directive, have been discussed in the scientific literature less for rheophilic cyprinids than for salmonids (Rubin et al, 2004;Zeh & Donni, 1994).…”
An ecologically orientated flood protection project was implemented at the Austrian lowland Sulm River. Habitat modelling was conducted during a 3-year monitoring program to assess the effects of river bed embankment and the initiation of a new meander by constructing an initial side channel, and allowing self-developing side erosion. Hydrodynamic and physical habitat models were combined with statistical methods. This study focused on the necessity for including stability analysis when modelling spawning grounds. The critical erosion parameter of the cobbles at spawning grounds was analysed using numerical modelling combined with substrate maps of potential spawning grounds of nase (Chondrostoma nasus). Due to the specific characteristics of this reach of the Sulm River, instability of the riffles can hamper successful reproduction in nase. Spawning grounds of Chondrostoma nasus and their stability must be guaranteed at least for the duration of incubation. This morphodynamic necessity should be incorporated in future restoration projects and when artificially restoring spawning habitats.
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