An integrated approach to hydropower impact assessment. I. Environmental features of some Norwegian hydro-electric lakes

This paper launches concepts instrumental to environmental impact assessment (EIA) studies on hydropower schemes and lake regulations. Norwegian hydro-electric lakes (hydrolakes) and their environmental features are described, and evaluated against non-manipulated waters. A tentative classification of hydrolakes vs. natural waters is proposed. The need for a multiple approach to habitat classification is emphasized. Recommendations for future biological impact assessment approaches are suggested.Hydrolakes differ broadly from natural lakes by combining physical features not ordinarily co-occurring in non-manipulated water bodies. Storage type hydrolakes (reservoirs) feature winter draw-downs and enhancement of yearly level fluctuations; whereas other types of hydro-electric lakes have elevated water levels throughout winter. Hydrochemistry and optics of the studied hydrolakes exhibited no clear differences to non-impacted Norwegian inland waters. All lakes had signs of sublacustrine erosional activity related to internal waves and thermocline movements.     

Responses of Estuarine Benthic Invertebrates to Sediment Burial: The Importance of Mobility and Adaptation

Estuarine benthic organisms are frequently subjected to disturbance events caused by hydrodynamic processes that disrupt and move the sediment in which the animals reside, however the mechanisms by which physical disturbance processes affect infaunal and epifaunal populations and communities remain poorly resolved. The responses of three infaunal and two epifaunal estuarine benthic species to sediment disturbance (burial) were compared in laboratory experiments. Overburden stress (kPa) was calculated to quantify the force exerted on organisms by sediment burial for 6 d. At the levels tested (0–16 kPa), increasing overburden stress did not significantly decrease survival or growth of juvenile burrowing bivalves, Macoma balthica (Linnaeus). Survival of juveniles and adults of the tubiculous polychaete Streblospio benedicti (Webster) and neonates of the burrow-forming amphipod Leptocheirus plumulosus (Shoemaker) declined exponentially with increasing overburden stress. The mean S. benedicti survival rate was 4% of the control at an overburden stress of ≈4 kPa, while an overburden stress of 12 kPa was necessary to comparably reduce survival of L. plumulosus. At the low levels of overburden stress used in the experiments with epifauna (≤0.2 kPa), juvenile oyster Crassostrea virginica (Gmelin) did not suffer significant mortality at an overburden stress of 0.1 kPa. In contrast, the epifaunal tunicate Molgula manhattensis (DeKay) exhibited significant mortality when partially (one or two siphons exposed) or completely buried under sediment with an overburden stress of 0.2 kPa. Species-specific response to burial varied as a function of motility, living position, and inferred physiological tolerance of anoxic conditions while buried. We conclude that some benthic species exhibit mechanical and possibly physiological adaptations that may allow them to survive deposition events of the magnitude commonly encountered in estuarine environments.     

Temporal dynamics and spatial variation of algae in relation to hydrology and sediment characteristics in the Okefenokee Swamp,Georgia

In a 20-month study, phytoplankton and periphyton chl a, and dry mass of macroscopic algal aggregates in four marshes and a lake within the Okefenokee Swamp (Georgia, USA) were comparable to other wetlands and lake littoral areas. Chlorophyll levels in two marshes were inversely related to water level and phytoplankton at three marshes developed unimodal maxima following macrophyte dieback. Standing stocks in a vernally inundated marsh were greater than a nearby marsh which was permanently inundated; chlorophyll levels displayed longer blooms in the inundated marsh during periods of low rainfall or after drought. Field dynamics, sediment sorption characteristics and algal bioassays suggest that evaporative drawdown stimulates algae by release of nutrients from exposed peat, while high water levels reduce nutrient release from sediments and disperse phytoplankton through flushing. Equilibrium phosphate concentrations of sediments and algal levels were higher at an abandoned rookery than a nearby non-rookery area, indicating nutrient enrichment from residual guano deposits.     

Spatial Analysis of Bifenthrin Sediment Concentrations in California Waterbodies from 2001 to 2010: Identification of Toxic and Non-Toxic Areas

The objective of this article is to summarize and map bifenthrin sediment measurements from California waterbodies from 2001 to 2010 to show sites where bifenthrin has been measured in sediment (including both detected and non-detected concentrations) and where corresponding toxicity or its lack has been reported or predicted. Bifenthrin measurements were available from depositional areas at 359 sites with concurrent total organic carbon (TOC) measurements in California waterbodies and values from approximately 37% of these sites were below the level of detection. Sediment toxicity data based on Hyalella azteca single species ambient toxicity tests were available for 268 sites with concurrent bifenthrin measurements and 62% of these sites showed no significant toxicity. Sixteen percent of the 140 California sites with non-detected bifenthrin concentrations had some significant sediment toxicity thus suggesting that toxicity at these sites is due to factors other than bifenthrin. One percent TOC normalized bifenthrin measurements reported from 268 sites showed no predicted significant toxicity at 83% of the sites based on a comparison with a Hyalella azteca acute value of 6.1 ng/g while 99.3% of the sites showed no predicted significant toxicity based on a Chironomus tentans acute toxicity value of 177.5 ng/g. The test species toxicity data (i.e., Hyalella or Chironomus) used to predict bifenthrin toxicity in the field is therefore critical as the use of Hyalella toxicity data (a highly sensitive species to bifenthrin) may be overprotective and this species is less representative of most California waterbodies when compared with Chironomids.     

Linking nutrient limitation and water chemistry in upland lakes to catchment characteristics

Overbank sedimentation on river floodplains can result in significant reduction of the suspended sediment load transported by a river and can thus represent an important component of the catchment sediment budget. Such conveyance losses will also exert an important influence on sediment-associated contaminant fluxes and budgets. This contribution reports the results of a study of sediment-associated contaminants (i.e. total-P, Cr, Cu, Pb and Zn) fluxes in the River Swale (1346 km²) and River Aire (1002 km²) in Yorkshire, U.K., aimed at quantifying the role of overbank floodplain sedimentation in the sediment-associated contaminant budgets. The catchment of the River Aire is dominated by urban and industrial land use in its middle and lower reaches, whereas the River Swale drains a largely rural catchment, although there is a legacy of metal mining in its headwaters which impacts on heavy metal transport by the river. The results for the River Swale indicate that the conveyance losses associated with the deposition of sediment-associated contaminants on the floodplains bordering the main river can be as high as 47% of the total flux through the main channel system. Equivalent values for the River Aire range up to 26%. Contrasts between the two rivers reflect both the location of the contaminant sources within the catchments and the relative magnitude of the fine sediment deposition fluxes associated with their floodplains.     

Vertical distribution and release characteristics of nitrogen fractions in sediments in the estuaries of Dianchi Lake,China

Columnar sediment samples were collected from five representative estuaries of Dianchi Lake, China. And the vertical distribution of each fraction of nitrogen (IEF-N, CF-N, IMOF-N, OSF-N) were tested. The results showed that the TN content in sediments from areas A, B, C, D and E gradually decreased with depth between 0 and 15 cm, then sharply decreased with depth between 15 and 30 cm and stabilized at depth below 30 cm, indicating the exogenous input of N in these areas has not been controlled effectively. The proportion of TN occupied by various N fractions in the sediments ranked as follows: OSF-N > IMOF > CF-N > IEF-N. Correlation analysis results showed both IEF-N and IMOF-N were significantly correlated with the content of TFe₂O₃ + MnO + Al₂O₃ in deeper sediments, while no correlation in superficial sediments. The areas A and B have extremely high release risks for N in superficial sediments. However, the N in the sediments of areas C, D and E were in relative equilibrium with the overlying water, indicating release potential risk was relatively low.     

Effects of ants on water and soil losses from organically-managed citrus orchards in eastern Spain

Ants can play a key role in the erosion processes on agriculture land by modifying soil properties and increasing macropore flow. Ants are abundant in organically-managed orchards in the Mediterranean region due to climate conditions, no-till practices, no pesticide use, and the resulting vegetation cover. In order to determine the effect of ants on soil and water losses from these orchards growing on moderately-sloped land (4–8%), forty 1.0 m² plots (20 with ants mounts and 20 without ants — controls) were established during the summer of 2007. A rainfall simulator was used to apply 78 mm of water to each plot over a one-hour period, equivalent to a 20-year return-period thunderstorm. Runoff was collected at 1-minute intervals and sediment concentration measured every 10 minutes. Sediment concentrations were 300% higher on plots with ant mounds, but runoff rates were similar to the plots without ants. Average soil erosion rates averaged 41 kg ha⁻¹ h⁻¹ on the ant plots and 13 kg ha⁻¹ h⁻¹ on the control plots. The low erosion rates are due to the effect of the vegetation and litter cover in this organically-managed soil, which were little impacted by ant activity at the pedon scale.     

Influence of bacterial density on the exchange of phosphate between sediment and overlying water

Fluxes of phosphate across the sediment–water interface have been measured using inhibitors of bacterial activity sterilization and chloramphenicol and a control in order to quantify the influence of bacterial abundance on them. Results show that phosphate concentration in the interstitial water decreased when bacteria were present, in relation to treated aquaria. The measured (Jo) and theoretical fluxes (Jd) of phosphate also were higher when bacterial activity was suppressed. Mass balance calculated for Carbon, Nitrogen and Phosphorus in the sediment revealed a loss of theses compounds when bacterial activity was suppressed, and a net accumulation of Carbon and Phosphorus, and loss of Nitrogen under natural conditions.     

Habitat Segregation of a Functional Gene Encoding Nitrate Ammonification in Estuarine Sediments

Distribution and diversity of nrfA gene encoding dissimilatory nitrite reduction to ammonium (DNRA) in the sediments of the Colne River, North Essex, UK, were investigated. Sequencing cloned nrfA fragments amplified from environmental DNA enabled structure analysis of the bacterial community responsible for this pathway. The DNA was extracted from the sediment samples at different depths from the estuary ranging from freshwater to seawater regions, and amplified using specific PCR primer pairs targeting for the nrfA gene. Analysis of the nrfA clones showed two distinct clusters corresponding to their origins, namely, divided into the stable sites (marine and freshwater regions) and the unstable sites (brackish water region), where the tidal rise and fall constantly disturbs the environmental conditions. In addition, the nrfA clones from the deeper layer of the sediment formed a more homogenous community than those from the surface layer of the sediment. This may be due to more isolated and anaerobic conditions kept in the deeper sediment less influenced by the overlying water and other environmental factors. Most of the nrfA clones from the Colne estuarine sediments formed several distinct clusters including known nitrate ammonifiers such as Aeromonas, Shewanella, Desulfovibrio and Sulfurospillum. One of which was, however, related to Bacteroides but still quite divergent (～70% identity) and the rest forming unknown clusters of supposedly uncultured members of bacteria. This is the first trial to describe the nrfA partial sequences derived from a natural environment, with reference to their habitat-specific community structure.