Javascript must be enabled to continue!
Sediment Phosphorus Release in a Shallow Eutrophic Reservoir Cove
View through CrossRef
Abstract. Internal phosphorus (P) loading is a leading contributor to eutrophication in reservoirs and can cause harmful algal blooms as well as treatment issues for drinking water reservoirs. Coves are an area of reservoirs that have not received adequate attention, even though they experience higher nutrient and sediment deposition and primary production per unit area when compared to the pelagic zone of the reservoir. This study investigates a shallow eutrophic cove in a northwest Arkansas reservoir called Beaver Lake to better understand the cove’s potential to contribute to P loading and eutrophication within the reservoir. The study period was 3 to 16 July 2018. Water column profiles of depth, temperature, and dissolved oxygen were measured with a floating sensor platform that also contained a weather station. Cove bed sediment samples were collected at three locations in the cove and analyzed for chemical composition through Mehlich III extraction and P, nitrate + nitrite (N+N), and ammonia release rates with aerobic and anaerobic sediment core incubations. Bathymetry data were collected using a depth sonar system. Sensor platform profiles indicated dynamic bottom temperature and dissolved oxygen conditions with transient influxes of hypoxic waters that occurred several times for less than 24 h. The P release rates from bed sediment incubations were as high as 2.02 mg m-2 d-1 under aerobic conditions and 4.45 mg m-2 d-1 under anaerobic conditions. Upon initiation of nitrogen gas bubbling in the sediment cores, anaerobic conditions were delayed by the presence of N+N. Phosphorus release did not occur until denitrification decreased the N+N concentrations enough for reducing conditions to be present. For the study period, a P flux into the water of roughly 1 kg was determined using cove profiles, bathymetry, and P release rates. When compared to whole-lake P release averages for Beaver Lake, eutrophic coves are a disproportionate source of P per unit area within the reservoir. This may offer opportunities for more efficient use of internal loading remediation techniques, such as alum application. The results of this study also suggest that we should not continue to overlook shallow-area bed sediment P flux when considering the P mass balance of a reservoir. Keywords: Eutrophication, Sediment core incubation, Stratification.
American Society of Agricultural and Biological Engineers (ASABE)
Title: Sediment Phosphorus Release in a Shallow Eutrophic Reservoir Cove
Description:
Abstract.
Internal phosphorus (P) loading is a leading contributor to eutrophication in reservoirs and can cause harmful algal blooms as well as treatment issues for drinking water reservoirs.
Coves are an area of reservoirs that have not received adequate attention, even though they experience higher nutrient and sediment deposition and primary production per unit area when compared to the pelagic zone of the reservoir.
This study investigates a shallow eutrophic cove in a northwest Arkansas reservoir called Beaver Lake to better understand the cove’s potential to contribute to P loading and eutrophication within the reservoir.
The study period was 3 to 16 July 2018.
Water column profiles of depth, temperature, and dissolved oxygen were measured with a floating sensor platform that also contained a weather station.
Cove bed sediment samples were collected at three locations in the cove and analyzed for chemical composition through Mehlich III extraction and P, nitrate + nitrite (N+N), and ammonia release rates with aerobic and anaerobic sediment core incubations.
Bathymetry data were collected using a depth sonar system.
Sensor platform profiles indicated dynamic bottom temperature and dissolved oxygen conditions with transient influxes of hypoxic waters that occurred several times for less than 24 h.
The P release rates from bed sediment incubations were as high as 2.
02 mg m-2 d-1 under aerobic conditions and 4.
45 mg m-2 d-1 under anaerobic conditions.
Upon initiation of nitrogen gas bubbling in the sediment cores, anaerobic conditions were delayed by the presence of N+N.
Phosphorus release did not occur until denitrification decreased the N+N concentrations enough for reducing conditions to be present.
For the study period, a P flux into the water of roughly 1 kg was determined using cove profiles, bathymetry, and P release rates.
When compared to whole-lake P release averages for Beaver Lake, eutrophic coves are a disproportionate source of P per unit area within the reservoir.
This may offer opportunities for more efficient use of internal loading remediation techniques, such as alum application.
The results of this study also suggest that we should not continue to overlook shallow-area bed sediment P flux when considering the P mass balance of a reservoir.
Keywords: Eutrophication, Sediment core incubation, Stratification.
Related Results
The Change Law and Formation Cause of Sediment Erosion and Deposition in the Three Gorges Reservoir in the Past 20 Years
The Change Law and Formation Cause of Sediment Erosion and Deposition in the Three Gorges Reservoir in the Past 20 Years
During the past 20 years of the Three Gorges Reservoir impoundment , the incoming water and sediment conditions have changed constantly in the upper reaches of the Three Gorges, re...
Microbial control of sediment phosphorus release along a river-floodplain gradient
Microbial control of sediment phosphorus release along a river-floodplain gradient
Sediment phosphorus release, also referred to as internal loading,  typically delays the response of eutrophic waters to reductions in external nutrient inputs. Internal l...
Quantifying provenance of soil originated from mass movement on soil reservoir-bank using rare earth elements
Quantifying provenance of soil originated from mass movement on soil reservoir-bank using rare earth elements
Abstract:The reservoir-bank collapse has caused soil erosion and bank expansion in the lower Yellow River, which seriously affects the ecological environment and agricul...
Estimation of Sediment Load in Arun River Basin
Estimation of Sediment Load in Arun River Basin
The single sediment rating equation is often used to estimate the suspended load in river, The sediment concentration is assumed as a function of mean daily discharge using a power...
Sediment Transport On The River Bandon, Co. Cork, Ireland
Sediment Transport On The River Bandon, Co. Cork, Ireland
This thesis analyses sediment transport on the River Bandon, Co. Cork, Ireland. Bedload transport and suspended sediment transport were monitored on the River Bandon over an extend...
3D hydro-morphodynamic models as support tools for obtaining sustainable sediment management strategies of reservoirs
3D hydro-morphodynamic models as support tools for obtaining sustainable sediment management strategies of reservoirs
<p>Reservoir sedimentation reduces not only the available storage volume of reservoirs, but may also create other serious problems, such as an increase of bed levels ...
Diffused and localized sediment production processes in a distributed transport model
Diffused and localized sediment production processes in a distributed transport model
<p>The identification of preferential sediment production areas within a river basin is essential to improve predictions of sediment load and its sources, and to iden...
Effects of Soil Conditioners on Absorption of phosphorus by waxy corn and Phosphorus Transformation in High Phosphorus Soils
Effects of Soil Conditioners on Absorption of phosphorus by waxy corn and Phosphorus Transformation in High Phosphorus Soils
In this experiment, the effects of different types of conditioners and their application on the absorption and transformation of phosphorus in high phosphorus soils in facilities w...

