Efficient and predictable recovery of viruses from water by small scale ultrafiltration systems

2001 ◽  
Vol 47 (11) ◽  
pp. 1033-1041 ◽  
Author(s):  
L J Winona ◽  
A W Ommani ◽  
J Olszewski ◽  
J B Nuzzo ◽  
K H Oshima
Keyword(s):  
Surface Water ◽  
Hollow Fiber ◽  
Size Exclusion ◽  
Small Scale ◽  
Filter Surface ◽  
Water Conditions ◽  
Single Method ◽  
Waterborne Virus ◽  
Viral Adsorption ◽  
Elution Step

Current methods to concentrate viruses from large volumes of water are prone to inconsistent results and are costly and complex procedurally. Ultrafiltration can utilize size exclusion rather than adsorption and (or) elution to concentrate viruses and, therefore, may offer greater flexibility in developing methods that can provide more consistent recoveries among different viruses and widely varying water conditions. Two small scale ultrafiltration systems (hollow fiber and tangential flow) were tested with a virus suspended in 2 L of reagent grade, tap, ground, or surface water. Three model viruses were used (bacteriophages PP7 and T1 and poliovirus) to compare and characterize the recovery of viruses with the two ultrafiltration systems. Pretreatment of the ultrafilters with blocking agents and the use of elution agents can serve to prevent viral adsorption to the filter surface or to elute bound virus and keep viral agents suspended in the retentate. The use of a blocking and elution step concentrated viruses (>60% recovery) from widely varying water qualities, including surface water, such that a single method can be used to efficiently concentrate viruses from all of the water types tested. Both ultrafiltration systems appear to be able to efficiently recover viruses; however, the hollow fiber systems provided slightly better results in the 2-L volumes tested.Key words: ultrafiltration, waterborne virus, poliovirus, enterovirus.

Managing the impacts of mining on Ghana’s water resources from a legal perspective

2018 ◽  
Vol 1 (3) ◽  
pp. 156-165 ◽  
Author(s):  
Nasirudeen Abdul Fatawu
Keyword(s):  
Surface Water ◽  
Water Resources ◽  
Environmental Protection Agency ◽  
Large Scale ◽  
Small Scale ◽  
Mining Activities ◽  
Protection Agency ◽  
Environmental Laws ◽  
Mining Areas ◽  
Legal Perspective

Recent floods in Ghana are largely blamed on mining activities. Not only are lives lost through these floods, farms andproperties are destroyed as a result. Water resources are diverted, polluted and impounded upon by both large-scale minersand small-scale miners. Although these activities are largely blamed on behavioural attitudes that need to be changed, thereare legal dimensions that should be addressed as well. Coincidentally, a great proportion of the water resources of Ghana arewithin these mining areas thus the continual pollution of these surface water sources is a serious threat to the environmentand the development of the country as a whole. The environmental laws need to be oriented properly with adequate sanctionsto tackle the impacts mining has on water resources. The Environmental Impact Assessment (EIA) procedure needs to bestreamlined and undertaken by the Environmental Protection Agency (EPA) and not the company itself.

Surface-Water Conditions in Georgia, Water Year 2005

Data Series ◽  
10.3133/ds252 ◽  
2007 ◽  
Author(s):  
Jaime A. Painter ◽  
Mark N. Landers
Keyword(s):  
Surface Water ◽  
Water Conditions

Experimental investigation on water quality standard of Yangtze River water source heat pump

2012 ◽  
Vol 66 (5) ◽  
pp. 1103-1109 ◽  
Author(s):  
Zenghu Qin ◽  
Mingwei Tong ◽  
Lin Kun
Keyword(s):  
Water Quality ◽  
Surface Water ◽  
River Water ◽  
Heat Pump ◽  
Yangtze River ◽  
Water Source ◽  
Quality Standard ◽  
Heat Pumps ◽  
The Yangtze River ◽  
Water Conditions

Due to the surface water in the upper reaches of Yangtze River in China containing large amounts of silt and algae, high content of microorganisms and suspended solids, the water in Yangtze River cannot be used for cooling a heat pump directly. In this paper, the possibility of using Yangtze River, which goes through Chongqing, a city in southwest China, as a heat source–sink was investigated. Water temperature and quality of the Yangtze River in the Chongqing area were analyzed and the performance of water source heat pump units in different sediment concentrations, turbidity and algae material conditions were tested experimentally, and the water quality standards, in particular surface water conditions, in the Yangtze River region that adapt to energy-efficient heat pumps were also proposed. The experimental results show that the coefficient of performance heat pump falls by 3.73% to the greatest extent, and the fouling resistance of cooling water in the heat exchanger increases up to 25.6% in different water conditions. When the sediment concentration and the turbidity in the river water are no more than 100 g/m3 and 50 NTU respectively, the performance of the heat pump is better, which can be used as a suitable river water quality standard for river water source heat pumps.

scholarly journals Monitoring Lakes Surface Water Velocity with SAR: A Feasibility Study on Lake Garda, Italy

2021 ◽  
Vol 13 (12) ◽  
pp. 2293
Author(s):  
Marina Amadori ◽  
Virginia Zamparelli ◽  
Giacomo De Carolis ◽  
Gianfranco Fornaro ◽  
Marco Toffolon ◽  
...  
Keyword(s):  
Surface Water ◽  
Wind Waves ◽  
Test Site ◽  
Water Velocity ◽  
Surface Velocity ◽  
Medium Size ◽  
Small Scale ◽  
Lake Garda ◽  
Marine Applications

The SAR Doppler frequencies are directly related to the motion of the scatterers in the illuminated area and have already been used in marine applications to monitor moving water surfaces. Here we investigate the possibility of retrieving surface water velocity from SAR Doppler analysis in medium-size lakes. ENVISAT images of the test site (Lake Garda) are processed and the Doppler Centroid Anomaly technique is adopted. The resulting surface velocity maps are compared with the outputs of a hydrodynamic model specifically validated for the case study. Thermal images from MODIS Terra are used in support of the modeling results. The surface velocity retrieved from SAR is found to overestimate the numerical results and the existence of a bias is investigated. In marine applications, such bias is traditionally removed through Geophysical Model Functions (GMFs) by ascribing it to a fully developed wind waves spectrum. We found that such an assumption is not supported in our case study, due to the small-scale variations of topography and wind. The role of wind intensity and duration on the results from SAR is evaluated, and the inclusion of lake bathymetry and the SAR backscatter gradient is recommended for the future development of GMFs suitable for lake environments.

Effect of small-scale illegal mining on surface water and sediment quality in Ghana

2021 ◽  
pp. 1-26
Author(s):  
Humphrey Ferdinand Darko ◽  
Anthony Yaw Karikari ◽  
Anthony Appiah Duah ◽  
Bismark Awinbire Akurugu ◽  
Victor Mante ◽  
...  
Keyword(s):  
Surface Water ◽  
Sediment Quality ◽  
Small Scale ◽  
Illegal Mining ◽  
Water And Sediment ◽  
Water And Sediment Quality

scholarly journals Investigating patterns and controls of groundwater up-welling in a lowland river by combining Fibre-optic Distributed Temperature Sensing with observations of vertical hydraulic gradients

2012 ◽  
Vol 16 (6) ◽  
pp. 1775-1792 ◽  
Author(s):  
S. Krause ◽  
T. Blume ◽  
N. J. Cassidy
Keyword(s):  
Surface Water ◽  
Water Exchange ◽  
Structural Heterogeneity ◽  
Temperature Sensing ◽  
Small Scale ◽  
Lowland River ◽  
Fibre Optic ◽  
Distributed Temperature Sensing ◽  
Hydraulic Gradients ◽  
Cold Spots

Abstract. This paper investigates the patterns and controls of aquifer–river exchange in a fast-flowing lowland river by the conjunctive use of streambed temperature anomalies identified with Fibre-optic Distributed Temperature Sensing (FO-DTS) and observations of vertical hydraulic gradients (VHG). FO-DTS temperature traces along this lowland river reach reveal discrete patterns with "cold spots" indicating groundwater up-welling. In contrast to previous studies using FO-DTS for investigation of groundwater–surface water exchange, the fibre-optic cable in this study was buried in the streambed sediments, ensuring clear signals despite fast flow and high discharges. During the observed summer baseflow period, streambed temperatures in groundwater up-welling locations were found to be up to 1.5 °C lower than ambient streambed temperatures. Due to the high river flows, the cold spots were sharp and distinctly localized without measurable impact on down-stream surface water temperature. VHG patterns along the stream reach were highly variable in space, revealing strong differences even at small scales. VHG patterns alone are indicators of both, structural heterogeneity of the stream bed as well as of the spatial heterogeneity of the groundwater–surface water exchange fluxes and are thus not conclusive in their interpretation. However, in combination with the high spatial resolution FO-DTS data we were able to separate these two influences and clearly identify locations of enhanced exchange, while also obtaining information on the complex small-scale streambed transmissivity patterns responsible for the very discrete exchange patterns. The validation of the combined VHG and FO-DTS approach provides an effective strategy for analysing drivers and controls of groundwater–surface water exchange, with implications for the quantification of biogeochemical cycling and contaminant transport at aquifer–river interfaces.

Nanocomposite hollow fiber nanofiltration membranes: Fabrication, characterization, and pilot‐scale evaluation for surface water treatment

2019 ◽  
Vol 136 (45) ◽  
pp. 48205 ◽  
Author(s):  
Gulsum Melike Urper‐Bayram ◽  
Burcu Sayinli ◽  
Reyhan Sengur‐Tasdemir ◽  
Turker Turken ◽  
Enise Pekgenc ◽  
...  
Keyword(s):  
Water Treatment ◽  
Surface Water ◽  
Hollow Fiber ◽  
Pilot Scale ◽  
Nanofiltration Membranes ◽  
Scale Evaluation ◽  
Surface Water Treatment

Sensitivity Analysis of Hyporheic Exchange to Small Scale Changes In Gravel-Sand Flumebed Using A Coupled Groundwater-Surface Water Model

2020 ◽  
Author(s):  
Md Abdullah Al Mehedi ◽  
Nora Reichert ◽  
Frank Molkenthin
Keyword(s):  
Sensitivity Analysis ◽  
Surface Water ◽  
Reactive Transport ◽  
Time Integration ◽  
Longitudinal Direction ◽  
Numerical Approach ◽  
Hyporheic Exchange ◽  
Water Model ◽  
Small Scale ◽  
Flume Experiments

<p>Distribution of the hyporheic streamlines and residence time (HRT) is a crucial factor under streambed to understand the transport phenomena of environmental toxins, sediment metabolic rates in fluvial ecology as well as hydrological water budget. To quantify HRT, both the laboratory and numerical approach could serve as discerning tools. However, due to high heterogeneity in natural streambed sediment and topography, an efficient numerical model setup can prove to be pragmatic in comparison to tedious laboratory experiments for tracing streamlines. Moreover, repeatability of results, high amount of variation in the laboratory flumebed setup, greater insight into the 3D flow system and investigation possibilities with regard to individual streamlines or particular areas of HRT distribution cannot be well executed in laboratory. On the other hand, an automated generation of hyporheic streamlines with a range of various flumebed setups could propel a better understanding of the process and behavior of hyporheic streamlines and HRT distribution. Therefore, a robust numerical method could bestow to trace a large number of particles from various seeding locations at the flumebed. All of these facts enforce the necessity of numerical modeling of flume experiments to perceive the hyporheic exchange mechanisms at fieldwork and research, which are difficult to segregate under natural in-stream conditions. Keeping these issues in mind, we developed an automated numerical  method for quantifying the hyporheic exchange, where the surface water modeling software, HEC-RAS 5.0.5 and the subsurface flow and reactive transport code, MIN3P are coupled. A channel segment with a longitudinal dimension of 1 m and water surface elevation of 0.02 m is used for generating the hydraulic head distribution over the flumebed. A groundwater model domain of the dimensions of x:y:z = 1m:0.1m:0.1m is considered for the investigation of hyporheic exchange. A simple code for computing streamlines based on 4th order Runge-Kutta technique with the adaptive time integration method is developed using Matlab. Sensitivity analysis of streamline distribution and HRT to small scale changes (e.g. changes in dimension, distribution, and shape of the flumebed material) was performed, assuming a sand-gravel material mix. Various geometric shapes of gravel pieces (e.g. triangle, rectangle, trapezoid, and sphere) were used to vary the elevation of flumebed on a 1 mm scale. The results of the automated process show that the size, shape and distribution of trapezoidal gravel and sand portion in the streambed have a significant impact over hyporheic streamlines and HRT. High number and length of streamlines thus high HRT are found in case of the higher length of ridges created by the elevated portion of gravel pieces. In case of the increase of the length of gravel pieces along the longitudinal direction of flumebed, the length of streamlines and HRT decrease whereas the number of streamlines increase. Small scale hyporheic exchanges are found in case of increasing length of gravel pieces. Similar outcomes are also found for triangular and spherical gravel pieces. Both the number and length of streamlines are significantly reduced in case of the high number of gravel and sand portion on the streambed.</p>

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