This study evaluates a treatment system centered on forward osmosis (FO) to extract high-quality water from real brackish groundwater and wastewater. The groundwater had salinity of 4 g/L, while the wastewater sample consisted of a secondary effluent. These feed solutions were treated first in a FO step, achieving a recovery of >60%. Subsequently, the diluted draw solutions were subject to a nanofiltration (NF) step to regenerate their original osmotic pressure and to simultaneously collect a final permeate product. Magnesium chloride and sodium sulfate were both suitable draw solutes for this application. MgCl had a larger specific reverse salt flux and induced a more pronounced fouling-related flux decline with groundwater samples. NaSO was re-concentrated with a higher permeability NF membrane but may require the use of anti-scalants. The average fluxes obtained in high-recovery batch FO were between 5 and 11 L mh with an initial bulk draw osmotic pressure in the range of 12-15 bar. Relatively low flux decline was observed in fouling experiments with both samples, while physical cleaning proved promising to recover the related loss in productivity. The final product waters were all of very high quality, suggesting the potential of this coupled system for water reuse and desalination. Some challenges related to the relatively low water flux in the FO step, as well as the loss of draw solutes and the gradual change in composition of the draw solution, need further analysis to establish the technical and economic feasibility of the system.
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http://dx.doi.org/10.1016/j.watres.2019.01.014 | DOI Listing |
Microb Ecol
January 2025
MikroIker Research Group, Immunology, Microbiology and Parasitology Department, Faculty of Pharmacy, University of the Basque Country UPV/EHU, Paseo de La Universidad 7, 01006, Vitoria-Gasteiz, Spain.
The Añana Salt Valley (northern Spain) is a continental saltern consisting of a series of natural springs that have been used for salt production for at least 7000 years. This habitat has been relatively understudied; therefore, prokaryotic diversity was investigated through Illumina-based 16S rRNA gene sequencing to determine if the waters within the valley exhibit distinctive microbiological characteristics. Two main types of water were found in the valley: salty (approximately 200 g/L salinity) from the diapiric structure and brackish (≤ 20 g/L salinity) from shallow streams.
View Article and Find Full Text PDFMicroorganisms
November 2024
School of Earth System Science, Tianjin University, Tianjin 300072, China.
Contained arsenic (As) and unsafe brackish groundwater irrigation can lead to serious As pollution and increase the ecological risk in cultivated soils. However, little is known about how Fe oxides and microbes affect As migration during soil irrigation processes involving arsenic-contaminated brackish groundwater. In this study, the samples (porewater and soil) were collected through the dynamic soil column experiments to explore the As migration process and its effect factors during soil irrigation.
View Article and Find Full Text PDFEnviron Monit Assess
December 2024
US Geological Survey, Water Resources Mission Area, Moffett Field, CA, USA.
The US Geological Survey (USGS) is selecting and prioritizing basins, known as Integrated Water Science basins, for monitoring and intensive study. Previous efforts to aid in this selection process include a scientifically defensible and quantitative assessment of basins facing human-caused water resource challenges (Van Metre et al. in Environmental Monitoring and Assessment, 192(7), 458 2020).
View Article and Find Full Text PDFEnviron Geochem Health
December 2024
School of Water and Environment, Key Laboratory of Subsurface Hydrology and Ecological Effect in Arid Region of Ministry of Education, Chang'an University, Xi'an, Shaanxi, China.
With the excellent water quality, abundant water quantity and convenient and economical exploitation conditions, groundwater has become an important water source for the social and economic development and people's livelihood in the northeast margin of the Tibetan Plateau in China. This study employed geostatistics, mineral saturation index, Gibbs diagram, ion ratio coefficient, chloralkali index and other methods to reveal the chemical distribution characteristics, evolution law and hydrogeochemical formation mechanism of groundwater in the northeastern margin of the Tibetan Plateau. The results showed that the contents of main chemical components of groundwater in Beichuan increased continuously from 1980 to 2020 complicating the types of hydrochemistry due to intensive groundwater exploitation and potential pollution from chemical plants.
View Article and Find Full Text PDFHuan Jing Ke Xue
December 2024
College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China.
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