Controls and predictions of geogenic redox-sensitive contaminants in Danish groundwater
Groundwater is a crucial drinking water source, and maintaining its quality becomes increasingly important as global demand rises. This study examines the spatial distribution and controlling factors of five geogenic groundwater contaminants—arsenic (As), manganese (Mn), iron (Fe), ammonium (NH 4 ), and total phosphorus (P)—across Denmark using classification machine learning models. We trained the models using data from over 7,100 well intakes and 34 spatial covariates related to soil, geology, groundwater level, and recharge. The models achieved area under the curve scores ranging from 0.85 to 0.90. Predicted areas exceeding guideline thresholds for drinking water (As, Mn, Fe, NH 4 ) or ecological ecosystem status (P) cover 14% (As), 78% (Mn), 74% (Fe), 80% (NH 4 ), and 49% (P) of Denmark’s area; more than 60% are classified with high confidence, with uncertainty varying by monitoring density, among other factors. The 2D spatial predictions integrate multi-depth observations and reflect geological and hydrogeological controls. Elevated As levels were mainly associated with glacial meltwater sand and clay aquifers overlying pre-Quaternary marine clays. Feature importance analysis confirms that complex Quaternary layering, confining clay units, and redox-sensitive conditions—particularly in the presence of reactive Fe/Mn oxides and organic matter—drive As mobilization. All five contaminants tend to co-occur spatially under reducing conditions, indicating shared redox-driven release mechanisms. This study shows how national-scale, high-resolution datasets combined with machine learning can predict groundwater quality, aiding well siting and water treatment decisions, and provides transferable insights for regions with similar hydrogeological conditions. • As, Mn, Fe, NH 4 , and total P contaminants mapped across Danish groundwater. • Spatial predictions at 100×100 m resolution with AUC scores between 0.85 and 0.90. • High concentrations are linked to complex Quaternary geologies and redox processes. • High-confidence predictions enable improved groundwater and well management.
- Single Report
15
- 10.2172/781433
- Oct 25, 2000
Pacific Northwest National Laboratory conducted a proof-of-principle test at the Fort Lewis Logistics Center to determine the feasibility of using the innovative remedial technology In Situ Redox Manipulation (ISRM) to treat groundwater contaminated with dissolved TCE. ISRM creates a permeable treatment zone in the subsurface to remediate redox-sensitive contaminants in groundwater. The permeable treatment zone is created by injecting a chemical reducing agent (sodium dithionite with pH buffers) into the aquifer through a well to chemically reduce the naturally occurring ferric iron in the sediments to ferrous iron. Once the reducing agent has been given sufficient time to react with aquifer sediments, residual chemicals and reaction products are withdrawn through the same well. Redox-sensitive contaminants such as TCE, moving in a dissolved-phase plume through the treatment zone, are destroyed. TCE is degraded via reductive dechlorination within the treatment zone to benign degradation products (acetylene, ethylene). Analyses of sediment samples collected from post-test boreholes showed a high degree of iron reduction, which confirmed the effectiveness of the treatment zone.
- Research Article
83
- 10.1071/en04014
- Jan 1, 2005
- Environmental Chemistry
Environmental Context. Groundwater remediation is generally a costly, long-term process. In situ remediation using permeable reactive barriers, through which the groundwaters pass, is a potential solution. For redox-sensitive contaminants in groundwater, a metallic iron barrier (zerovalent iron, ZVI) can immobilize or degrade these dissolved pollutants. Scrap iron materials are a low-cost ZVI material but, because of the wide variation of scrap metal compositions, testing methods for characterizing the corrosion behaviour need to be developed. Abstract. Zerovalent iron (ZVI) has been proposed as reactive material in permeable in situ walls for contaminated groundwater. An economically feasible ZVI-based reactive wall requires cheap but efficient iron materials. From an uranium treatability study and results of iron dissolution in 0.002 M EDTA by five selected ZVI materials, it is shown that current research and field implementation is not based on a rational selection of application-specific iron metal sources. An experimental procedure is proposed which could enable a better material characterization. This procedure consists of mixing ZVI materials and reactive additives, including contaminant releasing materials (CRMs), in long-term batch experiments and characterizing the contaminant concentration over the time.
- Research Article
49
- 10.1007/s11270-005-7420-7
- Mar 1, 2005
- Water, Air, & Soil Pollution
Although permeable reactive barriers (PRB) technology appears to be a very suitable and cost effective option, the extent to which remediation results will be realized, greatly depends on the long-term integrity of the system. The formation of mineral precipitates is possibly a major factor in the long-term performance of PRB. Precipitates may passivate reactive surfaces by blocking electron-transfer sites, and thereby reduce the long-term reactivity of the granular iron to degrade groundwater contaminants. To evaluate the potential passivation impacts of inorganic groundwater chemistry, column experiments containing zero-valent iron (Fe0) were performed under anoxic conditions to treat two contrasting Danish groundwater types spiked with trichloroethylene (TCE). For most of the experiments using Danish groundwater types, a soft low alkalinity groundwater produced slightly higher TCE dechlorination rate than did a hard high alkalinity groundwater. Compared to a soft low alkalinity baseline groundwater, it was also found the dechlorination of TCE in the column was enhanced in the presence of 1 mM CaCO3 and 1 mM NaHCO3. The dechlorination of TCE in the presence of 1 mM KNO3 and 1 mM Na2SiO3 was found to decrease considerably compared with the baseline solution. The results suggest that the composition of field groundwater is likely to strongly affect the ability of Fe0 barriers to degrade TCE.
- Research Article
24
- 10.1016/j.chemosphere.2019.06.039
- Jun 5, 2019
- Chemosphere
Cr(VI) reduction by Fe(II) sorbed to silica surfaces