Transfer of trace organic compounds in an operational soil-aquifer treatment system assessed through an intrinsic tracer test and transport modelling

被引:6
作者
Guillemoto, Q. [1 ,2 ]
Picot-Colbeaux, G. [1 ]
Valdes, D. [2 ]
Devau, N. [1 ]
Mathurin, F. A. [1 ]
Pettenati, M. [1 ]
Kloppmann, W. [1 ]
Mouchel, J. -m. [2 ]
机构
[1] Bur Rech Geol & Minieres, French Geol Survey, 3 Ave Claude Guillemin,BP 6009, F-45000 Orleans, France
[2] Sorbonne Univ, CNRS, EPHE, UMR Metis 7619, Paris, France
关键词
Trace Organic Compounds; Soil-aquifer treatment; Reactive transport model; Sorption; Degradation; WASTE-WATER TREATMENT; 3 SELECTED BENZOTRIAZOLES; RIVER BANK FILTRATION; SEASONAL-VARIATIONS; EMERGING CONCERN; SORPTION; FATE; GROUNDWATER; MICROPOLLUTANTS; PHARMACEUTICALS;
D O I
10.1016/j.scitotenv.2022.155643
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil Aquifer Treatment (SAT) can provide supplementary treatment of trace organic compounds (TrOCs) such as phar-maceutical and industrial compounds present in Secondary Treated Wastewater (STWW). Concern on presence of un-regulated TrOCs in natural systems has raised recently as well as the interest in SAT systems for remediation. The present study quantifies, at the field scale over35 m of lateral groundwater flow, the effectiveness of the Agon-Coutainville SAT system (Manche, Normandy, France) for TrOCs removal by sorption and biodegradation through monitoring of seven TrOCs (oxazepam, carbamazepine, benzotriazole, tolyltriazole, caffein, paracetamol, ibuprofen) and major inorganic compounds as intrinsic tracers in STWW and groundwater during a 34-day STWW infiltration ex-periment during operational use of the SAT. Cationic exchanges and mixing between groundwater and STWW during the experiment were highlighted by major ions and geochemical simulations. Due to the low thickness of the unsatu-rated zone, a 1D analytical solution of the advection-dispersion equation (ADE) was applied on chloride data. Chloride was used as conservative intrinsic tracer to calibrate the horizontal flow and transport parameters such as the aquifer dispersion coefficient (D) and the average pore water velocity (nu) allowing estimation of the groundwater residence time. Transport and attenuation of the TrOCs were simulated assuming first-order degradation constant (mu) and linear retardation coefficient (R), calibrated to simulate the observed temporal changes in the breakthrough of TrOCs.
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页数:14
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