Longevity of granular iron in groundwater treatment processes: changes in solute transport properties over time.
Although progress has been made toward understanding the surface chemistry of granular iron and the mechanisms through which it attenuates groundwater contaminants, potential long-term changes in the solute transport properties of granular iron media have until now received relatively little attention. As part of column investigations of alterations in the reactivity of granular iron, studies using tritiated water (3H(2)O) as a conservative and non-partitioning tracer were periodically conducted to independently isolate transport-related effects on performance from those more directly related to surface reactivity. Hydraulic residence time distributions (HRTDs) within each of six 39-cm columns exposed to bicarbonate solutions were obtained over the course of 1100 days of operation. First moment analyses of the data revealed generally modest increases in mean pore water velocity (v) over time, indicative of decreasing water-filled porosity. Gravimetric measurements provided independent estimates of water-filled porosity that were initially consistent with those obtained from 3H(2)O tracer tests, although at later times, porosities derived from gravimetric measurements deviated from the tracer test results owing to mineral precipitation. The combination of gravimetric measurements and 3H(2)O tracer studies furnished estimates of precipitated mineral mass; depending on the assumed identity of the predominant mineral phase(s), the porosity decrease associated with solute precipitation amounted to 6-24% of the initial porosity. The accumulation of mineral and gas phases led to the formation of regions of immobile water and increased spreading of the tracer pulse. Application of a dual-region transport model to the 3H(2)O breakthrough curves revealed that the immobile water-filled region increased from initially negligible values to amounts ranging between 3% and 14% of the total porosity in later periods of operation. For the aged columns, mobile-immobile mass transfer coefficients (k(mt)) were generally in the range of 0.1-1.0 day(-1) and reflected a slow exchange of 3H(2)O between the two regions. Additional model calculations incorporating sorption and reaction suggest that although changes in HRTD can have an appreciable effect on trichloroethylene (TCE) transformation, the effect is likely to be minor relative to that stemming from passivation of the granular iron surface.
Department of Geography and Environmental Engineering, The Johns Hopkins University, 313 Ames Hall, 3400 N. Charles St., Baltimore, MD 21218-2686, USA. PeterVikesland@vt.edu
Peter J
PJ
Vikesland
Jörg
J
Klausen
Hubert
H
Zimmermann
A Lynn
AL
Roberts
William P
WP
Ball
D011232:Chemical Precipitation; D005374:Filtration / Q000379:methods; D006801:Humans; D007501:Iron / Q000737:chemistry*; D010539:Permeability; D013997:Time Factors; D014316:Tritium; D014872:Water Movements; D014874:Water Pollutants, Chemical; D018508:Water Purification
D014874:Water Pollutants, Chemical; D014316:Tritium; D007501:Iron