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Hydrogeochemical and Biological Processes Affecting the Long‐term Performance of an Iron‐Based Permeable Reactive Barrier
Author(s) -
Zolla Valerio,
Freyria Francesca Stefania,
Sethi Rajandrea,
Di Molfetta Antonio
Publication year - 2009
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq2007.0622
Subject(s) - permeable reactive barrier , zerovalent iron , environmental chemistry , sulfate , chemistry , environmental remediation , groundwater , environmental engineering , contamination , environmental science , geology , adsorption , geotechnical engineering , ecology , organic chemistry , biology
Despite the wide diffusion of zero‐valent iron (Fe 0 ) permeable reactive barriers (PRBs), there is still a great uncertainty about their longevity and long‐term performance. The aim of this study is to investigate the biological and the hydrogeochemical processes that take place at a Fe 0 installation located in Avigliana, Italy, and to derive some general considerations about long‐term performance of PRBs. The examined PRB was installed in November 2004 to remediate a chlorinated solvents plume (mainly trichloroethene and 1,2‐dichloroethene). The investigation was performed during the third year of operation and included: (1) groundwater sampling and analysis for chlorinated solvents, dissolved CH 4 , dissolved H 2 and major inorganic constituents; (2) Fe 0 core sampling and analysis by SEM‐EDS, XRD, and FTIR spectroscopy for the organic fraction; (3) in situ permeability tests and flow field monitoring by water level measurements. The study revealed that iron passivation is negligible, as the PRB is still able to effectively treat the contaminants and to reduce their concentrations below target values. Precipitation of several inorganic compounds inside the PRB was evidenced by SEM‐EDS and XRD analysis conducted on iron samples. Groundwater sampling evidenced heavy sulfate depletion and the highest reported CH 4 concentration (>5000 μg/L) at zero‐valent iron PRB sites. These are due to the intense microbial activity of sulfate‐reducers and methanogens, whose proliferation was most likely stimulated by the use of a biopolymer (i.e. guar gum) as shoring fluid during the excavation of the barrier. Slug tests within the barrier evidenced an apparent hydraulic conductivity two orders of magnitude lower than the predicted value. This occurrence can be ascribed to biofouling and/or accumulation of CH 4 (g) inside the iron filings.This experience suggests that when biopolymer shoring is planned to be used, long‐term column tests should be performed beforehand with initial bacterial inoculation and organic substrate dosing, in order to predict the effects of bacterial overgrowth and gas generation. During construction particular care should be taken in order to minimize the amount of used biopolymer so that complete breakdown can be achieved.