Mass-Transfer Limitations for Nitrate Removal in a Uranium-Contaminated Aquifer

摘要

A field test on in situ subsurface bioremediation of uranium(VI)is underway at the Y-12 National Security Complex in the Oak Ridge Reservation,Oak Ridge,TN.Nitrate has a high concentration at the site,which prevents U(VI)reduction,and thus must be removed.An acidic-flush strategy for nitrate removal was proposed to create a treatment zone with low levels of accessible nitrate.The subsurface at the site contains highly interconnected fractures surrounded by matrix blocks of low permeability and high porosity and is therefore subjectto preferential flow and matrix diffusion.To identify the heterogeneous mass transfer properties,we performed a novel forced-gradient tracer test,which involved the addition of bromide,the displacement of nitrate,and the rebound of nitrate after completion of pumping.The simplest conceptualization consistent with the data is that the pore-space consists of a single mobile domain,as well as a fast and a slowly reacting immobile domain.The slowly reacting immobile domain(shale matrix)constitutes over 80% of the pore volume and acts as a long-term reservoir of nitrate.According to simulations,the nitrate stored in the slowly interacting immobile domain in the fast flow layer,at depths of about 12.2-13.7 m,will be reduced by an order of magnitude over a period of about a year.By contrast,the mobile domain rapidly responds to flushing,and a low average nitrate concentration can be maintained if the nitrate is removed as soon as it enters the mobile domain.A field-scale experiment in which the aquifer was flushed with acidic solution confirmed our understanding of the system.For the ongoing experiments on mierobial U(VI)reduction,nitrate concentrations must be low in the mobile domain to ensure U(VI)reducing conditions.We therefore conclude that the nitrate leaching out of the immobile pore space must continuously be removed by in situ denitrification to maintain favorable conditions.