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l ORC TECHNICAL BULLETIN # IV.3a <br /> 1 <br /> Oxygen Release Compound,ORC® <br /> A Case Study of <br /> Oxygen Distribution in an Aquifer <br /> The most important and frequently asked questions with regard to ORC pertain to how <br /> the oxygen that is released gets distributed into the aquifer Essentially we are asked - <br /> "Where does the oxygen go?", with the implicit understanding that aerobically remediable <br /> compounds will be readily degraded when the oxygen arrives The question can be <br /> answered from either an experimental or a theoretical perspective Experimental <br /> evidence is always best, however, the specific results do not apply universally to all site <br /> conditions Models are therefore employed which attempt to extend the observations <br /> from experimental results to any given case <br /> This Technical Bulletin focuses on actual experimental oxygen distribution data from a <br /> major barrier project, commissioned by the New Mexico Environment Department, for <br /> a site near Albuquerque Technical Bulletin IV 2 discusses the theoretical basis of oxygen <br /> distribution in an aquifer as governed by advection, dispersion, retardation and utilization <br /> iTechnical Bulletin VI 3b presents a series of outputs from the Cleary-Ungs model that <br /> considers these factors and their combined effect on oxygen distribution The complete _ <br /> results of the BTEX remediation, as a function of oxygen availability at the New Mexico <br /> site, are discussed in Technical Bulletin 12c The intent here is to illustrate the isolated <br /> dynamics of oxygen distribution, independent of demand, in answer to the question <br /> "Where does the oxygen go?" <br /> At an abandoned gas station site near Albuquerque (Figure 1 a) a full scale remediation <br /> system was installed consisting of twenty 6-inch ORC® source wells and 54 monitoring <br /> points downgradient of the source wells (Figure lb) The vertical distribution of dissolved <br /> oxygen (DO) and BTEX was measured with probes located 3, 10, and 17 feet below the <br /> water table at the source and at variable depths with the monitoring points A total of 342 <br /> ORC filter socks were installed and the system was monitored to determine changes in <br /> DO and BTEX during the first three months <br /> A large volume of data was collected to determine the interaction between the ORC® <br /> derived oxygen and the existing BTEX plume For the purposes of this discussion, we <br /> will isolate the oxygen distribution as much as possible from the consumption factors - <br /> in order to show that oxygen becomes available and migrates downgradient m an effective <br /> . manner Figure 2a is a contour plot illustrating oxygen status in the study area <br />