An evaluation of horizontal recirculation using single-well tests, pumpingtests, tracer tests, and the colloidal borescope

Extensive hydrodynamic testing was performed as part of a program to evalua te horizontal recirculation as a means of removing contaminants from thin, interbedded aquifers. Two test sites, each containing a pair of horizontal recirculation wells, were evaluated using various hydraulic tests. Results of these evaluations showed that ground water was intercepted more than 100 feet beyond the wells. and that the hydraulic gradient increased by more t han two orders of magnitude. Aquifer heterogeneity: however, controlled the efficiency and uniformity of ground water flow Heterogeneity was assessed with a variety of techniques. Bromide tracer tests and the colloidal boresc ope provided the most useful data. For example, at an uncontaminated site, the leading edge of the bromide tracer traversed the 100 feet between the i njection and extraction wells in 21 hours, and the peak bromide concentrati on was observed in 2.6 days, compared with the four days predicted by a pum ping test. The resulting maximum velocity calculation was consistent with m easurements made with the borescope in preferential flow zones. Data obtain ed from a highly contaminated location indicated that assessments of aquife r heterogeniety are further complicated by the presence of DNAPL. Very low flow occurred in a highly contaminated zone, despite the fact that litholog ic descriptions indicated that this region contained permeable sand and gra vel.