| | Estimating nonaqueous phase liquid spatial variability using |
| | 0,91 | | MB | partitioning tracer higher temporal moments |
| | 19 | | stron |
| | 6497 | | ID | College of Engineering, University of Florida |
| | 2003 | | rok |
| | The use of interwell partitioning tracers to quantify the amount of nonaqueous phase liquid (NAPL) |
| | in porous media has been demonstrated in several laboratory and field tests. The primary emphasis |
| | of work to date has been on the use of first temporal moments of tracer breakthrough curve (BTC) |
| | data to estimate the average NAPL saturation. Here we extend the data analysis to the use of |
| | tracer BTC second and third temporal moments to estimate the statistical parameters characterizing |
| | the NAPL spatial distribution. In particular, we examine the fraction f of the streamlines that |
| | contain NAPL and the mean and standard deviation of the distribution of streamline |
| | trajectoryaverage NAPL saturations. Two models are presented based on discretizing tracer swept |
| | volumes into contaminated and uncontaminated zones. The models are applied to data from three- |
| | dimensional numerical simulations, two-dimensional flow laboratory experiments, and field tests at |
| | two sites (Hill Air Force Base, Utah, and a dry cleaner in Jacksonville, Florida). For all cases |
| | considered here, good agreement was found between expected (measured) and estimated values of |
| | f, the fraction of the tracer swept zone that contained NAPL. The effects of nonlinear and |
| | nonequilibrium partitioning as well as correlations between NAPL saturation and saturated hydraulic |
| | conductivity are also considered. INDEX TERMS: 1829 Hydrology: Groundwater hydrology; 1831 |
| | Hydrology: Groundwater quality; 1832 Hydrology: Groundwater transport; KEYWORDS: |
| | groundwater hydrology, groundwater quality, groundwater transport Estimating nonaqueous phase |
| | liquid spatial variability using partitioning tracer higher temporal moments |