Estimation of spatially variable residual nonaqueous phase liquid saturations in nonuniform flow fields using partitioning tracer data

Citation
Ai. James et al., Estimation of spatially variable residual nonaqueous phase liquid saturations in nonuniform flow fields using partitioning tracer data, WATER RES R, 36(4), 2000, pp. 999-1012
Citations number
27
Categorie Soggetti
Environment/Ecology,"Civil Engineering
Journal title
WATER RESOURCES RESEARCH
ISSN journal
00431397 → ACNP
Volume
36
Issue
4
Year of publication
2000
Pages
999 - 1012
Database
ISI
SICI code
0043-1397(200004)36:4<999:EOSVRN>2.0.ZU;2-1
Abstract
Estimates of spatially variable residual NAPL saturations S-N are obtained in heterogeneous porous media using first temporal moments of breakthrough curves (BTCs) obtained from multilevel samplers during in situ partitioning tracer tests. An approach is adopted in which the distribution of the log NAPL/water volumetric ratio (Y = In [S-N/(1 - S-N)]) and log hydraulic cond uctivity (F = ln K) are treated as spatially correlated random fields. A no nlinear Gauss-Newton search technique is used,to identify the spatial distr ibution of Y that minimizes the weighted sum of the deviation of the tempor al moment predictions from their measured values and the deviation of the e stimate of Y from its prior estimate obtained from the temporal moments of extraction well BTCs. Sensitivities required for the algorithm are obtained using a coupled flow and transport adjoint sensitivity method. In addition to obtaining optimal estimates for the spatial distribution of Y, the meth od also provides the estimation error covariance. The estimation error cova riance can be used to evaluate the information that may be obtained from al ternate pumping and monitoring configurations for tracer tests designed to detect NAPL in the subsurface. To this end, we tested the method using two different NAPL distributions (one with a random spatially correlated field and a second that was a block of NAPL) and three different pumping configur ations (a double five-spot pattern, an inverted double five-spot pattern, a nd a line-drive pattern). The results show that measured temporal moments a re more sensitive to Yin the double five-spot and inverted double five-spot patterns, and estimates produced in these configurations are slightly supe rior to those produced in the line-drive pattern.