USGS · 70023806
Evaluation of longitudinal dispersivity estimates from forced-gradient tracer tests in heterogeneous aquifers
Abstract
Converging radial-flow and two-well tracer tests are simulated in two-dimensional aquifers to investigate the effects of heterogeneity and forced-gradient test configuration on longitudinal dispersivity (??L) estimates, and to compare ??L estimates from forced-gradient tests with ??L values that characterize solute spreading under natural-gradient flow. Results indicate that in both mildly and highly heterogeneous aquifers, ??L estimates from two-well tests are generally larger than those from radial-flow tests. In mildly heterogeneous aquifers, ??L estimates from two-well tests with relatively large tracer transport distances are similar to ??L values from natural-gradient simulations. In highly heterogeneous aquifers, ??L estimates from two-well tests at all tracer transport distances are typically smaller than ??L values from natural-gradient simulations.
Explore related subjects
Keep this discovery
Explore connections, maps & timelines
C. R. Tiedeman, P. A. Hsieh. 2002. Evaluation of longitudinal dispersivity estimates from forced-gradient tracer tests in heterogeneous aquifers. https://pubs.usgs.gov/publication/70023806
Cite the original work for its findings. Save a collection to share your selection of sources.