Warren W. Wood

TL;DR: A large-scale natural gradient tracer experiment was conducted on Cape Cod, Massachusetts, to examine the transport and dispersion of solutes in a sand and gravel aquifer as discussed by the authors, where the nonreactive tracer, bromide, and the reactive tracers, lithium and molybdate, were injected as a pulse in July 1985 and monitored in three dimensions as they moved as far as 280 m downgradient through an array of multilevel samplers.

TL;DR: A large-scale natural gradient tracer experiment was conducted on Cape Cod, Massachusetts, to examine the transport and dispersion of solutes in a sand and gravel aquifer as discussed by the authors, where the nonreactive tracer, bromide, and the reactive tracers, lithium and molybdate, were injected as a pulse in July 1985 and monitored in three dimensions as they moved as far as 280 m downgradient through an array of multilevel samplers.

TL;DR: In this paper, the authors applied solute and isotopic methods for evaluating recharge fluxes, runoff, and spatial and temporal distribution of recharge in the Southern High Plains aquifer of Texas and New Mexico.

TL;DR: In this article, a conceptual model of a coastal sabkha near the Arabian Gulf is used as an example to illustrate the various water and solute fluxes, and it is shown that upward flux of ground water from underlying formations could be a major source of solutes in the Sabkha, but contribute only a small volume of the water.

TL;DR: Partial pressures of CO2, O2, N2, and Ar were monitored at two locations in the Ogallala aquifer system on the Southern High Plains of Texas as discussed by the authors.