Regarding the potential for desorption, chemical conditions in this zone are expected to be fairly constant, and therefore desorption events, generally driven by chemical perturbations such as an increase in pH [ 57 ], may not be significant.
← all excerpts
Comparing the Fate and Transport of MS2 Bacteriophage and Sodium Fluorescein in a Karstic Chalk Aquifer.
2
—
—
The sentences
The very large reduction in the tracer mass ratio value from the injection site to ABH1 suggests that the magnitude of phage loss relative to the solute tracer along this flow path is highly significant.