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In this context, recent studies have reported the triazole ring to bridge electron-donor and -acceptor groups as part of charge-transfer conduits in solution.
Solute transport in karst aquifers is primarily constrained to solution conduits where transport is rapid, turbulent, and relatively unrestrictive.
Solute transport in karst aquifers is primarily constrained to relatively complex and inaccessible solution conduits where transport is often rapid, turbulent, and at times constrictive.
Physical nonequilibrium models to fit breakthrough curves for tracer tests in solution conduits are now routinely employed.
Breakthrough curves generated from tracer tests in solution conduits are typically positively-skewed with long tails evident.
The PCNE model allows for partitioning open space in solution conduits into mobile and immobile flow regions with first-order mass transfer between the two regions to represent physical nonequilibrium in the conduit.
A two-region nonequilibrium model was used to calibrate initial solute-transport parameter estimates generated from tracer-breakthrough curves (TBCs) developed from tracer tests conducted in uni-axial solution conduits in karstic aquifers.
The geophysical measurements suggest the presence of a zone of low electrical resistivity (from ERI) and low electromagnetic wave velocity (from GPR) below the water table at depths of 4 9 m that corresponds to the depth of solution conduits seen in digital borehole images.
Where there is faulting, fracture density and the opportunity for conduits to develop through solution processes increase.
Mobile devices offer a promising solution as a conduit for behavioral intervention programs.
Accordingly, we find the solution with a conduit radius of 16 m to be the most fitting of the solutions shown in Fig. 5(b).
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