Studies on turbulent diffusion processes and evaluation of diffusivity values from hydrodynamic observations in Corpus Christi Bay

The physical process of dispersion which can be attributed to turbulence (turbulent diffusion) or shear (shear-augmented diffusion) within the flow field is very important as it ultimately governs the distribution of constituents of interest within the environment. A series of diffusion experiments were conducted in Corpus Christi Bay, TX with the purpose of characterizing turbulent diffusion through dispersion coefficients or turbulent diffusivity, Ki (i=x, y, z) dependent on the degree of randomness or turbulence intensity, I. ed with a boat-mounted acoustic doppler current profiler (ADCP), the Eulerian velocity time-series of fluid particles in random motion, ui was used in the evaluation of the Eulerian time-scale of turbulence, TE based on the velocity correlation function, RE with TE being related to the Lagrangian time-scale TL through a scaling parameter, β(=TL/TE). Surface currents were obtained with high frequency (HF) Radar equipment deployed over the study area from which the horizontal velocity gradients were determined. the spatial scale of the experiment (∼1000 m), the observed low horizontal gradients (∼10−4 s−1) allowed for the generation of velocity time-series from an ADCP mounted on a moving platform. A numerical scheme for evaluating turbulent diffusivity values ( K i = β u ′ i 2 ¯ T E ) was developed on the basis of Eulerian current measurements and calibrated through the statistics of an evolving dye patch for the scaling parameter β which in this scheme was found to be in the range 1–3.