Submarine ground water discharges (SGD) around the coasts of the Yucatan Peninsula are very common due to the karstic origin of the rocks, and the abundant rain. These discharges of brackish water into the coastal sea are strong enough to alter the thermohaline conditions, they can be preferential routes for salt intrusion, and also represent an important input of nutrients and pollutants. The mixing on these SGDs is a spontaneous and turbulent process, and its study is important for the understanding of dispersion of materials in regions influenced by these features. A set of measurements with two acoustic Doppler velochneters (Nortek-Vector) were done in a very active SGD in the coast of Quintana Roo, Mexico. The first instrument was installed in the entrance of the cave and the other one similar to 2m above, both sampling at 64 Hz. Consistent with previous studies, results show that sea level variability (waves and tides) dominates the flow and the turbulence levels. When the spring is inactive wave frequencies (short 0.1 Hz, and 0.03 Hz long waves) have a clear peak in eta i and w, but when the spring is active, turbulence (Kolmogorov law) permeates to short wave frequencies, and IG frequencies diminish in 11, but bulge in w at lower frequencies (0.01 Hz). Numerical modelling with Open Foam suggests that the shift in IG frequency could be driven by the spring geometry (depth and cave size) rather than forced by the incident waves.
