V43E-4935:
Mapping Densities in Analogue Laboratory Turbulent Plumes Using Dye Concentration
Abstract:
Changing tephra concentration in volcanic eruption columns is difficult to measure in the field dueto fluid opacity. The bulk fluid erupted may be higher density than the surrounding atmosphere at
the vent and then transition to positive buoyancy through the ingestion and heating of ambient air;
thus, the concentration of the plume fluid as it rises is critical to determining whether the material
rises in a sustained plume or collapses into a pyroclastic density current. We evaluate the changing
concentration of an analogue plume via tracer dye intensity and relate it to plume radius expansion and
vent distance. To calibrate our concentration metric, we calculated the density and dye concentration
of pre-determined tracer-water mixtures. The density of the solution was directly measured using a
micropipette and high precision balance. The calculated density falls within the standard error of the
measured density for each step. Five photographs were taken of each concentration using a mounted
Ex-FH100 digital camera with identical lighting. Using a MATLAB script, the RGB (Red-Green-Blue) color
value was extracted from five pixels located at the same coordinates in each image, confirming that
there was no inherent error caused by the camera and that the RGB value was the same across an
entire image. We created a color map to convert from the RGB color value of a pixel in an image to
its corresponding concentration. This method algorithm can then be applied to an analogue volcanic
tank model, using the color variations in the plume eddies to determine the tracer concentration, and
thereby density distribution, in the plume.