Mp. Dearnaley, DIRECT MEASUREMENTS OF SETTLING VELOCITIES IN THE OWEN TUBE - A COMPARISON WITH GRAVIMETRIC ANALYSIS, Journal of sea research, 36(1-2), 1996, pp. 41-47
Over the last two decades the Owen Tube or derivatives of the original
design have been used extensively to determine the settling velocitie
s of suspensions of cohesive material in the field. These gravimetric
measurements have been used as elements of basic research programmes a
nd also as important input parameters for predictions of siltation rat
es. During a two year research programme at HR Wallingford undertaken
between 1989 and 1991 consideration was given to an alternative techni
que for analysing the settling of cohesive material. This technique is
based upon obtaining high magnification video images of the processes
occurring within the settling column. The Video images are then analy
sed using a PC based image analysis system which enables settling velo
cities and floc dimensions to be determined. The technique has been ap
plied on a number of occasions over the past four years and was includ
ed in the European Intercalibration Exercise that took place on the ri
ver Elbe in June 1993. Analysis of the processed field data indicates
flee break-up, reflocculation and the development of significant circu
lations within the settling column during the withdrawal period requir
ed for the gravimetric analysis (typically a duration of about an hour
). The interpretation of the visual data obtained by the video image a
nalysis technique has indicated median settling Velocities significant
ly greater than those obtained from the gravimetric technique. The pap
er describes the field and analysis methods and results from the recen
t intercalibration on the Elbe. During this exercise an experiment was
undertaken whereby video image analysis was done on the results of fi
lming a settling column whilst the standard gravimetric technique was
applied. The paper also discusses the engineering applicability of the
results obtained and raises the question as to which technique provid
es the most representative rate of settlement of flocs in the natural
environment?