Gc. Nanson et al., EXPERIMENTAL MEASUREMENTS OF RIVER-BANK EROSION CAUSED BY BOAT-GENERATED WAVES ON THE GORDON RIVER, TASMANIA, Regulated rivers, 9(1), 1994, pp. 1-14
Erosion of natural river banks by boat-generated waves is an increasin
gly serious problem on the navigable reaches of many rivers, particula
rly on the middle and estuarine reaches. An experiment designed to lin
k bank erosion rates with easily measured wave characteristics, conduc
ted on the scenic lower Gordon River in Tasmania, provides information
useful for river management. Within a boat-generated wave train a num
ber of characteristics were measured and most showed a high correlatio
n with measured rates of bank retreat. Maximum wave height within the
train is the simplest measure and is associated with a major threshold
in erosive energy on unconsolidated sandy alluvium at wave heights of
30 to 35 cm. At maximum wave heights above 35 cm all but the most res
istant bank sediments erode. Reducing maximum wave heights to < 30 cm
by limiting boat speeds, and reducing the frequency of boat passages,
caused a dramatic decline in bank erosion along the river.