Rgd. Davidsonarnott et al., THE EFFECTS OF ARTIFICIAL PEBBLE CONCENTRATIONS ON EOLIAN SAND TRANSPORT ON A BEACH, Canadian journal of earth sciences, 34(11), 1997, pp. 1499-1508
A field experiment to measure the effects of differing concentrations
of pebbles on rate of eolian sediment transport was carried out on a s
and beach on the Northumberland Strait, New Brunswick. Square ceramic
tiles (0.15 m x 0.15 m) were used to replicate pebbles. These were dep
loyed in a stratified random array in a rectangular plot 5 m wide and
2 m deep at five different concentrations (surface covers of 19, 24, 2
9, 34, and 44%) and both singly (two dimensional) and stacked three hi
gh (three dimensional). An adjacent plot of similar size was left bare
and served as a control. Sediment transport was measured with pairs o
f vertical traps deployed downwind from each plot and wind speed with
three-cup anemometers. Nine data sets totalling 45 runs of 10 min dura
tion each were collected over a total of 4 days. Sediment transport ov
er the tiled plot was normalized against transport over the bare plot.
The results show an increase in sediment transport compared with the
bare surface for the lowest coverage, followed by a continuous decreas
e in transport with increasing coverage up to the maximum coverage emp
loyed. The rate of decrease was greatest for runs that utilized a thre
e-dimensional form, reflecting an increase in the effective area prote
cted. The results confirm laboratory experiments, which suggest that e
rosion and transport are initially enhanced by acceleration of flow ar
ound pebbles and more efficient transport over the hard surface, but t
har this is counteracted at higher coverage densities by the increasin
g area of protected surface.