Experimental results showed energy-efficient pseudohomogeneous-like fl
ow behaviour when a mixture of coarse (20-200 mm) granite rock in tar
sand tailings (-1 mm) in mass proportions 1:9 was transported at a tot
al volumetric solids concentration of 31% in a 0.44 m i.d. (D) pipelin
e loop. Similar results were obtained with an industrially comminuted
copper ore (-100 mm; mass median particle size 0.75 mm) when pumped in
a 0.2 m i.d. pipe at a concentration of 39%. The partially-stratified
friction loss model proposed by K.C. Wilson, G.R. Addie and R. Clift,
Slurry Transport Using Centrifugal Pumps, Elsevier, Oxford, 1992 [1]
predicted well the observed losses of an iron ore (relative solids den
sity 4.1, mass median particle size 0.42 mm) at a concentration of 23%
(D=0.1 m). With a slightly heavier and coarser iron ore the model ten
ded to underestimate losses at concentrations of 14-29%. The favourabl
e friction loss performance in some results may demonstrate how broad
particle size distributions and high concentrations may cause reduced
pipe wall friction without influence of true rheological mechanisms. A
n alternative way of characterizing experimental data in terms of exce
ss pressure gradient versus the ratio of mean velocity to hindered set
tling velocity is introduced. The flow conditions discussed here corre
spond to velocities that clearly exceed those for which there are risk
s of deposition at the bottom of the pipe.