
impact of a single particle with a surface. The angle determines the relative magnitude of
the two velocity components of the impact, namely the component normal to the surface
and the one parallel to the surface. The normal component will determine how long the
impact will last, that is, the contact time, t
c
, and the load. The product of t
c
and the tan-
gential velocity component determine the amount of sliding that takes place. The tangen-
tial velocity component also provides a shear loading to the surface, which is in addition to
the normal load related to the normal component of the velocity. Therefore, as the angle
changes, the amount of sliding that takes place also changes, as does the nature and mag-
nitude of the stress system. Both of these aspects influence the way a material wears. These
changes would also imply that different types of materials would exhibit different angular
dependencies as well.
As can be seen in Fig. 3.80, the effect of angle on erosion rate is significantly different
for ductile and brittle materials. W ith brittle material, the maximum erosion rate occurs at
normal impact, while for ductile material s it occurs at some intermediate and generally
much smaller angle. These differences can be understood in terms of the predominant
modes of damage associated with these types of materials.
As discussed in Sec. 3.3, brittle fracture tends to increase the amount of wear over
that caused by displacement, that is by cutting and plowing. As indicated in Fig. 3.20, this
could be by as much as 10 . As a general rule, brittle materials are more likely to fracture
under normal impact conditions, that is, impacting velocity perpendicular to the surface,
than ductile materials. Consequently, as the erosive condition moves from a more grazing
situation to a more normal impact, brittle materials would experience a greater tendency
to experience brittle fracture, which would tend to increasingly mask the ductile or cutting
contributions. For brittle materials, the erosion rate would then be expected to mono-
tonically increase with the angle.
For ductile materials, cutting and plowing are the predominant modes and fracture
is negligible. The model for single-cycle deformation indicates that the wear due to cutting
and plowing is proportional to the product of load and distance (see Eq. (3.20)). Since load
increases with angle and sliding decreases with angle, an intermediate angle should exist
where the product of the two is maximum.
This angular dependency is contained in b in Eq. (3.101). Assuming that b can be
separated into an angular factor, F, and a factor independ ent of angle, b
0
, and combining
several of the material-sensitive parameters and num erical factors into one, K
e
, the follow-
ing expression can be obtained:
V ¼
K
e
FMv
2
p
ð3:102Þ
Examining this equation for erosive-wear volume, it can be seen that it does not provide
an explicit dependency on duration or exposure. However, such a dependency is implicitly
contained in M, the total mass of particles. If Q is particle mass per unit time, then M is
Qt, where t is the time of exposure to the particle stream. Including this into Eq. (3.102),
the following form is obta ined for particle erosion:
V ¼
K
e
Fv
2
Qt
p
ð3:103Þ
Another variation of Eq. (3.102) is frequently encountered in the literature. Compar-
ison of erosive wear situations and resistance to erosion is often done in terms of the rela-
tive amount of material removed from the surface to the amount of abrasive particle
Copyright 2004 by Marcel Dekker, Inc. All Rights Reserved.