We report a study of the effect of shear deformation on the static structur
e factor, S(q), of a thermoreversible gel of organophilic colloidal silica
(a = 40 nm) in the solvent hexadecane. Small- and wide-angle light scatteri
ng measurements show that the quiescent structure of these gels is consiste
nt with that of fractal clusters with dimension cl = 2.4(independent of vol
ume fraction, phi) and finite radius (xi), which is a function of phi for t
he range 0.01 < phi < 0.1. Upon application of low shear rate deformation(g
amma less than or equal to 30 s(-1)), we observe an increase in xi and d, r
elative to the quiescent conditions. For this to be the case, mass conserva
tion requires that the number density of clusters be dramatically reduced u
pon shearing. The increase of d and xi and the concomitant decrease in the
number density of clusters point to the profound effect of shear on the lon
g-range structure of colloidal gels. At high shear rates (gamma > 30 s(-1))
we observe anisotropy of S(q) in the now-vorticity plane. The observed two
-lobe butterfly patterns are oriented in the now direction for all cp studi
ed. The anisotropy persists after cessation of shear, although some partial
relaxation is observed at the highest shear rate studied (gamma = 120 s(-1
)). Start-up of steady shear experiments performed for phi = 0.035 reveals
a monotonic increase of S(qi at low q (aq = 0.032), which is consistent wit
h an increase in both the fractal dimension, d, and cluster radius, xi. Com
parison of the time evolution of S(aq=0.032) with transient theological mea
surements performed under the same conditions reveals that the monotonic in
crease in S(aq = 0.032) occurs on a time scale identical to that required f
or the stress response to attain steady state.