Silica colloids and silica glass surfaces have often
been used as “model” systems to study coagulation,
rheology, contact angles, and surface forces. But the
silica−water interface is highly changeable and
reactive. It has stubbornly refused to conform to theoretical
models of an ideal hydrophilic substrate. In
this study we show why this is and demonstrate some of the diverse
properties of this surface. Surfaces
of fused quartz swell under water to form layers of silica gel. We
report here on how this well-known effect
shows up in surface force measurements. Peculiar effects occur
already at normal pH. Over a period of
time after the surfaces are immersed in water, identical interaction
patterns occur on approach and on
separation. The double-layer repulsion extends from large
distances down to the contact. Interaction
hysteresis develops later. Adhesion and other specific
interactions, particularly at short range, develop
with time. The evolution that extends for hours and days is
variable in its manifestations from experiment
to experiment. Precise conditions of solidification from the melt,
and aspects of the thermal history of the
glass transition during preparation of vitreous silica samples, can be
factors in this variability. Surface
degradation by formation of silica gel layers on contact with water can
be enhanced by cold plasma treatment
and by UV radiation. Pull-off forces increase with an increase of
contact time. They also show a memory
of conditions of previous contacts. Electrolytes enhance the
adhesion. Complicated polycondensation
equilibria, influenced by nonspecific and specific ion effects, pH,
nonionic solutes, and temperature distinguish
the chemistry of silicic acid. All are involved in the
interaction. These curious, history-dependent,
surface
forces were first reported half a century ago. They were
attributed by Malkina and Derjaguin to “water
structure”. The effects that led later to contentious and
disputed notions of hydration forces can be manifest
as an “extra” repulsion or an “extra” attraction. They are
here related to surface gelation. These surface
force observations have distinct parallels in thixotropy and other
peculiarities of “anomalous” coagulation
and rheological behavior of concentrated and diluted dispersions of
colloid silica in water. The effect of
“cold fusion” between macroscopic surfaces of pure silica in pure
water is here studied at room temperature
with a new interfacial gauge force measuring technique. This
spontaneous welding due to the presence
of water can be hindered by stray contact shear, which interferes with
observation by colloid probe and
surface force techniques. The peculiar properties of the
silica−water interface are discussed in connection
with earlier experimental work that led to theoretical notions of
polywater and non-DLVO forces.