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The colloidal suspensions used in this study consist of polystyrene
sulfate spheres 0.654
0.009
m in diameter (Catalog # 5065, Duke
Scientific, Palo Alto, CA), dispersed in
deionized water.
These spheres develop strongly negative surface charges due to dissociation
of their ionic surface groups.
Pair interaction measurements indicate an effective surface potential
of
meV [12].
An aqueous suspension of these spheres was purified by 3 months of dialysis
against deionized water followed by tumbling with mixed-bed ion
exchange resin.
Samples of the cleaned suspension were filled into sample
chambers at volume fractions
and
.
Both suspensions crystallized into face-centered cubic (FCC)
structures.
The remainder of this Article concerns the properties of these
two crystals.
The sample container depicted schematically in Fig. 1
is created by hermetically sealing the edges of a #1 glass coverslip
to a glass microscope slide with a high-purity UV curing adhesive
(Norland Optical Adhesive Type 88, Norland Products, New Brunswick, NJ).
The enclosed volume has a visible area of
and is roughly
m thick.
Access to the sample volume is provided by two glass tubes
extending from holes drilled
through the slide.
All parts were thoroughly cleaned before assembly [13]
and the finished sample cells
were flushed with deionized water in a nitrogen-purged glove
box before filling.
After filling, the tubes
serve as reservoirs of colloid and
contain mixed bed ion exchange resin to maintain the chemical
purity of the interior.
The ends of the tubes are continually flushed with water-saturated
Ar to prevent the suspension from becoming acidified by absorbing
CO2 from the air.
Applying an alternating pressure difference
across the tubes causes the colloid
to flow back and forth through
the sample cell and past the ion exchange resin,
and further lowers the ionic strength of the suspension.
Filled sample cells were allowed to equilibrate for
several weeks before the measurements we describe below were performed.
Observations were made with
an Olympus IMT-2 inverted
optical microscope.
A combination of a 100
N.A. 1.4 oil immersion objective and
a 10
video eyepiece
provides a total magnification of 172 nm/pixel on the attached
charge-coupled device camera, so that a single sphere's image
subtends an area of roughly
square pixels.
At this magnification, the 615
470 pixel field of view
corresponds to a visible area of 106
82
m2.
The
100 nm depth of focus of the optical system is comparable to
the diameter of a sphere so that only a single crystal layer is
resolved at a given focal depth.
We record the spheres' motions at 1/30 second intervals
using a SONY EVO-9650 Hi-8 computer-controlled video deck.
The video tapes are then digitized with a Data Translation
DT-3851A frame grabber before being analyzed.
Figures 2(a) and (c) show typical digitized images
of the two crystals' (111) planes
in the layer closest to the glass wall.
Each sphere in Fig. 2 appears as a bright blur
on a dark background.
We use precision image analysis techniques [4]
to locate the spheres' centroid to within 20 nm in the plane.
Their locations in a sequence of
video frames are then linked into trajectories
using a maximum likelihood algorithm [4].
The data for this study consists of the time-resolved sphere
trajectories
Small variations in atmospheric pressure cause the crystals to drift slightly relative to the imaging volume during data acquisition. To avoid artifacts introduced by this secular drift, we subtract off the mean displacement over the field of view at each time step. Typical trajectory sequences appear in Figs. 2(b) and (d).
Once the spheres' centroids have been located in the field of view, we
apply computational geometry techniques [14]
to analyze their distribution.
In particular, we use the Delaunay triangulation to uniquely
identify the set of nearest neighbors for each sphere in a snapshot.
Given the nearest-neighbor connectivity, we then calculate
lattice descriptors such as the mean nearest-neighbor
separation
and the principal reciprocal lattice vectors.
For the relatively dilute crystal shown
in Fig. 2(a),
the mean separation is
m.
Focusing up through the crystal reveals a
m interlayer spacing.
This is consistent with the FCC structure
and is inconsistent with a body-centered cubic (BCC) lattice whose
equivalent interlayer spacing would be only half as big
in this projection.
The corresponding lattice constant in
the FCC crystal's (111) plane is
m.
By an equivalent analysis, the
dense crystal also adopts the FCC structure, with
m and
m.
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The extent of the crystals' ordering can be measured with
the time-averaged pair correlation function
The angle-averaged structure factor,
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Hansen and Verlet [16] observed that the structure factor's first peak at q = q0 reaches the universal value S(q0) = 2.85 when fluids freeze to FCC crystals. Figure 4 reveals that both suspensions are crystallized according to the Hansen-Verlet criterion.
The spheres' dynamics further allow us to assess the crystal's
thermodynamic state.
Building upon a suggestion by Lindemann [17],
Gilvarry [18] postulated that crystals melt when
the ensemble averaged r.m.s. lattice displacement
Having established the crystals' states, we are in a position to probe the interactions responsible for their structure and dynamics. This is a useful goal in itself since measuring particle interactions is an important component in process control for a wide range of industrial applications [20]. Direct imaging is almost entirely noninvasive and nonperturbative and so offers possible benefits over electrokinetic and mechanical methods commonly used.