Isoelectric Point of Fluorite by Direct Force Measurements Using
Atomic Force Microscopy
Shoeleh Assemi,*
,²
Jakub Nalaskowski,
‡
Jan D. Miller,
‡
and William P. Johnson
²
Department of Geology and Geophysics and Department of Metallurgical Engineering, UniVersity of Utah,
Salt Lake City, Utah 84112
ReceiVed October 18, 2005. In Final Form: December 9, 2005
Interaction forces between a fluorite (CaF
2
) surface and colloidal silica were measured by atomic force microscopy
(AFM) in 1 × 10
-3
M NaNO
3
at different pH values. Forces between the silica colloid and fluorite flat were measured
at a range of pH values above the isoelectric point (IEP) of silica so that the forces were mainly controlled by the
fluorite surface charge. In this way, the IEP of the fluorite surface was deduced from AFM force curves at pH ∼9.2.
Experimental force versus separation distance curves were in good agreement with theoretical predictions based on
long-range electrostatic interactions, allowing the potential of the fluorite surface to be estimated from the experimental
force curves. AFM-deduced surface potentials were generally lower than the published zeta potentials obtained from
electrokinetic methods for powdered samples. Differences in methodology, orientation of the fluorite, surface carbonation,
and equilibration time all could have contributed to this difference.
Introduction
The surface charge of ionic solids in water is determined by
differential hydration of their lattice ions at the surface, which
depends on the crystal structure and the cleavage plane of the
crystal. Miller and Clara
1,2
demonstrated that the hydration energy
of the surface ions can be calculated for fluorite by considering
the lattice energy and surface Madelung constants.
Microelectrophoresis of powdered fluorite samples and
streaming potential measurements of fluorite crystals have yielded
different results. Several studies have shown that in the absence
of surface carbonation a high positive zeta potential for fluorite
is obtained.
3-6
Surface carbonation results in the change of the
character of the surface from fluorite (CaF
2
) to calcite (CaCO
3
),
with a low, positive surface potential and thus a lower IEP.
7
A
few studies report a lower IEP (∼pH 6.6) or a completely negative
surface.
8,9
The advent of atomic force microscopy (AFM)
10
has made it
possible to measure the interaction forces between a broad range
of surfaces and thus allow for the estimation of their surface
charge in different electrolyte solutions.
11
Interaction forces
between two particles can be measured by AFM using the colloidal
probe technique, where a sphere of the particle of choice can be
glued to the AFM tip. Attachment of a sphere to the tip removes
uncertainties in the interaction radius and allows a quantitative
analysis of the force data by fitting the data to existing models.
11-14
AFM has been widely used to determine the isoelectric point of
oxide surfaces such as silica and R-alumina.
11-13,15
In this letter,
we report the application of the colloidal probe technique to
estimate the surface potential and isoelectric point of CaF
2
in a
dilute electrolyte (1 × 10
-3
M NaNO
3
). This method can be
particularly useful for estimating the IEP of small mineralogical
samples at their different crystallographic planes.
Materials and Methods
Materials. Fluorite (CaF
2
) optical windows (13 mm × 2 mm)
were purchased from Harrick Scientific Corp. (Ossining, NY). The
fluorite window was cleaned using UV/ozone for 15 min prior to
AFM measurements. Characterization of the surface by X-ray
diffraction (X’Pert Texture, Phillips Analytical, MA), revealed a
(110) plane of orientation.
Silica particles with a nominal diameter of 4.70 μm (Bangs
Laboratories, Inc., IN) were cleaned by soaking in SC1 solution
(5:1:1 H
2
O/NH
4
OH/H
2
O
2
) and holding the suspension at about 80
°C for 15 min. The suspension was filtered through a 0.45 μm
disposable filter and left to dry inside the filter. The filter was then
cut, and the silica particles were spread on a precleaned glass slide
using a clean tungsten wire.
The AFM fluid cell, O-ring, and tubings were cleaned prior to
the experiment by rinsing with acetone/methanol/acetone and several
portions of deionized water, followed by blow drying with high-
purity nitrogen.
Deionized water was obtained from a Milli-Q system. The
resistivity of the water was above 18 MΩ cm in all experiments.
All of the glassware and plasticware were cleaned by overnight
soaking in 10% HNO
3
and copious rinses with deionized water.
Solutions were prepared using analytical-grade reagents.
Atomic Force Microscopy Measurements. AFM force mea-
surements were made using a Nanoscope IIIa (Veeco, Santa Barbara,
CA) scanning probe microscope in a fluid cell (Veeco). V-shaped,
gold-coated tipless silicon nitride cantilevers were obtained from
Veeco. The spring constant of the cantilevers was reported to be
0.12 N m
-1
by the manufacturer. The spring constant of the cantilevers
was determined to be 0.10 ( 0.003 N m
-1
using the Cleveland
method,
16
which relies on monitoring the shifts in the resonance
* Corresponding author. E-mail: sassemi@mines.utah.edu. Phone: (801)
585-1538.
²
Department of Geology and Geophysics.
‡
Department of Metallurgical Engineering.
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1403 Langmuir 2006, 22, 1403-1405
10.1021/la052806o CCC: $33.50 © 2006 American Chemical Society
Published on Web 01/21/2006