ELSEVIER Applied Surface Science 75 (1994) 197-203
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applied
surface science
Adsorption of anionic and cationic polymers on porous
and non-porous calcium carbonate surfaces
Robert B. Bjorklund *, Hans Arwin
Laboratory of Applied Physics, Link6ping University, S-581 83 Link6ping, Sweden
Lars J~irnstr6m
Swedish Pulp and Paper Research Institute, Box 5604, S-114 86 Stockholm, Sweden
(Received 15 May 1993; accepted for publication 8 June 1993)
Abstract
The adsorption of anionic and cationic polymers onto calcium carbonate surfaces was studied by ellipsometry.
Sodium polyacrylate was observed to both adsorb on and promote dissolution of polished limestone surfaces in
5 mM CaSO4 solution at pH 10.3. It was not possible to differentiate between the two processes when they occurred
simultaneously. Cationic starch adsorbed on the limestone surfaces at low concentrations and caused mineral
dissolution at higher concentrations. The adsorbed amount of starch was higher on surfaces which were first made
porous by partial dissolution than on freshly polished surfaces. Surfaces created by cleavage of Iceland spar calcite
were quite stable against dissolution and the amount of starch adsorbed determined by ellipsometry agreed well with
the adsorbed mass determined from batch adsorption experiments on ground calcite.
1. Introduction
Calcium carbonate is an important industrial
mineral used in both its natural and synthetic
forms in the rubber, plastic and paper industries.
In these applications, surface properties play an
important role in determining the effectiveness of
calcium carbonate as a bulk filler or as a func-
tional component in the final product. When
used as a pigment in the coating of paper and
board, the nature of the calcium carbonate is a
* Corresponding author.
major factor in determining many important
properties of the final product, such as dusting,
ink interactions and de-inking of waste paper.
Even the surface morphology of the mineral plays
a key role in this regard as reported by Keller and
Luner [1] that physi- and chemisorbed water
bound within the pore structure significantly in-
fluences the properties of calcium carbonates.
Surface studies of calcium carbonates often
deal with the colloidal properties of small calcite
particles in aqueous suspensions. The surface
charge has been extensively studied and has been
reported by Siffert and Fimbel [2] to be depen-
dent on the concentration of the dispersed cal-
cium carbonate, i.e. on the total surface area in
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