Christoffer
Abrahamsson
*ab,
Lars
Nordstierna
a,
Johan
Bergenholtz
c,
Annika
Altskär
d and
Magnus
Nydén
e
aDepartment of Chemical and Biological Engineering, Chalmers University of Technology, Kemivägen 10, 412 96, Gothenburg, Sweden. E-mail: abrahamc@chalmers.se
bSuMo Biomaterials, VINN Excellence Centre, Chalmers University of Technology, Gothenburg, 412 96, Sweden
cDepartment of Chemistry and Molecular Biology, University of Gothenburg, Kemivägen 10, 412 96, Gothenburg, Sweden
dStructure and Material Design, SIK – The Swedish Institute for Food and Biotechnology, SIK, PO Box 5401, 402 29 Gothenburg, Sweden
eIan Wark Research Institute, University of South Australia, Mawson Lakes Campus, Mawson Lakes, SA 5095, Australia
First published on 14th August 2015
Correction for ‘Magnetically induced structural anisotropy in binary colloidal gels and its effect on diffusion and pressure driven permeability’ by Christoffer Abrahamsson et al., Soft Matter, 2014, 10, 4403–4412.
I. Page 4409 – says: “This decline yields, when used in eqn (4) with S = 0, a ϕclay+bound corresponding to a bound water layer thickness of 1.4 nm, which is in the same range previously reported for clay dispersions in the literature.42,45,46”
Page 4409 – should be: “This decline yields, when used in eqn (4) with S = −1/2, a ϕclay+bound corresponding to a bound water layer thickness of 1.4 nm, which is in the same range previously reported for clay dispersions in the literature.42,45,46”
II. Page 4409 – eqn (5) says:
Page 4409 – should be:
III. Page 4410 – says: “This results in 1.53 ± 0.9 plates in the average clay aggregate.”
Page 4410 – should be: “This results in 1.53 ± 0.09 plates in the average clay aggregate.”
The Royal Society of Chemistry apologises for these errors and any consequent inconvenience to authors and readers.
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