Yu
Xi
a,
Alexia
Mercier
b,
Cheng
Kuang
c,
Jingwei
Yun
a,
Ashton
Christy
a,
Luke
Melo
a,
Maria T.
Maldonado
c,
James A.
Raymond
d and
Allan K.
Bertram
*a
aDepartment of Chemistry, University of British Columbia, 2036 Main Mall, Vancouver, BC V6T 1Z1, Canada. E-mail: bertram@chem.ubc.ca
bDepartment of Chemistry, Sorbonne University, 4 Place Jussieu, 75005 Paris, France
cDepartment of Earth, Ocean & Atmospheric Sciences, University of British Columbia, 2020 – 2207 Main Mall, Vancouver, BC V6T 1Z4, Canada
dSchool of Life Sciences, University of Nevada, 4505 S. Maryland Pkwy., Las Vegas, NV89154, USA
First published on 15th February 2022
Correction for ‘Concentrations and properties of ice nucleating substances in exudates from Antarctic sea-ice diatoms’ by Yu Xi et al., Environ. Sci.: Processes Impacts, 2021, 23, 323–334, DOI: 10.1039/D0EM00398K.
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Fig. 4 Number of INSs per mass of total material, nm,total, for the Nitzschia supernatant sample and cultured sea ice diatom and temperate diatom samples from Ickes et al.1 For the cultured samples, the total mass of material in the cultures was estimated using their reported number of cells1 and assuming a cell density of 1 g cm−3 and cell volume of 653 and 125 μm3 for Melosira arctica and Skeletonema marinoi respectively.2 The error bars were calculated based on 95% confidence intervals from the nucleation statistics.3 Also included for comparison are INSs per mass of material for other atmospherically relevant INSs.1,4–8 |
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