scholarly journals TmAFP Interaction with an Ice Lattice

2019 ◽  
Vol 33 (S1) ◽  
Author(s):  
Brendan MacGillivray ◽  
James Greig ◽  
Kathleen Bai ◽  
Celine Fu ◽  
Ayaka Fujikawa ◽  
...  
Keyword(s):  
1971 ◽  
Vol 10 (59) ◽  
pp. 299-308
Author(s):  
F. Prodi ◽  
C.T. Nagamoto

AbstractA new technique for precisely detecting chlorides in ice has been developed. It is based on a microchemical contact reaction which takes place when a thin surface layer of ice melts through a membrane filter previously soaked in a concentrated solution of silver nitrate and dried. The silver chloride thus formed is reduced to metallic silver under ultra-violet light. The results on natural hailstones and laboratory doped ice show that foreign molecules are mainly segregated along the grain boundaries rather than being captured in the ice lattice.The technique, which makes quantitative evaluations possible, appears promising in all experimental studies on natural ice (hailstones and sea ice) and on ice artificially grown in the laboratory (by accretion or by freezing of solutions).


1978 ◽  
Vol 21 (85) ◽  
pp. 123-141 ◽  
Author(s):  
G. C. Camplin ◽  
J. W. Glen ◽  
J. G. Paren

AbstractTo understand the recent dielectric measurements made on HF-doped ice single crystals requires a full knowledge of the concentration of electrical defects present in ice and their subsequent interactions. Previous interpretations of the behaviour of HF-doped ice have concentrated upon specific features in isolation, whereas this paper presents analyses of a data set of 139 temperature and impurity combinations from 17 HF-doped ice single crystals. The interpretation of the behaviour of these crystals is in terms of several possible theoretical models. All models are based upon the common assumptions that HF molecules enter the ice lattice substitutionally and that excess Bjerrum and ionic defects can be formed at the HF sites. They also use the theory of electrical conduction in ice by Jaccard (1959) and the defect equilibria analysis in ice by Kroger (1974).All models yield values for the concentration, mobility, energy of formation and charges for the different types of electrical defect considered to be generated.From the model which assumes that only three fluorine centres exist, the approximate derived values of the mobility and charge for the L-defect and positive ionic defect are as follows: μL = 5 × 10-8 m2 V-1 s-1 at 273 K, eDL = 0.44e; μ+ = 2.7 × 10-8 m2 V-1 s-1 at 273 K, e± 0.73e.Finally, using the derived defect conductivities and the Jaccard theory of electrical conduction, the relaxation tune of HF-doped ice has been successfully predicted over a wide range of temperature and fluoride concentration.


1994 ◽  
Vol 101 (4) ◽  
pp. 3216-3221 ◽  
Author(s):  
Nishikant Sonwalkar ◽  
Sidney Yip ◽  
S. Shyam Sunder

2013 ◽  
Vol 110 (11) ◽  
Author(s):  
Sebastian Gliga ◽  
Attila Kákay ◽  
Riccardo Hertel ◽  
Olle G. Heinonen

2019 ◽  
Vol 21 (7) ◽  
pp. 3903-3917 ◽  
Author(s):  
Poonam Pandey ◽  
Sairam S. Mallajosyula

Plausible structural alignment of antifreeze glycoprotein (AFGP) relative to the ice lattice highlighting the role of both Ala and GalNAc methyl groups binding to the ice plane.


1990 ◽  
Vol 14 ◽  
pp. 195-198 ◽  
Author(s):  
J.C. Moore ◽  
J.G. Paren ◽  
R. Mulvaney

The dielectric stratigraphy of a 130 m ice core from Dolleman Island, Antarctic Peninsula, shows large variations in the dielectric relaxation process and in conductivity. A comparison with the chemical stratigraphy of the core demonstrates the decisive role played by both acids and salts in determining the electrical behaviour of natural ice. The dielectric response is sensitive both to the type of impurity and to its distribution within the ice fabric. The evidence supports other observations of the localization of sulphuric acid at three-grain boundaries: in contrast, the salt impurity appears to be largely incorporated into the ice lattice. The overriding importance of the dielectric profiling technique is that it is the only profiling tool so far developed that is sensitive to the presence of salt in polar ice cores.


Author(s):  
Ali Khosravi ◽  
Jorge Augusto Lasave ◽  
Sergio Koval ◽  
Erio Tosatti

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