Ice growth on the cooling surface in a jacketed and stirred eutectic freeze crystallizer of aqueous Na 2 SO 4 solutions

2017 ◽  
Vol 175 ◽  
pp. 512-526 ◽  
Author(s):  
Mehdi Hasan ◽  
Roman Filimonov ◽  
Jemitias Chivavava ◽  
Joonas Sorvari ◽  
Marjatta Louhi-Kultanen ◽  
...  
Keyword(s):  
2017 ◽  
Vol 468 ◽  
pp. 46-53 ◽  
Author(s):  
Yoshimichi Hagiwara ◽  
Shoji Ishikawa ◽  
Ryota Kimura ◽  
Kazumasa Toyohara

Nanoscale ◽  
2019 ◽  
Vol 11 (44) ◽  
pp. 21147-21154 ◽  
Author(s):  
Raymond W. Friddle ◽  
Konrad Thürmer

Video microscopy and AFM are used to relate surface topography to a mineral's ability to promote ice growth. On feldspar, abundant as atmospheric dust, basic surface steps can facilitate condensation and freezing when air becomes saturated.


Processes ◽  
2021 ◽  
Vol 9 (2) ◽  
pp. 306
Author(s):  
Kazuya Taira ◽  
Tomonori Waku ◽  
Yoshimichi Hagiwara

The control of ice growth inside channels of aqueous solution flows is important in numerous fields, including (a) cold-energy transportation plants and (b) the preservation of supercooled human organs for transplantation. A promising method for this control is to add a substance that influences ice growth in the flows. However, limited results have been reported on the effects of such additives. Using a microscope, we measured the growth of ice from one sidewall toward the opposite sidewall of a mini-channel, where aqueous solutions of sodium chloride and antifreeze protein flowed. Our aim was to considerably suppress ice growth by mixing the two solutes. Inclined interfaces, the overlapping of serrated interfaces, and interfaces with sharp and flat tips were observed in the cases of the protein-solution, salt-solution, and mixed-solution flows, respectively. In addition, it was found that the average interface velocity in the case of the mixed-solution flow was the lowest and decreased by 64% compared with that of pure water. This significant suppression of the ice-layer growth can be attributed to the synergistic effects of the ions and antifreeze protein on the diffusion of protein.


2005 ◽  
Author(s):  
Egemen Ogretim ◽  
Wade W. Huebsch ◽  
Jim Narramore ◽  
Bob Mullins
Keyword(s):  

2001 ◽  
Vol 33 ◽  
pp. 399-406 ◽  
Author(s):  
N. L. Bindoff ◽  
G. D. Williams ◽  
I. Allison

AbstractIn July-September 1999, an extensive oceanographic survey (87 conductivity-, temperature-and depth-measuring stations) was conducted in the Mertz Glacier polynya over the Adélie Depression off the Antarctic coast between 145° and 150° E. We identify and describe four key water masses in this polynya: highly modified circumpolar deep water (HMCDW), winter water (WW), ice-shelf water (ISW) and high-salinity shelf water (HSSW). Combining surface velocity data (from an acoustic Doppler current-profiler) with three hydrographic sections, we found the HMCDW to be flowing westward along the shelf break (0.7 Sv), the WW and HSSW flowing eastwards underneath Mertz Glacier (2.0 Sv) and that there was a westward return flow of ISW against the continent (1.2 Sv). Using a simple box model for the exchanges of heat and fresh water between the principal water masses, we find that the polynya was primarily a latent-heat polynya with 95% of the total heat flux caused by sea-ice formation. This heat flux results from a fresh-water-equivalent sea-ice growth rate of 4.9−7.7 cm d−1 and a mass exchange between HMCDW and WW of 1.45 Sv The inferred ocean heat flux is 8−14 W m−2 and compares well with other indirect estimates.


1983 ◽  
Vol 88 (C5) ◽  
pp. 2917 ◽  
Author(s):  
Jane Bauer ◽  
Seelye Martin
Keyword(s):  

Author(s):  
Shaoli Cui ◽  
Weijia Zhang ◽  
Xueguang Shao ◽  
Wensheng Cai

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