Ice Adhesion Models to Predict Shear Stress at Shedding

被引:62
作者
Fortin, Guy [1 ]
Perron, Jean [1 ]
机构
[1] Univ Quebec Chicoutimi, Antiicing Mat Int Lab, Chicoutimi, PQ G7H 2B1, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Ice; adhesion; model; hydrophobic coating; icephobic coating; ice stress; ice strength; surface roughness; CREEP; STRENGTH; DENSITY;
D O I
10.1163/016942411X574835
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The model presented in this paper is the first step towards explaining the mechanisms of ice adhesion. Considerable work, however, remains to validate each term included in the model due to the lack of physical constants and parameters related to rough surfaces. The ice adhesion model at the ice-substrate interface is based on water behavior before and after freezing, substrate roughness and ice type. Within nanoseconds following impact, water occupies the substrate surface either partially before freezing when drops or rivulets form, or totally when a film is formed. The ice surface area in contact with the substrate is reduced due to the space between drops and rivulets. Due to the electrostatic attraction between water and substrate molecules, ice sticks to the substrate. The electrostatic force depends on the intensity of this bond, which is related to the work needed to maintain the drop shape over the surface and the distance between the water and substrate molecules. The water can also sink in and fill the cavities formed by adjacent surface roughness peaks when the surface tension force is less than the water pressure force. Following the phase change, on the order of microseconds for rime ice, and milliseconds for glaze ice, the ice mechanically locks onto the surface and must be broken down to be shed. This paper shows the development of a phenomenological model to predict the cohesive failure of ice, one that does not take into consideration rime ice porosity. The model assumes that ice near its freezing point is subject to internal and external strains, and that its cohesive strength corresponds to the failure stress. The failure stress is dependent on grain size and creep involving grain boundary sliding in a polycrystalline material at elevated temperatures. The next steps in the development of the model are to quantify the physical parameters, validate an idealized rough surface, as well as evaluate the effects of rime ice porosity and small grain sizes. (C) Koninklijke Brill NV, Leiden, 2012
引用
收藏
页码:523 / 553
页数:31
相关论文
共 34 条
[1]   ICE ADHESION TO HYDROPHILIC AND HYDROPHOBIC SURFACES [J].
BASCOM, WD ;
COTTINGTON, RL ;
SINGLETERRY, CR .
JOURNAL OF ADHESION, 1969, 1 (OCT) :246-+
[2]  
Boluk Y., 1996, 12860E TP TRANSP CAN
[3]   Wettability of porous surfaces. [J].
Cassie, ABD ;
Baxter, S .
TRANSACTIONS OF THE FARADAY SOCIETY, 1944, 40 :0546-0550
[4]  
CROUTCH VK, 1992, J COATING TECHNOL, V64, P41
[5]  
DRUEZ J, 1979, T CAN SOC MECH ENG, V5, P215
[6]  
DUVAL P, 1980, J GLACIOL, V25, P151, DOI 10.3189/S0022143000010364
[7]  
Ford T. F., 1962, AD0285093 NAV RES
[8]  
Fortin G., 2009, P 1 AIAA ATM SPAC EN, P1
[9]  
Fortin G., 2010, P 2 AIAA ATM SPAC EN, P1
[10]  
Itagaki K., 1984, P 2 INT WORKSH ATM I, P95