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Journal articles on the topic 'Ice mechanics'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 August 2024

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1

Weiss, Jérôme, and Véronique Dansereau. "Linking scales in sea ice mechanics." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 375, no. 2086 (2017): 20150352. http://dx.doi.org/10.1098/rsta.2015.0352.

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Mechanics plays a key role in the evolution of the sea ice cover through its control on drift, on momentum and thermal energy exchanges between the polar oceans and the atmosphere along cracks and faults, and on ice thickness distribution through opening and ridging processes. At the local scale, a significant variability of the mechanical strength is associated with the microstructural heterogeneity of saline ice, however characterized by a small correlation length, below the ice thickness scale. Conversely, the sea ice mechanical fields (velocity, strain and stress) are characterized by long

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2

Ma¨a¨tta¨nen, Mauri. "Advance in Ice Mechanics in Finland." Applied Mechanics Reviews 40, no. 9 (1987): 1200–1207. http://dx.doi.org/10.1115/1.3149551.

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In Finland, 110 years of winter navigation has been a natural initiator of ice mechanics research. It has brought with it sea ice monitoring and statistics, ice forecasting, the testing of mechanical properties, ship and icebreaker model testing and full-scale trials, ice resistant aids-to-navigation, and theoretical modelling and numerical simulations. Lately, a lot of ice mechanics research has been devoted to arctic offshore applications. A summary of the major developments is given in this paper.

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3

Jacobsen, Stefan, George W. Scherer, and Erland M. Schulson. "Concrete–ice abrasion mechanics." Cement and Concrete Research 73 (July 2015): 79–95. http://dx.doi.org/10.1016/j.cemconres.2015.01.001.

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4

Jordaan, Ian J. "Mechanics of ice–structure interaction." Engineering Fracture Mechanics 68, no. 17-18 (2001): 1923–60. http://dx.doi.org/10.1016/s0013-7944(01)00032-7.

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5

Dempsey, John P. "Research trends in ice mechanics." International Journal of Solids and Structures 37, no. 1-2 (2000): 131–53. http://dx.doi.org/10.1016/s0020-7683(99)00084-0.

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6

Wong, T. T., N. R. Morgenstern, and D. C. Segoz. "Ice rubble attenuation of ice loads on arctic offshore structures." Canadian Geotechnical Journal 28, no. 6 (1991): 881–95. http://dx.doi.org/10.1139/t91-104.

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A state of the art survey of ice rubble mechanics is first presented. This survey covers ice rubble morphology, laboratory testing of ice rubble, the study of the load transmission capability of existing rubble fields, and field measurements in ice rubble surrounding offshore structures. Then, the implementation of a new plasticity model for normally consolidated broken ice into an existing finite element stress analysis code is described. The resulting program is validated using triaxial test data. Using this model, a two-dimensional parametric study on ice force transmission through a ground

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7

Chung, Jin S. "Special Issue on Ice Mechanics: Introduction." Applied Mechanics Reviews 40, no. 9 (1987): 1192. http://dx.doi.org/10.1115/1.3149549.

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8

Pralong, A., K. Hutter, and M. Funk. "Anisotropic damage mechanics for viscoelastic ice." Continuum Mechanics and Thermodynamics 17, no. 5 (2006): 387–408. http://dx.doi.org/10.1007/s00161-005-0002-5.

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9

Beemer, Darryl L., Wei Wang, and Arun K. Kota. "Durable gels with ultra-low adhesion to ice." Journal of Materials Chemistry A 4, no. 47 (2016): 18253–58. http://dx.doi.org/10.1039/c6ta07262c.

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10

Liu, Xiaozhou, Ben Li, Yaodan Zhang, and Chen Zhang. "Comprehensive Fracture Model of Reservoir Ice Layers in the Northeastern Cold Region of China." Sustainability 14, no. 12 (2022): 7326. http://dx.doi.org/10.3390/su14127326.

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Meteorological and hydrological changes have an important influence on the ice formation mechanism and the detailed structure of ice materials in cold reservoirs, and directly determine the mechanical properties of ice materials. Based on long-term meteorological and hydrological monitoring data, and detailed structural evolution analysis of ice materials, combined with fracture mechanics and energy methods, a comprehensive fracture model of ice materials in cold regions is established. At the same time, the fracture mechanics test results and simulation results of ice materials are compared,

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11

Bradley, David. "No ice, ice, baby." Materials Today 36 (June 2020): 4. http://dx.doi.org/10.1016/j.mattod.2020.04.022.

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12

Schwarz, Joachim. "Advances in Ice Mechanics in West Germany." Applied Mechanics Reviews 40, no. 9 (1987): 1208–13. http://dx.doi.org/10.1115/1.3149552.

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Ice research in West Germany (Federal Republic of Germany) started after World War II with the first small ice tank built at HSVA in Hamburg in 1958. The discovery of hydrocarbons in the Arctic and the membership in the Scientific Committee for Antarctic Research led to the need for model tests and the advancing ice modelling techniques. In 1984 a new, large ice model basin was built at HSVA. Substantial progress has been made in the experimental research of basic ice mechanics and ice forces for the past 20 years. Computational methods and quantum statistical approach have recently been intro

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13

Sinha, N. K., G. W. Timco, and R. Frederking. "Recent Advances in Ice Mechanics in Canada." Applied Mechanics Reviews 40, no. 9 (1987): 1214–31. http://dx.doi.org/10.1115/1.3149553.

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Work on the mechanics of ice, which has been carried forward on a broad front in Canada, has resulted in a number of significant advances in the last 10 years. The factors influencing the growth of various types of sea ice have been quantified fundamentally and methods for examining the resulting material structure have been developed. Extensive work has been done on strength and deformation characteristics of ice. A significant effort has been the development of analytical expressions to describe the rheological behavior of ice. Elastic modulus, Poisson’s ratio, and creep were also treated. A

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14

Xie, Qiang, Tianhui Hao, Chao Wang, Zhenhang Kang, Zhonghua Shi, and Jifeng Zhang. "The Mechanical Mechanism and Influencing Factors of Ice Adhesion Strength on Ice-Phobic Coating." Journal of Marine Science and Engineering 9, no. 3 (2021): 315. http://dx.doi.org/10.3390/jmse9030315.

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Ice accretion can cause problems on polar ships, ocean platforms, and in other marine industries. It is important to understand the interface debonding behavior between ice and the surface of equipment. In this work, we created a mechanical model to analyze the interface debonding behavior between a square-based ice cuboid and an elastic coating base, using contact mechanics and fracture mechanics. Three-dimensional (3D) finite element (FE) simulation was used to simulate the interface debonding for normal and shear separation. A bilinear cohesive zone model (CZM) was used to simulate the inte

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15

Sodhi, Devinder S., and Gordon F. N. Cox. "Advances in Sea Ice Mechanics in the USA." Applied Mechanics Reviews 40, no. 9 (1987): 1232–42. http://dx.doi.org/10.1115/1.3149554.

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A brief review of significant advances in the field of sea ice mechanics in the United States is presented in this paper. Emphasis is on ice forces on structures, as the subject relates to development of oil and gas resources in the southern Beaufort Sea. The main topics discussed here are mechanical properties, ice–structure interaction, modeling of sea ice drift, and oil industry research activities. Significant advances in the determination of ice properties are the development of testing procedures to obtain consistent results. Using stiff testing machines, researchers have been able to id

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16

Bridges, Robert, Kaj Riska, Mark Hopkins, and Ying Wei. "Ice interaction processes during ice encroachment." Marine Structures 67 (September 2019): 102629. http://dx.doi.org/10.1016/j.marstruc.2019.05.007.

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17

Maslin, Mark. "Tying celestial mechanics to Earth’s ice ages." Physics Today 73, no. 5 (2020): 48–53. http://dx.doi.org/10.1063/pt.3.4474.

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18

Zhang, Xi, Yongli Huang, Sanmei Wang, Lei Li, and Chang Q. Sun. "Supersolid Skin Mechanics of Water and Ice." Procedia IUTAM 21 (2017): 102–10. http://dx.doi.org/10.1016/j.piutam.2017.03.043.

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19

Richter-Menge, Jacqueline A. "US research in ice mechanics: 1987–1990." Cold Regions Science and Technology 20, no. 3 (1992): 231–46. http://dx.doi.org/10.1016/0165-232x(92)90031-o.

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20

Wang, Xiao Liang, Guang Fan Li, and Juan Du. "Triaxial Test Study on Marine Sediments Sample with Simulated Combustible Ice." Applied Mechanics and Materials 580-583 (July 2014): 376–79. http://dx.doi.org/10.4028/www.scientific.net/amm.580-583.376.

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Combustible ice is a kind of efficient and clean energy that has the potential to be exploited in the future, exploiting combustible ice needs to understand its mechanical properties. Combustible ice is another important feature of soil which is different from soil, in order to correctly understand the distinction, this paper using soil mechanics triaxial test method, to study the mechanical properties of combustible ice. Different from previous study, this article put forward the concept of simulated combustible ice, namely through baking powder, sodium chloride, and Marine sedimentary soil t

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21

Tulaczyk, Slawek, W. Barclay Kamb, and Hermann F. Engelhardt. "Basal mechanics of Ice Stream B, west Antarctica: 1. Till mechanics." Journal of Geophysical Research: Solid Earth 105, B1 (2000): 463–81. http://dx.doi.org/10.1029/1999jb900329.

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22

Peltier, W. R., and L. P. Solheim. "Dynamics of the ice-age Earth: Solid mechanics and fluid mechanics." Journal de Physique IV (Proceedings) 12, no. 10 (2002): 85–104. http://dx.doi.org/10.1051/jp4:20020454.

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23

Hibler, W. D., and S. J. Vavrus. "Pre-industrial multiple equilibrium sea-ice flow states due to plastic ice mechanics." Cold Regions Science and Technology 76-77 (June 2012): 92–108. http://dx.doi.org/10.1016/j.coldregions.2012.01.008.

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24

Ladanyi, Branko. "Creep of frozen slopes and ice-filled rock joints under temperature variation." Canadian Journal of Civil Engineering 33, no. 6 (2006): 719–25. http://dx.doi.org/10.1139/l05-112.

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Owing to climate warming trends, there has been an increasing interest in recent years in the accelerating creep of rock glaciers and frozen slopes. In the field of glaciology, the creep of glaciers has been extensively studied, observed, and analyzed for more than 100 years. Many valuable and detailed theoretical models have been proposed through the years for simulating the creep behavior of glaciers. This synthesis paper has no intention of proposing another one. Its purpose is only to supply to these models a potential geotechnical background, borrowed from the connected fields of frozen g

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25

Khoo, H. A., and T. M. Hrudey. "Constitutive Model for Ice." Journal of Engineering Mechanics 118, no. 2 (1992): 259–79. http://dx.doi.org/10.1061/(asce)0733-9399(1992)118:2(259).

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26

Case, John A., and Andrew Barnard. "Marine and lacustrine ice fracture detection." Journal of the Acoustical Society of America 154, no. 4_supplement (2023): A133. http://dx.doi.org/10.1121/10.0023029.

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Ice fracturing has been extensively studied and modeled. With increased interest in ice mechanics and fracturing in recent years in climate science, fisheries, and for cultural impacts, detecting and classifying fracturing events has become an important problem to consider. Fractures primarily occur due to stress relief within an ice sheet during temperature shifts and ice movement. These events create mechanical waves within the sheet that couple into the water column which can then be detected as pressure and particle velocity fluctuations. Machine learning algorithms will be used to detect

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27

Gogoladze, D. Z., and A. T. Bekker. "Numerical Modeling of the Ice-Conical Structure Interaction Process Using Element Erosion Technique." IOP Conference Series: Earth and Environmental Science 988, no. 5 (2022): 052056. http://dx.doi.org/10.1088/1755-1315/988/5/052056.

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Abstract Nowadays, the Finite Element Analysis method is widely used, including in the field of fracture mechanics, because to the grown of computing power. Numerical modeling of fracture mechanics is a developing method in the Ice-Structure Interaction field. One of the approaches to modeling ice failure is the Finite Element Method with Element Erosion Technique, which is widely used among researchers. However, the question of using a material model that most accurately describes the behavior of ice taking into account its physical and mechanical characteristics remains open. Also, researche

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28

Hallam, S. D., and T. J. O. Sanderson. "Advances in Ice Mechanics in the United Kingdom." Applied Mechanics Reviews 40, no. 9 (1987): 1193–99. http://dx.doi.org/10.1115/1.3149550.

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The United Kingdom has made substantial contributions during the last few years to the field of ice mechanics and ice forces on offshore structures. Experimental studies have been carried out in the field and in the laboratory, and significant advances have been made in theoretical understanding. This paper summarizes the most recent contributions.

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29

Schoof, Christian. "On the mechanics of ice-stream shear margins." Journal of Glaciology 50, no. 169 (2004): 208–18. http://dx.doi.org/10.3189/172756504781830024.

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AbstractWe investigate the mechanics of ice-stream shear margins based on the assumption that the underlying bed behaves plastically. Sliding is assumed to occur if a prescribed, locally defined yield stress is attained, while no sliding is assumed possible if basal shear stress is lower than the yield stress. Mathematically, the ice-flow problem takes the form of a contact problem, in which the zones of sliding are part of the solution and cannot be prescribed arbitrarily. Simplistic assumptions about the location of till failure, or about mechanical conditions at the bed, predict stress sing

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30

van den Berg, Marnix, Raed Lubbad, and Sveinung Løset. "Repeatability of ice-tank tests with broken ice." Marine Structures 74 (November 2020): 102827. http://dx.doi.org/10.1016/j.marstruc.2020.102827.

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31

Goldstein, R. V., and N. M. Osipenko. "Some aspects of strength in sea ice mechanics." Physical Mesomechanics 18, no. 2 (2015): 139–48. http://dx.doi.org/10.1134/s102995991502006x.

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32

Weeks, W. F., and Garry Timco. "Preface [to special section on Sea Ice Mechanics]." Journal of Geophysical Research: Oceans 103, no. C10 (1998): 21737. http://dx.doi.org/10.1029/98jc01361.

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33

Dobrodeev, A. A., N. Yu Klementyeva, and K. E. Sazonov. "Large ship motion mechanics in “narrow” ice channel." IOP Conference Series: Earth and Environmental Science 193 (October 30, 2018): 012017. http://dx.doi.org/10.1088/1755-1315/193/1/012017.

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34

Dyer, Ira. "ACOUSTICS 1987: Arctic ambient noise: Ice source mechanics." Journal of the Acoustical Society of America 84, no. 5 (1988): 1941–42. http://dx.doi.org/10.1121/1.397162.

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35

Nixon, Wilfred A. "Application of Fracture Mechanics to Ice/Structure Interactions." Journal of Cold Regions Engineering 2, no. 1 (1988): 1–12. http://dx.doi.org/10.1061/(asce)0887-381x(1988)2:1(1).

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36

Craw, Lisa, Chao Qi, David J. Prior, David L. Goldsby, and Daeyeong Kim. "Mechanics and microstructure of deformed natural anisotropic ice." Journal of Structural Geology 115 (October 2018): 152–66. http://dx.doi.org/10.1016/j.jsg.2018.07.014.

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37

Liu, C. H., and L. H. N. Lee. "On fracture mechanics in lifting an ice sheet." International Journal of Fracture 28, no. 3 (1985): 189–97. http://dx.doi.org/10.1007/bf00018492.

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38

Schulson, Erland M. "Low-speed friction and brittle compressive failure of ice: fundamental processes in ice mechanics." International Materials Reviews 60, no. 8 (2015): 451–78. http://dx.doi.org/10.1179/1743280415y.0000000010.

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39

Bennett, Matthew R. "Ice streams as the arteries of an ice sheet: their mechanics, stability and significance." Earth-Science Reviews 61, no. 3-4 (2003): 309–39. http://dx.doi.org/10.1016/s0012-8252(02)00130-7.

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40

Pegler, Samuel S. "Marine ice sheet dynamics: the impacts of ice-shelf buttressing." Journal of Fluid Mechanics 857 (October 25, 2018): 605–47. http://dx.doi.org/10.1017/jfm.2018.741.

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Marine ice sheets are continent-scale glacial masses that lie partially submerged in the ocean, as applies to significant regions of Antarctica and Greenland. Such ice sheets have the potential to destabilise under a buoyancy-driven instability mechanism, with considerable implications for future sea level. This paper and its companion present a theoretical analysis of marine ice sheet dynamics under the effect of a potentially dominant control of the buttressing force generated by lateral stresses on the downstream floating component of the ice sheet (the ice shelf). The analysis reveals crit

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41

Bushuk, Mitchell, David M. Holland, Timothy P. Stanton, Alon Stern, and Callum Gray. "Ice scallops: a laboratory investigation of the ice–water interface." Journal of Fluid Mechanics 873 (June 28, 2019): 942–76. http://dx.doi.org/10.1017/jfm.2019.398.

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Ice scallops are a small-scale (5–20 cm) quasi-periodic ripple pattern that occurs at the ice–water interface. Previous work has suggested that scallops form due to a self-reinforcing interaction between an evolving ice-surface geometry, an adjacent turbulent flow field and the resulting differential melt rates that occur along the interface. In this study, we perform a series of laboratory experiments in a refrigerated flume to quantitatively investigate the mechanisms of scallop formation and evolution in high resolution. Using particle image velocimetry, we probe an evolving ice–water bound

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42

Walker, Dan, Neil Bose, Hajime Yamaguchi, and Stephen J. Jones. "Hydrodynamic loads on ice-class propellers during propeller-ice interaction." Journal of Marine Science and Technology 2, no. 1 (1997): 12–20. http://dx.doi.org/10.1007/bf01245933.

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43

Miodownik, Mark. "Ice aesthetics." Materials Today 8, no. 2 (2005): 6. http://dx.doi.org/10.1016/s1369-7021(05)00687-5.

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44

Smirnov, V. N., S. M. Kovalev, and A. A. Nubom. "SELF-EXCITED OSCILLATIONS IN THE DRIFTING ICE COVER OF THE ARCTIC OCEAN." DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS 47, no. 3 (2019): 122–38. http://dx.doi.org/10.29006/1564-2291.jor-2019.47(3).11.

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During the monitoring of physical-mechanical state of the ice cover of the Arctic Ocean a wide spectrum of oscillation and wave processes was in the system ice-water studied. The investigations were carried out on the drifting stations “North Pole” with seismometers and tiltmeters. Vertical and horizontal displacements in the ice field characterize parameters of wave processes caused by compression and ridging of ice-mechanical self-excited oscillations. Mechanics of appearance and propagation of waves can be considered with an account of elastic-viscous properties of the ice cover. A phenomen

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45

Karr, D. G. "A Damage Mechanics Model for Uniaxial Deformation of Ice." Journal of Energy Resources Technology 107, no. 3 (1985): 363–68. http://dx.doi.org/10.1115/1.3231202.

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A one-dimensional stress-strain relationship is developed for pure polycrystalline ice subjected to uniaxial compression. The model is based on the continuous damage theories and includes the effects of elastic, plastic and brittle deformation mechanisms. A damage law for ice is established based on a statistical model for internal microfracture. Quantitative results are presented by directly relating the formation of internal cracks to published acoustic emission response of ice samples subjected to compression.

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46

Schulson, Erland M. "Friction of sea ice." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, no. 2129 (2018): 20170336. http://dx.doi.org/10.1098/rsta.2017.0336.

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Static and kinetic friction play a fundamental role in sea-ice mechanics. The coefficient of static friction increases with hold time under normal load and is modelled in terms of creep and fracture of asperities in contact. The coefficient of kinetic friction exhibits velocity strengthening at lower speeds and velocity weakening at intermediate speeds. Strengthening is modelled in terms of asperity creep and hardness; weakening is modelled in terms of a progressive increase in the true area of contact wetted by meltwater produced through frictional heating. The concept is introduced of contac

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47

Sayed, M., and R. M. W. Frederking. "Model of Ice Rubble Pileup." Journal of Engineering Mechanics 114, no. 1 (1988): 149–60. http://dx.doi.org/10.1061/(asce)0733-9399(1988)114:1(149).

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48

MINCHEW, BRENT, MARK SIMONS, HELGI BJÖRNSSON, et al. "Plastic bed beneath Hofsjökull Ice Cap, central Iceland, and the sensitivity of ice flow to surface meltwater flux." Journal of Glaciology 62, no. 231 (2016): 147–58. http://dx.doi.org/10.1017/jog.2016.26.

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AbstractThe mechanical properties of glacier beds play a fundamental role in regulating the sensitivity of glaciers to environmental forcing across a wide range of timescales. Glaciers are commonly underlain by deformable till whose mechanical properties and influence on ice flow are not well understood but are critical for reliable projections of future glacier states. Using synoptic-scale observations of glacier motion in different seasons to constrain numerical ice flow models, we study the mechanics of the bed beneath Hofsjökull, a land-terminating ice cap in central Iceland. Our results i

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49

Klein-Paste, Alex, and Nirmal K. Sinha. "Microstructural investigation of ice surfaces after rubber–ice and sand–ice sliding friction tests." Tribology International 43, no. 5-6 (2010): 1151–57. http://dx.doi.org/10.1016/j.triboint.2009.12.036.

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50

Azarnejad, A., and T. M. Hrudey. "A numerical study of thermal ice loads on structures." Canadian Journal of Civil Engineering 25, no. 3 (1998): 557–68. http://dx.doi.org/10.1139/l97-119.

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A numerical model is presented for the prediction of the three-dimensional stress field in an ice sheet due to temperature changes, as a function of time, under a variety of conditions. The model relies on two separate computer programs for the thermal and mechanical aspects of the problem. The thermal program uses the finite difference method to calculate the temperature distribution through the thickness of the ice cover under a variety of meteorological input conditions. The mechanical part of the analysis is conducted using the finite element method. A degenerate shell element is used, whi

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