FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2939856912> ?p ?o ?g. }

• W2939856912 endingPage "1186" @default.
• W2939856912 startingPage "1167" @default.
• W2939856912 abstract "Abstract. Recent high-resolution pan-Arctic sea ice simulations show fracture patterns (linear kinematic features or LKFs) that are typical of granular materials but with wider fracture angles than those observed in high-resolution satellite images. Motivated by this, ice fracture is investigated in a simple uni-axial loading test using two different viscous–plastic (VP) rheologies: one with an elliptical yield curve and a normal flow rule and one with a Coulombic yield curve and a normal flow rule that applies only to the elliptical cap. With the standard VP rheology, it is not possible to simulate fracture angles smaller than 30∘. Further, the standard VP model is not consistent with the behavior of granular material such as sea ice because (1) the fracture angle increases with ice shear strength; (2) the divergence along the fracture lines (or LKFs) is uniquely defined by the shear strength of the material with divergence for high shear strength and convergent with low shear strength; (3) the angle of fracture depends on the confining pressure with more convergence as the confining pressure increases. This behavior of the VP model is connected to the convexity of the yield curve together with use of a normal flow rule. In the Coulombic model, the angle of fracture is smaller (θ=23∘) and grossly consistent with observations. The solution, however, is unstable when the compressive stress is too large because of non-differentiable corners between the straight limbs of the Coulombic yield curve and the elliptical cap. The results suggest that, although at first sight the large-scale patterns of LKFs simulated with a VP sea ice model appear to be realistic, the elliptical yield curve with a normal flow rule is not consistent with the notion of sea ice as a pressure-sensitive and dilatant granular material." @default.
• W2939856912 created "2019-04-25" @default.
• W2939856912 creator A5007627846 @default.
• W2939856912 creator A5009150889 @default.
• W2939856912 creator A5017565455 @default.
• W2939856912 creator A5080125372 @default.
• W2939856912 date "2019-04-09" @default.
• W2939856912 modified "2023-10-14" @default.
• W2939856912 title "Simulating intersection angles between conjugate faults in sea ice with different viscous–plastic rheologies" @default.
• W2939856912 cites W1543363978 @default.
• W2939856912 cites W1641294341 @default.
• W2939856912 cites W1759556418 @default.
• W2939856912 cites W1875502629 @default.
• W2939856912 cites W1910754480 @default.
• W2939856912 cites W1929676829 @default.
• W2939856912 cites W1964965775 @default.
• W2939856912 cites W1966285639 @default.
• W2939856912 cites W1976400686 @default.
• W2939856912 cites W1980777882 @default.
• W2939856912 cites W1983126642 @default.
• W2939856912 cites W1986312912 @default.
• W2939856912 cites W1997016397 @default.
• W2939856912 cites W2001748840 @default.
• W2939856912 cites W2001754652 @default.
• W2939856912 cites W2002312361 @default.
• W2939856912 cites W2011868703 @default.
• W2939856912 cites W2012228140 @default.
• W2939856912 cites W2013143827 @default.
• W2939856912 cites W2013335593 @default.
• W2939856912 cites W2014035535 @default.
• W2939856912 cites W2014988998 @default.
• W2939856912 cites W2015426195 @default.
• W2939856912 cites W2016088782 @default.
• W2939856912 cites W2028048043 @default.
• W2939856912 cites W2030313781 @default.
• W2939856912 cites W2032110467 @default.
• W2939856912 cites W2034729531 @default.
• W2939856912 cites W2037497238 @default.
• W2939856912 cites W2043890918 @default.
• W2939856912 cites W2047646918 @default.
• W2939856912 cites W2053719646 @default.
• W2939856912 cites W2055708888 @default.
• W2939856912 cites W2057313876 @default.
• W2939856912 cites W2063085794 @default.
• W2939856912 cites W2064306427 @default.
• W2939856912 cites W2064491829 @default.
• W2939856912 cites W2069390842 @default.
• W2939856912 cites W2074741587 @default.
• W2939856912 cites W2075235892 @default.
• W2939856912 cites W2077200936 @default.
• W2939856912 cites W2082225381 @default.
• W2939856912 cites W2085097206 @default.
• W2939856912 cites W2089361639 @default.
• W2939856912 cites W2093839124 @default.
• W2939856912 cites W2096896494 @default.
• W2939856912 cites W2104713109 @default.
• W2939856912 cites W2110089296 @default.
• W2939856912 cites W2120361215 @default.
• W2939856912 cites W2140291031 @default.
• W2939856912 cites W2145060547 @default.
• W2939856912 cites W2149927623 @default.
• W2939856912 cites W2167313631 @default.
• W2939856912 cites W2170790198 @default.
• W2939856912 cites W2233082033 @default.
• W2939856912 cites W2281689620 @default.
• W2939856912 cites W2466369935 @default.
• W2939856912 cites W2590471558 @default.
• W2939856912 cites W2614998559 @default.
• W2939856912 cites W2721690067 @default.
• W2939856912 cites W2783225743 @default.
• W2939856912 cites W2888472733 @default.
• W2939856912 cites W2894864879 @default.
• W2939856912 cites W334951106 @default.
• W2939856912 cites W4231178516 @default.
• W2939856912 cites W4234864407 @default.
• W2939856912 cites W4239058796 @default.
• W2939856912 cites W4253301371 @default.
• W2939856912 doi "https://doi.org/10.5194/tc-13-1167-2019" @default.
• W2939856912 hasPublicationYear "2019" @default.
• W2939856912 type Work @default.
• W2939856912 sameAs 2939856912 @default.
• W2939856912 citedByCount "17" @default.
• W2939856912 countsByYear W29398569122019 @default.
• W2939856912 countsByYear W29398569122020 @default.
• W2939856912 countsByYear W29398569122021 @default.
• W2939856912 countsByYear W29398569122022 @default.
• W2939856912 countsByYear W29398569122023 @default.
• W2939856912 crossrefType "journal-article" @default.
• W2939856912 hasAuthorship W2939856912A5007627846 @default.
• W2939856912 hasAuthorship W2939856912A5009150889 @default.
• W2939856912 hasAuthorship W2939856912A5017565455 @default.
• W2939856912 hasAuthorship W2939856912A5080125372 @default.
• W2939856912 hasBestOaLocation W29398569121 @default.
• W2939856912 hasConcept C121332964 @default.
• W2939856912 hasConcept C127313418 @default.
• W2939856912 hasConcept C187320778 @default.
• W2939856912 hasConcept C205093917 @default.
• W2939856912 hasConcept C2524010 @default.

• next