ライフサイエンスコーパス: ductile

1 uced into a nanocomposite bcc Mg is far more ductile, 50% stronger, and retains its strength after ex

2 Pure titanium transforms from ductile alpha to brittle omega at 9 GPa, creating seriou

3 For perfectly ductile and perfectly brittle structures, the empirical

4 igid oceanic plates from the underlying warm ductile asthenosphere.

5 ates regulate the transition from brittle to ductile behaviour.

6 is related to the effective accommodation of ductile body-centered cubic dendrites at 77 K, character

7 For testing, we used invasive ductile carcinoma of the breast to query the literature

8 xpression included retinal cells of the eye, ductile cells of the salivary gland, exocrine cells of t

9 crodiffraction to discover how PLLA acquired ductile character and found that the crimping process cr

10 ductively cooling plates from the underlying ductile, convecting mantle.

11 , mineralized outer shell surrounding a more ductile core.

12 anisms that control mechanical properties of ductile crystalline materials.

13 ity and impact toughness, resulting from the ductile crystalline phases distributed uniformly within

14 gement, while that in consolidated silver is ductile deformation and flow of material.

15 gments, while wear in the silver occurred by ductile deformation and flow of materials.

16 ismic sliding (where high temperatures allow ductile deformation), with the deep aseismic zone exhibi

17 gh diffuse in width upon entering the deeper ductile domain aided by fluids and do not project as nar

18 ation as large as ~30%, at the same level of ductile face-centered-cubic metals.

19 itude higher breaking energy via a distinct, ductile failure mode.

20 her confinement or slower loading results in ductile failure once the brittle-ductile transition is c

21 er, the recent discovery of abundant brittle-ductile fault textures in silicic lavas has led to the c

22 a system of seismic asperities embedded in a ductile fault zone matrix.

23 high temperature the plastic deformation and ductile flow is meditated by the <110>{111} dislocation

24 grees C diamond crystals exhibit significant ductile flow with corresponding yield strength of 7.9 an

25 o identify the lower crust, characterized by ductile flow.

26 me contributing to this layer by melting and ductile flow.

27 acks, whereas SERM treatments lead to a more ductile fracture and mainly increase crack length with a

28 ontrolled, as for example has been shown for ductile fracture in metallic materials.

29 interior by a subsurface layer of liquid or ductile ice.

30 n mains compared with the alternative, lined ductile iron.

31 ergy dissipation by local plasticity in thin ductile layers on increasing the resistance to cracking

32 avor of elastic shell buckling, resulting in ductile-like deformation and recoverability.

33 ity and that mantle fluids can penetrate the ductile lithosphere, even in regions where there is no s

34 odel that simulates stress transfer from the ductile lower crust and upper mantle to the brittle uppe

35 n mantle fluids are able to flow through the ductile lower crust.

36 extension through the vertical extrusion of ductile lower-crust material, driven by a crustal densit

37 Ductile materials can absorb spikes in mechanical force,

38 r findings demonstrate that microtubules are ductile materials with self-healing properties, that the

39 e concepts can be used to rapidly design new ductile materials.

40 inute traces of bismuth in copper cause this ductile metal to fail in a brittle manner?

41 riting is used to pattern highly conductive, ductile metallic interconnects, springs, and freestandin

42 Intrinsically ductile metals are prone to catastrophic failure when ex

43 mechanostable muscle protein titin, a highly ductile model reconciles data over 10 orders of magnitud

44 scales and the insight for future design of ductile nanocrystalline metals.

45 Our work suggests that nature uses a ductile network of hydrogen bonds to engineer function o

46 Here we present a strong and ductile non-equiatomic HEA obtained after friction stir

47 ur results suggest that dwell can occur in a ductile noncracking target due to flow reversal.

48 width of 50-200 m reaching to the top of the ductile part of the crust, by observations on seismic gu

49 resent the activity of creep fracture in the ductile part of the lithosphere occurring over cracks wi

50 bre composed of a brittle core embedded in a ductile polymer cladding, cold-drawing results in a surp

51 s known quantitatively regarding its brittle-ductile properties and yield strength at high temperatur

52 ne substantially reduces the strength in the ductile regime within a certain temperature window.

53 Es) on faults in the vicinity of the brittle-ductile (seismic-aseismic) transition.

54 Direct dating of ductile shear zones and calculation of uplift/exhumation

55 ieved in our models by the formation of weak ductile shear zones.

56 ure is a robust dynamical feedback, in which ductile strain first localizes in relatively weak, quart

57 od only for the limiting cases of brittle or ductile structures.

58 etrical model applicable to brittle films on ductile substrates.

59 We show that the more ductile surfaces of cancellous bone are a result of redu

60 obility being responsible for the brittle to ductile temperature transition.

61 brittle fracture in pristine silicon versus ductile tensile deformation in fully lithiated silicon.

62 and continuously cover the entire range from ductile to brittle.

63 ed after recrystallization exhibits a higher ductile-to-brittle transition temperature which increase

64 GPa, near the ideal limit, with a remarkable ductile-to-brittle transition with decreasing twin size.

65 brittle compressive strength and the brittle-ductile transition are consistent with data from a varie

66 mechanistic underpinnings of the brittle-to-ductile transition governed by atomic bonding and lithia

67 The brittle to ductile transition in densified silica glass can be attr

68 We observe a brittle-to-ductile transition in samples with orthogonally oriented

69 results in ductile failure once the brittle-ductile transition is crossed.

70 s by nanoindentation show a rapid brittle-to-ductile transition of fracture as the lithium-to-silicon

71 in subduction zones, occur below the brittle-ductile transition, where high pressures render friction

72 ustal permeability, particularly the brittle-ductile transition.

73 ritical reinforcement volume for the brittle-ductile transition.

74 abrupt and dramatic size-induced "brittle-to-ductile" transition occurs around 100 nm.

75 ropic strength profiles identify the brittle-ductile transitions in lithospheric strength.

76 of milk-producing epithelial cells that form ductile tubules surrounded by a myoepithelial cell layer

77 domains of filamin and titin are kinetically ductile when pulled from their two termini, making them

78 indicate that ScCo, ScIr, and YCd should be ductile, whereas each was previously proposed to be brit

79 site of squid rhodopsin to be malleable and ductile, while that of bovine rhodopsin is rigid and sti

80 Importantly, the 60 vol.% Ap-SFRP remains ductile with 7% flexural elongation at lower temperature