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1 ed melt inclusions (with a mean value of 145 megapascals).
2  strength of the graphene fiber reaches 1080 megapascals.
3 meters, with a triggering threshold of ~0.07 megapascals.
4 ng to large pressure changes of the order of megapascals.
5 as low as 0.0004 at pressures as high as 7.5 megapascals.
6 , we achieve yarn strengths greater than 460 megapascals.
7 he pressure of the melt by approximately 500 megapascals.
8  cent and a tensile strength of around 2,000 megapascals.
9 an excellent work-hardening capacity of >300 megapascals.
10           The peak traction is sigma(0) ~ 60 megapascals.
11 ummit, reducing its internal pressure by ~17 megapascals.
12 Our material has a tensile strength of 1,300 megapascals and 10 per cent elongation, showing superior
13 ic acid), achieves a tensile strength of 6.9 megapascals and a hysteresis of 16.6%.
14 ltrawide modulus tunability (10 pascals to 1 megapascal) and superior mechanical properties, includin
15 cals-higher than mammalian muscle (about 0.3 megapascals) and comparable to ceramic piezoelectric act
16 to ceramic piezoelectric actuators (about 40 megapascals)-and strains of about 0.6 per cent, operatin
17 ditions of 300 degrees to 350 degrees C, 100 megapascals, and 4 to 5 months in the absence of microbi
18    Young's moduli for NFVB in situ (6.3 MPa [megapascals]) and in vivo (11.8 MPa) were approximately
19 arbonate-urethane and is soft but tough (~15 megapascal at a rupture strain of >2).
20 per mil as pressure increases from 15 to 800 megapascals at 380 degrees C.
21 red modulus for an ultralight material (12.3 megapascals at a density of 7.2 milligrams per cubic cen
22 give static stress drop estimates (~12 to 15 megapascals) compatible with theoretical radiation effic
23  range of Young's modulus (in kilopascals to megapascals) demonstrate the capability of the device to
24 ed to a leaf water potential (psi w) of -2.0 megapascal during vegetative growth.
25 esistance of the ground to penetration of >4 megapascals, equivalent to >2 megapascal uniaxial compre
26  ultralightweight objects to ultrastrong (>1 megapascal) for picking up and lifting heavy objects.
27  to generate mechanical stresses of about 17 megapascals-higher than mammalian muscle (about 0.3 mega
28              We infer that an increase of >1 megapascal in pore pressure in rocks with low compressib
29 xceeding 2000 hours at 750 degrees C and 100 megapascals in air, and resistance to oxidation in air w
30  stem water potentials of approximately -1.2 megapascals in drought experiments.
31 study had a threshold strength of 482 +/- 20 megapascals, in fair agreement with the theory.
32 tor can generate contractile stress up to 27 megapascals, lift objects 380 times heavier than itself,
33 itiation fracture toughnesses of 262 and 459 megapascal-meters(1/2) (MPa.m(1/2)) for CrMnFeCoNi and C
34 material with a mechanical strength of 404.3 megapascals, more than eight times that of natural wood.
35 thin the orbit ranged between +0.25 and -1.4 MegaPascal (MPa) for tympanic rupture, +3 and -1 MPa for
36  the canine corneal strips was 1.54 +/- 0.43 megapascal (MPa).
37 h and fracture toughness [ approximately 200 megapascals (MPa) and approximately 30 MPa.m(1/2)] repre
38 oli strain MG1655 at pressures of 68 to 1680 megapascals (MPa) in diamond anvil cells.
39 and a Root Mean Squared Error (RMSE) of 5.09 Megapascals (MPa) on the held-out test set.
40 tensile modulus, for example, from 800 to 20 megapascals (MPa), upon exposure to a chemical regulator
41  newtons [N]) and tooth pressures (718-2,974 megapascals [MPa]) promoting crack propagation in bones,
42                            Under hundreds of megapascals of apparent negative pressure, the bandgap t
43  hydrostatic pressure mimicking shallow (0.1 megapascal or MPa) and deep-sea (5-15 MPa; representativ
44 fficients of mu < 0.002 at pressures up to 5 megapascals or more, has to date not been attained in an
45 ic pressure of the cell sap declined by 0.14 megapascal over 5 hours.
46 istent with a steady-state stress of tens of megapascal over a 100-nanometer scale region near the mo
47 emperatures and a Clapeyron slope of about 6 megapascal per kelvin.
48 or different rates of fluid injection, slow (megapascals per hour) versus fast (megapascals per secon
49 on, slow (megapascals per hour) versus fast (megapascals per second).
50 rittle, with low fracture toughness (about 4 megapascals per square-root metre)(3,6).
51 h of 12.7 +/- 3.8 gigapascals and 488 +/- 57 megapascals, respectively.
52 s C and elevated pressures (50, 100, and 200 megapascals) revealed a facile, pressure-enhanced synthe
53 th a relatively high stress drop of about 20 megapascals, showing that large stresses can accumulate
54 bacterium under conditions (55 degrees C, 10 megapascals) simulating a methane-bearing subsurface.
55  for example, an ultimate stress of 23.5 2.7 megapascals, strain levels of 2,900 450 per cent, toughn
56  satisfy the well known observations of 1-10 megapascal stress drops and limited heat production.
57 lization pressures (with a mean value of 270 megapascals) than olivine-hosted melt inclusions (with a
58                          At 400°C and 40 megapascals, the in situ pH of the fluids, ranging from
59  and coalescence in basaltic magmas from 100 megapascals to surface.
60 etration of >4 megapascals, equivalent to >2 megapascal uniaxial compressive strength.
61 ength of metre-sized boulders is 0.44 to 1.7 megapascals, which is low compared to that of solid terr
62  the UFG structure was doubled to around 710 megapascals, with a uniform ductility of 45 per cent and