ライフサイエンスコーパス: ascent

1 volatile-driven decompression during conduit ascent.

2 e bioconcentration dynamics following spring ascent.

3 irth weight of approximately 100 g/1000 m of ascent.

4 radient closely follows the line of steepest ascent.

5 od is quickly maximized by cyclic coordinate ascent.

6 nes were carried to the surface during magma ascent.

7 ary and undergo little lateral deflection on ascent.

8 o dose modification was more frequent in the ASCENT (31%) than in the control arm (15%).

9 tude and achieved even higher levels upon re-ascent, a feature that is positively associated with qui

10 On ascent after a diving exposure, the dissolved gas can ac

11 arch behavior was consistent with a gradient ascent algorithm that utilized directional cues in the p

12 n international perspective, we consider the ascent and decline of the autopsy, the legal frameworks

13 trials involving level-ground walking, ramp ascent and descent, and stair ascent and descent.

14 walking, ramp ascent and descent, and stair ascent and descent.

15 tensity curves showed a significantly slower ascent and diminished maximum intensity in pancreas graf

16 Wilson and Head model kimberlite ascent and eruption by considering the propagation of a

17 Here we present a new model of kimberlite ascent and eruption, emphasizing the extremely unsteady

18 Other flight modes including vertical ascent and fast forward flight are more mechanically and

19 of noble gases during mantle melting, magma ascent and near-surface degassing.

20 sult of entrainment of ambient mantle during ascent, and also on whether initial plume upwelling is a

21 as 17.8 months (95% CI, 16.0 to 19.5) in the ASCENT arm and 20.2 months (95% CI, 18.8 to 23.0) in the

22 erim analysis, more deaths were noted in the ASCENT arm, and the trial was halted.

23 estimate energy expenditure during stairway ascent at speeds chosen by the participants.

24 After 66 d at altitude and ascent beyond 6400 m, mitochondrial densities fell by 21

25 ation and the latitude of that circulation's ascent branch.

26 The vertical ascent by prostate cancer cells from the lowlands to the

27 ecreased relative role during the outbreak's ascent compared to non-receipt [OR 0.16 (0.01, 0.84) for

28 One mechanism for degassing during magma ascent, consistent with observations, is the generation

29 Ascent decreased the arterio-central venous concentratio

30 ilibrium processes to play a key role on the ascent dynamics.

31 our understanding of such disequilibria and ascent dynamics.

32 After the spring ascent from deep waters, C. hyperboreus approach equilib

33 barotrauma due to lung overexpansion during ascent from depth.

34 Ascent from ground level to the conditions of 7000 to 80

35 troleum fluids dissolved into the sea during ascent from the pared wellhead (1,505 m depth) to the se

36 dence interval [CI], 6.95-23.66; P < 0.001), ascent greater than 400 m/day (aOR, 5.89; 95% CI, 3.78-9

37 ssociated with the ACE genotype in the rapid ascent group (p = 0.01) with a relatively sustained Sa(O

38 he ACE genotype and remained so for the slow ascent group, in whom the fall in Sa(O(2)) with ascent w

39 Rapid ascent (n = 32) and slow ascent groups (n = 40), ascending to approximately 5,000

40 Timescales of magma ascent in conduit models are typically assumed to be muc

41 g from initial hypoxia is maintained upon re-ascent in humans or re-exposure to hypoxia in mice and a

42 d narrowing of the convective zone, enhanced ascent, increased high clouds, suppressed low clouds, an

43 This ascent is driven by buoyancy forces, which are enhanced

44 therm exhibits an hysteresis loop; a gradual ascent is observed at higher pressures during adsorption

45 ter acclimatization to high altitude upon re-ascent is seen in humans; however, the molecular basis f

46 from Mount Etna's 2001 eruption and a magma ascent model to constrain timescales for crystallization

47 Rapid ascent (n = 32) and slow ascent groups (n = 40), ascendi

48 truders throughout, and probably before, the ascent of ants to ecological dominance, with ancient gro

49 forces, such as urine flow, that prevent the ascent of bladder microbes.

50 he hypothesis that in these experiments, the ascent of intermediate-fitness compensatory mutants, rat

51 with the common "complex" diseases, and the ascent of man has been the product of 3.5 billion years

52 affects the thermal evolution of Earth, the ascent of mantle plumes, settling of subducted oceanic l

53 sence of these drugs commonly results in the ascent of mutations that ameliorate these costs, rather

54 ve rhyolite eruption indicate that the rapid ascent of rhyolite occurred through dyking and that melt

55 The ongoing ascent of sequencing technologies has enabled researcher

56 rconnected network, culminating in the rapid ascent of the basalt relative to the surrounding solid m

57 avaginal inoculation and confirmed the rapid ascent of the chlamydial organisms from the lower to upp

58 We show that the initial ascent of the meltwater outflow from the ice shelf cavit

59 ikely an influential factor that impeded the ascent of the parent magma and allowed the formation of

60 e classic model of pathogenesis proposes the ascent of UPEC by the urethra and external adherence to

61 TP, effectively short-circuiting the slower ascent of water vapor across the cold tropical tropopaus

62 As a test case, the invasive ascents of the Tepui by highly metastatic PC-3 and nonin

63 r solubility in magma reveals that, for many ascent paths, exsolution may be more efficiently achieve

64 The strong relation between magma ascent rate and disequilibrium crystallization and exsol

65 Their morphology, aspect ratio, inferred ascent rate, and temperature show that they are passivel

66 Ascent rates during these dives were significantly slowe

67 ses (reservoir chambers) with variable magma ascent rates, mostly within 48 hours.

68 ess, about 45 percent of air in the tropical ascent region at 21 kilometers is of mid-latitude origin

69 rkable stabilization due to asymmetry in the ascent region from the (E)-isomer to ITS.

70 reater depth are probably channelized during ascent, so preventing direct re-equilibration with shall

71 the thermal path experienced by magma during ascent strongly controls degassing, vesiculation, magma

72 taxa is consistent with slower responses in ascent than descent toward carrying capacity.

73 During ascent, the device is evacuated as it equilibrates with

74 The rate of migration increases with ascent through the intermediate zone (average 2-6.4 micr

75 ole in its bladder colonization and eventual ascent through the ureters, against urine flow, to invad

76 the PLM descent time in comparison with its ascent time.

77 oclase reaches equilibrium in 1-2 h, whereas ascent times were <1 h.

78 This approach--documenting magma ascent timescales from the mantle beneath a convergent m

79 es at low altitude (LA) and following active ascent to 4559 m (HA).

80 ll as on day 2 (MG2) and 4 (MG4) after rapid ascent to 4559 m.

81 As inspired oxygen availability falls with ascent to altitude, some individuals develop high-altitu

82 arterial blood from 10 climbers during their ascent to and descent from the summit of Mount Everest.

83 Subacute exposure (19 d after initiating ascent to Everest base camp, 5300 m) was not associated

84 The path to translation, like the ascent to Everest, is certainly littered with corpses.

85 nosine levels are rapidly induced by initial ascent to high altitude and achieved even higher levels

86 During ascent to high altitude and pulmonary edema, the alveola

87 Ascent to high altitude is associated with a fall in the

88 vestigate changes of intraocular pressure on ascent to high altitude.

89 g exposure to hypobaric hypoxia on a gradual ascent to Mount Everest Base Camp (5,300 m).

90 ers, and shapes the output of the DCN in its ascent to the inferior colliculi.

91 rtial melting in the mantle followed by melt ascent to the surface and gas exsolution.

92 mixing and mobilization of coal and basalt, ascent to the surface, explosive combustion, and the atm

93 ASCENT treatment was associated with shorter survival th

94 hey attribute to troposphere to stratosphere ascent via the Asian monsoon.

95 ent group, in whom the fall in Sa(O(2)) with ascent was genotype independent.

96 However, Sa(O(2)) with ascent was significantly associated with the ACE genotyp

97 usceptible individuals during the outbreak's ascent, with all ORs for each of those age groups vs. gr

98 c hypoxic conditions in the weeks before the ascent would be helpful.