ライフサイエンスコーパス: turbulent flow

1 ive control strategies for drag reduction in turbulent flow.

2 vides a way to quantify irreversibility in a turbulent flow.

3 urs when motile phytoplankton are exposed to turbulent flow.

4 ous to the local kinetic energy of eddies in turbulent flow.

5 sediment motion will begin when subjected to turbulent flow.

6 a restricted perception field swimming in a turbulent flow.

7 trophy (a measure of rotational energy) of a turbulent flow.

8 profiles from slow laminar flow to fast near-turbulent flow.

9 or kink to achieve a crossing, thus avoiding turbulent flow.

10 m in atherosclerosis progression at sites of turbulent flow.

11 ures is fundamental to the energy cascade in turbulent flows.

12 fluid dynamics for modeling two-dimensional turbulent flows.

13 ring formation and screw-like patterns in 3D-turbulent flows.

14 nalyze inertial particles in more complex or turbulent flows.

15 ral bottleneck for a better understanding of turbulent flows.

16 with the transition from laminar to quantum turbulent flows.

17 ecedented capabilities for the simulation of turbulent flows.

18 a universal description of extreme events in turbulent flows.

19 s an experimental challenge in particular in turbulent flows.

20 ar self-organization, defines a new class of turbulent flows.

21 tanding of the onset of turbulence and fully turbulent flows.

22 correspond to the intermittency observed in turbulent flows.

23 ng for the fluctuating forces encountered in turbulent flows.

24 al means for simulating high Reynolds number turbulent flows.

25 a universal scaling for polymer scission in turbulent flows.

26 nsive drag reducers in large Reynolds number turbulent flows.

27 osclerosis preferentially occurs in areas of turbulent flow and low fluid shear stress, whereas lamin

28 orrect small-scale properties of atmospheric turbulent flow and solar irradiance, and retain consiste

29 of different spatial scales existing in the turbulent flow and, in turn, alter the turbulence energy

30 s widespread in nature in laminar as well as turbulent flows and acts on different spatial scales fro

31 tly simulating high-dimensional PDFs of both turbulent flows and other chaotic systems that can usefu

32 ed diffusion resemble the self-similarity of turbulent flows and the role of viscous dissipation.

33 olisms for early life in a simple model of a turbulent flow, and find that balancing the turnover tim

34 anding of the interactions between boulders, turbulent flow, and instream habitat quality and availab

35 Enstrophy is an intrinsic feature of turbulent flows, and its transport properties are essent

36 thetic drag reducing polymers in large scale turbulent flow applications.

37 f velocity that tend to homogenize fluids in turbulent flows are absent, and molecular diffusion acro

38 Turbulent flows are highly intermittent--for example, th

39 Understanding turbulent flows arising from random dispersive waves tha

40 - and scale-dependent complexities of actual turbulent flows around an idled, utility-scale floating

41 S can distinguish laminar, transitional, and turbulent flows as well as identify approaching objects

42 tionary water while the other was exposed to turbulent flow at 20 cm/s.

43 mum stationary film thickness) to establish turbulent flow at Reynolds numbers (Re) as high as 9000.

44 cord the hydraulic history of gravity-driven turbulent flow at the time of Roman operation.

45 e being generated by dynamo action driven by turbulent flows at high conductivity.

46 performed in an open channel flume to obtain turbulent flow-based habitat complexity metrics importan

47 ps that can facilitate the estimation of the turbulent flow-based habitat complexity metrics in bould

48 oulder placement in rock-ramp arrangement on turbulent flow-based habitat complexity metrics.

49 ensity functions (PDFs) of a fully developed turbulent flow can be reconstructed with a set of unstab

50 f long-chain flexible polymer dissolved in a turbulent flow can drastically change flow properties, s

51 The transition from laminar to turbulent flow can involve a sequence of instabilities i

52 that collective movements of fish schools in turbulent flow can reduce the total energetic cost of lo

53 The turbulent flow, characteristic of active nematics, is in

54 Boulder-induced variations in turbulent flow characteristics affect the quality and av

55 drupole-tandem mass spectrometry with online turbulent flow chromatography for sample cleanup and ana

56 s metabolites from microsomal proteins using turbulent flow chromatography.

57 phase extraction have been achieved with the turbulent-flow column-switching technique.

58 comparable drag reduction performance under turbulent flow conditions as aqueous PEO solutions, whil

59 ynolds number as the least significant under turbulent flow conditions.

60 Turbulent flow created by pumping solutions through a sm

61 c (predator, prey, conspecific) and abiotic (turbulent flow, current) sources among hatchery-reared s

62 tter is especially important-will sheared or turbulent flows disrupt organism groups?

63 In turbulent flows, energy flux, the cornerstone of turbule

64 usion, and protection from thrombosis in the turbulent flow environment within the beating heart.

65 g equations, can be harnessed to predict how turbulent flows evolve.

66 icle-size resolving model, which couples the turbulent flow field within the vegetated volume and the

67 The turbulent flow fields and aerosol dynamics of particles

68 tion of previously unimaginable shock-driven turbulent flow fields that are of significant importance

69 The models are then embedded in turbulent flow fields to gain an understanding of the in

70 IPS pipe capable of withstanding laminar and turbulent flows for 180 and 90 minutes, respectively.

71 at, in both B. subtilis and P. aeruginosa, a turbulent flow forms in the tube and a zone of clearing

72 low-dimensional models of globally unstable turbulent flows from experimental measurements, with bro

73 the velocity time series of fully-developed turbulent flows, generated by (i) a regular grid; (ii) a

74 ated by shear stresses in highly fluctuating turbulent flow, has not been feasible.

75 of transport and dissipation of energy in a turbulent flow have not been completely understood.

76 Turbulent flows have been used for millennia to mix solu

77 which corresponds to sediment particles and turbulent flows impacting along the riverbed where the r

78 rizontal transport properties of the oceanic turbulent flow in which they are embedded.

79 ational description to numerically construct turbulent flows in a holographic superfluid in two spati

80 lity stochastic generation of spatiotemporal turbulent flows in complex, three-dimensional domains.

81 ance the predictive modeling and analysis of turbulent flows in environmental science and engineering

82 Turbulent flows in nature and technology possess a range

83 es a new scenario that can be common to many turbulent flows in photonic quantum fluids, hydrodynamic

84 The model explains turbulent flows in terms of the dipole stress that the b

85 Variability of turbulent flows in the atmosphere and oceans exhibits re

86 e mixing but less well the manner in which a turbulent flow influences it; but the latter is the more

87 The advection of a passive substance by a turbulent flow is important in many natural and engineer

88 ely 10-1000 microm) one can assume the local turbulent flow is isotropic, with no distinction between

89 timization confirmed a previous finding that turbulent flow is more favorable than laminar flow in de

90 conditions and in theory, the transition to turbulent flow is triggered by flow separation under the

91 dern computers, anything beyond the simplest turbulent flows is too chaotic and multiscaled to be dir

92 d field of sensory perception, swimming in a turbulent flow, is examined from first principles and a

93 s attention is the large-scale nature of the turbulent flows near transition once they are establishe

94 Transition from laminar to turbulent flow occurring over a smooth surface is a part

95 In this paper, the encounter problem in a turbulent flow of large Reynolds number is re-examined f

96 n involving deposition from a ground-hugging turbulent flow of rock fragments, salts, sulphides, brin

97 ism in the underlying silty ice, followed by turbulent flow of the lowest approximately 90 m of ice.

98 can extract critical length scales from the turbulent flows of an active nematic, anticipate contrac

99 In the present work, we study three turbulent flows of systematically increasing complexity.

100 Fishes moving through turbulent flows or in formation are regularly exposed to

101 pathogenesis of atherosclerosis at sites of turbulent flow, potentially through the inhibition of fi

102 theory assumes that energy transport in a 3D turbulent flow proceeds through a Richardson cascade whe

103 r a flow rate sufficiently high to exhibit a turbulent-flow profile.

104 ll-mixed yet simple microfluidic device with turbulent flow profiles in the reaction regions.

105 f thinner yet denser biofilms under high and turbulent flow regimes of drinking water, in comparison

106 However, simulations of turbulent flows remain hindered by the inability of heur

107 ructures and their statistical properties in turbulent flows remains largely unclear and is thus a ce

108 Here, we consider bubble pinch-off in a turbulent flow representative of natural conditions in t

109 The use of turbulent flow resulted in a faster and more rugged extr

110 cts were injected directly into an automated turbulent flow sample clean-up system, coupled to a liqu

111 he universal statistical properties that all turbulent flows share despite their different large-scal

112 y Simulation (ILES) is proposed for unsteady turbulent flow simulations involving the three-dimension

113 The predictive capabilities of turbulent flow simulations, critical for aerodynamic des

114 en qualitatively visualizing the large-scale turbulent flow structures around full-scale turbines do

115 ustering" of inertial particles in isotropic turbulent flow suggests a hidden mechanism of particle-p

116 Following its injection onto a column at turbulent flow, the drug and its metabolites are backwas

117 In two-dimensional turbulent flow, the seemingly random swirling motion of

118 Finally we argue that in a turbulent flow, these punctuated energy injections can s

119 Remarkably, in turbulent flows this process is severely hindered by the

120 Turbulent flow through vegetation are characterized by a

121 A method utilizing turbulent flow to perform ultrafast separations and scre

122 locity profiles of compressible wall-bounded turbulent flows to the incompressible law of the wall, i

123 nd numerical evidence that three-dimensional turbulent flow tracks, episodically but repeatedly, the

124 Upon crossing the laminar-to-turbulent flow transition regime, a significant reductio

125 0-2.4%) at 67 and 80 mm water depth, with a turbulent flow, velocities ranging from 0.4 to 1.8 m/s,

126 applies on models of the vWF molecule within turbulent flow was examined here.

127 ly resembles vortex shedding in hydrodynamic turbulent flows, was observed in sheep epicardial tissue

128 tic diffusion model of particle transport in turbulent flowing water.

129 + 1 dimensional PDF of a chemically reactive turbulent flow, we achieve reductions in memory and comp

130 of oil-particle aggregates (OPAs) formed in turbulent flows, we elucidated a new mechanism of partic

131 flow) and from inside the aneurysm segment (turbulent flow) were analyzed by flow cytometry and comp

132 on the model example of particle tracking in turbulent flows, which is particularly challenging due t

133 our fundamental understanding of multiphase turbulent flows will be beneficial for analyses of a wid

134 and a 2D Navier-Stokes model representing a turbulent flow with a localized perturbation.

135 that are interspersed in a smoother and less turbulent flow with a near-radial magnetic field.

136 These results were obtained for turbulent flows with Reynolds numbers 10,000 to 32,500.

137 curately generate inhomogeneous, anisotropic turbulent flows within complex domains.