ライフサイエンスコーパス: surface wave

1 itting and conversion of propagation wave to surface wave.

2 red near the surface with an interference of surface waves.

3 cal ground displacements during the Rayleigh surface waves.

4 , which is estimated from 300- to 500-second surface waves.

5 istics to conventional grating coupled Bloch surface waves.

6 water strider relies on momentum transfer by surface waves.

7 so by generating longitudinal or transverse surface waves.

8 ne-hertz GPS receivers also detected seismic surface waves 750 to 3800 kilometers from the epicenter,

9 cattering-immune propagation of a nontrivial surface wave across a three-dimension physical step.

10 sensitive measurements of the near-field of surface waves across the metasurface show the contrastin

11 and fidelity of crustal images obtained from surface-wave analyses.

12 because of the combination of unusually long surface waves and seismic stations near the local earthq

13 ries of experiments, emphasizing film flows, surface waves, and thermal convection.

14 In our model, these surface waves are driven by the travelling wave of elect

15 are encoded on the sample boundary), and the surface waves are Rayleigh waves.

16 mensional photonic crystals sustaining Bloch surface waves are tailored with a monoclonal antibody fo

17 ilometers), during times that high-amplitude surface waves arrive from the mainshock (less than 200 s

18 The generation of Bloch surface waves as a function of azimuthal angle has simil

19 be coupled into propagating electromagnetic surface waves at a metal-dielectric interface known as s

20 teering, ultrasound lens design and acoustic surface wave-based applications.

21 retrieve empirical Green's function (EGF) of surface waves between stations.

22 ltilayer, it supports a guided mode, a Bloch surface wave (BSW) confined in one dimension.

23 (PSi) grating-coupled Bloch surface and sub-surface wave (BSW/BSSW) biosensor is demonstrated to siz

24 The top segment supports Bloch surface waves (BSWs) at the excitation wavelength and th

25 interact with both internal modes and Bloch surface waves (BSWs) of the 1DPC.

26 ping, by taking advantage of a stop-band for surface waves, but also selective mode conversion of sur

27 the fluorophores thought to be lost by lossy surface waves can be recovered as emission by adjustment

28 demonstrate for the first time a dielectric surface wave cloak from engineered gradient index materi

29 The surface wave cloak is fabricated from a metallic backed

30 od agreement and performance as an effective surface wave cloak.

31 We show that the surface wave component can mutually cancel the direct tr

32 The conditions for Bloch surface wave coupling can be achieved by rotating both p

33 In addition, predictions from surface-wave-derived models are largely incompatible wit

34 The surface wave direction is switchable with the polarizati

35 approach can be generalised to all kinds of surface waves, either for the coupling and discriminatio

36 ent a novel optical structure design, termed surface-wave-enabled darkfield aperture (SWEDA), which c

37 xcitation, where energy is mostly carried by surface waves, energy reflection and redirection might l

38 m to the phase matching conditions for Bloch surface wave excitation.

39 f an M = 6.9 quake remotely triggered by the surface waves from an M = 6.6 quake 4,800 kilometres awa

40 As surface waves from the 26 December 2004 earthquake in Su

41 The distortion of the shape of the surface wave fronts due to the curvature is corrected wi

42 n California yields hundreds of short-period surface-wave group-speed measurements on interstation pa

43 However, azimuthally generated Bloch surface waves have enhanced angular sensitivity compared

44 Surface waves in topological states of quantum matter ex

45 re-emerged on the possibility to manipulate surface waves, in particular, towards the THz and optica

46 gths of MHA layer are unaffected whereas the surface wave is significantly increased, thereby paving

47 The polarity of the phase profile of the surface waves is found to be strongly correlated to the

48 interferometry and multichannel analysis of surface waves (MASW).

49 displacements as arising from the driving of surface wave modes in which potential energy is stored i

50 Here we combine long-period surface-wave observations with simultaneous Global Posit

51 ion at microwave frequencies of an analogous surface wave phenomenon whereby a metasurface supports a

52 Surface waves play an important role in the exchange of

53 in long-periodic NCAI-SNSPDs grating-coupled surface waves promote EM-field transportation to the NbN

54 ssibility of using nanocomposites to control surface wave propagation through advanced additive manuf

55 Interestingly, large transverse surface waves require a smaller additional noncollapse s

56 ssical dynamic fracture theories predict the surface wave speed to be the limiting speed for propagat

57 ely couple free-space beams into any type of surface wave, such as focused surface plasmon polaritons

58 e to E-field enhancement via grating-coupled surface waves synchronized with the NbN stripes in S-ori

59 In contrast, when surface wave systems are the focus, it has been shown th

60 displacements in Alaska and large-amplitude surface waves throughout western North America.

61 he function of this array may be to generate surface waves to power gliding.

62 was developed to assess the contribution of surface waves to the observed nighttime E. coli replenis

63 Here, using surface wave tomography, we establish the lateral extent

64 Here we report temporal changes of surface wave velocity over a large area associated with

65 Surface wave velocity, a nondestructive measure of tissu

66 steeper fault derived from seismic body and surface waves, we approximated free oscillation amplitud

67 iderations suggest that the so called "lossy surface waves" which quench fluorescence are due to indu

68 ng center using phase-delay times of seismic surface waves, which show anomalous polarization anisotr

69 Anomalous launch of a surface wave with different handedness phase control is

70 sitive mode index, and another that supports surface waves with negative mode index.

71 arrow band of frequencies: one that supports surface waves with positive mode index, and another that