Rayleigh Sound Wave Propagation on a Gallium Single Crystal in a Liquid He3 Bath G

Total Page:16

File Type:pdf, Size:1020Kb

Load more

Rayleigh sound wave propagation on a gallium single crystal in a liquid He3 bath

G. Bellessa

To cite this version:

G. Bellessa. Rayleigh sound wave propagation on a gallium single crystal in a liquid He3 bath. Journal de Physique Lettres, Edp sciences, 1975, 36 (5), pp.137-139. ꢀ10.1051/jphyslet:01975003605013700ꢀ. ꢀjpa-00231172ꢀ

HAL Id: jpa-00231172 https://hal.archives-ouvertes.fr/jpa-00231172

Submitted on 1 Jan 1975

  • HAL is a multi-disciplinary open access
  • L’archive ouverte pluridisciplinaire HAL, est

archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés.

L-137

RAYLEIGH

GALLIUM

SINGLE

SOUND

WAVE

CRYSTAL IN

PROPAGATION

A

ON

A

He3 BATH

LIQUID

G. BELLESSA

Laboratoire de

des Solides

91405

Physique

Centre

(*)

Université

France

Paris-Sud,

d’Orsay,

Orsay,

Résumé.

un monocristal de

Nous décrivons

de

l’observation de la

d’ondes

sur

propagation

d’études sont

élastiques

Rayleigh

entre 40 MHz et 120 MHzet

Les

gallium.

d’étude la

fréquences

basse est K. La

comprises

la

et

vitesse

l’atténuation sont étudiées

le bain

à

des

0,4

température

tures différentes. L’atténuation des ondes de

plus

tempéraà des tem-

d’He3 est aussi étudiée

Rayleigh par

et des

différentes.

pératures

fréquences

Abstract.

We

the

report

observation of the

to 120 MHzand

sound wave

on

a

Rayleigh

propagation

gallium

and the

the He3

at

down to 0.4 K. The

single crystal

frequencies up

temperatures

velocity

by

attenuation are studied

at different

The

attenuation of

waves

temperatures.

and

Rayleigh bath is also

studied at different

temperatures

frequencies.

Elastic surface waves have been

studied

quartz

combs are

comb teeth are 20

other of 40

on the ZnS film

The

extensively

and lithium

evaporated

1).

(Fig.

on

wide and

are distant from each

materials,

piezoelectric

mainly

p.

niobate

waves on

There are also some

films

studies of

Each comb consists

of teeth and is

40

[1].

Rayleigh

on

~.

a

distant from its

0.5

6

mm.

A

RF

piezoelectric

evaporated

glass

neighbour by

pulse

substrate

The effects of thin

metallic films eva-

is

between one comb

[2].

on

(about

duration)

gas

applied

a

substrate have been

and the

metallic

is

porated

studied

piezoelectric

sample (the

sample

grounded).

and the effects of the

electrons on the

[3, 4]

of

waves have been observed

propagation

Rayleigh

the

(mainly

transition).

normal-superconducting

However the

of these effects are

small,

magnitude

because the thickness of the

much smaller than the

films are

evaporated

In this

wave

Rayleigh wavelength.

ofthe

we

the observation

a

letter,

report

on

Rayleigh

We

single crystal.

the attenuation

propagation

gallium

report

varia-

some

results about

preliminary

transition and

tion in the

normal-superconducting

waves

He3.

aboutthe attenuationof

Rayleigh

byliquid

The

is

single crystal

Experimental technique.

made with

in

The

a

mold

which

plastic

single crystal

very pure gallium

has two

machined and

faces

is not

wave

FIG. 1.

for

wave

the

polished

[5].

Experimental

arrangement

are the

Rayleigh

gene-

ration. The

c

axis

axis ofthe Gallium

a, b,

surfaces for the

crystallographic

good

Rayleigh

with

the

usual notations.

crystal

are obtained

this method. The

propagation

directly by

flat surfaces of the

are normal to the

b

gallium crystal

film

ZnS

of

is

axis

and

onto the

a

(Fig. 1)

evaporated (about

A

the

wave

is

on the metal surface if

Rayleigh

generated

This

film

6

000

A)

crystal.

piezoelectric

of

the RF

is

the wave-

such that

frequency

pulse

acts as an electro-mechanical transducer. Twometallic

of the

wave

the teeth

length

Rayleigh

equals

propagates

reaches the second comb

spacing.
The acoustic surface

wave

normal to the

comb teeth and

is

Laboratoire associe au C.N.R.S.

(*)

(which

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyslet:01975003605013700

L-138

well

to the first

after

a

certain

time. At

TABLE

I

one)

is observed on

parallel

an RFpulse

this time

the

second comb.

in

at

waves velocities

105

Rayleigh

(in

cm/s)

gallium

no reflexion of the

Weobserve

combs. So

case of bulk acoustic

on the

pulse

The

b

axis

is normal

different

(in Kelvin).

temperatures

and the

sound

there are no successive

and it is not

echoes

in the

(as

to the

The

is

the

c

a.~is.

surface

propagation

along

wave

to make an

waves)

possible

velocities

the bulk

for

propagation

measurement of the attenuation.

absolute

In

order to

three

evaporate

the

b

axis are taken

K. R.

and

along

from

Lyall

do

it

would be

to

this,

necessary

J. F. Cochran

[6].

metallic combs on the

2

shows the

crystal. Figure

that we observe on the

second comb

delayed pulse

after

and detection. The first saturated

to the

amplification

excitation of the

waves

on

pulse corresponds

pulsed

emitter comb. We have observed

at 40 MHz

Rayleigh

80 MHz and

gallium

(fundamental),

harmonics).

120 MHz(2nd and 3rd

We have also

the

in

K

a

field

put

sample

At 0.4

magnetic

to the

is

there

a

(normal

surface).

sharp

super-

In the normal

in the attenuation in the

transition

of

the

change

vicinity

conducting

(around 60 Oe).

2

it

the attenuation increases

to

kOe.

Then

state,

up

remains

constant

to 10 kOe. The total

roughly

up

K

MHz

and 80

is

variation of the attenuation at 0.4

found to be :

Attenuation of

waves

He~.

rayleigh

by liquid

of

The main mechanism of

absorption

Rayleigh

compres-

waves

ambient

media is the emission of

by

sional waves in

the fluid

the

during

propagation [1].

This

for the attenuation :

process

gives

FIG. 2.

to the the

Recorder

wave

of

the

The

first saturated

a)

tracing

delayed

pulse corresponding

train.

to

Rayleigh

pulse corresponds

excitation of the emitter comb.

Recorder

  • of
  • pulsed

b)

versus the

tracing

the

variation

level. Out

delayed

sample

changed by

pulse amplitude

liquid

liquid

at 1.2 K.

where

the

is the fluid

the

the

in

sound

pp

density, VF

of the

velocity

the

wave.

means

surface

out of the He3 bath. The

level is

fluid,

solid,

p

density

VR

Rayleigh

He3

and ÅR

liquefying

gaz

slowly

and the

of the

a

velocity

wavelength

we start from

surface out of

of the

wave

Experimentally,

sample

and attenuation

to measure the

measurements.

wave

There

Velocity

are two

the He3 bath and we record the

amplitude

Rayleigh

liquid

ways

Rayleigh

velocity.

to the

delayed pulse corresponding

,

Thefirst one is to measure the transit time ofthe

between the two combs. The second is to

pulse.

train

Wethen

and werecord

as soon as

the

level in the

(Fig. 2).

change

  • the
  • adjust

a

decrease ofthe

cryostat

delayed pulse

of the RF

in order to obtain the

on the receiver

frequency

largest amplitude

pulse

of the

He3 covers the

recorder

the attenuation does not

amplitude

liquid

sample

delayed pulse

surface.

2

shows such

a

As

tracing.

Figure

comb. This last method is the most sensitive because

can be seen on the

curve,

to its final value. We shall

the

of the comb’ is

ofthe numberofteeth andour combs

to the

selectivity

proportional

consider this

fall

directly

square

are

(40 teeth)

varia-

In

later. Wehave measured the attenuation

point

I

Table

the results of our

selective

[1 ].

gives

very

different

and

tion for

frequencies.

temperatures

measurements at different

and the bulk

temperatures

comparison

measure the attenuation

the ratio of the

we do not

in the two

to the

order to

take

variation,

wave velocities for

As we have written

from ref.

(taken

[6]).

pulse heights

simply

we cannot

measure the

above,

errors

This method can introduce

ofthe

cases.

owing

absolute attenuation but wecan measure the variation

Weavoid this

non-linearity

amplifiers.

possible

ofthe attenuationversus

The

attenuation

4.2

and

temperature.

the RF

generator amplitude

difficulty, by changing

is found to be

constant between

K

roughly

in

to obtain the same

We then take the ratio

the two

corresponding

Our results are

in order

pulse height

1.1

K(superconducting

transition

Below 1.1

K

of Ga).

sensitive to the

of the

cases.

is

the attenuation

very

temperature.

of the

values

generator amplitude.

have found for

We

the variation of the attenuation

in Table II. There is no measurement at

and 1.2 K because the attenuation of

reported

of surface waves at 80 MHz :

,

120 MHz

waves in

is

above the

11

0.5

K) -

K)

~(0.4

dB/cm .

gallium

very large

Rayleigh

o~(1.2

L-139

TABLE II

In

variation

conclusion let us

consider the

covers the

attenuation

surface

.

as

the

Measured values

waves in

the attenuation

just

In

maximum

liquid

sample

of

(in

dB/cm)

(leal

of

this case the

attenuation curve has successi-

He3.

is

(Fig. 2).

the

Rayleigh

gallium by liquid

a

and

2

a

minimum before

its

calculated value

1.

At 0.4

K

Gallium

vely

reaching

obtained from

eq.

final value

the

minimum

corres-

is

T

is

the

wave.

F

and

the

(in Fig.

amplitude

superconducting.

temperature

to the

This

behaviour

attenuation

the

ponds

can be

maximum).

frequencyof

Rayleigh

into account the effect ofan

surface. The attenuation

explained by taking

helium film

the

on

sample

does

not consider

return

to

(1)

any

waves on the surface

process leading

of the emitted

eq.

compressional

helium

film

on the

a

there is

If,

sample.

sample,

to

it is then

instead ofa semi-infinite

media,

reflections.

necessary

the

consider such

wave radiates

Schematically

Rayleigh

a

wave

which is almost

compressional

transition

and

temperature

significant

it

has

the

superconducting

is

to Arc

normal to the surface

(the

angle

compressional

of the film and then returns

therefore

equal

notbeen

possible

to

obtain

a

value.

The

calculated

(leal is

The

wave is reflected

sin

40).

VF/VR

on the

calculated

values are

obtained from

value

eq. (1).

surface

sample

upper

toward the

smaller than

therefore seems there is

the

systematically

experi-

surface. There are

mental ones. It

attenuation

the

wave.

wave and the

If the interferences are

interferences between

Rayleigh

mechanism other than that due to the

emission of

reflected

compressional

waves

the

It is

compressional

during

to consider in the

propagation.

if

d

destructive i.e.

2 d

is

+

(2 n

1)

(where

in the

~,F/2

not

case the

necessary

present

from frictional

the film thickness

there is an attenuation maximum. There is also an

and the

wavelength

fluid),

attenuation

losses

process arising

[1].

This mechanism

x

indeed

a

attenuation

gives

negligible

minimum

if

attenuation

2 d ^~

Thus

the maxi-

~p.

MHz. At 0.4

at 80

K

to

5

10-3

equal

(Ga

dB/cm

mumand the minimum of the attenuation in

2

figure

is then

the

attenuation

superconducting),

by

would

and

to

a

thickness of

film

correspond

0.5 ~

~,F/4

He3 versus

does not deviate

liquid

frequency

appre-

if

the

/!.F/2

1 ~

respectively. Experimentally,

from

a

linear law in

with

ciably

agreement

longer proportional

what weare

(1).

to

eq.

film thickness was well defined there would

be

absorp-

At 1.2

K

the attenuation is no

tion resonances for

resonances would be

thicknesses and these

In our case the film

many

very sharp.

the

here

is,

frequency. Perhaps,

beginning,

surface wave attenuation

observing

at its

the effect of the electrons on the

thickness is

not well defined and we observe

resonance.

probably

helium.

This

by liquid

Kapitza

a

only

very damped

in the

effect is involved

resistance

pro-

Theauthor is indebted to L.

Dumoulinand M. Boix

for useful

advices about the

and to J. Joffrin for

blem

and has been observed in

[7]

gallium [8]. Expe-

necessary

riments at

date this

are

to eluci-

frequencies

evaporation

fruitful

discussion.

higher

techniques

a

interesting point.

References

K. and

Mason

edited

France S. A. for the

of

DRANSFELD,

SALZMANN, E.,

Acoustics,

1970,

J.

[1]

[2]

Physical

by

supply

very pure gallium.

49

P.

(Academic, NewYork)

vol.

219.

K. R. and

COCHRAN,

J.

Can. J.

1076.

W.

7,

LYALL,

F.,

Teor. Fiz. 43

[6]

Phys.

(1971)

p.

44

A.

Zh.

1535

K. and

INABA, R., KAJIMURA,

MIKOSHIBA, N.,

[7] ANDREEV,

F.,

(1962)

(Sov. Phys.

Appl. Phys.

Eksp.

(1963) 1084).

F. J. and

JETP 16

2495.

(1973)

AKAO, F.,

409.

Rev.

Lett. 30A

WAGNER, F., KOLLARITS,

YAQUB, M.,

  • [8]
  • [3]

[4] [5]

Phys.

(1969)

Rev. B 7

Phys.

1117.

119.

Lett. 32

KRÄTZIG, E.,

(1973)

to P. DE LA

(1974)

Phys.

of Alusuisse

The author is indebted

BRETÈQUE

Recommended publications
  • Ellipticity of Seismic Rayleigh Waves for Subsurface Architectured Ground with Holes

    Ellipticity of Seismic Rayleigh Waves for Subsurface Architectured Ground with Holes

    Experimental evidence of auxetic features in seismic metamaterials: Ellipticity of seismic Rayleigh waves for subsurface architectured ground with holes Stéphane Brûlé1, Stefan Enoch2 and Sébastien Guenneau2 1Ménard, Chaponost, France 1, Route du Dôme, 69630 Chaponost 2 Aix Marseille Univ, CNRS, Centrale Marseille, Institut Fresnel, Marseille, France 52 Avenue Escadrille Normandie Niemen, 13013 Marseille e-mail address: [email protected] Structured soils with regular meshes of metric size holes implemented in first ten meters of the ground have been theoretically and experimentally tested under seismic disturbance this last decade. Structured soils with rigid inclusions embedded in a substratum have been also recently developed. The influence of these inclusions in the ground can be characterized in different ways: redistribution of energy within the network with focusing effects for seismic metamaterials, wave reflection, frequency filtering, reduction of the amplitude of seismic signal energy, etc. Here we first provide some time-domain analysis of the flat lens effect in conjunction with some form of external cloaking of Rayleigh waves and then we experimentally show the effect of a finite mesh of cylindrical holes on the ellipticity of the surface Rayleigh waves at the level of the Earth’s surface. Orbital diagrams in time domain are drawn for the surface particle’s velocity in vertical (x, z) and horizontal (x, y) planes. These results enable us to observe that the mesh of holes locally creates a tilt of the axes of the ellipse and changes the direction of particle movement. Interestingly, changes of Rayleigh waves ellipticity can be interpreted as changes of an effective Poisson ratio.
  • Development of an Acoustic Microscope to Measure Residual Stress Via Ultrasonic Rayleigh Wave Velocity Measurements Jane Carol Johnson Iowa State University

    Development of an Acoustic Microscope to Measure Residual Stress Via Ultrasonic Rayleigh Wave Velocity Measurements Jane Carol Johnson Iowa State University

    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1995 Development of an acoustic microscope to measure residual stress via ultrasonic Rayleigh wave velocity measurements Jane Carol Johnson Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Applied Mechanics Commons Recommended Citation Johnson, Jane Carol, "Development of an acoustic microscope to measure residual stress via ultrasonic Rayleigh wave velocity measurements " (1995). Retrospective Theses and Dissertations. 11061. https://lib.dr.iastate.edu/rtd/11061 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quali^ of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and inqvoper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note win indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overk^.
  • Group Velocity Measurements of Earthquake Rayleigh Wave by S Transform and Comparison with MFT

    Group Velocity Measurements of Earthquake Rayleigh Wave by S Transform and Comparison with MFT

    EARTH SCIENCES RESEARCH JOURNAL Earth Sci. Res. J. Vol. 24, No. 1 (March, 2020): 91-95 GEOPHYSICS Group Velocity Measurements of Earthquake Rayleigh Wave by S Transform and Comparison with MFT Chanjun Jianga,b,c, Youxue Wanga,b*, Gaofu Zengd aSchool of Earth Science, Guilin University of Technology, Guilin 541006, China. bGuangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin 541006, China. cBowen College of Management, Guilin University of Technology, Guilin 541006, China. dChina Nonferrous Metals (Guilin) Geology and Mining Co,. Ltd, Guilin 541006, China. * Corresponding author: [email protected] ABSTRACT Keywords: Earthquake Rayleigh waves; group Based upon the synthetic Rayleigh wave at different epicentral distances and real earthquake Rayleigh wave, S velocity; S transform; Multiple Filter Technique. transform is used to measure their group velocities, compared with the Multiple Filter Technique (MFT) which is the most commonly used method for group-velocity measurements. When the period is greater than 15 s, especially than 40 s, S transform has higher accuracy than MFT at all epicenter distances. When the period is less than or equal to 15 s, the accuracy of S transform is lower than that of MFT at epicentral distances of 1000 km and 8000 km (especially 8000 km), and the accuracy of such two methods is similar at the other epicentral distances. On the whole, S transform is more accurate than MFT. Furthermore, MFT is dominantly dependent on the value of the Gaussian filter parameter α , but S transform is self-adaptive. Therefore, S transform is a more stable and accurate method than MFT for group velocity measurement of earthquake Rayleigh waves.
  • Some Observations on Rayleigh Waves and Acoustic Emission in Thick Steel Plates#∞

    Some Observations on Rayleigh Waves and Acoustic Emission in Thick Steel Plates#∞

    SOME OBSERVATIONS ON RAYLEIGH WAVES AND ACOUSTIC #∞ EMISSION IN THICK STEEL PLATES M. A. HAMSTAD National Institute of Standards and Technology, Materials Reliability Division (853), 325 Broadway, Boulder, CO 80305-3328 and University of Denver, School of Engineering and Computer Science, Department of Mechanical and Materials Engineering, Denver, CO 80208 Abstract Rayleigh or surface waves in acoustic emission (AE) applications were examined for nomi- nal 25-mm thick steel plates. Pencil-lead breaks (PLBs) were introduced on the top and bottom surfaces as well as on the plate edge. The plate had large transverse dimensions to minimize edge reflections arriving during the arrival of the direct waves. An AE data sensor was placed on the top surface at both 254 mm and 381 mm from the PLB point or the epicenter of the PLB point. Also a trigger sensor was placed close to the PLB point. The signals were analyzed in the time domain and the frequency/time domain with a wavelet transform. For most of the experiments, the two data sensors had a small aperture (about 3.5 mm) and a high resonant frequency (about 500 kHz). These sensors effectively emphasized a Rayleigh wave relative to Lamb modes. In addition, finite-element modeling (FEM) was used to examine the presence or absence of Rayleigh waves generated by dipole point sources buried at different depths below the plate top surface. The resulting out-of-plane displacement signals were analyzed in a fashion similar to the experimental signals for propagation distances of up to 1016 mm for out-of-plane dipole sources.
  • Estimation of Near-Surface Shear-Wave Velocity by Inversion of Rayleigh Waves

    Estimation of Near-Surface Shear-Wave Velocity by Inversion of Rayleigh Waves

    GEOPHYSICS, VOL. 64, NO. 3 (MAY-JUNE 1999); P. 691–700, 8 FIGS., 2 TABLES. Estimation of near-surface shear-wave velocity by inversion of Rayleigh waves ∗ ∗ ∗ Jianghai Xia , Richard D. Miller , and Choon B. Park as the earth–air interface. Rayleigh waves are the result of in- ABSTRACT terfering P- and Sv-waves. Particle motion of the fundamental The shear-wave (S-wave) velocity of near-surface ma- mode of Rayleigh waves moving from left to right is ellipti- terials (soil, rocks, pavement) and its effect on seismic- cal in a counterclockwise (retrograde) direction. The motion wave propagation are of fundamental interest in many is constrained to the vertical plane that is consistent with the groundwater, engineering, and environmental studies. direction of wave propagation. Longer wavelengths penetrate Rayleigh-wave phase velocity of a layered-earth model deeper than shorter wavelengths for a given mode, generally is a function of frequency and four groups of earth prop- exhibit greater phase velocities, and are more sensitive to the erties: P-wave velocity, S-wave velocity, density, and elastic properties of the deeper layers (Babuska and Cara, thickness of layers. Analysis of the Jacobian matrix pro- 1991). Shorter wavelengths are sensitive to the physical proper- vides a measure of dispersion-curve sensitivity to earth ties of surficial layers. For this reason, a particular mode of sur- properties. S-wave velocities are the dominant influ- face wave will possess a unique phase velocity for each unique ence on a dispersion curve in a high-frequency range wavelength, leading to the dispersion of the seismic signal.
  • Modeling and Control of Surface Acoustic Wave

    Modeling and Control of Surface Acoustic Wave

    MODELING AND CONTROL OF SURFACE ACOUSTIC WAVE MOTORS This thesis has been completed in partial fulfillment of the requirements of the Dutch Institute of Systems and Control (DISC) for graduate study. The research described in this thesis has been conducted at the department of Electrical Engineering at the University of Twente, Enschede and has been financially supported by the Innovative Oriented Research Program (IOP) Precision Technology from the Dutch Ministry of Economic Affairs. Title: Modeling and Control of Surface Acoustic Wave Motors Author: P.J. Feenstra ISBN: 90-365-2235-8 Copyright c 2005 by P.J. Feenstra, Enschede, The Netherlands No part of° this work may be reproduced by print, photocopy or any other means without the permission in writing from the publisher. Printed by PrintPartners Ipskamp, Enschede, Netherlands MODELING AND CONTROL OF SURFACE ACOUSTIC WAVE MOTORS PROEFSCHRIFT ter verkrijging van de graad van doctor aan de Universiteit Twente, op gezag van de rector magnificus, prof. dr. W.H.M. Zijm, volgens besluit van het College voor Promoties in het openbaar te verdedigen op donderdag 22 september 2005 om 13.15 uur door Philippus Jan Feenstra geboren op 31 maart 1975 te Workum, Nederland Dit proefschrift is goedgekeurd door: prof. dr. ir. J. van Amerongen, promotor dr. ir. P.C. Breedveld, assistent-promotor Contents Contents v 1 An introduction to SAW motors 1 1.1 Introduction ................................. 1 1.2 Definition and history ............................ 2 1.3 Classification of SAW motors ........................ 5 1.3.1 Translations ............................. 6 1.3.2 Constrained circular motions .................... 6 1.3.3 Rotations .............................. 6 1.3.4 Combinations ...........................
  • Surface-Wave Inversion for Near-Surface Shear-Wave Velocity

    Surface-Wave Inversion for Near-Surface Shear-Wave Velocity

    Surface-wave inversion for near-surface shear-wave velocity estimation at Coronation field Huub Douma ∗ (ION Geophysical/GXT Imaging solutions) and Matthew Haney (Boise State University) SUMMARY The method is a one-dimensional finite-element method. Even though in this work we use only Rayleigh waves, the method We study the use of surface waves to invert for a near-surface can be extended to Love waves (Haney & Douma, 2011a). shear-wave velocity model and use this model to calculate Since we are inverting dispersion curves, the inversion method shear-wave static corrections. We invert both group-velocity is inherently one-dimensional. Hence, lateral heterogeneity is and phase-velocity measurements, each of which provide in- obtained by applying the method, e.g., below receiver stations. dependent information on the shear-wave velocity structure. Even though the inversion is one-dimensional, the obtained For the phase-velocity we use both slant-stacking and eikonal models could be used as initial models for true 3D methods tomography to obtain the dispersion curves. We compare mod- that can help further refine the models. els and static solutions obtained from all different methods us- ing field data. For the Coronation field data it appears that the The data set we use for this work is the Coronation data set, phase-velocity inversion obtains a better estimate of the long- which is a large 3D-3C data set from eastern Alberta, Canada. wavelength static than does the group-velocity inversion. We show results from only one receiver line. The number of individual source-receiver pairs in this receiver line is over 100,000.
  • Rayleigh Wave Velocity Dispersion for Characterization of Surface Treated Aero Engine Alloys

    Rayleigh Wave Velocity Dispersion for Characterization of Surface Treated Aero Engine Alloys

    RAYLEIGH WAVE VELOCITY DISPERSION FOR CHARACTERIZATION OF SURFACE TREATED AERO ENGINE ALLOYS Bernd KOEHLER, Martin BARTH FRAUNHOFER INSTITUTE FOR NONDESTRUCTIVE TESTING, Dresden Branch, Dresden, Germany [email protected] Joachim BAMBERG, Hans-Uwe BARON MTU AERO ENGINES GMBH, Nondestructive Testing (TEFP), Munich, Germany ABSTRACT. In aero engines mechanically high stressed components made of high-strength alloys like IN718 and Ti6Al4V are usually surface treated by shot-peening. Other methods, e.g. laser-peening, deep rolling and low plasticity burnishing are also available. All methods introduce compressive residual stress desired for minimizing sensitivity to fatigue or stress corrosion failure mechanisms, resulting in improved performance and increased lifetime of components. Beside that, also cold work is introduced in an amount varying from method to method. To determine the remaining life time of critical aero engine components like compressor and turbine discs, a quantitative non-destructive determination of compressive stresses is required. The opportunity to estimate residual stress in surface treated aero engine alloys by SAW phase velocity measurements has been re-examined. For that, original engine relevant material IN718 has been used. Contrary to other publications a significant effect of the surface treatment to the ultrasonic wave velocity was observed which disappeared after thermal treatment. Also preliminary measurements of the acousto-elastic coefficient fit into this picture. INTRODUCTION Materials used for discs in aero engines are titanium and nickelbase-superalloys. The components of these alloys are surface treated to induce compressive stress which adds to the tensile stress created during turbine operation [1], [2]. Thereby, the total maximum tensile stress in the critical surface regions of the engine components is limited, leading to a longer lifetime.
  • A Methodology for the Analysis of the Rayleigh-Wave Ellipticity

    A Methodology for the Analysis of the Rayleigh-Wave Ellipticity

    127 EARTH SCIENCES RESEARCH JOURNAL Earth Sci. Res. SJ. Vol. 17, No. 2 (December, 2013): 127 - 133 SEISMOLOGY A methodology for the analysis of the Rayleigh-wave ellipticity V. Corchete Higher Polytechnic School, University of Almeria, 04120 ALMERIA, Spain ABSTRACT Key words: Ellipticity, multiple filter technique (MFT), time variable filtering (TVF), inversion. In this paper, a comprehensive explanation of the analysis (filtering and inversion) of the Rayleigh-wave ellipticity is performed, and the use of this analysis to determine the local crustal structure beneath the recording station is described. This inversion problem and the necessary assumptions to solve are described in this paper, along with the methodology used to invert the Rayleigh-wave ellipticity. The results presented in this paper demostrate that the analysis (filtering and inversion) of the Rayleigh-wave ellipticity is a powerful tool, for studying the local structure of the crust beneath the recording station. Therefore, this type of analysis is very useful for studies of seismic risk and/or seismic design, because it provides local earth models in the range of crustal depths. RESUMEN Palabras clave: Elipticidad; filtro técnico múltiple; filtrado temporal variable; inversión. En este artículo, será realizada una explicación fácil de comprender del análisis (filtrado e inversión) de la elipticidad de la onda Rayleigh, así como, de su aplicación para determinar la estructura local bajo la estación de registro. Este problema de inversión y los necesarios supuestos para
  • 8 Surface Waves and Normal Modes

    8 Surface Waves and Normal Modes

    8 Surface waves and normal modes Our treatment to this point has been limited to body waves, solutions to the seismic wave equation that exist in whole spaces. However, when free surfaces exist in a medium, other solutions are possible and are given the name surface waves. There are two types of surface waves that propagate along Earth’s surface: Rayleigh waves and Love waves. For laterally homogeneous models, Rayleigh waves are radially polarized (P/SV) and exist at any free surface, whereas Love waves are transversely polarized and require some velocity increase with depth (or a spherical geometry). Surface waves are generally the strongest arrivals recorded at teleseismic distances and they provide some of the best constraints on Earth’s shallow structure and low-frequency source properties. They differ from body waves in many respects – they travel more slowly, their amplitude decay with range is generally much less, and their velocities are strongly frequency dependent. Surface waves from large earthquakes are observable for many hours, during which time they circle the Earth multiple times. Constructive interference among these orbiting surface waves, to- gether with analogous reverberations of body waves, form the normal modes,or free oscillations of the Earth. Surface waves and normal modes are generally ob- served at periods longer than about 10 s, in contrast to the much shorter periods seen in many body wave observations. 8.1 Love waves Love waves are formed through the constructive interference of high-order SH surface multiples (i.e., SSS, SSSS, SSSSS, etc.). Thus, it is possible to model Love waves as a sum of body waves.
  • Lecture 4 Surface Waves and Dispersion

    Lecture 4 Surface Waves and Dispersion

    Observational Seismology Lecture 4 Surface Waves and Dispersion GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Surface Wave Dispersion GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Observations stretched stretched dispersed PS SS SSS wave packet surface waves Body waves Impulsive, short period (but later arrivals are stretched out due to attenuation). Higher frequencies make waves “sharper”. Surface waves Dispersed, arrive in wave packets. But note a wave packet might be a single wavelet (oceanic arrivals). GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Reminder Period T Phase velocity v = f λ Amp f – frequency = 1/T (s-1) λ - wavelength (m) t But a whole spectrum of different period or frequency waves are emitted from an earthquake because earthquake rupture is a complex fracture process. GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Body waves Body waves all travel at the same velocity even if they are different frequencies, as travelling through the body of the Earth where velocity changes are gradual (except for major discontinuities). Reminder 1/ 2 ⎛ 4 ⎞ K S + .µ α = ⎜ 3 ⎟ ⎜ ρ ⎟ ↓v increasing ⎝ ⎠ 1/ 2 ⎛ µ ⎞ β = ⎜ ⎟ ⎝ ρ ⎠ Velocity just depends on local elastic properties, e.g, of core or mantle GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Types of surface waves Love wave Rayleigh wave GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Surface waves Surface waves travel close to surface depth z Amplitude of surface waves decays exponentially with depth Amplitude −Z Z0 A(z) = A0 e Characteristic depth Amplitude at surface of penetration At Z = Z0 A(z) = A0 / e ~ A0 / 2 i.e., the amplitude at the characteristic depth of penetration is approx.
  • Rayleigh Wave Interactions with Tribological Contacts

    Rayleigh Wave Interactions with Tribological Contacts

    Rayleigh Wave Interactions with Tribological Contacts Eng Seng OOI Thesis submitted for the degree of Doctor of Philosophy Department of Mechanical Engineering University of Sheffield March 2015 Summary The use of ultrasonic reflectometry is a proven method of condition monitoring machine systems. The working principles are simple. A burst of ultrasonic signal is sent to the interface of interest where reflection of the signal takes place. The manner in which reflection takes place depends on the properties of the interface. As such, the reflected signal carries information regarding the interface that can be extracted with proper techniques. However, the use of ultrasonic reflectometry in condition monitoring is not without its limitations. Conventional ultrasound techniques make use of ultrasonic bulk waves that travel through the body of a given material. Problems arise when the medium through which the wave travels is attenuative. This prevents any passage of ultrasonic signals as most of the energy will be absorbed by the material. In addition, most components have complex designs, requiring that the signal pass through multiple interfaces before reaching the interface of interest. Reflections occur at these intermediate interfaces, reducing the overall energy content of the signal. In order to overcome these issues, the use of Rayleigh wave as an alternative is researched in the work carried out here. Instead of having to travel through the bulk of the material, Rayleigh waves function by propagating along the free surface of the said material, thereby circumventing the existing issues with the use of conventional bulk waves. The research here was carried out to seek an understanding of how Rayleigh waves interact with a contact interface.