نتایج جستجو برای: continuous surface waves

تعداد نتایج: 977296  

Journal: :international journal of civil engineering 0
a. haddad gh. shafabakhsh

local site conditions have a strong effect on ground response during earthquakes. two important soil parameters that control the amplification effects of seismic motions by a soil column are the soil hysteretic damping ratio and shear wave velocity. this paper presents the results of in situ damping ratio measurements performed using continuous surface wave attenuation data at a site in semnan ...

2002
Eric Debayle Malcolm Sambridge

correlation between r i and each geographical point r j belonging to path j (Fig.1 b) : Continuous regionalization for massive surface waves dataset Eric Debayle 1 and Malcolm Sambridge Institut de physique du globe de Strasbourg, CNRS and Université Louis Pasteur, Strasbourg, France ([email protected]) Research School of Earth Science, Australian National University, Canberra, Aus...

Journal: :فیزیک زمین و فضا 0
رامین موقری ژوهشگاه بین المللی زلزله شناسی و مهندسی زلزله، تهران غلام جوان دولوئی پژوهشگاه بین المللی زلزله شناسی و مهندسی زلزله، تهران مژگان نوروزی پژوهشگاه بین المللی زلزله شناسی و مهندسی زلزله، تهران احمد سدیدخوی گروه فیزیک زمین، موسسه ژئوفیزیک دانشگاه تهران

the mixture of natural and artificial seismic sources with random distributions cause diffuse wave field with random amplitudes and phases called noise. when noise is analyzed in a long-term process, it contains surface waves which are spread in all directions. thus, ambient noise contains data relevant to the surface waves. in recent years, as broadband seismic networks have been distributed v...

2012
E. Shamonina

A theory is presented combining effective-medium theory with that of magnetoinductive (MI) waves propagating by virtue of coupling between the resonant elements. The resulting circuit equations for the split-ring resonator (SRR) loaded transmission line are shown to be analogous to those describing a continuous anisotropic magnetic plasma exhibiting spatial dispersion due to interelement coupli...

2005
R. Porter D. V. Evans

In this paper, surface waves in the presence of an infinite periodic array of obstacles of rectangular cross-section are considered. Rayleigh–Bloch surface waves are described by a localised wave motion which does not propagate energy away from the array. The periodicity of the array implies the existence of a cut-off frequency below which Rayleigh–Bloch surface waves may be sought. Such soluti...

2004
P. Burgholzer C. Hofer B. Reitinger G. Paltauf A. Mohammed H. P. Degischer D. Loidl P. Schulz

Laser ultrasonics is based on the generation of elastic waves by transient surface heating or ablation with short laser pulses. These waves are traveling through the sample, are reflected and scattered at interfaces and the backside of the sample. To realize an ultrasound measurement device we have used either an interferometer coupled to a continuous wave laser (contact-free) or the sample was...

2010
R. C. MORGAN

where f(6) is a continuous function of 6. This radiation condition is more explicit than the usual Sommerfeld condition, and, by its very nature, rules out surface waves as they are oscillating and nondecaying along the boundary. It was found to be equally convenient to state and prove uniqueness for all N and \m9^ ±iK. The explicit far field behavior mentioned above is not required; rather we ...

2012
Kurt Ehlers George Oster

We propose a model for the self-propulsion of the marine bacterium Synechococcus utilizing a continuous looped helical track analogous to that found in Myxobacteria [1]. In our model cargo-carrying protein motors, driven by proton-motive force, move along a continuous looped helical track. The movement of the cargo creates surface distortions in the form of small amplitude traveling ridges alon...

ژورنال: :علوم و مهندسی زلزله 0
ایمان عشایری دانشگاه رازی کرمانشاه مهنوش بیگلری دانشگاه رازی کرمانشاه مجید رضایی صفت دانشگاه رازی کرمانشاه

انرژی لرزه ای حاصل از یک منبع زیرزمینی به شکل امواج لرزه ای در سازه های سطحی پخش می شود. این امواج که امواج حجمی نامیده شده اند، تغییر شکلهای حجمی بوسیله امواج فشاری، یا تغییر شکلهای برشی بوسیله موج برشی و یا با توجه به شرایط مرزی خاص در فصل مشترک لایه ها و یا در سطح زمین تغییر شکلهای دیگری به وجود می آورند. شرایط مرزی مربوط به سطح آزاد اجازه می دهد علاوه بر معادلات حرکت، پاسخهای اضافی دیگری نی...

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