Gravity Waves from Instantons
The geometry of a naked singularity created by standing waves near a Schwarzschild horizon,

Ilya Mandel
PACS numbers: 04.25.-g, 04.25.Nx, 04.30.-w
arXiv:gr-qc/0505149v1 30 May 2005
I.
INTRODUCTION AND SUMMARY
It is very important, in gravitational astronomy, to have accurate computations of the gravitational waves from the inspiral of a black hole binary [1]. However, computing these waves is extremely challenging: for the last ≈ 25 cycles of inspiral waves, post-Newtonian approximations fail [2], and numerical relativity can not yet evolve the full dynamical equations in this regime. It appears that the best hope for accurately computing the BBH inspiral waves is by a quasi-stationary approximation [3, 4]. In this approximation, the energy and angular momentum of the binary are conserved by the imposition of standing gravitational waves, and the spacetime has a helical Killing vector field. The standing-wave radiation required to keep the orbit stationary is computed by demanding that the energy contents of the gravitational waves (GW) be minimized [4]. Standing-wave radiation consists of a sum of ingoing and outgoing radiation at infinity, and downgoing and upgoing radiation at the black-hole horizons. The physical spacetime, with purely outgoing waves at infinity and downgoing waves at the horizons, can be recovered from the standing-wave spacetime by adding a perturbative radiation-reaction field [5]. The solution for the BBH inspiral consists of a series of quasi-stationary solutions
Thermal gravitational waves

v12
3kTc . 12
For a core temperature of Tc 10 7 K , the velocity of the particles is of the order of
8 10 5 m / s . For a star of density 200 g / cc 2 10 5 kg / m 3 , the numbeting in these values we get the power of thermal gravitational waves emitted as,
10 9 Watt at a frequency of 1017 Hz . E
2
The flux of thermal gravitational waves from the sun, received at earth is of the order of half a watt. 2. Thermal gravitational waves from compact stars In the case of white dwarfs, the number density is of the order of n1 n2 10 37 m 3 , and the velocity corresponding to the white dwarf temperature of Tc 10 8 K , is of the order of 2 10 6 m / s . The volume of the white dwarf is of the order of 4 1018 m 3 and the frequency corresponding to the temperature Tc 10 8 K is And for a white dwarf,
与引力波有关的英文诗句

与引力波有关的英文诗句 Title: Embracing the Invisible.In the ethereal dance of the universe,。
A secret rhythm plays, unseen and unheard,。
Yet felt in the tiniest tremors,。
Of space-time, warped and torn.Gravitational waves, silent symphony,。
Weave through the vast canvas of cosmos,。
An intangible harmony,。
That stirs the soul of the infinite.They tremble through the fabric of space,。
Like ripples on a vast ocean of stars,。
Altering the very weave of reality,。
In a dance of creation and destruction.These waves, invisible and elusive,。
Carry within them the echoes of big bangs,。
The whispers of colliding galaxies,。
The stories of a universe in flux.They are the echoes of creation,。
The breath of the universe,。
The whispers of the gods,。
The songs of the stars.They whisper through the void,。
In a language of quantum secrets,。
A language of strings and fields,。
托福阅读第三篇tpo75R -3原文+译文+题目+答案+背景知识

托福阅读第三篇tpo75R-3原文+译文+题目+答案+背景知识原文 (1)译文 (4)题目 (7)答案 (13)背景知识 (14)原文Seismic Waves①Seismic waves-energy waves produced by earthquakes-permit scientists to determine the location,thickness,and properties of Earth's internal zones.They are generated when rock masses are suddenly disturbed,such as when they break or rupture.Vibrations spread out in all directions from the source of the disturbance, traveling at different speeds through parts of Earth's crust and interior that differ in chemical composition and physical properties.The principal categories of these waves are primary,secondary,and surface. All three types of waves are recorded on an instrument called a seismograph.②Primary waves,or P-waves,are the speediest of the three kinds of waves and therefore the first to arrive at a seismograph station after there has been an earthquake.They travel through the upper crust of Earth at speeds of4to5kilometers per second,but near the base of the crust they speed along at6or7kilometers per second.In these primary waves,pulses of energy are transmitted as a succession of compressions and expansions that parallel the direction of propagation of the wave itself.Thus,a given segment of rock set in motion during an earthquake is driven into its neighbor and bounces back.The neighbor strikes the next particle and rebounds and subsequent particles continue the motion.Vibrational energy is an accordion-like push-pull movement that can be transmitted through solids,liquids and gases.Of course,the speed of Pwave transmission will differ in materials of different density and elastic properties.③Secondary waves,or S-waves,travel1to2kilometers per second slower than do P-waves.Unlike the movement of P-waves,rock vibration in secondary waves is at right angles to the direction of propagation of the energy.This type of wave is easily demonstrated by tying a length of rope to a hook and then shaking the free end.A series of undulations will develop in the rope and move toward the hook-thatis,in the direction of propagation.Any given particle along the rope, however,will move up and down in a direction perpendicular to the direction of propagation.It is because of their more complex motion that S-waves travel more slowly than Pwaves.They are the second group of oscillations to arrive at a seismograph station.Unlike Pwaves, secondary waves will not pass through liquids or gases.④Both P-and S-waves are sometimes also termed body waves because they are able to penetrate deep into the interior or body of our planet.Body waves travel faster in rocks of greater elasticity,and their speeds therefore increase steadily as they move downward into more elastic zones of Earth's interior and then decrease as they begin to make their ascent toward Earth's surface.The change in velocity that occurs as body waves invade rocks of different elasticity results in a bending or refraction of the wave.The many small refractions cause the body waves to assume a curved travel path through Earth.⑤Not only are body waves subjected to refraction,but they may also be partially reflected off the surface of a dense rock layer in much the same way as light is reflected off a polished surface.Many factorsinfluence the behavior of body waves.An increase in the temperature of rocks through which body waves are traveling will cause a decrease in velocity,whereas an increase in confining pressure will cause a corresponding increase in wave velocity.In a fluid where no rigidity exists,S-waves cannot propagate and P-waves are markedly slowed.⑥Surface waves are large-motion waves that travel through the outer crust of Earth.Their pattern of movement resembles that of waves caused when a pebble is tossed into the center of a pond.They develop whenever P-or S-waves disturb the surface of Earth as they emerge from the interior.Surface waves are the last to arrive at a seismograph station.They are usually the primary cause of the destruction that can result from earthquakes affecting densely populated areas.This destruction results because surface waves are channeled through the thin outer region of Earth,and their energy is less rapidly scattered into the large volumes of rock traversed by body waves.译文地震波①地震波是由地震产生的能量波,它们使科学家能够确定地球内部区域的位置、厚度和性质。
【英语】阅读理解记叙文训练题经典

【英语】阅读理解记叙文训练题经典一、英语阅读理解记叙文(含答案详细解析)1.根据短文内容,判断正误。
I was 15 months old, a happy and carefree kid, until the day I fell. It was a bad fall. I landed on a piece of glass that cut my eye badly. From then on, my injured, sightless, cloudy gray eye lived on with me.Sometimes people asked me embarrassing (使人难堪的) questions. Whenever kids played games, I was the "monster". I was always imagining that everyone looked down on(瞧不起)me. Yet mum would say to me, "Hold your head up high and face the world." I began to depend on that saying. As a child, I thought mum meant, "Be careful,or you will fall down or bump into something because you are not looking. "As a teenager, I usually looked down to hide my shame. But I found that when I held my head up high, people liked me.In high school, I even became the class president, but inside I still felt like a monster. All I really wanted was to look like everyone else. When things got really bad, I would cry to my mum and she would look at me with loving eyes and say," Hold your head up high and face the world. Let them see the beauty that is inside instead of your appearance(外貌) ."My mum's love was the sunshine that made me bright. I had faced hard times, and learned not only to be confident(自信的) but also to have deep compassion(同情) for others. "Hold your head up high "has been heard many times in my home. I say it to my children. The gift my mum gave me will live on.(1)The writer imagined that everyone looked down on her because of her appearance. (2)People always asked her embarrassing questions.(3)The writer's mum said "Hold your head up high" to her to make her more confident. (4)The writer understood the saying very well as a child.(5)The writer is living with a warm and brave heart now.【答案】(1)1(2)0(3)1(4)0(5)1【解析】【分析】本文讲了作者小时候因眼睛受伤导致外貌变丑而心情低落,在妈妈的帮助之下改变自己并变得自信的故事。
海面的波浪英语作文

海面的波浪英语作文The waves on the sea surface are a captivating and ever-changing sight. Let's explore the beauty and dynamics of these mighty waves.One of the remarkable aspects of the waves is their constant motion. They roll and tumble, driven by the forces of the wind and the ocean.The size and shape of the waves vary, ranging from small ripples to massive swells that can reach impressive heights.The sound of the waves crashing against the shore is both powerful and soothing. It creates a unique symphony that is a part of the coastal experience.The waves play a crucial role in shaping the coastline. They erode and shape the land, creating dramatic cliffs and sandy beaches.For surfers and water sports enthusiasts, the waves offer an exciting playground. They provide opportunities for thrilling rides and a connection with the power of the ocean.Observing the waves can be a meditative and calming experience. It allows us to connect with nature and appreciate the vastness of the sea.In conclusion, the waves on the sea surface are a source of inspiration and beauty, adding to the allure of the ocean.。
科技英语翻译练习

Atomic clocks in space could detect gravitational wavesClocks in space: narrowband gravitational-wave detector could take off. A proposal for a gravitational-wave detector made of two space-based atomic clocks has been unveiled by physicists in the US. The scheme involves placing two atomic clocks in different locations around the Sun and using them to measure tiny shifts in the frequency of a laser beam shone from one clock to the other. The designers claim that the detector will complement the LISA space-based gravitational-wave detector, which is expected to launch in 2034.太空中的原子钟可以探测到引力波太空中的时钟:窄带引力波探测器可能会大展宏图。
美国物理学家公布了一个由两个太空原子钟组成的引力波探测器的方案。
该方案包括在太阳周围的不同位置放置两个原子钟来测量从一个时钟向另一个时钟发出的激光束频率的微小变化。
设计人员称,该探测器将增强预计2034年发射的激光干涉空间天线(LISA):天基引力波探测器。
Gravitational waves are ripples in the fabric of space-time that are created when masses are accelerated. In February of this year, the LIGO collaboration announced the first-ever direct detection of gravitational waves – from the merger of two black holes – using a pair of kilometer -sized interferometers in the US. Just last week, a second detection was announced by LIGO from a different black-hole merger.引力波是时空结构中质量加速时产生的波纹。
天文学课件之15

Water in a Wave
Only the wave travels, the water circles Crests are formed from local water
– the faster it travels – the deeper water moves as it passes – the more energy it contains for a given amplitude
Tsunamis(海啸) are very long wavelength, very deep, very high energy waves
Tidal Resonance
Water Waves
Sloshing involves deep water waves: the whole liquid moves back and forth Surface waves only affect the liquid’s top
Water’s Motion
The power of tsunamis
Breaking Waves
Surface waves slow down in shallow water Waves bunch as the water gets shallower Waves get taller as the water gets shallower Waves break when water can’t form crest – Gradually sloping bottom: rolling surf – Steeply sloping bottom: plunging breakers
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We perform a first principles computation of the spectrum of gravity waves produced in open inflationary universes. The background spacetime is taken to be the continuation of an instanton saddle point of the Euclidean no boundary path integral. The two-point tensor correlator is computed directly from the path integral and is shown to be unique and well behaved in the infrared. We discuss the tensor contribution to the cosmic microwave background anisotropy and show how it may provide an observational discriminant between different types of primordial instantons. I. INTRODUCTION
∗ Aspirant
FWO-Vlaanderen
† email:T.Hertog@ ‡ email:N.G.Turok@
1
quantization of perturbations to be well posed [3], [4], [5]. In this paper we compute the spectrum of gravity waves for both Coleman-De Luccia and Hawking-Turok instantons. This paper is a companion to ref. [5], where scalar fluctuations about open inflationary instantons were calculated. Here we perform the analogous calculation for the tensor fluctuations and discuss possible observable signals in the CMB anisotropy power spectrum. The calculation is performed in the framework of the Euclidean no boundary proposal due to Hartle and Hawking [6], as discussed in [5]. The correlator is computed in the Euclidean region where it is uniquely determined by a Gaussian integral, and then analytically continued in the coordinates of the classical background solution into the Lorentzian region of interest. Our main result for the tensor correlator (32) is given in a form which is straightforward to compute numerically. We defer detailed numerical calculations of the CMB anisotropies to a future paper [7] in which both scalar and tensor contributions for a variety of scalar potentials will be discussed. There have over the last few years been many papers exploring similar calculations, mostly making one approximation or another [9], [10], [11]. Very recently, Garriga et. al. have independently obtained formulae for the scalar and tensor correlators similar to ours [12]. These formulae have been numerically implemented in ref. [14] which gives results for some examples of Coleman-De Luccia instantons calculated without approximation. We feel that the derivation given here is significantly clearer than in these papers, and that our method has several important conceptual advantages. First, all earlier authors performed a mode by mode analysis. In this framework, one requires a prescription for the vacuum state for each perturbation mode and this is taken to be the state in which the positive frequency modes are regular on the lower half of the instanton. This prescription is rather ad hoc. In contrast, our method is to simply perform the Euclidean no boundary path integral. This automatically gives a unique Greens function. There is no need for an additional prescription, indeed imposing one is contrary to the spirit of the no boundary proposal (see the discussion in [5]). The whole idea of the Euclidean no boundary proposal is that an essentially topological prescription should define the initial state of the universe. Analyticity arises because the background solution is a solution to a differential equation. Divergent fluctuation modes have infinite Euclidean action and are therefore suppressed in the path integral. Second, in the matching method of Garriga et. al., they devote a great deal of effort to determining the action for perturbations in region II, the part of the Lorentzian spacetime exterior to the open universe region. This introduces considerable technical complexity since the spatial hypersurfaces used in their canonical quantisation approach are inhomogeneous in region II. Our approach is to analytically continue directly from the Euclidean region into the open universe. Region II is just a part of the continuation route with no special significance. Third, as emphasised in [5], we deal throughout directly with the real space correlator. In this approach ‘super-curvature’ modes are automatically included and their relation to the ‘sub-curvature’ modes is thereby made clear. A related fact is that we find that the real space correlator to be infrared finite even in perfect de Sitter space, as mentioned below. Finally, Garriga et. al. only give formulae for equal-time correlators. To compute the microwave anisotropies one requires the unequal-time correlator, which we give here. We are also careful to define the continuation of the conformal time coordinate into the Euclidean region, which is not explained in ref. [14]. The paper is organised as follows. In section 2 we describe the relevant inflationary universe scenario provides an appealing explanation for the smoothness and flatness of the present universe, as well as a mechanism for the origin of density fluctuations. Until recently it was believed that inflation inevitably predicted a flat Ω0 = 1 universe. However in [1] it was shown that with mild fine tuning an open universe is also possible. The potential must have a sharp false vacuum in which the field is assumed to have become trapped. The field is then assumed to tunnel out via an instanton known as the Coleman-De Luccia instanton [2], producing a bubble within which slow roll inflation occurs. The interior of the bubble produced via the Coleman-De Luccia instanton is an infinite inflating open universe. Such models provide important counter-examples to the standard folklore but require quite contrived scalar field potentials. Recently, however, Hawking and one of us showed that open inflation can occur much more generally. We found a new class of instantons [3] that exist for essentially any inflationary potential, and provide saddle points of the Euclidean path integral. The continuation of these instantons is similar to that of the ColemanDe Luccia instantons, and they define initial conditions for open inflationary universes. Although the Hawking-Turok instantons are singular, the singularity is mild enough for the