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High Resolution FTS in Astronomy at 7 to 15 Microns 7至15微米的天文高分辨率FTS
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1989.wa3
D. Jennings
Infrared molecular and atomic lines in planets, stars, and dust clouds can only be resolved using the highest available spectral resolution. The Fourier transform spectrometer is presently the only type of spectrometer capable of resolving powers near 105 which can operate at arbitrary wavelengths in the infrared. However, because noise in a spectrum increases with resolution, working at high resolution requires maximum sensitivity. In the thermal infrared, radiation from the sky and warm optics is the dominant source of noise in a spectrum. In order to achieve 105 resolving power on even the brightest sources in the mid-infrared, special techniques must be used to minimize background radiation.
行星、恒星和尘埃云中的红外分子和原子线只能用最高的可用光谱分辨率来分辨。傅里叶变换光谱仪是目前唯一一种能够在任意波长的红外光谱中工作的分辨率接近105的光谱仪。然而,由于频谱中的噪声随着分辨率的增加而增加,因此在高分辨率下工作需要最大的灵敏度。在热红外中,来自天空和热光学的辐射是光谱中主要的噪声源。为了在中红外线最亮的光源上达到105的分辨能力,必须使用特殊的技术来减少背景辐射。
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引用次数: 0
Characteristics of a High Resolution Fourier Transform Spectrometer to Measure Atmospheric Gas Species in Emission from Space: the MIPAS Mission 测量空间发射大气气体的高分辨率傅立叶变换光谱仪的特性:MIPAS任务
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.fd4
D. Lamarre, J. Giroux, H. Buijs
In this paper we present the characteristics of the MIPAS instrument, its measurement objectives and several unique features related to high resolution emission measurements.
在本文中,我们介绍了MIPAS仪器的特点,它的测量目标和几个独特的特点有关的高分辨率发射测量。
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引用次数: 0
Isotope Shift in B I at 2090 Å as a Probe of Cosmic Nucleosynthesis 2090年b1的同位素位移Å作为宇宙核合成的探测
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.thd4
S. Johansson, U. Litzén, Jörg Kasten, M. Kock
Determination of the cosmic abundance of the light elements Li, Be and B is critical for the understanding of how these elements have been formed in the Universe. The Standard Model for the Big Bang nucleosynthesis, which assumes a uniform density, and its complementary model, the Non-uniform Density Model (see e.g. Kajino and Boyd, 1990), differ considerably in their predictions of Be- and B-production . However, recent determinations of the abundance of Be (Gilmore et al. 1991) and B (Duncan et al. 1992) in metal-poor stars are orders of magnitude larger than those predicted from any Big Bang nucleosynthesis model. The isotopes 9Be, 10B and 11B are therefore thought to have been produced by cosmic spallation, primarily when high-energy protons and α-particles collide with CNO nuclei in the interstellar medium.
确定Li、Be和B等轻元素的宇宙丰度对于理解这些元素是如何在宇宙中形成的至关重要。假设密度均匀的大爆炸核合成标准模型和它的补充模型非均匀密度模型(见Kajino和Boyd, 1990)在对Be-和b -产生的预测上有很大的不同。然而,最近对金属贫乏恒星中Be (Gilmore etal . 1991)和B (Duncan etal . 1992)丰度的测定比任何大爆炸核合成模型所预测的要大几个数量级。因此,同位素9Be、10B和11B被认为是由宇宙散裂产生的,主要是当高能质子和α-粒子在星际介质中与CNO核碰撞时产生的。
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引用次数: 0
FTS Observation of CO Fundamental Bands in Cool Stellar Atmospheres 低温恒星大气中CO基波段的FTS观测
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1989.mb4
G. Wiedemann, T. Ayres, D. Jennings
The infrared ro-vibration spectrum of carbon monoxide provides a powerful observational diagnostic for the investigation of late-type stellar atmospheres. At temperatures of several thousands of degrees, CO vibrational states up to v=7 and rotational states up to j≈100 are populated. The corresponding lines are formed over, and therefore probe, a large range in altitude. The strongest fundamental lines (Δv=1) originate in the upper photosphere and in the chromosphere, regions which are only inadequately described by present stellar atmosphere theories. Numerical simulations have shown that CO affects the stellar atmospheric structure through cooling in optically thin lines (e.g. Johnson, 1973). CO observations are important, because the model predictions can be tested reliably only from observations of species that are intimately involved. This is particularly true in view of the dilemma posed by the contradicting results of 'conventional' chromospheric diagnostics and first CO Δv=1 observations on the Sun (Ayres and Testerman, 1981) and Arcturus (Heasley et al., 1978). The present study has been conducted to establish CO fundamental bands as an observational diagnostic for the higher layers of cool stellar atmospheres.
一氧化碳的红外无振动谱为研究晚期恒星大气提供了有力的观测诊断。在几千度的温度下,CO的振动态高达v=7,旋转态高达j≈100。相应的线是在一个很大的高度范围内形成的,因此可以探测到。最强的基本线(Δv=1)起源于上层光球层和色球层,这是目前恒星大气理论所不能充分描述的区域。数值模拟表明,CO通过光学细线的冷却作用影响恒星大气结构(例如Johnson, 1973)。CO观测很重要,因为只有通过对密切相关的物种的观测才能可靠地检验模式预测。考虑到“传统”色球诊断和对太阳(Ayres and Testerman, 1981)和大角星(Heasley et al., 1978) CO Δv=1观测的矛盾结果所造成的困境,这一点尤其正确。本研究的目的是建立CO基本波段,作为低温恒星大气高层的观测诊断。
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引用次数: 0
Band Centers and Line Positions of Hot Bands of 13C16O2 and 16O13C18O in the 15 Micron Region 13C16O2和16O13C18O在15微米区域热带的带中心和线位置
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.fd6
M. Esplin, M. Hoke
A high-resolution interferometer and high-temperature absorption cell have been used in a continuing measurement program of rotation-vibration spectra of the isotopes of carbon dioxide in different spectral regions. This paper covers results for the isotopes 13C16O2 and 16O13C18O with band centers in the spectral region 600 to 800 cm-1. Only a few experimental details will be given here; additional details may be found in the literature.1 The experimental components include an infrared source, a radiation chopper, a high-temperature single-pass gas-sample absorption cell, a Michelson interferometer with "cat’s eye" mirrors employing a step-and-integrate mirror motion, and two liquid-helium-cooled detectors. A carbon dioxide gas sample was contained in the 1.75 meter single-pass stainless-steel sample cell. The central one meter section of the cell was maintained at a temperature of 800K, with temperature gradients in the end segments of the cell, ending with the cell windows at room temperature. For this study a stepping mirror displacement of 75 cm was used, giving a resolution (FWHM) of 0.006 cm-1 with triangular apodization.
采用高分辨率干涉仪和高温吸收池对不同光谱区二氧化碳同位素的旋转振动谱进行了连续测量。本文介绍了13C16O2和16O13C18O两种同位素在600 ~ 800 cm-1波段中心的结果。这里只给出一些实验细节;更多的细节可以在文献中找到实验组件包括一个红外源,一个辐射斩波器,一个高温单通道气体样品吸收电池,一个带有“猫眼”镜面的迈克尔逊干涉仪,采用步进集成镜运动,以及两个液氦冷却探测器。在1.75米的单道不锈钢样品池中含有二氧化碳气体样品。细胞中央1米截面保持800K温度,细胞端段温度梯度,以室温下的细胞窗结束。本研究采用位移为75 cm的步进镜,分辨率(FWHM)为0.006 cm-1,三角形apoed。
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引用次数: 0
High Resolution Infrared Fourier Transform Emission Spectroscopy and Rotational Spectroscopy of Metal Hydrides: 2Σ+ State of CaH 金属氢化物的高分辨率红外傅立叶变换发射光谱和旋转光谱:2Σ+ CaH的状态
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.thd6
C. Frum, J. Oh, E. Cohen, H. Pickett
Calcium hydride is an important astrophysical molecule which has been detected in the Sun [1,2] and other stars [3]. It is also believed that this free radical is an important constituent of the interstellar medium [4]. However, a search for the CaH in interstellar medium is hindered by the unavailability of accurate frequencies for the low-N rotational transitions.
氢化钙是一种重要的天体物理分子,已在太阳[1,2]和其他恒星[3]中被探测到。也有人认为这种自由基是星际介质的重要组成部分[4]。然而,由于无法获得低n旋转跃迁的精确频率,阻碍了对星际介质中CaH的搜索。
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引用次数: 0
Fourier Transform Spectra of the A2Σ+ (v=0) -X2∏ (v=o) Band of OH OH的A2Σ+ (v=0) -X2∏(v=o)波段的傅里叶变换光谱
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.thd2
G. Stark, J. Brault, M. Abrams
The hydroxyl radical plays an important role in a variety of atmospheric, astrophysical, and chemical processes. Both absorption in, and fluorescence from, the strong (0-0) band of the A2Σ+ - X2∏ system are widely used in concentration measurements of OH (e.g., Stimpfle et al. 1990; Desgroux and Cottereau 1991).
羟基自由基在各种大气、天体物理和化学过程中起着重要作用。A2Σ+ - X2∏系统强(0-0)波段的吸收和荧光均广泛用于OH浓度测量(例如,stimple等人,1990;Desgroux and Cottereau 1991)。
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引用次数: 1
Fourier-Transform Spectroscopy of Ozone Broadening 臭氧展宽的傅立叶变换光谱
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1989.wa7
M. A. Smith, C. Rinsland, V. Devi
Until recently, very few measurements of broadening of O3 absorption lines have been made (see Table IV of Ref. 1), covering only about 230 different vibration-rotation lines. However, investigators desiring to accurately model infrared radiative transfer in the terrestrial atmosphere require spectroscopic parameters (including air-broadened halfwidths) for thousands of vibration-rotation lines (2). Self-broadened halfwidths are needed for accurate quantitative analysis of laboratory spectra of gas mixtures containing high concentrations of ozone. In the studies reported here, the broad spectral coverage possible with Fourier transform spectroscopy has enabled us to measure air- and nitrogen-broadened halfwidths and shifts for about 70 ozone lines in the 9 μm region, and self-broadened halfwidths for over 160 ozone lines in the 4-14 μm region. The results are compared with previous measurements and calculations.
直到最近,很少对O3吸收谱线的加宽进行测量(见参考文献1的表4),只覆盖了大约230种不同的振动-旋转谱线。然而,希望准确模拟地球大气中红外辐射传输的研究人员需要数千条振动-旋转线的光谱参数(包括空气加宽半宽度)(2)。对于含有高浓度臭氧的气体混合物的实验室光谱,需要自加宽半宽度进行精确的定量分析。在本文报道的研究中,傅里叶变换光谱的广谱覆盖范围使我们能够测量9 μm区域约70条臭氧线的空气和氮加宽半宽度和位移,以及4-14 μm区域160多条臭氧线的自加宽半宽度。结果与以往的测量和计算结果进行了比较。
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引用次数: 0
Far-Infrared Fourier-Transform Spectroscopy of the Stratosphere 平流层的远红外傅立叶变换光谱
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.fc2
W. Traub
Fourier-transform spectroscopy of the thermal emission spectrum of the Earth’s stratosphere is a technique of growing importance in the study of ozone-layer chemistry. The far-infrared part of this thermal spectrum, here roughly 7-700 cm-1, includes detectable transitions of many species which are key indicators of the degree to which catalytic reactions of chlorine and bromine compounds are able to destroy ozone. A unique advantage of measuring thermal emission is that the instrument can examine the stratosphere at night as easily as it does the day. It is this combination of circumstances, namely the ability to measure species such as OH and HO2, and the ability to measure throughout the day-night cycle, which has made the far-infrared Fourier-transform spectrometer (FTS) a valuable asset in the study of the stratospheric ozone layer.
地球平流层热发射光谱的傅里叶变换光谱是臭氧层化学研究中日益重要的一项技术。热光谱的远红外部分,这里大约是7-700厘米-1,包括许多物种的可探测的转变,这是氯和溴化合物催化反应能够破坏臭氧的程度的关键指标。测量热发射的一个独特的优点是,该仪器可以在夜间像白天一样容易地检查平流层。正是这种情况的结合,即测量OH和HO2等物质的能力,以及测量整个昼夜周期的能力,使远红外傅立叶变换光谱仪(FTS)成为研究平流层臭氧层的宝贵资产。
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引用次数: 0
Stratospheric Fourier Transform Spectroscopy 平流层傅立叶变换光谱学
Pub Date : 1900-01-01 DOI: 10.1364/hrfts.1992.fd3
M. Coffey, W. Mankin
For more than 15 years our project in the Atmospheric Chemistry Division of NCAR has flown a Fourier transform spectrometer aboard aircraft to record the infrared absorption spectrum of the stratosphere. These spectra, now totaling more than 45,000, have been used to derive the concentrations of a number of stratospheric gases and to define their latitudinal, seasonal and diurnal variations.
15年来,我们在NCAR大气化学部门的项目一直在飞机上使用傅里叶变换光谱仪来记录平流层的红外吸收光谱。这些光谱,现在总共超过45000个,已经被用来得出一些平流层气体的浓度,并确定它们的纬度、季节和日变化。
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引用次数: 0
期刊
High Resolution Fourier Transform Spectroscopy
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