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首页> 外文期刊>The Journal of Chemical Physics >Integrated absorption intensity and Einstein coefficients for the O_2 a~1#DELTA#_g-X~3#SIGMA#_g~- (0,0) transition: A comparison of cavity ringdown and high resolution Fourier transform spectroscopy with a long-path absorption cell
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Integrated absorption intensity and Einstein coefficients for the O_2 a~1#DELTA#_g-X~3#SIGMA#_g~- (0,0) transition: A comparison of cavity ringdown and high resolution Fourier transform spectroscopy with a long-path absorption cell

机译:O_2 a〜1#DELTA#_g-X〜3#SIGMA#_g〜-(0,0)跃迁的积分吸收强度和爱因斯坦系数:腔衰荡和高分辨率傅里叶变换光谱与长距离吸收的比较细胞

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摘要

The two experimental techniques of cavity ringdown spectroscopy and high-resolution, long-path Fourier transform spectroscopy have been used to measure quantitative absorption spectra and determine the integrated absorption intensity (S _(int, B)) for the O_2 a ~1#DELTA#_g - X ~3#SIGMA#_g~- (0, 0) band. Einstein A-factors and radiative lifetimes for the O_2 a ~1#DELTA#_g #upsilon# = 0 state have been derived from the S_(int,B) values. The two methods give values for the integrated absorption intensity that agree to within 2%. The value recommended from the results of this study is S_(int, B) = 3.10 +- 0.10 * 10~(-24) cm molecule~(-1), corresponding to an Einstein-A coefficient of A = 2.19 +- 0.07 * 10~(-4) s ~(-1) and a radiative lifetime of #tau#_(rad) = 76 min. The measurements are in excellent agreement with the recent absorption study of Lafferty et al. [Appl. Opt. 37, 2264 (1998)] and greatly reduce the uncertainty in these parameters, for which accurate values are required for determination of upper stratospheric and mesospheric ozone concentrations.
机译:腔衰荡光谱法和高分辨率长距离傅里叶变换光谱法的两种实验技术已用于测量定量吸收光谱并确定O_2 a〜1#DELTA的积分吸收强度(S _(int,B)) #_g-X〜3#SIGMA#_g〜-(0,0)波段。从S_(int,B)值推导了O_2 a〜1#DELTA#_g#upsilon#= 0状态的爱因斯坦A因子和辐射寿命。两种方法给出的积分吸收强度值均在2%以内。该研究结果推荐的值为S_(int,B)= 3.10 +-0.10 * 10〜(-24)cm分子〜(-1),对应于爱因斯坦-A系数A = 2.19 +-0.07 * 10〜(-4)s〜(-1),#tau #_(rad)的辐射寿命= 76分钟。这些测量与Lafferty等人的最新吸收研究非常吻合。 [应用选择。 37,2264(1998)]并大大减少了这些参数的不确定性,为此需要确定准确的数值来确定平流层和中层上方的臭氧浓度。

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