首页> 外文期刊>Journal of Quantitative Spectroscopy & Radiative Transfer >Quantum-mechanical vs. semi-classical spectral-line widths and shifts from the line core in the non-impact region for the Ar-perturbed/K-radiator system
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Quantum-mechanical vs. semi-classical spectral-line widths and shifts from the line core in the non-impact region for the Ar-perturbed/K-radiator system

机译:量子力学与半经典光谱线的宽度和相对于Ar扰动/ K辐射器系统非影响区域中线芯的偏移

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New quantum-mechanical (QM) and semi-classical (SC) shifts (d's) and widths (HWHM's, w's) were measured from the line core of computed full spectral-line shapes for the Ar-perturbed/K-radiator system (K/Ar). The initial state of our model was based on a 4p(2) P-3/2,P-1/2 pseudo-potential for the K/Ar system, and the final state on a zero potential. The Fourier transform of the line shape formed the basis for the computations. Excellent agreement was found between the QM and SC values of d and of w in a high-pressure (P) non-impact region, which was characterized by a root P dependence of w and a P dependence of d. These agreements were shown to be another example of a c orrespondence between classical (SC) quantities and QM quantities in the limit of large quantum numbers. Typically at P = 1 x 10(6) Torr and T = 400 K, w(QM) = 448 cm(-1) and w(SC) = 479 cm(-1) where the deviation from the mean is +/-3.3 %. Also, d(QM) = -3815 cm(-1) and d(SC) = -3716 cm(-1), where the deviation from the mean is +/-1.3%. A new general method was formulated which yielded a definite pressure P-0, which was defined as an upper limit to the low-pressure impact approximation and a lower limit to the non-impact region. (C) 2007 Elsevier Ltd. All rights reserved.
机译:新的量子力学(QM)和半经典(SC)位移(d's)和宽度(HWHM's,w's)是根据Ar扰动/ K辐射器系统(K / Ar)。我们模型的初始状态基于K / Ar系统的4p(2)P-3 / 2,P-1 / 2伪电势,而最终状态基于零电势。线形的傅立叶变换构成了计算的基础。在高压(P)非撞击区域中,d和w的QM和SC值之间发现了极好的一致性,其特征在于w的根P依赖性和d的P依赖性。这些协议被证明是经典(SC)数量和QM数量在大量子数范围内的对应关系的另一个示例。通常在P = 1 x 10(6)Torr和T = 400 K的情况下,w(QM)= 448 cm(-1)和w(SC)= 479 cm(-1),其中与均值的偏差为+/- 3.3%。同样,d(QM)= -3815 cm(-1)和d(SC)= -3716 cm(-1),与平均值的偏差为+/- 1.3%。制定了一种新的通用方法,该方法产生确定的压力P-0,该压力被定义为低压冲击近似值的上限和非冲击区域的下限。 (C)2007 Elsevier Ltd.保留所有权利。

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