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Water vapor millimeter wave foreign continuum: A Lanczos calculation in the coordinate representation

机译:水蒸气毫米波外来连续体:坐标表示中的Lanczos计算

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The water vapor foreign-continuum absorption has been calculated theoretically from first principles for the millimeter wave spectral region as a function of frequency f and temperature T. The calculatons are made using the Lanczos algorithm by writing the resolvent operator (omega-L)~(-1) as continued fractions. In order to guarantee the quick convergence of the continued fractions the line space of H_2O is divided into two subspaces: one consists of the positige resonance lines and the other the negative ones. By ignoring the coupling between them, (omega-L)~(-1) is expressed as a sum of two continued fractions. The parameters appearing in each of the fractions re functions of the matrix elements of powers of the Liouville operator L between the starting vectors spanning the corresponding subspaces. In the present work, we have taken into account all powers of L up to 5. Whith the coordinate representation in which the orientatons of the H_2O-N_2 collision pair are chosen as the basis functions in Hilbert space, the anisotropic interaction potential is diagonal, and calculations of the matrix elements are transformed to multidimensional integrations, we assume that the anisotropic potential has rotational symmetry about the Z axis of H_2O, and consists of the long-raonge dipole-quadrupole part and a short-range repulsive site-site model. Once the parameters of the continued fractions are known, one can calculate the poles and residues and then carry out the ensemble average voer the translational motion. Within the quasistatic approximation, one can treat the latter classically and obtain contributions to the absorption coefficient at the poles. Finally, the absorption coefficient at frequency f can be derived by an interpolation method. The results are fitted to a simple function of f and T, and are compared with experimental data dn with two different versions of Liebe's empirical model. In general, the theoretical results are in good agreement with the experiment. Meanwhile, the magnitudes of the theoretical absorption are between those of the 1989 and 1993 versions, but the temperature dependence is closer to the latter one.
机译:理论上是根据毫米波光谱区域的第一原理计算出水蒸气异连续谱吸收率的,该吸收率是频率f和温度T的函数。使用Lanczos算法,通过编写可分辨算子(omega-L)〜( -1)作为连续分数。为了保证连续分数的快速收敛,H_2O的线空间分为两个子空间:一个由正共振线组成,另一个由负共振线组成。通过忽略它们之间的耦合,(ω-L)〜(-1)表示为两个连续分数的总和。出现在每个分数中的参数是跨越相应子空间的起始向量之间的Liouville算子L的幂的矩阵元素的函数。在目前的工作中,我们考虑了L的所有幂次,直到5。在Hilbert空间中,选择H_2O-N_2碰撞对的方向作为基函数的坐标表示,各向异性的相互作用势是对角的,并将矩阵元素的计算转换为多维积分,我们假设各向异性势围绕H_2O的Z轴具有旋转对称性,并且由长距离偶极四极子部分和短程排斥位点-位点模型组成。一旦知道连续分数的参数,就可以计算极点和残差,然后执行平移运动的整体平均。在准静态近似中,可以经典地处理后者并获得极点处的吸收系数的贡献。最后,可以通过插值方法得出频率为f的吸收系数。将结果拟合为f和T的简单函数,并与使用两种不同版本的Liebe经验模型的实验数据dn进行比较。通常,理论结果与实验吻合良好。同时,理论吸收的幅度在1989年和1993年之间,但温度依赖性更接近于后者。

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