By Kate Southwood
March 18, 1925. The day starts as the other wet, spring day within the small payment of Marah, Illinois. however the city lies without delay within the direction of the worst twister in US heritage, in an effort to descend abruptly noon and go away the neighborhood in ruins. by way of dusk, 1000s can be homeless and 1000s extra will lie within the streets, useless or grievously injured. just one guy, Paul Graves, will nonetheless have every little thing he begun the day with -- his family members, his domestic, and his company, all miraculously intact.
Based at the historical Tri-State twister, "Falling to Earth" follows Paul Graves and his younger kin within the 12 months after the hurricane as they fight to appreciate their very own destiny and that in their devastated city, as they watch Marah resurrect itself from the ruins, and as they miscalculate the starting to be resentment and hostility round them with tragic effects.
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1967, 71, 856; see also refs. 49 and 526. 66 D. A. Kohl and L. S . Bartell, J. Chem. , 1969, 51, 2891, 2896. 61 (a) L. S. Theory and Accuracy 29 r , may here be the vector from an arbitrary origin to the m'th nucleus. The three last terms in equation (57) are thus nucleus-nucleus, electron-nucleus, and electron-electron contributions respectively. The elastically scattered intensity may be written where E(r) = r2 s p (r') [ s p ( r + r') dQ] dT/ (60) Dm(r), P(r), and E(r) may be obtained by MO calculations, and the theoretical intensity functions (57) or (59) may be compared with the corresponding experimental functions.
P. 2698; ( d ) S. P. Arnesen and H. M. , p. 2711; (e) L. S. Bartell and J. E . Jacob, J. Chem. , 1970, 53, 2231 ;cf) G . Gundersen and K. Hedberg, unpublished results for TeF,. I. L. K a l e and J . Karle, J. Chem. , 1950, 18, 963. (a) J. A. Hoerni, Phys. , 1956, 102, 1530; (b) A. C. Yates and A. Tenney, Phys. Rev. (A), 1972, 5, 2474. *O Various approaches have been chosen. Bonham and co-workers base the discussion on the Born series, Bartell and Wong use a partial wave expansion modified to handle systems without spherical symmetry, and Yates uses the theory developed in ref.
J. Anzer. Chem. ,1964, 86, 3493; (e) C. Tavard, D. Nicolas, and M. Rouault, J . Chim. , 1967, 64, 541; (f) D. T. Cromes and J. €3. Mann, J. Chem. , 1967, 47, 1892; (8)D. T. , 1969, 50, 4857; see also ref. 15g. l8 S. J. Cyvin, 'Molecular Vibrations and Mean Square Amplitudes', Universitetsforlaget, Oslo, and Elsevier, Amsterdam, 1968. l7 13 Theory and Accuracy where hih) = I0 1 if2r> lftl Ihlcos ( T i - 75) exp(-h215 s2) (26) Using the two first terms in (24) and the approximation the result is It has been shownlg that if a distance distribution corresponding to the ground state of the Morse oscillator is used for Pi&), the expression (27) is to a first approximation replaced by K~~ which may be called the asymmetry constant, is related to the constant a in the Morse potential and to the mean amplitude.
Falling to Earth by Kate Southwood