@article {2168,
	title = {The complexes: RhCl(P-N)(THP), where P-N is P,N-chelated o-diphenylphosphino-N,N-dimethylaniline and THP is tris(hydroxymethyl)phosphine, and RhCl[(O)P-N][THP(O)] containing O-bonded phosphine oxides},
	journal = {Inorganica Chimica Acta},
	volume = {361},
	number = {11},
	year = {2008},
	note = {ISI Document Delivery No.: 323VATimes Cited: 3Cited Reference Count: 42Lorenzini, Fabio Patrick, Brian O. James, Brian R.},
	month = {Jul},
	pages = {3199-3204},
	type = {Article},
	abstract = {{The complex RhCl(P-N)(THP) (1) is synthesized under argon from RhCl(cod)(THP) and P-N, and is structurally characterized; P-N = P, N-chelated o-diphenylphosphino-N,N-dimethylaniline},
	keywords = {BEARING O-N, BIDENTATE PHOSPHINES, CATALYTIC-OXIDATION, HYDROFORMYLATION, LIGANDS, LOW-TEMPERATURE, N-DIMETHYLANILINYL SUBSTITUENTS, OXIDATION, PALLADIUM(II) COMPLEXES, phosphanes, phosphine oxides, phosphines, REACTIVITY, RHODIUM COMPLEXES, RHODIUM(I) COMPLEXES, X-ray structure},
	isbn = {0020-1693},
	url = {<Go to ISI>://000257475300029},
	author = {Lorenzini, F. and Patrick, B. O. and James, Brian R.}
}
@article {1558,
	title = {Measurements of the vapor pressure of cubic ice and their implications for atmospheric ice clouds},
	journal = {Geophysical Research Letters},
	volume = {33},
	number = {17},
	year = {2006},
	note = {ISI Document Delivery No.: 081QHTimes Cited: 17Cited Reference Count: 38Shilling, J. E. Tolbert, M. A. Toon, O. B. Jensen, E. J. Murray, B. J. Bertram, A. K.},
	month = {Sep},
	pages = {5},
	type = {Article},
	abstract = {Under conditions commonly found in Earth{\textquoteright}s atmosphere, water can form two solid phases; hexagonal ice (I-h) and cubic ice (I-c). Recent reports have suggested that Ic may form in the atmosphere under a wider range of conditions than previously believed. In light of these reports, the formation of Ic has been suggested as one contributing factor for in-situ observations of persistent in-cloud supersaturations in cold cirrus. However, an accurate evaluation of the contribution of Ic formation to the observed supersaturations requires knowledge of the saturation vapor pressure of Ic, which has not been measured. In this manuscript, we report direct measurements of the vapor pressure of Ic over the temperature range 180 - 190 K. Over this temperature range, the vapor pressure of the cubic phase is 10.5 +/- 2.5\% higher than that of the hexagonal phase. Field measurements of in-cloud supersaturations made during CRYSTAL-FACE are also re-analyzed and discussed.},
	keywords = {AMORPHOUS WATER ICE, ASTROPHYSICAL IMPLICATIONS, CIRRUS CLOUDS, ELECTRON DIFFRACTION, FORMS, GLASSY, HEXAGONAL ICE, LOW-TEMPERATURE, SPECTRA, WATER, X-RAY-DIFFRACTION},
	isbn = {0094-8276},
	url = {<Go to ISI>://000240331600005},
	author = {Shilling, J. E. and Tolbert, M. A. and Toon, O. B. and Jensen, E. J. and Murray, B. J. and Bertram, A. K.}
}
@article {4471,
	title = {Rotational spectra and hyperfine constants of ZrO and ZrS},
	journal = {Journal of Chemical Physics},
	volume = {110},
	number = {22},
	year = {1999},
	note = {ISI Document Delivery No.: 199FFTimes Cited: 32Cited Reference Count: 49},
	month = {Jun},
	pages = {10715-10724},
	type = {Article},
	abstract = {The pure rotational spectra of ZrO and ZrS have been recorded using cavity Fourier transform microwave spectroscopy in the frequency range 9-26 GHz. The molecules were generated by laser ablation of a solid Zr rod in the presence of 0.05\% of O-2 or H2S, respectively, in either argon or neon. Rotational spectra of five previously unobserved isotopomers of ZrO in the X(1)Sigma(+) state have been measured. Spectra for all five (ZrS)-S-32 isotopomers and for the (ZrS)-Zr-90-S-34 isotopomer in natural abundance have also been measured; this is the first report of pure rotational transitions for ZrS. Transitions in several excited vibrational states were also measured for the most abundant isotopomers of both species. Atomic mass-dependent Born-Oppenheimer breakdown correction terms were determined by fitting the data obtained for each molecule to a Dunham-like expression. Values for the equilibrium bond lengths of the two species were also calculated from the results of these fits. For both the (ZrS)-Zr-91-S-32 and (ZrO)-Zr-91-O-16 isotopomers, nuclear hyperfine structure due to the zirconium nucleus was observed and values for eQ(q0) (Zr-91) and C-I (Zr-91) have been determined. A rotational transition in the low lying a (3)Delta state of ZrS has also been observed. (C) 1999 American Institute of Physics. [S0021-9606(99)00121-X].},
	keywords = {BORN-OPPENHEIMER APPROXIMATION, COEFFICIENTS, DEPENDENCE, DIATOMIC-MOLECULES, DIPOLE-MOMENTS, DUNHAM, FOURIER-TRANSFORM SPECTROSCOPY, ISOTOPE, LOW-TEMPERATURE, METAL-OXIDES, REFRACTORY MOLECULES, ZIRCONIUM OXIDE},
	isbn = {0021-9606},
	url = {<Go to ISI>://000080469200010},
	author = {Beaton, S. A. and Gerry, M. C. L.}
}
