Optical constant of ammonium hydrosulfide ice and ammonia ice
Journal of the Optical Society of America B: Optical Physics 24:1 (2007) 126-136
Abstract:
Thin-film transmission spectra of ammonium hydrosulfide (NH4SH) ice and ammonia (NH3) ice between 1300 and 12,000 cm-1 were used to determine the ice's optical constants. The films were grown on a sapphire substrate, and a Fourier-transform spectrometer and a grating spectrometer were used together to record the spectra. Lambert's law was used to directly determine the imaginary component of the complex refractive indices; from this, the real component was derived using the Kramers-Kronig algorithm. It is shown that, contrary to what is expected, the optical constants determined for NH3 ice at 80 K are in good agreement with those in the cubic phase, rather than the metastable one. The phase of the NH4SH ice was observed to change from amorphous to polycrystalline as the film was annealed to 160 K. © 2006 Optical Society of America.Optical constants of ammonium hydrosulfide ice and ammonia ice
Journal of the Optical Society of America B Optica Publishing Group 24:1 (2007) 126
Two T dwarfs from the UKIDSS early data release
Astronomy and Astrophysics 466:3 (2007) 1059-1064
Abstract:
Contexf. We report on the first ultracool dwarf discoveries from the UKIRT Infrared Deep Sky Survey (UKIDSS) Large Area Survey Early Data Release (LAS EDR), in particular the discovery of T dwarfs which are fainter and more distant than those found using the 2MASS and SDSS surveys. Aims. We aim to show that our methodologies for searching the ∼27 deg2 of the LAS EDR are successful for finding both L and T dwarfs via cross-correlation with the Sloan Digital Sky Survey (SDSS) DR4 release. While the area searched so far is small, the numbers of objects found shows great promise for near-future releases of the LAS and great potential for finding large numbers of such dwarfs. Methods. Ultracool dwarfs are selected by combinations of their YJH(K) UKIDSS colours and SDSS DR4 z - J and i - z colours, or, lower limits on these red optical/infrared colours in the case of DR4 dropouts. After passing visual inspection tests, candidates have been followed up by methane imaging and spectroscopy at 4 m and 8 m-class facilities. Results. Our main result is the discovery following CHMars Climate Sounder: An investigation of thermal and water vapor structure, dust and condensate distributions in the atmosphere, and energy balance of the polar regions
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 112:E5 (2007) ARTN E05S06
Simulating physical weathering of basalt on Earth and Mars
GEOCHIMICA ET COSMOCHIMICA ACTA 71:15 (2007) A1068-A1068