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HST SPECTROSCOPIC OBSERVATIONS OF JUPITER AFTER THE COLLISION OF COMET SHOEMAKER-LEVY 9

机译:彗星鞋匠级9碰撞后木星的HST光谱观察

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Ultraviolet spectra obtained with the Hubble Space Telescope identified at least 10 molecules and atoms in the perturbed stratosphere near the G impact site, most never before observed in Jupiter. The large mass of sulfur-containing material, more than 10(14) grams in S-2 alone, indicates that many of the sulfur-containing molecules S-2, CS2, CS, H2S, and S+ may be derived from a sulfur-bearing parent molecule native to Jupiter. If so, the fragment must have penetrated at least as deep as the predicted NH4SH cloud at a pressure of approximately 1 to 2 bars, Stratospheric NH3 was also observed, which is consistent with fragment penetration below the cloud tops. Approximately 10(7) grams of neutral and ionized metals were observed in emission, including Mg II, Mg I, Si I, Fe I, and Fe II. Oxygen-containing molecules were conspicuous by their absence; upper limits for SO2, SO, CO, SiO, and H2O are derived, [References: 36]
机译:用哈勃太空望远镜获得的紫外光谱识别出在G撞击点附近的平流层中至少有10个分子和原子,这在木星中从未见过。大量的含硫物质,仅在S-2中就超过10(14)克,这表明许多含硫分子S-2,CS2,CS,H2S和S +可能源自硫-木星天然的母体分子。如果是这样,那么碎片必须在大约1至2 bar的压力下至少穿透了与预测的NH4SH云一样深的深度,还观察到了平流层NH3,这与碎片在云层顶部的穿透是一致的。在发射中观察到大约10(7)克中性和离子化金属,包括Mg II,Mg I,Si I,Fe I和Fe II。含氧分子的缺乏是显而易见的。得出SO2,SO,CO,SiO和H2O的上限,[参考:36]

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