Abundances of trace constituents in Jupiter's atmosphere inferred from Herschel/PACS observations

C. Gapp, M. Rengel, P. Hartogh, H. Sagawa, H. Feuchtgruber, E. Lellouch, G. Villanueva
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Abstract

On October 31, 2009, the Photodetector Array Camera and Spectrometer (PACS) on board the Herschel Space Observatory observed far-infrared spectra of Jupiter in the wavelength range between 50 and 220$\ as part of the program "Water and Related Chemistry in the Solar System". The spectra have an effective spectral resolution between 900 and 3500, depending on the wavelength and grating order. We investigate the disk-averaged chemical composition of Jupiter's atmosphere as a function of height using these observations. We used the Planetary Spectrum Generator (PSG) and the least-squares fitting technique to infer the abundances of trace constituents. The PACS data include numerous spectral lines attributable to ammonia (NH$_3$), methane (CH$_4$), phosphine (PH$_3$), water (H$_2$O), and deuterated hydrogen (HD) in the Jovian atmosphere and probe the chemical composition from $p 275$\,mbar to $p 900$\,mbar. From the observations, we infer an ammonia abundance profile that decreases from a mole fraction of $(1.7 $ at $p 900$\,mbar to $(1.7 $ at $p 275$\,mbar, following a fractional scale height of about $0.114$. For phosphine, we find a mole fraction of $(7.2 $ at pressures higher than $(550 100)$\,mbar and a decrease of its abundance at lower pressures following a fractional scale height of $(0.09 0.02)$. Our analysis delivers a methane mole fraction of $(1.49 $. Analyzing the HD $R(0)$ line at $112.1\ yields a new measurement of Jupiter's D/H ratio, $ D/H $. Finally, the PACS data allow us to put the most stringent $3 upper limits yet on the mole fractions of hydrogen halides in the Jovian troposphere. These new upper limits are $<1.1 $ for hydrogen fluoride (HF), $<6.0 $ for hydrogen chloride (HCl), $<2.3 $ for hydrogen bromide (HBr) and $<1.2 $ for hydrogen iodide (HI) and support the proposed condensation of hydrogen halides into ammonium halide salts in the Jovian troposphere.
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通过赫歇尔/PACS观测推断木星大气中痕量成分的丰度
2009年10月31日,作为 "太阳系中的水和相关化学 "计划的一部分,赫歇尔空间天文台上的光电探测器阵列照相机和分光计(PACS)观测到了木星波长范围在50到220美元之间的远红外光谱。根据波长和光栅阶数的不同,这些光谱的有效光谱分辨率在 900 到 3500 之间。我们利用这些观测数据研究了木星大气的盘平均化学成分与高度的函数关系。我们使用行星光谱发生器(PSG)和最小二乘拟合技术来推断痕量成分的丰度。PACS数据包含了大量可归因于木卫二大气中氨(NH$_3$)、甲烷(CH$_4$)、膦(PH$_3$)、水(H$_2$O)和氘化氢(HD)的光谱线,并探测了从p 275$\,mbar到p 900$\,mbar的化学成分。根据观测结果,我们推断出氨的丰度曲线,其摩尔分数从p 900$\,mbar时的$(1.7)下降到p 275$\,mbar时的$(1.7),分数尺度高度约为0.114$。对于磷化氢,我们发现在压力高于(550 100)美元/毫巴时,其摩尔分数为(7.2)美元,而在压力较低时,其丰度会随着(0.09 0.02)美元的分数尺度高度而下降。我们的分析得出甲烷的摩尔分数为$(1.49 $。分析112.1美元处的HD $R(0)$线可以得到木星的D/H比值$D/H $。最后,PACS数据使我们能够对木星对流层中卤化氢的摩尔分数提出最严格的3美元上限。这些新的上限分别为:氟化氢(HF)小于1.1美元,氯化氢(HCl)小于6.0美元,溴化氢(HBr)小于2.3美元,碘化氢(HI)小于1.2美元。
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