论文标题
嵌入在彗星粉尘颗粒中的丰富氢硫化铵
Abundant ammonium hydrosulphide embedded in cometary dust grains
论文作者
论文摘要
氢硫化铵早已被认为至少存在于巨型行星的某些层。它的辐射产品可能是木星上看到的红色的原因。以前在67p/churyumov-gerasimenko彗星上检测到了几种铵盐,即NH3和酸的产物。酸H2S是67p昏迷的第五大分子,其次是NH3。为了寻找盐NH4+SH-,我们分析了Rosetta任务期间的Rosetta/Rosina双聚焦质谱仪的原位测量。直接从核直接升华时,NH3和H2S似乎是彼此独立的。但是,我们观察到在灰尘撞击过程中这两个物种之间存在很强的相关性,清楚地表明了盐。我们发现NH4+SH-是迄今为止最丰富的盐,在灰尘冲击中比水更丰富。我们还发现所有先前检测到的铵盐和氟化铵。氨和酸的量相互平衡,证实氨主要以嵌入粉尘粒的盐形式。同素体S2和S3在撞击中得到了强大的增强,而H2S2及其片段HS2未检测到,这很可能是NH4+SH-辐射的结果。这使得盐的原始起源可能。我们的发现可能解释了彗星中氮的明显耗尽,也许可以帮助解决恒星形成区域中缺失的硫的谜语。
Ammonium hydrosulphide has long since been postulated to exist at least in certain layers of the giant planets. Its radiation products may be the reason for the red colour seen on Jupiter. Several ammonium salts, the products of NH3 and an acid, have previously been detected at comet 67P/Churyumov-Gerasimenko. The acid H2S is the fifth most abundant molecule in the coma of 67P followed by NH3. In order to look for the salt NH4+SH-, we analysed in situ measurements from the Rosetta/ROSINA Double Focusing Mass Spectrometer during the Rosetta mission. NH3 and H2S appear to be independent of each other when sublimating directly from the nucleus. However, we observe a strong correlation between the two species during dust impacts, clearly pointing to the salt. We find that NH4+SH- is by far the most abundant salt, more abundant in the dust impacts than even water. We also find all previously detected ammonium salts and for the first time ammonium fluoride. The amount of ammonia and acids balance each other, confirming that ammonia is mostly in the form of salt embedded into dust grains. Allotropes S2 and S3 are strongly enhanced in the impacts, while H2S2 and its fragment HS2 are not detected, which is most probably the result of radiolysis of NH4+SH-. This makes a prestellar origin of the salt likely. Our findings may explain the apparent depletion of nitrogen in comets and maybe help to solve the riddle of the missing sulphur in star forming regions.