Agrawal Rachana, Seager Sara, Iakubivskyi Iaroslav, Buchanan Weston P, Glidden Ana, Seager Maxwell D, Bains William, Huang Jingcheng, Petkowski Janusz J
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139.
Department of Physics, Massachusetts Institute of Technology, Cambridge, MA 02139.
Proc Natl Acad Sci U S A. 2025 Aug 19;122(33):e2425520122. doi: 10.1073/pnas.2425520122. Epub 2025 Aug 11.
The discovery of thousands of exoplanets and the emergence of telescopes capable of exoplanet atmospheric characterization have intensified the search for habitable worlds. Due to selection biases, many exoplanets under study are planets deemed inhospitable because their surfaces are too warm to support liquid water. We propose that such planets could still support life through ionic liquids: Liquid salts with negligible vapor pressure that can persist on warm planets with thin atmospheres, where liquid water cannot. Ionic liquids have not previously been considered as naturally occurring substances, and thus have not been discussed in planetary science. We demonstrate in laboratory experiments that ionic liquids can form from planetary materials: Sulfuric acid combined with nitrogen-containing organic molecules. Sulfuric acid can be volcanic in origin, and organic compounds are commonly found on planetary bodies. The required planetary surface is water-depleted and must support sulfuric acid transiently in liquid phase to dissolve organics, followed by evaporation of excess liquid-conditions spanning approximately 300 K at 10 atm to 350-470 K at 0.01 atm. Because ionic liquids have extremely low vapor pressures, they are not prone to evaporation, allowing small droplets or pools to persist without ocean-like reservoirs. Ionic liquids' minuscule vapor pressure at room temperature suggests possible stability on planets with negligible atmospheres, shielded by magnetic fields or rock crevices against harsh cosmic radiation. Ionic liquids can stably dissolve enzymes and other biomolecules, enabling biocatalysis and offering a plausible solvent for life-broadening the definition of habitable worlds.
数千颗系外行星的发现以及能够对系外行星大气进行特征描述的望远镜的出现,加剧了对宜居世界的探索。由于选择偏差,许多正在研究的系外行星被认为不适宜居住,因为它们的表面温度过高,无法支持液态水存在。我们提出,这类行星仍可能通过离子液体来支持生命:离子液体是蒸气压可忽略不计的液态盐,在大气稀薄的温暖行星上能够留存,而液态水在这样的行星上则无法存在。离子液体此前未被视为天然存在的物质,因此在行星科学中也未被讨论过。我们在实验室实验中证明,离子液体可以由行星物质形成:硫酸与含氮有机分子结合。硫酸可能源自火山活动,而有机化合物在行星体上普遍存在。所需的行星表面缺水,并且必须暂时支持硫酸处于液相以溶解有机物,随后多余的液体蒸发——条件范围大致为10个大气压下约300K至0.01个大气压下350 - 470K。由于离子液体的蒸气压极低,它们不易蒸发,使得小液滴或小水池能够留存,而无需类似海洋的储水体。离子液体在室温下极小的蒸气压表明,在大气可忽略不计的行星上,它们可能具有稳定性,受到磁场或岩石裂缝的保护,免受 harsh cosmic radiation的影响。离子液体能够稳定地溶解酶和其他生物分子,实现生物催化,并为生命提供一种合理的溶剂——拓宽了宜居世界的定义。 (注:“harsh cosmic radiation”未找到准确对应中文术语,暂保留英文)