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“Tholin”. Jialin Li1, Xinting Yu2, Ella Sciamma-O’Brien3, Chao He4, Joshua A

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“Tholin”. Jialin Li1, Xinting Yu2, Ella Sciamma-O’Brien3, Chao He4, Joshua A 52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 2675.pdf Comparison Study of Surface Energies for Titan Haze Analogs “Tholin”. Jialin Li1, Xinting Yu2, Ella Sciamma-O’Brien3, Chao He4, Joshua A. Sebree5, Farid Salama3, Sarah M. Hörst4, Xi Zhang2, 1Department of Physics, University of California Santa Cruz, 1156 High Street, Santa Cruz, CA 95064 ([email protected]). 2Depart- ment of Earth and Planetary Sciences, University of California Santa Cruz, 1156 High Street, Santa Cruz, CA 95064. 3NASA Ames Research Center, Space Science Astrobiology Division, Astrophysics Branch, Moffett Field, CA 94035. 4Department of Earth and Planetary Sciences, Johns Hopkins University, 3400 N. Charles Street, Baltimore, MD 21218. 5Department of Chemistry and Biochemistry, University of Northern Iowa, 1227 W 27th St, Cedar Falls, IA 50614 Introduction: Titan, the largest moon of Saturn, is implications for cloud formation, aerosol-lake interac- known for its thick and hazy atmosphere with rich and tions, sand transport and dune formation on Titan’s complex organic materials. Numerous chemical reac- surface [10]. tions are initiated in Titan’s upper atmosphere, result- ing in the formation of complex organic aerosol parti- Methods: We have measured the surface energy for cles that form the thick haze layers. One of the main seven samples from three different laboratories. Two efforts to better understand the chemistry of the haze is tholin samples were produced in the Planetary Haze through the synthetic analog materials of Titan’s haze, Research (PHAZER) chamber at Johns Hopkins Uni- tholins. Several groups have been involved in the pro- versity (JHU) from an initial N2:CH4 (95:5) gas mix- duction of tholins and analyses of its physical, chemi- ture using two energy sources: an AC glow discharge cal, and optical properties. Distinct laboratory setups and a hydrogen UV Lamp [11]. Four tholins samples were developed to simulate the various processes that were produced in the Cosmic Simulation Chamber drive photochemistry in Titan’s atmosphere (e.g.[1]). (COSmIC) at NASA Ames Research Center (ARC) The experimental conditions used to produce Titan from four different initial gas mixtures: N2:CH4 (95:5), aerosol analogs have an impact on their chemical and N2:CH4:C2H2 (94.5:5:0.5), Ar:CH4 (95:5), and physical properties, e.g.[2]. Thus, it would be prema- Ar:CH4:C2H2 (94.5:5:0.5), using cold plasma discharge ture to extract the property of one specific laboratory- as the energy source [12]. One tholin sample was pro- made tholin and assume it applies to the actual Titan duced in the Photochemical Aerosol Chamber at Uni- haze analogs. However, only a few studies (e.g. [1,3]) versity of Northern Iowa (UNI) [13] from an initial gas have compared tholin samples made in different labo- mixture of N2:CH4 (95:5) using a deuterium lamp as ratories. The study presented here, which aims to char- the energy source. acterize a bulk physicochemical property of tholins To measure the surface energy of a tholin sample, made by different laboratory groups with distinct labo- a droplet of a test liquid is dispensed onto the sample, ratory set-ups and experimental conditions, has the using a microsyringe, to form a sessile drop. The test potential to reveal common traits between tholins. liquids used are HPLC-grade water (FisherChemi- Traits that are shared by several tholins can be expect- calTM) and diiodomethane (>99%, ACROS Organic- ed to be present in Titan aerosols. sTM). Each drop process is recorded as video using an Here we present the results to our comparison goniometer (Osilla). Contact angles are then measured study of tholin samples through one specific property: by both the Ossila software and contact angle plugin of surface energy. The change of free energy when the the ImageJ software. A comparison test confirmed Os- surface area of a solid is increased by a unit area is illa and ImageJ return similar contact angle values and defined as surface energy. The free energy change is can be used interchangeably. The Owens-Wendt-Ra- equivalent to the energy needed to separate two con- bel-Kaelble (OWRK) and Wu analytical methods are tacting solid surfaces per unit area, determining adhe- then used to estimate the surface energies of each sion and wettability of surfaces and any intervening tholin from contact angle measurements. Both assume medium [4]. It has been theorized that the total surface the surface energy and surface tension can be parti- energy be divided into different components, and these tioned into a dispersive component and a polar compo- individual component values can be informative of the nent. All experiments are performed inside a dry glove independent intermolecular forces [5]. Surface energy box (relative humidity RH <1%) flowed with 99.999% can reveal the fundamental bulk chemical make-up, purity dry nitrogen cohesiveness and wetting properties of a material. Haze particles can act as cloud condensation nuclei for Results and Discussion: The surface energies of all various condensable simple organic molecules to form tholin samples spanned from 45-75 mJ/m2 and are list- condensation clouds [6,7], fall to the surface where ed in Table 1. The surface energies of JHU samples they partake in fluvial and aeolian processes, and be- were similar to previous measurements [14]. For the come dune materials and sediments in the polar lakes JHU tholin samples, the one produced with plasma [8,9]. Surface energy of the Titan hazes has important (JHU-plasma) has a more substantial polar component 52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 2675.pdf than the one produced with UV (JHU-UV). This can be estimated from the measured tholin surface energies attributed to the deuterium lamp used to produce JHU- and the surface tensions and surface energies of ethane UV, which does not emit the range of photons required and methane. All samples wetted completely with to directly dissociate nitrogen in the gas mixture as methane and most completely with ethane, suggesting compounds containing nitrogen are the main contribu- that tholins are likely ideal cloud condensation nuclei tors to the polar components of the tholins’ surface (CCN) for heterogeneous nucleation despite their in- energy. Not having a source of dissociated molecular solubility in these hydrocarbons [1]. Due to the low nitrogen lowers the polar component and therefore the contact angles between methane and ethane, tholin total surface energy of JHU-UV. The UNI tholin sam- particles are unlikely to float on the hydrocarbon lakes ple (UNI-UV) has a similar overall surface energy and from capillary forces. The high dispersive components surface energy partitioning pattern to JHU-UV. Despite among all tholin samples can lead to similar behaviors their different experimental conditions, the resem- towards methane-ethane cloud formation and aerosol- blance can be attributed to their common energy lake interactions. As both methane and ethane have source, the deuterium lamp, and the same initial gas small polar components of surface energy and surface mixing ratio. tension, the dispersive components will be the deter- mining factor. The small contact angles can then be Table 1: Derived surface energy of tholin from different attributed to this shared characteristic, implying clouds methods, all units in mJ/m2. Both the values of the total sur- can likely condensate effectively with haze particles as face energy γstot can be divided into the dispersive, γsd, and the CCN and that haze particles that fall to the hydro- polar, γsp, components. carbon lakes would sink to the bottom. Conclusion and future work: To gain insight into the processes involving the haze on Titan, we com- pared the surface energy of haze analogs “tholins” made in three laboratories and found that a high dis- persive component of surface energy ranging from 30- 50 mJ/m2, is present among all samples. The estimated contact angle between two hydro- carbons present on Titan, methane and ethane, and the tholins, calculated from the surface energy of tholin, are small. The common trait of high dispersive compo- With a cold plasma discharge, dissociation of nents suggest that Titan haze particles are likely good the molecular nitrogen is possible resulting in for for- cloud condensation nuclei for methane and ethane mation of polar compounds in the N2-based mixtures clouds and sink to the bottom as they sediment. These which participate in the polar component of surface surface energy measurements can also be connected to energy, as seen with JHU-plasma. For the tholins pro- other properties of tholins like optical constants, which duced by plasma chemistry at ARC, although adding we plan to investigate in the future. heavier precursors in the initial gas mixture results in a more complex chemistry [12], the surface energies are References: not necessarily higher. When comparing the ARC N2- CH4 and ARC N2-CH4-C2H2 samples, the total and [1] Cable, M. L. et al. (2012), ChRv, 112, 1882. [2] polar components of surface energy of the tholin with- Imanaka, H. et al. (2004), Icarus, 168(2), 344. [3] Coll, out acetylene is much higher. Addition of acetylene, a P. et al. (2013), P&SS, 77, 91. [4] Israelachvili, J. N. non-polar hydrocarbon precursors, increased the C/N, (2011), Intermolecular and Surface Forces (3rd ed.; thus reducing the polar component of surface energy New York: Academic). [5] Fowkes, F. M. (1964), Ind. compared to ARC N2-CH4. As expected, the ARC Ar- & Eng. Chem., 56, 40. [6] Curtis, D. B. et al. (2008), CH4-C2H2 and ARC Ar-CH4 have polar components Icarus, 195(2), 792. [7] Lavvas, P. et al. (2011), Icarus, close to 0 mJ/m2. Their initial gas mixtures contained 215, 732.
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