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Materials Data on LiCuS by Materials Project

LiCuS crystallizes in the orthorhombic Pbcn space group. The structure is three-dimensional. there are three inequivalent Li1+ sites. In the first Li1+ site, Li1+ is bonded to four S2- atoms to form a mixture of distorted corner and edge-sharing LiS4 trigonal pyramids. There are a spread of Li–S bond distances ranging from 2.48–2.96 Å. In the second Li1+ site, Li1+ is bonded to four S2- atoms to form a mixture of distorted corner and edge-sharing LiS4 tetrahedra. There are a spread of Li–S bond distances ranging from 2.41–2.91 Å. In the third Li1+ site, Li1+ is bonded in a distorted trigonal non-coplanar geometry to three S2- atoms. There are a spread of Li–S bond distances ranging from 2.45–2.50 Å. There are three inequivalent Cu1+ sites. In the first Cu1+ site, Cu1+ is bonded in a linear geometry to two equivalent S2- atoms. Both Cu–S bond lengths are 2.17 Å. In the second Cu1+ site, Cu1+ is bonded in a distorted linear geometry to two equivalent S2- atoms. There are one shorter (2.16 Å) and one longer (2.17 Å) Cu–S bond lengths. In the third Cu1+ site, Cu1+ is bonded in a linear geometry to two equivalent S2- atoms. There are one shorter (2.16 Å) and one longer (2.17 Å) Cu–S bond lengths. There are three inequivalent S2- sites. In the first S2- site, S2- is bonded in a 6-coordinate geometry to four Li1+ and two equivalent Cu1+ atoms. In the second S2- site, S2- is bonded in a 6-coordinate geometry to four Li1+ and two equivalent Cu1+ atoms. In the third S2- site, S2- is bonded in a 5-coordinate geometry to three Li1+ and two equivalent Cu1+ atoms.

36 MATERIALS SCIENCE↗

The Importance of Lake Overflow Floods for Early Martian Landscape Evolution: Insights From Licus Vallis

Open-basin lake outlet valleys are incised when water breaches the basin-confining topography and overflows. Outlet valleys record this flooding event and provide insight into how the lake and surrounding terrain evolved over time. Here we present a study of the paleolake outlet Licus Vallis, a >350 km long, >2 km wide, >100 m deep valley that heads at the outlet breach of an approx.30 km diameter impact crater. Multiple geomorphic features of this valley system suggest it records a more complex evolution than formation from a single lake overflow flood. This provides unique insight into the paleohydrology of lakes on early Mars, as we can make inferences beyond the most recent phase of activity..

Goudge, T. A.↗

Chromatographic and Spectroscopic Study of the Interaction between Polysulfides and Copper Sulfides

To mitigate the “polysulfide shuttle” in lithium–sulfur batteries, different hosting materials that can interact with the polysulfide species physically or chemically have been widely investigated. Copper sulfides as one type of material are believed to have strong chemical interactions with the polysulfide species to consequently influence the performances of Li–S batteries. In this work, high-performance liquid chromatography (HPLC), electrospray ionization mass spectrometry (ESI/MS), scanning electron microscopy with energy-dispersive X-ray spectrometry (SEM-EDS), and inductively coupled plasma optical emission spectroscopy (ICP-OES) were used to systematically investigate the interactions between ether-based polysulfide solutions and copper sulfides (as well as silver sulfide). Furthermore, based on chromatographic and spectroscopic results, the interactions between polysulfides and Cu 2 S can be classified into two types of reactions: one is the redox reaction with the formation of CuS, while another is the complexation reaction with the formation of soluble LiCuS n (n ≥ 4). Contrarily, Ag 2 S (and CuS) shows no interactions with polysulfides. Accordingly, the cycling behaviors of Li–S batteries with copper sulfides as hosting materials or with copper as additives were explained reasonably.

25 ENERGY STORAGE↗