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High-Salinity Fluid Downslope Flow on Regolith Layer Examined by Laboratory Experiment: Implications for Recurring Slope Lineae on Martian Surfaces

Numerous dark linear recurrent features called Recurring Slope Lineae (RSL) are observed on Martian surfaces, hypothesized as footprints of high-salinity liquid flow. This paper experimentally examined this “wet hypothesis” by analyzing the aspect ratios (length/width) of the flow traces on the gran...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awduron: Yoshiki Tabuchi, Arata Kioka, Takeshi Tsuji, Yasuhiro Yamada
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: MDPI AG 2025-07-01
Cyfres:Fluids
Pynciau:
Mynediad Ar-lein:https://www.mdpi.com/2311-5521/10/7/183
Tagiau: Ychwanegu Tag
Dim Tagiau, Byddwch y cyntaf i dagio'r cofnod hwn!