FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4378907300> ?p ?o ?g. }

• W4378907300 abstract "Ablation waves involve solid substrate such as ice or soluble rocks. Ablation by sublimation or dissolution under turbulent winds or liquid flows may lead to the development of transverse linear bedforms (ablation waves) on volatile or soluble susbtrates. In glaciology, geomorphology, karstology and planetology, these ablation waves may provide relevant morphological markers to constrain the flows that control their formation. For that purpose, we describe a unified model, that couples mass transfers and turbulent flow dynamics and takes into account the relationship between the viscosity of the fluid and the diffusivity of the ablated material, for both sublimation and dissolution waves. From the stability analysis of the model, we derive three scaling laws that relate the wavelength, the migration velocity and the growth time of the waves to the physical characteristics (pressure, temperature, friction velocity, viscous length, ablation rate) of their environment through coefficients obtained numerically. The laws are validated on terrestrial examples and laboratory experiments of sublimation and dissolution waves. Then, these laws are plotted in specific charts for dissolution waves in liquid water, for sublimation waves in N 2 -rich atmospheres (e.g., Earth, Titan, Pluto) and in CO 2 -rich atmospheres (e.g., Mars, Venus). They are applied to rock dissolution on the walls of a limestone cave (Saint-Marcel d’Ardèche, France), to H 2 O ice sublimation on the North Polar Cap (Mars) and to CH 4 ice sublimation in Sputnik Planitia (Pluto), to demonstrate how they can be used (1) either to derive physical conditions on planetary surfaces from observed geometric characteristics of ablation waves (2) or, conversely, to predict geometric characteristics of ablation waves from measured or inferred physical conditions on planetary surfaces. The migration of sublimation waves on regions of the Martian North Polar Cap and sublimation waves candidates on Pluto are discussed." @default.
• W4378907300 created "2023-06-01" @default.
• W4378907300 creator A5009412108 @default.
• W4378907300 creator A5038182615 @default.
• W4378907300 creator A5046256675 @default.
• W4378907300 date "2023-05-30" @default.
• W4378907300 modified "2023-10-03" @default.
• W4378907300 title "Scaling laws for ablation waves formed by ice sublimation and rock dissolution: applications to the Earth, Mars and Pluto" @default.
• W4378907300 cites W1587047283 @default.
• W4378907300 cites W1588463162 @default.
• W4378907300 cites W1597513210 @default.
• W4378907300 cites W1630567614 @default.
• W4378907300 cites W1963722072 @default.
• W4378907300 cites W1968464942 @default.
• W4378907300 cites W1976338108 @default.
• W4378907300 cites W1981614797 @default.
• W4378907300 cites W1983079246 @default.
• W4378907300 cites W1984601650 @default.
• W4378907300 cites W1986594007 @default.
• W4378907300 cites W1991980856 @default.
• W4378907300 cites W1992188874 @default.
• W4378907300 cites W1997866121 @default.
• W4378907300 cites W2000100809 @default.
• W4378907300 cites W2005198714 @default.
• W4378907300 cites W2010417599 @default.
• W4378907300 cites W2016149577 @default.
• W4378907300 cites W2016200726 @default.
• W4378907300 cites W2016471989 @default.
• W4378907300 cites W2016972446 @default.
• W4378907300 cites W2020249145 @default.
• W4378907300 cites W2020905882 @default.
• W4378907300 cites W2021519515 @default.
• W4378907300 cites W2023722096 @default.
• W4378907300 cites W2024789945 @default.
• W4378907300 cites W2025057625 @default.
• W4378907300 cites W2025663379 @default.
• W4378907300 cites W2025818923 @default.
• W4378907300 cites W2027789402 @default.
• W4378907300 cites W2028130343 @default.
• W4378907300 cites W2032961824 @default.
• W4378907300 cites W2034620163 @default.
• W4378907300 cites W2035624426 @default.
• W4378907300 cites W2038491844 @default.
• W4378907300 cites W2040729273 @default.
• W4378907300 cites W2042154709 @default.
• W4378907300 cites W2044104498 @default.
• W4378907300 cites W2044611079 @default.
• W4378907300 cites W2056627274 @default.
• W4378907300 cites W2056775505 @default.
• W4378907300 cites W2064729831 @default.
• W4378907300 cites W2065346059 @default.
• W4378907300 cites W2065378548 @default.
• W4378907300 cites W2067287517 @default.
• W4378907300 cites W2067652619 @default.
• W4378907300 cites W2068129820 @default.
• W4378907300 cites W2068601385 @default.
• W4378907300 cites W2070529447 @default.
• W4378907300 cites W2073151954 @default.
• W4378907300 cites W2081066434 @default.
• W4378907300 cites W2081598710 @default.
• W4378907300 cites W2081741931 @default.
• W4378907300 cites W2086370805 @default.
• W4378907300 cites W2087647331 @default.
• W4378907300 cites W2087801168 @default.
• W4378907300 cites W2089710357 @default.
• W4378907300 cites W2101107193 @default.
• W4378907300 cites W2110420344 @default.
• W4378907300 cites W2128971099 @default.
• W4378907300 cites W2131543945 @default.
• W4378907300 cites W2139315028 @default.
• W4378907300 cites W2144686850 @default.
• W4378907300 cites W2147553070 @default.
• W4378907300 cites W2151346430 @default.
• W4378907300 cites W2151651999 @default.
• W4378907300 cites W2161926515 @default.
• W4378907300 cites W2167420953 @default.
• W4378907300 cites W2169798625 @default.
• W4378907300 cites W2199001370 @default.
• W4378907300 cites W2298696681 @default.
• W4378907300 cites W2323609601 @default.
• W4378907300 cites W2344188539 @default.
• W4378907300 cites W2409823238 @default.
• W4378907300 cites W2417497218 @default.
• W4378907300 cites W2438770523 @default.
• W4378907300 cites W2515082864 @default.
• W4378907300 cites W2550987443 @default.
• W4378907300 cites W2559969888 @default.
• W4378907300 cites W2563844585 @default.
• W4378907300 cites W2570865274 @default.
• W4378907300 cites W2576732653 @default.
• W4378907300 cites W2586113662 @default.
• W4378907300 cites W2595103090 @default.
• W4378907300 cites W2604250636 @default.
• W4378907300 cites W2616553056 @default.
• W4378907300 cites W2756021820 @default.
• W4378907300 cites W2762210775 @default.
• W4378907300 cites W2766984293 @default.
• W4378907300 cites W2792314031 @default.
• W4378907300 cites W2807454817 @default.
• W4378907300 cites W2888388222 @default.

• next