Abstract We simulate Venus’ evolution with a coupled one-dimensional solar-atmosphere-lithosphere-mantle-core model to predict currently unobservable features and its eruptive mass flux. We identified four distinct evolutionary pathways that simultaneously match the atmospheric abundances of water and carbon dioxide as well as the lack of a core dynamo. These scenarios are characterized by (I) generally monotonic cooling, (II) a low mantle melt fraction in which Venus' volcanically active phase is ending, (III) a small inner core, and (IV) oscillations of internal properties. Through random forest classification, we determined that the key parameters that distinguish these types are the initial mantle water abundance, the mantle viscosity, the dehydration stiffening strength, the eruption efficiency, and the melting point of the core. In each of the plausible histories, Venus retains at least one Earth ocean’s worth of water in its mantle and remains volcanically active today. Venus’ lack of a current geodynamo allows for thermal histories with an initially large inner core in our parameter sweep. In 88% of plausible histories, we found that Venus possessed a past magnetic field. The results strongly disfavor recent high eruption rate estimates, but are consistent with lower estimates. Current resurfacing estimates also strongly disfavor the low melt scenario, implying that Venus is not nearly volcanically “dead.” These predictions are testable with anticipated data, and the model can be applied to exoplanets to predict their properties.
Garcia et al. (Fri,) studied this question.
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