Origin of water in the terrestrial planets

By M. Drake. 2005

159 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/d8256673d4366ece8be1a029a91f07839d8a9eee

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In Astronomy and Astrophysics

Citations in the corpus

Heterogeneous distribution of H2O in the Martian interior: Implications for the abundance of H2O in depleted and enriched mantle sources (2016, background): “…hydrologic cycle is still open to debate (Greeley 1987; Karlsson et al. 1992; Squyres and Kasting 1994; Phillips et al. 2001; Craddock and Howard 2002; Treiman 2003; Borg and Drake 2005; Paige 2005; Hurowitz and McLennan 2007; Tosca et al. 2008; Tosca and Knoll 2009; Di Achille and Hynek 2010).”
THE COMPOSITIONAL DIVERSITY OF EXTRASOLAR TERRESTRIAL PLANETS. I. IN SITU SIMULATIONS (2010, background): “Water can also potentially be incorporated into a planetary body via adsorption onto solid grains within the disk (Drake 2005).”
A SPITZER SURVEY OF MID-INFRARED MOLECULAR EMISSION FROM PROTOPLANETARY DISKS. I. DETECTION RATES (2010, background): “This suggests that the formation of oceans on ter- restrial planets may not require seeding by a late veneer from the outer reaches of a planetary system, such as the late heavy bombardment event, if water can efficiently adsorb to grains (e.g. Drake 2005; Muralidharan et al. 2008).”
Thermal Properties of Rocks and Density of Fluids (2014, background): “Stimpfl et al. (2004) and Drake (2005) calculated that the amount of water adsorbed in the Earth during accretion could have been as much as 1–3 Earth oceans.”
Water and astrobiology (2007, background): “This prospect has been explored by Drake (2005), who concluded that enough water could have been adsorbed onto grains from Solar nebular gas to supply up to three oceans to the growing Earth.”
Hydrous melting of the martian mantle produced both depleted and enriched shergottites (2012, unknown): “[21] Drake (2005) MAPS 40.”