The Earth was shaped by H2 atmospheres

On the origin of the Earth’s water and the demographics of the Gaia and Keperly planets. Insights from the first principles

It is a mystery that the water on Earth came from the ocean and that it is less dense than it should be because it is made of metallic iron. Young and colleagues show that interactions between a young planet and its atmosphere might explain both in one fell swoop and the state of the Earth’s mantle.

The catalogs of the Gaia and Keperly industries. I. The demographic of the planet is dependent on stellar mass and age. Astron. J. 160,108 was published in 2020.

Petigura, E. A., Howard, A. W. & Marcy, G. W. Prevalence of Earth-size planets orbiting Sun-like stars. It was Proc. Natl Acad. Sci. USA 110, 19273–19278 (2013).

Zellner, B., Leake, M., Morrison, D. & Williams, J. The E asteroids and the origin of the enstatite achondrites. Geochim. There’s a dog and it’s cute. Acta 41, 1759–1767 (1977).

Gupta, A. & Schlichting, H. E. Sculpting the valley in the radius distribution of small exoplanets as a by-product of planet formation: the core-powered mass-loss mechanism. The day was Mon. Not. R. Astron. Soc. 487, 24–33 (2019).

Lammer, H. et al. Constraining the early evolution of Venus and Earth through atmospheric Ar, Ne isotope and bulk K/U ratios. Icarus 339, 113551 (2020).

Mars had chondritic volatiles before it came in contact with the ozone layer. Science 377,320–324, was published in 1992.

The outer core’s chemical composition was examined by first principles calculations. Earth is a planet. Sci. Lett. 531, 116009 (2020).

Anderson, O. L., Dubrovinsky, L., Saxena, S. K. & LeBihan, T. Experimental vibrational Grüneisen ratio values for ∈-iron up to 330 GPa at 300 K. Geophys. Res. Lett. 28, 399–402 (2001).

The evidence for an Earth-like geology of exoplanets can be found in the oxygen fugacities of extrasolar rocks. Science 347, 347–377 (2019).

The internal structure of Mercury: effects of silicate composition on internal and external solubility of molecular hydrogen in liquid iron. Re. Lett. 37, 38-49

Effect of Si on liquid Fe compressibility is relevant in core materials. Geophys. There is a Res. Lett. 31, L07604 was published in 2004.

W. M. and R. D. were able to measure the hydrogen solubility in liquid iron. Metall. There is a person that is called a Mater. Trans. B 5 was published in 1974.

The effects of composition on the thermal component of impact-driven atmospheric loss are studied. Mon. Not. There is R. Astron. Soc. 501, 587–595 (2021).

Riner, M. A., Bina, C. R., Robinson, M. S. & Desch, S. J. Internal structure of Mercury: implications of a molten core. J. Geophys. Res. Planets 114, E02913 were published in 2008.

Hirschmann, M., Withers, A., Ardia, P. & Foley, N. Solubility of molecular hydrogen in silicate melts and consequences for volatile evolution of terrestrial planets. The planet Earth. Lett.35, 38–49 is published in 2012

Source: https://www.nature.com/articles/s41586-023-05823-0

Statistical mechanics of sputey at high pressure. Xiang, Y., Fan, W. & Gong, X

Xiang, Y., Sun, D., Fan, W. & Gong, X. Generalized simulated annealing algorithm and its application to the thomson model. Phys. Lett. A 233, 216–220 (1997).

Some rock and ice are found in the interiors of water worlds. Sci. Rep. 12, 13055 (2022).

In this paper, interaction parameters are estimated fromliquid structure and heat of solution at infinite dilution. High Temp. The figure of a man, as reported by the Mater. Procedures 31, 202–108 were conducted.

Righter, K., Rowland, R.II, Yang, S. & Humayun, M. Activity coefficients of siderophile elements in Fe–Si liquids at high pressure. Geochem. There was a Persp. Lett. 15, 44–49 (2020).

The lattice dynamics of sputey at high pressure were studied by Karki, Wentzcovitch, and de Gironcoli. The article was published in the journal of Ps. Rev. B 62.

Katsura, T. et al. The thermal expansion of forsterite is determined by the degree to which the upper mantle has adiabatic thermophilicity. There is an instrument known as the ps. Earth Planet. Inter. 174 was published in 2009.

Young, E. D. et al. High-temperature equilibrium isotope fractionation of non-traditional stable isotopes: experiments, theory, and applications. Chem. Geol. 395, 176–195 (2015).

Pringle, E. A.; Moynier, F.; Savage, P. S.; Badro, J. and Barrat,J.-A. Silicon atoms are present in angrites and planetesimals. Proc. National Acad. The USA’s science journal,Sci. USA, had a piece about 17029–17032.

It was called Bockelée-Morvan, D. Herschel measurements of the D/H and 16O/18O ratios in water in the Oort-cloud comet C/2009P1 (Garradd). Astron. There are astrophys. 544, L15 (2012).

The origin of and loss of hydrogen envelopes from the sub to the super-Earths can be found in this paper. The day started on Mon. Not. R. Astron. Soc. 439, 3225–3238 (2014).

Pahlevan, K., Schaefer, L. & Hirschmann, M. M. Hydrogen isotopic evidence for early oxidation of silicate Earth. Earth Planet. Lett. 526, 115770.

Barnes, J. J. et al. The moon’s water comes from the lunar highlands. Earth is a planet. Sci. Lett. 390, 244–252 (2014).

Previous post The Tenneesee commission will vote on whether or not to remove a lawmaker
Next post Michael Jordan sold his 1998 NBA Finals sneakers for a record amount