• New bulk composition model of Mars: Yoshizaki 2020 


Also, palmitic acid was the major saturated fatty acid, and oleic and linoleic acids were the major unsaturated fatty acids in buckwheat seeds of Korean and Chinese cultivars (c ho

Plain Language Summary To estimate core compositions of terrestrial planets using geophysical data with high‐pressure physical property of core‐forming materials, we measure the

• Model core composition of Mars while matching the geochemistry of the Martian mantle (Ni, Co, Cr, Nb/Ta, W). • Accreting with low FeO content not consistent with

‣ core S composition inferences deduced from geodesy data and interior modeling are in agreement with geochemical constraints (xS≲21wt%). ‣ but those results are not in agreement

(2009) and experimental data (green: solid circle – solid iron, solid square – carbide, and open symbols – coexisting liquid) at 5 GPa from Chabot et al. (2008) are also plotted

• models with an inner core can have mantle boundary temperatures below the mantle solidus 1Gyr after formation and agree with the timing of occurrence of the lunar dynamo, but

• models with an inner core can have an early dynamo, a core-mantle boundary temperature below the mantle solidus after ~400Ma, and an early surface magnetic field in agreement

• at high (10 wt%) CaCl 2 concentrations, single (dissolved) PpPTA chains show a relatively strong interaction with chloride ions through hydrogen bond formation by the amide