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The high-temperature mechanical properties of an in-situ toughened silicon carbide have been examined at temperatures from ambient to 1300C with the objective of optimizing structural performance.
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Recent work with the green alga Dunaliella salina showed the presence of a approximately 20 kDa chloroplast protein that was recognized by polyclonal antibodies raised against the isolated LHC-II [Webb M.R. and Melis A. (1995) Plant Physiol. 107: 885]. In this report, a characterization of the approximately 20 kDa polypeptide is presented. It is shown that it is localized in the chloroplast envelope membrane of D. salina. The abundance of this protein is constant on a per cell basis and independent of the light regime during cell growth. The approximately 20 kDa polypeptide is easily degraded to a approximately 19 kDa product during sample preparation. A limited amino acid sequence of 21 residues from the free N-terminus of the approximately 19 kDa product was obtained. On the basis of this partial sequence, it was concluded that the approximately 20 kDa polypeptide is not a degradation product of a known LHC-II but rather a novel protein. The approximately 20 kDa polypeptide did not cross-react with antibodies raised against the Cbr (carotene biosynthesis-related) gene product and showed a different electrophoretic mobility from the latter. Light-shift experiments suggest that the approximately 20 kDa polypeptide is not an ELIP (early light-inducible protein). Possible functions of the approximately 20 kDa protein are discussed.
We present ab initio calculations of the zero‐temperature composition dependent spin transition pressures in rocksalt (B1) (Mg 1−x ,Fe x )O. We predict that the spin transition pressure decreases with increasing Mg content, consistent with experimental results. At high‐pressure, we find that the effective size of Mg is smaller than high‐spin Fe but quite close to low‐spin Fe, consistent with a simple compression argument for how Mg reduces the spin transition pressure. We also show that the spin transition is primarily driven by the volume difference between the high‐spin and low‐spin phases, rather than changes in the electronic structure with pressure. The volume contraction at the transition is found to depend non‐monotonically on Fe content. For FeO we predict a B1 → iB8 transition at 63 GPa, consistent with previous results. However, we also predict an unexpected reverse transition of high‐spin iB8 → low‐spin B1 at approximately 400 GPa.