Jianxi Zhu

TL;DR: In this paper, the authors investigated magnetite exsolution in ilmenite from Fe-Ti oxide gabbro in the Xinjie intrusion, SW China and found that the magnetite lamellae have close-packed oxygen planes and directions parallel to those in the host ilmenites with {111}Mag//(0001)Ilm and![Formula]

TL;DR: Hydrothermal carbons with a low graphitization degree contain more PFRs for Fe(III) reducing, significantly enhancing the Fenton catalytic activity of Fh, indicating that HTC act as electron donors due to the abundant carbon-centered persistent free radicals (PFRs) to decrease the H2O2 consumption by Fe( III), which subsequently inhibits the generation of less active O2•- and promote the utilization efficiency of H2 O2.

TL;DR: In this article, the dynamic evolution of the resistive kink mode with electron diamagnetic drift was investigated by employing a three-dimensional toroidal Hall-MHD code CLT.

TL;DR: This study combines molecular dynamics (MD) and Monte Carlo (MC) simulations to disclose the swelling behavior of rectorite and compare with montmorillonite and finds that the bilayer hydrate of Na-rectorite is more thermodynamically stable than the monolayers hydrate, which is similar to Na-montMorillonite.

TL;DR: In this paper, the authors investigated the origin and evolution of rare earth element (REE) deposits in the weathering crusts of metamorphic sandstone and showed that the most common types of rare Earth element (REE) are found in the metamorphics of metamodal sandstones.