Olivine is abundant in the Earth's upper mantle; it has applications in catalysts to enhance their stability in structures. The olivine-type catalysts were prepared by co-precipitation and hydrothermal synthesis and tested in the auto-thermal reforming (ATR) of acetic acid (AC), a model compound from bio-oil, for hydrogen production. In the meantime, the natural olivine impregnated with Ni was also tested. Characterisations of XRD, nitrogen physisorption, temperature-programmed reduction, and SEM-EDX were used to find the structure-reactivity relationship. The results indicate that the natural olivine produced a low H2 yield close to 0.17 mole of H2 per 1 mole of AC, while the olivine impregnated with Ni produced a H2 yield of from 2.19 mole to 2.73 mole of H2 per mole of AC. The olivine catalyst prepared by hydrothermal synthesis performed better in both activity and stability: the H2 yield achieved 3.06 mole of H2 per mole of AC and remained stable, which could be attributed to the higher surface area and stability with Ni inserted in the skeleton of olivine.
Western Yunnan is the well‐known polymetallic province in China. It is characterized by copper‐gold mineralization related to Cenozoic alkali‐rich porphyry. This paper analyzes the silicon isotope data obtained from four typical alkali‐rich porphyry deposits based on the dynamic fractionation principle of silicon isotope. The study shows that the ore materials should originate mainly from alkali‐rich magmas, together with silicon‐rich mineralizing fluids. The process of mineralization was completed by auto‐metasomatism, i.e. silicon‐rich mineralizing fluids (including alkali‐rich porphyry and wall‐rock strata) replaced and altered the country rocks and contaminated with crustal rocks during the crystallization of alkali‐rich magmas. Such a process is essentially the continuance of the metasomatism of mantle fluids in crust's mineralization. This provides important evidence of silicon isotopic geochemistry for better understanding the mineralization of the Cenozoic alkali‐rich porphyry polymetallic deposits
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