冯 岳川

Dr. 冯 岳川


Research Focus & Metrics

Academic Career Length

4Years (2023-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2023 in Acta Petrologica Sinica
Verified
Journal Article
Closed access
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冯岳冯 岳川
冯 岳川
JDJun Deng
Jun Deng
HYHaoCheng YU
HaoCheng YU
QFQiang Fu
Qiang Fu
TCTao Cui
Tao Cui
SLShanShan LI
ShanShan LI

胶东地区是我国最大的黄金基地, 探明黄金资源储量超过5000t。胶东地区金矿床主要发育两种矿化样式, 即浸染状细脉-网脉型矿化和石英-硫化物脉型矿化, 金主要以可见金形式赋存于黄铁矿和石英中。玲珑金矿田位于招平断裂带北端, 同时发育两种矿化样式的矿体, 是研究金赋存状态的理想选区, 理清金的赋存状态对于选择合适的选冶工艺以及揭示金的成矿作用和富集机制具有重要的研究意义。在详实的野外地质调查基础上, 通过显微岩相学观察、电子探针分析与矿物自动定量分析, 对胶东玲珑金矿田两种不同矿化样式的样品中可见金的赋存状态进行了对比研究, 探讨了金成矿过程。玲珑金矿田两种矿化样式矿石中金矿物的赋存状态并无显著差异, 金矿物主要为银金矿和自然金。嵌布状态为裂隙金、包体金、粒间金, 以粒间金和包体金为主。金矿物粒度以微粒-细粒为主, 石英脉中偶见中粒-粗粒金矿物。金矿物主要以独立矿物形式以及与黄铜矿、方铅矿等硫化物共生的形式赋存于黄铁矿中。石英-黄铁矿阶段金矿物成色高于石英-多金属硫化物阶段金矿物成色, 主要是受到成矿温度的影响。浸染状细脉-网脉型样品金矿物比石英-硫化物脉型样品金矿物具有更高的金成色, 是由于两种矿化样式沉淀机制差异导致。


10 October 2024 in Water
Verified
Journal Article
Open access
PDF file
MSMin Sun
Min Sun
冯岳冯 岳川
冯 岳川
YZYao Zhao
Yao Zhao
XWXingrun Wang
Xingrun Wang
Various green materials like biochar and Fe0 (nano-scale zerovalent iron, nZVI) have been applied to remediate aqueous Cr(VI) contamination, but few studies have tried to further improve the performance of nZVI and/or biochar composites with different sulfidation methods. Here, we modified a hybrid material of nZVI@biochar with Na2S and pyrite (FeS2), applied it to remove aqueous Cr(VI) under different experimental conditions, and revealed key factors influencing Cr(VI) removal performance. The results show that pyrite loading is an effective sulfidation method to increase the Fe and S contents in composites. FeSx-nZVI@BC (1:1) had a Cr(VI) removal efficiency of ~95% with 5 mg/L Cr(VI) loaded, which was much higher than other hybrid composites. The Cr(VI) removal efficiency of FeSx-nZVI@BC showed a decreasing trend under pH conditions that increased from pH 3 to pH 9. The presence of dissolved oxygen and aqueous Cu2+ and Cd2+ could significantly suppress the removal of aqueous Cr(VI), while humic acids at different concentrations did not suppress Cr(VI) removal. After the reaction, it was observed with an energy-dispersive spectrometer (SEM-EDS) that most Cr in the solid phase was closely associated with pyrite minerals. X-ray photoelectron spectroscopy (XPS) spectra, together with the Fe2+-quenching method, confirmed that Fe (Fe2+ or Fe0) acted as the main electron donor, contributing to ~90% of the Cr(VI) reduction. Our study indicates that pyrite loading could further improve the performance of remediation materials and that the pyrite-loaded nZVI@BC composite is a green material with strong potential to be applied in the remediation of water contaminated by Cr(VI).