Recently, it was reported that using CO as a flotation gas increases the flotation of auriferous pyrite from high carbonate gold ores of the Carlin Trend. In this regard, the influence of CO on bubble attachment at fresh pyrite surfaces was measured in the absence of collector using an induction timer, and it was found that nitrogen bubble attachment time was significantly reduced from 30 ms to less than 10 ms in CO saturated solutions. Details of CO bubble attachment at a fresh pyrite surface have been examined by atomic force microscopy (AFM) measurements and molecular dynamics (MD) simulations, and the results used to describe the subsequent attachment of a N bubble. As found from MD simulations, unlike the attached N bubble, which is stable and has a contact angle of about 90°, the CO bubble attaches, and spreads, wetting the fresh pyrite surface and forming a multilayer of CO molecules, corresponding to a contact angle of almost 180°. These MDS results are complemented by in situ AFM images, which show that, after attachment, CO nano-/microbubbles spread to form pancake bubbles at the fresh pyrite surface. In summary, it seems that CO bubbles have a propensity to spread, and whether CO exists as layers of CO molecules (gas pancakes) or as nano-/microbubbles, their presence at the fresh pyrite surface subsequently facilitates film rupture and attachment of millimeter N bubbles and, in this way, improves the flotation of pyrite.
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http://dx.doi.org/10.1021/acs.langmuir.8b02929 | DOI Listing |
Environ Res
December 2024
State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, No. 73 Huanghe Road, Nangang District, Harbin, 150090, China. Electronic address:
Iron-dependent denitrification has been substantially investigated worldwide due to the advantages of low cost, high efficiency, and synchronized phosphorous removal. However, differences in nitrogen metabolism processes with different iron-based materials as electron donors have not been systematically studied. This study investigated the efficacy of nitrogen and phosphate removal using various iron-based materials as electron donors.
View Article and Find Full Text PDFSci Total Environ
November 2024
Department of Earth Sciences, National Cheng Kung University, Tainan 70101, Taiwan.
Chemical weathering is a pivotal geochemical process that shapes the carbon cycling and climates in the critical zone. Among its critical drivers, river discharge holds a particular significance, especially in the orogenic landscapes. Here, we examined the impact of discharge on mineral weathering in southwestern (SW) Taiwan by analyzing river water chemistry across a wide discharge range.
View Article and Find Full Text PDFLangmuir
August 2024
School of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China.
The effect of seawater on the flotation of sulfide minerals is a hot research topic at the present. Using seawater instead of fresh water to separate lead-sulfur can save fresh water resources and reduce lime consumption, which has broad prospects in terms of economic and environmental protection. Many studies have shown that divalent calcium and magnesium ions in seawater are hydrolyzed to form hydroxyl complexes under alkaline pH values, which affects the flotation separation of sulfide ore.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
July 2024
Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA 94720.
Climate influences near-surface biogeochemical processes and thereby determines the partitioning of carbon dioxide (CO) in shale, and yet the controls on carbon (C) weathering fluxes remain poorly constrained. Using a dataset that characterizes biogeochemical responses to climate forcing in shale regolith, we implement a numerical model that describes the effects of water infiltration events, gas exchange, and temperature fluctuations on soil respiration and mineral weathering at a seasonal timescale. Our modeling approach allows us to quantitatively disentangle the controls of transient climate forcing and biogeochemical mechanisms on C partitioning.
View Article and Find Full Text PDFAn Acad Bras Cienc
April 2024
Universidade Federal do Rio Grande do Sul, Instituto de Geociências, Av. Bento Gonçalves, 9500, 91501-970 Porto Alegre, RS, Brazil.
The thorough redox alteration of a lava flow is an undescribed feature in intraplate basaltic provinces. The Early Cretaceous (134.5 Ma) Paraná Province displays that alteration in the major Muralha Flow.
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