Deactivation mechanism of KCl and K2SO4 poisoned V2O5/WO3-TiO2 catalyst on gaseous elemental mercury oxidation

Fuel ◽  
2020 ◽  
Vol 278 ◽  
pp. 118245
Author(s):  
Jingyuan Hu ◽  
Guangqian Luo ◽  
Zehua Li ◽  
Mengyuan Liu ◽  
Renjie Zou ◽  
...  
Keyword(s):  
Elemental Mercury ◽  
Mercury Oxidation ◽  
Gaseous Elemental Mercury ◽  
Tio2 Catalyst ◽  
Deactivation Mechanism

Mechanistic and kinetic studies of elemental mercury oxidation over a RuO2/rutile TiO2 catalyst

2017 ◽  
Vol 7 (20) ◽  
pp. 4669-4679 ◽  
Author(s):  
Zhouyang Liu ◽  
Vishnu Sriram ◽  
Can Li ◽  
Joo-Youp Lee
Keyword(s):  
Kinetic Study ◽  
Ruthenium Oxide ◽  
Kinetic Studies ◽  
Elemental Mercury ◽  
Oxidation Catalyst ◽  
Mechanistic Study ◽  
Mercury Oxidation ◽  
Rutile Tio2 ◽  
Tio2 Catalyst

A mechanistic study using in situ DRIFTS and a kinetic study were conducted on a ruthenium oxide based mercury oxidation catalyst.

Ceria–zirconia modified MnOx catalysts for gaseous elemental mercury oxidation and adsorption

2016 ◽  
Vol 6 (6) ◽  
pp. 1792-1803 ◽  
Author(s):  
Deshetti Jampaiah ◽  
Samuel J. Ippolito ◽  
Ylias M. Sabri ◽  
James Tardio ◽  
P. R. Selvakannan ◽  
...  
Keyword(s):  
Elemental Mercury ◽  
Mercury Oxidation ◽  
Gaseous Elemental Mercury

The developed ceria–zirconia modified MnOx catalysts were found to exhibit enhanced Hg0 oxidation and removal performance.

Impact of SO2 on elemental mercury oxidation over CeO2–TiO2 catalyst

2013 ◽  
Vol 219 ◽  
pp. 319-326 ◽  
Author(s):  
Hailong Li ◽  
Chang-Yu Wu ◽  
Ying Li ◽  
Liqing Li ◽  
Yongchun Zhao ◽  
...  
Keyword(s):  
Elemental Mercury ◽  
Mercury Oxidation ◽  
Tio2 Catalyst

scholarly journals Enhanced production of oxidised mercury over the tropical Pacific Ocean: a key missing oxidation pathway

2014 ◽  
Vol 14 (3) ◽  
pp. 1323-1335 ◽  
Author(s):  
F. Wang ◽  
A. Saiz-Lopez ◽  
A. S. Mahajan ◽  
J. C. Gómez Martín ◽  
D. Armstrong ◽  
...  
Keyword(s):  
Marine Boundary Layer ◽  
Oxidation Mechanism ◽  
Elemental Mercury ◽  
Atmospheric Mercury ◽  
Mercury Oxidation ◽  
Gaseous Elemental Mercury ◽  
Enhanced Production ◽  
Modelling Studies ◽  
Aquatic Food ◽  
The Stability

Abstract. Mercury is a contaminant of global concern. It is transported in the atmosphere primarily as gaseous elemental mercury, but its reactivity and deposition to the surface environment, through which it enters the aquatic food chain, is greatly enhanced following oxidation. Measurements and modelling studies of oxidised mercury in the polar to sub-tropical marine boundary layer (MBL) have suggested that photolytically produced bromine atoms are the primary oxidant of mercury. We report year-round measurements of elemental and oxidised mercury, along with ozone, halogen oxides (IO and BrO) and nitrogen oxides (NO2), in the MBL over the Galápagos Islands in the equatorial Pacific. Elemental mercury concentration remained low throughout the year, while higher than expected levels of oxidised mercury occurred around midday. Our results show that the production of oxidised mercury in the tropical MBL cannot be accounted for by bromine oxidation only, or by the inclusion of ozone and hydroxyl. As a two-step oxidation mechanism, where the HgBr intermediate is further oxidised to Hg(II), depends critically on the stability of HgBr, an additional oxidant is needed to react with HgBr to explain more than 50% of the observed oxidised mercury. Based on best available thermodynamic data, we show that atomic iodine, NO2, or HO2 could all play the potential role of the missing oxidant, though their relative importance cannot be determined explicitly at this time due to the uncertainties associated with mercury oxidation kinetics. We conclude that the key pathway that significantly enhances atmospheric mercury oxidation and deposition to the tropical oceans is missing from the current understanding of atmospheric mercury oxidation.

Investigation of Gaseous Elemental Mercury Oxidation by Non-thermal Plasma Injection Method

2017 ◽  
Vol 31 (10) ◽  
pp. 11013-11018 ◽  
Author(s):  
Jinjing Luo ◽  
Qiang Niu ◽  
Youxian Xia ◽  
Yinan Cao ◽  
Rupeng Du ◽  
...  
Keyword(s):  
Thermal Plasma ◽  
Elemental Mercury ◽  
Mercury Oxidation ◽  
Injection Method ◽  
Gaseous Elemental Mercury ◽  
Plasma Injection ◽  
Non Thermal Plasma

Support effect of Mn-based catalysts for gaseous elemental mercury oxidation and adsorption

2018 ◽  
Vol 8 (1) ◽  
pp. 297-306 ◽  
Author(s):  
Yinghong Wu ◽  
Wenqing Xu ◽  
Yang Yang ◽  
Jian Wang ◽  
Tingyu Zhu
Keyword(s):  
Elemental Mercury ◽  
Support Effect ◽  
Impregnation Method ◽  
Mercury Oxidation ◽  
Gaseous Elemental Mercury

Mn-Based catalysts with a Mn loading of 4 wt% were prepared using an impregnation method.

scholarly journals Air Concentrations of Gaseous Elemental Mercury and Vegetation–Air Fluxes within Saltmarshes of the Tagus Estuary, Portugal

Atmosphere ◽  
2021 ◽  
Vol 12 (2) ◽  
pp. 228
Author(s):  
Rute Cesário ◽  
Nelson J. O’Driscoll ◽  
Sara Justino ◽  
Claire E. Wilson ◽  
Carlos E. Monteiro ◽  
...  
Keyword(s):  
Leaf Area ◽  
Elemental Mercury ◽  
Ambient Air ◽  
Tagus Estuary ◽  
Contaminated Site ◽  
Gaseous Elemental Mercury ◽  
Mercury Flux ◽  
Sarcocornia Fruticosa ◽  
Air Concentrations

In situ air concentrations of gaseous elemental mercury (Hg(0)) and vegetation–atmosphere fluxes were quantified in both high (Cala Norte, CN) and low-to-moderate (Alcochete, ALC) Hg-contaminated saltmarsh areas of the Tagus estuary colonized by plant species Halimione portulacoides (Hp) and Sarcocornia fruticosa (Sf). Atmospheric Hg(0) ranged between 1.08–18.15 ng m−3 in CN and 1.18–3.53 ng m−3 in ALC. In CN, most of the high Hg(0) levels occurred during nighttime, while the opposite was observed at ALC, suggesting that photoreduction was not driving the air Hg(0) concentrations at the contaminated site. Vegetation–air Hg(0) fluxes were low in ALC and ranged from −0.76 to 1.52 ng m−2 (leaf area) h−1 for Hp and from −0.40 to 1.28 ng m−2 (leaf area) h−1 for Sf. In CN, higher Hg fluxes were observed for both plants, ranging from −9.90 to 15.45 ng m−2 (leaf area) h−1 for Hp and from −8.93 to 12.58 ng m−2 (leaf area) h−1 for Sf. Mercury flux results at CN were considered less reliable due to large and fast variations in the ambient air concentrations of Hg(0), which may have been influenced by emissions from the nearby chlor-alkali plant, or historical contamination. Improved experimental setup, the influence of high local Hg concentrations and the seasonal activity of the plants must be considered when assessing vegetation–air Hg(0) fluxes in Hg-contaminated areas.

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