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John Munthe

Researcher at Chalmers University of Technology

Publications -  105
Citations -  9431

John Munthe is an academic researcher from Chalmers University of Technology. The author has contributed to research in topics: Mercury (element) & Aqueous solution. The author has an hindex of 48, co-authored 105 publications receiving 8653 citations. Previous affiliations of John Munthe include Finnish Environment Institute.

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Atmospheric mercury species over central and Northern Europe. Model calculations and nordic air and precipitation network for 1987 and 1988

TL;DR: In this article, a chemical scheme based upon current knowledge of physicochemical forms and transformation reactions of atmospheric mercury has been implemented into a regional pollutant dispersion model for Europe, which is capable of simulating long-range transport of mercury from Central Europe to Scandinavia.
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Forestry practices increase mercury and methyl mercury output from boreal forest catchments.

TL;DR: The results indicate that clear-cutting and/or soil treatment significantly increases the mobility of TotHg and MeHg accumulated in forest soil and may thus be an important factor for the total input of Hg to boreal freshwater ecosystems.
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Xylem sap as a pathway for total mercury and methylmercury transport from soils to tree canopy in the boreal forest

TL;DR: In this article, xylem sap concentrations of total Mercury (THg) and MeHg were measured in sap drained from different levels along the boles of freshly cut 100 year old Norway spruce (Picea abies) and Scots pine (Pinus sylvestris).
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Cycling of mercury between water, air, and soil compartments of the environment

TL;DR: In this article, the direction and magnitude of volatilization fluxes associated with transfer processes of Hg in the natural environment are investigated. But the results of the field measurements reported here point to the importance of the natural phenomena of emission or re-emission (i.e., volatilation processes) involving the release of volatile Hg species from lake and soil surfaces into the overlying air, at least under warm weather conditions.