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Biogeochemistry of a Forested Ecosystem
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In this article, Biogeochemistry of a forested ecosystem, Biogeochemical properties of forested ecosystems, and biogeochemistry in forested environments, the authors present a biogeochemical model of forest ecosystems.Abstract:
Biogeochemistry of a forested ecosystem , Biogeochemistry of a forested ecosystem , مرکز فناوری اطلاعات و اطلاع رسانی کشاورزیread more
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The Biogeochemical Cycle of Silicon in Two Temperate Forest Ecosystems
TL;DR: The biogeochemical cycle of silicon was modelled in two temperate forested ecosystems with the help of four natural reservoirs: vegetation, soil organic matter, soil minerals and soil solutions as mentioned in this paper.
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Canopy processing of acidic precipitation by coniferous and hardwood forests in New England.
TL;DR: Results from comparative throughfall chemistry studies in New Hampshire indicate that northern hardwood canopies produce a throughfall solution chemistry that is less acid and higher in basic cations than either direct precipitation or throughfall solutions derived from nearby subalpine balsam fir forests.
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Microbial consumption of nitric and sulfuric acids in acidified north temperate lakes1
John W. M. Rudd,Carol A. Kelly,Vincent L. St. Louis,Raymond H. Hesslein,Akira Furutani,M. H. Holoka +5 more
TL;DR: In this article, rates of sulfate reduction and denitrification were measured in the sediments of unacidified, experimentally acidified, and atmospherically acidified lakes in North America and Norway.
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Retention and release of S from A freshwater wetland
TL;DR: A freshwater wetland at the Experimental Lakes Area in northwestern Ontario stored most of the SO42− received annually from precipitation, runoff and experimental additions as discussed by the authors, and the S budget was determined for a small fen spray irrigated with H2SO4 and HNO3.
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Concentration and flux of solutes from snow and forest floor during snowmelt in the West-Central Adirondack region of New York
TL;DR: In this article, the authors evaluated solute concentrations in snowpack, and in meltwater collected from snow and forest floor lysimeters in the west-central Adirondack Mountains of New York during the spring snowmelt period, 29 March through 15 April 1984.