The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F11%3A00360220" target="_blank" >RIV/60077344:_____/11:00360220 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1007/s10933-011-9526-9" target="_blank" >http://dx.doi.org/10.1007/s10933-011-9526-9</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10933-011-9526-9" target="_blank" >10.1007/s10933-011-9526-9</a>

Result language
angličtina
Original language name
The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation
Original language description
The sediment record from a 5.3-m core from Sargent Mountain Pond, Maine USA indicates strong co-evolutionary relationships among climate, vegetation, soil development, runoff chemistry, lake processes, diatom community, and water and sediment chemistry.The lake was transformed from a more productive, high P, high pH, low DOC system into an oligotrophic, relatively low P, acidic, humic lake over a period of 16,600 years, a natural trend that continues. In contrast to many human-affected lakes that become increasingly eutrophic, many lakes become more oligotrophic during their history. The precursors for that are: (1) absence of human land-use in watersheds, (2) bedrock lithology and soil with a paucity of soluble Ca-rich minerals, and (3) vegetation that promotes the accumulation of soil organic matter, podzolization, and increased export of metal-DOC complexes, particularly Al.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DA - Hydrology and limnology
OECD FORD branch
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Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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