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Коломыцев В.А.
Потенциал заболачивания таежных ландшафтов
// Болотные экосистемы севера Европы: разнообразие, динамика,
углеродный баланс, ресурсы и охрана. Материалы международного симпозиума (Петрозаводск, 30 августа – 2 сентября 2005 г.). Петрозаводск: КарНЦ РАН, 2006. C. 121-129
V.A. Kolomytsev. Роtеntial of paludification in taiga landscapes of Karelia // Mire Ecosystems in Northern Europe: Diversity, Dynamics, Carbon Balance, Resources and Conservation. Proceedings of International Symposium (Petrozavodsk: August 30 – September 2, 2005). Petrozavodsk, 2006. Pp. 121-129
The potential of paludification is one of the most important indexes of
that process. It is determinated by mean slope weight value of paludified forests
and mires. The potential of paludification depends on the landscape relief morphogenesis. It intensifies with increasing of mean slope weight value of paludification surfaces. The obtained data testify the process of paludification in the north taiga sub–zone and decreasing of its activity in the mid–taiga subzone. It becomes apparent strongly in landscapes with hilly ridge relief. The potential of paludification of denudation–tectonic landscapes in the north taiga sub–zone 3–4 times as large than in the mid–taiga sub–zone but there is no difference in landscapes with plain relief.
that process. It is determinated by mean slope weight value of paludified forests
and mires. The potential of paludification depends on the landscape relief morphogenesis. It intensifies with increasing of mean slope weight value of paludification surfaces. The obtained data testify the process of paludification in the north taiga sub–zone and decreasing of its activity in the mid–taiga subzone. It becomes apparent strongly in landscapes with hilly ridge relief. The potential of paludification of denudation–tectonic landscapes in the north taiga sub–zone 3–4 times as large than in the mid–taiga sub–zone but there is no difference in landscapes with plain relief.
Last modified: January 11, 2007