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Sphagnum peat moss is a frequently used growth medium for the cultivation of houseplants and forest plants, is obtained by harvesting peat bogs in the circumboreal area and then distributed across the globe. [65] Peat moss is a crucial substrate for forest plant nursery production, as it significantly enhances the quality and survival of ...
All mires are initially fens when the peat starts to form, and may turn into bogs once the height of the peat layer reaches above the surrounding land. A quagmire is a floating (quaking) mire, bog, or any peatland being in a stage of hydrosere or hydrarch (hydroseral) succession, resulting in pond-filling yields underfoot (floating mats).
Also, agricultural and forestry-drained peat bogs actively release more CO 2 annually than is released in peat energy production in Finland. The average regrowth rate of a single peat bog, however, is indeed slow, from 1,000 up to 5,000 years. Furthermore, it is a common practice to forest used peat bogs instead of giving them a chance to renew ...
The Bog - a putrescent lowland in Saint-Henri, Quebec known for its diverse array of toads and squires; Burns Bog - in British Columbia, the largest domed peat bog in North America; Eagle Hill Bog - A small spaghnum bog on Campobello Island, New Brunswick; Johnville Bog & Forest Park - Sherbrooke, Quebec, a sphagnum bog
Muskeg is approximately synonymous with bog or peatland, and is a standard term in Canada and Alaska. The term became common in these areas because it is of Cree origin; maskek ( ᒪᐢᑫᐠ ) meaning "low-lying marsh".
A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. [1] [2] It is one of the main types of wetland along with marshes, swamps, and bogs. Bogs and fens, both peat-forming ecosystems, are also known as mires. [2] The unique water chemistry of fens is a result of the ground or surface water input.
Lithuania's first peat moss cultivation trial was in 2011, in Aukštumala Moor in Nemunas Delta Regional Park. Researchers from Vilnius Institute of Botany transplanted sections of Sphagnum from a neighbouring degraded raised bog to the exposed peat surface. They found that 94% of the patches survived and expanded to the exposed peat.
[10] [11] This peat accumulation often forms a convex shape called a dome, which could rise up to 4 m (13 ft) on coastal peat and up to 18 m (59 ft) on inland peat. [1] At the beginning of its formation, peat is largely topogenous or minerotrophic, receiving high nutrient input from rivers or groundwaters .