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  2. Peat - Wikipedia

    en.wikipedia.org/wiki/Peat

    Peat forms when plant material does not fully decay in acidic and anaerobic conditions. It is composed mainly of wetland vegetation: principally bog plants including mosses, sedges and shrubs. As it accumulates, the peat holds water. This slowly creates wetter conditions that allow the area of wetland to expand.

  3. Soil acidification - Wikipedia

    en.wikipedia.org/wiki/Soil_acidification

    Impacts of acidic water and Soil acidification on plants could be minor or in most cases major. In minor cases which do not result in fatality of plant life include; less-sensitive plants to acidic conditions and or less potent acid rain. Also in minor cases the plant will eventually die due to the acidic water lowering the plants natural pH.

  4. Bog - Wikipedia

    en.wikipedia.org/wiki/Bog

    [2] [3] They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink. [4] [5] Bogs occur where the water at the ground surface is acidic and low in nutrients. A bog usually is found at a freshwater soft spongy ground that is made up ...

  5. Sphagnum - Wikipedia

    en.wikipedia.org/wiki/Sphagnum

    Sphagnum is a genus of approximately 380 accepted species [2] [3] of mosses, commonly known as sphagnum moss, also bog moss and quacker moss (although that term is also sometimes used for peat). Accumulations of Sphagnum can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16 ...

  6. Raised bog - Wikipedia

    en.wikipedia.org/wiki/Raised_bog

    Larger accumulations of water in the middle of the bogs are called kolks or bog ponds (of humic acid-rich water); the wet area on the outer margins is known as a moat or lagg. Genuine ombrotrophic bogs on the North German Plain are usually sharply divided into two layers: an underlying black peat layer, which is strongly decomposed, and an ...

  7. Ombrotrophic - Wikipedia

    en.wikipedia.org/wiki/Ombrotrophic

    This deficiency is a key characteristic of these ecosystems. However, while ombrotrophic peat decomposes slowly, some nutrient release does occur. For example, microelements like zinc (Zn), copper (Cu), and manganese (Mn) are easily mobilized. Additionally, the presence of more nutrient-demanding species in drainage channels draining ...

  8. Aulacomnium palustre - Wikipedia

    en.wikipedia.org/wiki/Aulacomnium_palustre

    The pH of water, peat, and/or soil is usually acidic to neutral in mires with ribbed bog moss, although ribbed bog moss tolerates mildly alkaline conditions. For example, ribbed bog moss grows in extremely acidic peatlands overlying permafrost in spruce taiga of Alaska but also grows in calcareous bogs in Birds Hill Provincial Park.

  9. Sphagnum fuscum - Wikipedia

    en.wikipedia.org/wiki/Sphagnum_fuscum

    S. fuscum grows in areas with high sulphur and nitrogen depositions, which is concomitant with the decreased pH of the soil. [6] Sphagnum has also been used historically for medicinal purposes. The moss itself has antimicrobial properties, and was therefore used as an effective filler for wounds to prevent infection.

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