Search Results - Peat, I. M.~

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    Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations by Helena Stewart, Tom Bradwell, Joanna Bullard, Robert D. McCulloch, Ian Millar

    Published 2022
    “…Marked peaks in increased minerogenic dust deposition at: c. 5.4-5.1 ka BP, c. 4.0-3.9 ka BP, c. 2.8-2.6 ka BP, c. 1.0 ka BP and c. 0.3 ka BP occur against a backdrop of low dust deposition during the mid-Holocene (c. 5.04.0 ka BP) and increased background levels of dust during the neoglacial period (…”
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    Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations by Helena Stewart, Tom Bradwell, Joanna Bullard, Robert D. McCulloch, Ian Millar

    Published 2023
    “…Marked peaks in increased minerogenic dust deposition at: c. 5.45.1, 4.03.9, 2.82.6, 1.0 and 0.3 ka BP occur against a backdrop of low dust deposition during the mid-Holocene (c. 5.04.0 ka BP) and increased background levels of dust during the neoglacial period (…”
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    Adsorption of heavy metals in slow sand filters by Nur Muhammad, Jeremy Parr, Michael D. Smith, Andrew D. Wheatley

    Published 1998
    “…Activated carbon is very effective in removing heavy metals, but is readily soluble under extreme pH conditions (Huang and Blankenship, 1989). Peat moss has been found as very effective in adsorbing heavy metals (Ho, 1995). …”
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    Determining patterns in the composition of dissolved organic matter in fresh waters according to land use and management by Christopher A. Yates., Penny J. Johnes, Francesca L. Brailsford, Christopher D. Evans, Richard P. Evershed, Helen Glanville, Davey L. Jones, Charlotte E. M. Lloyd, Miles R. Marshall, Alun T. Owen

    Published 2022
    “…DOM composition was assessed through organic matter stoichiometry (organic carbon: organic nitrogen; organic carbon: organic phosphorus; C/N(P)DOM) and metrics derived from ultra-violet (UV)/visible spectroscopic analysis of DOM such as specific UV absorption (a254 nm; SUVA254). …”
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    Reconstructing the Holocene coastal development of the Laurentine Shore by Andrew R. Bicket

    Published 2009
    “…A sea level reconstruction based on multi-proxy palaeo-environmental analysis of a silt/peat sedimentary transition from the base of a Roman piscina suggests that the sea level at ca. 2400 ± 40 BP was around 1.25 ± 0.2 m below modern sea level. …”
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