2 edition of Geochemistry of selected Maine peat deposits found in the catalog.
Geochemistry of selected Maine peat deposits
Stephen A. Norton
Includes bibliographical references (p. 38-39).
|Statement||by Stephen A. Norton.|
|Series||Bulletin / Maine Geological Survey ;, 34, Bulletin (Maine Geological Survey) ;, 34.|
|LC Classifications||QE119 .A3 no. 34, TN840.U5 .A3 no. 34|
|The Physical Object|
|Pagination||iv, 39 p. :|
|Number of Pages||39|
|LC Control Number||91623111|
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Geochemistry of selected Maine peat deposits. Augusta, Me.: Maine Geological Survey, Dept. of Conservation, (OCoLC) Material Type: Government publication, State or province government publication: Document Type: Book: All Authors / Contributors: Stephen A Norton.
Norton SA () Geochemistry of selected Maine peat deposits. Bull Maine Geol Surv –39 Google Scholar Norton SA, Evans GC, Kahl JS () Comparison of Hg and Pb fluxes to hummocks and hollows of ombrotrophic Big Heath Bog and to nearby Sargent Mt.
Pond, Maine, by: 8. Four basic types of peat and stages of peat deposits formation in the Holocene are distinguished: the organomineral layer of the sediments in a paleolake (up Geochemistry of selected Maine peat deposits book ± 60 years ago), the low moor. Peat accumulation rates in selected Maine peat deposits.
Kimmo Tolonen, Ronald B. Davis, and Lissa S. Widoff. Maine Geological Survey, Bulletin Study of peat accumulation rates in Geochemistry of selected Maine peat deposits book deposits. Includes comparative diagrams and tables of accumulation rates, pollen diagrams, moss increment and radio-carbon dates, and decomposition studies.
Cornelia Clermont Cameron (–) was an American geologist who researched peat as a soil additive and energy source. She was born inand was the daughter of two scientist.
Her mother, Harriet Clearman Cameron, had a masters in Geology and a Ph.D in mater: University of Iowa. Dating recent peat deposits (i.e., past } yrs of peat accumulation) has emerged as an important yet challenging task for estimating rates of organic matter accumulation and atmospheric pollutant deposition in peatlands.
Due to their ombrotrophic nature and the tendency for Sphagnum-derived peat to have high cation exchange capacity, peatlands are ideal archives of atmospheric Cited by: Geochemistry of the peat bog at Etang de la Gruère, Jura Mountains, Switzerland, and its record of atmospheric Pb and lithogenic trace metals (Sc, Ti, Y, Zr, and REE) si 14C yr BP.
The Geochemistry of selected Maine peat deposits book suites are more oxidized and hydrous and are selected from representative causative I-type intrusions from porphyry and high-sulfidation epithermal Cu-Au deposits (Batu Hijau, Indonesia, and Tampakan, Philippines), porphyry Cu-Mo-Au deposits (Sar Cheshmeh, Iran; Dexing, eastern China; and Jiama, southern Tibet), porphyry Cu-Mo.
ELEMENT CONCENTRATIONS IN SOILS AND OTHER SURFICIAL MATERIALS OF THE CONTERMINOUS UNITED STATES By HANSFORD T. SHACKLETTE and JOSEPHINE G. BOERNGEN ABSTRACT Samples of soils or other regoliths, taken at a depth of approxi- mately 20 cm from locations about 80 km apart throughout the conter.
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His peer-reviewed publications on the use of spectroscopy include: quantifying biochemical content in leaf spectra, discriminating conifer species, examining post-fire surface cover, and characterizing the impact of oil.
Education: B.A., Geography, University of Colorado, M.S., Geology, Colorado State University, About Me: I began my career at the USGS in with research focusing on fluvial geomorphology and sedimentology of anastomosing river channels; wetland hydrology; surficial uranium deposits; and the geology and geochemistry of radon in rocks and soils.
This banner text can have markup. web; books; video; audio; software; images; Toggle navigation. To examine if IHSS activities were in accordance with its motto “bring together scientists in the coal, soil, and water sciences with interests in humic substances”, we classified the communications presented on organic matter, between the (7th) and (13th) IHSS international conferences into the following scientific domains: general studies on natural organic matter (NOM) (e.g Cited by: Coal begins as peat, which consists of loosely consolidated layers of various mixtures of plant and mineral matter.
Peat accumulates in wetlands called "peat swamps," "bogs," or "mires." In this report, the term "peat swamp" is used to indicate a peat-forming wetland.
Figure 6 is a photograph of the Okefenokee Swamp, which is a modern. Dating recent peat deposits (i.e., past ∼ yrs of peat accumulation) has emerged as an important yet challenging task for estimating rates of organic matter accumulation and atmospheric pollutant deposition in peatlands.
Due to their ombrotrophic nature and the tendency for Sphagnum-derived peat to have high cation exchange capacity, peatlands are ideal archives of atmospheric pollution Cited by: Organic petrology developed as coal petrology at the beginning of the 20th century dedicated mainly to the study of coals because of their utilization Cited by: Geochemistry of selected oil and source rock samples from Cambrian and Ordovician strata, Ohio-West Virginia-Tennessee part of the Appalachian Basin,Open-File Report Hydrology of the Texas Gulf Coast aquifer systems,Open-File Report Peatlands play a key role in the global carbon cycle, sequestering and releasing large amounts of carbon.
Despite their importance, a reliable method for the quantification of peatland thickness and volume is still missing, particularly for peat deposits located in the tropics given their limited accessibility, and for scales of measurement representative of peatland environments (i.e., of Cited by: 2.
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() Zirconium bearing minerals from. High rates of peat accretion were reported of about 1 mm yr −1 for a coastal mangrove peatland in Belize, Central America [Wooller et al., ], – mm yr −1 for a coastal peat dome in Panama [Phillips and Bustin, ] and mm yr −1 for peatlands on the Orinioco River Delta of Venezuela, South America [Aslan et al., Cited by: Recent Publications - Geomorphology, Soil Genesis, and Classification.
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past’ elevation of’ intertidal’ marshes’ as’ they’ formed’ on stable’ Pleistocene’ basement.’ Peat’ deposits’ were’ collected from’ a’ range’ of’ depths’ by’ sediment’ coring’ and were’ radiocarbon.
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