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  1. Article: Effect of biogas generation on radon emissions from landfills receiving radium-bearing waste from shale gas development.

    Walter, Gary R / Benke, Roland R / Pickett, David A

    Journal of the Air & Waste Management Association (1995)

    2012  Volume 62, Issue 9, Page(s) 1040–1049

    Abstract: Unlabelled: Dramatic increases in the development of oil and natural gas from shale formations will result in large quantities of drill cuttings, flowback water, and produced water. These organic-rich shale gas formations often contain elevated ... ...

    Abstract Unlabelled: Dramatic increases in the development of oil and natural gas from shale formations will result in large quantities of drill cuttings, flowback water, and produced water. These organic-rich shale gas formations often contain elevated concentrations of naturally occurring radioactive materials (NORM), such as uranium, thorium, and radium. Production of oil and gas from these formations will also lead to the development of technologically enhanced NORM (TENORM) in production equipment. Disposal of these potentially radium-bearing materials in municipal solid waste (MSW) landfills could release radon to the atmosphere. Risk analyses of disposal of radium-bearing TENORM in MSW landfills sponsored by the Department of Energy did not consider the effect of landfill gas (LFG) generation or LFG control systems on radon emissions. Simulation of radon emissions from landfills with LFG generation indicates that LFG generation can significantly increase radon emissions relative to emissions without LFG generation, where the radon emissions are largely controlled by vapor-phase diffusion. Although the operation of LFG control systems at landfills with radon source materials can result in point-source atmospheric radon plumes, the LFG control systems tend to reduce overall radon emissions by reducing advective gas flow through the landfill surface, and increasing the radon residence time in the subsurface, thus allowing more time for radon to decay. In some of the disposal scenarios considered, the radon flux from the landfill and off-site atmospheric activities exceed levels that would be allowed for radon emissions from uranium mill tailings.
    Implications: Increased development of hydrocarbons from organic-rich shale formations has raised public concern that wastes from these activities containing naturally occurring radioactive materials, particularly radium, may be disposed in municipal solid waste landfills and endanger public health by releasing radon to the atmosphere. This paper analyses the processes by which radon may be emitted from a landfill to the atmosphere. The analyses indicate that landfill gas generation can significantly increase radon emissions, but that the actual level of radon emissions depend on the place of the waste, construction of the landfill cover, and nature of the landfill gas control system.
    MeSH term(s) Biofuels ; Computer Simulation ; Extraction and Processing Industry ; Industrial Waste/analysis ; Models, Chemical ; Radon/analysis ; Waste Management
    Chemical Substances Biofuels ; Industrial Waste ; Radon (Q74S4N8N1G)
    Language English
    Publishing date 2012-09-26
    Publishing country United States
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ZDB-ID 1003064-5
    ISSN 1096-2247 ; 0894-0630 ; 1047-3289
    ISSN 1096-2247 ; 0894-0630 ; 1047-3289
    DOI 10.1080/10962247.2012.696084
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  2. Book ; Online: Ages and stable isotope ratios from speleothem calcite from Cold Water Cave, Iowa, supplementary data to: Dorale, Jeffrey A; Gonz?lez, Luis A; Reagan, Mark K; Pickett, David A; Murrell, Michael T; Baker, Richard G (1992): A high-resolution record of Holocene climate change in speleothem calcite from Cold Water Cave, Northeast Iowa. Science, 258, 1626-1630

    Dorale, Jeffrey A / Baker, Richard G / Gonz?lez, Luis A / Murrell, Michael T / Pickett, David A / Reagan, Mark K

    2008  

    Abstract: High-precision uranium-thorium mass spectrometric chronology and 18O-13C isotopic analysis of speleothem calcite from Cold Water Cave in northeast Iowa have been used to chart mid-Holocene climate change. Significant shifts in d18O and d13C isotopic ... ...

    Abstract High-precision uranium-thorium mass spectrometric chronology and 18O-13C isotopic analysis of speleothem calcite from Cold Water Cave in northeast Iowa have been used to chart mid-Holocene climate change. Significant shifts in d18O and d13C isotopic values coincide with well-documented Holocene vegetation changes. Temperature estimates based on 18O/16O ratios suggest that the climate warmed rapidly by about 3?C at 5900 years before present and then cooled by 4?C at 3600 years before present. Initiation of a gradual increase in ?d13C at 5900 years before present suggests that turnover of the forest soil biomass was slow and that equilibrium with prairie vegetation was not attained by 3600 years before present.
    Language English
    Dates of publication 2008-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    Note This dataset is supplement to doi:10.1126/science.258.5088.1626
    DOI 10.1594/PANGAEA.707291
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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