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3 edition of Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity found in the catalog.

Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity

Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity

project summary

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Published by U.S. Environmental Protection Agency, Air and Energy Engineering Research Laboratory in Research Triangle Park, NC .
Written in English

    Subjects:
  • Soil permeability -- Research -- Florida

  • Edition Notes

    Other titlesCorrelation of Florida soil gas permeabilities with grain size, moisture, and porosity
    StatementVern C. Rogers and K.K. Nielson
    ContributionsNielson, K. K, Air and Energy Engineering Research Laboratory
    The Physical Object
    FormatMicroform
    Pagination1 v
    ID Numbers
    Open LibraryOL14717687M

    Landfill Gas Collection and Destruction Systems: Evaluating Toxic Emissions and Potential Health Risk Karnig Ohannessian, Anna Peteranecz,and Thomas Kear Soil grain size and cohesiveness. It is generally much easier to extract contaminants from a permeable sandy soil than froma low permeability clay soil. Organic carbon and clay content   Permeability of soils in Mississippi. USGS Publications Warehouse. O'Hara, Charles G. The permeability of soils in Mississippi was determined and mapped using a geogra+soils+

    A widely used empirical correlation for granular materials that accounts for the spread of grain sizes is the Kozeny–Carmen equation (modified from Bear, ): ρw g (d50)2 n3 K= () μ (1 − n)2 In the above, ρw g/μ is the unit weight/viscosity of water, n is porosity, and d50 is the median grain :// Soil permeabilities greater than in/hr may be considered high, and permeabilities less than in/hr may be considered low in terms of soil-gas transport. Soils with low permeability may generally be considered to have a lower radon potential than more permeable soils with similar radium ://

    Percent oxygen in soil gas. Adjust air flow and blower pressure to achieve at least 5% oxygen in soil gas. Permeability of soil dictates combination of pressure and air flow required to force air into the pore space. Excessive air flow. Reduce air flow until oxygen is between 5% and 15% Naturally occurring contaminant attenuation processes are investigated in a petroleum-hydrocarbon contaminated shallow aquifer, near Bemidji, MN. At this site, the biodegradation of hydrocarbons operates mostly under methanogenic conditions and generates CO₂ and CH₄. The main objectives of this study are to determine whether the full suite of noble gases, including He, Ne, Ar, Kr, and Xe


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Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity Download PDF EPUB FB2

Porosity, f, the volume of void spaces per total sam-ple volume (total porosity completely filled by gas, or partially filled by liquid), can be represented as f = 1 -(V s /V), which is one minus Get this from a library.

Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity: project summary. [Vern C Rogers; K K Nielson; Air and Energy Engineering Research Laboratory.] Correlation of Florida soil-gas permeabilities with grain size, moisture, and porosity [microform]: pro Here they once stood; the tragic end of the Apalachee missions; Residential Radon resistant construction feature selection system [electronic resource]: project summar Conference: Radon transport properties of soil classes for estimating indoor radon entry Radon emanation from the soil depends upon its radium content and mineralogy, porosity, grain size, moisture content, and permeability through host rock and soil (Barnet ).

The high levels of   Introduction. As global exploration of shale gas intensifies there is significant risk associated with the pursuit of shale gas resources that are deeply buried (i.e., Haynesville Formation, Mississippi, USA; Mainland Resource Inc., ) due to diagenetic and metamorphic processes that reduce porosity, alter pore size distributions and reduce :// Field measurements were used to benchmark a simple new predictive correlation between soil has permeability and soil grain size, moisture, and porosity.

The correlation was incorporated with a previous diffusion correlation into the new Radon Emanation and Dwellings (RAETRAD) code, that calculates radon generation and two-dimensional transport   Depth profiles of a sediment grain size, b seismic reflection data (from TAN survey) and interpreted facies, c pore water salinity, d porosity, e methane concentration, f plots of HCO 3 vs.

Cl   An overview was made of dry matter (DM) and quality losses that occur during the ensiling process from the field through the feeding phase. The aim was to review the relevant published literature of the last 15 yr focusing on developments achieved after the publication of the book Silage Science and review discusses the factors affecting DM and quality losses in terms of field The effect of grain size on the hydrodynamics of mudflow surge from a tailings dam-break.

Jing, Xiaofei, Chen, Yulong, Xie, Dan, Williams, David J., Wu, Shangwei, Wang, Wensong and Yin, Tianwei (). The effect of grain size on the hydrodynamics of mudflow surge from a tailings dam-break. Applied Sciences, 9 (12)doi: oEPA United States Environmental Protection Agency Center for Environmental Research Information Cincinnati OH C./ Research and Development EPA//N/ February ORD Publications Announcement April - January The Environmental Protection Agency's Office of Research and Development announces the availability of printed publications on a wide range of ?Dockey=QTTXT.

This book is dedicated to all oil, gas, and petrochemical engineering professionals for wet sand about 50°–60° depending on size, shape, and moisture. Angstrom: A unit of length equal to 10 −10 m.

19 A Archie Correlation: Empirical relationships between the formation resistiv-ity factor, the porosity, the water saturation, and the Hydrocarbon production, gas recovery from shale, CO2 storage and water management have a common scientific underpinning: multiphase flow in porous media.

This book provides a fundamental description of multiphase flow through porous rock, with emphasis on the understanding of displacement processes at the pore, or micron, :// assessment of soil data records from the Florida Soil Characterization Data Retrieval System (University of Florida, ).

Model output includes soil moisture content, nitrogen species concentrations (Figure 3) and the fraction of total nitrogen reaching the aquifer, and mass flux. Root water and nutrient uptake modules are included in Aerial radiometric data can provide an estimate of radon source strength over a region, but the amount of radon that is able to enter a home from the soil is dependent on several local factors, including soil structure, grain size distribution, moisture content, and permeability, as well as type of house construction and its structural ://?Dockey= Annual redistribution of soil moisture suction and soil moisture density beneath two different surface covers and the associated heaves at the Onderstepoort test site near Pretoria, in G.

Aitchison (Ed.), Moisture Equilibria and Moisture Changes in Soils beneath Covered Areas, A Symposium in Print, Butterworths, Sydney, pp. –   Abstract. Environmental Effects of Conservation Practices on Grazing Lands, Special Reference Briefs U.S.

Department of Agriculture, National Agricultural Library. This bibliography is one in a multi-volume set developed by the Water Quality Information Center at the National Agricultural Library in support of the U.S.

Department of Agriculture’s Conservation Effects The moisture content of the soil is particularly important for the workability. Some soils are always easy to work, whereas other soils have strict limitations with regard to the water content. Generally, sandy soils are easier to work than clayey soils and well-textured soils are easier to work than massive soils [32].

Sediment samples were analyzed for Eh and pH using slurries ( vol. with DI water) in the field and for occluded gas concentrations, metal (Ba, Co, Cr, Cu, Fe, Mn, Ni, Pb and Zn) concentrations, moisture content, organic carbon content, and grain size in the Soil erosion results in the removal of important topsoil and, with it, nutrients, C and porosity.

A decline in soil organic matter principally affects soil biological and microbiological properties, but also impacts on soil physical properties because of the link with soil ://. florida geological survey special publication no.

34 florida's ground water quality monitoring program background hydrogeochemistry i 9rdep ga issn special publication no. 34 department letter of transmittali of natural resources olog~i florida An illustration of an open book. Books. An illustration of two cells of a film strip.

Video. An illustration of an audio speaker. Audio. An illustration of a " floppy disk. Software. An illustration of two photographs. Images. An illustration of a heart shape Donate. An illustration of text ellipses. The 10th Annual Meeting and Jubilee celebration will be held at the New Orleans Ernest N.

Morial Convention Center, in walking distance from the historic French Quarter and the Riverwalk. Conference hotels will be adjacent to Convention Center in the Warehouse and Arts Districts. Plan to attend, engage in cutting edge research on porous media, and enjoy one of the most historic cities in ?print=1&view=standard.