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159 related items for PubMed ID: 16203082

  • 1. Dissolution of a multicomponent DNAPL pool in an experimental aquifer.
    Lee KY, Chrysikopoulos CV.
    J Hazard Mater; 2006 Feb 06; 128(2-3):218-26. PubMed ID: 16203082
    [Abstract] [Full Text] [Related]

  • 2. Laboratory evidence of natural remobilization of multicomponent DNAPL pools due to dissolution.
    Roy JW, Smith JE, Gillham RW.
    J Contam Hydrol; 2004 Oct 06; 74(1-4):145-61. PubMed ID: 15358491
    [Abstract] [Full Text] [Related]

  • 3. A controlled field experiment on groundwater contamination by a multicomponent DNAPL: dissolved-plume retardation.
    Rivett MO, Allen-King RM.
    J Contam Hydrol; 2003 Oct 06; 66(1-2):117-46. PubMed ID: 14516944
    [Abstract] [Full Text] [Related]

  • 4. Natural remobilization of multicomponent DNAPL pools due to dissolution.
    Roy JW, Smith JE, Gillham RW.
    J Contam Hydrol; 2002 Dec 06; 59(3-4):163-86. PubMed ID: 12487412
    [Abstract] [Full Text] [Related]

  • 5. Solvent release into a sandy aquifer. 2. Estimation of DNAPL mass based on a multiple-component dissolution model.
    Broholm K, Feenstra S, Cherry JA.
    Environ Sci Technol; 2005 Jan 01; 39(1):317-24. PubMed ID: 15667112
    [Abstract] [Full Text] [Related]

  • 6. Variations in expression of carbon isotope fractionation of chlorinated ethenes during biologically enhanced PCE dissolution close to a source zone.
    Morrill PL, Sleep BE, Seepersad DJ, McMaster ML, Hood ED, LeBron C, Major DW, Edwards EA, Lollar BS.
    J Contam Hydrol; 2009 Nov 03; 110(1-2):60-71. PubMed ID: 19818530
    [Abstract] [Full Text] [Related]

  • 7. Influence of mass transfer characteristics for DNAPL source depletion and contaminant flux in a highly characterized glaciofluvial aquifer.
    Maji R, Sudicky EA.
    J Contam Hydrol; 2008 Nov 14; 102(1-2):105-19. PubMed ID: 18929427
    [Abstract] [Full Text] [Related]

  • 8. Effect of source variability and transport processes on carbon isotope ratios of TCE and PCE in two sandy aquifers.
    Hunkeler D, Chollet N, Pittet X, Aravena R, Cherry JA, Parker BL.
    J Contam Hydrol; 2004 Oct 14; 74(1-4):265-82. PubMed ID: 15358496
    [Abstract] [Full Text] [Related]

  • 9. The significance of heterogeneity on mass flux from DNAPL source zones: an experimental investigation.
    Page JW, Soga K, Illangasekare T.
    J Contam Hydrol; 2007 Dec 07; 94(3-4):215-34. PubMed ID: 17706832
    [Abstract] [Full Text] [Related]

  • 10. PCE dissolution and simultaneous dechlorination by nanoscale zero-valent iron particles in a DNAPL source zone.
    Fagerlund F, Illangasekare TH, Phenrat T, Kim HJ, Lowry GV.
    J Contam Hydrol; 2012 Apr 01; 131(1-4):9-28. PubMed ID: 22326687
    [Abstract] [Full Text] [Related]

  • 11. Intermediate-scale 2D experimental investigation of in situ chemical oxidation using potassium permanganate for remediation of complex DNAPL source zones.
    Heiderscheidt JL, Siegrist RL, Illangasekare TH.
    J Contam Hydrol; 2008 Nov 14; 102(1-2):3-16. PubMed ID: 18774622
    [Abstract] [Full Text] [Related]

  • 12. Effectiveness of nanoscale zero-valent iron for treatment of a PCE-DNAPL source zone.
    Taghavy A, Costanza J, Pennell KD, Abriola LM.
    J Contam Hydrol; 2010 Nov 25; 118(3-4):128-42. PubMed ID: 20888664
    [Abstract] [Full Text] [Related]

  • 13. Modeling field-scale cosolvent flooding for DNAPL source zone remediation.
    Liang H, Falta RW.
    J Contam Hydrol; 2008 Feb 19; 96(1-4):1-16. PubMed ID: 17988760
    [Abstract] [Full Text] [Related]

  • 14. Effects of biomass accumulation on microbially enhanced dissolution of a PCE pool: a numerical simulation.
    Chu M, Kitanidis PK, McCarty PL.
    J Contam Hydrol; 2003 Aug 19; 65(1-2):79-100. PubMed ID: 12855202
    [Abstract] [Full Text] [Related]

  • 15. Bioaugmentation for treatment of dense non-aqueous phase liquid in fractured sandstone blocks.
    Schaefer CE, Towne RM, Vainberg S, McCray JE, Steffan RJ.
    Environ Sci Technol; 2010 Jul 01; 44(13):4958-64. PubMed ID: 20524648
    [Abstract] [Full Text] [Related]

  • 16. Two-dimensional DNAPL migration affected by groundwater flow in unconfined aquifer.
    Kamon M, Endo K, Kawabata J, Inui T, Katsumi T.
    J Hazard Mater; 2004 Jul 05; 110(1-3):1-12. PubMed ID: 15177722
    [Abstract] [Full Text] [Related]

  • 17. Assessing the impacts of partial mass depletion in DNAPL source zones I. Analytical modeling of source strength functions and plume response.
    Falta RW, Suresh Rao P, Basu N.
    J Contam Hydrol; 2005 Aug 05; 78(4):259-80. PubMed ID: 16019108
    [Abstract] [Full Text] [Related]

  • 18. Plume persistence caused by back diffusion from thin clay layers in a sand aquifer following TCE source-zone hydraulic isolation.
    Parker BL, Chapman SW, Guilbeault MA.
    J Contam Hydrol; 2008 Nov 14; 102(1-2):86-104. PubMed ID: 18775583
    [Abstract] [Full Text] [Related]

  • 19. Characterisation of a DNAPL source zone in a porous aquifer using the Partitioning Interwell Tracer Test and an inverse modelling approach.
    Dridi L, Pollet I, Razakarisoa O, Schäfer G.
    J Contam Hydrol; 2009 Jun 26; 107(1-2):22-44. PubMed ID: 19395120
    [Abstract] [Full Text] [Related]

  • 20. Dip-angle influence on areal DNAPL recovery by co-solvent flooding with and without pre-flooding.
    Boyd GR, Li M, Husserl J, Ocampo-Gómez AM.
    J Contam Hydrol; 2006 Jan 10; 82(3-4):319-37. PubMed ID: 16303209
    [Abstract] [Full Text] [Related]

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