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178 related items for PubMed ID: 15358491

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

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

  • 3. 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]

  • 4. 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]

  • 5. 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]

  • 6. Dissolution of dense non-aqueous phase liquids in vertical fractures: effect of finger residuals and dead-end pools.
    Yang Z, Niemi A, Fagerlund F, Illangasekare T, Detwiler RL.
    J Contam Hydrol; 2013 Jun 05; 149():88-99. PubMed ID: 23608741
    [Abstract] [Full Text] [Related]

  • 7. 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]

  • 8. Removal of DNAPL contamination from the saturated zone by the combined effect of vertical upward flushing and density reduction.
    Hofstee C, Gutiérrez Ziegler C, Trötschler O, Braun J.
    J Contam Hydrol; 2003 Dec 07; 67(1-4):61-78. PubMed ID: 14607470
    [Abstract] [Full Text] [Related]

  • 9. 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]

  • 10. Field study of TCE diffusion profiles below DNAPL to assess aquitard integrity.
    Parker BL, Cherry JA, Chapman SW.
    J Contam Hydrol; 2004 Oct 14; 74(1-4):197-230. PubMed ID: 15358493
    [Abstract] [Full Text] [Related]

  • 11. Laboratory investigation of flux reduction from dense non-aqueous phase liquid (DNAPL) partial source zone remediation by enhanced dissolution.
    Kaye AJ, Cho J, Basu NB, Chen X, Annable MD, Jawitz JW.
    J Contam Hydrol; 2008 Nov 14; 102(1-2):17-28. PubMed ID: 18420303
    [Abstract] [Full Text] [Related]

  • 12. Long-term ground penetrating radar monitoring of a small volume DNAPL release in a natural groundwater flow field.
    Hwang YK, Endres AL, Piggott SD, Parker BL.
    J Contam Hydrol; 2008 Apr 04; 97(1-2):1-12. PubMed ID: 18258330
    [Abstract] [Full Text] [Related]

  • 13. Relative contribution of DNAPL dissolution and matrix diffusion to the long-term persistence of chlorinated solvent source zones.
    Seyedabbasi MA, Newell CJ, Adamson DT, Sale TC.
    J Contam Hydrol; 2012 Jun 04; 134-135():69-81. PubMed ID: 22591740
    [Abstract] [Full Text] [Related]

  • 14. Simulating the evolution of an ethanol and gasoline source zone within the capillary fringe.
    Yu S, Freitas JG, Unger AJ, Barker JF, Chatzis J.
    J Contam Hydrol; 2009 Feb 27; 105(1-2):1-17. PubMed ID: 19110339
    [Abstract] [Full Text] [Related]

  • 15. 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]

  • 16. 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]

  • 17. 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 01; 65(1-2):79-100. PubMed ID: 12855202
    [Abstract] [Full Text] [Related]

  • 18. Multiphase flow and transport caused by spontaneous gas phase growth in the presence of dense non-aqueous phase liquid.
    Roy JW, Smith JE.
    J Contam Hydrol; 2007 Jan 30; 89(3-4):251-69. PubMed ID: 17079051
    [Abstract] [Full Text] [Related]

  • 19. Convergence of DNAPL source strength functions with site age.
    Chen X, Jawitz JW.
    Environ Sci Technol; 2009 Dec 15; 43(24):9374-9. PubMed ID: 19928794
    [Abstract] [Full Text] [Related]

  • 20. Modelling the migration of contaminants through variably saturated dual-porosity, dual-permeability chalk.
    Brouyère S.
    J Contam Hydrol; 2006 Jan 10; 82(3-4):195-219. PubMed ID: 16303208
    [Abstract] [Full Text] [Related]

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