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  • 2000-2004  (7)
Medientyp
Sprache
Erscheinungszeitraum
  • 2000-2004  (7)
Jahr
Fachgebiete(RVK)
  • 1
    In: Vadose Zone Journal, Wiley, Vol. 3, No. 4 ( 2004-11), p. 1309-1321
    Kurzfassung: Mobile–immobile models (MIM) have rarely been used for inverse simulation of measurements of variably saturated water flow and contaminant transport. We evaluated two MIM approaches with water transfer across the mobile and immobile regions either based on relative saturation (Se) differences, MIM(Se), or pressure head ( h ) differences, MIM( h ), for inverse simulation of transient water flow and Br − transport in aggregated soil. Six undisturbed Ap soil columns (14.7‐cm length and diameter) at wet, medium, and dry initial water contents were subjected to application of 0.005 L Br − solution of 1000 mg L −1 and subsequent irrigation of 1 cm h −1 for 3 h. Two similar irrigations were applied after 7 and 14 d. Measurements comprised pressure heads at depths of 2.8 and 12.8 cm, average soil column water contents, outflow, and effluent solute concentrations. This experimental information was used for simultaneous optimization of van Genuchten soil hydraulic parameters for mobile and immobile regions, the dispersivity, and the first‐order rate coefficients for water and solute transfer. In total, eight parameters were estimated for MIM(Se) and 10 parameters for MIM( h ). The inverse MIM approaches described the various hydraulic and transport data adequately. Physical nonequilibrium was more pronounced for wet and dry than for intermediate initial moisture, while initial moisture had no obvious effect on the total Br − lost. For wet and dry initial conditions, parameter estimates seemed fairly reliable, with the exception of the highly correlated saturated water contents in mobile and immobile regions. MIM( h ) yielded parameters that appeared physically more consistent with observations, but required smaller time steps than MIM(Se) to overcome oscillations of pressure heads. Both MIM approaches were found to be suitable for inverse simulation of physical nonequilibrium transport during variably saturated flow.
    Materialart: Online-Ressource
    ISSN: 1539-1663 , 1539-1663
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2004
    ZDB Id: 2088189-7
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 2002
    In:  Water Resources Research Vol. 38, No. 7 ( 2002-07), p. 26-1-26-11
    In: Water Resources Research, American Geophysical Union (AGU), Vol. 38, No. 7 ( 2002-07), p. 26-1-26-11
    Materialart: Online-Ressource
    ISSN: 0043-1397
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2002
    ZDB Id: 2029553-4
    ZDB Id: 5564-5
    SSG: 13
    SSG: 14
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    Wiley ; 2002
    In:  Soil Science Society of America Journal Vol. 66, No. 5 ( 2002-09), p. 1430-1438
    In: Soil Science Society of America Journal, Wiley, Vol. 66, No. 5 ( 2002-09), p. 1430-1438
    Kurzfassung: Dual‐permeability model simulations and sensitivity studies indicate that preferential solute leaching in structured soil is intensified by a limited solute mass transfer between preferential flow paths and matrix. It is currently unknown how much aggregate skins may affect solute mass transfer. The objective of this study was to evaluate the effect of a skin layer on the effective diffusion coefficient, D e , of water saturated soil aggregates. In a diffusion experiment, the concentration decrease of Br − and Cl − in a solution being in contact with soil aggregates was measured. Aggregates with intact and removed surface skins were studied. Two different theoretical approaches were compared: (i) fitting a modified analytical solution of Crank for diffusion out of a solution of limited volume into a plane sheet to obtain D e for intact and for skin‐removed aggregates; and (ii) calibrating a numerical solution for diffusion through a two‐layer system to estimate D e of the skin layer and the interior part, separately. The D e ‐values of the skins differed for Br − and Cl − Using the first approach, D e was six (Br − ) and 15 (Cl − ) times smaller for the intact than for the skin‐removed aggregates. The second approach resulted in effective diffusion coefficients of the skin layer being 30 (Br − ) and 45 (Cl − ) times smaller than those of the interior parts. Aggregate skins may reduce diffusive anion transfer between interaggregate region and soil matrix, an effect which may significantly influence preferential solute transport in structured soil.
    Materialart: Online-Ressource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2002
    ZDB Id: 241415-6
    ZDB Id: 2239747-4
    ZDB Id: 196788-5
    ZDB Id: 1481691-X
    SSG: 13
    SSG: 21
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2004
    In:  Journal of Hydrology Vol. 289, No. 1-4 ( 2004-4), p. 239-257
    In: Journal of Hydrology, Elsevier BV, Vol. 289, No. 1-4 ( 2004-4), p. 239-257
    Materialart: Online-Ressource
    ISSN: 0022-1694
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2004
    ZDB Id: 240687-1
    ZDB Id: 1473173-3
    SSG: 13
    SSG: 14
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 5
    Online-Ressource
    Online-Ressource
    Wiley ; 2002
    In:  Soil Science Society of America Journal Vol. 66, No. 1 ( 2002), p. 26-
    In: Soil Science Society of America Journal, Wiley, Vol. 66, No. 1 ( 2002), p. 26-
    Materialart: Online-Ressource
    ISSN: 1435-0661
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2002
    ZDB Id: 241415-6
    ZDB Id: 196788-5
    ZDB Id: 1481691-X
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 6
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 2004
    In:  Water Resources Research Vol. 40, No. 7 ( 2004-07)
    In: Water Resources Research, American Geophysical Union (AGU), Vol. 40, No. 7 ( 2004-07)
    Kurzfassung: Dual‐permeability models contain a lumped mass transfer term that couples equations for water flow in the soil matrix and fracture systems. Linear first‐order transfer terms cannot accurately calculate water transfer between the domains during early times of pressure head nonequilibrium. In this study, a second‐order equation for water transfer into spherical rock matrix blocks [ Zimmerman et al. , 1993 , 1996 ] was adapted and evaluated comprehensively for water transfer into and out of variably saturated soil matrix blocks of different hydraulic properties, geometries, and sizes, for different initial and boundary conditions. Numerical solutions of the second‐order term were compared with respective results obtained with a first‐order term and a one‐dimensional horizontal flow equation. Accurate results were obtained after implementing two modifications in the second‐order term. First, the hydraulic conductivity was calculated as a weighted arithmetic average of conductivities that used pressure heads in matrix and fracture. For a time‐variable pressure head boundary condition, a fixed weighting factor of 17 could be applied irrespective of texture, initial condition, and matrix block size up to 10 cm. Second, if direction of water transfer changed (to or from matrix), the initial pressure head was reset to the equilibrium pressure head at the time of transfer reversal. The modified second‐order term was implemented into a dual‐permeability model, which closely approximated reference results obtained with a two‐dimensional flow model. For rectangular slab‐type or comparable geometry of soil matrix, the modified second‐order term considerably improves the accuracy of dual‐permeability models to simulate variably saturated preferential flow in soil.
    Materialart: Online-Ressource
    ISSN: 0043-1397 , 1944-7973
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2004
    ZDB Id: 2029553-4
    ZDB Id: 5564-5
    SSG: 13
    SSG: 14
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 7
    Online-Ressource
    Online-Ressource
    Wiley ; 2002
    In:  Soil Science Society of America Journal Vol. 66, No. 1 ( 2002-01), p. 26-36
    In: Soil Science Society of America Journal, Wiley, Vol. 66, No. 1 ( 2002-01), p. 26-36
    Kurzfassung: Skins of soil aggregates often consist of clayey or clay‐organic coatings which may affect preferential flow in aggregated soils. The objective was to determine hydraulic properties of samples with intact and removed (cut) skins and interior/skin hydraulic conductivity ratios for estimating mass transfer parameters in dual‐permeability models. Soil aggregates from the C sd ‐horizon of a clay‐loam glacial till soil (Stagnic Calcaric Regosol) were analyzed. A tension‐imbibition apparatus was used for measuring water uptake of multiple aggregates at boundary matric potential heads of −1 and −5 cm. Sorptivities were used to calculate mean weighted water diffusivities and final water contents to fit wetting retention functions. Water retention and hydraulic conductivity functions for the skin layer were derived from differences in water contents and hydraulic resistances between intact and cut samples. Water absorption rates were generally smaller for intact than for cut aggregates. The water retention function of cut was shifted towards smaller water contents compared with intact samples. Mean water diffusivity of intact was 4.5 times smaller than that of cut samples. The interior/skin ratio in unsaturated hydraulic conductivity was about 12 in the measured matric potential head range. The ratio was up to 70 near water saturation and dropped below unity for soil water potentials smaller −1000 cm of water. Aggregate skins may be regarded as a separate porous domain whose hydraulic properties may control water transfer between inter‐ and intraaggregate pore domains in structured soils.
    Materialart: Online-Ressource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2002
    ZDB Id: 241415-6
    ZDB Id: 2239747-4
    ZDB Id: 196788-5
    ZDB Id: 1481691-X
    SSG: 13
    SSG: 21
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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