Indirect estimation of near-saturated hydraulic conductivity from readily available soil information

Geoderma

Volumn 108, Issue 1-2, 2002, Pages 1-17

  Jarvis, N J ^a   Zavattaro, L ^b   Rajkai, K ^c   Reynolds, W D ^d   Olsen, P A ^e   McGechan, M ^f   Mecke, M ^g   Mohanty, B ^h   Leeds Harrison, P B ⁱ   Jacques, D ^j  

^a SWEDISH UNIVERSITY OF AGRICULTURAL SCIENCES   (Sweden)

^b UNIVERSITY OF TURIN   (Italy)

^c INSTITUTE OF EXPERIMENTAL MEDICINE   (Hungary)

^d HARROW RESEARCH AND DEVELOPMENT CENTRE   (Canada)

^e STATOIL   (Norway)

^f SCOTTISH AGRICULTURAL COLLEGE   (United Kingdom)

^g UNIVERSITY OF HELSINKI   (Finland)

^h U S SALINITY LABORATORY   (United States)

ⁱ CRANFIELD UNIVERSITY   (United Kingdom)

^j UNIVERSITY OF LEUVEN   (Belgium)

more..

Author keywords

Effective porosity; Geometric mean particle size; Near saturated hydraulic conductivity; Pedotransfer function; Tension infiltrometer

Indexed keywords

HYDRAULIC CONDUCTIVITY; MACROPORE; PEDOTRANSFER FUNCTION; SOIL PROPERTY; SOIL WATER; SOLUTE TRANSPORT;

EID: 18444399637     PISSN: 00167061     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7061(01)00154-9     Document Type: Article

References (46)

1. Macroporosity to characterize spatial variability of hydraulic conductivity and effects of land management
2. Simple field method for determining unsaturated hydraulic conductivity
3. Moisture release characteristics and porosity of twelve Scottish soil series and their variability
4. Calculation of hydraulic conductivities of soils from texture and organic matter content
5. Soil Physics with Basic
6. Combining laboratory and field measurements to define the hydraulic properties of soil
7. Some steady-state solutions to the unsaturated flow equation with application to evaporation from a water table
8. A dual-porosity model for simulating the preferential movement of water and solutes in structured porous media
9. A multiple-pore-region concept to modeling mass transfer in subsurface media
10. Water retention, porosity, and density of field soils
11. Unsaturated transport processes in undisturbed heterogeneous porous media: I. Inorganic contaminants
12. The MACRO model (Version 3.1)
13. Near-saturated hydraulic conductivity in soils of contrasting texture as measured by tension infiltrometers
14. Measurement and prediction of near-saturated hydraulic conductivity for use in dual-porosity models
15. Permeability calculated from desaturation data
16. Evaluation of a dual-porosity to predict field-scale solute transport in a macroporous soil
17. A consistent set of parametric models for the two-phase flow of immiscible fluids in the subsurface
18. Pedotransfer functions to estimate soil water retention parameters for a modified Brooks-Corey type model
19. Estimating saturated hydraulic conductivity from soil morphology
20. Evaluation of methods for inferring air and water properties of soils from field morphology
21. Estimation of the saturated hydraulic conductivity in clay soils from soil moisture retention data
22. Temporal variation in the hydraulic conductivity of a tilled clay soil as measured by tension infiltrometers
23. Evaluation and development of hydraulic conductivity pedotransfer functions for Australian soil
24. New piecewise continuous hydraulic functions for modeling preferential flow in an intermittent-flood irrigated field
25. Estimation of water retention characteristics from the bulk density and particle size distribution of Swedish soils
26. Estimation of soil water properties
27. Predicting saturated hydraulic conductivity utilizing fractal principles
28. Determination of hydraulic conductivity using a tension infiltrometer
29. Use of contact material in tension infiltrometer measurements
30. Solute transport in undisturbed columns of an aggregated tropical soil: Preferential flow effects
31. A unifying quantitative analysis of soil texture
32. Obtaining soil hydraulic properties for water balance and leaching models from survey data: 2. Hydraulic conductivity
33. Measuring unsaturated sorptivity and hydraulic conductivity using multiple disc permeameters
34. Accuracy of the saturated hydraulic conductivity prediction by pedo-transfer functions compared to the variability within FAO textural classes
35. Evaluation of pedo-transfer functions
36. Transient flow from tension infiltrometers: I. The two-parameter equation
37. Transient flow from tension infiltrometers: II. Four methods to determine sorptivity and conductivity
38. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils
39. On describing and predicting the hydraulic properties of unsaturated soils
40. Is regression what you really want?
41. Measurement of surface-soil hydraulic properties: Disk permeameters, tension infiltrometers, and other techniques
42. Steady infiltration from a shallow circular pond
43. Functional sensitivity analysis of four methods to generate soil hydraulic functions