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Measurement of Soil Physical Properties in the Field

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Summary

Increasing efforts have been spent in the past two decades on field measurement of soil physical properties and on the development of transport models. Here a summary is given of the characteristics of field soils gleaned from such measurements. The principle feature of field soils is their variability over many length and time scales. Issues involved in measurements in a heterogeneous environment are considered. These include the interaction of measurement scale with perceived variability, soil-imposed weighting of measurements, the Heisenberg uncertainty principle, the use of correlations, inverse measurement techniques, and soil macrostructure and biological activity. Some criteria for field measurements are identified. Predictive frameworks for interpreting and using field data are discussed. These range from the fully deterministic to stochastic theories. The successes and limitations of these are considered. Finally, some remaining problem areas are identified.

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References

  • Bear J (1972) Dynamics of fluids in porous media. Elsevier, New York Beven K, Germann PF (1982) Macropores and water flow in soils. Water Resour Res 18: 1311–1325

    Google Scholar 

  • Bouma JA, Denning JG (1975) A comparison of hydraulic conductivities calculated with morphometric and physical methods. Soil Sci Soc Am Proc 38: 124–127

    Google Scholar 

  • Bouma JA, Jongerius A, Boersma O, Jager A, Schoonderbeek D (1977) The function of different types of macropores during saturated flow through four swelling soil horizons. Soil Sci Soc Am J 41: 945–950

    Google Scholar 

  • Bouma JA, Wösten JHL (1979) Flow patterns during extended saturated flow in two undisturbed swelling clay soils with different macro sturctures. Soil Sci Soc Am J 43: 16–22

    Google Scholar 

  • Bouwer H (1964) Unsaturated flow in ground-water hydraulics. J Hydraul Div Am Soc Civ Eng 90 (HY5): 121–144

    Google Scholar 

  • Bouwer H (1966) Rapid field measurement of air entry value and hydraulic conductivity of soil as significant parameters in flow system analysis. Water Resour Res 2: 727–738

    Google Scholar 

  • Brakensiek DL, Engleman RL, Rawls WJ (1980) Variation within texture classes of soil water parameters. Paper No 2006 Am Soc Agr Eng Summer Meeting, San Antonio, Texas

    Google Scholar 

  • Bresler E, Dagan G (1979) Solute transport in unsaturated heterogeneous soil at field scale: 2. Applications. Soil Sci Soc Am J 43: 467–472

    Google Scholar 

  • Bresler E, Dagan G (1981) Convective and pore scale dispersive solute transport in unsaturated heterogeneous fields. Water Resour Res 17: 1683–1693

    Google Scholar 

  • Bresler E, Dagan G (1983) Unsaturated flow in spatially variable fields: 2. Application of water flow models to various fields. Water Resour Res 19: 421–428

    Google Scholar 

  • Broadbridge P, White I (1988) Constant rate rainfall infiltration: A versatile nonlinear model: 1. Analytic solution. Water Resour Res 24: 145–154

    Google Scholar 

  • Brooks RH, Corey AT (1966) Properties of porous media affecting fluid flow. J Irrig Drain Div Am Soc Civ Eng 92 (IR2): 61–88

    Google Scholar 

  • Burgess TM, Webster R, McBratney, AB (1981) Optimal interpolation and isarithmic mapping of soil properties: IV. Sampling strategy. J Soil Sci 32: 643–659

    Google Scholar 

  • Burrough PA (1983) Problems of superimposed effects in statistical study of the spatial variation of soil. Agric Water Manage 6: 123–143

    Google Scholar 

  • Byers E, Stephens DB (1983) Statistical and stochastic analysis of hydraulic conductivity and particle size in a fluvial sand. Soil Sci Soc Am J 47: 1072–1081

    Google Scholar 

  • Cary JW (1973) Soil water flow meters with thermocouple outputs. Soil Sci Soc Am Proc 37: 176–181

    Google Scholar 

  • Chuoke RL, van Meurs P, van der Poel C (1959) The instability of slow, immiscible, viscous liquid-liquid displacements in permeable media. Trans Am Inst Min Metall Pet Eng 216: 188–194

    Google Scholar 

  • Clothier BE (1988) Measurement of soil physical properties in the field: Commentary. This volume, pp

    Google Scholar 

  • Clothier BE, Knight JH, White I (1981a) Burgers’ equation: Application to field constant-flux infiltration. Soil Sci 132: 255–261

    Google Scholar 

  • Clothier, BE, White I (1981) Measurement of sorptivity and soil water diffusivity in the field. Soil Sci Soc Am J 45: 241–245

    Google Scholar 

  • Clothier BE, White I (1982) Water diffusivity of a field soil. Soil Sci Soc Am J 46: 636–640

    Google Scholar 

  • Clothier BE, White I, Hamilton GJ (1981b) Constant-rate rainfall infiltration: Field experiments. Soil Sci Soc Am J 45: 245–249

    Google Scholar 

  • Curtis GP, Roberts PV, Reinhard M (1986) A natural gradient experiment on solute transport in a sand aquifer: 4. Sorption of organic solutes and its influence on mobility. Water Resour Res 22: 2059–2067

    Google Scholar 

  • Cushman JH (1984) On unifying the concepts of scale, instrumentation, and stochastics in development of multiphase transport theory. Water Resour Res 20: 1668–1678

    Google Scholar 

  • Cushman JH (1986) On measurement, scale and scaling. Water Resour Res 22: 129–134

    Google Scholar 

  • Cushman JH (1987) More on stochastic models. Water Resour Res 23: 750–752

    Google Scholar 

  • Dagan G (1976) Comment on ‘A stochastic-conceptual analysis of one dimensional ground water flow in nonuniform homogeneous media’ by RA Freeze. Water Resour Res 12: 567

    Google Scholar 

  • Dagan G (1986) Statistical theory of groundwater flow and transport: Pore to laboratory, laboratory to formation, and formation to regional scale. Water Resour Res 22: 120S–143S

    Google Scholar 

  • Dagan G (1987) Theory of solute transport by groundwater. Ann Rev Fluid Mech 19: 183–215

    Google Scholar 

  • Dagan G, Bresler E (1979) Solute dispersion in unsaturated heterogeneous soil at field scale: 1. Theory. Soil Sci Soc Am J 43: 461–467

    Google Scholar 

  • Dagan G, Bresler E (1983) Unsaturated flow in spatially variable fields: 1. Derivation of models of infiltration and redistribution. Water Resour Res 19: 413–420

    Google Scholar 

  • de Vries DA (1987) The theory of heat and moisture transfer in porous media revisted. Int J Heat Mass Transfer 30: 1343–1350

    Google Scholar 

  • Dirksen CA (1972) A versatile soil water flux flow meter. In: Proc 2nd Symp on Fundamentals of Transport Phenomena in Porous Media, vol 2, IAHR, ISSS, University of Guelph, Ontario, pp 425–442

    Google Scholar 

  • Dirksen CA (1975) Determination of soil water diffusivity by sorptivity measurement. Soil Sci Soc Am Proc 39: 22–27

    Google Scholar 

  • Dixon RM (1972) Controlling infiltration in biomodal porous solids: Air-earth interface concept. In: Proc 2nd Symp on Fundamentals of Transport Phenomena in Porous Media, vol 2, IAHR, ISSS, University of Guelph, Ontario, pp 107–117

    Google Scholar 

  • Duffy C, Wierenga PJ, Kselik RA (1981) Variations in infiltration rate based on soil survey information and field measurements. New Mexico Agr Exper Stat Bull 680: 1–40

    Google Scholar 

  • Freeze RA (1975) A stochastic conceptual analysis of one-dimensional groundwater flow in nonuniform homogeneous media. Water Resour Res 11: 725–741

    Google Scholar 

  • Freeze RA (1976) Reply. Water Resour Res 12: 568

    Google Scholar 

  • Freyberg DL (1986) A natural gradient experiment on solute transport in a sand aquifer: 2. Spatial moments and the advection and dispersion of nonreactive tracers. Water Resour Res 22: 2031–2046

    Google Scholar 

  • Gardner WR (1958) Some steady state solutions of the unsaturated moisture flow equation with application to evaporation from a water table. Soil Sci 85: 228–232

    Google Scholar 

  • Gardner WR (1974) The permeability problem. Soil Sci 117: 243–249

    Google Scholar 

  • Gelhar LW (1974) Stochastic analysis of phreatic aquifers. Water Resour Res 10: 539–545

    Google Scholar 

  • Gelhar LW (1986) Stochastic subsurface hydrology from theory to applications. Water Resour Res 22: 135S–145S

    Google Scholar 

  • Gelhar LW, Axness CL (1983) Three-dimensional stochastic analysis of macro-dispersion in aquifers. Water Resour Res 19: 161–180

    Google Scholar 

  • Gollan T, Passioura JB, Munns R (1986) Soil water status affects the stomatal conductance of fully turgid wheat and sunflower leaves. Aust J Plant Physiol 13: 459–464

    Google Scholar 

  • Greacen W (1981) (ed) Soil water asssessment by the neutron method. CSIRO

    Google Scholar 

  • Melbourne Gutjahr A (1985) Spatial variability: geostatistical methods. In: Nielsen DR, Bouma J (eds) Soil spatial variability, Pudoc, Wageningen, pp 9–28

    Google Scholar 

  • Hassan HM, Warrick AW, Amoozegar-Fard A (1983) Sampling volume effects on determining salt in a soil profile. Soil Sci Soc Am J 47: 1265–1267

    Google Scholar 

  • Hawley ME, Richard HM, Thomas JJ (1982) Volume-accuracy relationship in soil moisture modeling. J Irrig Drain Proc ASCE 108: 1–11

    Google Scholar 

  • Hill DE, Parlange J-Y (1972) Wetting front instability in layered soils. Soil Sci Soc Am Proc 36: 697–702

    Google Scholar 

  • Hoeksema RJ, Kitanidis PK (1985) Analysis of spatial structure of properties of selected aquifers. Water Resour Res 21: 563–572

    Google Scholar 

  • Jackson RD (1988) Surface temperature and surface energy balance. This volume, pp

    Google Scholar 

  • Journel AG (1986) Geostatistics: models and tools for earth sciences. Math Geol 18: 119–139

    Google Scholar 

  • Jury WA (1985) Spatial variability of soil physical parameters in solute migration: A critical literature review. Top Rep EA 4228. Elec Power Res Inst, Palo Alto, California, 80 pp

    Google Scholar 

  • Jury WA (1988) Solute transport and dispersion. This volume, pp

    Google Scholar 

  • Kanchanasut P, Scotter DR, Tillman RW (1978) Preferential solute movement through soil voids: 2. Experiments with saturated soil. Aust J Soil Res 16: 269–276

    Google Scholar 

  • Knight JH (1988) Solute transport and dispersion: Commentary. This volume, PP

    Google Scholar 

  • Mackay DM, Freyberg DL, Roberts PV, Cherry JA (1986) A natural gradient experiment on solute transport in a sand aquifer: 1. Approach and overview of plume movement. Water Resour Res 22: 2017–2029

    Google Scholar 

  • Mandelbrot BB (1983) The fractal geometry of nature. WH Freeman, San Francisco

    Google Scholar 

  • Mantoglou A, Gelhar LW (1987a) Stochastic modeling of large-scale transient unsaturated flow systems. Water Resour Res 23: 37–46

    Google Scholar 

  • Mantoglou A, Gelhar LW (1987b) Capillary tension head variance, mean soil moisture content, and effective specific soil moisture capacity of transient unsaturated flow in stratified soils. Water Resour Res 23: 47–56.

    Google Scholar 

  • Mantoglou A, Gelhar LW (1987c) Effective hydraulic conductivities of transient unsaturated flow in stratified soils. Water Resour Res 23: 57–67

    Google Scholar 

  • Matheron G (1971) The theory of regionalized variables and its applications. Ecole des Mines de Paris, Fontainebleau, France

    Google Scholar 

  • McBratney AB, Webster R (1983) How many observations are needed for regional estimation of soil properties? Soil Sci 135: 177–183

    Google Scholar 

  • Miller EE (1980) Similitude and scaling of soil-water phenomena. In: Applications of soil physics, Academic Press, New York, pp 300–318

    Google Scholar 

  • Miller EE, Miller RD (1956) Physical theory for capillary flow phenomena. J Appl Phys 27: 324–333

    Google Scholar 

  • Moore ECS (1898) Sanitary engineering: a practical treatise on the collection, removal and final disposal of sewage and the design and construction of works of drainage and sewerage. BT Batsford, London

    Google Scholar 

  • Morel-Seytoux HJ (1973) Two-phase flows in porous media. Adv Hydrosci 9: 119–202

    Google Scholar 

  • Mualem Y (1974) A conceptual model of hysteresis. Water Resour Res 10: 514–520

    Google Scholar 

  • Mualem Y (1976) A new model for predicting the hydraulic conductivity of unsaturated media. Water Resour Res 12: 513–522

    Google Scholar 

  • Myers LE, van Bavel CH (1963) Measurement and evaluation of water table elevations. Paper presented at 5th Congress, International Committee on Irrigation and Drainage, Tokyo

    Google Scholar 

  • Nielsen DR, Biggar JW (1967) The physical characterization of field soils. In: Bradley EF, Denmead OT (eds) The collection and processing of field data. Interscience ( Wiley ), New York

    Google Scholar 

  • Nielsen DR, Biggar JW, Erh KT (1973) Spatial variability of field-measured soil-water properties. Hilgardia 42: 215–259

    Google Scholar 

  • Nielsen DR, Reichardt K, Wierenga PJ (1983) Characterization of field-measured soil-water properties. Intern Atomic Energy Agency Symp on Isotopes and Radiation Technology. In: Soil physics and irrigation studies, Aix-en-Provence, France, pp 18–22

    Google Scholar 

  • Nielsen DR, van Genuchten MTh, Biggar JW (1986) Flow and solute transport processes in the unsaturated zone. Water Resour Res 22: 89S–108S

    Google Scholar 

  • Parlange J-Y (1975) Determination of soil water diffusivity by sorptivity measurements. Soil Sci Soc Am Proc 39: 1011–1012

    Google Scholar 

  • Peck AJ, Luxmore RJ, Stolzy JL (1977) Effects of spatial variability of soil hydraulic properties in water budget modelling. Water Resour Res 13: 348–354

    Google Scholar 

  • Perroux KM, White I (1988) Designs for disc permeameters. Soil Sci Soc Am J, in press

    Google Scholar 

  • Philip GM, Watson DF (1986) Matheronian geostatistics - quo vadis? Math Geol 18: 93–117

    Google Scholar 

  • Philip JR (1957) The theory of infiltration: 4. Sorptivity and algebraic infiltration equations. Soil Sci 84: 257–265

    Google Scholar 

  • Philip JR (1958) The theory of infiltration: 7. Soil Sci 85: 333–357

    Google Scholar 

  • Philip JR (1967) Sorption and infiltration in heterogeneous media. Aust J Soil Res 5: 1–10

    Google Scholar 

  • Philip JR (1969) Theory of infiltration. Adv Hydrosci 5: 215–296

    Google Scholar 

  • Philip JR (1970) Flow in porous media. Ann Rev Fluid Mech 2: 177–204

    Google Scholar 

  • Philip JR. (1973) On solving the unsaturated flow equation: 1. The flux concentration relation. Soil Sci 116: 328–335

    Google Scholar 

  • Philip JR (1975a) Stability analysis of infiltration. Soil Sci Soc Am Proc 39: 1042–1049

    Google Scholar 

  • Philip JR (1975b) The growth of disturbances in unstable infiltration flows. Soil Sci Soc Am Proc 39: 1049–1053

    Google Scholar 

  • Philip JR (1980) Field heterogeneity: Some basic issues. Water Resour Res 16: 443–448

    Google Scholar 

  • Philip JR (1985) Reply to Comments on “Steady infiltration from spherical cavities”. Soil Sci Soc Am J 49: 788–789

    Google Scholar 

  • Philip JR (1986a) Linearized unsteady multidimensional infiltration. Water Resour Res 22: 1717–1727

    Google Scholar 

  • Philip JR (1986b) Issues in flow and transport in heterogeneous porous media. Transp Porous Media 1: 319–338

    Google Scholar 

  • Philip JR (1987) The quasilinear analysis, the scattering analog, and other aspects of infiltration and seepage. In: Fok Y-S (ed) Infiltration development and application, Water Resour Res Centre, Honolulu, Hawaii, pp 1 - 27

    Google Scholar 

  • Philip JR (1988) Quasianalytic and analytic approaches to unsaturated flow. This volume, pp

    Google Scholar 

  • Philip JR, Knight JH (1974) On solving the unsaturated flow equation: 3. New quasi-analytic technique. Soil Sci 117: 1–13

    Google Scholar 

  • Raats PAC (1973) Unstable wetting fronts in uniform and non-uniform soils. Soil Sci Soc Am Proc 39: 1049–1053

    Google Scholar 

  • Raats PAC (1988) Quasianalytical and analytical approaches to unsaturated flow: Commentary. This volume, pp

    Google Scholar 

  • Raats PAC, Gardner WR (1971) Comparison of empirical relationships between pressure head and hydraulic conductivity and some observations on radially symmetric flow. Water Resour Res 7: 921–928

    Google Scholar 

  • Rao PV, Rao PSC, Davidson JM, Hammond LC (1979) Use of goodness-of-fit tests for characterizing the spatial variability. Soil Sci Soc Am J 43: 274–278

    Google Scholar 

  • Reichardt K, Libardi PL, Nielsen DR (1975) Unsaturated hydraulic conductivity determination by a scaling technique. Soil Sci 120: 165–168

    Google Scholar 

  • Reichardt K, Nielsen DR, Biggar JW (1972) Scaling of horizontal infiltration into homogeneous soils. Soil Sci Soc Am Proc 36: 241–245

    Google Scholar 

  • Ritchie JT (1972) Model for predicting evaporation from a row crop with incomplete cover. Water Resour Res 8: 1204–1213

    Google Scholar 

  • Ritchie JT (1983) Efficient water use and crop production: Discussion on the generality of relations between biomass production and évapotranspiration. In: Limitations to efficient water use in crop production, Am Soc Agron, Special Publication, pp 29–44

    Google Scholar 

  • Ritchie JT, Kissel DE, Burnet E (1972) Water movement in undisturbed swelling clay soils. Soil Sci Soc Am Proc 36: 874–879

    Google Scholar 

  • Roberts PV, Goltz MN, Mackay DM (1986) A natural gradient experiment on solute transport in a sand aquifer: 3. Retardation estimates and mass balances for organic solutes. Water Resour Res 22: 2047–2058

    Google Scholar 

  • Russo D, Bresler E (1980) Scaling soil hydraulic properties of a heterogeneous field. Soil Sci Soc Am J 44: 681–684

    Google Scholar 

  • Russo D, Jury WA (1987a) A theoretical study of the estimation of the correlation scale in spatially variable fields: 1. Stationary fields. Water Resour Res 23: 1257–1268

    Google Scholar 

  • Russo D, Jury WA (1987b) A theoretical study of the estimation of the correlation scale in spatially variable fields: 2. Nonstationary fields. Water Resour Res 23: 1269–1279

    Google Scholar 

  • Scotter DR (1978) Preferential solute movement through larger soil voids: 1. Some computations using simple theory. Aust J Soil Res 16: 257–267

    Google Scholar 

  • Simmons CS, Nielsen DR, Biggar JW (1979) Scaling of field-measured soil-water properties: I. Methodology. Hilgardia 47: 77–102

    Google Scholar 

  • Sisson JB, Wierenga PJ (1981) Spatial variability of steady-state infiltration rates as a stochastic process. Soil Sci Soc Am J 45: 699–704

    Google Scholar 

  • Smiles DE, Kirby JM (1988) One-dimensional solid-liquid separation. This volume, pp

    Google Scholar 

  • Smiles DE, Harvey AG (1973) Measurement of moisture diffusivity in wet swelling systems. Soil Sci 116: 391–399

    Google Scholar 

  • Smiles DE, Perroux KM, Zegelin SJ (1981) Absorption of water by soil: some effects of a saturated zone. Soil Sci Soc Am J 44: 1153–1158

    Google Scholar 

  • Sposito G (1986) The “physics” of soil-water physics. Water Resour Res 22: 82S–88S

    Google Scholar 

  • Sposito G, Jury WA (1985) Inspectional analysis in the theory of water flow through unsaturated soil. Soil Sci Soc Am J 49: 791–798

    Google Scholar 

  • Sposito G, Jury WA (1986) Group invariance and field scale solute transport. Water Resour Res 22: 1743–1748

    Google Scholar 

  • Sposito G, Jury WA, Gupta VK (1987) Reply. Water Resour Res 23: 753–754

    Google Scholar 

  • Sudicky EA (1986) A natural gradient experiment on solute transport in a sand aquifer: Spatial variability of hydraulic conductivity and its role in the dispersion process. Water Resour Res 22: 2069–2082

    Google Scholar 

  • Sully MJ, Flocchini RG, Nielsen DR (1987) Linear distribution of naturally occurring radionuclides in a mollic xerofluvent. Soil Sci Soc Am J 51: 276–281

    Google Scholar 

  • Talsma T (1988) Evaluation of the well permeameter as a field method of measuring hydraulic conductivity. Aust J Soil Res 25: 361–368

    Google Scholar 

  • Tillotson PM, Nielsen DR (1984) Scale factors in soil science. Soil Sci Soc Am J 48: 953–959

    Google Scholar 

  • Topp GC, Davis JL, Annan AP (1980) Electromagnetic determination of soil water content: Measurements in coaxial transmission lines. Water Resour Res 16: 574–582

    Google Scholar 

  • Truesdell C (1984) An idiot’s fugitive essays on science. Springer, Berlin

    Google Scholar 

  • van Genuchten MTh (1980) A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci Soc Am J 44: 892–898

    Google Scholar 

  • Vieira SR, Nielsen DR, Biggar JW (1981) Spatial variability of field-measured infiltration rate. Soil Sci Soc Am J 45: 1040–1048

    Google Scholar 

  • Warrick AW (1983) Parameters in infiltration equations. In: Advances in infiltration, ASAE, New York, pp 69–81

    Google Scholar 

  • Warrick AW, Lomen DO, Yates SR (1985) A generalized solution to infiltration. Soil Sci Soc Am J 49: 34–38

    Google Scholar 

  • Warrick AW, Mullen GW, Nielsen DR (1977) Scaling of field-measured soil hydraulic properties using a similar media concept. Water Resour Res 13: 355–362

    Google Scholar 

  • Warrick AW, Nielsen DR (1980) Spatial variability of soil physical properties in the field. In: Applications of soil physics, Academic Press, New York, pp 319–344

    Google Scholar 

  • Weir GJ (1986) Steady infiltration from large shallow ponds. Water Resour Res 22: 1462–1468

    Google Scholar 

  • Weir GJ (1987) Steady infiltration from small shallow ponds. Water Resour Res 23: 733–736

    Google Scholar 

  • White I (1988) Comment on “A natural gradient experiment on solute transport in a sand aquifer: spatial variability of hydraulic conductivity and its role in the dispersion process” by Sudicky EA. Water Resour Res, in press

    Google Scholar 

  • White I, Broadbridge P (1988) Constant rate rainfall infiltration: A versatile nonlinear model. 2. Applications of solutions. Water Resour Res 24: 155–162

    Google Scholar 

  • White I, Colombera PM, Philip JR (1976) Experimental study of wetting front instability induced by sudden change of pressure gradient. Soil Sci Soc Am J 40: 824–829

    Google Scholar 

  • White I, Colombera PM, Philip JR (1977) Experimental studies of wetting front instability induced by gradual change of pressure gradient and by heterogeneous porous media. Soil Sci Soc Am J 41: 483–489

    Google Scholar 

  • White I, Perroux KM (1987) Use of sorptivity to determine field soil hydraulic properties. Soc Sci Soc Am J 51: 1093–1101

    Google Scholar 

  • White I, Perroux KM (1988) Estimation of unsaturated hydraulic conductivity from field sorptivity measurements. Soil Sci Soc Am J, in press

    Google Scholar 

  • White I, Sully MJ (1987) Macroscopic and microscopic capillary length and time scales from field infiltration. Water Resour Res 23: 1514–1522

    Google Scholar 

  • Wilson DJ, Ritchie AIM (1986) Neutron moisture meters - the dependence of their response on soil parameters. Aust J Soil Res 24: 11–23

    Google Scholar 

  • Wooding RA (1968) Steady infiltration from a shallow circular pond. Water Resour Res 4: 1259–1273

    Google Scholar 

  • Yeh T-C, Gelhar LW, Gutjahr AL (1985a) Stochastic analysis of unsaturated flow in heterogeneous soils. 1. Statistically isotropic media. Water Resour Res 21: 447–456

    Google Scholar 

  • Yeh T-C, Gelhar LW, Gutjar AL (1985b) Stochastic analysis of unsaturated flow in heterogeneous soils. 2. Statistically anisotropic media with variable a. Water Resour Res 21: 457–464

    Google Scholar 

  • Yeh T-C, Gelhar LW, Gutjahr AL (1985c) Stochastic analysis of unsaturated flow in heterogeneous soils. 3. Observations and applications. Water Resour Res 21: 465–471

    Google Scholar 

  • Youngs EG, Price RI (1981) Scaling of infiltration behaviour in dissimilar porous materials. Water Resour Res 17: 1065–1070

    Google Scholar 

  • Zegelin SJ, White I, Jenkins DR (1988) Improved field probes for soil-water content and electrical conductivity measurement using time domain reflectometry. Water Resour Res, submitted

    Google Scholar 

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White, I. (1988). Measurement of Soil Physical Properties in the Field. In: Steffen, W.L., Denmead, O.T. (eds) Flow and Transport in the Natural Environment: Advances and Applications. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-73845-6_5

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  • DOI: https://doi.org/10.1007/978-3-642-73845-6_5

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