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Brooks and Corey equation
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Journal Article
Scaling and Estimation of Evaporation and Transpiration of Water across Soil Textures
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2005
Vadose Zone Journal (2005) 4 (2): 418–427.
...Joseph A. Kozak; Lajpat R. Ahuja; Liwang Ma; Tim R. Green Abstract A recent study showed all parameters in the Brooks-Corey equations of soil hydraulic properties are strongly correlated to the pore-size distribution index (λ). These λ values relate and can scale cumulative infiltration and water...
Image
The Brooks and Corey equation (dashed line) fitted to the point (time domai...
in Forward Prediction of Height-Averaged Capillary Pressure–Saturation Parameters Using the BC-vG Upscaler
> Vadose Zone Journal
Published: 01 August 2013
Fig. 2. The Brooks and Corey equation (dashed line) fitted to the point (time domain reflectometry) capillary pressure–saturation data (solid circles) for silica sand no. 8 from Sakaki and Illangasekare (2007) .
Image
Comparison of solutions of the generalized Richards equation that utilized ...
in Validity of the Generalized Richards Equation for the Analysis of Pumping Test Data for a Coarse-Material Aquifer Contribution of the Department of Geology and Geophysics and Water Resources Research Center, University of Hawai‘i, Honolulu, HI. WRRC Contributed Paper CP-2005-01.
> Vadose Zone Journal
Published: 01 February 2005
Fig. 5. Comparison of solutions of the generalized Richards equation that utilized the van Genuchten and Brooks and Corey functions.
Journal Article
Estimation of dynamic petrophysical properties of water-bearing sands invaded with oil-base mud from the interpretation of multiple borehole geophysical measurements
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 18 September 2012
Geophysics (2012) 77 (6): D209–D227.
...). Numerical simulation of mud-filtrate invasion yields the postinvasion radial distribution of water saturation. Rocks are assumed water wet, whereas rock-fluid properties such as saturation-dependent capillary pressure and relative permeability are described in parametric form via Brooks-Corey’s equation...
Journal Article
Forward Prediction of Height-Averaged Capillary Pressure–Saturation Parameters Using the BC-vG Upscaler
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 August 2013
Vadose Zone Journal (2013) 12 (3): vzj2012.0174.
...Fig. 2. The Brooks and Corey equation (dashed line) fitted to the point (time domain reflectometry) capillary pressure–saturation data (solid circles) for silica sand no. 8 from Sakaki and Illangasekare (2007) . ...
Journal Article
Modeling the Primary Drainage Curve of Prefractal Porous Media
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 November 2005
Vadose Zone Journal (2005) 4 (4): 959–966.
.... To estimate D from β it is necessary to know the values for b and P d . The Brooks and Corey (1964) empirical water retention equation is widely used for parameterizing main drying branch data. This model takes the form: 18 \batchmode \documentclass[fleqn,10pt,legalpaper]{article...
Journal Article
The Shape of the Transpiration Reduction Function under Plant Water Stress Funding provided by the framework of the Dutch National Research Programme Climate Changes Spatial Planning and by CAPES-MEC, Brazil.
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 February 2007
Vadose Zone Journal (2007) 6 (1): 124–139.
... are presented for five types of analytical soils: a constant diffusivity, Green and Ampt, Brooks and Corey, versatile nonlinear, and exponential soil. While in the case of constant diffusivity, relative transpiration decreases as a linear function of water content, for the remaining four cases the decrease...
Journal Article
Implications and Application of the Raats Superclass of Soils Equations
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 August 2016
Vadose Zone Journal (2016) 15 (8): vzj2016.02.0012.
.... [1] reduces to the model of Brooks and Corey (1964 , 1966) Solving Eq. [32] for S yields Note that Eq. [32] holds only for h ≥ h * because for h < h * S becomes >1, which is impossible. Equation [33] implies that only the product βγ can be identified, so that one of them...
Journal Article
Numerical simulation of water injection into layered fractured carbonate reservoir analogs
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 October 2006
AAPG Bulletin (2006) 90 (10): 1473–1493.
... mobility (equation 3) and the shape of the fractional flow function (equation 4). We calculate the relative permeability of the rock matrix using the Brooks and Corey (1964) model with an exponent of 2. This value is frequently applied to highly nonuniform materials (cf., Helmig, 1997...
Journal Article
Correspondence and Upscaling of Hydraulic Functions for Steady-State Flow in Heterogeneous Soils
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2004
Vadose Zone Journal (2004) 3 (2): 527–533.
... this context, we investigated two major issues involving soil hydraulic properties: (i) hydraulic parameter correspondence among some of the more commonly used soil hydraulic conductivity functions (i.e., the Gardner [G], Brooks–Corey [BC], and van Genuchten [VG] equations) and (ii) their application...
Image
Saturation-dependent capillary pressure and relative permeability input to ...
in Estimation of in situ hydrocarbon saturation of porous rocks from borehole measurements of spontaneous potential
> Geophysics
Published: 09 November 2020
Figure 7. Saturation-dependent capillary pressure and relative permeability input to the numerical simulations of mud-filtrate invasion. (a) Capillary pressure is described with Brooks and Corey’s (1964) parametric model for values of entry pressure equal to 3.5, 14, and 31 kPa and λ
Image
Two-phase fluid flow properties of slip-surface cataclasites from the 90-Fa...
in Two-phase fluid flow properties of cataclastic fault rocks: Implications for CO 2 storage in saline aquifers
> Geology
Published: 01 January 2012
the 90-Fathom fault. Curves shown were fitted to data using equations developed by Brooks and Corey (1964 , 1966) .
Image
The van Genuchten equation functions for different column heights predicted...
in Forward Prediction of Height-Averaged Capillary Pressure–Saturation Parameters Using the BC-vG Upscaler
> Vadose Zone Journal
Published: 01 August 2013
Fig. 4. The van Genuchten equation functions for different column heights predicted from a single set of point Brooks and Corey parameters (saturated water content θ s = 0.35 m 3 m −3 , θ r = 0.01 m 3 m −3 , bubbling capillary pressure head h b = 10 cm, and pore-size distribution index λ
Image
The van Genuchten equation (dashed line) fitted to height-averaged (Tempe c...
in Forward Prediction of Height-Averaged Capillary Pressure–Saturation Parameters Using the BC-vG Upscaler
> Vadose Zone Journal
Published: 01 August 2013
Fig. 3. The van Genuchten equation (dashed line) fitted to height-averaged (Tempe cell) capillary pressure–saturation data (solid circles) for silica sand no. 8 from Sakaki and Illangasekare (2007) compared with the van Genuchten equation predicted (solid line) from point Brooks and Corey
Journal Article
Quantifying Transient Soil Moisture Dynamics Using Multipoint Direct-Current Resistivity in Homogeneous Sand All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 February 2011
Vadose Zone Journal (2011) 10 (1): 286–298.
... determined by the Brooks–Corey equation ( Brooks and Corey, 1964 ), and Z (m) is the location of the sand–atmosphere boundary ( Fig. 3a ). Hydraulic relationships were estimated by the Brooks–Corey equation ( Brooks and Corey, 1964 ). The system boundary conditions are described in Fig. 2b , with the note...
Journal Article
Experimental and Numerical Investigation of Flow Phenomena in Nonisothermal, Variably Saturated Bentonite–Crushed Rock Mixtures
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2003
Vadose Zone Journal (2003) 2 (2): 239–246.
.... As shown in Fig. 7 , both the Brooks–Corey and van Genuchten models represented the measured capillary pressure curves for intermediate saturations reasonably well. However, potentially significant deviations existed near full saturation and complete dryness. Equations [2] and [3] were used to convert...
Journal Article
Derivation and Validation of a New Soil Pore-Structure-Dependent Flux–Saturation Relationship
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2017
Vadose Zone Journal (2017) 16 (5): 1–15.
...) , with Richards’ equation and the Brooks–Corey hydraulic model ( Brooks and Corey, 1964 ), and gave consistent simulations with the measured horizontal and vertical soil moisture profiles. However, here, no specific hydraulic property model is used, which means that the results in this research need...
Journal Article
An Improved Green–Ampt Infiltration and Redistribution Method for Uneven Multistorm Series All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2009
Vadose Zone Journal (2009) 8 (2): 470–479.
... are the parameters of the Brooks and Corey (1964) equation, where h b [L] is the bubbling pressure and λ (dimensionless) is the pore-size distribution index; and K r is the relative unsaturated hydraulic conductivity function. In this case, Ogden and Saghafian (1997) showed that the function G (θ i ,θ o...
Journal Article
An Air–Water Interfacial Area Based Variable Tortuosity Model for Unsaturated Sands
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 May 2006
Vadose Zone Journal (2006) 5 (2): 764–776.
..., Washington , DC . Warrick , A.W. 2003 . Soil water dynamics . Oxford Univ. Press, Oxford , UK . Table 2. Summary statistics for the Brooks–Corey–Burdine (BCB) and van Genuchten–Mualem (VGM) models. Residual mean squared deviation Linear regression equation † and r 2...
Journal Article
Field-Scale Water Flow Simulations Using Ensembles of Pedotransfer Functions for Soil Water Retention
A. K. Guber, Ya. A. Pachepsky, M. Th. van Genuchten, W. J. Rawls, J. Simunek, D. Jacques, T. J. Nicholson, R. E. Cady
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 January 2006
Vadose Zone Journal (2006) 5 (1): 234–247.
... are listed in the Appendix A. 1 1 A FORTRAN code to estimate water retention with PTFs of this work is available on request from the corresponding author. Six of the PTFs estimated parameters of the Brooks–Corey equation ( Brooks and Corey, 1964 ): 2 \batchmode \documentclass[fleqn,10pt,legalpaper...
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