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Eastern Cape Province South Africa (1)
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Asia
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Ordos Basin (6)
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North America
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Pacific Ocean
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Los Alamos County New Mexico
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Los Alamos National Laboratory (1)
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stable isotopes
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deuterium (1)
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Nd-144/Nd-143 (4)
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O-18/O-16 (2)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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Sm-147/Nd-144 (1)
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Sr-87/Sr-86 (4)
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metals
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U-238 (1)
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U-238/U-234 (1)
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U-238/U-235 (1)
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alkali metals
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rubidium
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Rb-87/Sr-86 (1)
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sodium (2)
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alkaline earth metals
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calcium
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Sr/Ca (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr/Ca (1)
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Sr-87/Sr-86 (4)
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chromium (1)
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platinum ores (2)
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rare earths
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neodymium
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Nd-144/Nd-143 (4)
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Sm-147/Nd-144 (1)
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samarium
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Sm-147/Nd-144 (1)
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technetium
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Tc-99 (1)
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nitrogen (4)
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oxygen
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O-18/O-16 (2)
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phosphorus (1)
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S-34/S-32 (1)
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Invertebrata
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Pleistocene
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Tertiary
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Paleogene
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Dongying Formation (1)
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Eocene (2)
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Oligocene (3)
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Shahejie Formation (2)
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Mesozoic
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Middle Cretaceous (1)
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Upper Cretaceous
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Vivian Formation (1)
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Jurassic
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Arab Formation (1)
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Triassic
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Upper Triassic
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Xujiahe Formation (1)
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Yanchang Formation (5)
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Paleozoic
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Berea Sandstone (3)
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Cambrian
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Carboniferous
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Benxi Formation (1)
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Lower Carboniferous
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Mabou Group (1)
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Devonian
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Upper Devonian (2)
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Horton Group (3)
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lower Paleozoic
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Rose Run Sandstone (1)
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Ordovician
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Lower Ordovician (1)
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Majiagou Formation (1)
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Meguma Group (3)
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Upper Ordovician
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Red River Formation (1)
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Permian
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upper Paleozoic (1)
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Precambrian
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Stillwater Complex (1)
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Proterozoic
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Neoproterozoic
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igneous rocks
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metamorphic rocks
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orthosilicates
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nesosilicates
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zircon group
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sheet silicates
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chlorite group
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chlorite (1)
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clay minerals
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kaolinite (3)
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montmorillonite (1)
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smectite (1)
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illite (1)
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mica group
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muscovite (4)
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serpentine group
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chrysotile (1)
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sulfates
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gypsum (1)
-
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sulfides (1)
-
-
Primary terms
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absolute age (8)
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academic institutions (1)
-
Africa
-
Southern Africa
-
South Africa
-
Eastern Cape Province South Africa (1)
-
-
-
-
Asia
-
Arabian Peninsula
-
Qatar (1)
-
Rub' al Khali (1)
-
Saudi Arabia (1)
-
United Arab Emirates (1)
-
-
Far East
-
China
-
Bohaiwan Basin (1)
-
Guangdong China
-
Leizhou Peninsula (1)
-
-
Hainan China (1)
-
Hebei China (1)
-
Henan China (1)
-
Jiangxi China (1)
-
North China Platform (1)
-
Ordos Basin (6)
-
Qaidam Basin (1)
-
Shandong China
-
Dongying Depression (1)
-
-
Sichuan Basin (1)
-
Taihang Mountains (1)
-
Xinjiang China
-
Tarim Basin (1)
-
-
-
Japan
-
Honshu
-
Aichi Japan (1)
-
Gifu Japan (1)
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Gumma Japan (1)
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Ibaraki Japan (1)
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Kanagawa Japan (1)
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Saitama Japan (1)
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Tokyo Japan (1)
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Kyushu
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Kumamoto Japan (1)
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Korea
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South Korea
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Kangwon South Korea (1)
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Vietnam (1)
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Indian Peninsula
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India (2)
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Middle East
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Cyprus (1)
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Israel (2)
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Syria (1)
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Atlantic Ocean
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Gulf of Mexico (3)
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North Sea
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Skagerrak (1)
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Scotian Shelf (1)
-
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South Atlantic
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Southwest Atlantic (1)
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-
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atmosphere (6)
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Australasia
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Australia
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Western Australia (1)
-
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New Zealand
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Lake Taupo (1)
-
-
-
bacteria
-
coliform bacteria
-
Escherichia
-
Escherichia coli (1)
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Pseudomonas (1)
-
-
bibliography (2)
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brines (1)
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Canada
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Eastern Canada
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Maritime Provinces
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Nova Scotia
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Cobequid Fault (2)
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Colchester County Nova Scotia (1)
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Halifax County Nova Scotia (1)
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Pictou County Nova Scotia (1)
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-
-
Meguma Terrane (4)
-
Newfoundland and Labrador
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Newfoundland (1)
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Quebec (3)
-
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Western Canada
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Alberta (4)
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British Columbia (1)
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Canadian Cordillera (1)
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Manitoba (1)
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Saskatchewan (1)
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carbon
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C-13/C-12 (1)
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C-14 (2)
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organic carbon (2)
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-
Cenozoic
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Quaternary
-
Holocene
-
lower Holocene (1)
-
upper Holocene (1)
-
-
Pleistocene
-
upper Pleistocene (2)
-
-
-
Tertiary
-
Neogene
-
Miocene
-
Crater Flat Tuff (1)
-
Guantao Formation (1)
-
Paintbrush Tuff (1)
-
Tiva Canyon Member (1)
-
Topopah Spring Member (2)
-
-
-
Paleogene
-
Dongying Formation (1)
-
Eocene (2)
-
Oligocene (3)
-
-
Shahejie Formation (2)
-
-
-
chemical analysis (1)
-
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Brooks and Corey model
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Image
Total mobility curves derived from the Brooks-Corey model for different oil...
in Numerical simulation of water injection into layered fractured carbonate reservoir analogs
> AAPG Bulletin
Published: 01 October 2006
Figure 11 Total mobility curves derived from the Brooks-Corey model for different oil-water viscosity ratios ranging from 1 to 100. For values near 1, λ t has a distinct minimum at intermediate saturations. This feature is lost at higher ratios, removing an associated stabilizing effect
Journal Article
Effect of Soil Hydraulic Properties Model on Slope Stability Analysis Based on Strength Reduction Method
Publisher: Geological Society of India
Published: 01 May 2014
Jour. Geol. Soc. India (2014) 83 (5): 586–594.
...Muhammad Mukhlisin; Marlin Ramadhan Baidillah; Aniza Ibrahim; Mohd. Raihan Taha Soil hydraulic properties models which have been proposed were derived based on the empirical fitting curve such as Brooks-Corey model (BC) and Van Genuchten model (VG), or based on soil pore radius distribution...
Image
Comparison of the experimental water retention curve and the predicted wate...
in A Genetic Algorithm for Predicting Pore Geometry Based on Air Permeability Measurements
> Vadose Zone Journal
Published: 01 May 2005
Fig. 6. Comparison of the experimental water retention curve and the predicted water retention curve based on the Brooks-Corey model.
Image
Plots showing α parameter equivalence when h 0 → ∞ between (a) the Gardn...
in Correspondence and Upscaling of Hydraulic Functions for Steady-State Flow in Heterogeneous Soils
> Vadose Zone Journal
Published: 01 May 2004
Fig. 1. Plots showing α parameter equivalence when h 0 → ∞ between (a) the Gardner and van Genuchten models and (b) the Gardner and Brooks–Corey models.
Image
Graphs of the function φ and F 1 for different choices of S 0 illustr...
in An Improved Semi-Analytical Solution for Verification of Numerical Models of Two-Phase Flow in Porous Media
> Vadose Zone Journal
Published: 01 February 2007
Figure 1. Graphs of the function φ and F 1 for different choices of S 0 illustrate why the original iterative process fails after the first iteration. Brooks-Corey model uses λ = 2.
Image
Local solution of h (0) and S (0) for different values of u . h (0...
in Effective Parameter Functions for the Richards Equation in Layered Porous Media
> Vadose Zone Journal
Published: 01 August 2006
Fig. 2. Local solution of h (0) and S (0) for different values of u . h (0) is made dimensionless with H . The curves are for a Brooks–Corey model with λ = 2 and κ 1 /κ 2 = 2.
Image
Influence of the skewness on the effective averaging schemes for α̅*̅ = 6.0...
in On the Effective Averaging Schemes of Hydraulic Properties at the Landscape Scale
> Vadose Zone Journal
Published: 01 January 2006
Fig. 5. Influence of the skewness on the effective averaging schemes for α̅*̅ = 6.0 and h = 0.5: (a) Gardner model, (b) Brooks–Corey model, (c) van Genuchten model. E , effective parameter coefficient; CS, coefficient of skewness; h , dimensionless suction head at surface; α̅*̅, mean value
Image
Influence of the skewness on the effective averaging schemes for α̅*̅ = 6.0...
in On the Effective Averaging Schemes of Hydraulic Properties at the Landscape Scale
> Vadose Zone Journal
Published: 01 January 2006
Fig. 3. Influence of the skewness on the effective averaging schemes for α̅*̅ = 6.0 and h = 5.0: (a) Gardner model, (b) Brooks–Corey model, (c) van Genuchten model. E , effective parameter coefficient; CS, coefficient of skewness; h , dimensionless suction head at surface; α̅*̅, mean value
Image
Layer-by-layer (a) relative permeability and (b) capillary pressure functio...
in Petrophysical inversion of borehole array-induction logs: Part I — Numerical examples
> Geophysics
Published: 15 August 2006
the modified Brooks-Corey model (see Table 5 , actual value section). (c) Time average of the rate of mud-filtrate invasion for pre- and postremoval of mudcake.
Image
Influence of the skewness on the effective averaging schemes for α̅*̅ = 1.0...
in On the Effective Averaging Schemes of Hydraulic Properties at the Landscape Scale
> Vadose Zone Journal
Published: 01 January 2006
Fig. 4. Influence of the skewness on the effective averaging schemes for α̅*̅ = 1.0 and h = 5.0: (a) Gardner model, (b) Brooks–Corey model, (c) van Genuchten model. E , effective parameter coefficient; CS, coefficient of skewness; h , dimensionless suction head at surface; \batchmode
Image
Dependence of log-scale relative permeability ( k r w ) on h...
in Permeability of methane hydrate-bearing sandy silts in the deep-water Gulf of Mexico (Green Canyon Block 955)
> AAPG Bulletin
Published: 01 May 2022
-Corey model ( Brooks and Corey, 1964 ), if hydrate is nonwetting or pore filling, is plotted as the dashed black line using a water fitting parameter ( n w = 3.5) and a residual water saturation ( S r w = 0.15) obtained from the relative permeability relationship in a Berea
Image
Effect of the characteristic particle size ( D 50 ) on (a) saturated water...
in Characterization of Thermal, Hydraulic, and Gas Diffusion Properties in Variably Saturated Sand Grades
> Vadose Zone Journal
Published: 01 April 2016
the van Genuchten model (vG, filled circle) and the Brooks–Corey model (B-C, open circle). In (b), the solid line and the dotted lines show K sat – D 50 relations from the parameterized models, Eq. [3] and [4] , respectively. We assumed a fluidity of 9.81 × 10 6 m −1 s −1 at 20°C for K sat
Image
(a) Variable tortuosity (τ a ) based Brooks–Corey–Burdine model predictions...
in An Air–Water Interfacial Area Based Variable Tortuosity Model for Unsaturated Sands
> Vadose Zone Journal
Published: 01 May 2006
Fig. 7. (a) Variable tortuosity (τ a ) based Brooks–Corey–Burdine model predictions and unsaturated hydraulic conductivity, K , measurements and (b) the standard Brooks–Corey–Burdine model predictions and K measurements (the solid line represents the regression line and the dotted line
Image
Water retention data with Brooks–Corey (1964) model fit for clean sand, and...
in Experimental Observations and Numerical Modeling of Coupled Microbial and Transport Processes in Variably Saturated Sand
> Vadose Zone Journal
Published: 01 May 2005
Fig. 6. Water retention data with Brooks–Corey (1964) model fit for clean sand, and data measured from tensiometers and TDR probes during the column experiment.
Journal Article
Geophysics Dissertation Abstracts
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 25 January 2013
Geophysics (2013) 78 (1): Z1.
... and WRCs with increasing clay content. Based on the well known Brooks-Corey model, an empirical approach is developed, which relates the relative relaxation time at partial saturation to the relative hydraulic conductivity K rel , i.e., the ratio of the unsaturated and the saturated conductivities...
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.
...Fig. 1. Plots showing α parameter equivalence when h 0 → ∞ between (a) the Gardner and van Genuchten models and (b) the Gardner and Brooks–Corey models. ...
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.
..., representing the approximate time needed to reconfigure the setup for the subsequent gas injection experiment. Heating was resumed, and gas was injected at prescribed pressures for approximately 16.9 d. Both the Brooks–Corey and van Genuchten models were used to describe the two-phase relative permeability...
Image
Relative permeability functions calculated with the Brooks and Corey (1964...
in Unsaturated Hydraulic Conductivity Measurements with Centrifuges: A Review 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.
> Vadose Zone Journal
Published: 01 August 2009
F ig . 8. Relative permeability functions calculated with the Brooks and Corey (1964) relative permeability function using the optimized parameters of the Brooks and Corey (1964) capillary pressure model; γ is the capillary pressure span.
Journal Article
Relative hydraulic conductivity in the vadose zone from magnetic resonance sounding — Brooks-Corey parameterization of the capillary fringe
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 12 April 2011
Geophysics (2011) 76 (3): G61–G71.
... as a cumulative pore size distribution. However, a strictly physical formulation of the WRC is very difficult. Thus, in soil physics, empirical models are the common choice. A frequently used model for the WRC is the model of Brooks and Corey (1964) (hereafter referred to as BC): The governing parameter...
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.
...Figure 11 Total mobility curves derived from the Brooks-Corey model for different oil-water viscosity ratios ranging from 1 to 100. For values near 1, λ t has a distinct minimum at intermediate saturations. This feature is lost at higher ratios, removing an associated stabilizing effect...
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