Delft Dredging Engineering:

DHLLDV

©Dr.ir. S.A. Miedema

DSCRC

©Dr.ir. S.A. Miedema

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	Home (3447 Hits) Whats new The Delft Head Loss & Limit Deposit Velocity Framework (DHLLDV) The Delft Sand, Clay & Rock Cutting Model (DSCRC) Dr.ir. Sape A. Miedema (12944 Hits) Introduction Short Curriculum Vitae Awards Bibliography Reports

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DSCRCM

	General Cutting of Sand, Clay & Rock (709 Hits) The Cutting of Dry Sand (491 Hits) The Important Specific Energy Graphs (242 Hits) Subpages: Specific Energy in Sand (824 Hits) Specific Energy in Clay (569 Hits) Specific Energy in Rock (516 Hits) The Basic Soil Mechanics Equations (455 Hits) The Delft Sand, Clay & Rock Cutting Model Book (12907 Hits) 01 The DSCRC Model Book Cover 02 Contents of the DSCRC Model Book. IOS Press: The Delft Sand, Clay & Rock Cutting Model

DHLLDV

	Slurry Transport: Fundamentals, A Historical Overview & The DHLLDV Framework. (13780 Hits) 03 Uniform Sands & Gravels 04 Graded Sands & Gravels 01 Description of the DHLLDV Framework. 02 The DHLLDV Framework Book Cover. 05 Contents of the Slurry Transport Book. Flow Regimes (302 Hits) Subpages: Regime 1: Stationary or Fixed Bed, No Sheet Flow (659 Hits) Regime 2: Stationary or Fixed Bed, Sheet Flow or Suspension (497 Hits) Regime 3: Sliding Bed (Coarse) with Sheet Flow or Fixed Bed (Fine) with Suspension (636 Hits) Regime 4: Sliding Bed (Coarse) with Sheet Flow or Fixed Bed (Fine) with Suspension (626 Hits) Regime 5: Heterogeneous Transport (555 Hits) Regime 6: Homogeneous Transport (468 Hits) Regime 7: Sliding Flow (467 Hits) Regime 8: Stationary or Sliding Bed, Cvt (540 Hits) Regime 5-6: Pseudo Homogeneous Transport (615 Hits) Scenarios (222 Hits) Subpages: Excess Hydraulic Gradient (985 Hits) The Excess Hydraulic Gradient Scenario 1: Fine Sands (1003 Hits) Scenario 1: The Hydraulic Gradient Scenario 1: The Relative Excess Hydraulic Gradient Scenario 2A: Medium Sands (814 Hits) Scenario 2A: The Hydraulic Gradient Scenario 2A: The Relative Excess Hydraulic Gradient Scenario 2B: Coarse Sands (786 Hits) Scenario 2B: The Hydraulic Gradient Scenario 2B: The Relative Excess Hydraulic Gradient Scenario 3: Gravels (844 Hits) Scenario 3: The Hydraulic Gradient Scenario 3: The Relative Excess Hydraulic Gradient Standard Graphs (251 Hits) Subpages: Dp=0.0254 m (1 inch) (2870 Hits) 11: Dp=0.0254 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.0254 m, A Comparison Of Different Models 06: Dp=0.0254 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.0254 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.0254 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.0254 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.0254 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.0254 m, Uniform Sands & Gravels, d=1 mm Dp=0.0508 m (2 inch) (2305 Hits) 11: Dp=0.0508 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.0508 m, A Comparison Of Different Models 06: Dp=0.0508 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.0508 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.0508 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.0508 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.0508 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.0508 m, Uniform Sands & Gravels, d=1 mm Dp=0.1016 m (4 inch) (2519 Hits) 11: Dp=0.1016 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.1016 m, A Comparison Of Different Models 06: Dp=0.1016 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.1016 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.1016 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.1016 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.1016 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.1016 m, Uniform Sands & Gravels, d=1 mm Dp=0.1524 m (6 inch) (2723 Hits) 11: Dp=0.1524 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.1524 m, A Comparison Of Different Models 06: Dp=0.1524 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.1524 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.1524 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.1524 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.1524 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.1524 m, Uniform Sands & Gravels, d=1 mm Dp=0.2032 m (8 inch) (2313 Hits) 11: Dp=0.2032 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.2032 m, A Comparison Of Different Models 06: Dp=0.2032 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.2032 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.2032 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.2032 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.2032 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.2032 m, Uniform Sands & Gravels, d=1 mm Dp=0.2540 m (10 inch) (1934 Hits) 11: Dp=0.2540 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.2540 m, A Comparison Of Different Models 06: Dp=0.2540 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.2540 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.2540 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.2540 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.2540 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.2540 m, Uniform Sands & Gravels, d=1 mm Dp=0.3000 m (about 12 inch) (2072 Hits) 11: Dp=0.3000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.3000 m, A Comparison Of Different Models 06: Dp=0.3000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.3000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.3000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.3000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.3000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.3000 m, Uniform Sands & Gravels, d=1 mm Dp=0.4000 m (about 16 inch) (1990 Hits) 11: Dp=0.4000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.4000 m, A Comparison Of Different Models 06: Dp=0.4000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.4000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.4000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.4000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.4000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.4000 m, Uniform Sands & Gravels, d=1 mm Dp=0.5000 m (about 20 inch) (2036 Hits) 11: Dp=0.5000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.5000 m, A Comparison Of Different Models 06: Dp=0.5000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.5000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.5000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.5000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.5000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.5000 m, Uniform Sands & Gravels, d=1 mm Dp=0.6000 m (about 24 inch) (1941 Hits) 11: Dp=0.6000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.6000 m, A Comparison Of Different Models 06: Dp=0.6000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.6000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 03: Dp=0.6000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.6000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.6000 m, Uniform Sands & Gravels, d=1 mm 04: Dp=0.6000 m, Graded Sands & Gravels, 9 Fractions Dp=0.7000 m (about 28 inch) (1561 Hits) 11: Dp=0.7000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.7000 m, A Comparison Of Different Models 06: Dp=0.7000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.7000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.7000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.7000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.7000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.7000 m, Uniform Sands & Gravels, d=1 mm Dp=0.7620 m (30 inch) (3884 Hits) 02: Dp=0.7620 m, Uniform Sands & Gravels, 9 Particle Diameters 03: Dp=0.7620 m, Graded Sands & Gravels, d=1 mm 10: Dp=0.7620 m, A Comparison Of Different Models 05: Dp=0.7620 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 06: Dp=0.7620 m, The Transition Heterogeneous-Homogeneous Flow Regimes 01: Dp=0.7620 m, Uniform Sands & Gravels, d=1 mm 04: Dp=0.7620 m, Graded Sands & Gravels, 9 Fractions 11: Dp=0.7620 m, Wasp, Wilson & SRC versus DHLLDV Dp=0.8000 m (about 32 inch) (1558 Hits) 11: Dp=0.8000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.8000 m, A Comparison Of Different Models 06: Dp=0.8000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.8000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.8000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.8000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.8000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.8000 m, Uniform Sands & Gravels, d=1 mm Dp=0.9000 m (about 36 inch) (1780 Hits) 11: Dp=0.9000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=0.9000 m, A Comparison Of Different Models 06: Dp=0.9000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=0.9000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=0.9000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=0.9000 m, Graded Sands & Gravels, d=1 mm 02: Dp=0.9000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=0.9000 m, Uniform Sands & Gravels, d=1 mm Dp=1.0000 m (about 40 inch) (1833 Hits) 11: Dp=1.0000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=1.0000 m, A Comparison Of Different Models 06: Dp=1.0000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=1.0000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=1.0000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=1.0000 m, Graded Sands & Gravels, d=1 mm 02: Dp=1.0000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=1.0000 m, Uniform Sands & Gravels, d=1 mm Dp=1.1000 m (about 44 inch) (3617 Hits) 11: Dp=1.1000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=1.1000 m, A Comparison Of Different Models 06: Dp=1.1000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=1.1000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=1.1000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=1.1000 m, Graded Sands & Gravels, d=1 mm 02: Dp=1.1000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=1.1000 m, Uniform Sands & Gravels, d=1 mm Dp=1.2000 m (about 48 inch) (1983 Hits) 11: Dp=1.2000 m, Wasp, Wilson & SRC versus DHLLDV 10: Dp=1.2000 m, A Comparison Of Different Models 06: Dp=1.2000 m, The Transition Heterogeneous-Homogeneous Flow Regimes 05: Dp=1.2000 m, The Limit Deposit Velocity, Slip Factor & The Bed Fraction 04: Dp=1.2000 m, Graded Sands & Gravels, 9 Fractions 03: Dp=1.2000 m, Graded Sands & Gravels, d=1 mm 02: Dp=1.2000 m, Uniform Sands & Gravels, 9 Particle Diameters 01: Dp=1.2000 m, Uniform Sands & Gravels, d=1 mm Summary with 6 pipe diameters (16930 Hits) 02 The Relative Excess Hydraulic Gradient, Cvt, Uniform Sands & Gravels 01 The Relative Excess Hydraulic Gradient, Cvs, Uniform Sands & Gravels 04 The Durand Froude number FL for the Limit Deposit Velocity, Uniform Sands & Gravels 05 The Bed Height & Slip Factor, Uniform Sands & Gravels 06B The Relative Excess Hydraulic Gradient, Graded Sands & Gravels, Cvt 08 Comparing 12 Models based on the transition heterogeneous-homogeneous 03 The Limit Deposit Velocity, Uniform Sands & Gravels 07 The Bed Height & Slip Factor, Graded Sands & Gravels 09 Comparing 22 Models based on the Relative Excess Hydraulic Gradient 06A The Relative Excess Hydraulic Gradient, Graded Sands & Gravels, Cvs 10 Comparing Heterogeneous Models based on the Relative Excess Hydraulic Gradient Experimental Data (257 Hits) Subpages: 1978 Kazanskij (14201 Hits) 01 Kazanskij (1978) Comparing Models 02 Silin et al. (1958) Sand ,Dp=0.103 m, d=0.38 mm 03 Silin et al. (1958) Sand ,Dp=0.206 m, d=0.34 mm 04 Silin et al. (1958) Sand ,Dp=0.410 m, d=0.27 mm 05 Silin et al. (1958) Sand ,Dp=0.614 m, d=0.30 mm 06 Silin et al. (1958) Sand ,Dp=0.800 m, d=0.30 mm 07 Silin et al. (1958) Sand ,Dp=0.900 m, d=0.30 mm 08 Fuhrboter (1961) Sand ,Dp=0.300 m, d=0.26 mm 09 Fuhrboter (1961) Sand ,Dp=0.300 m, d=0.44 mm 10 Fuhrboter (1961) Sand ,Dp=0.300 m, d=0.83 mm 11 Karasik (1973) Sand ,Dp=0.307 m, d=0.20 mm 12 Kazanskij (1978) Sand ,Dp=0.450 m, d=0.426 mm 1955 Newitt et al. (16591 Hits) 02 Newitt et al. (1955) Heterogeneous 01 Newitt et al. (1955) Flow Regimes 03 Newitt et al. (1955) Sliding Bed 04 Newitt et al. (1955) Coal 05 Newitt et al. (1955) Gravel 06 Newitt et al. (1955) MnO2 07 Newitt et al. (1955) Sand B 08 Newitt et al. (1955) Sand C 10 Newitt et al. (1955) Gravel E 09 Newitt et al. (1955) Sand D 1952 Durand & Condolios (15880 Hits) 07 Durand & Condolios (1952) All Experiments 08 Durand & Condolios (1955) Limit Deposit Velocity 06 Durand & Condolios (1952) Diameters & Concentrations 01 Durand & Condolios (1952) Dp=0.0406 m, d=0.04 mm 02 Durand & Condolios (1952) Dp=0.15 m, d=0.44 mm 03 Durand & Condolios (1952) Dp=0.15 m, d=2.04 mm 04 Durand & Condolios (1952) Dp=0.15 m, d=0.44 mm 05 Durand & Condolios (1952) Dp=0.15 m, d=2.04 mm 1955 Worster & Denny (1040 Hits) 01 Worster & Denny (1955) 1967 Zandi & Govatos (1093 Hits) 01 Zandi & Govatos (1967) All Data 1960 Gibert (16048 Hits) 07 Gibert (1960) All Experiments 08 Gibert (1960) Particle Froude Number 09 Gibert (1960) Limit Deposit Velocity 01 Gibert (1960) Sands & Gravels 02 Gibert (1960) Dp=0.15 m, d=0.20 mm 03 Gibert (1960) Dp=0.15 m, d=0.37 mm 04 Gibert (1960) Dp=0.15 m, d=0.89 mm 05 Gibert (1960) Dp=0.15 m, d=2.04 mm 06 Gibert (1960) Dp=0.15 m, d=4.2 mm 1977 Turian & Yuan (819 Hits) 01 Turian & Yuan (1977) correlations 1972 Yagi et al. (12904 Hits) 01 Yagi et al. (1972) Sand all 02 Yagi et al. (1972) Gravel all 03 Yagi et al. (1972) Limit Deposit Velocity 04 Yagi et al. (1972) Different Sands & Gravels 05 Yagi et al. (1972) Slip Ratio 06 Yagi et al. (1972) Coarse Sand, Dp=0.1552 m, d=0.91 mm. 07 Yagi et al. (1972) Gravel, Dp=0.0807 m, d=8.00 mm. 1906 Blatch (2526 Hits) 01 Blatch (1906) Two Sands 02 Blatch (1906) d=0.20 mm 03 Blatch (1906) d=0.55 mm 04 Blatch (1906) d=0.20 mm Copper Pipe 05 Blatch (1906) d=0.55 mm Copper Pipe 06 Blatch (1906) d=0.55 mm Steel Pipe 1970 Babcock (1942 Hits) 01 Babcock (1970) All Data 02 Babcock (1970) Concentrations 03 Babcock (1970) Figure 7 & 8 04 Babcock (1970) Figure 9 1937 OBrien & Folsom (1163 Hits) 01 OBrien & Folsom (1937) Homogeneous Transport d=0.17 mm 02 OBrien & Folsom (1937) Homogeneous Transport d=0.27 mm 1952 Soleil & Ballade (2528 Hits) 01 Soleil & Ballade (1952) Dp=0.58 m, d=0.45 mm 02 Soleil & Ballade (1952) Dp=0.58 m, d=0.55 mm 03 Soleil & Ballade (1952) Dp=0.58 m, d=0.64 mm 04 Soleil & Ballade (1952) Dp=0.70 m, d=0.45 mm 05 Soleil & Ballade (1952) Dp=0.70 m, d=0.55 mm 06 Soleil & Ballade (1952) Dp=0.70 m, d=0.64 mm 1961 Fuhrboter (12403 Hits) 02 Fuhrboter (1961) Dp=0.30 m, d=0.26 mm 03 Fuhrboter (1961) Dp=0.30 m, d=0.44 mm 04 Fuhrboter (1961) Dp=0.30 m, d=0.83 mm 01 Fuhrboter (1961) Sk & Skt 05 Fuhrboter (1961) LDV 1965 Thomas (749 Hits) 01 Thomas (1965) Apparent Viscosity 1976 Thomas (18458 Hits) 01 Thomas (1976) Coal ,Dp=0.0522 m, d=0.19 mm 02 Thomas (1976) Coal ,Dp=0.1075 m, d=0.19 mm 03 Thomas (1976) Coal ,Dp=0.1585 m, d=0.19 mm 04 Thomas (1976) Coal ,Dp=0.2085 m, d=0.19 mm 05 Thomas (1976) Coal ,Dp=0.2631 m, d=0.19 mm 06 Thomas (1976) Coal ,Dp=0.3150 m, d=0.19 mm 07 Thomas (1976) Iron Ore ,Dp=0.1075 m, d=0.04 mm 08 Thomas (1976) Iron Ore ,Dp=0.1585 m, d=0.04 mm 09 Thomas (1976) Iron Ore ,Dp=0.2085 m, d=0.04 mm 10 Thomas (1976) Iron Ore ,Dp=0.2631 m, d=0.04 mm 11 Thomas (1976) Iron Ore ,Dp=0.3150 m, d=0.04 mm 12 Thomas (1976) Sand ,Dp=0.0522 m, d=0.18 mm 13 Thomas (1976) Sand ,Dp=0.1075 m, d=0.18 mm 14 Thomas (1976) Sand ,Dp=0.1585 m, d=0.18 mm 15 Thomas (1976) Sand ,Dp=0.2631 m, d=0.18 mm 16 Thomas (1976) Sand ,Dp=0.3150 m, d=0.18 mm 17 Thomas (1976) Sand ,Dp=0.0522 m, d=0.48 mm 18 Thomas (1976) Sand ,Dp=0.1075 m, d=0.48 mm 1958 Silin et al. (15503 Hits) 06 Silin et al. (1958) Sand ,Dp=0.614 m, d=0.29 mm 08 Silin et al. (1958) Sand ,Dp=0.900 m, d=0.25 mm 07 Silin et al. (1958) Sand ,Dp=0.800 m, d=0.33 mm 01 Silin et al. (1958) Sand ,Dp=0.024 m, d=0.16 mm 02 Silin et al. (1958) Sand ,Dp=0.024 m, d=0.34 mm 03 Silin et al. (1958) Sand ,Dp=0.103 m, d=0.41 mm 04 Silin et al. (1958) Sand ,Dp=0.206 m, d=0.34 mm 05 Silin et al. (1958) Sand ,Dp=0.410 m, d=0.23 mm 1938 Howard (799 Hits) 01 Howard (1938) 1939 Siegfried (894 Hits) 01 Siegfried (1939) 1980 Kazanskij (1163 Hits) 01 Kazanskij (1980) Sand ,Dp=0.50 m, d=1.5 mm, Low Concentration 02 Kazanskij (1980) Sand ,Dp=0.50 m, d=1.5 mm, High Concentration 1987 Doron & Barnea (12411 Hits) 01 Doron & Barnea (1987) Acetal ,Dp=0.0508 m, d=3.0 mm, Cvt=0.05 02 Doron & Barnea (1987) Acetal ,Dp=0.0508 m, d=3.0 mm, Cvt=0.08 03 Doron & Barnea (1987) Acetal ,Dp=0.0508 m, d=3.0 mm, Cvt=0.12 04 Doron & Barnea (1987) Acetal ,Dp=0.0508 m, d=3.0 mm, Cvt=0.15 05 Doron & Barnea (1987) Acetal ,Dp=0.0508 m, d=3.0 mm, Cvt=0.187 06 Doron & Barnea (1987) Acetal, LSDV & Minimum Hydraulic Gradient 1971 Kazanskij (906 Hits) 01 Kazanskij (1971) Sand ,Dp=0.0508 m, d=0.2 mm 1967 Wiedenroth (2446 Hits) 01 Wiedenroth (1967) Sand ,Dp=0.125 m, d=2.2 mm, low concentration. 02 Wiedenroth (1967) Sand ,Dp=0.125 m, d=2.2 mm, high concentration. 03 Wiedenroth (1967) Gravel ,Dp=0.125 m, d=4.45 mm. 04 Wiedenroth (1967) Gravel ,Dp=0.125 m, d=5.95 mm. 05 Wiedenroth (1967) Sand ,Dp=0.125 m, d=0.2 mm. 06 Wiedenroth (1967) Sand ,Dp=0.125 m, d=0.9 mm. 1979 Boothroyde (2120 Hits) 01 Boothroyde (1979) Gravel ,Dp=0.20 m, d=4.3 mm. 02 Boothroyde (1979) Gravel ,Dp=0.20 m, d=10.0 mm. 03 Boothroyde (1979) Markham Fines ,Dp=0.20 m, d=0.20 mm. 04 Boothroyde (1979) Markham Fines ,Dp=0.20 m, d=0.20 mm, with Thomas (1965) viscosity. 1982 Clift (3214 Hits) 01 Clift (1982) Crushed Granite Narrow Graded ,Dp=0.2032 m, d=0.68 mm. 02 Clift (1982) Crushed Granite Narrow Graded ,Dp=0.44 m, d=0.68 mm. 03 Clift (1982) Crushed Granite Broad Graded ,Dp=0.2032 m, d=0.68 mm. 04 Clift (1982) Sand, Dp=0.49 m, d=0.60 mm. 06 Clift (1982) Masonry Sand, Dp=0.44 m, d=0.42 mm. 05 Clift (1982) Masonry Sand, Dp=0.2032 m, d=0.42 mm. 07 Clift (1982) Foundry Sand, Dp=0.2032 m, d=0.29 mm. 08 Clift (1982) Foundry Sand, Dp=0.44 m, d=0.29 mm. 2014 Vlasak (1017 Hits) 01 Vlasak (2014) Gravel, Dp=0.10 m, d=11.0 mm. Publications Slurry Transport (253 Hits) Subpages: DHLLDV Publications (618 Hits) Other Publications on Slurry Transport by S.A.Miedema (542 Hits) Publications by other authors (891 Hits) 2 Layer Model (16063 Hits) 01 Wilson (1992) Hydrostatic Stress Approach with the Televantos (1979) Bed Shear Stress Approach 02 Miedema & Ramsdell (2014) Normal Stress Approach with the Televantos (1979) Bed Shear Stress Approach 03 Miedema & Ramsdell (2014) Weight Approach with the Televantos (1979) Bed Shear Stress Approach 04 Wilson (1992) Hydrostatic Stress Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 05 Miedema & Ramsdell (2014) Normal Stress Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 06 Miedema & Ramsdell (2014) Weight Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 07 Summary: The Hydraulic Gradient, Cvs 08 Summary: The Relative Excess Hydraulic Gradient, Cvs 09 Summary: The Hydraulic Gradient, Cvt 10 Summary: The Relative Excess Hydraulic Gradient, Cvt 11 Summary: The Normalised ExcessHydraulic Gradient, Cvt 12 The Wilson (1992) & Wilson (1997) Fit Functions Animations (402 Hits) Subpages: Animations Large & Slow (845 Hits) Animations Small & Fast (825 Hits) 3 Layer Model + Download Excel Workbook (17011 Hits) 06 Miedema & Ramsdell (2014) Weight Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 12 Comparing 2LM & 3LM 01 Wilson (1992) Hydrostatic Stress Approach with the Televantos (1979) Bed Shear Stress Approach 02 Miedema & Ramsdell (2014) Normal Stress Approach with the Televantos (1979) Bed Shear Stress Approach 03 Miedema & Ramsdell (2014) Weight Approach with the Televantos (1979) Bed Shear Stress Approach 04 Wilson (1992) Hydrostatic Stress Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 05 Miedema & Ramsdell (2014) Normal Stress Approach with the Miedema & Matousek (2014) Bed Shear Stress Approach 07 Summary: The Hydraulic Gradient, Cvs 08 Summary: The Relative Excess Hydraulic Gradient, Cvs 09 Summary: The Hydraulic Gradient, Cvt 10 Summary: The Relative Excess Hydraulic Gradient, Cvt 11 Summary: The Normalised ExcessHydraulic Gradient, Cvt

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