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dodecane

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Plot showing the horizontal permeability to dodecane measured in samples from the organic-rich siliceous mudstone (sample PN3-108; squares) and dolomitic calcareous sandstone (sample PND-17; circles) lithofacies (as examples) at the effective stress conditions specified in our test program (see Figure 4). The arrows indicate the direction of loading and unloading paths. The vertical, gray-shaded rectangle represents the range of in situ mean effective stresses (σ′m) (1038 [7.16 MPa]–1665 psi [11.48 MPa]) inferred for the depths of the samples tested. The relationship between permeability and effective stress during the second unloading path (tests 4–6) is given by fitting the exponential relationship: k = k0 exp (−α (Pc − Pp) (Best and Katsube, 1995). In sample PND-17, the coefficients are k0 = 2122 nd and α = 0.0010 MPa−1 (coefficient of determination [R2] = 0.94) (gray dotted line); in sample PN3-108, the coefficients are k0 = 149 nd and α = 0.0366 MPa−1 (R2 = 0.83) (gray dashed line). Pc = confining pressure; Pp = pore pressure.
Published: 01 February 2024
Figure 7. Plot showing the horizontal permeability to dodecane measured in samples from the organic-rich siliceous mudstone (sample PN3-108; squares) and dolomitic calcareous sandstone (sample PND-17; circles) lithofacies (as examples) at the effective stress conditions specified in our test
Image
Horizontal effective matrix permeability to dodecane (km) of all of the samples measured by lithofacies. For each lithofacies, the top and bottom lines represent the maximum and minimum values, respectively. The top and bottom edges of the gray box mark the first and third percentiles, respectively. The median value is the horizontal line within the box. Values that fall beyond the lower limit (25th percentile − 1.5 × interquartile range) and the upper limit (75th percentile + 1.5 × interquartile range) represent outliers. The n represents the number of permeability measurements conducted at confining pressure (Pc) − pore pressure (Pp) = 4500 psi (cross) and Pc − Pp = 8500 psi (circles) per lithofacies.
Published: 01 February 2024
Figure 9. Horizontal effective matrix permeability to dodecane ( k m ) of all of the samples measured by lithofacies. For each lithofacies, the top and bottom lines represent the maximum and minimum values, respectively. The top and bottom edges of the gray box mark the first and third
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Pressure drop vs. time for a dodecane displacement of water. The saturation distributions in pictures A–E correspond with the letters on the line plot.
Published: 01 November 2012
Fig. 2. Pressure drop vs. time for a dodecane displacement of water. The saturation distributions in pictures A–E correspond with the letters on the line plot.
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2024
AAPG Bulletin (2024) 108 (2): 293–326.
...Figure 7. Plot showing the horizontal permeability to dodecane measured in samples from the organic-rich siliceous mudstone (sample PN3-108; squares) and dolomitic calcareous sandstone (sample PND-17; circles) lithofacies (as examples) at the effective stress conditions specified in our test...
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Journal Article
Published: 01 November 2012
Vadose Zone Journal (2012) 11 (4): vzj2012.0024.
...Fig. 2. Pressure drop vs. time for a dodecane displacement of water. The saturation distributions in pictures A–E correspond with the letters on the line plot. ...
FIGURES | View All (10)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 2011
AAPG Bulletin (2011) 95 (4): 537–558.
... of Compounds Extracted from Cuttings Sampled in the Interval 4953 to 5099 m (16,250–16,729 ft) and (B) Pyrolyzed to 600°C and (C) 1000°C* (A) 4953–5099 m Nonpyrolysis Extraction Rt GC-MS Qual % 15.80 Dodecane 96 5.05 17.36 Tridecane 97 48.83 18.81 Tetradecane 98 31.46...
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Journal Article
Published: 01 November 2004
Vadose Zone Journal (2004) 3 (4): 1276–1285.
...Patrick Höhener; Heinz Surbeck Abstract The potential use of the naturally occurring noble gas 222 Rn as a tracer for vadose zone contamination by nonaqueous phase liquids (NAPLs) is studied experimentally and theoretically. n -Dodecane was chosen as the model NAPL. In batch experiments containing...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1995
AAPG Bulletin (1995) 79 (1): 19–28.
... overlying a source rock. A dyed oil (dodecane) was injected into the lowest corner at a rate of 1 cm 3 /day, and it exited the highest corner at atmospheric pressure. Oil movement was followed visually, and average oil saturations through the 2.5-cm thickness of the model were determined by ultrasonic...
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Journal Article
Published: 01 May 2004
Vadose Zone Journal (2004) 3 (2): 592–601.
... 0.18 water without dye 2 II: Blob velocity acrylic 20, 85 0.25 n-dodecane injected manually
   with syringe III: Rivulet width glass 20 0.25 dyed water 5, 10, 27 glass 85 0.25 dyed water 5, 10, 27, 56 acrylic 20, 85 0.25 dyed water 5, 10, 27, 56 IV: Rivulet flow...
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Journal Article
Published: 01 February 2005
Vadose Zone Journal (2005) 4 (1): 163–174.
... saturation S lr 0.08 0.17 Max. entrapped NAPL saturation, S̅ ne max 0.232 0.154 Max. residual NAPL saturation, S̅ nr max 0.106 0.232 Table 4. Fluid properties of the NAPLs used in the transient column experiments. Property Soltrol 220 Dodecane NAPL...
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Journal Article
Journal: Interpretation
Published: 18 May 2022
Interpretation (2022) 10 (3): SD61–SD74.
... the air in the sample chamber and the pore of the rock. The relative vacuum degree reached 75 kPa for 48 h. Then, n-dodecane was injected into the sample chamber under pressure. The pressure was maintained at 15 MPa for 48 h. The saturated samples were removed from the sample chamber, placed in a sealed...
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Journal Article
Published: 01 November 2020
Russ. Geol. Geophys. (2020) 61 (11): 1260–1282.
... 9 H 18 O 2 ); 23, Tridecane (C 13 H 28 ); 24, Thiophene, 3-heptyl- (C 11 H 18 S); 25, Decanoic acid (C 10 H 20 O 2 ); 26, Dodecanal (C 12 H 24 O); 27, 1-Tetradecane (C 14 H 28 ); 28, Tetradecane (C 14 H 30 ); 29, Thiophene, 2-octyl- (C 12 H 20 S); 30, 2-Tridecanone (C 13 H 26 O); 31, 1-Pentadecene...
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Image
Drainage capillary pressure and pore throat size distribution curves in samples tested for permeability. (A, B) Organic-rich siliceous mudstone samples PN5-12 (km = 7 to 9 nd) and PN3-108 (km = 22 to 29 nd). (C, D) Sample PND-3 (km < 1 nd) from the argillaceous mudstone lithofacies. (E, F) Sample PN4-18-1 (km = 422–508 nd) from the dolomitic calcareous mudstone lithofacies, and sample PND-17 (km = 2004–2041 nd) from the dolomitic calcareous sandstone lithofacies. Curves were obtained using mercury injection capillary pressure (MICP) measurements on whole sample in PN5-12, and crushed samples in PN3-108, PND-3, PN4-18-1, and PND-17. ϕHg = MICP porosity; Dt = modal pore throat diameter; km = horizontal effective matrix permeability to dodecane; Pde = extrapolated displacement pressure determined from a hyperbolic fit to the displacement curve and its projection to a horizontal asymptote (see Thomeer, 1960); Pt = threshold pressure; Vp = pore volume.
Published: 01 February 2024
in PN5-12, and crushed samples in PN3-108, PND-3, PN4-18-1, and PND-17. ϕ Hg = MICP porosity; D t = modal pore throat diameter; k m = horizontal effective matrix permeability to dodecane; P de = extrapolated displacement pressure determined from a hyperbolic fit to the displacement curve
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Total ionic current (TIC) chromatogram of volatiles from fluid inclusions in diamond from the Pozdnyaya kimberlite pipe, Luchakan field (a) and reconstructed ion chromatograms for the current of ions with: b, m/z (43 + 57 + 71 + 85); c, m/z 60; d, blank control sample. 1, carbon dioxide (CO2); 2, water (H2O); 3, propanal (C3H6O); 4, butanal (C4H8O); 5, acetic acid (C2H4O2); 6, pentanal (C5H10O); 7, 1-heptene (C7H14); 8, heptane (C7H16); 9, hexanal (C6H12O); 10, butanoic acid (C4H8O2); 11, 3-octene, (E)-(C8H16); 12, 3-octene, (Z)-(C8H16); 13, octane (C8H18); 14, butanoic acid, 3-methyl- (C5H10O2); 15, heptanal (C7H14O); 16, pentanoic acid (C5H10O2); 17, benzaldehyde (C7H6O); 18, nonane (C9H20); 19, hexanoic acid (C6H12O2); 20, 1-hexanol, 2-ethyl-(C8H18O); 21, heptanoic acid (C7H14O2); 22, nonanal (C9H18O); 23, octanoic acid (C8H16O2); 24, decanal (C10H20O); 25, dodecane (C12H26); 26, nonanoic acid (C9H18O2); 27, undecanal (C11H22O); 28, n-decanoic acid (C10H20O2); 29, dodecanal (C12H24O); 30, tetradecane (C14H30); 31, 2-tridecanone (C13H26O); 32, tridecanal (C13H26O); 33, 1-pentadecene (C15H30); 34, pentadecane (C15H32); 35, dodecanoic acid (C12H24O2); 36, tetradecanal (C14H28O); 37, tridecanoic acid (C13H26O2); 38, 2-pentadecanone (C15H30O); 39, pentadecanal (C15H30O); 40, tetradecanoic acid (C14H28O2).
Published: 01 October 2018
O 2 ); 22, nonanal (C 9 H 18 O); 23, octanoic acid (C 8 H 16 O 2 ); 24, decanal (C 10 H 20 O); 25, dodecane (C 12 H 26 ); 26, nonanoic acid (C 9 H 18 O 2 ); 27, undecanal (C 11 H 22 O); 28, n -decanoic acid (C 10 H 20 O 2 ); 29, dodecanal (C 12 H 24 O); 30, tetradecane (C 14 H 30 ); 31, 2
Journal Article
Published: 01 November 2004
Vadose Zone Journal (2004) 3 (4): 1262–1275.
... 114.23  1.88 9 121.0 9 5.15 11    0.66 11 0.55  Decane 15.99 0.730 148.28  0.175 9 197.85 10 6.25 11    0.052 11 0.49  Dodecane  9.50 0.749 170.34  0.0157 9 296.77 10 7.24 11    0.0037 11 0.44 Cycloalkanes  Methyl-cyclo-pentane  5.79 0.7486  84.16...
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Journal Article
Journal: Clay Minerals
Published: 10 January 2022
Clay Minerals (2021) 56 (3): 250–259.
... and small d 003 values are 26.25 and 32.18 kJ mol –1 , respectively. For the reaction mechanism experiment, CHCA was dissolved in n-dodecane. After reaction at 423 K for 2 h, the liquid was separated from the suspension via filtration and analysed using gas chromatography and mass spectroscopy (GC-MS...
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Journal Article
Published: 01 October 2021
Russ. Geol. Geophys. (2021) 62 (10): 1157–1174.
... (C 10 H 8 ); 24. Octanoic acid (C 8 H 16 O 2 ); 25. Decanal (C 10 H 20 O); 26. Nonanoic acid (C 9 H 18 O 2 ); 27. Undecanal (C 11 H 22 O); 28. Decanoic acid (C 9 H 20 O 2 ); 29. Dodecanal (C 12 H 24 O); 30. 1-Pentadecene (C 15 H 30 ); 31. Pentadecane (C 15 H 32 ); 32. Undecanoic acid (C 11 H 22 O 2...
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Journal Article
Published: 01 May 2006
Vadose Zone Journal (2006) 5 (2): 570–598.
... × 10.5 × 0.25 Plexiglas dodecane saturated both Conrad et al., 2002 surfactant flushing, in situ chemical oxidation 60.5 × 60 × 1 glass trichloroethene saturated heterogeneous Dai and Reitsma, 2002 in situ chemical oxidation 86 × 30 × 2.8 F: glass B: aluminum tetrachloroethene...
Journal Article
Journal: Elements
Published: 01 August 2014
Elements (2014) 10 (4): 271–276.
... Ford samples have a relatively low V/Mo ratio, indicating more oxic conditions. The stratigraphic distribution of the samples using a 20 ppm Mo cut-off for anoxic sediments is displayed on the right (after Piper and Calvert 2009 ). Depth is in feet. Imbibition experiments with dodecane...
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Journal Article
Published: 01 November 2000
Russ. Geol. Geophys. (2000) 41 (11): 1539–1553.
... 0.88 0.85 0.64 n -Undecane (C 11 H 24 ) 1.00 0.62 0.80 0.76 0.58 n -Dodecane (C 12 H 26 ) 0.91 0.52 0.69 0.71 0.53 n -Tridecane (C 13 H 28 ) 0.85 0.45 0.59 0.63 0.53 n -Tetradecane (C 14 H 30 ) 0.79 0.42 0.55 0.59 0.50 n -Pentadecane (C 15 H 32 ) 0.75 0.43...
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