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Boise Sandstone

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Journal Article
Journal: Interpretation
Published: 18 April 2016
Interpretation (2016) 4 (2): SF55–SF65.
... relaxivity, which links relaxation time and pore size, varies within the pore system. To analyze and alter pore surface relaxivity, we saturated Boise sandstone cores with positively charged zirconia nanoparticle dispersions in which nanoparticles can be adsorbed onto the sandstone pore wall, while...
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<b>Boise</b> <b>sandstone</b> secular relaxation distributions. Secular relaxation at eac...
Published: 23 September 2016
Figure 6. Boise sandstone secular relaxation distributions. Secular relaxation at each echo spacing was characterized by the volume-weighted mean value of each distribution; these secular relaxation means decrease for larger τ .
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<b>Boise</b> <b>sandstone</b> inverse volumetrically weighted mean secular relaxation val...
Published: 23 September 2016
Figure 10. Boise sandstone inverse volumetrically weighted mean secular relaxation values measured as a function of echo spacing with a superposed best-fit line. The slope of this best-fit line indicates an internal gradient of G = 0.0671    T / m .
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The      T  1      distribution of <b>Boise</b> <b>sandstone</b> cores saturated with pur...
Published: 18 April 2016
Figure. 2. The T 1 distribution of Boise sandstone cores saturated with pure fluids at different pH values: core 1 saturated with DI water at pH 6.98, core 2 saturated with HNO 3 at pH 3.13, core 3 also saturated with HNO 3 at pH 3.13, core 4 saturated with TMAH
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The       T    1       distribution of <b>Boise</b> <b>sandstone</b> cores 9 and 10 after...
Published: 18 April 2016
Figure. 4. The T 1 distribution of Boise sandstone cores 9 and 10 after flushing with two pore volumes of DI water and TMAH at pH 9.07, respectively.
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The       T    1       distributions of <b>Boise</b> <b>sandstone</b> cores 7 and 8 after...
Published: 18 April 2016
Figure. 6. The T 1 distributions of Boise sandstone cores 7 and 8 after flushing with two pore volumes of DI water and HNO 3 at pH 3.13, respectively.
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Change in length of <b>Boise</b> <b>sandstone</b> as function of internal and external pr...
Published: 01 August 1958
Fig. 2. Change in length of Boise sandstone as function of internal and external pressure.
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V   P   and  V   S   as function of pressure in Berea and <b>Boise</b> <b>sandstones</b>....
Published: 01 February 2001
Figure 8. V P and V S as function of pressure in Berea and Boise sandstones. The measurements were made at room dry conditions. Velocity in Berea increases significantly with pressure; it does not change much in Boise.
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PSEUDO BULK VOLUME COMPRESSIBILITIES OF <b>BOISE</b> <b>SANDSTONES</b>
Published: 01 August 1958
Table V. PSEUDO BULK VOLUME COMPRESSIBILITIES OF BOISE SANDSTONES
Journal Article
Published: 01 February 2008
The Canadian Mineralogist (2008) 46 (1): 277–278.
... Valley” (Fig. 7.6), or “Shale overlying sandstone in Colorado” (Fig. 8.12)? Errors of spelling are rare, but a dandy is found on Fig. 2.9. Some of the 19 th -century dates on pages 2–7 have mistakenly been transposed into the 20 th and the Black Hills are not to the west of Wyoming (p. 6). Careful...
Journal Article
Journal: Geophysics
Published: 22 April 2009
Geophysics (2009) 74 (3): E125–E133.
... River Plain, Idaho : Idaho Geological Survey Bulletin, 29 . Pettyjohn F. Potter P. Siever R. , 1973 , Sand and sandstone : Springer-Verlag New York, Inc. Reboulet E. C. Barrash W. , 2003 , Core, grain-size, and porosity data from the Boise Hydrogeophysical Research...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1059–1073.
... or impossible. In this paper, we use porosity data from well logs and grain-size distribution (GSD) data from core to investigate four pebble- and cobble-dominated units that have been identified in porosity logs in deposits at a research well field (Boise Hydrogeophysical Research Site). Lacking direct...
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Journal Article
Published: 01 September 2006
Journal of Environmental and Engineering Geophysics (2006) 11 (3): 171–184.
...William P. Clement; Warren Barrash Abstract To determine the distribution of heterogeneities in the saturated zone of an unconfined aquifer in Boise, ID, we compute tomograms for three adjacent well pairs. The fluvial deposits consist of unconsolidated cobbles and sands. We used a curved-ray...
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