Difference between revisions of "Displacement pressure"

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The pressure at which mercury first enters the sample (after the mercury has filled any surface irregularities on the sample) is termed the ''displacement pressure'' (''P''<sub>d</sub>).<ref>Vavra, C.L., J. G. Kaldi, and R. M. Sneider, [http://archives.datapages.com/data/specpubs/methodo1/data/a095/a095/0001/0200/0221.htm Capillary pressure] in D. Morton-Thompson and A. M. Woods, eds., Development Geology Reference Manual: [http://store.aapg.org/detail.aspx?id=612 AAPG Methods in Exploration 10], p. 221-225.</ref>
| image  = development-geology-reference-manual.png
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| series  = Methods in Exploration
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==References==
| title  = Development Geology Reference Manual
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{{reflist}}
| part    = Laboratory methods
 
| chapter = Capillary pressure
 
| frompg  = 221
 
| topg    = 225
 
| author  = Charles L. Vavra, John G. Kaldi, Robert M. Sneider
 
| editor = ''Needs editor''
 
| link    = http://archives.datapages.com/data/specpubs/methodo1/data/a095/a095/0001/0200/0221.htm
 
| pdf    = http://archives.datapages.com/data/specpubs/methodo1/images/a095/a0950001/0200/02210.pdf
 
}}
 
The pressure at which mercury first enters the sample (after the mercury has filled any surface irregularities on the sample) is termed the ''displacement pressure'' (''P''<sub>d</sub>).
 
  
 
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Latest revision as of 14:13, 24 July 2014

The pressure at which mercury first enters the sample (after the mercury has filled any surface irregularities on the sample) is termed the displacement pressure (Pd).[1]

References

  1. Vavra, C.L., J. G. Kaldi, and R. M. Sneider, Capillary pressure in D. Morton-Thompson and A. M. Woods, eds., Development Geology Reference Manual: AAPG Methods in Exploration 10, p. 221-225.

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