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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
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| chapter = Capillary pressure
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| frompg  = 221
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| topg    = 225
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| author  = Charles L. Vavra, John G. Kaldi, Robert M. Sneider
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| editor = ''Needs editor''
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| link    = http://archives.datapages.com/data/specpubs/methodo1/data/a095/a095/0001/0200/0221.htm
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| pdf    = http://archives.datapages.com/data/specpubs/methodo1/images/a095/a0950001/0200/02210.pdf
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}}
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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>).
      
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