10,323
edits
Changes
Jump to navigation
Jump to search
Line 1:
Line 1: − {{publication + − | image = development-geology-reference-manual.png+ − | series = Methods in Exploration+ − | title = Development Geology Reference Manual+ − | 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>).
no edit summary
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>
==References==
{{reflist}}
}}
{{stub}}
{{stub}}