Pore water density in a saturated bentonite

This paper reports the average pore water density (ρwp) measured on a Japanese bentonite, which was compacted to a dry density (ρd) range from 0.3 to 1.8 Mg/m3 and saturated under a water pressure of 2.7 MPa. It was found that ρwp monotonically increased from ∼1.0 Mg/m3 at ρd of 0.3 Mg/m3 to ∼1.23 Mg/m3 at ρd of 1.8 Mg/m3. Paper review shows methodology of accurately measuring ρwp in a full range of water content (w) is not available. An upper boundary of ρwp for montmorillonite was drawn, and proportions of water at different swelling states were estimated.