2004
DOI: 10.1023/b:mete.0000029874.77156.7b
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Macroscopic Fluctuations in the Density of Water

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Cited by 4 publications
(4 citation statements)
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“…Another picture is formed when the minimal admissible concentration difference between the touching water objects with different compositions is high enough for the interphase tension to be higher than the elasticity coefficient of the grid of hydrogen bridges. In such cases, judging by laboratory data (11,12), turbulent mass transport forms near the phase interface, accompanied by density fluctuations, protuberance formation, opalescence, and an increase in the megahertz dielectric permittivity. Such phenomena should be expected in the zones near sites where high-pollution wastewater is discharged into river flow.…”
Section: Discussionmentioning
confidence: 99%
“…Another picture is formed when the minimal admissible concentration difference between the touching water objects with different compositions is high enough for the interphase tension to be higher than the elasticity coefficient of the grid of hydrogen bridges. In such cases, judging by laboratory data (11,12), turbulent mass transport forms near the phase interface, accompanied by density fluctuations, protuberance formation, opalescence, and an increase in the megahertz dielectric permittivity. Such phenomena should be expected in the zones near sites where high-pollution wastewater is discharged into river flow.…”
Section: Discussionmentioning
confidence: 99%
“…They provide measurement accuracy with an accuracy of δ0 = ±0.02%. The most accurate calibration tool is the primary standard with the error δ0 = 2•10 -4 % [19].…”
Section: Discussionmentioning
confidence: 99%
“…The density of water varies within ±0.0000135g/cm 3 . This value can significantly affect the sensor reading, causing an error of 0.00135% [19].…”
Section: Discussionmentioning
confidence: 99%
“…The wood samples were then placed into the capsule and submerged into the water making sure to lower the capsule to the same level as it was zeroed. The reading on the OHAUS scale was recorded as the volume of the sample after determining the proper density of the water at room temperature (20 ºC), which was done by treating the scale reading as unitless and multiplying that reading by the density of water at 20 ºC (0.998199 g/cm 3 ) (Aleksandrov et al 2004). Density samples were oven-dried at 105 ºC until a constant mass was achieved.…”
Section: Wood Densitymentioning
confidence: 99%