Imaginary Part of the Surface Tension of Water
We report a direct measurement of the imaginary part of the surface tension of water through a dynamic scheme using a thin vertical glass fiber of diameter of 3 tun with one end glued onto a cantilever beam and the other end touching a water-air interface. The frequency dependence of the dissipation...
Saved in:
Published in | Chinese physics letters Vol. 31; no. 7; pp. 152 - 155 |
---|---|
Main Author | |
Format | Journal Article |
Language | English |
Published |
01.07.2014
|
Subjects | |
Online Access | Get full text |
ISSN | 0256-307X 1741-3540 |
DOI | 10.1088/0256-307X/31/7/076801 |
Cover
Summary: | We report a direct measurement of the imaginary part of the surface tension of water through a dynamic scheme using a thin vertical glass fiber of diameter of 3 tun with one end glued onto a cantilever beam and the other end touching a water-air interface. The frequency dependence of the dissipation factor experienced by the glass fiber is exactly calculated through measuring the phase delay with various frequencies when the glass fiber is forced to oscillate vertically. We find the same intercept at the dissipation factor axis for different frequency dependences of the dissipation factor for different depths by which the glass fiber is dipped into water. This nonzero dissipation factor at zero frequency presents direct evidence of the existence of the imaginary part of surface tension of water and yields a complex surface tension of water σ^* = 0.073 + i(0.017 ± 0.002) N/m at room temperature. |
---|---|
Bibliography: | XIONG Xiao-Min, CHEN Lan , ZUO Wen-Long, LI Long-Fei, YANG Yue-Bin, PANG Zhi-Yong, ZHANG Jin-Xiu( 1 School of Physics and Engineering, Sun Yat-Sen University, Guangzhou 510275 ; 2State Key Laboratory of Optoelectronic Materials and Technologies, Guangzhou 510275 ;3 Guangdong Provincial Key Laboratory of Photovoltaics Technologies, Guangzhou 510006 ;4School of Information Science and Technology, Sun Yat-Sen University, Guangzhou 510006) 11-1959/O4 We report a direct measurement of the imaginary part of the surface tension of water through a dynamic scheme using a thin vertical glass fiber of diameter of 3 tun with one end glued onto a cantilever beam and the other end touching a water-air interface. The frequency dependence of the dissipation factor experienced by the glass fiber is exactly calculated through measuring the phase delay with various frequencies when the glass fiber is forced to oscillate vertically. We find the same intercept at the dissipation factor axis for different frequency dependences of the dissipation factor for different depths by which the glass fiber is dipped into water. This nonzero dissipation factor at zero frequency presents direct evidence of the existence of the imaginary part of surface tension of water and yields a complex surface tension of water σ^* = 0.073 + i(0.017 ± 0.002) N/m at room temperature. ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0256-307X 1741-3540 |
DOI: | 10.1088/0256-307X/31/7/076801 |