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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. 相似文献
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Measurement of the friction coefficient of a fluctuating contact line using an AFM-based dual-mode mechanical resonator 下载免费PDF全文
A dual-mode mechanical resonator using an atomic force microscope (AFM) as a force sensor is developed. The resonator consists of a long vertical glass fiber with one end glued onto a rectangular cantilever beam and the other end immersed through a liquid-air interface. By measuring the resonant spectrum of the modified AFM cantilever, one is able to accurately determine the longitudinal friction coefficient ξv along the fiber axis associated with the vertical oscillation of the hanging fiber and the traversal friction coefficient ξh perpendicular to the fiber axis associated with the horizontal swing of the fiber around its joint with the cantilever. The technique is tested by measurement of the friction coefficient of a fluctuating (and slipping) contact line between the glass fiber and the liquid interface. The experiment verifies the theory and demonstrates its applications. The dual-mode mechanical resonator provides a powerful tool for the study of the contact line dynamics and the rheological property of anisotropic fluids. 相似文献
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采用一种新的相转移法制备了双层包裹的Fe3O4正己烷磁流体.首先,以油酸钠作为表面改性剂,对化学共沉淀制备的Fe3O4纳米颗粒进行双层包裹,制备了稳定的水基磁流体,在此基础上,通过加入乙酸(CH3COOH)将亲水颗粒转变为亲油颗粒,并用萃取的方法将亲油颗粒成功转移到正己烷相.傅里叶变换红外光谱(FTIR)表明,通过调整pH值可以将双层包裹的磁性颗粒外层带有的亲水基团油酸根R—COO-转变为亲油的R—COOH,从而使得包裹的颗粒既可溶于极性载液也可溶于非极性载液.利用X射线衍射仪(XRD)、振动样品强磁计(VSM)和透射电子显微镜(TEM)对Fe3O4颗粒的形貌、组成及磁流体的性质进行了表征.结果表明,利用这种新的相转移法可以保证颗粒在单分散下充分包裹并避免团聚.制备的正己烷磁流体稳定性好,长期放置未发生分层现象.通过蒸发正己烷,可以得到不同固含量的磁流体并可以将其与其它油基载液互溶,从而得到不同载液的Fe3O4油基磁流体. 相似文献
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提出探测复杂力学振动系统耦合振动模式的方法:通过测量力学振动系统中某一易于探测的振动模式对外力的响应行为,在该振动模式应变落后于应力的相位差-频率谱(表观机械能耗散-频率谱)中,除了能观察到与被测量振动模式本征频率所对应的相位变化外,与被测量振动模式耦合的其他振动模式也表现为共振吸收峰;从共振吸收峰的性质,如峰位、峰宽、峰高等可以得到相应耦合振动模式的本征频率、损耗以及耦合强度等信息.以倒扭摆力学系统为例,通过测量扭摆的扭转振动模式应变落后于应力的相位差-频率谱研究了扭摆系统中摆杆的进动振动模式. 相似文献
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