首页> 外文会议>American Chemical Society Division of Environmental Chemistry Symposium >WATER VAPOR ABSORPTION IN THE POLYAMIDE ACTIVE LAYER OF REVERSE OSMOSIS (RO) MEMBRANES
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WATER VAPOR ABSORPTION IN THE POLYAMIDE ACTIVE LAYER OF REVERSE OSMOSIS (RO) MEMBRANES

机译:反渗透(RO)膜的聚酰胺活性层中的水蒸气吸收

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Many of the basic thermodynamic and physical properties of the active layers of interfacially polymerized membranes are essentially unknown. In this work, we use combined measurements of water uptake and biaxial stress as a function of relative humidity to gain insights on the interactions of water with a commercial reverse osmosis (RO) membrane, FT-30 manufactured by Dow Liquid Separation (Midland, Ml). The active layer of the commercial RO membranes is attached to either a quartz crystal microbalance or a glass cover-slip using cured polyimide as an adhesion layer. The polysulfone support layer of the membrane is then dissolved in DMF (N,N-dimethylformamide). We use a laser-scanning optical system to measure the changes in curvature of the glass cover-slip and in this way determine the changes in the biaxial stress of the polyamide layer created by swelling of the polyamide layer by water absorption. Both the microbalance sample and the stress sample are placed in a sealed box in which the humidity can be controlled. The mass change of the polyamide layer is 1.2 μg cm~(-2) when the humidity changes from 0% to 90% and the corresponding biaxial stress change is -35 MPa (compressive); this water uptake corresponds to 6% of the mass of the polyamide layer. The changes in water absorption with partial pressure of water vapor more closely resemble a Langmuir adsorption isotherm than the Flory-Huggins theory of polymer solutions. If we nevertheless use the Flory-Huggins theory to analyze the data, the interaction parameter at high humidity is χ~≈ 2, which is comparable to the value of % for nylon. Comparisons of water uptake and biaxial stress indicate that the partial specific volume of water is larger at high humidity than at low humidity.
机译:界面聚合膜的活性层的许多基本热力学和物理性质基本上是未知的。在这项工作中,我们使用的是水吸收和双轴应力的组合测量作为相对湿度的函数,以获得对水与商业反渗透(RO)膜的相互作用的洞察,由Dow液体分离制造的FT-30(Midland,ML )。使用固化的聚酰亚胺作为粘合层,将商业RO膜的活性层附着于石英晶体微迁移或玻璃盖滑移。然后将膜的聚砜支撑层溶解在DMF(N,N-二甲基甲酰胺)中。我们使用激光扫描光学系统来测量玻璃盖滑动曲率的变化,并以这种方式确定通过吸水溶胀聚酰胺层产生的聚酰胺层的双轴应力的变化。微稳态样品和应力样品都置于密封盒中,其中可以控制湿度。当湿度从0%变化至90%时,聚酰胺层的质量变化为1.2μgcm〜(-2),并且相应的双轴应力变化为-35MPa(压缩);该水吸收对应于聚酰胺层质量的6%。水蒸气部分压力的吸水变化更像是琅勃伦吸附等温,比聚合物溶液的绒毛 - Huggins理论。如果我们仍然使用麦伦 - Huggins理论来分析数据,高湿度的相互作用参数是χ〜≈2,其与尼龙的%相当。水吸收和双轴应力的比较表明,在低湿度下,部分特异的水体积大于低湿度。

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