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Direct observation of anisotropic growth of water films on minerals driven by defects and surface tension

机译:直接观察缺陷和表面张力驱动的矿物膜的各向异性生长

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Knowledge of the occurrences of water films on minerals is critical for global biogeochemical and atmospheric processes, including element cycling and ice nucleation. The underlying mechanisms controlling water film growth are, however, misunderstood. Using infrared nanospectroscopy, amplitude-modulated atomic force microscopy, and molecular simulations, we show how water films grow from water vapor on hydrophilic mineral nanoparticles. We imaged films with up to four water layers that grow anisotropically over a single face. Growth usually begins from the near edges of a face where defects preferentially capture water vapor. Thicker films produced by condensation cooling completely engulf nanoparticles and form thicker menisci over defects. The high surface tension of water smooths film surfaces and produces films of inhomogeneous thickness. Nanoscale topography and film surface energy thereby control anisotropic distributions and thicknesses of water films on hydrophilic mineral nanoparticles.
机译:对矿物质的水膜出现的了解对于全球生物地球化学和大气过程至关重要,包括元素循环和冰成核。然而,控制水膜生长的潜在机制是误解的。使用红外纳米谱检测,振幅调节原子力显微镜和分子模拟,我们展示了水膜如何从水蒸气中生长在亲水性矿物纳米粒子上。我们拍摄了多达四个水层的电影,这些水层在单个面上各向异性生长。生长通常从面部的近边缘开始,其中缺陷优先捕获水蒸气。通过冷凝冷却完全吞气纳米颗粒产生的厚膜,并形成较厚的半月形上过度的缺陷。水平滑膜表面的高表面张力并产生不均匀厚度的薄膜。纳米级地形和薄膜表面能量,从而控制亲水性矿物纳米颗粒上的各向异性分布和厚度的水膜。

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