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采用不对称流场流分离-多检测技术对火山灰纳米颗粒进行表征,并研究其在水介质中的归宿。

Characterization of volcanic ash nanoparticles and study of their fate in aqueous medium by asymmetric flow field-flow fractionation-multi-detection.

机构信息

IUniversité de Pau et des Pays de l'Adour/E2S UPPA, CNRS, Institut des Sciences Analytiques et de Physico-Chimie pour l'Environnement et les Matériaux (IPREM), UMR 5254, Helioparc, 2 Avenue Pierre Angot, 64053, Pau Cedex, 9, France.

National University of Science and Technology 'MISIS', Moscow, 119049, Russia.

出版信息

Environ Sci Pollut Res Int. 2021 Jun;28(24):31850-31860. doi: 10.1007/s11356-021-12891-0. Epub 2021 Feb 22.

Abstract

Dimensional and elemental characterization of environmental nanoparticles is a challenging task that requires the use of a set of complementary analytical methods. Asymmetric flow field-flow fractionation coupled with UV-Vis, multi-angle laser light scattering and ICP-MS detection was applied to study the nanoparticle fraction of a volcanic ash sample, in a Milli-Q water suspension at pH 6.8. It has been shown that the separated by sedimentation nanoparticle fraction of the Klyuchevskoy volcano ash suspension contains 3 polydisperse populations for which size ranges (expressed in gyration radius, rG), hydrodynamic behaviours (evaluated via shape index) and elemental compositions are different. These 3 populations did not dissolve over the 72-h study but aggregated and settled out differently. Thus, the population of particles with gyration radii <140 nm (P1), which contained 6% AlO and represented approximately 20% by mass of the nanoparticle fraction, remained in suspension without observable aggregation. The populations P2 and P3, which represented 67% and 13% by mass in the initial suspension, covered the rG range 25-250 nm and contained 17% and 15% AlO, respectively. Over time, populations P2 and P3 aggregated and their concentration in suspension at 72 h decreased by approximately 40% compared with the initial suspension. The decrease of these nanoparticle populations occurred either from the beginning of the temporal monitoring (P2) or after 30 h (P3). Aggregation generated a new population (P4) in suspension with rG up to 300 nm and mostly consisting of P2. This population represented only up to 6 to 7% of the nanoparticle fraction and decreased beyond 50 h. As a result, the trace elements present in the nanoparticle fraction and monitored (Cu and La) were also no longer found in the suspension. The results obtained can offer additional insights into the fate of volcanic ash nanoparticles in the environment.

摘要

环境纳米颗粒的维度和元素特征是一项具有挑战性的任务,需要使用一系列互补的分析方法。本文采用不对称流场流分离技术与紫外-可见、多角度激光光散射和 ICP-MS 检测联用的方法,研究了在 pH 值为 6.8 的 Milli-Q 水悬浮液中,火山灰样品的纳米颗粒部分。结果表明,沉降分离得到的火山灰悬浮液纳米颗粒部分包含 3 个多分散群体,它们的粒径范围(以回转半径 rG 表示)、流体力学行为(通过形状指数评估)和元素组成均不同。这 3 个群体在 72 小时的研究过程中并未溶解,而是以不同的方式聚集和沉降。因此,回转半径小于 140nm 的颗粒群体(P1)在悬浮液中保持稳定,没有观察到明显的聚集,其包含 6%的 AlO,占纳米颗粒部分的质量约为 20%。而 P2 和 P3 群体则分别代表初始悬浮液中 67%和 13%的质量,覆盖了 25-250nm 的 rG 范围,分别含有 17%和 15%的 AlO。随着时间的推移,P2 和 P3 群体发生聚集,其在 72 小时悬浮液中的浓度比初始悬浮液下降了约 40%。这些纳米颗粒群体的减少要么从时间监测开始(P2),要么在 30 小时后(P3)发生。聚集产生了一个新的悬浮颗粒群体(P4),其回转半径高达 300nm,主要由 P2 组成。该群体仅占纳米颗粒部分的 6%至 7%,并在 50 小时后减少。结果,纳米颗粒部分中监测到的微量元素(Cu 和 La)也不再存在于悬浮液中。研究结果可为深入了解火山灰纳米颗粒在环境中的归宿提供更多的认识。

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