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Study on the Behavior of Colloidal Hematite: Effects of Ionic Composition and Strength and Natural Organic Matter in Aqueous Environments

Authors
Lee, Woo-ChunLee, Sang-WooKim, Soon-Oh
Issue Date
Aug-2020
Publisher
KOREA SOC ECONOMIC & ENVIRONMENTAL GEOLOGY
Keywords
colloidal hematite; behavior; aqueous environment; ionic composition and strength; natural organic matter
Citation
ECONOMIC AND ENVIRONMENTAL GEOLOGY, v.53, no.4, pp 347 - 362
Pages
16
Indexed
SCOPUS
ESCI
KCI
Journal Title
ECONOMIC AND ENVIRONMENTAL GEOLOGY
Volume
53
Number
4
Start Page
347
End Page
362
URI
https://scholarworks.gnu.ac.kr/handle/sw.gnu/6364
DOI
10.9719/EEG.2020.53.4.347
ISSN
1225-7281
2288-7962
Abstract
Iron (hydro)oxides in aqueous environments are primarily formed due to mining activities, and they are known to be typical colloidal particles disturbing surrounding environments. Among them, hematites are widespread in surface environments, and their behavior is controlled by diverse factors in aqueous environments. This study was conducted to elucidate the effect of environmental factors, such as ionic composition and strength, pH, and natural organic matter (NOM) on the behavior of colloidal hematite particles. In particular, two analytical methods, such as dynamic light scattering (DLS) and single-particle ICP-MS (spICP-MS), were compared to quantify and characterize the behavior of colloidal hematites. According to the variation of ionic composition and strength, the aggregation/dispersion characteristics of the hematite particles were affected as a result of the change in the thickness of the diffuse double layer as well as the total force of electrostatic repulsion and van der Walls attraction. Besides, the more dispersed the particles were, the farther away the aqueous pH was from their point of zero charge (PZC). The results indicate that the electrostatic and steric (structural) stabilization of the particles was enhanced by the functional groups of the natural organic matter, such as carboxyl and phenolic, as the NOM coated the surface of colloidal hematite particles in aqueous environments. Furthermore, such coating effects seemed to increase with decreasing molar mass of NOM. On the contrary, these stabilization (dispersion) effects of NOM were much more diminished by divalent cations such as Ca2+ than monovalent ones (Na+), and it could be attributed to the fact that the former acted as bridges much more strongly between the NOM-coated hematite particles than the latter because of the relatively larger ionic potential of the former. Consequently, it was quantitatively confirmed that the behavior of colloidal hematites in aqueous environments was significantly affected by diverse factors, such as ionic composition and strength, pH, and NOM. Among them, the NOM seemed to be the primary and dominant one controlling the behavior of hematite colloids. Meanwhile, the results of the comparative study on DLS and spICP-MS suggest that the analyses combining both methods are likely to improve the effectiveness on the quantitative characterization of colloidal behavior in aqueous environments because they showed different strengths: the main advantage of the DLS method is the speed and ease of the operation, while the outstanding merit of the spICP-MS are to consider the shape of particles and the type of aggregation.
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