2014
DOI: 10.1016/j.clay.2014.10.004
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Effects of humic acid release from sepiolite on the interfacial and rheological properties of alkaline dispersions

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Cited by 10 publications
(9 citation statements)
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“…Their formation and hydrodynamic sizes are strongly influenced by ionic size and metal ions (Von Wandruszka et al, 1997), especially Mg 2+ and Ca 2+ ions, pH and ionic strength. It is worth noting that although such structures of HAs could be responsible for the thermodynamically stable sepiolite suspensions (inhibited gel formation) in natural system as represented in Figure 12 and their sizes determined by Benli (2014), were also directly observed by high-resolution AFM images, were also changed in the range of 18-63  8 nm at pH 11.5. In an early review (Frenkel et al, 1992;Tarchitzky et al, 1993), it was shown that humic and fulvic acids were added to reference clay suspensions, which always increased colloidal stability.…”
Section: Discussionmentioning
confidence: 96%
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“…Their formation and hydrodynamic sizes are strongly influenced by ionic size and metal ions (Von Wandruszka et al, 1997), especially Mg 2+ and Ca 2+ ions, pH and ionic strength. It is worth noting that although such structures of HAs could be responsible for the thermodynamically stable sepiolite suspensions (inhibited gel formation) in natural system as represented in Figure 12 and their sizes determined by Benli (2014), were also directly observed by high-resolution AFM images, were also changed in the range of 18-63  8 nm at pH 11.5. In an early review (Frenkel et al, 1992;Tarchitzky et al, 1993), it was shown that humic and fulvic acids were added to reference clay suspensions, which always increased colloidal stability.…”
Section: Discussionmentioning
confidence: 96%
“…This does not necessarily mean that HA molecules and their metal complexes are sorbed within the micropores. Because of the small size of micropores (<2 nm), penetration of HA molecules with a radius of gyration of 2.1 nm (Österberg et al, 1993) and their metal complexes which have the size range of 18-63  8 nm at pH 11.5 (Benli, 2014), seems unlikely. A more reasonable explanation is sorption at the mouths of such pores or their blocking of sepiolite's micro/meso pores for larger structured pseudomicellar domains by organic macromolecules or both.…”
Section: Discussionmentioning
confidence: 99%
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“…During contact mode measurements, NSC36/Cr-Au type of cantilevers was selected. Before measurements, all samples were specifically prepared similarly to our previous study (12). Briefly, one drop of 1% of sepiolite dispersion contains Ag-NPs (theoretically 50 mg/L silver content) were dropped on the cleavage of fresh mica substrate.…”
Section: Atomic Force Microscopy (Afm) Studiesmentioning
confidence: 99%
“…Size Measurement Procedure: The depositing procedure on high-quality mica was previously defined for sepiolite fibers [24], montmorillonite, and smectite type clay minerals [25,26]. To spread precipitated Fe and Zn suspension (0.1 g in 50 ml H2O), a dilute suspension of 1 ml was dropped on the freshly cleaved mica surface followed by drying the sample in a Petri dish at room conditions for 24 hours.…”
Section: Atomic Force Microscopy (Afm) Imaging Andmentioning
confidence: 99%