2015
DOI: 10.4028/www.scientific.net/amr.1092-1093.635
|View full text |Cite
|
Sign up to set email alerts
|

Study on Effect Characteristics and Mechanism of <i>Sta</i><i>phylococcus aureus</i> on Albite

Abstract: In order to more deeply understand the mechanism between microorganism and atmospheric inhaled mineral fine particles. Albite, the typical mineral fine particle in the atmosphere, was used as the research object. This study investigated the air common bacteria-Staphylococcus aureusacted on albite for 7 days. By inductively coupled plasma (ICP), zeta potentials analyzer, fourier transform infrared spectroscopy (FTIR) and scanning electron microscope (SEM) testing means, we can analyse soluble ions, surface char… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
2
0

Year Published

2019
2019
2023
2023

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 8 publications
0
2
0
Order By: Relevance
“…The change in structural orderliness can be determined by the increase in intensity, number, and sharpness, as well as by the shifts in band frequencies of the peaks [19]. It is known that the main infrared characteristic peaks of albite occur at 400–1300 cm −1 [27]. In this range, there were four similar bands in the starting albite and organoalbite samples, which appeared at approximately 472, 532, 778, and 1030 cm −1 .…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The change in structural orderliness can be determined by the increase in intensity, number, and sharpness, as well as by the shifts in band frequencies of the peaks [19]. It is known that the main infrared characteristic peaks of albite occur at 400–1300 cm −1 [27]. In this range, there were four similar bands in the starting albite and organoalbite samples, which appeared at approximately 472, 532, 778, and 1030 cm −1 .…”
Section: Resultsmentioning
confidence: 99%
“…In this range, there were four similar bands in the starting albite and organoalbite samples, which appeared at approximately 472, 532, 778, and 1030 cm −1 . The two obvious peaks centered at 472 cm −1 and 532 cm −1 , represented the bending vibration of Si–O–Si and the coupling between the O–Si–O deformation and the Na–O stretching, respectively [27,28]. The band at 778 cm −1 was attributed to Si–O–Si bending vibrations, while the Si–O symmetric bond stretching bands could be seen in the region of 900–1200 cm −1 centered at 1030 cm −1 [19,29].…”
Section: Resultsmentioning
confidence: 99%