2016
DOI: 10.1007/978-3-319-39193-9_84-1
|View full text |Cite
|
Sign up to set email alerts
|

Carbonate Minerals and the CO2-Carbonic Acid System

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2020
2020
2021
2021

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(1 citation statement)
references
References 61 publications
0
1
0
Order By: Relevance
“…The carbon is mainly due to the presence of bicarbonate anions because the FTIR spectrum shows typical bands at 1385 and 1283 cm –1 assignable to CO stretching and C–O–H bending vibrations, respectively . Because the pH of the nanosheet dispersion was found to be in the range of 8.1–8.2, the bicarbonate ion is a major species by considering the change in the molar concentrations of CO 2 , HCO 3 – , and CO 3 2– as a function of pH in water . The XRD pattern of the restacked nanosheets shows the peaks characteristic of the interstratified structure composed of α- and β-phase hydroxide layers (Figure S11b).…”
Section: Resultsmentioning
confidence: 99%
“…The carbon is mainly due to the presence of bicarbonate anions because the FTIR spectrum shows typical bands at 1385 and 1283 cm –1 assignable to CO stretching and C–O–H bending vibrations, respectively . Because the pH of the nanosheet dispersion was found to be in the range of 8.1–8.2, the bicarbonate ion is a major species by considering the change in the molar concentrations of CO 2 , HCO 3 – , and CO 3 2– as a function of pH in water . The XRD pattern of the restacked nanosheets shows the peaks characteristic of the interstratified structure composed of α- and β-phase hydroxide layers (Figure S11b).…”
Section: Resultsmentioning
confidence: 99%