2015
DOI: 10.1016/j.catcom.2015.07.005
|View full text |Cite
|
Sign up to set email alerts
|

Effect of structure and acidity of acid modified clay materials on synthesis of octahydro-2H-chromen-4-ol from vanillin and isopulegol

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
14
0

Year Published

2017
2017
2024
2024

Publication Types

Select...
8

Relationship

0
8

Authors

Journals

citations
Cited by 26 publications
(19 citation statements)
references
References 11 publications
(15 reference statements)
0
14
0
Order By: Relevance
“…A significant increase in the specific surface of the acid-modified clays promotes wide use of such material for removal of heavy metals, radionuclides and for oil refining [15][16][17][18][19]. The transformation of the structure and properties of bentonite under the influence of acids, mostly under sulfuric and hydrochloric acids, have been studied by different authors [20][21][22][23][24][25][26]. Using ultrasound and microwaves in addition to an acid treatment intensifies smectite mineral transformation [27].…”
Section: Introductionmentioning
confidence: 99%
“…A significant increase in the specific surface of the acid-modified clays promotes wide use of such material for removal of heavy metals, radionuclides and for oil refining [15][16][17][18][19]. The transformation of the structure and properties of bentonite under the influence of acids, mostly under sulfuric and hydrochloric acids, have been studied by different authors [20][21][22][23][24][25][26]. Using ultrasound and microwaves in addition to an acid treatment intensifies smectite mineral transformation [27].…”
Section: Introductionmentioning
confidence: 99%
“…15 The acid-catalyzed Prins reaction of pulegols with various aldehydes containing electron-donating and electron-withdrawing substituents is often used for the synthesis of biologically active octahydro-2 H -chromen-4-ols. 16…”
Section: Resultsmentioning
confidence: 99%
“…The occurrence of amorphous silica in kaolin clay samples can be explained by the presence of humps, peaks or large bands within the range of 15-25 • . Meanwhile, the peak observed in the X-ray diffractograms at the 2 θ range above than 66 • represents the quartz phase and 2 θ range less than 15 • reflects the presence of illite phase [27]. As seen in Figure 5, alternation occurs in the peaks of the catalysts after acid activation.…”
Section: Mineral Compositionmentioning
confidence: 94%
“…After acid activation, the morphological differences are apparent at high magnification. In the activated metakaolin micrograph showed the small particles and well-bonded aggregates rather than scattered particles [27]. There was minor particle dispersion in the activated K1 sample into the plate-like shaped particle.…”
Section: Morphology Of Raw Kaolin and Acid Activated Metakaolinmentioning
confidence: 95%
See 1 more Smart Citation