2020
DOI: 10.1088/1742-6596/1655/1/012013
|View full text |Cite
|
Sign up to set email alerts
|

Structural and Morphological Properties of Undoped and Manganese Doped Hematite Nanoparticles Prepared by Ball Milling Method

Abstract: Hematite nanoparticles of undoped and manganese doped were synthesized from natural sand of Logas District Kuansing Regency Riau Province by ball milling method. Structural and morphological properties of these compounds were studied using X-Ray Diffractometer (XRD) and Scanning electron microscope (SEM) respectively. Crystalline structure, lattice parameters, morphologies of the synthesized compounds were studied and the results are discussed. X-ray diffraction (XRD) confirmed the presence of a hematite (α-Fe… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2022
2022
2022
2022

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(1 citation statement)
references
References 17 publications
0
1
0
Order By: Relevance
“…The diffraction peaks at 23.91, 33.32, 35.71, 40.71, 49.53, 54.14, 57.72, 62.54, and 63.93° correspond to the (012), (104), (110), (113), (024), (116), (018), (214), and (030) diffractions of pure hematite (α-Fe 2 O 3 ). , The compositional (changing the Fe/O ratio from 3:4 to 2:3) and structural modifications are both involved in the phase transformation from Fe 3 O 4 to α-Fe 2 O 3 . The process is called oxygen dissociation and can occur at temperatures starting from 700 to 1000 °C, but the exact temperature varies due to composition and oxygen partial pressure.…”
Section: Resultsmentioning
confidence: 99%
“…The diffraction peaks at 23.91, 33.32, 35.71, 40.71, 49.53, 54.14, 57.72, 62.54, and 63.93° correspond to the (012), (104), (110), (113), (024), (116), (018), (214), and (030) diffractions of pure hematite (α-Fe 2 O 3 ). , The compositional (changing the Fe/O ratio from 3:4 to 2:3) and structural modifications are both involved in the phase transformation from Fe 3 O 4 to α-Fe 2 O 3 . The process is called oxygen dissociation and can occur at temperatures starting from 700 to 1000 °C, but the exact temperature varies due to composition and oxygen partial pressure.…”
Section: Resultsmentioning
confidence: 99%