| Literature DB >> 31741599 |
Selim Kayaci1, Ahmet Tabak2, Irmak Durur-Subasi3, Tugba Eldes4, Vaner Koksal5, Murat Sirin6, Yusuf Kemal Arslan7.
Abstract
PURPOSE: The purpose of our study was to conduct a chemical analysis of extracranial foreign bodies (FBs) causing artifacts in cranial magnetic resonance imaging (MRI) and to investigate the association between chemical composition, magnetic susceptibility, and artifact size.Entities:
Keywords: Artifact; glass; magnetic resonance imaging; magnetism; stone
Year: 2019 PMID: 31741599 PMCID: PMC6857268 DOI: 10.4103/ijri.IJRI_211_18
Source DB: PubMed Journal: Indian J Radiol Imaging ISSN: 0970-2016
Figure 1 (A-C)Example radiological images from selected patients. (A) Foreign body in the scalp after a traffic accident (stone sample). Ax. MRI artifact in the parietal aspect of the sagittal plane; Ay. Cranial CT reveals material 5.1 × 5 mm in the right parietal aspect of the sagittal plane; Az. 3D cranial CT image of the same patient. (B) Foreign body in the scalp due to head trauma (glass sample). Bx. Artifact in the parietal aspect of the sagittal plane of cranial MRI; By. Glass particle measuring 15 × 2.6 mm in left parietal aspect of the coronal plane on cranial CT; Bz. 3D cranial CT image of the same patient. (C) Patient who underwent surgery due to chronic subdural hematoma. Cx. Cranial MRI in postoperative month 2 showing signal distortion appearing as bone loss in the left frontal burr-hole region; Cy. No foreign body that could cause an artifact in the burr hole region was detected in 3D cranial CT
Figure 2Calculation of surface area of the artifact volume with Image J analysis program
Magnetic susceptibility, artifact volume values and volume of the foreign bodies
| Case no- sample | Magnetic susceptibility | Artifact volumes (cm3) | Volume of the foreign bodies (cm3) |
|---|---|---|---|
| 1-Stone | 9260 | 3.6 | 0.078 |
| 2-Stone | >10000 | 4.2 | 0.087 |
| 3-Stone | >10000 | 9.2 | 0.147 |
| 4-Stone | >10000 | 4.8 | 0.164 |
| 5-Stone | >10000 | 7.8 | 0.299 |
| Mean | >10000 | 5.9 | 0.155 |
| 6-Glass | 720 | 1.8 | 0.357 |
| 7-Glass | 5980 | 2.4 | 0.097 |
| 8-Glass | 440 | 2.2 | 0.164 |
| 9-Glass | 5680 | 3.2 | 0.268 |
| 10-Glass | 890 | 3.0 | 0.230 |
| Mean | 2742 | 2.5 cm3 | 0.223 |
It shows that positive relationship between magnetic susceptibility and artifact volume (r=0.92; P<0.001)
Figure 3 (A and B)SEM and EDS images of the glass (A) and stone (B) samples. Ax. SEM image of stone sample; Ay. EDS results of stone sample. Bx. SEM image of glass sample; By. EDS results of glass sample
Element composition determined by EDS
| Element composition and ratios (%) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Case no- sample | Fe | Al | Si | Mg | Na | Ti | Mn | K | Ca | 0 | Other elements |
| 1-Stone | 0.5 | 1.2 | 41.5 | 0 | 0.7 | 0 | 0 | 0 | 0.3 | 55.8 | 0 |
| 2-Stone | 1.4 | 0.3 | 0.9 | 7.6 | 0 | 0 | 0 | 0 | 23.3 | 52.5 | 13.0 |
| 3-Stone | 13.7 | 8.2 | 15.8 | 6.9 | 0 | 0.2 | 0.2 | 1.2 | 1.2 | 52.5 | 0.3 |
| 4-Stone | 2.2 | 9.3 | 25 | 0.5 | 1.0 | 0.3 | 0 | 1.7 | 4.6 | 55.4 | 0.1 |
| 5-Stone | 11.3 | 7.1 | 12.2 | 6.2 | 0 | 1.4 | 0.3 | 0.1 | 4.2 | 55.8 | 0.2 |
| Mean | 5.82 | 5.22 | 19.4 | 4.31 | 0.34 | 0.38 | 0.25 | 0.6 | 6.72 | 54.4 | 2.7 |
| 6-Glass | 0 | 1.5 | 44.6 | 0 | 2.7 | 0 | 0 | 0.9 | 0.1 | 50.2 | 1.0 |
| 7-Glass | 0.2 | 0 | 29.6 | 0 | 13.5 | 0 | 0 | 0 | 4.2 | 52.5 | 0 |
| 8-Glass | 0 | 1.5 | 42.4 | 0 | 3.3 | 0 | 0 | 0 | 0 | 50.9 | 1.9 |
| 9-Glass | 0.2 | 3.8 | 4.8 | 1.1 | 0.3 | 0 | 0 | 0 | 15.4 | 50.2 | 24.8 |
| 10-Glass | 0 | 0.6 | 29.9 | 2.6 | 10.1 | 0 | 0 | 0 | 5.3 | 51.5 | 0.6 |
| Mean | 0.08 | 1.48 | 29.6 | 0.74 | 5.98 | 0 | 0 | 0 | 5.0 | 51.2 | 5.6 |
For all stone samples, the standard deviation (SD) of Fe was±0.2. In one of the stone samples, the SD of Ca was±0.2. In three of the glass samples, the SD of Si was±0.2. For all other elements in other samples, the SD was ±0.1
Figure 4 (A and B)X-RD values of the stone (A) and glass (B) samples. The X-RD spectra of the stone samples revealed peaks of Fe2O3 at approximately 24.42 (2q) and 50.14 (2q) degrees, of Al2Ca (SiO4) at 22.02 (2q) and 27.84 (2q) degrees, of SiO2 at 26.67 (2q) and 39.56 (2q) degrees, and of TiO2 at 25.70 (2q) degrees. The X-RD spectra of the glass samples revealed no phase peaks
Figure 5 (A and B)FT-IR spectra of the stone (A) and glass (B) samples. The peaks detected in the glass samples in the 1100-400 cm-1 range indicate the presence of Al2Ca (SiO4) and Na2SiO3, and metal oxide (M-O) peaks in the 600-400 cm-1 range demonstrate Fe, Al, Mg, and TiO2 content