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Updated: Jul 16, 2026

Scanning Skeletal Remains for Bone Mineral Density in Forensic Contexts
Published on: January 29, 2018
Application of biochemical and X-ray diffraction analyses to establish the postmortem interval.
M J Prieto-Castelló1, J P Hernández del Rincón, C Pérez-Sirvent
1Faculty of Medicine, Legal and Forensic Medicine Division, University of Miguel Hernández, Apdo correos 18, San Juan, Alicante, Spain. mjose.prieto@umh.es <mjose.prieto@umh.es>
Determining the time since death from bone remains is challenging. This study suggests that X-ray diffraction and biochemical analysis of urea, potassium, and sulfur in cortical bone offer a promising method for dating osseous remains.
Area of Science:
- Forensic Anthropology
- Biochemistry
- Materials Science
Background:
- Accurate determination of the postmortem interval (PMI) from skeletal remains is crucial for legal and scientific purposes.
- Establishing PMI is complex due to numerous intrinsic and extrinsic factors influencing decomposition.
- Existing methods for dating bone remains have limitations.
Purpose of the Study:
- To evaluate the effectiveness of X-ray diffraction (XRD) and biochemical component analysis in determining the postmortem interval (PMI) of bone remains.
- To compare the utility of medullar and cortical bone zones for dating osseous remains.
Main Methods:
- Analysis of 69 long bones from cadavers with documented interment times (7-54 years).
- Measurement of chemical components: potassium, sulfur, nitrogen, urea, total protein, and phosphorus.
- Assessment of X-ray diffraction (XRD) parameters, specifically the degree of crystallinity in mineral components.
Main Results:
- Both XRD parameters and biochemical analyses showed potential for dating bone remains.
- Specific biochemical markers (urea, potassium, sulfur) demonstrated utility, particularly in the cortical bone zone.
- The combination of XRD and biochemical analysis in the cortical bone zone appears most informative for PMI estimation.
Conclusions:
- The combined use of X-ray diffraction and biochemical analyses, especially for urea, potassium, and sulfur in the cortical bone, presents a viable alternative method for dating osseous remains.
- Cortical bone analysis provides more useful information for calculating the postmortem interval compared to medullar bone.
- This approach could enhance the accuracy and reliability of forensic age estimation from skeletal evidence.
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