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WIDENING THE FRONTIERS IN FORENSIC IDENTIFICATION: PROBING BURNED HUMAN BONES WITH NEUTRON TECHNIQUES PO 4 3- OH - CO 3 2- Bioapatite Carbonates substitute phosphate and hydroxyl groups In vivo Exposure to heating Increase in Crystallinity Organic material degradation Changes in the content of carbonates, phosphates and hydroxyls Possible formation of new inorganic phases In parallel with the macroscopic alterations: color, shape and size Compromising the application of the Bioanthropological methods Mamede AP , Vassalo AR, Makhoul C, Gonçalves D, Parker SF, Kockelman W, Marques MPM and Batista de Carvalho LAE INTRODUCTION Acknowledgement to finantial support from: Portuguese FCT – SFRH/BPD/84268/2012; UID/MULTI/00070/2013; PTDC/IVC- ANT/1201/2014; POCI-01-0145-FEDER-016766; PEst-OE/SADG/UI0283/2013 STFC Rutherford Appleton Laboratory – ISIS Neutron Facility, RB 1400034, 1510054, 1710008 RESULTS TOSCA MAPS Rietveld refinement of neutron diffraction data of human femur burned at A)1000ºC (using hexagonal hydroxyapatite as model); B) 900ºC; C) 800ºC; D) 700ºC under controlled conditions D-space / Å B 1 2 3 4 1 2 3 D-space / Å Intensity / counts A 1 2 3 4 1 2 3 D-space / Å 1 2 3 4 1 0.5 1.5 D Simulation of a real fire in a caravan Ref/600ºC Pelvis Humerus (Prox) Humerus (Dist) 200 400 600 800 1000 1200 1400 1600 1800 2000 Wavenumber / cm -1 Ref/700ºC (OH) lib 1 st overt n 4 (PO 4 ) Ref/600ºC Pelvis Humerus (Prox) Humerus (Dist) 50 100 150 200 250 300 350 400 450 500 Wavenumber / cm -1 Ref/700ºC 2 (PO 4 ) 2 (HPO 4 ) Ca-PO 4 Ca-PO 4 Ca-PO 4 Estimated maximum temperature 600-700ºC D-space / Å 1 2 3 4 1 2 C Intensity / counts EXPERIMENTAL CONCLUSIONS Modern human femora and humeri were sectioned and burned in an electric oven for 120min. at 400 to 1000ºC (100ºC increment) Emperimentally burned samples under controlled consitions were grinded and analysed through INS (MAPS and TOSCA) and neutron diffraction (GEM), at ISIS- Rutherford Appleton Laboratory. GEM data was analysed with GSAS-EXPGUI to perform the Retveld refinement Different regions of human humeri and pelvis were burned in a caravan in order to simulate a real fire situation. These samples were also grinded and analysed on TOSCA. *M.P.M. Marques, et al. (2018) Heat-induced Bone Diagenesis Probed by Vibrational Spectroscopy, Scientific Reports IN PRESS MAPS data for human femur burned 400-1000ºC, and HAp refence from NIST * TOSCA data for human femur burned 400-1000ºC, and HAp refence from NIST * All HAp vibrational modes observed c onfirming the hydroxylation of bioapatite The narrowing of the signals with increasing temperatures evidences dimensional changes of the bioapatite crystals (increasing crystallinity) No organic material above 600ºC Crystal lattice (Ca-PO 4 ) signals are related with the short-range order and hydrogen-bonding profile within the crystalline framework, changes in these suggest crystal dimensional alterations as temperature increased No organic material (>600ºC) 1 st overtone observable (>600ºC) 3 (Ca-OH): Barely seen in humerus (prox) and pelvis samples (700ºC) Absent in humerus (dist)(<600ºC ) Neutron techniques provided unprecedented and valuable information on heat-induced changes within bone’s inorganic structure and composition Dimensional changes in bioapatite´s crystal definitely occurring between 700-800ºC The results are not compromised by the presence of contaminants INS at TOSCA allowed us to estimate the maximum temp reached in the caravan’s experiments GEM data of the bone samples burned under controled conditions fit the HAp model except the 700ºC burned sample because at this temperature traces of bioapatite (carbonates) is present (suggesting 700-800ºC to be a crucial interval to the understanding of the heat-induced changes within bone’s submicrostructure) Two different models needed for the refinement at temperatures below 700ºC, HAp & carbonated apatite SYSTEMATIC ERRORS in this model unable to complete the refinement

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WIDENING THE FRONTIERS IN FORENSIC IDENTIFICATION: PROBING BURNED HUMAN BONES WITH NEUTRON TECHNIQUES

PO43-

OH-

CO32-

Bioapatite

Carbonates substitute phosphate and

hydroxyl groups

In vivo Exposure to

heating• Increase in Crystallinity

• Organic material degradation

• Changes in the content of carbonates,

phosphates and hydroxyls

• Possible formation of new inorganic

phases

In parallel with the macroscopic alterations:

color, shape and size

Compromising the application of the

Bioanthropological methods

Mamede AP, Vassalo AR, Makhoul C, Gonçalves D, Parker SF, Kockelman W, Marques MPM and Batista de Carvalho LAE

INTR

OD

UCT

ION

Acknowledgement to finantial support from:

Portuguese FCT – SFRH/BPD/84268/2012; UID/MULTI/00070/2013; PTDC/IVC-

ANT/1201/2014; POCI-01-0145-FEDER-016766; PEst-OE/SADG/UI0283/2013

STFC Rutherford Appleton Laboratory – ISIS Neutron Facility, RB 1400034, 1510054, 1710008

RES

ULT

S

TOSCA

MAPS

Rietveld refinement of neutron diffraction data of human femur burned at A)1000ºC (using hexagonal

hydroxyapatite as model); B) 900ºC; C) 800ºC; D) 700ºC under controlled conditions

D-space / Å

B

1 2 3 4

1

2

3

D-space / Å

Inte

nsity

/ c

oun

ts

A

1 2 3 4

1

2

3

D-space / Å1 2 3 4

1

0.5

1.5

D

Simulation of a real fire in a caravan

Ref/600ºC

Pelvis

Humerus (Prox)

Humerus (Dist)

200 400 600 800 1000 1200 1400 1600 1800 2000

Wavenumber / cm-1

Ref/700ºC

(OH

) lib

1stovert

n4 (P

O4)

Ref/600ºC

Pelvis

Humerus (Prox)

Humerus (Dist)

50 100 150 200 250 300 350 400 450 500

Wavenumber / cm-1

Ref/700ºC

𝜈2(P

O4)

𝜈2(H

PO

4)

Ca-

PO

4

Ca-

PO

4

Ca-

PO

4

Estimated

maximum

temperature

600-700ºC

D-space / Å1 2 3 4

1

2

C

Inte

nsity

/ c

oun

ts

EXPERIMENTAL

CONCLUSIONS

• Modern human femora and humeri were sectioned and burned in an electric oven

for 120min. at 400 to 1000ºC (100ºC increment)

• Emperimentally burned samples under controlled consitions were grinded and

analysed through INS (MAPS and TOSCA) and neutron diffraction (GEM), at ISIS-

Rutherford Appleton Laboratory.

• GEM data was analysed with GSAS-EXPGUI to perform the Retveld refinement

• Different regions of human humeri and pelvis were burned in a caravan in order

to simulate a real fire situation. These samples were also grinded and analysed

on TOSCA.

*M.P.M. Marques, et al. (2018) Heat-induced Bone Diagenesis Probed by Vibrational Spectroscopy,

Scientific Reports IN PRESS

MAPS data for human femur burned 400-1000ºC, and HAp refence from NIST *

TOSCA data for human femur burned 400-1000ºC, and HAp refence from NIST *

• All HAp vibrational modes observed confirming

the hydroxylation of bioapatite

• The narrowing of the signals with increasing

temperatures evidences dimensional changes of

the bioapatite crystals (increasing crystallinity)

• No organic material above 600ºC

• Crystal lattice (Ca-PO4) signals are related with

the short-range order and hydrogen-bonding

profile within the crystalline framework, changes

in these suggest crystal dimensional alterations as

temperature increased

No organic material (>600ºC)

1st overtone observable (>600ºC)

𝝂3(Ca-OH): • Barely seen in humerus (prox) and

pelvis samples (700ºC)• Absent in humerus (dist)(<600ºC )

•Neutron techniques provided

unprecedented

and valuable information on heat-induced

changes within bone’s inorganic structure

and composition

•Dimensional changes in bioapatite´s

crystal

definitely occurring between 700-800ºC

•The results are not compromised by the

presence of contaminants

• INS at TOSCA allowed us to estimate the

maximum temp reached in the caravan’s

experiments

• GEM data of the bone samples burned

under controled conditions fit the HAp model

except the 700ºC burned sample because at

this temperature traces of bioapatite

(carbonates) is present (suggesting 700-800ºC to be a

crucial interval to the understanding of the heat-induced changes

within bone’s submicrostructure)

• Two different models needed for the

refinement at temperatures below 700ºC,

HAp & carbonated apatite

SYSTEMATIC ERRORS in this model

unable to complete the refinement