TY - JOUR
T1 - Thermogravimetric analysis of property changes and weight loss in incinerated bone
AU - Ellingham, S. T.D.
AU - Thompson, T. J.U.
AU - Islam, Meez
PY - 2015/11/15
Y1 - 2015/11/15
N2 - Thermogravimetric analysis (TGA) and differential scanning calorimetry (DSC) are thermal analyses techniques, which can give vital information about a material's properties and phase transitions when exposed to heating. This study utilised a combined TGA-DSC approach to determine how exposure to varying temperatures and different heating regimes affect the decomposition of skeletal hard tissue. It was found that an accelerated heating rate causes the onset of phase changes in the bone matrix to be delayed to higher temperatures. The progression of matrix changes within a certain phase is also highly dependent on the rate of heating. Longer exposure times or slower heating rates increase progression of decomposition within a certain phase, progression to a different material phase however will only occur after a key "activation temperature" is reached. These findings have important implications for the subsequent analytical investigations of burnt bone.
AB - Thermogravimetric analysis (TGA) and differential scanning calorimetry (DSC) are thermal analyses techniques, which can give vital information about a material's properties and phase transitions when exposed to heating. This study utilised a combined TGA-DSC approach to determine how exposure to varying temperatures and different heating regimes affect the decomposition of skeletal hard tissue. It was found that an accelerated heating rate causes the onset of phase changes in the bone matrix to be delayed to higher temperatures. The progression of matrix changes within a certain phase is also highly dependent on the rate of heating. Longer exposure times or slower heating rates increase progression of decomposition within a certain phase, progression to a different material phase however will only occur after a key "activation temperature" is reached. These findings have important implications for the subsequent analytical investigations of burnt bone.
UR - http://www.scopus.com/inward/record.url?scp=84940373712&partnerID=8YFLogxK
U2 - 10.1016/j.palaeo.2015.08.009
DO - 10.1016/j.palaeo.2015.08.009
M3 - Article
AN - SCOPUS:84940373712
SN - 0031-0182
VL - 438
SP - 239
EP - 244
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
ER -