Osteoarthritis (OA) of the knee causes pain, limits activity and impairs quality of life. Raman microspectroscopy can provide information about the chemical changes that occur in OA, to enhance our understanding of its pathology. The objective of this study is to detect OA severity in human cartilage and subchondral bone using Raman microspectroscopy and explore corresponding mechanical properties of the subchondral bone. OA tibial plateaus were obtained from total knee replacement surgery with REC (18/LO/1129) and HRA approval. Medial tibial plateau, representing a major weight-bearing area, was graded according to the International Cartilage Repair Society (ICRS) scoring system. Nine samples (3 samples of each graded as moderate, severe and very severe) were selected for Raman and mechanical analyses.Abstract
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Methods
Development of more effective diagnostic and therapeutic solutions is vital to tackling the growing challenge of bone diseases and disorders in aging societies. Spatially offset Raman spectroscopy (SORS) enables the chemical specificity of conventional Raman spectroscopy to be combined with sub-surface probing. SORS has successfully been applied to transcutaneous investigations of underlying bone and shows great potential to become an The volume within the complex hierarchical bone tissue probed by SORS depends on the specimen's optical properties. Understanding the actual sampling depth is important to correctly assign detected chemical changes to specific areas in the bone. This study explores the hypothesis that the effective Raman signal recovery from certain depths requires different spatial offsets depending on the bone mineralisation. SORS depth investigations were conducted on three bones with significantly different mineralisation levels. Thin slices (0.6 – 1.0 mm thickness) were cut from deer antler, horse metacarpal and whale tympanic bulla and stacked together (4 – 7 layers; 4.1 – 4.7 mm total thickness). A 0.38 mm thin slice of polytetrafluoroethylene (PTFE) served as reference sample and was inserted in between the layers of stacked bone slices. Raman spectra were acquired at 30 s using 830 nm excitation. A quantitative relation between the SORS offset and the primarily interrogated depth inside the bone was established. Maximum accessible depths at small offset strongly depend on the mineralisation level. Using large spatial offsets of 7 – 9 mm PTFE signal recovery depths of 4.4 – 4.6 mm through cortical bone can be realized with only minor dependence on the bone mineralisation. These findings highlight the potential of SORS for medical diagnostics by enabling the non-invasive detection of bone conditions characterised by chemical alterations several millimetres inside compact bone tissue (e.g. infections, tumours, etc.).
