“…First, MR is only indirectly proportional to mineral density so would not be expected to have high correlations with calcium content (Nixon 1987). Second, M R has only rarely and unsuccessfully been used as a quantitative method; Jenkins et al (1989) measured TI and T, relaxation times of vertebral bodies and could not distinguish between age, sex, or location in the spine. The technique's potential sources of error are many and include: 1) positioning of the region of interest, since large errors can result from small changes in position (Jenkins et al 1989); 2 ) slice thickness limitations of 5 mm in this study; 3) edge effects at interfaces between low and high signal intensity, such as cortical bone and endosteal callus (Clark and Kelly 1988); 4) chemical shift between interfaces of fat-bound protons bordering hydrated tissues such as endosteal callus and trabecular bone; 5) focal field inhomogeneity from irregularly deposited calcium within the callus; 6) volume averaging of two opposing tissue planes with markedly different signal characteristics such as cortical bone and periosteal or endosteal callus; and 7) pulse imperfections of the hardware (Majumdar et al 1986).…”