Gjr. Cook et al., Differences in skeletal kinetics between vertebral and humeral bone measured by F-18-fluoride positron emission tomography in postmenopausal women, J BONE MIN, 15(4), 2000, pp. 763-769
We have sought to investigate regional differences in skeletal kinetics bet
ween lumbar vertebrae and the humerus of postmenopausal women with F-18-flu
oride positron emission tomography (PET). Twenty-six women, mean age 62 yea
rs, had dynamic PET scans of the lumbar spine and lower humerus after the i
njection of 180 MBq F-18-fluoride ion. Plasma arterial input functions (IFs
) were calculated from a mean IF measured arterially from 10 women and scal
ed according to late individual venous activity. Vertebral and humeral time
activity curves were measured by placing regions of interest (ROI) over lu
mbar vertebrae and the humeral shaft. Using a three-compartmental model and
nonlinear regression analysis the macroconstant Ki, representing plasma cl
earance of fluoride to bone mineral, and the individual rate constants K1 (
related to regional skeletal blood flow) and k2 to k4 describing transport
between plasma, an extracellular fluid compartment and a bone mineral compa
rtment, were measured. Mean vertebral Ki (3.47 x 10(-2) mi min-l ml-l) and
K1 (1.08 x 10(-1) ml.min(-1) ml(-1)) were found to be significantly greater
than humeral Ki (1.64 x 10(-2) mi min-l ml-l; P < 0.0001) and K1 (3.90 x 1
0(-2) ml.min(-1) ml(-1); P < 0.0001) but no significant differences were fo
und in k2, k3, and k4. These findings confirm differences in regional skele
tal kinetics between lumbar vertebrae and the lower humerus. These observat
ions may help increase our understanding of the regional differences in pat
hophysiology and response to treatment that have been observed in sites con
sisting predominantly of either trabecular or cortical bone. F-18-fluoride
PET may prove to be a valuable technique in the noninvasive measurement of
regional skeletal metabolism.