CAMERON J R, SORENSON J
Science. 1963 Oct 11;142(3589):230-2. doi: 10.1126/science.142.3589.230.
The mineral content of bone can be determined by measuring the absorption by bone of a monochromatic, low-energy photon beam which originates in a radioactive source (iodine-125 at 27.3 kev or americium 241 at 59.6 kev). The intensity of the beam transmitted by the bone is measured by counting with a scintillation detector. Since the photon source and detector are well collimated, errors resulting from scattered radiation are reduced. From measurements of the intensity of the transmitted beam, made at intervals across the bone, the total mineral content of the bone can be determined. The results are accurate and reproducible to within about 3 percent.
骨矿物质含量可通过测量源于放射性源(27.3千电子伏特的碘-125或59.6千电子伏特的镅241)的单色低能光子束被骨的吸收来确定。通过闪烁探测器计数来测量透过骨的光束强度。由于光子源和探测器经过良好准直,散射辐射导致的误差得以减小。通过在骨上间隔测量透过光束的强度,可确定骨的总矿物质含量。结果的准确度和可重复性在约3%以内。