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首页> 外文期刊>NMR in biomedicine >Bone mineral ~(31)P and matrix-bound water densities measured by solid-state ~(31)P and ~1H MRI
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Bone mineral ~(31)P and matrix-bound water densities measured by solid-state ~(31)P and ~1H MRI

机译:固态〜(31)P和〜1H MRI测量的骨矿物质〜(31)P和基质结合水密度

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摘要

Bone is a composite material consisting of mineral and hydrated collagen fractions. MRI of bone is challenging because of extremely short transverse relaxation times, but solid-state imaging sequences exist that can acquire the short-lived signal from bone tissue. Previous work to quantify bone density via MRI used powerful experimental scanners. This work seeks to establish the feasibility of MRI-based measurement on clinical scanners of bone mineral and collagen-bound water densities, the latter as a surrogate of matrix density, and to examine the associations of these parameters with porosity and donors' age. Mineral and matrix-bound water images of reference phantoms and cortical bone from 16 human donors, aged 27– 97 years, were acquired by zero-echo-time 31-phosphorus (~(31)P) and 1-hydrogen (~1H) MRI on whole body 7T and 3T scanners, respectively. Images were corrected for relaxation and RF inhomogeneity to obtain density maps. Cortical porosity was measured by micro-computed tomography (μCT), and apparent mineral density by peripheral quantitative CT (pQCT). MRI-derived densities were compared to X-ray-based measurements by least-squares regression. Mean bone mineral ~(31)P density was 6.74 ± 1.22 mol/l (corresponding to 1129 ± 204mg/cc mineral), and mean bound water ~1H density was 31.3± 4.2mol/l (corresponding to 28.3 ± 3.7 %v/v). Both ~(31)P and bound water (BW) densities were correlated negatively with porosity (~(31)P: R~2=0.32, p<0.005; BW: R~2 = 0.63, p<0.0005) and age (~(31)P: R~2 = 0.39, p<0.05; BW: R~2=0.70, p<0.0001), and positively with pQCT density (~(31)P: R~2=0.46, p<0.05; BW: R~2=0.50, p<0.005). In contrast, the bone mineralization ratio (expressed here as the ratio of ~(31)P density to bound water density), which is proportional to true bone mineralization, was found to be uncorrelated with porosity, age or pQCT density. This work establishes the feasibility of image-based quantification of bone mineral and bound water densities using clinical hardware.
机译:骨是由矿物质和水合胶原部分组成的复合材料。由于极短的横向弛豫时间,骨骼的MRI具有挑战性,但是存在固态成像序列,可以从骨骼组织中获取短暂的信号。先前通过MRI量化骨密度的工作使用了功能强大的实验扫描仪。这项工作试图建立在骨矿物质和胶原结合的水密度的临床扫描仪上进行基于MRI的测量的可行性,后者是基质密度的替代品,并检查这些参数与孔隙率和供体年龄之间的关系。通过零回波时间31磷(〜(31)P)和1-氢(〜1H)获得了16位年龄在27-97岁之间的供体的参考体模和皮质骨的矿物质和基质结合水图像分别在全身7T和3T扫描仪上进行MRI。校正图像的弛豫和RF不均匀性以获得密度图。通过微计算机断层扫描(μCT)测量皮质孔隙率,通过外围定量CT(pQCT)测量表观矿物质密度。通过最小二乘回归将MRI得出的密度与基于X射线的测量值进行比较。平均骨矿物质〜(31)P密度为6.74±1.22 mol / l(相当于1129±204mg / cc矿物质),平均结合水〜1H密度为31.3±4.2mol / l(相当于28.3±3.7%v / v)。 〜(31)P和束缚水(BW)密度均与孔隙率(〜(31)P:R〜2 = 0.32,p <0.005; BW:R〜2 = 0.63,p <0.0005)呈负相关〜(31)P:R〜2 = 0.39,p <0.05; BW:R〜2 = 0.70,p <0.0001),且与pQCT密度呈正相关(〜(31)P:R〜2 = 0.46,p <0.05 ;体重:R〜2 = 0.50,p <0.005)。相反,发现与真正的骨矿化成比例的骨矿化率(此处表示为〜(31)P密度与结合水密度的比值)与孔隙率,年龄或pQCT密度无关。这项工作建立了使用临床硬件对骨矿物质和结合水密度进行基于图像的量化的可行性。

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