Schreiner L J, Cameron I G, Funduk N, Miljković L, Pintar M M, Kydon D N
Waterloo NMR Centre, University of Waterloo, Ontario, Canada.
Biophys J. 1991 Mar;59(3):629-39. doi: 10.1016/S0006-3495(91)82278-0.
The nuclear magnetic resonance spin-grouping technique has been applied to dentin from human donors of different ages. The apparent T2, T1, and T1 rho have been determined for natural dentin, for dentin which has been dried in vacuum, and for dried dentin which has been rehydrated in an atmosphere with 75% relative humidity. All apparent spin relaxation has been analyzed for exchange between the spin groups in which the dentin protons exist; the analyses incorporate the results of selective inversion recovery T1 measurements which better probe the effects of exchange. The exchange analyses of the high fields and rotating frame spin-lattice relaxation have also been correlated to determine uniquely the inherent relaxation parameters of the proton spin groups constituting the dentin magnetization. The natural dentin contains protons on water, protein, and hydroxy apatite; these spins contribute 50%, 45%, and 5% to the total dentin proton magnetization, respectively. The water exists in three distinct environments, the dynamics of each environment has been modeled. In the natural dentin 30% of the water undergoes uni-axial reorientation. 52% of the water has similar relaxation characteristics to bound water hydrating a large molecule, and the majority of the remaining water acts as bulk water undergoing isotropic reorientation. The results are independent of the age of the donor.
核磁共振自旋分组技术已应用于不同年龄人类供体的牙本质。已测定了天然牙本质、真空干燥牙本质以及在相对湿度75%的气氛中再水化的干燥牙本质的表观T2、T1和T1ρ。对牙本质质子所在自旋组之间的交换进行了所有表观自旋弛豫分析;分析纳入了选择性反转恢复T1测量结果,该测量能更好地探测交换效应。还对高场和旋转框架自旋晶格弛豫的交换分析进行了关联,以唯一确定构成牙本质磁化的质子自旋组的固有弛豫参数。天然牙本质中的质子存在于水、蛋白质和羟基磷灰石上;这些自旋分别对牙本质总质子磁化贡献50%、45%和5%。水存在于三种不同环境中,对每种环境的动力学进行了建模。在天然牙本质中,30%的水进行单轴重排。52%的水具有与大分子水合结合水相似的弛豫特性,其余大部分水作为进行各向同性重排的体相水。结果与供体年龄无关。