首页> 外文会议>Conference on lasers in dentistry >Ablation in teeth with the free-electron laser around the absorption peak of hydroxyapatite (9.5 um) and between 6.0 and 7.5 um
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Ablation in teeth with the free-electron laser around the absorption peak of hydroxyapatite (9.5 um) and between 6.0 and 7.5 um

机译:用自由电子激光围绕羟基磷灰石(9.5μm)的吸收峰和6.0和7.5μm

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Pulsed IR laser ablation on dental hard substances was studied in the wavelength range between 9.5 and 11.5 $mu@m with the Free-Electron Laser (FEL) in Nieuwegein/NL and between 6.0 and 7.5 $mu@m with the FEL at Vanderbilt University in Nashville/TN. Depth, diameter and volume of the ablation crater were determined with a special silicon replica method and subsequent confocal laser topometry. The irradiated surfaces and the ejected debris were examined with an SEM 9.5 - 11.5 $mu@m: depth, diameter and volume of the ablation crater are greater and the ablation threshold is lower for ablation with a wavelength corresponding to the absorption max. of hydroxyapatite (9.5 $mu@m), compared to ablation at wavelengths with lower absorption (10.5 - 11.5 $mu@m). For all wavelengths, no thermal cracking can be observed after ablation in dentine, however a small amount of thermal cracking can be observed after ablation in enamel. After ablation at 9.5 $mu@m, a few droplets of solidified melt were seen on the irradiated areas, whereas the debris consisted only of solidified melt. In contrast, the surface and the debris obtained from ablation using the other wavelengths showed the natural structure of dentine 6.0 - 7.5 $mu@m: the depth of the ablation crater increases and the ablation threshold decreases for an increasing absorption coefficient of the target material. Different tissue components absorbed the laser radiation of different wavelengths (around 6.0 $mu@m water and collagen, 6.5 $mu@m collagen and water, 7.0 $mu@m carbonated hydroxyapatite). Nevertheless the results have shown no major influence on the primary tissue absorber.
机译:上牙体硬物质脉冲IR激光烧蚀在之间9.5和11.5 $亩的波长范围内进行了研究@米与自由电子激光器(FEL)在尼沃海恩/ NL和6.0和7.5之间$亩@米与FEL在Vanderbilt大学在纳什维尔/ TN。深度,直径和消融火山口的体积用一种特殊的硅复制法和随后的共聚焦激光形态测量来确定。照射表面和所喷出的碎屑,检查用SEM 9.5 - 11.5 $亩@米:深度,直径和消融火山口的容积是较大的和烧蚀阈值是与对应于最大吸收波长为消融更低。的羟基磷灰石(9.5 $亩@米),相比于具有较低吸收波长消融(10.5 - 11.5 $亩@米)。对于所有波长,无热裂解可以在牙质消融后观察到的,但热裂化的少量可以在搪瓷消融后进行观察。在9.5 $亩@米消融后,凝固的熔体的几个液滴看到的照射区域,而碎片仅包括固化熔体。与此相反,在表面和从使用其他波长烧蚀所得碎屑表明牙本质6.0的自然结构 - 7.5 $亩@ m是消融火山口的深度增加和烧蚀阈值用于目标材料的增加的吸收系数减小。不同的组织成分吸收不同的波长(约6.0 $亩@米水和胶原蛋白,6.5 $亩@米胶原和水,7.0 $亩@米碳酸羟基磷灰石)的激光辐射。然而结果却显示在主组织吸收无重大影响。

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