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Midinfrared ablation of dentin with the Vanderbilt FEL

机译:使用范德比尔特FEL进行牙本质中红外消融

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Abstract: Absorption spectra of 0.1 - 0.2 mm thick, dehydrated sections of human teeth were measured in the transmission mode with a Bruker FT-IR spectrometer from 2.5 - 20 $mu@m. Absorption peaks for amide I, II and III, carbonate and phosphate were identified. Craters were ablated in dentin and enamel using a tunable FEL at 6.45 $mu@m at various fluences. Pulse duration: 3 $mu@s; spot size (Gaussian, FWHM): 300 $mu@m; repetition rate: 10 Hz. Crater depth and width were measured from digitized optical images. Ablation rates were computed from crater depth and volume data. Selected specimens were examined with scanning electron microscopy to determine ablation surface characteristics. Depth of thermal damage and dentinal tubule morphology were estimated from SEM examination of fractures through ablation sites. Functions describing crater depth vs. number of pulses (quadratic function) were not the same as crater volume vs. number of pulses (linear function). Crater depth decreases with successive pulses, concurrently, the crater width increases. Thus, each pulse removes approximately a constant volume. Material was observed to flow through the dentinal tubules during and after ablation. Patent tubules on crater walls and floor were observed with SEM. Ablation rates in dentin were approximately 3$MUL those in enamel at 6.45 $mu@m. Ablation rates and surface characteristics varied across wavelengths from 5.8 to 8.0 $mu@m.!7
机译:摘要:用Bruker FT-IR光谱仪以透射模式在2.5-20μμm的范围内测量了0.1-0.2 mm厚的人体牙齿脱水部分的吸收光谱。确定了酰胺I,II和III,碳酸盐和磷酸盐的吸收峰。使用可调的FEL,以不同的通量在6.45μm的火山口中烧蚀牙本质和牙釉质中的火山口。脉冲持续时间:3 $ mu @ s;光斑尺寸(高斯,半高宽):300 $ mu @ m;重复频率:10 Hz。火山口的深度和宽度是从数字化光学图像中测得的。烧蚀率是由火山口深度和体积数据计算得出的。通过扫描电子显微镜检查选择的样品,以确定烧蚀表面特征。热损伤深度和牙本质小管形态是通过通过消融部位进行的SEM扫描评估的。描述火山口深度与脉冲数的函数(二次函数)与火山口体积与脉冲数的函数(线性函数)不同。弹坑深度随着连续脉冲而减小,同时,弹坑宽度增加。因此,每个脉冲去除大约恒定的体积。在消融期间和消融后,观察到材料流过牙本质小管。用扫描电镜观察到火山口壁和地板上的小管。牙本质的消融速率约为牙釉质的消融速率(6.45μm@ mUL的消融速率的3%)。烧蚀速率和表面特性在5.8至8.0 $mu@m.!7的波长范围内变化。

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