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METHOD OF DETERMINING GRADIENT OF TEMPERATURES IN THE PROCESS OF TEMPERATURE VARIATION OF ANISOTROPIC MONOCRYSTALS
METHOD OF DETERMINING GRADIENT OF TEMPERATURES IN THE PROCESS OF TEMPERATURE VARIATION OF ANISOTROPIC MONOCRYSTALS
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机译:确定各向异性单晶温度变化过程中温度梯度的方法
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the invention u043eu0442u043du043eu0441u0438u0442u0441u00a0 radiation u043fu0438u0440u043eu043cu0435u0442u0440u0438u0438. the purpose of u0438u0437u043eu0431u0440u0435u0442u0435u043du0438u00a0 - improved accuracy of temperature gradient and heat u0438u0437u043cu0435u0440u0435u043du0438u00a0 u0440u0430u0441u043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 u043fu043eu043bu00a0. u0434u043bu00a0 u0440u0435u0448u0435u043du0438u00a0 this task through u0430u043du0438u0437u043eu0442u0440u043eu043fu043du044bu0439 single crystal u043fu0435u0440u043fu0435u043du0434u0438u043au0443u043bu00a0u0440u043du043e its optical axis of laser radiation through the diffraction grating, through to u043eu0442u043eu0440u043eu0439 form many u043au043eu043du043eu0441u043au043eu043fu0438u0447u0435u0441u043au0438u0445 figures from various sites u043cu043eu043du043eu043au0440u0438u0441u0442u0430u043bu043bu0430.in the process of u043du0430u0433u0440u0435u0432u0430u043du0438u00a0 u043cu043eu043du043eu043au0440u0438u0441u0442u0430u043bu043bu0430 log periodic u0438u0437u043cu0435u043du0435u043du0438u00a0 u0438u043du0442u0435u043du0441u0438u0432u043du043eu0441u0442u0435u0439 radiation in each u043au043eu043du043eu0441u043au043eu043fu0438u0447u0435u0441u043au043eu0439 body caused by the movement of u0438u0437u043eu0445u0440u043eu043c, and compare them with each other, then u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 dislocation of the extreme values in each of two periods u043au043eu043du043eu0441u043au043eu043fu0438u0447u0435u0441u043au0438u0445 figure, educated from sites u043cu043eu043du043eu043au0440u0438 u0441u0442u0430u043bu043bu0430 located on the u0440u0430u0441u0441u0442u043eu00a0u043du0438u0438 x from each other.and use these u0437u043du0430u0447u0435u043du0438u00a0 u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 gradient variation. 1 il.
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