真空干燥过程中山毛榉木材的温度分布

E. Dobrowolska, Andrzej Klimczak
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摘要

真空干燥过程中山毛榉木材的温度分布。分析了山毛榉木材在真空干燥过程中的温度分布和湿度变化。解吸现象发生的强度和水分通过木材解剖结构的体积流动,取决于绝对压力和过程的温度,被确定。研究发现,温度上升最快的是直接靠近加热板的次表层。在干燥阶段之间引入调节使整个元素的湿度和温度分布均匀成为可能。在分析木材三组分体积变化的基础上,发现干燥初始阶段以蒸汽形式去除的水分体积大于木结构空隙体积的20倍以上,在随后的阶段减小到0.27。1 m3木材在55℃干燥时的平均汽体积为13.9 m3/h,在接下来的阶段中,干燥温度为60℃时降至9.1 m3/h,干燥温度为65℃时降至3.1 m3/h。这些相的干燥速率分别达到0.15%/h、0.17%/h和0.075%/h。在干燥过程的实验过程中,在绝对压力为150 hPa的条件下,直接测量木材水分,采用等效水分,根据Hailwood-Horrobin模型确定,并考虑适当的计算因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Temperature distribution in beech wood during vacuum drying
Temperature distribution in beech wood during vacuum drying. The temperature distribution and changes in humidity in beech wood in the form of friezes during drying in a vacuum were analysed. The intensity of the occurring phenomena of desorption and the volumetric flow of moisture through the anatomical structures of the wood, depending on the absolute pressure and the temperature of the process, was determined. It was found that the fastest temperature increase took place in the subsurface layers directly adjacent to the heating plates. The introduction of conditioning between the drying phases made it possible to even out the humidity and temperature distribution in the entire element. On the basis of the analysis of changes taking place between the volumes of the three components of wood, it was found that the volume of moisture in the form of vapor removed in the initial phase of drying is over 20 times greater than the volume of voids in wood structures, and in the following phases it decreases to 0.27. The average volume of vapour removed from 1 m3 of wood at the temperature of 55℃ is 13.9 m3/h, decreasing in the following phases to 9.1 m3/h at the drying temperature of 60℃ and then 3.1 m3/h at the temperature of 65℃. The drying rates for these phases reach the value of 0.15%/h, 0.17%/h and 0.075%/h, respectively. Direct measurements of wood moisture, made during the experimental course of the drying process at an absolute pressure of 150 hPa, follow the equivalent moisture, determined on the basis of the Hailwood-Horrobin model, taking into account the appropriate calculation factors.
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