基于多孔毛管的温室热风采暖

通过对基于多孔毛管的温室热风采暖试验系统增温过程的研究,验证了该系统的实际增温效果.以多孔毛管进口温度、进口压力、出风孔径等试验因素,对多孔毛管进行保温围护,测量围护空间内温升数据,对不同试验因素条件下的热风增温过程进行试验分析.采用多项式回归方法对试验数据进行分析和计算,得出了围护空间内温升与毛管进口温度以及进口压力之间的数学关系.试验结果表明:不同毛管进口温度以及进口压力条件下,该热风增温系统可以使围护空间内温度升高4～9℃,且温升大小与多孔毛管进口温度和进口压力之间均为正相关关系,相对于进口温度,多孔毛管进口压力为围护空间内温升大小的主要影响因素.利用由多项式回归方法分析和计算得出的数学关系设定毛管进口温度和进口压力的大小,多孔毛管温室热风采暖系统可以满足温室冬季生产的实际增温需求.

多孔毛管温室冠层空间热风增温实验

为研究微孔散热条件下,多孔毛管沿程温度分布规律、温室冠层以下空间的垂直温度梯度及其与主要影响因素之间的关系,构建了多孔毛管温室空间热风增温实验系统。对多孔毛管进行保温围护,以毛管进口温度、进风压力、出风孔径等为实验参数,采集毛管前端孔口、中间孔口与末端孔口围护空间内温度数据,分析其在毛管沿程方向上和垂直空间内的分布规律。实验结果表明,毛管沿程出风孔口围护空间温升略有降低;垂直空间内温升呈先上升后下降的驼峰状变化趋势。不同进口温度、进风压力条件下,构建的热风增温系统可以使围护空间内距地面800～1 200 mm高度空间内的温度升高2.5～6.2℃。

掩埋多孔毛管水流特性的试验研究

以渗灌毛管的灌水试验为研究对象,通过试验分析得到了掩埋毛管流量和压力的变化特性。对于任一出水孔,随着供水时间的延长,压力水头和总水头都在不断增大。但是,这个增加值并不大,仅仅只有最大压力值的10%。随着四周土壤含水量的增加,孔口内外水势梯度不断减小,出水速率也逐渐减小,流量和压力随管长方向不断减小。由于流量随时间不断减小,使得水头损失也不断减小,压力随时间增大。同时在试验中还发现,水流运动的界面并不是管道的出水孔界面,而是在出水孔四周形成的不规则多边形界面。

Methodology for Determination of Moisture Distribution

The aim of the research is to determine the capillary conductivity coefficient as a characteristic material moisture parameter of the building materials using a non-destructive method while using microwave radiation. Available documents are usually focused on the description of diffusion and similar works are based on the difference of partial pressure [I]. Publication will introduce experimental measurements the transport of humidity in porous material in a non-stationary state. As a result may be obtaining of data for formulation of humidity profiles with the help of experimentally built measuring apparatus without influence of human factor. Aim is verification of mentioned method of measurement for description of moisture parameters building materials applicable for practice. Complication in the determination of moisture parameters is various porous textures and the remains effect of condensation and transport influence of liquid moisture by diffusion in porous material. At the present time does not exist for standard use computational theory to description of transport of dampness in building materials. Moisture in porous medium is transported by the help of the capillary forces. The liquid moisture gradient is an indicator of moving of liquid moisture in a porous material through capillaries. This phenomenon is called capillary conductivity of moisture. Purpose presents measurement of material specimen for formulation of capillary conductivity coefficient and its dependence on moisture. The specimen of porous material is subjected to an isothermal moisture intake process. The transient moisture distribution in the specimen during the process is determined, at different stages of the process. Methodology of data scanning with the help of microwave radiation and data processing is processed for numerical computation on the basis known physics laws. The outputs of measurements can be used for evaluation of physical properties of building materials.