检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:赵亮[1] 魏秀英[2] 李里特[2] 董仁杰[1]
机构地区:[1]中国农业大学水利与土木工程学院,北京100083 [2]中国农业大学食品科学与营养工程学院,北京100083
出 处:《农业工程学报》2006年第12期110-112,共3页Transactions of the Chinese Society of Agricultural Engineering
基 金:北京市教育委员会共建项目建设计划资助(XK100190441)
摘 要:冰动态蓄冷问题的实质是伴随有潜热释放或吸收的移动界面导热问题。由于已有的文献对自然冷贮藏系统的热力学分析涉及较少,而冰融化与凝固过程中传热规律的研究又是大规模制冰的关键,故该文从传热学角度出发,将自然冷贮藏系统中蓄冷水箱进行简化,通过试验得到相变界面随时间变化的实际曲线。在理论计算中,考虑冰层和水的导热量与水的相变潜热释放量之和等于冰层与外界的对流换热量建立数学模型,得到冰厚随时间变化的理论关系曲线。与实际曲线比较表明,理论模型能够反映冰一维动态蓄冷的实际进程。The nature of glacial dynamic refrigeration is heat conduction in companion with the release and absorption of latent heat. The heat transfer rule is the key to large-scale ice making, while few were reported in the literature about thermodynamic analysis in preservation system with natural cool resources. The authors studied glacial thickness fluctuant curve with simplified test device and took heat transfer into account. In theory, the authors developed the complete mathematical model and indicated that the sum of thermal and latent heat flux between water and ice layer was equal to the heat of convection between ice and environment. In comparison with experimental curve, the theoretical model can reveal the real process of one-dimensional dynamic cool storage of ice. Simulating three-dimenslonal dynamic refrigeration should be considered in the further study.
分 类 号:S379.2[农业科学—农产品加工] O552.6[农业科学—农艺学]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.249