通过对湘北地区某乡村砖混结构民居的围护结构特点以及室内热环境状况进行调研,发现该类建筑存在围护结构热工性能差、建筑能耗高、室内热环境质量低等问题。针对上述问题,结合夏热冬冷地区的地域气候特点,提出了合理选择建筑朝向、改...通过对湘北地区某乡村砖混结构民居的围护结构特点以及室内热环境状况进行调研,发现该类建筑存在围护结构热工性能差、建筑能耗高、室内热环境质量低等问题。针对上述问题,结合夏热冬冷地区的地域气候特点,提出了合理选择建筑朝向、改善围护结构热工性能、控制窗墙比以及自然通风等适应性的被动式建筑设计优化方案,利用Ecotect软件分析了上述优化策略对室内热环境改善的影响。通过正交试验方法设计试验方案,并计算分析了9组方案在全年典型日的P M V值,得到湘北民居最优设计方案。展开更多
All gold deposits in North-Eastern Hunan are of vein type, and hosted by the low grade metamorphic rocks of Lengjiaxi Group of the Middle Proterozoic Era. Their geochemical characteristics show that the ore-forming ma...All gold deposits in North-Eastern Hunan are of vein type, and hosted by the low grade metamorphic rocks of Lengjiaxi Group of the Middle Proterozoic Era. Their geochemical characteristics show that the ore-forming materials came from their host rocks. Oreforming fluids are rich in CO2 and SO2-4,with high Na+/K+ ratio, low Cl - and varied δ18O and δD values, showing that they are from multisources. These gold deposits were formed by a series of tectonic-thermal events which reworked the Lengjiaxi Group. There are two main stages of tectonic-thermal events: the Wulingian Period forming the auriferous quartz veins by syntectonic metamorphic differentiation, and the Indosinian-Yanshanian peroid causing re formation and enrichment of the former auriferous quartz veins.展开更多
文摘通过对湘北地区某乡村砖混结构民居的围护结构特点以及室内热环境状况进行调研,发现该类建筑存在围护结构热工性能差、建筑能耗高、室内热环境质量低等问题。针对上述问题,结合夏热冬冷地区的地域气候特点,提出了合理选择建筑朝向、改善围护结构热工性能、控制窗墙比以及自然通风等适应性的被动式建筑设计优化方案,利用Ecotect软件分析了上述优化策略对室内热环境改善的影响。通过正交试验方法设计试验方案,并计算分析了9组方案在全年典型日的P M V值,得到湘北民居最优设计方案。
文摘All gold deposits in North-Eastern Hunan are of vein type, and hosted by the low grade metamorphic rocks of Lengjiaxi Group of the Middle Proterozoic Era. Their geochemical characteristics show that the ore-forming materials came from their host rocks. Oreforming fluids are rich in CO2 and SO2-4,with high Na+/K+ ratio, low Cl - and varied δ18O and δD values, showing that they are from multisources. These gold deposits were formed by a series of tectonic-thermal events which reworked the Lengjiaxi Group. There are two main stages of tectonic-thermal events: the Wulingian Period forming the auriferous quartz veins by syntectonic metamorphic differentiation, and the Indosinian-Yanshanian peroid causing re formation and enrichment of the former auriferous quartz veins.
