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严寒地区高湿室内环境水平开合屋盖轨道连接处构造设计研究
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作者 李妍 李弘玉 李铁军 《建筑与文化》 2020年第5期77-78,共2页
当前我国开合屋盖的研究与实践发展方兴未艾,但在开合屋盖的开合方式与构造节点等方面仍需进一步深入。文章基于已有的开合屋盖的节点构造措施,分析严寒地区高湿环境水平开合屋盖轨道连接处所遇到的问题,提出一种在此建筑环境中轨道连... 当前我国开合屋盖的研究与实践发展方兴未艾,但在开合屋盖的开合方式与构造节点等方面仍需进一步深入。文章基于已有的开合屋盖的节点构造措施,分析严寒地区高湿环境水平开合屋盖轨道连接处所遇到的问题,提出一种在此建筑环境中轨道连接处的气密、水密构造,有效降低建筑耗能,提高室内环境质量,为之后的实际工程项目提供有效的解决方案。 展开更多
关键词 严寒地区 水平开合屋 轨道节点 构造设计
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新生代西昆仑隆升的地层学和沉积学记录 被引量:33
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作者 金小赤 王军 +1 位作者 陈炳蔚 任留东 《地质学报》 EI CAS CSCD 北大核心 2001年第4期459-467,共9页
西昆仑北坡的新生代沉积在很大程度上良好地记录了新生代西昆仑的隆升过程。区域性不整合面和沉积界面记录了隆升的阶段性;沉积环境变化反映了山体和盆地在格局上的变化;沉积物厚度、粒度变化显示了隆升的幅度和速率。就西昆仑的情况看... 西昆仑北坡的新生代沉积在很大程度上良好地记录了新生代西昆仑的隆升过程。区域性不整合面和沉积界面记录了隆升的阶段性;沉积环境变化反映了山体和盆地在格局上的变化;沉积物厚度、粒度变化显示了隆升的幅度和速率。就西昆仑的情况看,海相环境(塔里木海湾)由晚白垩世持续到渐新世,尽管此时海湾已退缩到西部。在此期间,形成了石膏层、瓣鳃类介壳灰岩和杂色砂泥质沉积。中新世全面出现了陆相沉积。中新世2000~3000m的沉积厚度表明了相对较高的隆升速率。从中新世后期开始的厚达2000~3000m的磨拉石沉积,其粒度向上加大,显示从中新世后期到早更新世隆升速率高而且是加速的。磨拉石沉积被早更新世的一次强烈的构造脉动所打断,它使磨拉石沉积和较老的沉积在许多地方高角度向盆地方向倾斜甚至直立、倒转。水平盖在磨拉石和更老地层之上的中—晚更新世河流和冲积扇相粗粒沉积是重新隆升的标志,亦可视为磨拉石沉积的继续。由昆仑山流向塔里木盆地的河流将中—上更新统及更老沉积切割50~100m以上,表明全新世以来的隆升速率是相当高的。 展开更多
关键词 西昆仑 新生代 隆升 沉积记录 地层 海相环境 水平盖 磨拉石层
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Microclimatic Experimentation Applied to Insulating Horizontal Coverage in Mexicali, Mexico 被引量:1
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作者 Zalia Haro-Rincon Nestor Santillfin-Sot1 +2 位作者 Rafael Garcia-Cueto Sara Ojeda-Benltez AlejandroLambert-Arista 《Journal of Environmental Science and Engineering(A)》 2013年第9期561-568,共8页
The thermal response of hedges alters the urban climate, resulting in energy and comfort affectations that impact city dwellers, so the aim of this study is to analyze the energy fluxes of urban horizontal coverage, e... The thermal response of hedges alters the urban climate, resulting in energy and comfort affectations that impact city dwellers, so the aim of this study is to analyze the energy fluxes of urban horizontal coverage, especially expanded polystyrene waterproofed with elastomeric paint in the city of Mexicali, Baja California, located northwest of Mexico. The experiment was realized on summer of 2011 and 2012 by using four components radiometric sensor, eddy covariance equipment, which was possible to analyze the behavior and intensities of heat fluxes using the model Q* = QE + QG + QH + QF + QD. The results show that in both campaigns the sensible heat flux exceeds the net radiation, in 2011 the net radiation was 31.41 W/mE and sensible heat flux of 74.9 W/m2, in 2012 resulted 43.46 W/m2 and 87.32 W/mE, respectively. This additional heat flux is attributed to the thermal influence of the air conditioning units, which changes the energy balance model to Q* = QH + QF + QD. With the results arise the need for experimentation on a larger scale in which it is possible to model the flow in housing development. The knowledge of the energy balance model will help to propose materials that minimize the thermal impact to the city of Mexicali. 展开更多
关键词 Energy fluxes coating insulating coverage thermal impact urban climatology.
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轻型门式刚架结构设计中几个问题的探讨
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作者 王新刚 崔长中 《陕西建筑》 2010年第10期16-18,共3页
轻型门式刚架结构在我国得到了广泛应用,工程实践中遇到一些国家标准规范尚未完善或不明确的问题。本文对门式刚架的适用范围、摇摆柱的应用、屋盖纵向水平支撑的设置、冷弯薄壁型钢檩条的设计计算中遇到的几个问题进行探讨,以期为门... 轻型门式刚架结构在我国得到了广泛应用,工程实践中遇到一些国家标准规范尚未完善或不明确的问题。本文对门式刚架的适用范围、摇摆柱的应用、屋盖纵向水平支撑的设置、冷弯薄壁型钢檩条的设计计算中遇到的几个问题进行探讨,以期为门式刚架的设计提供一些实用经验。 展开更多
关键词 局部夹层 摇摆柱 纵向水平支撑 冷弯薄壁型钢檩条
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Characteristics of the lower layer of sandstorms in the Minqin desert-oasis zone 被引量:9
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作者 ZHAO Ming ZHAN KeJie +7 位作者 YANG ZiHui FANG ErTian QIU GuoYu WANG QiangQiang ZHANG YinChang GUO ShuJiang LI AiDe ZHANG JingChun 《Science China Earth Sciences》 SCIE EI CAS 2011年第5期703-710,共8页
By measuring the sand-dust flux,vertical deposition,and the wind velocity throughout 19 sandstorms in the Minqin region,we quantitatively analyzed the horizontal distribution and vertical variation in sandstorm charac... By measuring the sand-dust flux,vertical deposition,and the wind velocity throughout 19 sandstorms in the Minqin region,we quantitatively analyzed the horizontal distribution and vertical variation in sandstorm characteristics under different land cover conditions.The effect of different land cover on mitigating sandstorms was also investigated.The results indicated that,in the surface layer ranging from 0-50 m,the intensity of sand-dust horizontal flux and concentration of sand-dust decreased with the increase of the height in the desert and the edge of oasis,whereas the two physical quantities increased slightly with the increase of the height in the oasis.The two physical quantities obey power function well under all three cover conditions.Moreover,in the desert and at the edge of oasis,the sand-dust vertical deposition decreased with the increase of the height.But a partial unimodal distribution at the oasis site and the maximum deposition occurred at the height of 9 m,which corresponds to the middle height of farmland protection forest.The annual flux that passed through a section of 1 m in width and 50 m in height was 9169 kg in the desert,5318 kg at the edge of oasis,and 2345 kg in the oasis.And the annual fluxes at the edge of oasis and in the oasis are 42% and 74% less,respectively,than that in the desert.This implies that the wind break forest significantly reduced the intensity of sandstorms. 展开更多
关键词 Minqin the lower layer sand-dust horizontal flux vertical deposition
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