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基于Fluent的冰塞融化模拟 被引量:4
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作者 王军 石磊 《山西建筑》 2009年第15期362-363,共2页
针对冰塞的消融问题研究相对较少的现状,基于Fluent软件利用热力学及河冰水力学原理对冰塞的融化进行了初步模拟和探究,在已知河段的天气、水文等情况下对河面冰塞消融进行了模拟分析,从而有效模拟冰塞融化的状态。
关键词 冰塞融化 FLUENT 凝固和融化模型 模拟
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新疆石河子冻土特征及冻土融化期地温、冻土深度预报研究
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作者 王啸天 尹育红 +2 位作者 李红英 高宇 许浩翊 《中国农学通报》 2022年第16期97-102,共6页
为了确保春季播种安全,有必要开展播种期地温的监测和冻土融化深度预报业务。利用新疆农八师冻土气象观测资料,运用相关系数和线性回归方法,分析冻土特征及融化过程中地温变化、深度变化规律,建立春季冻土融化预报模型。结果表明,新疆... 为了确保春季播种安全,有必要开展播种期地温的监测和冻土融化深度预报业务。利用新疆农八师冻土气象观测资料,运用相关系数和线性回归方法,分析冻土特征及融化过程中地温变化、深度变化规律,建立春季冻土融化预报模型。结果表明,新疆农八师垦区稳定冻土期在11月中旬至翌年3月下旬,冻土最大深度呈逐年变浅趋势,倾向率为-5.4 cm/10 a;冻土结冻日期推后,倾向率为2.0 d/10 a;冻土化通日期提前,倾向率为-1.5 d/10 a。冻土融化期在3月中旬至4月上旬,冻土融化速率在3.1~4.0 cm/d之间。春季地温与平均气温、冻土融化深度与正积温具有显著的正相关,以此建立了相应的预报模型。10 cm地温预报模型历史回代准确率在96%以上,冻土融化深度预报模型历史回代准确率在94%以上。通过模型可以开展春季地温和土壤融化预报业务。 展开更多
关键词 新疆冻土 播种期地温 冻土特征 冻土融化预报模型 春季冻土融化
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积冰密度对机翼除冰过程影响的数值研究 被引量:5
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作者 雷桂林 郑梅 +1 位作者 董威 郭之强 《空气动力学学报》 CSCD 北大核心 2018年第6期958-965,共8页
针对不同类型的积冰,采用数值方法研究了不同冰密度对于电加热除冰过程中热传导及冰融化过程的影响。选取了典型结冰条件下所生成的两种霜冰及明冰作为分析对象,以标准的三维电加热除冰模型作为数值模拟研究模型,设置温度监测点,取金属... 针对不同类型的积冰,采用数值方法研究了不同冰密度对于电加热除冰过程中热传导及冰融化过程的影响。选取了典型结冰条件下所生成的两种霜冰及明冰作为分析对象,以标准的三维电加热除冰模型作为数值模拟研究模型,设置温度监测点,取金属蒙皮与冰的交界面作为监测面,在电加热除冰过程中记录监测点及监测面的温度变化情况。通过比较不同密度积冰融化过程中监测点与监测面的温度变化情况,分析积冰密度对冰融化过程的影响。计算结果表明,冰密度对电热除冰过程具有明显的影响,积冰密度降低会提高积冰温度升高的速度,使得积冰初始融化的时刻提前,整个融化过程缩短。 展开更多
关键词 霜冰 明冰 密度 电加热除冰 融化模型 融化
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双液滴对不同润湿性冷表面连续撞击的数值模拟
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作者 胡安杰 袁侨伟 +1 位作者 郭凯月 刘东 《Transactions of Nanjing University of Aeronautics and Astronautics》 EI CSCD 2023年第6期714-726,共13页
采用凝固/熔化模型和VOF(Volume-of-fluid)模型相结合的数值模拟方法研究了双液滴在低速条件下以不同的润湿性连续冲击冷表面的冻结行为。对比了液滴两种接触模式(扩散接触和收缩接触)下的液滴铺展及相变过程。模拟结果表明,液滴的聚结... 采用凝固/熔化模型和VOF(Volume-of-fluid)模型相结合的数值模拟方法研究了双液滴在低速条件下以不同的润湿性连续冲击冷表面的冻结行为。对比了液滴两种接触模式(扩散接触和收缩接触)下的液滴铺展及相变过程。模拟结果表明,液滴的聚结对液滴的形态有显著影响。当双液滴连续冲击亲水表面时,扩散接触的最大扩散因子相比单液滴增加26%~38%,收缩接触的最大扩散因子比单个液滴冲击增加15%~30%。而在超疏水表面上,单、双液滴冲击之间的最大扩散系数差异小于2%,可以忽略不计。此外,对双液滴在低温下与超疏水表面发生碰撞进行分析,得到完全反弹、部分反弹和完全粘附3种撞击结果在不同接触模式下液滴聚合以及凝固过程的影响规律。 展开更多
关键词 双液滴 结冰 凝固融化模型 VOF模型 超疏水表面
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基于Fluent的蓄冰槽气体取冷特性研究
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作者 茅靳丰 吉少杰 +1 位作者 李伟华 李永 《建筑热能通风空调》 2015年第1期52-54,31,共4页
为了探讨不同进气状态下的蓄冰槽释冷特性,通过对蓄冰槽与进风气体的耦合传热过程分析,建立了矩形蓄冰槽内外两侧的二维传热模型,基于CFD软件Fluent对不同进风温度、进风速度的工况进行了数值模拟,得到出风温度和冰的融化率在不同工况... 为了探讨不同进气状态下的蓄冰槽释冷特性,通过对蓄冰槽与进风气体的耦合传热过程分析,建立了矩形蓄冰槽内外两侧的二维传热模型,基于CFD软件Fluent对不同进风温度、进风速度的工况进行了数值模拟,得到出风温度和冰的融化率在不同工况下随时间的变化特性。结果表明:进风温度越高,出风温度越高,同时出风温度的降幅越大,进风温度对融冰速率的影响越明显;进风速度越大,出风温度减少量越小,进风速度对融化速率的影响越弱。 展开更多
关键词 凝固融化模型 气固耦合传热 融化速率
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Surface energy balance of Bayi Ice Cap in the middle of Qilian Mountains,China 被引量:2
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作者 QING Wen-wu HAN Chun-tan LIU Jun-feng 《Journal of Mountain Science》 SCIE CSCD 2018年第6期1229-1240,共12页
Energy balance at the glacier surface is important for understanding the impacts of climate change on glaciers. Here, we analyzed the characteristics of the glacier surface energy fluxes along with their contributions... Energy balance at the glacier surface is important for understanding the impacts of climate change on glaciers. Here, we analyzed the characteristics of the glacier surface energy fluxes along with their contributions to glacier melt on Bayi Ice Cap in Qilian Mountains by using a point-scale energy balance model. The half-hourly meteorological data from an automatic weather station(AWS) located on the glacier was used to drive the energy balance model. The model simulated results could accurately represent the mass-balance observations from the stake near the weather station during summer 2016. Our results showed the net radiation(86%) played an important role in the surface energy balance, and the contribution of the turbulent heat fluxes(14%) to the energy budget was relatively less important. A distinct behavior of energy balance, as compared to other continental glaciers in China(e.g., two adjacent glaciers Laohugou No. 12 Glacier and Qiyi Glacier), is the fact that a sustained period of positive turbulent latent flux exists on Bayi Ice Cap during August, causing faster melt rate in the month of August. Our study also presented the effect of frequent summer snowfall in slowing down surface melt by changing the surface albedo during the beginning of the melting season. 展开更多
关键词 Surface melting Energy balance Turbulent latent flux Summer snowfall GLACIER
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Desilication kinetics of calcined boron mud in molten sodium hydroxide media 被引量:3
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作者 NING Zhi-qiang SONG Qiu-shi +2 位作者 ZHAI Yu-chun XIE Hong-wei YU Kai 《Journal of Central South University》 SCIE EI CAS CSCD 2016年第9期2191-2198,共8页
Desilication kinetics of calcined boron mud(CBM) occurring in molten sodium hydroxide media was investigated. The effects of factors such as reaction temperature and Na OH-to-CBM mass ratio on silicon extraction effic... Desilication kinetics of calcined boron mud(CBM) occurring in molten sodium hydroxide media was investigated. The effects of factors such as reaction temperature and Na OH-to-CBM mass ratio on silicon extraction efficiency were studied. The results show that silicon extraction efficiency increases with increasing the reaction time and Na OH-to-CBM mass ratio. There are two stages for the desilication process of the calcined boron mud. The overall desilication process follows the shrinking-core model, and the first and second stages of the process were determined to obey the shrinking-core model for surface chemical reaction and the diffusion through the product layer, respectively. The activation energies of the first and second stages were calculated to be 44.78 k J/mol and 15.94 k J/mol, respectively. 展开更多
关键词 boron mud sodium hydroxide silicon dioxide KINETICS DESILICATION
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Multiresolution Fusion of Remote Sensing Images Based on Resolution Degradation Model
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作者 LIJunli SUNJiabing MAOXi 《Geo-Spatial Information Science》 2005年第1期50-56,共7页
A new method based on resolution degradation model is proposed to improve both spatial and spectral quality of the synthetic images. Some ETM+ panchromatic and multispectral images are used to assess the new method. I... A new method based on resolution degradation model is proposed to improve both spatial and spectral quality of the synthetic images. Some ETM+ panchromatic and multispectral images are used to assess the new method. Its spatial and spectral effects are evaluated by qualitative and quantitative measures and the results are compared with those of IHS, PCA, Brovey, OWT(Orthogonal Wavelet Transform) and RWT(Redundant Wavelet Transform). The results show that the new method can keep almost the same spatial resolution as the panchromatic images, and the spectral effect of the new method is as good as those of wavelet-based methods. 展开更多
关键词 image fusion resolution degradation model spectral distortion artificialvisual effect remote sensing
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Mechanism of slope failure in loess terrains during spring thawing 被引量:1
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作者 XU Jian WANG Zhang-quan +2 位作者 REN Jian-wei WANG Song-he JIN Long 《Journal of Mountain Science》 SCIE CSCD 2018年第4期845-858,共14页
Slope failure in loess terrains of Northern China during spring thawing period is closely related to the freeze-thaw cycling that surface soils inevitably experienced. Field surveys were carried out on natural and art... Slope failure in loess terrains of Northern China during spring thawing period is closely related to the freeze-thaw cycling that surface soils inevitably experienced. Field surveys were carried out on natural and artificial slopes in thirteen surveying sites located in the Northern Shaanxi, the center of Loess Plateau, covering five characteristic topographic features including tablelands, ridges, hills, gullies and valleys. Based on the scale that is involved in freeze-thaw cycling, the induced failures can be classified into three main modes, i.e., erosion, peeling and thaw collapse, depending on both high porosity and loose cementation of loess that is easily affected. Model tests on loess slopes with gradients of 53.1°, 45.0° and 33.7° were carried out to reveal the heat transfer, water migration and deformation during slope failure. The surface morphology of slopes was photographed, with flake shaped erosion and cracks noted. For three slope models, time histories for the thermal regime exhibit three obvious cycles of freeze and thaw andthe maximum frost depth develops downwards as freeze-thaw cycling proceeds. Soil water in the unfrozen domain beneath was migrated towards the slope surface, as can be noticed from the considerable change in the unfrozen water content, almost synchronous with the variation of temperature. The displacement in both vertical and horizontal directions varies over time and three obvious cycles can be traced. The residual displacement for each cycle tends to grow and the slopes with higher gradients are more sensitive to potentially sliding during freeze-thaw cycling. 展开更多
关键词 Freeze and thaw LOESS Slope failure Water migration Heat transfer
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