THE IMPACT OF THE CONTEMPORARY CLIMATIC CHANGE ON CHINAS THERMAL RESOURCES

ＴＨＥＩＭＰＡＣＴＯＦＴＨＥＣＯＮＴＥＭＰＯＲＡＲＹＣＬＩＭＡＴＩＣＣＨＡＮＧＥＯＮＣＨＩＮＡＳＴＨＥＲＭＡＬＲＥＳＯＵＲＣＥＳ￥ＬｉｕＹｕｎｆｅｎ（刘允芬）（ＣｏｍｍｉｓｓｉｏｎｆｏｒＩｎｔｅｇｒａｔｅｄＳｕｒｖｅｙｏｆＮａｔｕｒａｌＲｅｓｏｕｒｃ...     

Porothermoelastic analyses of anisotropic hollow cylinders with applications

It has been known that material anisotropy and thermal stresses affect borehole stability significantly. Aiming at the experimental studies associated with borehole stability in anisotropic (transversely isotropic) poroelastic materials subject to non‐isothermal conditions, this paper details and applies an anisotropic porothermoelastic solution to an unjacketed hollow cylinder in a triaxial set‐up. Numerical analyses are presented to demonstrate thermal and material anisotropy effects on the pore pressure and the stress concentrations in and around the geometry of a hollow cylinder subjected to thermal and stress perturbations. Copyright © 2004 John Wiley & Sons, Ltd.     

五极纵轴测深法在郑州地区热水资源勘探中的应用

郑州市区的地下热水来自增温地层，在使用电法勘探确定热水层位和埋深时，用五极纵轴测深法与对称四极测深法相结合，取得了良好的地质效果。     

棒在星系恒星形成中的作用

从理论Ｎ体模拟、射电辐射、红外辐射以及统计比较等几个方面，概述了棒在星系恒星形成中的作用，并讨论了在这一问题研究中出现的互相予盾的一些结果。     

短周期食双星V361Lyr和近相接的不接双星

短周期食双星Ｖ３６１Ｌｙｒ（ｐ＝０．３０９６天）可能是观测到的最短周期的由非简并天体且成的近相接双星，本文采用Ｋａｌｕｚｎｙ１９８９年观测到的Ｖ和Ｉ光变曲线进行了详细的测光分析。考虑到次子星上由于吸积而引起热斑在径度方向的可能延伸效应，而采用了多热斑模型近似，结果取得了对观测到的畸变光变曲线的很好的拟合。     

地幔载流子热传导机制初步研究

本文采用Fermi量子统计方法,对地幔电导率和载流子热传导机制问题进行了理论上的探讨。讨论结果表明,在过渡带和下地幔中,以往被忽视的载流子热导将成为热传递的主要机制.此外,本文还指出在高温高压下活化能A对地幔电导率变化速率有重要影响。     

Comptonization in the vicinity of the black hole horizon

Using a Monte Carlo method, we derive spectra arising from Comptonization taking place close to a Kerr black hole. We consider a model consisting of a hot thermal corona Comptonizing seed photons emitted by a cold accretion disc. We find that general relativistic effects are crucial for the emerging spectra in models, which involve significant contribution of radiation produced in the black hole ergosphere. As a result of this contribution, spectra of hard X-ray emission produced in the vicinity of a rapidly rotating black hole strongly depend on the inclination of the line of sight, with larger inclinations corresponding to harder spectra. Remarkably, such anisotropy could be responsible for properties of the X-ray spectra of Seyfert galaxies, which appear to be intrinsically harder in type 2 objects than in type 1, as reported recently.     

空调系统对城市大气温度影响的模拟研究

人为热排放对城市边界层气候效应的影响起着举足轻重的作用。在人为热源的组成中,建筑物内部的能源消耗、热量产生以及室内外热量传输与交换,对于城市热环境的改变有着非常重要的作用。因此,为研究室内空调系统的产热和通过屋顶、墙面、地面进行室内外热量传输扩散,并对室外热环境产生的影响,运用WRF（Weather Research and Forecasting Model）模式,选取BEP+BEM城市冠层参数化方案,即基于多层城市冠层方案BEP（Building Effect Parameterization）增加室内空调系统影响的建筑物能量模式BEM（Building Energy Model）的方案,以南京2010年8月2—3日,夏季三伏天晴天小风天气作为背景天气进行模拟研究。结果表明,采用WRF模式考虑空调系统室内、外能量交换的BEP+BEM参数化方案,能够更好地模拟出夏季晴天城市近地层气温。当假设空调全天开启时,白天模拟值与观测值吻合较好。夜间温度模拟值高于观测值,在22时—次日00时（北京时）,存在1℃左右的偏差。白天空调系统开启对于城市近地层气温的影响不明显,而夜间使得城市气温普遍升高0.6℃,尤其是在居民区密集的地方,22—23时最大有2℃左右的升温。当调整室内空调目标温度从25℃调至27℃时,空调系统能量总释放量减少12.66%,13—16时温度下降最大,平均约为1℃,建筑物越是密集,温度下降幅度越大。      

Study of thermal properties of supraglacial debris and degree-day factors on Lirung Glacier,Nepal

The extensive debris that covers glaciers in the ablation zone of the Himalayan region plays an important part in regulating ablation rates and water availability for the downstream region. The melt rate of ice is determined by the amount of heat conducted through debris material lying over the ice. This study presents the vertical temperature gradients, thermal properties in terms of thermal diffusivity and thermal conductivity, and positive degree-day factors for the debris-covered portion of Lirung Glacier in Langtang Valley, Nepal Himalaya using field-based measurements from three different seasons.Field measurements include debris temperatures at different debris thicknesses, air temperature, and ice melt during the monsoon(2013), winter(2013), and pre-monsoon(2014) seasons. We used a thermal equation to estimate thermal diffusivity and thermal conductivity, and degree-day factors(DDF) were calculated from cumulative positive temperature and ice melt of the measurement period. Our analysis of debris temperature profiles at different depths of debris show the daily linear gradients of-20.81 °C/m, 4.05 °C/m, and-7.79 °C/m in the monsoon, winter, and pre-monsoon seasons, respectively. The values of thermal diffusivity and thermal conductivity in the monsoon season were 10 times greater than in the winter season. The large difference in these values is attributed to surface temperature and moisture content within the debris. Similarly, we found higher values of DDFs at thinner debris for the pre-monsoon season than in the monsoon season although we observed less melting during the pre-monsoon season. This is attributed to higher cumulative temperature during the monsoon season than in the pre-monsoon season. Our study advances our understanding of heat conductivity through debris material in different seasons, which supports estimating ice melt and discharge from glacierized river basins with debris-covered glaciers in the Himalayan region.     

Improvement and Evaluation of the Latest Version of WRF-Lake at a Deep Riverine Reservoir

The WRF-lake vertically one-dimensional(1D) water temperature model, as a submodule of the Weather Research and Forecasting(WRF) system, is being widely used to investigate water–atmosphere interactions. But previous applications revealed that it cannot accurately simulate the water temperature in a deep riverine reservoir during a large flow rate period, and whether it can produce sufficiently accurate heat flux through the water surface of deep riverine reservoirs remains uncertain. In this st...