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MC型碳化物的稳态/非稳态凝固转化机制 被引量:6
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作者 陈瑶 王华明 《中国有色金属学报》 EI CAS CSCD 北大核心 2002年第2期305-308,共4页
分析了平衡凝固MC碳化物规则块状八面体稳态生长的条件及影响MC碳化物稳态生长的因素。结果表明 :凝固过程中局部冷却速度的改变以及熔体中局部热流方向的扰动 ,都将影响熔体中MC碳化物形成元素的扩散 ,导致MC碳化物偏离稳态生长条件 。
关键词 MC型碳化物 稳态/非稳态生长 凝固机制
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叶片水H_2^(18)O富集的研究进展 被引量:15
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作者 温学发 张世春 +1 位作者 孙晓敏 于贵瑞 《植物生态学报》 CAS CSCD 北大核心 2008年第4期961-966,共6页
植物叶片水H218O富集对大气中O2和CO2的18O收支有着重要影响。蒸腾作用使植物叶片水H218O富集,而植物叶片水H218O富集的程度主要受大气水汽δ18O和植物蒸腾水汽δ18O的影响。过去,通过引入稳态假设(蒸腾δ18O等于茎水δ18O)得到Craig-Go... 植物叶片水H218O富集对大气中O2和CO2的18O收支有着重要影响。蒸腾作用使植物叶片水H218O富集,而植物叶片水H218O富集的程度主要受大气水汽δ18O和植物蒸腾水汽δ18O的影响。过去,通过引入稳态假设(蒸腾δ18O等于茎水δ18O)得到Craig-Gordon模型的闭合形式,或将植物整个叶片水δ18O经过Péclet效应校正后得到植物叶片水δ18O的富集程度。然而,在几分钟到几小时的短时间尺度上,植物叶片蒸腾δ18O是变化的,稳态假设是无法满足的。最近成功地实现了对大气水汽δ18O和δD的原位连续观测,观测精度(小时尺度)可达到甚至优于稳定同位素质谱仪的观测精度。在非破坏性条件下,高时间分辨率和连续的大气水汽δ18O和蒸腾δ18O的动态观测,将提高植物叶片水H218O富集的预测能力。该文综述了植物叶片水H218O富集的理论研究的新进展、研究焦点和观测方法所存在的问题,旨在进一步加深理解植物叶片水H218O富集的过程及其机制。 展开更多
关键词 定同位素 Craig-Gordon模型 稳态/非稳态
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Temperature field distribution of burnt surrounding rock in UCG stope 被引量:10
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作者 Xin Lin Wang Zuotang +4 位作者 Huang Wengang Kang Guojun Lu Xuefeng Zhang Peng Wang Jianhua 《International Journal of Mining Science and Technology》 SCIE EI 2014年第4期573-580,共8页
In order to study temperature field distribution in burnt surrounding rock and to determine ranges of burnt surrounding rock, coal-wall coking cycle and heat influence in the underground coal gasification(UCG) stope, ... In order to study temperature field distribution in burnt surrounding rock and to determine ranges of burnt surrounding rock, coal-wall coking cycle and heat influence in the underground coal gasification(UCG) stope, based on the Laplace transform and inversion formula, we studied the temperature analytical solution of one-dimensional unsteady heat conduction for multi-layer overlying strata under the first and the forth kinds of boundary conditions, and we also carried out a numerical simulation of twodimensional unsteady heat conduction by the COMSOL multiphysics. The results show that when the boundary temperature of surrounding rock has a linear decrease because of a directional movement of heat source in the UCG flame working face, the temperature in surrounding rock increases first and then decreases with time, the peak of temperature curve decreases gradually and its position moves inside surrounding rock from the boundary. In the surrounding rock of UCG stope, there is an envelope curve of temperature curve clusters. We analyzed the influence of thermophysical parameters on envelope curves and put forward to take envelope curve as the calculation basis for ranges of burnt surrounding rock, coal-wall coking cycle and heat influence. Finally, the concrete numerical values are given by determining those judgement standards and temperature thresholds, which basically tally with the field geophysical prospecting results. 展开更多
关键词 Underground coal gasification (UCG) Temperature distribution Laplace transform Envelope curve Burnt surrounding rock Coking cycle
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