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选取年雷击大地密度、产值密度和人口密度3个因子作为评判指标,利用模糊综合评判法对厦门市6个区的雷电灾害风险进行了评估.结果显示:厦门市各区雷电灾害风险受地闪频次、经济发展和人口密度分布不均等因素的影响,思明区为高风险区,翔安区为低风险区,其余4个区为中等风险区.该划分为厦门市防雷部门针对本地实际情况制定科学、合理、经济的防雷设计方案提供了更为细致的参考. 相似文献
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利用雷州半岛2007年7、8月常规地面气象观测资料和闪电定位资料,分析了闪电活动与24 h降水量及雨强的关系,结果表明:雷州半岛盛夏地闪频数的最大值中心在其东侧海面上,地闪高发带沿海岸线呈南北向分布;地闪频次存在明显的日变化特征,13:00～18:00为闪电高发时段;无闪电时,有41.3%的降水事件24 h降水量≤1 mm,61.5%的降水事件雨强≤1 mm·h-1;有闪电时相应的事件概率分别为25.9%和37.7%;24 h降水量>30 mm的事件大多发生在有闪电的情况下,无闪电时极少发生;雨强概率分布的日变化特征不明显;有闪电活动时,雨强均值变化幅度加大. 相似文献
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Microphysical characteristics of sea fog over the east coast of Leizhou Peninsula, China 总被引：1，自引：0，他引：1
Microphysical properties of sea fog and correlations of these properties were analyzed based on the measurements from a comprehensive field campaign carried out from 15 March to 18 April 2010 on Donghai Island (21°35’’N, 110°32’5’’E) in Zhanjiang, Guangdong Province, China. There were four types of circula- tion pattern in favor of sea fog events in this area identified, and the synoptic weather pattern was found to influence the microphysical properties of the sea fogs. Those influenced by a warm sector in front of a cold front or the anterior part of low pressure were found to usually have a much longer duration, lower visibility, greater liquid water content, and bigger fog droplet sizes. A fog droplet number concentration of N≥1 cm-3 and liquid water content of L≥0.001 g m-3 can be used to define sea fogs in this area. The type of fog droplet size distribution of the sea fog events was mostly monotonically-decreasing, with the spectrum width always being >20 μm. The significant temporal variation of N was due in large part to the number concentration variation of fog droplets with radius <3 μm. A strong collection process appeared when droplet spectrum width was >10 μm, which subsequently led to the sudden increase of droplet spectrum width. The dominant physical process during the sea fog events was activation with subsequent condensational growth or reversible evaporation processes, but turbulent mixing also played an important role. The collection process occurred, but was not vital. 相似文献
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搭建了光纤布里渊频移测量系统,实现了色散位移光纤20 ℃到820 ℃布里渊频移的测量,并对测量数据进行拟合. 在环境温度大范围变化时,目前采用的布里渊频移-温度一阶线性关系式对测量数据分析误差较大,针对这个问题,本文从纯石英光纤的结构特点和材料的物性系数出发,在分析光纤的热膨胀系数、光纤密度、折射率、弹性模量和泊松比与宽范围温度关系的基础上,根据布里渊频移与各物性参数的关系式理论推导了宽范围温度变化与布里渊频移之间的二次项关系式. 理论推导结果与实验数据基本符合,验证了理论分析的正确性,从而为光纤宽范围布 相似文献
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深部煤层含气量变化特征与浅部有所不同,实测数据极少,需要研发新的方法对其进行预测。本文以鄂尔多斯盆地东部主煤层为对象,分析了影响吸附常数的地质因素。基于煤样在不同温度条件下的高压甲烷等温吸附实验,采用主成分分析方法,探讨了深部煤层含气量预测方法。选取温度、镜质组反射率、水分含量、灰分产率、镜质组含量、惰质组含量6个因素进行主成分分析,提取出3个主成分,获得吸附常数与3个主成分之间的多元一次函数关系,根据朗格缪尔方程并结合含气饱和度建立了深部煤层含气量预测模型。采用这一模型,对鄂尔多斯盆地东部深部煤层进行了实例研究。结果表明,煤层含气量随埋深的变化存在一个临界深度,临界深度大致在750~1200m之间,随煤级及地层温度和地层压力而呈规律性变化。在临界深度以浅,煤层含气量随埋深的增大而增高;超过临界深度后,含气量随埋深的增大而减低。 相似文献