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31.
襄樊——广济断裂西段的三里岗——三阳地区出露有构造混杂岩,以含蛇绿岩残块为特征,经历了复杂的构造变形和演化过程。不同区段的构造解析与对比表明,中生代以来该构造混杂岩带主要遭受了4期变形构造的叠加改造:1)高温塑性变形(D1),表现为蛇绿岩残块内部具网状强应变带和透镜状弱应变域相互交织的构造变形样式,强应变带形成以镁铁质糜棱岩为特征的高温韧性剪切带,显示深层次构造变形特征;2)逆冲推覆变形(D2),构造混杂岩带发育叠瓦状逆冲推覆构造和双冲构造,南界韧性剪切带是构造混杂岩带整体运移的主推覆面,发育长英质糜棱岩,形成于中等构造层次,岩石中发育镁铁质糜棱岩糜棱面理的褶皱构造,显示陆内逆冲推覆对先期高温塑性变形构造的叠加改造;3)韧脆性右行平移剪切(D3),形成构造混杂岩带内部浅层次构造变形,构造混杂岩带南侧的花山群钙质片岩揉皱变形,形成枢纽近直立的不对称褶皱,指示右行平移剪切变形;4)伸展正断层(D4),主要发育于构造混杂岩带北侧,呈NW——SE向展布,控制晚白垩世断陷盆地的形成与沉积充填。  相似文献   
32.
将《地震学刊》更名为《防灾减灾工程学报》10余年的历程进行了分析,阐述了《学报》采取诸多举措,从一个濒危的省级地方刊物成长为国内外认可的优秀核心期刊。其影响力不断扩大,学术水平不断提高,成为业内科研人员学术交流的前沿阵地。  相似文献   
33.
从办刊宗旨的演变过程、发表论文专业结构调整、对自由投稿的发掘引导、专刊约稿的组织出版、学术会议的推动促进等方面,探讨了《防灾减灾工程学报》在拓展稿源渠道方面的实践,并提出了改进措施。  相似文献   
34.
结合计算判断法和经验对比法,构建了葡萄酒产业生命周期模型,从产业规模、产业市场结构、技术进步与效率以及政府角色四个维度出发,对中国葡萄酒产业发展阶段进行综合评判。应用皮尔生长曲线测算了中国葡萄酒产业各阶段演进时间、产业发展规模与速度以及产业峰值。结果表明,中国葡萄酒产业正处于成长期早期阶段,并在产品研发、产品市场消费结构、技术创新、产业组织提升等方面正进入一个重大的调整与升级时期。2013年和2019年分别为中国葡萄酒产业发展的"起飞点"与"飞跃点"。2026年开始中国葡萄酒产业将进入成熟期,届时产值将达到1 216.598×108元,并不断趋于产业饱和值1 541.949×108元,未来产业发展空间巨大。本研究对制订与产业生命周期阶段相吻合的政策,以实现产业的长期动态协调与均衡发展具有重要意义。  相似文献   
35.
模糊聚类方法研究堤坝渗漏   总被引:6,自引:0,他引:6  
樊哲超  陈建生  董海洲  赵霞 《岩土力学》2006,27(7):1214-1218
稳定同位素、水化学的方法是研究堤防渗漏是一种十分有效的方法,以往人们大多只是定性的分析判断。结合北江大堤工程实例,尝试应用模糊聚类方法,选取22个水样稳定同位素和水化学值作为指标特征值,并赋与不同的权重,进行模糊聚类分析,聚类结果表明,T12孔和T9孔北5 m处涌水、江水和T9孔北排水沟出水在稳定同位素和水化学成分的Cl-及TDS上表现出了较大的相关性,可能为同一补给来源,为堤坝渗漏通道的判断提供了佐证。  相似文献   
36.
The dynamics of the teleconnection between the Indian Ocean Dipole(IOD) in the tropical Indian Ocean and El Ni?o-Southern Oscillation(ENSO) in the tropical Pacific Ocean at the time lag of one year are investigated using lag correlations between the oceanic anomalies in the southeastern tropical Indian Ocean in fall and those in the tropical Indo-Pacific Ocean in the following winter-fall seasons in the observations and in high-resolution global ocean model simulations. The lag correlations suggest that the IOD-forced interannual transport anomalies of the Indonesian Throughflow generate thermocline anomalies in the western equatorial Pacific Ocean, which propagate to the east to induce ocean-atmosphere coupled evolution leading to ENSO. In comparison, lag correlations between the surface zonal wind anomalies over the western equatorial Pacific in fall and the Indo-Pacific oceanic anomalies at time lags longer than a season are all insignificant, suggesting the short memory of the atmospheric bridge. A linear continuously stratified model is used to investigate the dynamics of the oceanic connection between the tropical Indian and Pacific Oceans. The experiments suggest that interannual equatorial Kelvin waves from the Indian Ocean propagate into the equatorial Pacific Ocean through the Makassar Strait and the eastern Indonesian seas with a penetration rate of about 10%–15% depending on the baroclinic modes. The IOD-ENSO teleconnection is found to get stronger in the past century or so. Diagnoses of the CMIP5 model simulations suggest that the increased teleconnection is associated with decreased Indonesian Throughflow transports in the recent century, which is found sensitive to the global warming forcing.The dynamics of the teleconnection between the Indian Ocean Dipole(IOD)in the tropical Indian Ocean and El Ni?o-Southern Oscillation(ENSO)in the tropical Pacific Ocean at the time lag of one year are investigated using lag correlations between the oceanic anomalies in the southeastern tropical Indian Ocean in fall and those in the tropical Indo-Pacific Ocean in the following winter-fall seasons in the observations and in high-resolution global ocean model simulations.The lag correlations suggest that the IOD-forced interannual transport anomalies of the Indonesian Throughflow generate thermocline anomalies in the western equatorial Pacific Ocean,which propagate to the east to induce ocean-atmosphere coupled evolution leading to ENSO.In comparison,lag correlations between the surface zonal wind anomalies over the western equatorial Pacific in fall and the Indo-Pacific oceanic anomalies at time lags longer than a season are all insignificant,suggesting the short memory of the atmospheric bridge.A linear continuously stratified model is used to investigate the dynamics of the oceanic connection between the tropical Indian and Pacific Oceans.The experiments suggest that interannual equatorial Kelvin waves from the Indian Ocean propagate into the equatorial Pacific Ocean through the Makassar Strait and the eastern Indonesian seas with a penetration rate of about 10%–15%depending on the baroclinic modes.The IOD-ENSO teleconnection is found to get stronger in the past century or so.Diagnoses of the CMIP5 model simulations suggest that the increased teleconnection is associated with decreased Indonesian Throughflow transports in the recent century,which is found sensitive to the global warming forcing.  相似文献   
37.
纳米纤维可以填补有机涂层中存在的孔隙和微裂纹,并提高其抗腐蚀能力。本文介绍了一种利用静电纺丝方法在Q235碳钢表面制备纳米纤维,并与有机环氧树脂复合,进而提高树脂防腐性能的技术。制备了环氧-纤维复合涂层(PAN-NFs/EP),采用电化学方法以及盐雾实验对复合涂层的防腐性能进行了表征,结果表明嵌入了纳米纤维的环氧复合涂层,其电化学阻抗提高了两个数量级,防腐性能明显提高。本研究对静电纺丝技术在海洋防腐中的应用具有一定的参考价值。  相似文献   
38.
文章以青岛汇泉湾为例,分析了汇泉湾海滩砂粒粗化的原因,并就如何保护好海滩旅游资源提出一些建议.  相似文献   
39.
40.
赵霞  李建平 《大气科学进展》2009,26(6):1125-1136
The persistence barrier refers to the lag correlation of sea surface temperature anomalies (SSTA) showing a rapid and significant decline in a specific season, regardless of the starting month. This implies that there is a decrease in forecast skill for SSTA in this specific season. This paper investigates the possible causes for the persistence barrier of SSTA in the South China Sea (SCS) and its adjacent regions from the perspective of interannual-interdecadal time scales. The results show that the persistence barrier of SSTA exists not only in the SCS, but also in the vicinity of Indonesia south of the equator. The SCS barrier occurs around October--November, while the occurrence of the barrier in the Indonesia region is around November--December. For these two regions, the occurrence of the persistence barrier is closely associated with the interdecadal variability of SSTA, as well as the interannual variability. The persistence barriers in the SCS and the Indonesia region do not exist alone if the interdecadal variability is not considered, because SSTA have a short memory of less than 4 months, regardless of the starting month. Moreover, the influence of the interdecadal variability of SSTA on the persistence barrier of SSTA in the SCS and the Indonesia region may be associated with SSTA in the Indian Ocean and the western Pacific, but is not closely associated with the Pacific Decadal Oscillation. However, compared with the spring persistence barrier (SPB) of ENSO, the close relationship between the persistence barriers in the SCS and the Indonesia region and the interdecadal variability is unique, since the ENSO SPB is not significantly affected by such variability. In addition, although the persistence barriers in both the SCS and the Indonesia region are quite obvious in strong ENSO cases, the interdecadal variability of SSTA also plays a non-negligible role in this relationship.  相似文献   
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