内衬非开挖管道修复技术及其应用分析

内衬非开挖管道修复技术是在不开挖情况下,利用原管位资源,采取相关技术在现有管道内安装内衬的方式使管道获得再生,可以重新获得30～50年的使用寿命.对内衬法非开挖管道修复技术的工艺原理进行了介绍,对其应用前景进行了分析.     

潮汐对瞬态气候响应模拟的影响研究

In this study, the impact of oceanic processes on the sensitivity of transient climate change is investigated using two sets of coupled experiments with and without tidal forcing, which are termed Exp_Tide and Exp_Control,respectively. After introducing tidal forcing, the transient climate response(TCR) decreases from 2.32 K to 1.90 K,and the surface air temperature warming at high latitudes decreases by 29%. Large ocean heat uptake efficiency and heat storage can explain the low TCR in Exp_Tide. Approximately 21% more heat is stored in the ocean in Exp_Tide(1.10×10~(24) J) than in Exp_Control(0.91×10~(24) J). Most of the large ocean warming occurs in the upper 1 000 m between 60°S and 60°N, primarily in the Atlantic and Southern Oceans. This ocean warming is closely related to the Atlantic Meridional Overturning Circulation(AMOC). The initial transport at mid-and high latitudes and the decline in the AMOC observed in Exp_Tide are both larger than those observed in Exp_Control. The spatial structures of AMOC are also different with and without tidal forcing in present experiments. The AMOC in Exp_Tide has a large northward extension. We also investigated the relationship between AMOC and TCR suggested by previous studies using the present experiments.     

非开挖管道翻转内衬修复技术的探讨

本文重点介绍了翻转内衬修复技术的原理、工序、技术特点等,并概括介绍了其它几种非开挖修复技术修复城市燃气埋地管道的方法,最后展望了翻衬法的应用及推广前景。     

英国排水管道修复新技术

德国与英国的管道修复公司合作开发出一种称为Epros SeaLiner的原位固化法管道修复技术,其包括衬管材料、特制树脂和技术工艺。应用该技术能在地下水渗入破损管道的条件下施工,可靠密封衬管与宿主管之间环状间隙和枝管重开处的接头,彻底克服内衬修复及接口重开所致的渗漏问题。     

南海上层经向翻转环流的低频变化

The low-frequency variability of the shallow meridional overturning circulation(MOC) in the South China Sea(SCS) is investigated using a Simple Ocean Data Assimilation(SODA) product for the period of 1900–2010. A dynamical decomposition method is used in which the MOC is decomposed into the Ekman, external mode, and vertical shear components. Results show that all the three dynamical components contribute to the formation of the seasonal and annual mean shallow MOC in the SCS. The shallow MOC in the SCS consists of two cells: a clockwise cell in the south and an anticlockwise cell in the north; the former is controlled by the Ekman flow and the latter is dominated by the external barotropic flow, with the contribution of the vertical shear being to reduce the magnitude of both cells. In addition, the strength of the MOC in the south is found to have a falling trend over the past century, due mainly to a weakening of the Luzon Strait transport(LST) that reduces the transport of the external component. Further analysis suggests that the weakening of the LST is closely related to a weakening of the westerly wind anomalies over the equatorial Pacific, which leads to a southward shift of the North Equatorial Current(NEC) bifurcation and thus a stronger transport of the Kuroshio east of Luzon.     

CMIP5地球系统模式溶解氧模拟结果分析

本文基于常用的统计方法,通过与WOA09观测的海洋溶解氧浓度数据进行比较,定量地评估了9个CMIP5地球系统模式在历史排放试验中海洋溶解氧气候态特征的模拟能力。在海表,由于地球系统模式均能很好地模拟海表温度（SST）,模式模拟的海表溶解氧浓度分布与观测一致,模拟结果无论是全球平均浓度偏差还是均方根误差均接近0,空间相关系数与标准偏差接近1。在海洋中层以及深层这些重要水团所在的区域,各模式的模拟能力则差异较大,尤其在溶解氧低值区（OMZs）所在的500m到1000m,各模式均出现全球平均偏差、均方根误差的极大值以及空间相关系数的极小值。在海洋内部,模式偏差的原因比较复杂。经向翻转环流和颗粒有机碳通量均对模式的偏差有贡献。分析结果表明物理场偏差对溶解氧偏差的贡献较大。一些重要水团,比如北大西洋深水,南极底层水以及北太平洋中层水在极大程度上影响了溶解氧在这些海区的分布。需要指出的是,虽然在海洋内部各模式模拟的溶解氧浓度偏差较大,但是多模式平均结果却能表现出与观测较好的一致性。     

海原断裂干盐池拉分盆地中央断层的形成机制探讨

拉分盆地内部的"对角线式中央断层",不仅在拉分盆地的消亡过程中发挥着重要作用,还对大地震的发生具有重要控制作用,研究其形成演化具有重要的意义.然而,与拉分盆地相比,专门针对中央断层的研究较少,制约了人们对拉分盆地乃至走滑断裂带构造演化过程的理解.文中以海原断裂带中段的干盐池拉分盆地为例,对盆地内的中央断层开展了地质地貌...     

地理信息科学基于慕课和翻转课堂教学模式的探索与实践

推进信息技术与教育教学的深度融合,通过课程内容、教学模式与教学方法的改革,打造高阶性、创新性和具有挑战度的金课是目前我国高等教育的重要任务.随着科技的发展和互联网的普及,传统地理信息科学教学模式中以课堂为载体、以教师为主导的教育形式已经满足不了大学生和社会公众对于了解和掌握知识的需求,急需探索一种新的教学模式让学生更加...     

翻转课堂+多维度考核体系下的工程测量学实践教学改革

工程测量学是测绘工程专业的核心课程,是实际测绘工作过程中应用最多的课程之一,其实践教学效果的好坏直接影响学生毕业后的就业质量。本文针对当前工程测量学实践教学当中存在的突出问题,提出了以翻转课堂+多维度考核体系并重的实践教学模式,经过两年的教学改革,在实践内容、实践教学方法和考核体系等方面取得了丰硕的研究成果,并在其他课程中推广应用。