半硬半软岩隧道塌方的力学特性及处理方法分析

由于蛟岭隧道出口横断面一半为硬岩,结构完整,而另一半为软岩,为风化岩层,且较为破碎,所以在隧道开挖时,硬岩一侧刚度较大,变形较小,自稳能力大;软岩一侧与之相反,遇水软化,流变性明显,所以在软硬岩交界面处,产生滑移,导致塌方,从而在软岩一侧采取了地表加固和掌子面管棚注浆的处理,形成了与硬岩接近的强度,使隧道周围形成一个承载环,并对处理段进行了监测,监测数据分析表明处理后迅速达到稳定。     

Carbon isotope characteristics,origin and distribution of the natural gases from the Tertiary salty lacustrine facies in the West Depression Region in the Qaidam Basin

Since the Meso-Cenozoic, controlled by paleoclimate, a series of fresh to brackish water basins and salt to semi-salt water basins were developed in wet climatic zones and in dry climate zones in China, respectively[1]. The geological and geochemical char…     

基于小波去噪的非等间隔变形监测数据GM(1,1)预测方法研究

在小波去噪和非等间隔GM(1,1)的基础上提出基于小波去噪的非等间隔GM(1,1)组合模型的预测方法,并且通过矿区实测数据模拟实验对三种方法进行对比分析。结果表明,小波去噪的模拟精度高于非等间隔GM(1,1),组合模型的预计精度高于单独使用非等间隔GM(1,1),验证了该方法的实用性和可靠性。     

Mapping land subsidence over the eastern Beijing city using satellite radar interferometry*

Beijing City has suffered from groundwater-induced subsidence since the late 1930s and the over-exploration of groundwater could lead to subsidence as much as ?12.0 cm?yr^?1. Previous studies on the ground deformation at Beijing City mainly focused on the period before the year of 2014 when a mega-engineering project was launched to reduce water shortage in Beijing. To study the most recent ground deformation, 19 L-band ALOS-1 PALSAR images (June 2007–January 2011), 24 C-band Sentinel-1 SAR images (June 2015–November 2016) together with 9 ALOS-2 PALSAR acquisitions (September 2014–February 2017) were analysed in this work. Levelling measurements were exploited to verify the ALOS-1-based time series InSAR (TS-InSAR) result while Sentinel-1 and ALOS-2 result were cross-verified with each other. Furthermore, the whole study area was divided into four sub-zones, and the result indicated that the subsidence rates over five townships, Cuigezhuan, Jinzhan, Liyuan, Songzhuang and Yanjiao were accelerating and more attentions should be paid. On the contrary, the town centre of Douge Zhuang township experienced a decreasing trend between these two temporal-periods. Additionally, the time series measurements with respect to five selected measurement points and the profile line along the subsidence hot spots were analysed.     

安徽滁河断裂带温泉的水化学和同位素特征及成因分析

笔者等以安徽滁河断裂带内的6个温泉为主要研究对象,分析了水样的水化学特征,利用氢氧同位素对温泉的补给方程进行估算,并提出温泉的成因模式。研究区温泉阳离子以Ca2+和Mg2+为主,根据SO2-4和HCO-3的相对含量的不同,可以将水样分为两组,A组水样（富HCO-3）的主要离子的质量浓度均低于B组（富SO2-4）水样,A组水样的水化学类型为HCO-3—Ca2+·Mg2+; B组水样的（除AH16 4为SO2-4—Ca2+外）水化学类型为SO2+4—Ca2+·Mg2+。A组水样的稀土元素含量高于B组,二者均在NASC标准化图解上表现出平坦型的配分模式,且都表现出轻稀土富集和Eu正异常的特征。水样的氢氧稳定同位素组成表明温泉的补给来源都是大气降水,补给区温度约为13~15 ℃。A组温泉的补给高程为120~160 m低于B组温泉的200~260 m,且A组温泉的热储温度为45~70℃,低于B组温泉的热储温度70~105 ℃。地下水经历深循环获得大地热流加热后沿断裂带上升出地表。     

雪崩灾害的遥感量化分析与工程选线

为评估雪崩灾害对道路工程方案的影响与危害,基于多时相高分辨率IKONOS卫星立体图像或机载激光雷达数据生成雪崩灾害区域高密度、高精度数字地面模型(DEM)与高分辨率数字正射影像(DOM),自动提取雪崩灾害的成灾与孕灾因子,并进行量化动态分析,采用层次分析法构建雪崩灾害加权评估模型,实现工程选址及方案比选与优化设计.该方法在西藏墨脱公路的应用表明,雪崩灾害的遥感量化分析与评估,全面、准确地对区域雪崩灾害进行了定性与定量分析,科学、合理地确定了工程方案.     

山东省海洋牧场现状与发展思路

海洋牧场是一种新型海洋渔业生产方式,以生态系统构建为核心,科学开发利用海洋资源。山东省是海洋牧场建设较早省份之一,在海洋牧场创新发展方面做了大量有益探索,取得较好成效,走出了一条经济发展与环境改善双赢之路,为全国现代化海洋牧场建设做出示范引领。文章阐述了山东省海洋牧场建设历程和现状,总结了经验做法,分析了面临的机遇与挑战,并提出下一步发展思路,以期为我国海洋牧场建设与决策提供参考。     

福建沿海鲸鲨时空分布初探及保护对策

搁浅、误捕和救助记录是研究野生动物分布和获取其基本生物学数据的重要来源,尤其是对那些缺少系统性野外调查的物种。本研究收集了福建沿海2006—2019年间鲸鲨（Rhincodon typus）的搁浅、误捕和救助记录,初步探讨福建沿海鲸鲨的时空分布情况,并提出相应的保护对策。共收集福建沿海鲸鲨搁浅、误捕和救助记录30例,包括搁浅10例、误捕18例和救助2例,其中福州鲸鲨记录大部分在平潭岛附近,这可能与平潭海域上升流带来的丰富生物资源有关;所有记录中有28例（93.3%）发生在6—10月,表明夏秋季可能是鲸鲨在福建沿海活动的高峰期。此外,有体长记录的22条鲸鲨中,17条（77.3%）为幼年个体,可能是因为幼年鲸鲨偏好在高生产力的近岸海域聚集以获取充足的食物,因此也更容易搁浅或被误捕。较多的误捕记录（60.0％）提示渔业活动对鲸鲨有较大威胁。因此,建议建立全省甚至全国性的鲸鲨搁浅误捕数据库,进一步严格和规范渔业管理,改进渔具以降低误捕鲸鲨的概率,加强对公众（特别是渔民）的宣传教育,以更好地保护这一濒危物种。     

Studies on Factors Influencing Hydrodynamic Characteristics of Plates Used in Artificial Reefs

As a simplified model of artificial reefs, a series of plate models punched with square or circular openings are designed to investigate the effects of openings on the hydrodynamic characteristics of artificial reefs. The models are grouped by various opening numbers and opening-area ratios. They are physically tested in a water flume or used in the numerical simulation to obtain the drag force in the uniform flow with different speeds. The simulation results are found in good agreement with the experimental measurements. By the non-dimensional analysis, the drag coefficient specified to each model is achieved and the effects of openings are examined. It is found that the key factor affecting the drag coefficient is the open-area ratio. Generally, the drag coefficient is a linear function of the open area ratio with a minus slope. The empirical formulae for the square and circular openings respectively are deduced by means of the multiple regression analysis based on the measured and numerical data. They will be good references for the design of new artificial reefs. As a result of numerical simulation, the vorticity contours and pressure distribution are also presented in this work to better understand the hydrodynamic characteristics of different models.     

南海北部陆丰凹陷LF14井中新世古水深变化及沉降特征*

南海北部陆丰凹陷内LF14井记录了早中新世至早上新世的海相沉积地层。古水深重建结果显示研究井位在早中新世突然发生海侵, 水深迅速上升至最大值275m, 随后经数次波动, 整体处于中—外陆架环境, 共记录了5个完整的海侵—海退层序。回剥分析方法重建的LF14井沉降史揭示了研究井位在中中新世(17.5—10Ma)处于快速沉降期, 快速沉降导致的凹陷内沉积物的可容纳空间发育速率高和陆源物质供给充足是造成该阶段沉积速率高的两个重要因素; 晚中新世—早上新世(10—4.53Ma)处于弱沉降期, 推测东沙运动导致凹陷内的沉积物可容纳空间发育速率变小和陆源物质供给减少, 造成该时期内研究井位沉积速率低。最后, 依据定量重建的古水深变化在研究层段识别出一系列短暂存在的构造上升事件。