我国高碘卤水分布规律及其形成(续1)——世界高碘卤水的分布回顾

根据国内外大量实际资料,从碘的分布情况及其所处的地质条件,结合石油和天然气形成过程、油气藏类型及其分布特点,探讨高碘卤水分布的规律及其形成条件,在此基础上指出了我国的找碘方向。     

地震动位移峰值对斜拉桥地震反应的影响

根据同一加速度反应谱拟合了加速度峰值相同、速度峰值相同、位移峰值不同的两组地震动时程。以大跨斜拉桥的三维模型为例，在以上两组时程的激励下，应用有限元立法，对斜拉桥的地震反应进行了分析。计算结果表明：在弹性阶段，地震动位移峰值时斜拉桥的动力响应影响不明显；但当结构进入弹塑性阶段时，在位移峰值较大的一组地震动激励下，桥梁的墩底弯矩和塔顶位移会有更大的响应。     

甘肃省农村民房地基基础及其安全问题

对甘肃省农村非工程结构民房地基进行了分类,对各类型地基基础的特性和存在的安全性问题进行了讨论,提出了提高民房抗震能力的改进措施。认为需要通过技术培训、宣传和民房建设管理等途径来提高农村地区民房建设水平。     

Magnetic and ground probing radar measurements for soil pollution mapping in the industrial area of Val Basento (Basilicata Region, Southern Italy): a case study

The joint application of electromagnetic techniques for near-surface exploration is a useful tool for soil pollution monitoring and can also contribute towards describing the spatial distribution of pollutants. The results of a geophysical field survey that was carried out for characterizing the heavy metal and waste disposal soil pollution phenomena in the industrial area of Val Basento (Basilicata region, Southern Italy) are presented here. First, topsoil magnetic susceptibility measurements have been carried out for defining the spatial distribution of superficial pollution phenomena in the investigated area. Second, detailed and integrated measurements based on a high-resolution magnetic mapping and ground probing radar (GPR) profiling have been applied to investigate the subsurface in two industrial areas located in more polluted sites that were identified during the first phase. Our monitoring strategy discloses the way to rapidly define the zone characterized by high pollution levels deriving from chemical industries and traffic emissions and to obtain the way information about the presence of local buried sources of contamination.     

Delimitation of ground failure zones due to land subsidence using gravity data and finite element modeling in the Querétaro valley, México

Sedimentary basins of arid and semiarid zones are often subject to regimes of intense ground-water withdrawal as it is normally the only source of water for development of communities. An associated phenomenon is land subsidence, which can develop to ground failures, and consequently, damage to infrastructure. Aquifer deformation can be analyzed using a stress–strain or a flux–force approach depending on the aquifer material (compact or loose) and on whether the water withdrawal forms a predominant flow direction toward a cone of depression. Geometry of the aquifer system also plays an important role as uneven thickness induces differential compaction and hence, tensional and shear stresses on the ground mass. In this work we present a stress–strain approach to analyze subsidence for an unconfined aquifer of varying thickness; this is done in two steps, namely when the aquifer is in equilibrium, and when it is totally depleted. Using this scheme in a region where ground failure is evident, a portion of the aquifer system of the Querétaro valley is analyzed. The geometry of the hydrologic basement is first modeled using gravity measurements properly correlated with wells and field data. Then a stress analysis is implemented using the finite element method in order to identify probable zones of ground weakness, which are calibrated with known ground failures. The results indicate that both, tensional and shear stress are present, which induce ground failure in the form of surface faults.     

浅析乐都地倾斜观测资料

通过对乐都地倾斜EW向和NS向观测资料的分析，初步分析了其异常特征，认为乐都地倾斜在震前具有一定的异常反映。     

雷达差分干涉测量及其在地表沉降中的应用与展望

阐述了雷达差分干涉测量(D-InSAR)的基本原理,概括了国内外目前应用比较广泛的D-InSAR模型,针对长时间序列的城市地表沉降监测,应用较多的是基于相干点目标选择,相关的技术包括PSI、SBAS、CRT、CTA。通过多景数据的套合达到消除大气误差相位的目的。进一步总结了相关D-InSAR技术在地表沉降方面的应用进展。相关研究表明,D-InSAR技术能够应用于城市地表沉降监测,并且能够达到较高精度,逐步形成了完善的理论体系和技术处理流程。而且随着技术的发展,监测的时间尺度也在不断扩大、进一步拓展D-InSAR的试验区域。多种数据的结合和补充、方法的有效结合以及与传统的GPS、水准仪测量方法的结合是今后进一步关注的焦点和研究重点。     

Ground subsidence,Quaternary faults and vulnerability of utilities and transportation networks in Thessaly,Greece

Ground fissures and subsidence have caused extensive damage in structures and the utility networks (roads, railroad line, Larisa NATO airport, telecommunication network) in the plain of Thessaly, central Greece, in the last 20 years. The fact that these fissures are parallel to Quaternary faults controlling the structural evolution of the Thessaly basin, marked by intense recent seismic activity, led some scientists to regard them as manifestation of tectonic creep, even premonitory phenomena of major future seismic events. A careful study of the geometric characteristics and of the kinematics of these ground fissures, however, revealed that they only reflect shear failure of the ground due to compaction of loose sediments following significant decline of the groundwater level due to over-pumping; i.e. a geotechnical and not a tectonic process. Furthermore, theoretical considerations and modeling predict surface fissuring along zones of anomalous basement, normal-fault controlled topography. This explains the correlation between ground fissures and active Quaternary normal faults.     

Hydrogeological conditions and quality of ground waters in northern Banat,Pannonian basin

Geological relationships, hydrogeology and chemical composition of ground water in northern Banat were studied through the period 2000–2004 using the available background data from published and unpublished sources. Northern Banat is the extreme northeastern part of the Republic of Serbia and a geotectonic part of the vast Pannonian depression. The source of domestic and industrial water supply is only groundwater from artesian and subartesian aquifers of Lower Pleistocene (Q₁¹) and Upper Pleistocene (Pl₃²) sand deposits. The ground water, “peculiar” in chemical composition, is the only source of drinking water in the arid area. A notable variation in the chemical composition of artesian waters within the same geotectonic unit (Pannonian basin), abstracted for municipal water supplies of Kikinda, Novi Knezevac and Djala, has attracted attention of these authors. Our paper attempts to interpret the variation in the chemical composition of ground water and the cause of the variation by the interaction of ground water and rocks forming the aquifers on the case example of the water supply sources for the three mentioned towns. With respect to the depth and lithology of the aquifers, we interpret the varied chemical compositions of waters in the mentioned sources as a consequence of natural factors (geological environment), geological relationships and hydrogeological conditions.