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51.
本文对西安国贸大厦沉降监测技术方案进行了讨论,着重结合有关工程地质资料对沉降进行了几何分析和物理分析,探讨了沉降引发的原因及建筑物变形规律  相似文献   
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53.
Wang  Zhaohui  Lei  Mingdan  Ji  Shuanghui  Xie  Changliang  Chen  Jiazhuo  Li  Weiguo  Jiang  Tao 《中国海洋湖沼学报》2022,40(6):2322-2342
Journal of Oceanology and Limnology - Surface sediment samples were collected in three different functional sea areas in Qingdao coast, East China, including the inner Jiaozhou Bay, the Laoshan...  相似文献   
54.
5.12汶川特大地震发生后,灾区地面交通瘫痪,遥感技术为准确掌握灾情发挥了宏观快速的优势.灾区震后遥感影像来源丰富,通过分析从不同遥感平台和传感器获取到的灾区震后遥感影像的特点,探讨了多源遥感影像的处理方法,特别是针对非标准航空影像处理提出了解决思路.并归纳了基于多源数据进行震害信息提取,确定滑坡、泥石流等地质灾害体地理位置的几种技术及方法.  相似文献   
55.
The Dongfang1-1 gas field (DF1-1) in the Yinggehai Basin is currently the largest offshore self-developed gas field in China and is rich in oil and gas resources. The second member of the Pliocene Yinggehai Formation (YGHF) is the main gas-producing formation and is composed of various sedimentary types; however, a clear understanding of the sedimentary types and development patterns is lacking. Here, typical lithofacies, logging facies and seismic facies types and characteristics of the YGHF are identified based on high-precision 3D seismic data combined with drilling, logging, analysis and testing data. Based on 3D seismic interpretation and attribute analysis, the origin of high-amplitude reflections is clarified, and the main types and evolution characteristics of sedimentary facies are identified. Taking gas formation upper II (IIU) as an example, the plane distribution of the delta front and bottom current channel is determined; finally, a comprehensive sedimentary model of the YGHF second member is established. This second member is a shallowly buried “bright spot” gas reservoir with weak compaction. The velocity of sandstone is slightly lower than that of mudstone, and the reflection has medium amplitude when there is no gas. The velocity of sandstone decreases considerably after gas accumulation, resulting in an increase in the wave impedance difference and high-amplitude (bright spot) reflection between sandstone and mudstone; the range of high amplitudes is consistent with that of gas-bearing traps. The distribution of gas reservoirs is obviously controlled by dome-shaped diapir structural traps, and diapir faults are channels through which natural gas from underlying Miocene source rocks can enter traps. The study area is a delta front deposit developed on a shallow sea shelf. The lithologies of the reservoir are mainly composed of very fine sand and coarse silt, and a variety of sedimentary structural types reflect a shallow sea delta environment; upward thickening funnel type, strong toothed bell type and toothed funnel type logging facies are developed. In total, 4 stages of delta front sand bodies (corresponding to progradational reflection seismic facies) derived from the Red River and Blue River in Vietnam have developed in the second member of the YGHF; these sand bodies are dated to 1.5 Ma and correspond to four gas formations. During sedimentation, many bottom current channels (corresponding to channel fill seismic facies) formed, which interacted with the superposed progradational reflections. When the provenance supply was strong in the northwest, the area was dominated by a large set of delta front deposits. In the period of relative sea level rise, surface bottom currents parallel to the coastline were dominant, and undercutting erosion was obvious, forming multistage superimposed erosion troughs. Three large bottom current channels that developed in the late sedimentary period of gas formation IIU are the most typical.  相似文献   
56.
文章通过论述海洋环境监测的CalCOFI计划经验与海洋环境监测在经济与管理方面的重要意义,最终得出如下结论:(1)加强海洋环境监测能力建设,提高监测的质量与水平;(2)加强对海洋环境的动态跟踪与管理;(3)积极做好海洋环境监测信息的发布工作,完善海洋环境监测预警机制。  相似文献   
57.
利用第29次南极科考期间在普里兹湾海区释放的8个Argos漂流浮标所获的总计662 d的数据,对普里兹湾及其邻近海域的表层海流特征进行了分析,并和以前的研究结果进行对比,结果表明:普里兹湾西部和北部表层海流基本呈现向西的流动,说明此地区的表层海流以沿南极大陆的逆时针沿岸流为主。普里兹湾东部海流呈现先向南再向西或先向南再向北的流动,普里兹湾西北部海流呈现向南的流动。8个浮标平均流速在0.02—0.20 m·s~(-1)之间,最大流速为1.57 m·s~(-1),流速1.0 m·s~(-1)的大流速区主要集中在普里兹湾、克洛斯角外侧、达恩利角外侧海域,流速1.5 m·s~(-1)的大流速区只出现在普里兹湾、克洛斯角外侧两处海域。  相似文献   
58.
于丹丹  徐成华  骆祖江  顾问  周玲玲 《地质通报》2023,42(11):2006-2013
南京汤泉地区地下热水资源丰富,阐明其补给来源及成因模式,对于地下热水的科学开发意义重大。采用水化学及同位素地球化学分析方法对其进行了系统研究。结果表明,研究区地下热水与浅层冷水水化学组成差异明显,热储温度为63~75℃,循环深度为1.8~2.3 km。大气降水入渗是地下热水的补给来源,补给高程范围为321~539 m;循环周期为2046~6474 a;地下热水上涌过程中会混入比例为4%~26%的浅部岩溶冷水。经分析,该地热系统成因上属于中低温对流型,补给区主要为老山复背斜构造内的碳酸盐岩裸露区,依靠区域大地热流供热,热储层主要为上震旦统白云岩,盖层为寒武系、白垩系及第四系,地下热水经深循环沿NEE向与NW向断裂交会通道向上运移,并与浅部冷水发生混合,形成本区的地热异常。  相似文献   
59.
With a continuously increasing population and better food consumption levels, improving the efficiency of arable land use and increasing its productivity have become fundamental strategies to meet the growing food security needs in China. A spatial distribution map of medium- and low-yield cropland is necessary to implement plans for cropland improvement. In this study, we developed a new method to identify high-, medium-, and low-yield cropland from Moderate Resolution Imaging Spectroradiometer (MODIS) data at a spatial resolution of 500 m. The method could be used to reflect the regional heterogeneity of cropland productivity because the classification standard was based on the regionalization of cropping systems in China. The results showed that the proportion of high-, medium-, and low-yield cropland in China was 21%, 39%, and 40%, respectively. About 75% of the low-yield cropland was located in hilly and mountainous areas, and about 53% of the high-yield cropland was located in plain areas. The five provinces with the largest area of high-yield cropland were all located in the Huang-Huai-Hai region, and the area amounted to 42% of the national high-yield cropland area. Meanwhile, the proportion of high-yield cropland was lower than 15% in Heilongjiang, Sichuan, and Inner Mongolia, which had the largest area allocated to cropland in China. If all the medium-yield cropland could be improved to the productive level of high-yield cropland and the low-yield cropland could be improved to the level of medium-yield cropland, the total productivity of the land would increase 19% and 24%, respectively.  相似文献   
60.
杭州湾海域春、秋季鱼类种类组成和数量分布   总被引:8,自引:0,他引:8  
采用底层拖网法,用渔获率作为鱼类资源数量分布的指标,进行了杭州湾调查海域2012年5月(春季)、10月(秋季)2个季节的鱼类种类组成、区系特点、数量分布等研究。结果表明:(1)杭州湾海域春、秋两季共获得并鉴定出的鱼类有31种,隶属于9目15科,其中以石首鱼科和■虎鱼科的种类为最多,各有5种,分别占总种数的16.7%;鳀科鱼类次之,有4种,占总种数的13.3%,优势种有睛尾蝌蚪■虎鱼、龙头鱼、刀鲚、棘头梅童鱼;(2)根据鱼类适温性可将该海域的鱼类分为暖水性、暖温性和冷温性3种适温类型,以暖温性种类为主,暖水性种类次之,而冷温性种类极少,仅有1种;(3)根据其生态习性,可分为河口性、沿岸性和近海性3种生态类群;(4)渔获数量分布规律是春季在调查海域的内侧或者说中西部较高,而湾口较低,秋季则正好相反。  相似文献   
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