里耶地下秦代古城护城河空间位置低损探查   总被引：2，自引：1，他引：1  

何满潮  韩雪  周旭荣  刘成禹  还祥生 《工程地质学报》2006,14(5):661-664

文物遗址勘察在工程地质勘察领域具有特殊性。根据前期对遗址的部分发掘,考古专家推断里耶秦代古城墙遗址周围是被埋入地下的古护城河,且河底可能埋藏有珍贵文物。古护城河空间位置的精确测定对该遗址保护、继续发掘和开发利用具有重要意义。古护城河被地表沉积物掩埋、部分古河段与近代池塘重叠、常规勘探可能破坏珍贵文物、电磁干扰较严重等给古护城河空间精确定位带来了很大困难。本文针对这些难题采用切合实际的高密度电法和改进的轻便取芯触探相结合的综合探查方法实现了精确定位,实践证明该方法在文物遗址勘察方面具有许多传统勘探方法无法比拟的优点。  相似文献   

滇西大平掌铜多金属矿床流体包裹体研究   总被引：4，自引：0，他引：4  

李峰  庄凤良 《岩石学报》2000,16(4):581-586

大平掌铜多金属矿床由块状硫休物矿体（上部）和细脉浸染状矿体（下部）组成。前者的包裹体型简单,均一温度、盐度和捕获压力较低,后者以包体类型复杂、均一温度及捕获压力较高为特征,其差异与成矿流体演化有关,研究表明,成矿液体以富Ｋ＾＋、Ｎａ＾＋、Ｃｌ＾＋、ＳＯ＾２－４、Ｆ＾－、ＣＯ２和ＣＯ为主,属中低温、中盐度的Ｋ质溶液,主要来源于海水,并有深部岩浆水的混合。  相似文献   

强震作用下地铁车站结构损伤破坏的高效分析方法          下载免费PDF全文

范益  陈力  还毅  郑康 《地震工程学报》2019,41(3):672-678

地下结构的关键构件(如柱子等)在地震作用下可能发生破坏,进而影响结构体系的整体稳定性。在借鉴传统反应位移法的基础上,提出了一种新的位移时程反应分析方法,采用该方法对日本神户大开地铁车站进行地震响应分析。结果表明:位移时程反应分析方法能够考虑土-结构相互作用、材料非线性、几何非线性、水平地震与竖向地震的耦合作用及地震动传播的时空效应,适用于地下结构地震反应分析,利用该方法得出的地铁车站结构变形及损伤破坏与实际震害观察具有较好的一致性,并指出大开地铁车站结构的整体垮塌是由于柱子剪坏和高轴压联合作用所致。  相似文献   

基于Wi-Fi信号的地震废墟被困人员侦查系统     

李海林  郭勇  白芬玉  冯贝  陈志远 《震灾防御技术》2017,12(4):985-996

针对震后大面积废墟下被困人员快速准确检测与定位的需求,本文提出了基于Wi-Fi信号的地震灾害人员侦查技术。以嵌入式技术为基础,涉及FSK通信、Wi-Fi定位、Wi-Fi定位算法等方面的研究,提出Wi-Fi热点中继设备和显控中心平台切实可行的设计解决方案,研制出能够实现震后大面积废墟下被困人员快速定位的设备,并提出设备布设方案。为我国地震救援提供一种有效的技术手段。  相似文献   

High Individual Variability in Beak Stable Isotopes of Jumbo Squid off Peruvian Exclusive Economic Zone(EEZ) Waters in the Analysis of Migratory and Foraging Ecology     

LIU Bilin  JIN Yue  CHEN Xinjun  LI Jianhua  QIAN Weiguo  LIU Na  HUAN Mengyao 《中国海洋大学学报(英文版)》2019,(1):232-238

Stable isotopes(δ¹³C and δ¹⁵N) have been widely used to track cephalopod habitat, migration and trophic structure. In this study, we analyzed the δ¹³C and δ¹⁵N values in 245 Dosidicus gigas beaks collected during 2009–2010 and in 2013 off Peruvian Exclusive Economic Zone(EEZ) waters. High individual variation in beak stable isotopes was shown with values ranging from-19.4‰ to-15.8‰ for δ¹³C and from 5.0‰ to 15.1‰ for δ¹⁵N. A generalized additive model(GAM) showed that latitude, mantle length and distance to shelf break significantly described the isotope variation with deviance ranging from 16.6% in δ¹³C to 36.3% in δ¹⁵N. Large variability in beak δ¹³C values for a given size and sampling station indicated that D. gigas off the Peruvian EEZ waters migrate in different ways when they occupy a large range of habitats for their ontogeny. Low baseline δ¹⁵N values suggested that spatial changes in diet trophic level may be the main determinative factor in beak δ¹⁵N variation. We conclude that high variability in beak δ¹⁵N values for a given set of explanatory variables indicated that D. gigas is an opportunistic predator with highly diverse dietary habitats. This study further develops our knowledge of the life history of D. gigas in such a highly dynamic region.  相似文献   

近断层地震作用下多层RC框架火灾后抗震性能分析     

钱胜力  陈鑫  孙勇  毛小勇  刘涛  还毅 《地震工程与工程振动》2021,41(1):219-227

为研究近断层地震动特性对火灾后多层RC框架抗震性能的影响,以火灾后某多层RC框架结构为研究对象,结合火灾后现场材料的检测与鉴定报告,开展了结构火灾前后在近场有脉冲和无脉冲地震作用下的结构动力弹塑性时程分析,对比分析了近场有脉冲和无脉冲地震动特性对火灾前后RC框架结构整体的抗震性能的影响.研究结果表明:火灾后,整体结构地...  相似文献   

极低频海洋噪声与风的相关性研究          下载免费PDF全文

黄浩南  杨燕明  阮海林  翁晋宝 《应用海洋学学报》2023,42(2):255-263

风通过影响海洋表面从而产生200 Hz以上的深海环境噪声,但有研究指出,通过风生表面波之间的非线性相互作用产生的驻波,能够与海床共振构成海底微震,从而产生10 Hz以下的噪声。针对这一新型风生噪声机制,本研究对威克岛海域10 Hz以下的极低频噪声进行了分析。比较了不同频率下海洋环境噪声功率谱级与风速的相关性,并讨论了风速和风向对设立在威克岛南北部二组水听器三联体信号的影响,结果表明2 Hz处的海洋环境噪声级与风速相关性最好,而风速和风向变化越剧烈海洋环境极低频噪声与风速风向的相关性越好。  相似文献   

上海外高桥港区停泊船聚类分析与异常检测     

郑海林  胡勤友  杨春  陈金海  梅强 《地球信息科学学报》2018,20(5):640-646

停泊船空间分布规律挖掘,在海事监管、港口管理和航运公司船队管理方面有着重要意义。现有研究主要针对船舶停泊点进行空间聚类以识别码头和锚地,缺乏对码头、锚地内船舶停泊特征分析,及码头和锚地外的异常停船的检测。因此,利用海量船舶自动识别系统（AIS）数据探索船舶停泊规律显得很有必要,且具备可行性。根据海况设定停泊速度阈值和停泊位置变化量阈值,建立停船判定模型。按港区、船型筛选,获取2016年1至11月外高桥港区集装箱船停泊记录。根据类中心点密度和聚类数量,设定邻域半径（ε）和邻域密度（MinPts）,采用密度聚类（DBSCAN）算法对船舶停泊点进行密度聚类,并将聚类结果与外高桥港区码头、锚地分布图进行比较,生成可疑停船列表。对比船舶历史轨迹,明确可疑停船列表中船舶真实停泊记录,筛选出异常停船。研究发现,2016年1至11月外高桥港区船舶异常停泊点位于圆圆沙锚地至吴淞口锚地间的南港水道和江亚南沙锚地附近的南港水道航段。船舶停泊前、后位置变化幅度小,而速度变化幅度大,推测船舶突发故障是其异常停泊的原因。海事主管部门（MSA）可根据船舶水上移动通信业务识别码（MMSI）快速锁定航运公司,加强岸上船舶安全管理。船舶停泊位置和时间能够记录船舶发生故障地点及其持续时间,为船队管理提供重要依据。  相似文献   

Influence of canopy and topographic position on soil moisture response to rainfall in a hilly catchment of Three Gorges Reservoir Area,China   总被引：2，自引：0，他引：2  

Liu  Muxing  Wang  Qiuyue  Guo  Li  Yi  Jun  Lin  Henry  Zhu  Qing  Fan  Bihang  Zhang  Hailin 《地理学报(英文版)》2020,30(6):949-968

Rainfall provides essential water resource for vegetation growth and acts as driving force for hydrologic process, bedrock weathering and nutrient cycle in the steep hilly catchment. But the effects of rainfall features, vegetation types, topography, and also their interactions on soil water movement and soil moisture dynamics are inadequately quantified. During the coupled wet and dry periods of the year 2018 to 2019, time-series soil moisture was monitored with 5-min interval resolution in a hilly catchment of the Three Gorges Reservoir Area in China. Three hillslopes covered with evergreen forest(EG), secondary deciduous forest mixed with shrubs(SDFS) and deforested pasture(DP) were selected, and two monitoring sites with five detected depths were established at upslope and downslope position, respectively. Several parameters expressing soil moisture response to rainfall event were evaluated, including wetting depth, cumulative rainfall amount and lag time before initial response, maximum increase of soil water storage, and transform ratio of rainwater to soil water. The results indicated that rainfall amount is the dominant rainfall variable controlling soil moisture response to rainfall event. No soil moisture response occurred when rainfall amounts was 8 mm, and all the deepest monitoring sensors detected soil moisture increase when total rainfall amounts was 30 mm. In the wet period, the cumulative rainfall amount to trigger surface soil moisture response in EG-up site was significantly higher than in other five sites. However, no significant difference in cumulative rainfall amount to trigger soil moisture response was observed among all study sites in dry period. Vegetation canopy interception reduced the transform ratio of rainwater to soil water, with a higher reduction in vegetation growth period than in other period. Also, interception of vegetation canopy resulted in a largeraccumulated rainfall amount and a longer lag time for initiating soil moisture response to rainfall. Generally, average cumulative rainfall amount for initiating soil moisture response during dry period of all sites(3.5–5.6 mm) were less than during wet period(5.7–19.7 mm). Forests captured more infiltration water compared with deforested pasture, showing the larger increments of both soil water storage for the whole soil profile and volumetric soil water content at 10 cm depth on two forest slopes. Topography dominated soil subsurface flow, proven by the evidences that less rainfall amount and less time was needed to trigger soil moisture response and also larger accumulated soil water storage increment in downslope site than in corresponding upslope site during heavy rainfall events.  相似文献   

深圳东部近岸海域溶解氧的时空分布特征     

庄晓珊  桓清柳  彭莹  王节亮  庞仁松  周凯 《热带海洋学报》2018,37(5):98-105

根据2012—2016年的9个浮标自动监测数据, 分析了深圳东部近岸海域溶解氧浓度的时空分布特征及其与主要水质参数的相关关系。结果表明, 大亚湾海域溶解氧浓度含量在2.15~14.86mg·L^-1之间, 平均值为7.31mg·L^-1, 大鹏湾海域整体表层溶解氧浓度范围为1.43~15.61mg·L^-1, 平均值为7.13mg·L^-1; 在时间分布上, 深圳东部海域溶解氧含量呈现白天高于夜间, 春、夏、秋季低, 冬季高的趋势; 在空间分布上, 深圳东部海域溶解氧含量呈现出夏秋季大亚湾高于大鹏湾, 春冬季大亚湾和大鹏湾相差不大的特点。Pearson相关性分析表明, 该海区溶解氧含量与温度、盐度、浊度及叶绿素a存在显著的线性相关性, 且相关关系呈现出随季节变化的差异性。  相似文献