沁水盆地煤层气气源岩地球化学特征及气源潜力分析     

王万春陶明信  任军虎康晏 张小军 《煤田地质与勘探》2005,33(5):22-25

对比研究了山西沁水盆地李雅庄煤矿、寺河煤矿和附城七一煤矿煤岩的地球化学特征,讨论了煤岩的热演化程度、可溶有机质含量、生物标志化合物特征。在此基础上,分析了热成因煤层气与次生生物成因煤层气的气源潜力,对研究区煤层气勘探有实际意义。   相似文献   

渤海湾水环境系统多级灰关联评价   总被引：6，自引：1，他引：5  

王红莉  姜国强  陶建华 《海洋技术学报》2004,23(4):48-52,57

水环境评价指标体系的构建及水环境质量的综合评价分析是制定水环境保护对策的一个重要环节。文章在介绍了水环境指标因子选择方法的基础上,应用多级灰色关联评估理论及其模型对渤海湾近岸海域水环境质量状况进行了综合评价,并分析了近10a来渤海湾水环境质量变化趋势及导致近岸海域海水富营养化状况的可能原因。  相似文献   

油气储层自生高岭石发育特点及其对物性的影响   总被引：18，自引：0，他引：18  

曹剑  张义杰  胡文瑄  张越迁  唐勇  姚素平  陶国亮 《矿物学报》2005,25(4):367-373

以准噶尔盆地腹部侏罗系砂岩油气储层为例,在野外与岩芯观测的基础之上,通过显微和扫描电镜鉴定,并结合粉末X射线衍射和电子探针成分分析,发现有大量自生高岭石发育于储层长石溶蚀后的孔隙中,可以很少或大量原地沉淀,使得储层物性变好或变差。这些自生高岭石是含油气酸性流体与砂岩中碱性长石发生水岩反应的产物,在油源断裂附近的中粒一中粗粒砂岩层中,含油气流体活动强度大、渗流速度较高,高岭石易于迁移至别处．储层物性得到改善．反之高岭石则倾向于原地沉淀．储层物性变差。  相似文献   

基于系统保护规划理论的广西海域优先保护格局分析     

李潇  刘昭阳  王晓莉  吴玥  左国成  陶以军 《海洋通报》2021,40(2)

基于广西海域红树林、珊瑚礁、海草床等生境数据,在系统保护规划理论框架下,利用Marxan软件构建了广西海域优先保护格局以识别保护空缺。结果表明:广西海域优先保护区集中在三娘湾、合浦、涠洲岛海域,部分区域游离在现有保护体系外。与广西海洋生态红线对比,保护空缺主要分布在沿岸滩涂分布区、红树林分布区和涠洲岛珊瑚礁分布区。本研究首次基于系统保护规划理论,研究了广西海域优先保护格局,为广西海域的保护规划管理提供了科学性建议。  相似文献   

关中盆地地下水动态监测网络设计与应用     

陶虹  丁佳  刘文波 《中国地质灾害与防治学报》2012,23(2):122-126

本文在关中盆地现有监测网的基础上,基于GIS技术,采用建设监测剖面与编制地下水动态类型图相结合的方法,对关中盆地地下水动态监测网进行了优化调整,形成4横5纵共9条监测剖面、239个监测点的地下水动态监测网,其中潜水监测井120个,承压水监测井119个;利用原有监测井165个,新增监测井74个。新建监测网能够较全面地控制关中盆地区域地下水动态变化,在2011年＂严重缺水地区地下水监测项目＂中,以动态监测数据为依据,确定了主要干旱区位置,为政府应急抗旱找水打井提供了技术支撑。  相似文献   

城市湖泊水环境修复组合工艺效果研究——以深圳市荔枝湖治理工程为例   总被引：3，自引：0，他引：3  

毛献忠  桂安  陶益  张锡辉 《湖泊科学》2008,20(4):456-462

以深圳市荔枝湖为例,通过历时9个月的水质连续监测,研究该湖水污染综合治理工程实施后不同治理工艺的处理效果.研究表明,自动过滤工艺TP和COD平均去除率分别为33.6%和16.2%;生物砾石床工艺TP和COD平均去除率分别为39.O%和21.3%;人工湿地工艺TP和COD平均去除率分别为80.2%和56.1%.通过荔枝湖四湖总磷串联模型,计算在设计初始条件下,采用组合治理工艺时湖水恢复为地表Ⅳ类水所需要的时间.计算表明工艺每天运行24h,需要2.5d可将各湖TP浓度降至O.1mg/L以下,TP总去除量为7.27kg,去除率为46.%.  相似文献   

THE 3-D VELOCITY STRUCTURE OF CRUST AND UPPERMOST MANTLE AND ITS TECTONIC IMPLICATIONS IN FUJIAN PROVINCE          下载免费PDF全文

LI Xi-bing  XIONG Zhen  FAN Xiao-ping  TAO Xiao-san  PENG Xiao-bo 《地震地质》2019,41(5):1206-1222

It is important to detect the fine velocity structures of the crust and uppermost mantle to understand the regional tectonic evolution, earthquake generation processes, and to conduct earthquake risk assessment. The inversion of uppermost mantle velocity and Moho depth are strongly influenced by crustal velocity heterogeneity. In this study, we collected first arrivals of Pg and Pn and secondary arrivals of Pg wave from the seismograms recorded at Fujian provincial seismic network stations. New 3-D P-wave velocities were inverted by multi-phase joint inversion method in Fujian Province. Our results show that the fault zones in Fujian Province have various velocity patterns. The shallow crust is characterized by high velocity that represents mountains, while the mid-lower crust shows low velocities. The anomalous velocities are correlated closely with tectonic faults in Fujian Province. Velocity anomalies mainly show NE-trending distribution, especially in the mid-lower crust and uppermost mantle, which is consistent with the NE-trending of the regional main fault zones. Meanwhile, a part of velocity patterns show NW trending, which is related to the secondary NW-oriented faults. Such velocity distribution also shows a geological structural pattern of "zoning in east-west direction and blocking in north-south direction" in Fujian area. In the crust, a low velocity zone is found along Zhenghe-Dapu fault zone as mentioned by previous study, however our result shows the low velocity exists at depth of 20~30km in mid-lower crust. Compared with previous study, this low velocity zone is larger and deeper both in range and depth. The crustal thickness of 28~35km from our joint inversion is similar to the results from the receiver functions of previous studies. The thinnest crust(28km)is observed at offshore in the north of Quanzhou; while the thickest crust(35km)is located west of Zhangzhou near the Zhenghe-Dapu fault zone. Generally, thinner crustal thickness is found in offshore of Fujian Province, and thicker crustal thickness is in the mainland. However, we also found that crustal thickness becomes thinner along the east side of Yongan-Jinjiang Fault. The values of Pn velocities in the region vary from 7.71 to 8.26km/s. The velocity distribution of the uppermost mantle presents a large inhomogeneity, which is correlated with the distribution of the fault zone. High Pn velocity anomalies are found mainly along the west side of the Zhenghe-Dapu fault zone(F₂), and the east side of the Shaowu-Heyuan fault zone(F₁), which is strip-shaped throughout the central part of Fujian. Low Pn velocity anomalies are observed along the coast and Taiwan Straits, including the Changle-Zhaoan fault zone, the coastal fault zone, and the Fuzhou Basin. We also found a low Pn velocity anomaly zone, which extends to the coast, in the Shaowu-Heyuan fault zone at the junction of the Fujian, Guangdong and Jiangxi Provinces. In the west of Taiwan Straits, both high and low Pn velocity anomalies are observed. Our results show that the historical strong earthquakes(larger than magnitude 6.0) are mainly distributed between positive and negative anomaly zones at different depth profiles of the crust, and similar anomalies distribution also exists at the uppermost mantle, suggesting that the occurrence of strong earthquakes in the region is not only related to the anomalous crustal velocity structure, but also affected by the velocity anomaly structure from the uppermost mantle.  相似文献   

考虑双向碰撞效应的连续斜交桥地震响应研究          下载免费PDF全文

陶源  徐略勤  姚凯  李静文 《地震工程学报》2019,41(2):360-369

为研究双向碰撞效应对连续斜交桥地震响应的影响,采用Kelvin-Voigt模型模拟桥台伸缩缝处的纵向碰撞现象,采用简化滞回模型模拟挡块与主梁的横向碰撞过程,针对某三跨连续斜交桥进行参数对比研究。研究表明,双向碰撞对主梁横向位移的影响远比纵向位移大,其中桥台间隙对主梁平面转角的影响最大,且平面转角随桥台间隙的增大而减小;横向碰撞对墩柱曲率变形的影响远比纵向碰撞大,其中挡块强度的影响特别大,当挡块强度由0%增至50%时,墩柱纵、横向曲率均值分别增大13.43倍、7.21倍。随着斜交角的增大,梁端纵向位移不断增大,横向位移和平面转角则先增后减;墩底纵向曲率不断增大,横向曲率经历先增后减\,再增的过程;纵向碰撞效应先减弱后增强,而横向碰撞效应则先增强后减弱。由于横向碰撞对墩柱的影响远大于纵向碰撞,因此在斜交角为15°～45°时,宜设法降低横向碰撞效应。  相似文献   

粤东五华河流域的化学风化与CO₂吸收   总被引：1，自引：1，他引：0  

张超  高全洲  陶贞  陈晓宏  解晨骥  林培松  张胜华  李姗迟  李元 《湖泊科学》2013,25(2):250-258

基于对粤东五华河干流和支流水体的物理、化学组成测试数据,应用质量平衡法和相关分析法探讨湿热山地丘陵地区岩石化学风化过程对大气CO₂的吸收.结果表明:五华河水体的总溶解性固体含量(77.11 mg/L)接近于世界河流的平均值(65 mg/L);离子组成以Ca²⁺、Na⁺和HCO₃^-为主,可溶性Si次之.五华河流域化学径流组成主要源自硅酸盐矿物化学风化过程的贡献,碳酸盐矿物的贡献较少;大气和土壤CO₂是流域内岩石化学风化的主要侵蚀介质.与同一气候带其他河流相比较,五华河流域岩石化学风化过程对大气CO₂的吸收通量(2.14×105mol/(km²·a))较低,这主要是由于流域内缺乏碳酸盐岩所导致.  相似文献   

5000米智能地质钻探技术与装备研发          下载免费PDF全文

张金昌  刘凡柏  黄洪波  梁健  王瑜  吴敏  陶士先 《探矿工程》2020,47(4):1-8

深部钻探技术是解决深地探测科技问题的必要手段之一。本文主要介绍了“十三五”国家重点研发计划 “5000米智能地质钻探技术装备研发及应用示范” 项目方案,项目从构建大深度绳索取心钻孔口径系列、钻具级配、装备配置等入手,开展了钻进智能控制、钻机关键技术与装备、高性能绳索取心钻杆、小口径高效系列钻具、环保冲洗液体系与废浆处理技术、钻探技术装备集成与示范等研究,拟突破智能控制、自动化、轻量化与模块化等关键技术,形成以绳索取心工艺为主体的特深孔地质岩心钻探装备与技术体系,为我国深部探测计划提供技术与装备支撑。  相似文献