A GIS-based approach for detecting pollution sources and bioavailability of metals in coastal and marine sediments of Chabahar Bay,SE Iran     

《Chemie der Erde / Geochemistry》2015,75(2):185-195

Chabahar Bay in SE of Iran is a shallow semi-enclosed environment affected by anthropogenic activities. In this paper, 19 sediment samples were collected and concentration of selected metals (Cu, Pb, Zn, Cd, Ni, Cr, Co, V and Fe) was determined using ICP-MS analytical method. Sediment samples from five stations were also selected for sequential extraction analysis and concentration of metals in each fraction was determined using ICP-OES. In order to investigate the environmental quality of Chabahar Bay, geographic information system (GIS) along with geochemical data, environmental indices and statistical analyses were used. Calculated contamination degree (C_d) revealed that most contaminated stations (Ch3, S1 and S3) are located SE of Chabahar Bay and contamination decreases in a NW direction. The S9 station, west of the bay, is also contaminated. High organic matter (OM) content in the sediments is most likely the result of fuel and sewage discharge from fishing vessels along with discharge of fishing leftovers. Significant correlation coefficient among OM, Fe, Cu, Pb, Zn and Cd seemingly reflects the importance of the role that OM and Fe oxy-hydroxides play in the metals mobility. The results of hierarchical cluster analysis (HCA), computed correlation coefficient and sequential extraction analysis suggest that Cu, Pb, Zn and Cd probably come from antifouling and sea vessel paints, while Ni, Cr, Co, V and Fe are most likely contributed by ophiolitic formations located north of the bay and/or deep sea sediments. Average individual contamination factors (ICFs) indicated that the highest health hazard from the bay is posed by Cu, Pb and Zn.  相似文献   

OBJECTIVE CLASSIFICATION OF THE TRACKS OF TROPICAL STORMS IN THE BAY OF BENGAL   总被引：1，自引：0，他引：1  

林志强  边巴扎西  文胜军  周振波 《热带气象学报(英文版)》2015,21(3):222-231

An objective analysis of tropical cyclone tracks is performed, with which the tracks of 131 tropical storms (TSs) in 1972-2011 are separated into three types that move west-, north- and northwestward, denoted as Types A, B and C, respectively. Type A (21 TSs and 16% of total) has the origin in the southwestern Bay of Bengal, with the TS in a unimodal distribution as its seasonal feature, occurring mainly in autumn; 18 of the 21 TSs (taking up 90%) land mostly on the western Bay coast (west of 85°E); 5% of Type-A TSs attains the wind speed of >42.7 to 48.9 m/s. Type A has little or no effect on Tibet. Type B (74 TSs, 56.6% of the total) has its preferable origin in the central Bay of Bengal, with the TS in a bimodal distribution as its seasonal pattern. This type denotes the travel in the north in spring, with the landfall of 67 of the 74 TSs (accounting for 91%) mainly on the middle coast of the Bay (85° to 95°E), and 19% of the TSs reaching the wind velocity of >42.7 to 48.9 m/s, which exert great effect on Tibet and it is this TS track that gives strong precipitation on its way through this region. Type C (36 TSs, 27.5% of the total) has its main origin in the southern part of the bay, and these TSs are formed largely in autumn, moving in the northwest direction, and 23 of the 36 TSs (64%) land mostly on the western Bay coast, lasting for a longer time, with almost no impact upon Tibet.  相似文献   

焦家断裂带南部覆盖区控矿构造带的研究及成矿前景分析     

贺春艳  郭国强  刘聪伟  曹春国  陈大磊  刘红旗 《山东国土资源》2015,31(7)

胶东西北部龙口莱州断裂带南段的朱宋朱桥段,俗称焦家断裂带,是胶东西北部三大控矿构造之一,相继勘查评价了焦家、新城、河西、河东、东季、马塘、望儿山、寺庄等一系列特大型、大型以及中小型金矿床,资源潜力巨大。由于焦家断裂带南段（寺庄以南）被第四系覆盖而去向不明,因此目前对焦家断裂带南延的位置争议较大。根据近年来在该区开展的一系列综合物探研究工作,初步建立了焦家主干断裂带南部覆盖区的断裂构造格架,认为其中F8（徐村院沟北王）断裂为焦家断裂的南延段,并对南部覆盖区的成矿前景进行了分析探讨。  相似文献   

冀中南平原土壤氟地球化学特征及其控制因素   总被引：1，自引：0，他引：1  

谷海峰  栾文楼  杜俊  陈志贤  蔡奎  李超 《物探与化探》2011,35(3):388-392

详细研究了冀中南平原土壤氟的地球化学特征,并探讨其控制因素。冀中南平原整体氟含量较高,且分布不均匀,具有明显分带性,分别出现4个高氟带和4个低氟带。氟在该区的分布明显受自然地理、地质因素和人为因素控制,且以自然地理、地质因素为主。在自然地理、地质因素中地貌起主导作用,而在人为因素中化肥为主导因素。  相似文献   

Geochemical Characteristics and Geological Significance of Early Permian Baya’ertuhushuo Gabbro in South Great Xing’an Range   总被引：1，自引：0，他引：1  

LIU Jianfeng  CHI Xiaoguo  ZHAO Zhi  ZHANG Xingzhou  MA Zhihong  WANG Tiefu  HU Zhaochu 《《地质学报》英文版》2011,85(1):116-129

Field geological investigation and geochemical analysis are carried out on Baya’ertuhushuo Gabbro in South Great Xing’an Range. Field investigation reveals that the gabbro is a magmatic intrusion rather than a component of an ophiolite suite as previously thought. Zircon laser ablation inductively coupled plasma mass spectroscopy (LA-ICP-MS) U-Pb dating indicates the gabbro was formed in 274–275?Ma, just as the widespread volcanic rocks of Dashizhai Formation (P1d), monzogranites and miarolitic alkali-feldspar granites in the study area. The gabbro has SiO2 content between 47.23 wt% and 50.17 wt%, high MgO and FeOT contents of 6.95–11.29 wt% and 7.32–12.24wt%, respectively, and it belongs to low-K tholeiitic series in the SiO2-K2O diagram. The Chondrite-normalized rare earth element (REE) patterns and primitive mantle-normalized spider diagrams of the gabbro are similar to those of Normal Mid-Ocean Ridge Basalt (N-MORB) except for the enrichment of large ion lithophile elements (LILE), such as Rb, Ba and K. In trace element tectonic discriminative diagrams, the samples are mainly plotted in the N-MORB field, and Zircon in?situ Lu-Hf isotopic analysis also indicates the gabbro originated from depleted mantle. Through synthetic studies of the geochemical characteristics and petrogenesis of Baya’ertuhushuo gabbro, volcanic rocks of Dashizhai Formation and granitoids in the area, it is suggested that the early Permian magmatism in the Xilinhot-Xiwuqi area formed in the tectonic setting of asthenosphere upwelling, which was caused by breaking-off of the subducted Paleo-Asian Ocean slab.  相似文献   

Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression     

倪金龙  郭颖  王智敏  刘俊来  林玉祥  李月 《中国地质大学学报(英文版)》2011,(3)

The Huimin (惠民) depression is a third-level tectonic element of the Bohai (渤海) Bay basin in eastern China. The central uplift belt is the most important oil and gas accumulation zone in the depression, but the lack of adequate geological studies in the area has greatly hindered exploration and development. In this article, using seismic data, fracture mechanics, and a combination of data on fault growth indices and fault throws, we present an analysis of tectonic activity in the central uplift belt and adja...  相似文献   

库区陡峻土质岸坡路基塌岸预测     

王哲 《中国地质灾害与防治学报》2011,22(2):39-44

对山区顺直陡峻岸坡路基塌岸的预测,与普通图解法比较,采用考虑土体内聚力的图解法可有效避免解算难以收敛的问题,更为符合塌岸的真实形态。通过预测实例的分析发现：天然休止角的提高可大幅减小塌岸范围;水下磨蚀角的提高则可有效减小塌岸深度;合理调节运行水位变幅,对控制塌岸范围和深度较为理想;而通过小范围抬高公路线位来控制塌岸的效果并不明显。对塌岸影响因素的深入分析,为塌岸段路基的治理提供了合理的思路。  相似文献   

地面沉降对渤海湾风暴潮灾害防治的影响研究     

王威  周俊  易长荣 《城市地质》2011,6(4):31-35

渤海湾沿海地区地面沉降严重、风暴潮灾害频发。本文以天津作为典型区域,对风暴潮潮位测定、风暴潮灾害和防风暴潮预案措施等方面开展研究,认为地面沉降对上述3方面均有的不同程度的影响,在风暴潮灾害防治中必须考虑地面沉降问题。  相似文献   

莱州市土地管理办公自动化系统建设     

肖刚  王金贵  贾华峰  张永玉 《山东地质》2011,(2):38-41

莱州市国土资源局土地管理办公自动化系统采用工作流技术,基于浏览器/服务器（B/S）三层体系结构设计,实现了土地管理办公自动化和国土信息的对外发布。系统采用可视化流程设计,并预留GIS接口,方便今后系统的扩展和升级。系统建成后,大大提高了莱州市国土资源局各业务部门的业务处理速度和协同工作效率。  相似文献   

渤海湾全新世贝壳堤与牡蛎礁:古气候与海面变化   总被引：6，自引：3，他引：3  

王宏  陈永胜  田立柱  李建芬  裴艳东  王福  商志文  范昌福  姜兴钰  苏盛伟  王海峰 《地质通报》2011,30(9):1405-1411

讨论了早全新世晚期以来渤海湾西岸贝壳堤平原成堤、西北岸牡蛎礁平原(及毗邻浅海区)建礁过程的同时性特征和气候变化与这一特征之间的关系,以及堤、礁记录的相对海面变化。堤、礁大致同时发育,可分为6期,依次分别被寒冷事件5、4、3、2和1分隔。堤底板前、后缘高差大致对应3m的大潮差、礁顶板大致对应海平面。据二者分别重建了南部贝壳堤平原、北部牡蛎礁平原的相对海面变化:南部自7ka cal BP以来基本与现代海平面等高,小的波动在±1m之间,压实固结作用抵消了中全新世的相对高海面;北部中全新世的相对海平面位置因新构造和固结压实双重下沉作用的影响,已位于现代海平面2~3m以下。  相似文献