香草坪花岗岩体年代学和地球化学特征   总被引：2，自引：0，他引：2  

李妩巍  王敢  陈卫锋  赵葵东 《铀矿地质》2010,26(4):215-221,227

香草坪岩体主要岩性为中粗粒斑状黑云母花岗岩,SHRIMP锆石U-Pb法年龄为211±2Ma,属于印支期岩浆作用产物。岩石地球化学特征研究表明,其ACNK,微量元素模式图曲线形态总体向右倾,以及轻稀土富集、Eu明显亏损的稀土配分模式曲线特征,与华南S型花岗岩的地球化学特征相似。该岩体高(87Sr/86Sr)i和低εNd(t)的特点,表明其可能是前寒武系中等成熟度的基底岩石经部分熔融形成的。该区基底岩石较高的铀含量,可为香草坪岩体提供充足的铀元素,形成铀元素的初始富集。  相似文献   

利用验潮站数据进行三种潮汐模型的精度分析     

胡志博  郭金运  宗干  张凯华 《海洋测绘》2014,(3):13-16

采用全球分布的565个验潮站水位资料对NAO.99b,CSR4.0和TPXO7.2三种潮汐模型进行精度评估。结果表明:在全球海洋范围内,NAO.99b模型精度最高;在黄海海域,TPXO7.2模型的精度最高;在东海和南海海域,则是NAO.99b模型最优;在深海海域,三种模型精度差异不大;在浅海海域,采用同化方法的潮汐模型比采用经验方法的潮汐模型更有优势。  相似文献   

Distribution and sources of heavy metals in the sediment of Xiangshan Bay   总被引：2，自引：0，他引：2  

SUN Weiping  YU Jianjun  XU Xiaoqun  ZHANG Weiyan  LIU Ruijuan  PAN Jianming 《海洋学报(英文版)》2014,33(4):101-107

Heavy metals in the surface sediments and sediment core from the Xiangshan Bay, a mariculture base on the coast of the East China Sea, were determined by inductively coupled plasma mass spectrometry(ICP–MS) in order to evaluate their levels and sources. The results showed that the levels of Cu, Pb, Zn, and Cr in the sediments of the bay have been generally influenced by anthropogenic inputs since the founding of the People's Republic of China. In particular, Cu and Zn were polluted to some extent, as evidenced by high enrichment factors. Organic matter, grain size, wastewater discharge, and low energy hydrodynamic environment played dominant roles in the heavy metal enrichment in the sediments. The ratio of terrigenous source to marine biogenic deposit of trace metals in the sediments was calculated, revealing that terrigenous inputs were the main source of Cu, Pb, and Zn, while biological pellets contributed much more to the enrichment of Cr and Cd. Considering the influence of biological sources on the enrichment of Cd and Cr, and the fact that the sediment has been polluted by Cu and Zn, the development of mariculture and discharge of wastewater into the Bay should be restricted.  相似文献   

东亚季风区近地面大气气溶胶中OCPs和PCBs纬度分布：以7Be为参照系     

杨永亮  耿存珍  李勇  张干  史双昕  朱晓华  焦杏春  谭科艳  于寒青 《地球化学》2014,(1):20-31

连续一年在北京、青岛、广州以每周3d的时间尺度同步采集近地面大气中气溶胶中7Be的测定数据以及在春、秋季节变换时期我国5个不同纬度城市大气气溶胶中7Be和典型持久性有机污染物（有机氯农药和多氯联苯1的同步观测数据,并对文献上发表的我国其他城市近地面大气中气溶胶中’Be年平均值数据进行了分析。通过对以上数据资料的总结和分析,观察到在东亚季风区近地表大气气溶胶中7Be浓度的年平均值呈现正态分布模式,并且在中纬度北纬40°N附近达到极大值。大气气溶胶中7Be在春、秋季节变换时期我国不同纬度城市的瞬时纬度分布仍呈现正态分布模式,但以30°N为最大值。在秋季大气颗粒相中HCHs和PCBs浓度最大值出现在30°N。气相中PCB-28所占百分比随纬度增高而增大,而颗粒相中PCB-28的纬度变化不大。蒸汽压较低的PCB-180在气相中的浓度基本上不随纬度变化,而颗粒相中PCB-180则基本上集中在纬度36。N左右,表明在东亚季风区大气中挥发性较低的POPs化合物具有某种纬度聚焦作用。以宇宙射线成因核素7Be作为大气环流的参照系,可以得出东亚季风区大气环流可影响持久性有机污染物纬度分布的结论。  相似文献   

中国旅游业碳减排潜力的空间关联网络结构及其影响因素     

王凯  余芳芳  胡奕  甘畅 《地理科学》2022,42(6):1034-1043

基于2000—2018年中国省际面板数据,利用“自下而上”法和Super-SBM模型测度30个省（区、市）的旅游业碳减排潜力,借助修正的引力模型和社会网络分析方法探究其空间关联网络特征及影响因素。结果表明：①中国旅游业碳减排潜力的空间关联日趋紧密,网络密度和网络关联数呈增长态势,网络效率和网络等级度呈下降态势;②东部区域在空间关联网络中居于核心位置,对降低旅游业碳减排潜力所需要素的掌控与支配能力较强;西部区域在网络中居于边缘位置,难以影响和控制其他省（区、市）;③北京、天津、江苏和上海属于“净受益”板块,广东、浙江和福建属于“经纪人”板块,吉林、内蒙古等23省（区、市）属于“净溢出”板块;④空间邻接关系、经济发展水平差异、产业结构差异、技术创新水平差异和旅游业人数规模差异共同驱动着中国旅游业碳减排潜力空间关联网络结构的形成与演化。  相似文献   

Scattering of elastic wave by a partially sealed cylindrical shell embedded in poroelastic medium     

Liu Gan‐Bin  Xie Kang‐He  Yao Hai‐lin 《国际地质力学数值与分析法杂志》2005,29(11):1109-1126

Scattering of an elastic wave by a cylindrical shell embedded in poroelastic medium is investigated theoretically with the assumption that the shell material is also a porous elastic medium. The porous medium is modellized via Biot's theory and the scattering by cylindrical shell is expressed by the definition of scattering matrix. The normal mode expansion technique is employed for analysing the scattering field, and the asymptotic solutions of displacements, stresses and pore pressure are derived. Two limiting cases‐scattering by a poroelastic cylinder in Biot medium and a elastic cylindrical shell in elastic medium are obtained from the general solutions. The dispersion curves of displacement amplitude at the interface of shell and medium is compared with the case of elastic shell. The scattering amplitude associated with the fast, slow and transverse waves are identified by numerical simulation. Furthermore, the influence of the poroelastic property of shell material on scattering amplitude is analysed. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

3-D BAROCLINIC NUMERICAL SIMULATION OF THE SOUTH CHINA SEA I. UPPER CIRCULATION     

蔡树群甘子钧  刘秦玉 《中国海洋湖沼学报》2001,19(3):208-216

A three-dimensional baroclinic shelf sea model was employed to simulate the seasonal characteristics of the South China Sea (SCS) upper circulation. The results showed that: in summer, an anticyclonic eddy, after its formation between the Bashi Channel and Dongsha Islands in the northeastern SCS, moves southwestward until it disperses slowly. There exists a northward western boundary current along the east shore of the Indo-China Peninsula in the western SCS and an anticyclonic gyre in the southern SCS. But at the end of summer and beginning of autumn, a weak local cyclonic eddy forms in the Nansha Trough, then grows slowly and moves westward till it becomes a cyclonic gyre in the southern SCS in autumn. At the beginning of winter, there exists a cyclonic gyre in the northern and southern SCS, and there is a southward western boundary current along the east shore of the Indo-China Peninsula. But at the end of winter, an anticyclonic eddy grows and moves toward the western boundary after forming in the Nansha Trough. The eddy‘s movement induces a new opposite sign eddy on its eastern side, while the strength of the southward western boundary current gets weakened. This phenomenon continues till spring and causes eddies in the southern SCS.  相似文献   

常德1631年大震事件的多场点群发式构造模型     

甘家思  刘锁旺  申重阳 《大地测量与地球动力学》1993,(4)

根据对常德1631年地震事件的史料鉴别,尤其是江陵为典型七度震害这一事实,运用震声传播方向和地光物理场以及地震烈度衰减关系,拟合推断此地震事件的序列主要由安乡北6 3/4级地震、常德北太阳山7级地震、澧县6级地震、大庸6级地震和澧县—安乡6 1/2级地震组成,相应的地震地质背景是江汉—洞庭地区晚更新世以来的剩余形变呈四象限分布。若考虑地震-构造相关分布为“Z”字型,则该地震事件的主控构造——太阳山断裂带东断裂具左旋走滑的力学机制。根据区域地震—构造相关发展过程,常德大震事件可视为1668年郯城8 1/2级地震的前震序列组成部分。  相似文献   

Scaling properties of Canadian flood flows     

Sheng Yue  Thian Yew Gan 《水文研究》2009,23(2):245-258

This study investigated the spatial scaling properties of Canadian flood flows, namely, annual maximum mean 1‐, 5‐ and 7‐day flows using both the product moments (PMs) and probability weighted moments (PWMs). Both approaches demonstrate that flood flows in climatic regions 1 (Pacific), 2 (South British Columbia mountains), 3 (Yukon and northern British Columbia), 6 (Northeastern forest), 7 (Great Lakes and St. Lawrence rivers), 8 (Atlantic), and 10 (Arctic tundra) exhibit simple scaling with scaling exponent θ/H close to 0·90, while flood flows in regions 4 (Prairie provinces), 5 (Northwestern forest), and 9 (Mackenzie) does not with scaling exponent θ/H close to 0·50. The plots of coefficient of variations of flood flows versus drainage area indicate that Cv remains almost constant in regions 1, 2, 3, 6, 7, 8, and 10, while it decreases as drainage area increases in regions 4, 5, and 9. These results demonstrate that the index flood method is applicable in climatic regions 1, 2, 3, 6, 7, 8, and 10, while it is not in climatic regions 4, 5, and 9. The physical backgroud of the simple scaling of flood flows in most Canadian climatic regions is that snowmelt or rain‐on‐snow runoff is a dominant flood‐generating mechanism across the country. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

Electro-osmotic permeability model based on ions migration     

Zhou  Jian  Gan  Qiyun  Tao  Yanli 《Acta Geotechnica》2022,17(6):2379-2393

Acta Geotechnica - Electro-osmotic permeability is a very important parameter in soil drainage and electrochemical remediation. The present widely used equation for calculating the electro-osmotic...  相似文献