四川九龙县溪谷输变电工程场地稳定性的岩体力学分析     

曹广鹏  李渝生  鲍杰 《地质灾害与环境保护》2011,22(4):46-49

溪谷输变电站工程场地具有较复杂的双层地质结构.岩土体拉分变形明显.场地后缘及底部岩土体的主应力和剪应力集中明显,堆积体内部岩体处于拉分松弛状态.岩土体的潜在变形模式以蠕滑-拉裂为主.在水库蓄水与地震共同作用的极限工况下.场地处于潜在不稳定状态.  相似文献   

遥感和光谱地质进展及其对矿产勘查的实践应用   总被引：1，自引：0，他引：1  

燕守勋  武晓波  周朝宪  刘朝晖  庄永成  曹春香  魏欣欣  于彩虹  肖春生 《地球科学进展》2011,26(1):13-29

根据2009年Economic Geology出版的专辑Remote Sensing and Spectral Geology,近年来发表的相关文献以及研究和应用的实践,对遥感与光谱地质进行了综述.内容从测谱学、TM/ETM和ASTER宽波段遥感应用,到地面和航空高光谱遥感应用与热红外遥感.传统的信息填图主要是解译,现...  相似文献   

北祁连山—阿拉善地区寒武纪构造—岩相古地理   总被引：1，自引：0，他引：1  

由伟丰  张海清  校培喜  曹宣铎  胡云绪  谢从瑞 《地球科学进展》2011,26(10):1092-1100

通过对大量野外露头资料的详细分析,结合前人对该区的研究成果,对北祁连山—阿拉善地区的地层划分,构造演化及沉积相类型进行了研究。对香山群、韩母山群进行了重新厘定,将香山群的时代厘定为寒武纪—奥陶纪,韩母山群厘定为震旦纪—寒武纪。在研究区共识别出4种沉积相类型：海岸相、浅海相、半深海相及深海—洋盆相。在上述研究的基础上,采...  相似文献   

Pressure Evolution and Hydrocarbon Migration-Accumulation in the Moliqing Fault Depression,Yitong Basin,Northeast China     

曹强  叶加仁  陆俊泽  黄胜兵  唐大卿 《中国地质大学学报(英文版)》2011,(3)

The Yitong(伊通) basin is a Late Mesozoic and Cenozoic continental sedimentary basin in Northeast China.On the basis of well tests and seismic data,we use the 2D modeling technique to rebuild the pressure evolution and hydrocarbon migration in the Moliqing(莫里青) fault depression of the Yitong basin.Based on the modeling results,four conclusions are drawn as follows.(1) The Eocene Shuangyang(双阳) Formation within the Moliqing fault depression had entirely undergone three epi-sodic cycles of pressure accumulation...  相似文献   

青海德合龙洼铜（金）矿流体包裹体特征及成矿作用分析   总被引：3，自引：0，他引：3       下载免费PDF全文

曹勇华  赖健清  康亚龙  樊俊昌 《地学前缘》2011,18(5):147-158

德合龙洼铜（金）矿床为青藏高原北东端的一个岩浆热液型矿床。研究发现矿石中石英发育富液相水溶液（Ⅰ型）、富气相水溶液（Ⅱ型）和含子矿物水溶液（Ⅲ型）3种类型的流体包裹体。Ⅰ型包裹体呈均一至液相,均一温度为187～413℃,盐度值（NaClequiv.,质量分数）则为2.0%～19.0%。Ⅱ型包裹体呈均一至气相,均一温度为...  相似文献   

Source Apportionment of PAHs Using Two Mathematical Models for Mangrove Sediments in Shantou Coastal Zone,China   总被引：2，自引：0，他引：2  

Qimin Cao  Guizhu Chen 《Estuaries and Coasts》2011,34(5):950-960

Thirty-five surface sediment samples collected from three mangroves in Shantou coastal zone, China in 2007 were analyzed for a suite of polycyclic aromatic hydrocarbons (PAHs). Two mathematical models were used to determine the profiles and relative contributions of PAH sources to the mangroves. The two models are principal component analyses (PCA) with multiple linear regression analysis (MLR) and positive matrix factorization (PMF). Both models identified five factors and gave excellent correlation coefficients between predicted and measured levels of 16 PAH compounds, but the results had some differences. The PAH contribution rate attributed to vehicular emission sources identified by PCA-MLR was 37.20%, but the rate identified by PMF was only 12.37%. The main sources identified by PCA-MLR were combination of biomass/coal combustion and vehicular emissions, whereas the main source identified by PMF was only biomass/coal combustion. The PMF analysis was the preferred model for the paper data set.  相似文献   

Erratum to: An application of a new method in permafrost environment assessment of Muli mining area in Qinghai-Tibet Plateau,China     

Wei Cao  Yu Sheng  Yinghong Qin  Jing Li  Jichun Wu 《Environmental Earth Sciences》2011,63(3):617-617

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Sorption and desorption behavior of lead on a Chinese kaolin   总被引：1，自引：0，他引：1  

Shengli Wang  Zhongren Nan  Xinde Cao  Qin Liao  Jiao Liu  Wenfei Wu  Ting Zhou  Cuicui Zhao  Wangqiang Jin 《Environmental Earth Sciences》2011,63(1):145-149

The sorption and desorption of Pb on kaolin from Suzhou, China were investigated. The sorption experiment was conducted in a 0.01 M NaNO₃ aqueous solution with respect to the effects of initial Pb concentration, pH, solid/solution ratio, and temperature. Langmuir and Freundlich models well described equilibrium isotherms of Pb sorption. Less than 5% of Pb sorbed was desorbed with 0.01 M NaNO₃ extraction, suggesting a dominant specific sorption of Pb. As the initial pH increased, the sorption of Pb on the kaolin increased. More than 60% of Pb was sorbed at pH 2.69 far below the point of zero net charge of the kaolin at 4.2, indicating a mechanism of Pb inner-sphere complex or by chemisorption. Lead sorption decreased with increasing temperature, indicating a process of exothermic sorption.  相似文献   

Research on the water use efficiency and foliar nutrient status of <Emphasis Type="Italic">Populus euphratica</Emphasis> and <Emphasis Type="Italic">Tamarix ramosissima</Emphasis> in the extreme arid region of China     

Sheng Kui Cao  Qi Feng  Yong Hong Su  Zong Qiang Chang  Hai Yang Xi 《Environmental Earth Sciences》2011,62(8):1597-1607

Seasonal variations in foliar stable carbon composition (δ¹³C) and nitrogen (N), phosphorus (P) and potassium (K) concentrations of Populus euphratica Olivier and Tamarix ramosissima Ledeb, as well as correlations between foliar δ¹³C values and N, P and K concentrations were studied in the Ejina oasis in the lower reaches of the Heihe River, northwestern China. Foliar δ¹³C values, and P and K concentrations significantly differed between species. Foliar δ¹³C signatures in T. ramosissima were significantly more enriched than those in P. euphratica, but P and K concentrations of P. euphratica were higher. The seasonal variations and patterns of these were similar. The total foliar δ¹³C values and N, P and K concentrations in both P. euphratica and T. ramosissima showed a descending trend. There were significantly positive correlations between foliar δ¹³C values and N and P concentration of both P. euphratica and T. ramosissima. For the relationship between foliar δ¹³C and K concentration, there appeared oppositely positive and negative correlations in P. euphratica and T. ramosissima, respectively, but they were not significant. The simple positive correlations of δ¹³C–P% and δ¹³C–N% suggested that N and P in P. euphratica and T. ramosissima behave in a similar manner. This study also showed that there were nutrient deficiencies; N and P nutriments were the co-limiting factors in P. euphratica, while it was P nutriment in T. ramosissima.  相似文献   

Impacts of atmosphere–sea ice–ocean interaction on Southern Ocean deep convection in a climate system model     

Libin Ma  Bin Wang  Jian Cao 《Climate Dynamics》2020,54(9):4075-4093

Deep convection in polar oceans plays a critical role in the variability of global climate. In this study, we investigate potential impacts of atmosphere–sea ice–ocean interaction on deep convection in the Southern Ocean (SO) of a climate system model (CSM) by changing sea ice–ocean stress. Sea ice–ocean stress plays a vital role in the horizontal momentum exchange between sea ice and the ocean, and can be parameterized as a function of the turning angle between sea ice and ocean velocity. Observations have shown that the turning angle is closely linked to the sea-ice intrinsic properties, including speed and roughness, and it varies spatially. However, a fixed turning angle, i.e., zero turning angle, is prescribed in most of the state-of-the-art CSMs. Thus, sensitivities of SO deep convection to zero and non-zero turning angles are discussed in this study. We show that the use of a non-zero turning angle weakens open–ocean deep convection and intensifies continental shelf slope convection. Our analyses reveal that a non-zero turning angle first induces offshore movement of sea ice transporting to the open SO, which leads to sea ice decrease in the SO coastal region and increase in the open SO. In the SO coastal region, the enhanced sea-ice divergence intensifies the formation of denser surface water descending along continental shelf by enhanced salt flux and reduced freshwater flux, combined with enhanced Ekman pumping and weakened stratification, contributing to the occurrence and intensification of continental shelf slope convection. On the other hand, the increased sea ice in the open SO weakens the westerlies, enhances sea-level pressure, and increases freshwater flux, whilst oceanic cyclonic circulation slows down, sea surface temperature and sea surface salinity decrease in the open SO response to the atmospheric changes. Thus, weakened cyclonic circulation, along with enhanced freshwater flux, reduced deep–ocean heat content, and increased stability of sea water, dampens the open–ocean deep convection in the SO, which in turn cools the sea surface temperature, increases sea-level pressure, and finally increases sea-ice concentration, providing a positive feedback. In the CSM, the use of a non-zero turning angle has the capability to reduce the SO warm bias. These results highlight the importance of an accurate representation of sea ice–ocean coupling processes in a CSM.  相似文献