3 resultados para Olympic
em Chinese Academy of Sciences Institutional Repositories Grid Portal
Resumo:
In this work, the photosynthetic performances of Enteromorpha prolifera thalli collected from the surface and bottom of the sea of Qingdao sea area were studied with chlorophyll fluorescence and oxygraph technology. The samples with the highest photosynthetic activity among their kinds, the floating thalli from the sea surface of the south of the Qingdao Olympic Sailing Center and the sedimentary thalli from the mud surface of the bottom Tuandao bay, were chosen as representatives of surface thalli and bottom thalli, respectively. The results showed that the maximal PSII quantum yield of the floating thalli was significantly lower than the normal level although their photosynthetic activities were relatively high; the photosynthetic potential of the thalli form the mud surface was extremely low. Thus, it is indicated that the floating thalli are seriously stressed by their environment and the thalli from the mud surface are already dead or are dying. On the other hand, the results of the laboratory cultivation showed that the sedimentary thalli cannot regain normal photosynthetic activity even under normal illumination conditions. Thus, the thalli from the mud surface cannot become reproductive source of the alga even if they can reach sea surface again. Therefore, a preliminary conclusion can be reached that, up to mid-July 2008, the environmental conditions of the Qingdao sea area are not suitable for the growth of the alga E. prolifera and for this reason the biomass of E. prolifera, in the area, could be declining.
Resumo:
稀土元素成矿与地壳的构造运动密切相关,稀土在中元古代具有大规模暴发性成矿特征。云南武定迤纳厂稀土铁铜矿床为昆阳群因民组出现稀土富集成矿的典型代表。本论文选择迤纳厂矿床为主要研究对象,系统研究矿床不同类型岩(矿)石和矿物的稀土元素地球化学特征,探讨富稀土的成矿流体、成矿物质来源和稀土元素成矿时代,揭示昆阳裂谷初期因民组稀土元素富集的地球化学机制。主要认识如下:1、迤纳厂矿床产于昆阳裂谷初期形成的禄丰一武定火山断陷盆地中。早中元古界昆阳群分布于绿汁江岩石圈断裂和小江一易门断裂的夹持地带,呈狭长状展布。迤纳厂矿床赋矿地层为昆阳群因民组上段的硅质白云岩和碱性火山岩(粗面安山岩)。矿体产出形态和矿石的结构构造等均显示矿体与赋矿地层同沉积特征;出现独立矿物氟碳饰矿、独居石及褐帘石,磷灰石、萤石、菱铁矿等矿物中也含有一定量的稀土,沿矿体走向和垂向稀土元素变化不大。2、矿体顶、底板围岩(石榴石黑云母片岩、钠长黑云母片岩等)的原岩为碱性火山岩(粗面安山岩),相对富集大离子亲石元素Ba、Cs、Rb、K、LRE日及贫Zr、Sr、Ti、Hf、HEE,为早元古代末期一中元古代早期交代富集地慢低程度部分熔融所形成的碱性火山岩。矿石稀土总量高(645-4443)×10-6,强烈富集轻稀土((La/Tb)N=17.3-81.1),稀土元素分布特征明显不同于矿区正常沉积的硅质白云岩和后期侵入的钠长石英斑岩及火山角砾岩,而与矿体顶、底板碱性火山岩中稀土元素配分特征基本一致,暗示稀土成矿物质来源与碱性火山岩有密切的关系;3、矿石中微量元素组合及变化特征与现代海底正在喷出的热液和热液沉积物中元素组合有较大的可比性,明显不同与火成碳酸岩型稀土矿床中的特征元素组合;在微量元素判别图解(Al-Fe-Mn、Fe/Ti-Al/(Al+Fe+Mn)、U-Th、Y-P2O5等)中,逸纳厂矿石均投影在热水沉积区,矿石的Y/Ho值与黑烟囱值接近,表明成矿流体为高温、还原性质,稀土成矿可能以热水沉积作用方式为主;4、对矿石中主要矿物萤石、菱铁矿、磁铁矿、石英、方解石的稀土元素特征研究表明,矿石沉积时不同矿物中稀土元素分布特征基本相同,主要受成矿流体中稀土分布特征制约。而后期变质作用形成的矿物,其稀土元素分布主要受矿物晶体结构控制。同期成矿流体从早期到晚期(块状矿石→条带状矿石),轻重稀土分异变小,稀土总量增加,条带状矿石中稀土含量最高;矿石黄铜矿6345值变化在一任3%0到2g%。范围,显示慢源硫特征;菱铁矿6r3C(8%-9.1%)、δ18O(-11.17%-15.37)‰指示成矿流体具岩浆来源和有机质的脱梭酸分解作用参与;成矿流体中稀土元素可能主要以(RE(CO3)3F)4-、(既(CO3)3F2)、(RE(F,Cl万等形式迁移,当温度降低时沉淀出氟碳饰矿等稀土矿物;5、矿石和萤石单矿物 Sm-Nd等时线年龄分别为1621士110Ma和15:38士43Ma,与矿区碱性火山岩错石的U-Pb年龄1676Ma、因民组顶部石英正长斑岩的错石U-P1。年龄1685Ma基本一致,也与因民组地层年龄1765M。较为接近,反映成矿时代为早元古代晚期和中元古代早期:这一时间也与一早元古代晚期一中元古代早期昆阳裂谷初始裂陷阶段,大量来自于地幔的碱性火山岩喷发事件相吻合。矿石。Nd(t):-2.87-3.60,萤石单矿物εNd(t):-3.93-5.90,变化范围较窄并全为负值,接近0,指示源区为富集地幔。同时结合矿床形成的构造一地质环境及矿体产出的地质形态,认为逛纳厂稀土铁铜矿床可能是在昆阳裂谷初期,在碱性火山岩浆喷发的间歇期,来自地幔富稀土、挥发份的成矿流体由火山喷流一同生沉积方式形成的矿床。6、昆阳群因民组地层中出现的稀土富集、成矿与我国的白云鄂博稀土REE-Fe-Nb超大型矿一床和澳大利亚的olympic Dam Cu-U-Au-Ag-REE超大型矿床,在成矿时代、产出大地构造背景、成矿物质来源等方面具有较大的相似性,均体现成矿受控于中元古代1.5Ga超大陆聚合前或随后裂解初始阶段伴随的非造山型碱性岩浆或热液作用,稀土来源于超大陆拼合前因板块俯冲交代而形成的富集地幔。
Resumo:
Risk perception is one of important subjects in management psychology and cognitive psychology. It is of great value in the theory and practice to investigate the social risk events that the public cares a lot especially in this social transition period. Furthermore, this study explored the factors that influence the risk perception and the results caused by risk perception. A survey including 30 hazards and 8 risk attributes was designed and distributed to about 3, 200 residents of 8 districts, Beijing. The major findings are listed as following: Firstly, combining the methods of system science and psychology, GAE program was used to indentify 7 groups of social risk events, such as national safe, government management, social stability, general mood of society, economic and finance, resources and environment & daily life problems. This study provided substance for the following studies and it was also a new attempt in research method which is of certain reference value for the related researches. Secondly, a scale of societal risk perception was designed and 2 factors were identified (Dread Risk & Unknown Risk). Reliability analysis, EFA and CFA show the reliability and validity of the societal risk questionnaire is good enough. The investigation using this scale showed that older participants and higher socioeconomic status perceived the societal hazards to be more threatening than did younger participants and lower socioeconomic status. However, there is no gender difference. Thirdly, structural equation model was used to analyze the influence factors and mechanism of societal risk perception. Risk taking, government support and social justice could influence societal risk perception directly. Government support moderated the relationship between government trust and societal risk perception. Societal risk perception influenced life satisfaction, public policy preferences and social development belief. Multi-group analysis was used to find out that the participants who have different socioeconomic status express different mechanism. Fourthly, the result of the research was used to explore the risk event of 2008 Olympic game. The results showed that government support and preparation of Olympic game influenced societal risk perception directly. Preparation moderated the relationship between government trust and risk perception. Risk perception influenced worry, effect of Olympic game and belief of successl. This result proved that risk perception could be used as an indicator. The indictor of risk perception was used to identify the characteristics of higher risk perception group. Finally, suggestions to the related decision were provide to the government.