994 resultados para 604
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This review paper provides a brief review on the development of ideas in the fields of the sea level change of the ECS (East China Sea), the history of the Yangtze River entering the sea and paleochannels in the shelf of the ECS since the Last Glacial Maximum (LGM). The paper summarizes two opposite theories about the Yangtze River entering the sea during the LGM. One theory is that the Yangtze River input a lacustrine in the north of Jiangsu province which was defunct in middle Holocene, and the river was once dry. The other was that the Yangtze River still existed and entered into the Okinawa Trough during the LGM, but scholars share different opinions on which course the river ran across and which place the river input the trough. This paper concludes future work is to study the evolution of the Yangtze River and the paleoclimate and the corresponding events as a whole from the view of regional and even global change, and more attention should be paid to the study on mud sediment, the Yangtze River's response to the changes in climate and sea-level, and the channel metamorphosis.
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本论文报道从海洋中分离到的一株聚磷菌的分离、鉴定、在系统发育中的地位、除磷特性、菌体内多磷酸盐颗粒的研究、D-海因酶和核苷二磷酸激酶基因的克隆及序列分析,为海水系统的生物除磷提供部分基础资料。 从黄海海域分离到聚磷菌Halomonas sp. YSR-3,菌体呈杆状,大小为3.5 μm×1 μm,革兰氏阴性,好氧生长,能运动。透射电镜观察发现,菌体内有致密颗粒。经DAPI染色确定该致密颗粒是多磷酸盐,亦可称为异染粒、迂回体。16S rDNA鉴定结果表明,YSR-3与Halomonas属中的marine bacterium B5-7有较高的同源性,相似值99%。YSR-3的生理生化特性:对氯霉素和卡那霉素敏感;淀粉水解呈阳性;反硝化和几丁质降解呈阴性;能将葡萄糖作为唯一碳源和能源。 对YSR-3的培养条件进行优化。以海水2216培养基、24 ℃、180 rpm、pH 6.5的条件培养,更利于菌体生长和菌体内多磷酸盐的形成。 对YSR-3的除磷特性进行研究。无磷培养时,菌体不能生长;用磷酸钾盐作为磷源时,菌体生长较好,形成多磷酸盐的菌体比例较高;较适合YSR-3菌体生长和多磷酸盐形成的磷源是KH2PO4,较适磷浓度为1.5 mmol/L。pH的变化影响菌株的生长、多磷酸盐形成和除磷效果。pH值为5时,菌体的数量几乎不增加,体内多磷酸盐和培养基中磷含量变化不大;pH值为6、7和8时,菌体生长良好,95%以上的菌体内形成多磷酸盐,培养基中磷含量明显下降。YSR-3在不同培养基中除磷量和除磷率不同。在高磷培养基中除磷量为0.7 mmol/L(磷含量由1.84 mmol/L降到1.14 mmol/L),除磷率为37.5%;在低磷培养基中除磷量为0.02 mmol/L(磷含量由0.028 mmol/L降到0.008 mmol/L),除磷率为72.2%。 以海洋聚磷菌Halomonas sp. YSR-3的总DNA为模板,用PCR法扩增D-海因酶基因和核苷二磷酸激酶基因,将扩增片段克隆到pGM-T载体,转化E.coli TOP10菌株,经蓝白斑筛选、菌落PCR得到阳性克隆,测序后对序列进行Blast比对分析。得到的D-海因酶基因序列长度为1510 bp,与Pseudomonas entomophila L48的海因酶基因序列的相似性为77%。翻译后的序列与Pseudomonas fluorescens Pf-5,Marinomonas sp. MED121,Burkholderia vietnamiensis G4的海因酶蛋白序列相似性分别为75%,73%,70%。得到的核苷二磷酸激酶基因序列长度为420bp,翻译后的序列与Loktanella vestfoldensis SKA53,Jannaschia sp. CCS1,Roseobacter sp. CCS2的核苷二磷酸激酶蛋白序列相似性分别为89%,86%,85%。 聚磷菌能将外界环境中的磷吸收到体内,并以多磷酸盐的形式储存。多磷酸盐对于细胞的生存和生长有很重要的作用,但目前对于多磷酸盐的形成过程以及过程调控还不是很清楚。在今后可以通过构建高效表达的重组菌,提高与除磷相关的酶的纯度及活性。同时可以将相关酶的基因进行突变,对基因表达的调控以及酶的代谢以及功能结构等多方面进行基础研究,使聚磷菌在生物除磷中得到广泛应用。
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A new lead(II) phosphonate, Pb[(PO3)(2)C(OH)CH3]center dot H2O (1) was hydrothermally synthesized and characterized by IR, elemental analysis, UV, TGA, SEM, and single crystal X-ray diffraction analysis. X-ray crystallographic study showed that complex 1 has a two-dimensional double layered hybrid structure containing interconnected 4- and 12-membered rings and shows an unusual (5,5)-connected (4(7) . 6(3)) (4(8) .6(2)) topology. (C) 2008 Elsevier B.V. All rights reserved.
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连续5年的封育对轻牧与重牧区金露梅灌丛产生了影响。结果表明:封育后轻牧与重牧区的丰富度指数、多样性指数和均匀度指数都有所下降;总盖度、枯草盖度和上下层株高增加,绿草盖度减少,群落内主要植物种群特征发生相应变化,轻牧区金露梅灌丛的莎草类、杂草类和金露梅的地上生物量减少,而枯草、禾草的生物量增加,其中枯草生物量增加显著(P
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Genomic constitutions of three taxa of Hystrix Moench, H. patula, H. duthiei ssp. duthiei and H. duthiei ssp. longearistata, were examined by meiotic pairing behavior and genomic in-situ hybridization. Meiotic pairing in hybrids of H. patula x Pseudoroegneria spicata (St), H. patula x Elymus wawawaiensis (StH), H. patula x H. duthiei ssp. longearistata, H. patula x Psathyrostachys huashanica (Ns(h)), H. duthiei ssp. duthiei x Psa. huashanica, H. duthiei ssp. longearistata x Psa. huashanica, Leymus multicaulis (NsXm) x H. duthiei ssp. longearistata averaged 6.53, 12.83, 1.32, 0.29, 5.18, 5.11 and 10.47 bivalents per cell, respectively. The results indicate that H. patula has the StH genome and H. duthiei ssp. duthiei and H. duthiei ssp. longearistata have the NsXm genome. Results of genomic in-situ hybridization analysis strongly supported the chromosome pairing data; therefore it is concluded that the type species of Hystrix, H. patula, should be included in Elymus, and that H. duthiei ssp. duthiei and H. duthiei ssp. longearistata should be transferred to Leymus.
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基于多变量T-S模型,根据文[l]中的FNN's-I型模糊神经网络结构,针对多输入多输出(MIMO)受控对象,提出了实用的多变量控制结构和算法,该方法在较少的先验知识的情况下能在线自学习有关模糊神经网络控制器的参数。最后将该控制方法应用于一实例仿真实验中,结果表明该方法是可行的、有效的。
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本文首先在总体分析国内外机器人误差分析方法的基础上,指明前人对机器人误差的分析多数着重于对关节变量的分析,而很少涉及关节参数误差对机器人轨迹误差的影响;然后从两自由度机器人入手,详细分析了机器人关节参数如杆长、起始角等对机器人轨迹误差的影响程度,并通过求解关节参数建立机器人的精确模型;最后分析了六自由度机器人关节参数对轨迹误差的影响程度,并用单纯形法对机器人的关节参数进行求解,建立机器人的精确模型并获得机器人的正确轨迹。本文提出用单纯形法优化求解机器人关节参数,经过仿真验证:对六自由度机器人关节参数的求解是有效的,完全可以建立机器人的精确模型,完成了预定的研究目标,具有一定的学术价值和现实意义。
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从生物成矿研究现状, 铊矿床地质概况着手, 通过中国西南低温成矿域中铊矿床实例, 讨论铊富集成矿的地质背景和生物成矿机制. 在铊矿床生物成矿研究中, 着重从生物富集与铊有相关性, 岩矿石中微古动物富集铊, 富铊矿石中生物化石铸型, 生物硫参与成矿和铊矿石中富生物成因有机碳几个方面进行讨论. 铊矿床经历了同生生物富集和后成热液改造二个成矿阶段, 由于后成热液改造作用强烈, 使同生生物富集矿石中生物残留无几, 故使矿床呈现出热液改造矿床的面貌.
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甘肃文县阳山金矿的探明黄金储量已达308t,平均品位4.74g/t,是我国地质勘查储量最大的金矿床。该矿床产于西秦岭造山带,是一个同碰撞形成的类卡林型金矿床,矿体受EW向韧脆性剪切带控制,赋矿围岩为泥盆系碳质千枚岩-板岩-碳酸盐-硅质岩和侵入其中的花岗斑岩脉。流体成矿过程包括:形成石英-绢云母-黄铁矿组合的早阶段,形成石英-黄铁矿-毒砂-方铅矿等多金属组合的主成矿阶段,形成碳酸盐-辉锑矿-石英网脉的晚阶段。 与矿体关系较为密切的花岗斑岩富集LILE 和 LREE, 亏损 Ba, Sr, Nb, Ta, P 和Ti,ΣREE=54.35~124.01 μg/g ,(La/Yb)N=9.72~27.80,δEu=0.70~0.89, ISr值为0.70806~0.71756,平均0.71107;εNd(t)平均-3.4;Nd模式年龄(T2DM)平均1.34(Ga)。表明花岗斑岩岩浆应源自成熟度较低的中元古代基底地壳物质。花岗斑岩的(206Pb/204Pb)220Ma、(207Pb/204Pb)220Ma和(208Pb/204Pb)220Ma的平均值分别为17.875、15.604和38.296,与秦岭微陆块的中元古代基底和碧口地体碧口群的Pb同位素组成一致。考虑到前人获得碧口群的年龄为1.235~1.367Ga,而秦岭微陆块沿勉略缝合带向南仰冲到碧口地体之上,我们认为由碧口群等组成的俯冲板片的变质脱水熔融作用导致了阳山金矿带花岗斑岩的形成。因此,阳山金矿带的花岗斑岩是扬子与华北大陆中生代碰撞造山过程中形成的同碰撞花岗岩类。 最新的S,Sr和Pb同位素研究表明:热液成矿早阶段的黄铁矿的34S值范围介于-15.5‰~6.59‰之间,总体离散性比较大,显示沉积地层来源的特征,硫同位素组成属离散型,不具有岩浆主导的成矿的塔式效应。花岗岩中黄铁矿硫同位素范围很集中,34S值处于-1.47‰~2.12‰之间,本区花岗斑岩不可能为成矿物质的主要来源。矿石硫化物的初始锶同位素比值范围较大(0.70877~0.71697,平均为0.71258),显示成矿物质并非单一来源,考虑到花岗斑岩先于矿床形成,只在后期构造作用的岩体部分成矿的地质事实,少量矿石中的低锶同位素比值黄铁矿有可能来自作为围岩的花岗斑岩,也可能来自基底物质。矿石硫化物Pb同位素206Pb/204Pb=17.552~18.853,平均18.260;207Pb/204Pb=15.574~15.928,平均15.685;208Pb/204Pb=37.894~39.293,平均38.680,变化范围比较大。μ=9.46~10.06,平均为9.65,ω值介于36.96~42.21,显示了铅源的物质成熟度较高,要求最佳物源是浅变质化学-碎屑沉积建造,恰好与本区泥盆构造层为浅变质细碎屑岩夹薄层灰岩系的特征一致,部分低Sr和Pb同位素比值的成矿物质可能来自于作为围岩的花岗斑岩和/或者基地物质。 总结前人阳山金矿床的H-O-C同位素体系的研究得出,初始成矿流体来源于碳酸盐地层或相似岩石建造的变质或/和改造脱水,成矿流体系统从早到晚、从深到浅,由变质热液演变为大气降水热液。与本文得出的结论一致。 总而言之, 阳山金矿矿成矿流体的来源早期具有变质水特征,应来自赋矿地层或相似岩性组合的改造或变质脱水作用,晚阶段大气水为主的流体性质。成矿物质主要来自于赋矿围岩。流体经过作为部分围岩的花岗斑岩时从中萃取少部分成矿物质,而导致了少部分的低锶、铅同位素的矿石硫化物组成。 在中生代扬子板块北缘(包括碧口地块)向南秦岭陆陆碰撞过程中,扬子北缘板片沿勉略断裂向北俯冲到南秦岭之下,下插板片增温增压,发生变质、脱水和部分熔融。碰撞中期,构造背景由挤压向伸展转变,减压增温的环境导致大量变质流体沿深大断裂向上运移,不断萃取围岩中大量成矿元素,并将成矿元素搬运至有利于流体聚集、成矿物质卸载的空间,使成矿物质富集成矿。阳山金矿床定位于泥盆系构造层中,成矿时代为190Ma左右,紧随花岗斑岩侵入作用(220Ma左右),主成矿作用发生于碰撞作用由挤压-伸展转变期的减压增温环境。成岩、成矿模式与CMF模式吻合。 阳山超大型金矿是世界罕见的碰撞造山带内类卡林型金矿床,其地质地球化学特征复杂、独特,流体性质主要与造山型金矿一致,矿床地质主要与卡林型金矿一致,部分特征兼与造山型和卡林型两类矿床之间,花岗斑岩本身成矿的特点又为阳山所特有,总体具有造山型向卡林型金矿过渡的性质。因此建议以“秦岭式”或“阳山式”类卡林型金矿床代表与阳山金矿具有类似成矿背景及地球化学性质的矿床。
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秦岭造山带是华北与扬子两大古板块的接合带,在空间上,自北而南,秦岭造山带可分为华北板块南缘(华熊地块)、北秦岭造山带、南秦岭造山带和扬子板块北缘等4个构造单元。小秦岭金矿田位于华熊地块北缘,是国内外学者共识的造山型金矿田,河南灵宝大湖金-钼矿床位于小秦岭金矿田,属断控脉状矿床。大湖金-钼矿床最先正是以金矿床进行勘查的,其黄金储量28t,平均品位8.7g/t。随着开采深度的加大,部分含金石英脉向深部转变为辉钼矿-石英脉,目前探明钼资源量已达中型规模。 本论文主要从区域地质背景、矿床地质特征、元素地球化学、同位素地球化学、流体包裹体地球化学、矿床年代学及成矿机理等角度对大湖金-钼矿床进行了较为系统的研究,主要获得如下认识: 成矿过程经历3个阶段:早阶段为黄铁矿-石英脉,遭受变形、破碎,应形成于挤压或压剪过程;中阶段为细粒的辉钼矿-黄铁矿-石英网脉,贯入到早阶段黄铁矿或石英矿物的裂隙(可呈共轭状),应形成于剪切环境;晚阶段石英-碳酸盐细脉具梳状构造,充填于张性或张扭性裂隙。 大湖金-钼矿床的金属硫化物ISr=0.70470-0.71312,平均0.70854;(143Nd/144Nd)i=0.51143-0.51215,平均0.51162;(206Pb/204Pb)i=17.033-17.285,(207Pb/204Pb)i=15.358-15.438,(208Pb/204Pb)i = 37.307-37.582。其围岩太华群样品平均值ISr=0.72294,(143Nd/144Nd)i=0.51107,(206Pb/204Pb)i=17.127-18.392,(207Pb/204Pb)i =15.416-15.604,(208Pb/204Pb)i=37.498-37.814,它们的平均值分别是17.547,15.470,37.616。通过金属硫化物及围岩太华群的对比,可以看出,成矿物质具有太华群和深部地幔混合的特征。 通过对不同阶段的含矿石英脉中的流体包裹体特征研究表明,早阶段只发育CO2-H2O型流体包裹体;中阶段流体包裹体类型复杂,有纯CO2型、CO2-H2O型、H2O-NaCl型和含子晶包裹体,指示流体沸腾作用强烈;而晚阶段只发育水溶液包裹体。早、中、晚3个阶段的流体包裹体均一温度分别集中在400-500℃、290-470℃、220-260℃;估计的早、中阶段流体的最低捕获压力分别为138-331MPa和78-237MPa,对应于成矿深度分别为13.8-11.0km和7.8-8.0km。早、中阶段的压力反应出静岩压力到静水压力的转变。成矿温度和压力明显高于浅部含金石英脉的成矿温度120-310℃,成矿压力100-150MPa。与野外观察到的“上金下钼”的空间关系一致。 大湖金-钼矿床辉钼矿-石英脉Re-Os同位素模式年龄较集中,介于215.4±5.4-255.6±9.6Ma,Re-0s等时线年龄为218±41Ma(MSWD=38,2σ误差),表明大湖金-钼矿的辉矿化形成于印支期。 三叠纪末,随着古秦岭洋的逐渐封闭,处在弧后转换带的深部岩石在挤压作用下发生变质脱水而形成初始成矿流体,成矿流体沿断裂带(韧性剪切带)向上迁移而引起大湖钼矿床成矿系统的发育。随着区域构造环境由挤压转为伸展,区域的变质脱水更强,形成大量成矿流体,变质流体上侵为浅层流体循环提供了的热能,而浅层构造也因减压扩容而为流体循环提供了通道,这无疑有利于浅层流体循环和混入成矿系统。同时,增温和减压也有利于成矿流体发生沸腾。因此,充足的流体、热以及强烈的流体沸腾等,势必导致发生最为强烈的成矿物质快速沉淀作用。随着挤压作用的减弱,伸展作用的增强,区域热异常消失,地壳深部组分发生亏损,流体以浅源大气降水占主导,成矿作用迅速衰竭,形成石英-碳酸盐网脉,对成矿作用贡献减弱。总之,通过对大湖金钼矿床研究表明,大湖金钼矿床形成于由挤压转向伸展的构造背景,这与矿床地质的特征一致。
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A high quality NaA zeolite membrane, which shows a H-2/n-C4H10 permselectivity of 106, has been synthesized on a seeded alpha-Al2O3 support by a multistage synthesis method.
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To investigate the psychological and behavioral status and their influencing factors of children left behind in rural areas in China, 604 students were chosen from primary fifth grade, junior second grade and senior first grade in high schools in local villages and towns of Chongqing and Guizhou to complete some investegations. The results showed that children left behind actually had some internalizing problems including depression, state-trait anxiety, social anxiety, low self-esteem and some social problems in campus; however, they had no delinquency or aggression behaviors. Low parents’ educational level, low life standards, no-good parent-child relationship, the long years parent spent outside, the long time parent spent outside every year, the young age of child when his parent left him, the low contact frequency between parent and child when parent went out for work, all can be the influencing factors made child behave some psychological or behavioral problems. Children left behind need some appropriate psychological intervention, to improve parent-child relationship, to help release internalizing problems and amend interpersonal relationship at school. Several advices may be useful to improve psychological and behavioral problems of children left behind, which are for parents who work outside home not to work long to 10 years, or stay out for work more than 10 months per year, or left child to work when he is younger than two years old, or contact child more than one month after the last contact when work outside home, and you’d better contact child once a day. All of these could be helpful for children left behind to overcome some psychological or behavioral problems.
Resumo:
The work reported here lies in the area of overlap between artificial intelligence software engineering. As research in artificial intelligence, it is a step towards a model of problem solving in the domain of programming. In particular, this work focuses on the routine aspects of programming which involve the application of previous experience with similar programs. I call this programming by inspection. Programming is viewed here as a kind of engineering activity. Analysis and synthesis by inspection area prominent part of expert problem solving in many other engineering disciplines, such as electrical and mechanical engineering. The notion of inspections methods in programming developed in this work is motivated by similar notions in other areas of engineering. This work is also motivated by current practical concerns in the area of software engineering. The inadequacy of current programming technology is universally recognized. Part of the solution to this problem will be to increase the level of automation in programming. I believe that the next major step in the evolution of more automated programming will be interactive systems which provide a mixture of partially automated program analysis, synthesis and verification. One such system being developed at MIT, called the programmer's apprentice, is the immediate intended application of this work. This report concentrates on the knowledge are of the programmer's apprentice, which is the form of a taxonomy of commonly used algorithms and data structures. To the extent that a programmer is able to construct and manipulate programs in terms of the forms in such a taxonomy, he may relieve himself of many details and generally raise the conceptual level of his interaction with the system, as compared with present day programming environments. Also, since it is practical to expand a great deal of effort pre-analyzing the entries in a library, the difficulty of verifying the correctness of programs constructed this way is correspondingly reduced. The feasibility of this approach is demonstrated by the design of an initial library of common techniques for manipulating symbolic data. This document also reports on the further development of a formalism called the plan calculus for specifying computations in a programming language independent manner. This formalism combines both data and control abstraction in a uniform framework that has facilities for representing multiple points of view and side effects.
Resumo:
The digital divide continues to challenge political and academic circles worldwide. A range of policy solutions is briefly evaluated, from laissez-faire on the right to “arithmetic” egalitarianism on the left. The article recasts the digital divide as a problem for the social distribution of presumptively important information (e.g., electoral data, news, science) within postindustrial society. Endorsing in general terms the left-liberal approach of differential or “geometric” egalitarianism, it seeks to invest this with greater precision, and therefore utility, by means of a possibly original synthesis of the ideas of John Rawls and R. H. Tawney. It is argued that, once certain categories of information are accorded the status of “primary goods,” their distribution must then comply with principles of justice as articulated by those major 20th century exponents of ethical social democracy. The resultant Rawls-Tawney theorem, if valid, might augment the portfolio of options for interventionist information policy in the 21st century