8 resultados para Modern Philosophical Interpretations and Misunderstandings

em Chinese Academy of Sciences Institutional Repositories Grid Portal


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Based on analyses of more than 600 surface sediment samples together with large amounts of previous sedimentologic and hydrologic data, the characteristics of modern sedimentary environments and dynamic depositional systems in the southern Yellow Sea (SYS) are expounded, and the controversial formation mechanism of muddy sediments is also discussed. The southern Yellow Sea shelf can be divided into low-energy sedimentary environment and high-energy sedimentary environment; the low-energy sedimentary environment can be further divided into cyclonic and anticyclonic ones, and the high-energy environment is subdivided into high-energy depositional and eroded environments. In the shelf low-energy environments, there developed muddy depositional system. In the central part of the southern Yellow Sea, there deposited the cold eddy sediments under the actions of a meso-scale cyclonic eddy (cold eddy), and in the southeast of the southern Yellow Sea, an anticyclonic eddy muddy depositional system (warm eddy sediment) was formed. These two types of sediments showed evident differences in grain size, sedimentation rate, sediment thickness and mineralogical characteristics. The high-energy environments were covered with sandy sediments on seabed; they appeared mainly in the west, south and northeast of the southern Yellow Sea. In the high-energy eroded environment, large amounts of sandstone gravels were distributed on seabed. In the high-energy depositional environment, the originally deposited fine materials (including clay and fine silt) were gradually re-suspended and then transported to a low-energy area to deposit again. In this paper, the sedimentation model of cyclonic and anticyclonic types of muddy sediments is established, and a systematic interpretation for the formation cause of muddy depositional systems in the southern Yellow Sea is given.

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A lithography-independent and wafer scale method to fabricate a metal nanogap structure is demon-strated. Polysilicon was first dry etched using photoresist (PR) as the etch mask patterned by photolithography.Then, by depositing conformal SiO_2 on the polysilicon pattern, etching back SiO_2 anisotropically in the perpendic-ular direction and removing the polysilicon with KOH, a sacrificial SiO_2 spacer was obtained. Finally, after metal evaporation and lifting-off of the SiO_2 spacer, an 82 nm metal-gap structure was achieved. The size of the nanogap is not determined by the photolithography, but by the thickness of the SiO_2. The method reported in this paper is compatible with modern semiconductor technology and can be used in mass production.

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The content and isotopic compositions of different sulphur species in pore-water and solid phases have been examined on five sediment cores taken from muddy sediment region in the Yellow Sea and the East China Sea. Relationships among these data have been investigated with the combination of morphology of mineral pyrite and organic matter so as to role out the diagenetic behaviour of sulphur species at the early stage of diagenesis in modern marine sediment and the origin of pyrite formation.

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新疆中部地区位于西北内陆干旱一半干旱区,是欧亚大陆的地理中心,是中纬度内陆干旱区代表性区域,也是全球变化敏感区域之一,基本特点是气候干旱、水资源匮乏、植被稀少、荒漠广布,生态系统脆弱。在研究区域内,天山山脉海拔高度差异5 000 m左右,随海拔梯度下降依次出现高山冰雪带、高山亚高山草甸带、森林带、草原带、荒漠带、沙漠带等明显完整的植被垂直带,是开展现代孢粉学和植被变化研究的理想地点。本报告在立足于该区前人工作的基础上,从表土花粉、空气花粉和现代植被之间的关系入手开展现代孢粉学研究,探讨了花粉与植被的关系。 在研究区内,选择新疆阜康市和吉木萨尔县为研究地点,设计了一条从天山博格达峰附近雪线开始直至古尔班通古特沙漠长约100 km、宽约20 km的样带。沿样带,从高山座垫植被和草甸带开始,经过中海拔地带的云杉林,置到低海拔的荒漠,在山地海拔每下降20~100 m采集一个表土花粉样品,平原每间隔10~20 km采集一个表土花粉样品,同时做现代植被调查,共采集80个表土花粉样品和调查了86个现代植被样方;在天山乌鲁木齐河河源区的大西沟,从一号冰川前缘开始,沿山谷向下直到谷口,按海拔100 m间隔采集了14个表土样品,对表土花粉与植被之间的关系进行了探讨。为了弄清空气花粉传播、散布与气象因子和植被的关系,沿样带从高山到沙漠分别在天池气象站、中国科学院阜康荒漠生态系统定位研究站和北沙窝草炭试验地设置了三个风标式空气花粉收集器,从2001年7月至2002年7月连续收集空气花粉雨,收集了跨2个年度1周年的1 14个空气花粉样品,依据分析结果研究了空气花粉的传播和散布规律以及与表土花粉和植被之间的关系,这在新疆地区乃至全国尚属首次。 根据表土花粉分析结果和现代植被样方资料的分析以及天山中段主要植物种类沿海拔高度的分布特征,天山中段北坡垂直植被带谱为:高山座垫植被(>3 400 m)、高山亚高山草甸(3 400-2 700 m)、山地云杉林(2 700-1 720 m)、森林草原过渡带(1 720-1 300 m)、蒿类荒漠(1 300-700 m)和典型荒漠(<700 m)。表土花粉谱基本上反映了相同海拔高度的现代植被带,特别是在云杉林带,表土中雪岭云杉(Picea schrenkiana)花粉占优势;在蒿类荒漠植被带表土中蒿属(Artemisia)植物花粉非常丰富;在典型荒漠植被带的表土中藜科(Chenopodiaceae)植物花粉占绝对优势,因此可依据这些建群种植物花粉含量峰值的位置划分植物群落。 空气花粉样品分析结果表明:空气中花粉主要是现生植物当年生长产出的花粉,盛花期的花粉数量能较好地反映当地的植被状况。空气中的乔木植物花粉主要有云杉(Picea),其次是柳属(Salix);灌木草本植物花粉主要是藜科和蒿属,其次是菊科(Compositae)、禾本科(Gramineae)、柽柳科(Tamaricaceae)和麻黄属(Ephedra);空气中的花粉数量与植物的花期相对应,云杉等乔木植物盛花期在夏季5月末至7月初,灌木草本植物盛花期在夏秋季节。气温、降水、风速和风向等气象条件对空气中花粉数量有很大影响,其中风速和风向影响最大。从空气花粉和表土花粉的分析结果与现生植被对比,新疆中部地区的山谷上升气流是导致花粉“爬坡”现象的主要动力,在一定条件下,上升气流搬运花粉的数量和能力是十分可观的。 空气中的花粉是现生植物当年生长产出的花粉,表土中的花粉是多年花粉落地沉积的积累,植物盖度大,该植物的花粉在空气中和表土中数量相对就大。在新疆中部地区,空气花粉能反映当地和附近周边方圆约50 km的植被状况,其花粉组合特征与表土花粉和当地现生植被分布的对比研究,可以较好地寻找花粉与植被的关系。本研究报告的研究成果不仅为新疆地区的孢粉学研究增添新的内容,而且将有助于合理解释新疆地层中、尤其是第四纪以来的地层孢粉,较客观地恢复过去的植被景观,同时可为本地区的大气环境检测提供有重要价值的参考资料。

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简要综述了宏观和微观领域的鸟类分类学研究进展。宏观领域介绍了传统形态分类学、数值分类学和支序 分类学, 结合鸣声分析强调支序分类学的应用。微观领域介绍了Sibley 分类系统和近年来出现的主要基于mtDNA 的鸟类系统学研究。通过对大量研究工作的分析提出该领域今后应进行综合性研究。

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Traditional agricultural systems are threatened world-wide mainly due to the introduction of modern agricultural techniques and the emigration of farm labourers from remote rural villages. The objective of the programme 'Globally Important Agricultural Heritage Systems' (GIAHS), initiated by the Food and Agriculture Organization (FAO) of the United Nations in 2002, is dynamic conservation of traditional agricultural systems. This article addresses the definition and content of agricultural heritage systems and discusses conservation options in the light of developing rural tourism. An explorative survey was conducted in Longxian village, situated in Zhejiang Province, southern China, focusing on the tourism potential of a typical Rice-Fish Agricultural System. The identification of heritage resources is a first step in the process of transforming an agricultural landscape into a cultural tourism landscape. However, the future of these landscapes is in the hands of a range of stakeholders and depends on their capacity to manage, in a sustainable way, tourism development strategies alongside conservation policies.

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Natural fluids with water-salt-gas are often found in every sphere of the Earth, whose physicochemical properties and geochemical behaviors are complicated. To study these properties and behaviors turns out to be one of the challenging issues in geosciences. Traditional approaches mainly depend on experiments and observations. However, it is impossible to obtain a large number of data covering a large T-P space of the Earth by experimental methods in the near future, which will hinder the advance of the theoretical study. Therefore, it is important to model natural fluids by advanced theoretical methods, by which limited experimental data can be extended to a large temperature-pressure-composition space. Physicochemical models developed in this dissertation are not only more accurate, but also extend the applied T-P-m region of the experimental data of the multi-fluid systems by about two times. These models provide the new and accurate theoretical tools for the geochemical research, especially for the water-rock interactions and the study of the fluid inclusions. The main achievements can be summarized as follows: (1) A solubility model on components of natural gases is presented. The solubility model on the systems of CH4-H2O-NaCl, C2H6-H2O-NaCl or N2-H2O-NaCl takes advantage of modern physicochemical theory and methods, and is an improvement over previous models whose prediction and precision are relatively poor. The model can predict not only the gas solubility in liquid phase but also water content in the gas phase. In addition, it can predict gases (methane or nitrogen) solubility in seawater and brine. Isochores can be determined, which are very important in the interpretation of fluid inclusions. (2) A density model on common aqueous salt solutions is developed. The density models with high precision for common aqueous salt solutions (H2O-NaCl, H2O-LiCl, H2O-KCl, H2O-MgCl2, H2O-CaCl2, H2O-SrCl2 or H2O-BaCl2) are absent in the past. Previous density models are limited to the relatively small range of experimental data, and cannot meet the requirement of the study of natural fluids. So a general density model of the above systems is presented by us based on the international standard density model of the water. The model exceeds the other models in both precision and prediction. (3) A viscosity model on common aqueous alkali-chloride solutions is proposed. Dynamic viscosity of water-salt systems, an important physics variable, is widely used in three-dimension simulation of the fluids. But in most cases, due to the lack of viscosity models with a wide T-P range, the viscosity of aqueous salt solutions is replaced by that of the water, giving rise to a relatively large uncertainty. A viscosity model with good prediction for the systems (H2O-NaCl, H2O-LiCl or H2O-KCl) is presented on the base of the international standard viscosity model of water and the density model developed before. (4) Equation of State applied in fluid inclusions. The best Equations of State in the world developed by others or us recently are applied in the study of the fluid inclusions. Phase equilibria and isochores of unitary system (e.g. H2O, CO2, CH4, O2, N2, C2H6 or H2S), binary H2O-NaCl system and ternary H2O-CH4-NaCl system are finished. From these programs and thermodynamic equations of coexisting ores, the physicochemical conditions before or after the deposits form can be determined. To some extent, it is a better tool.

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Seismic signal is a typical non-stationary signal, whose frequency is continuously changing with time and is determined by the bandwidth of seismic source and the absorption characteristic of the media underground. The most interesting target of seismic signal’s processing and explaining is to know about the local frequency’s abrupt changing with the time, since this kind of abrupt changing is indicating the changing of the physical attributes of the media underground. As to the seismic signal’s instantaneous attributes taken from time-frequency domain, the key target is to search a effective, non-negative and fast algorithm time-frequency distribution, and transform the seismic signal into this time-frequency domain to get its instantaneous power spectrum density, and then use the process of weighted adding and average etc. to get the instantaneous attributes of seismic signal. Time-frequency analysis as a powerful tool to deal with time variant non-stationary signal is becoming a hot researching spot of modern signal processing, and also is an important method to make seismic signal’s attributes analysis. This kind of method provides joint distribution message about time domain and frequency domain, and it clearly plots the correlation of signal’s frequency changing with the time. The spectrum decomposition technique makes seismic signal’s resolving rate reach its theoretical level, and by the method of all frequency scanning and imaging the three dimensional seismic data in frequency domain, it improves and promotes the resolving abilities of seismic signal vs. geological abnormal objects. Matching pursuits method is an important way to realize signal’s self-adaptive decomposition. Its main thought is that any signal can be expressed by a series of time-frequency atoms’ linear composition. By decomposition the signal within an over completed library, the time-frequency atoms which stand for the signal itself are selected neatly and self-adaptively according to the signal’s characteristics. This method has excellent sparse decomposition characteristics, and is widely used in signal de-noising, signal coding and pattern recognizing processing and is also adaptive to seismic signal’s decomposition and attributes analysis. This paper takes matching pursuits method as the key research object. As introducing the principle and implementation techniques of matching pursuits method systematically, it researches deeply the pivotal problems of atom type’s selection, the atom dictionary’s discrete, and the most matching atom’s searching algorithm, and at the same time, applying this matching pursuits method into seismic signal’s processing by picking-up correlative instantaneous messages from time-frequency analysis and spectrum decomposition to the seismic signal. Based on the research of the theory and its correlative model examination of the adaptively signal decomposition with matching pursuit method, this paper proposes a fast optimal matching time-frequency atom’s searching algorithm aimed at seismic signal’s decomposition by frequency-dominated pursuit method and this makes the MP method pertinence to seismic signal’s processing. Upon the research of optimal Gabor atom’s fast searching and matching algorithm, this paper proposes global optimal searching method using Simulated Annealing Algorithm, Genetic Algorithm and composed Simulated Annealing and Genetic Algorithm, so as to provide another way to implement fast matching pursuit method. At the same time, aimed at the characteristics of seismic signal, this paper proposes a fast matching atom’s searching algorithm by means of designating the max energy points of complex seismic signal, searching for the most optimal atom in the neighbor area of these points according to its instantaneous frequency and instantaneous phase, and this promotes the calculating efficiency of seismic signal’s matching pursuit algorithm. According to these methods proposed above, this paper implements them by programmed calculation, compares them with some open algorithm and proves this paper’s conclusions. It also testifies the active results of various methods by the processing of actual signals. The problems need to be solved further and the aftertime researching targets are as follows: continuously seeking for more efficient fast matching pursuit algorithm and expanding its application range, and also study the actual usage of matching pursuit method.