城市抗震防灾规划中建筑物易损性评价方法的研究

基于功能和后果的抗震设防理念,提出了城市建筑物的分类方法并根据不同类别采取不同抗震易损性评价方法,其中包括应用能力谱的理论易损性分析方法和快速群体震害预测方法等。根据这些方法和泉州市规划区内的房屋调查资料,对泉州市的房屋进行了震害预测,并通过泉州市建筑物地震易损性分析的结果,提出了针对性的抗震减灾策略。所发展的易损性评价方法和对策措施对其他城市编制抗震防灾规划也具有一定参考价值。     

Assessing impacts of deepwater sewage disposal: A case study from New South Wales, Australia

To overcome the problems of beach pollution Sydney Water constructed three deepwater sewage outfalls off North Head, Bondi and Malabar. The outfalls were commissioned over the period September 1990–July 1991. A 5-year multi-disciplinary environmental monitoring programme was set up to assess the impacts on the demersal fish and soft-bottom macro-invertebrate communities. Assessment of impact was based on an asymmetrical analysis of variance which provided an a priori orthogonal contrast between a single outfall and multiple control sites sampled before and after commissioning. Impacts were detected in both communities, included several commercially and recreationally important species of fish, and occurred with the greatest frequency in the soft-bottom community. The results are summarized, and several examples are presented and show that the direction and magnitude of the impacts varied among outfalls and taxa. The results are then discussed in terms of the needs of future monitoring and the implications for the assessment of human-induced impacts in other parts of the world.     

A system dynamics approach for urban water reuse planning: a case study from the Great Lakes region

Water reclamation and reuse practices are recently receiving growing attention due to increasing water scarcity, concerns about the effect of wastewater discharges on receiving water, and availability of high-performing and cost-effective water reuse technologies. However, incorporation of water reuse schemes into water/wastewater infrastructure systems is a complex decision making process, involving various economical, technological, and environmental criteria. System dynamics (SD) allows modeling of complex systems and provides information about the temporal and feedback behavior of the system. In this sense, a SD model of the existing water/wastewater system in Kalamazoo-Michigan, an urban area in the Great Lakes region, was created with the hypothetical incorporation of water reuse. The model simulates and optimizes the overall water system cost (including water, wastewater and water reuse components), accounting for future scenarios of population, economic growth and climate change. Results indicate significant levels of water reuse after an infrastructure build delay. The model also indicates that a decision to implement water reuse yields remarkably lower water withdrawals and lower water treatment costs even in a location with a relatively abundant water supply like Kalamazoo. This study emphasizes the fact that a true understanding of the practice of water reuse cannot be achieved without taking regional and climatic parameters into account.     

强震地面运动的超随机特性研究

简述了几种常用的地震动平稳随机模型，这几种地震动平稳随机模型的功率谱是一组光滑的函数，相应的自相关函数基本上是指数衰减的振荡函数，且很快衰减到零；但是真实地震动的归一化自相关函数则有一较显著的随机噪声项，这个随机噪声的幅值为0．15左右，这就是本文中所说的超随机特性。目前常用的地震动平稳随机模型没有考虑这个随机噪声项及其对结构反应的影响。本文将真实地震动的自相关函数分解为一确定性函数和一随机噪声的叠加，并对自相关函数中的噪声部分进行了分析，得出两条重要性质。本文的研究结果表明地震动加速度时程的平方和(SS)比峰值加速度(PGA)更好地量度了地震地面运动强度。由于归一化自相关函数的随机噪声部分所对应的功率谱的随机波动成分对频率的积分为零，即归一化自相关函数的噪声部分对地震动总功率或平方和的贡献为零，因此自相关函数的随机噪声项对地震动的幅值影响不大，但自相关函数的随机噪声项明显改变了地震动功率谱在频域上的分布特征，因此会对结构反应产生一定的影响。由于篇幅所限详细内容将在下一篇文章中作进一步探讨。     

基于ANP-SWOT模型的城市应急避难场所发展规划——以兰州市为例

合理的规划和建设城市应急避难场所可以增强城市抗灾能力,提高城市灾害韧性,降低灾害带来的人员伤亡和财产损失。在对兰州市应急避难场所的建设现状进行详细调研的基础上,利用ANP-SWOT模型对其发展规划进行分析。首先运用SWOT分析方法确定兰州市应急避难场所未来发展的内部优势和劣势、外部机会和威胁;其次运用ANP分析法构建兰州市应急避难场所发展规划的网络层次结构,结合专家咨询,通过赋值和对比分析确定最佳发展策略。结果显示,分布不均、数量不足、尚未形成专门的应急预案是制约兰州市应急避难场所发展的关键问题;最佳发展策略是加快推进兰州市应急避难场所的标准化规范化。     

On the entrainment in cumuli — A contribution to a case study

Summary The case study presented here is related to the thermodynamic analysis of entrainment and mixing in a shallow cumuls layer. The fair weather situation on 9. 9. 1983, Voves, is characterized by a field of scattered cumuli of the same depths and by a towering isolated cumulus. The clouds were sampled. Two types of analysis were used, the Paluch analysis and saturation point analysis, both of them making use of conserved parameters and a mixing line structure. Both methods gave similar results. For the small cumuli, lateral entrainment prevailed up to the highest penetration level while in the isolated cumulus, cloud top entrainment was the dominant mixing mechanism.

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Evidence of geomagnetic storm effects in the lower atmosphere: A case study

Disturbances produced by geomagnetic storms in the higher regions of the Earth’s atmosphere, such as in the ionospheric F2 region and in the lower ionosphere, are relatively better known than those produced at lower altitudes, where the effects of geomagnetic storms have been little studied. During magnetically perturbed conditions, some changes in pressure and temperature at high latitudes have been observed, from the surface level to heights of around 30 km, but there are no morphological studies and/or patterns of behavior. Moreover, the physical mechanisms are still unknown and what exists is a matter of controversy. Thus, the aim of this paper is to contribute to the vertical profile of the effects of geomagnetic storms as observed in the lower sectors of the atmosphere. For that, we study the variations of two atmospheric parameters (temperature and wind speed) during an intense geomagnetic storm (minimum Dst = −300 nT), at heights between about 6 km and 20 km. The data used were obtained from weather balloon flights carried out at low, mid and mid-high latitudes in different longitudinal sectors of the northern hemisphere, which took place twice per day: 00:00 and 12:00 UT. Small, but statistically significant changes in temperature and in zonal component of the neutral winds are observed at mid-high latitudes, which can be linked to short-term geomagnetic forcing. However, the results show different atmospheric response to the geomagnetic storm in the different longitudinal sectors at tropospheric and stratospheric levels, which suggests a regional character of the geomagnetic storms effects at tropospheric levels.     

Reducing sewage pollution in the Antarctic marine environment using a sewage treatment plant

Despite Antarctica being the largest pristine wilderness on Earth, many coastal Antarctic research stations release untreated sewage waste into the marine environment, which may have negative effects on local wildlife. In February 2003 a sewage treatment plant was installed at Rothera Research Station (Adelaide Island, Antarctic Peninsula). After one year of operation the sewage treatment plant had dramatically reduced the microbiological pollution in the near-shore marine environment around the outfall and seawater quality conformed to European Union Bathing Water Standards.     

A case study of the influx of upper mantle fluids into the crust

Geochemical and geophysical investigations in the Bohai Gulf and adjacent areas, China, indicate that uplift of the high-conductivity layer in the lithosphere coincides with the area of high heat flow. In this area are distributed abundant oil and gas fields in a Tertiary fault basin and also large quantities of basaltic rocks. Gas fields, mostly CO₂ bearing, occur at the basin margins, where a widespread alkaline olivine basalt has high contents of gold. Geochemical prospecting of the surface (soil and soil gas) in the area indicates that there is an anomaly zone of large-scale gold mineralization, and large gold deposits have been found in this area. Isotopic study demonstrates that CO₂ in the volcanic rocks and in the CO₂-bearing gas deposits are all derived from the mantle. Experiments show that Au- and CO₂-bearing hydrothermal fluids separated into vapor phase and liquid phases respectively due to a reduction of pressure and temperature over the temperature range from 250 to 290°C and at 22 M Pa. Au appears in the vapor phase rich in CO₂. That proves that it is possible that CO₂-bearing aqueous fluids (in gas phase) can carry gold and transport it from deeper parts of lithosphere to the surface.     

A case study:cross-well acoustic tomography in Fuyu oil-field

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Sediment budgeting: A case study in the Katiorin drainage basin,Kenya

The primary objective of this study was to compute a detailed budget for a small semiarid tropical drainage basin in Kenya. Results indicated that transfer of sediments (‘inputs’) from primary source areas was minor in comparison to changes in storage. The major sediment source area within the Katiorin drainage basin was the colluvial hillslope zone. The net change in storage within this zone was approximately 2100 Mg yr^?1. Surface wash and rilling were the dominant transport processes responsible for the remobilization of colluvial sediments. Sediment storage within the in-channel reservoir increased by 60 Mg yr^?1, which was minor when compared to the total store of sediment in this reservoir. During 1986, the channel network stored only a small fraction ( < 3 per cent) of the sediment delivered from the hillslope subsystem. Therefore, the in-channel reservoir had limited influence on sediment conveyance to the basin outlet. These data indicate that a static equilibrium condition cannot be assumed within the Katiorin drainage basin. Such an assumption would result in erosion estimates of approximately 5.5 mm yr^?1 for the entire basin (based on a sediment output of 7430 Mg km^?2 yr^?1 and a measured bulk density of 1.35 Mg m^?3). However, this masked the actual rates of 1.2 to 7.1 mm yr^?1 in subbasin primary source areas, and rates of 0.6 to 17 mm yr^?1 for colluvial material in the various subbasins. The extreme accelerated erosion rates resulted from minimal ground vegetation, steep slopes, soil crust formation, an erodible substrate, and a well-integrated drainage network for rapid conveyance of sediments from the hillslope subsystem to the basin outlet.     

A case study of a dust storm weather situation in the Sudan in April 1973

Summary In connection with an invasion of cold air from the north over the Sudan in April 1973, a major dust storm or rather, a dust storm complex, passed over most of the Sudan.The weather development during this dust storm period is described and illustrated in detail with the aid of synoptic weather and visibility maps, as well as time sections based on SYNOP, METAR, and radiosonde reports from Sudanese meteorological stations.With the aid of the synoptic maps it has been possible to follow the development and movement of the dust storm complex and its relation to the cold fronts preceding the cold air invasion, to the intertropical front (ITF), and to thunderstorm highs which developed within the monsoon air south of the ITF during the initial stage. It was also possible to follow the latitudinal displacements of the ITF, which were caused by the weather systems and associated pressure changes in the harmattan and the monsoon air masses on both sides of it.At the beginning of the dust storm the cold fronts from the north were fairly distinct, but they gradually lost their frontal character. The cold air advection, however, gave rise to increased instability in the lower atmospheric layers, which facilitated the development of dust storms. Eventually the cold fronts merged with the ITF, which, on the other hand, constituted a sharp demarcation line between the harmattan and the monsoon air masses during the whole period, particularly with regard to the air borne dust. From the time sections and the synoptic maps it is evident that the discrepancy in concentration of air borne dust was very sharp along the ITF, particularly during the latter part of the dust storm period. When the ITF slowed down and eventually approached its southernmost position and, simultaneously, the cold air invasion ceased, the dust accumulated in part in the southeastern areas and was in part drained out of the Sudan to the southwest, passing the Central African Republic.     

电离层对台风响应的全过程的特例研究

作为特例研究,本文对1988年和1990年两次强台风影响期间的电离层多普勒记录及相应的台风资料进行了细致的相关分析,目的是利用多普勒记录的连续性优点来了解电离层对登陆（或近海）强台风通过声重波响应的演化全过程.分析表明,在这两次台风影响期间,电离层形态中除有明显的波状扰动（中尺度声重波）出现外,还有一些值得注意的新现象：波动的时间演化表现出明显的幅度逐渐增加以及频率由高频向低频转变,在振幅很大的情况下日落后同时出现扩展F（Spread-F）现象,显示了声重波在激发电离层不规则结构方面的种子作用.这一演化过程与电离层中TIDs的线性传播理论一致,文中开展了对这一现象的非线性数值模拟,模拟结果基本上也与上述观测现象相吻合.     

Contribution to the study of phosphate ion desorption during the dilution of urban sewage outfalls in the marine environment

The study of continental effluents discharged into the marine environment has enabled us to show that phosphate ion concentration does not follow the linear law of dilution exhibited by a true solution. We were able to show that the dilution of sewage in seawater allows the particles and colloids to desorb phosphate ions, thus increasing the amount of already dissolved inorganic phosphate.     

吉林陨石中铁镍合金的磁学性质

铁镍合金是陨石中重要的磁性物质,其中铁纹石、镍纹石和四方镍纹石是球粒陨石中的主要铁镍合金.然而.迄今针对陨石中铁镍合金的磁学性质研究仍非常缺乏.本文研究了吉林陨石中的铁纹石、四方镍纹石、以及陨硫铁的磁学特征.实验表明,镍含量为6％～7％的铁纹石是该陨石中最主要的铁镍合金物质,它具有低矫顽力和高的热稳定性,居里温度～750℃.镍含量为～48％的四方镍纹石具有高矫顽力和高的热稳定性,居里温度～565℃,它是剩磁的主要载体.陨硫铁在室温为反铁磁性,不具有载剩磁能力,在60 K左右存在一个低温转换,在氩气中加热较稳定而在空气中加热被氧化转化为磁铁矿.这些研究结果为鉴定球粒陨石中的磁性物质提供了依据.     

A case study of the impact of cyclonic trajectories on sea-level extremes in the Gulf of Finland

Modelling of water levels in the Baltic Sea, aimed at evaluating the influence of the trajectories and propagation speeds of a deep idealized cyclone on sea-level extremes in the Gulf of Finland, is done using the hydrodynamic model BSM6. An analytical expression for determination of the atmospheric pressure in this cyclone takes into account the existence of the cold front and the time evolution of the cyclone intensity. The empirical parameters in this relation are based on those of the deep cyclone ‘Erwin’ which passed over the Baltic Sea region in 2005.