基于生态足迹方法的武汉市自然资本分析

生态足迹方法是目前研究自然资本状况的常用方法之一,能够较好地体现区域可持续发展态势.文章运用生态足迹方法对武汉市1995年、2000 年、2005年自然资本消长情况进行了量化研究、对比分析,研究结果表明:武汉市1995年、2000 年、2005年的自然资本需求和供给比例分别达到18.402∶1、20.765∶1、27.276∶1,供需矛盾显著;人均生态赤字分别达到2.4206 hm2·人-1、2.5163 hm2·人-1、2.9009 hm2·人-1,呈逐年上升趋势,成为制约武汉市可持续发展的瓶颈之一.生态用地类型分析显示,耕地、水域、化石能源用地赤字明显,应作为武汉市改善自然资本状况重点关注的对象.文章提出了倡导市民合理消费,同时健全绿色保障制度体系、优化城市生态服务功能等对策和措施,旨在为武汉市实现可持续发展提供依据.     

黄河源区生态破坏现状及保护对策

黄河源区自然条件严酷,生态环境脆弱。随着黄河源区资源开发力度逐步加大,草场和灌丛植被遭到不同程度的破坏,生态环境日趋恶化。具体表现为草原退化严重,水土流失加剧,土地荒漠化扩大,水源涵养能力大为降低。因此,保护黄河源区生态环境,建立黄河源头特殊生态功能保护区已刻不容缓。     

微生物易利用基质对PCP厌氧降解的影响

本文主要研究了微生物易利用基质对厌氧反应器内ＰＣＰ厌氧降解性及处理效率的影响，结果表明，ＰＣＰ对厌氧污泥代谢葡萄糖有抑制作用，则适量的微重复铁利用基质有利于促进ＰＣＰ的脱氯和降解代谢，且随着反应器进水中水中ＰＣＰ的提高，达到相近降解效率所需的微生物易利用基质的需要量也相应增加；废水中ＰＣＰ剩余量和废水中糖的初始浓度呈显著负相关。     

液相催化氧化吸收烟气中SO_2的研究

本文报告了水溶液催化氧化吸收烟气中的SO_2对各种因素,包括催化剂浓度和种类、反应温度、SO_2浓度和烟气流量,以及烟气中氧气含量和反应后溶液中SO_3~(2-)和SO_4(2-)浓度与催化剂浓度的定量关系进行了研究。当催化剂浓度为0.05mol/l,SO_2浓度1000—2000ppm,温度25℃时,SO_2吸收率85％以上。并初步讨论了液相催化氧化吸收SO_2反应机理。     

Low-reactive circulating fluidized bed combustion (CFBC) fly ashes as source material for geopolymer synthesis

In this contribution, low-reactive circulating fluidized bed combustion (CFBC) fly ashes (CFAs) have firstly been utilized as a source material for geopolymer synthesis. An alkali fusion process was employed to promote the dissolution of Si and Al species from the CFAs, and thus to enhance the reactivity of the ashes. A high-reactive metakaolin (MK) was also used to consume the excess alkali needed for the fusion. Reactivities of the CFAs and MK were examined by a series of dissolution tests in sodium hydroxide solutions. Geopolymer samples were prepared by alkali activation of the source materials using a sodium silicate solution as the activator. The synthesized products were characterized by mechanical testing, scanning electron microscopy (SEM), X-ray diffractography (XRD), as well as Fourier transform infrared spectroscopy (FTIR). The results of this study indicate that, via enhancing the reactivity by alkali fusion and balancing the Na/Al ratio by additional aluminosilicate source, low-reactive CFAs could also be recycled as an alternative source material for geopolymer production.     

Enhancement of turbulent scalar mixing and its application by a multihole nozzle in selective catalytic reduction of NOx

The mixing characteristics of a passive scalar in the turbulent flow of a selective catalytic reduction process were numerically and experimentally investigated, focusing especially on an injection nozzle with multiple holes for the reducing agent. The multihole injection nozzle studied has six holes that are perpendicular to the ambient flue gas flow and are located near the tip of the nozzle. Large eddy simulation was applied to the turbulent flow and mixing fields to elucidate the mixing mechanism of the proposed nozzle compared with the single-hole nozzle that is commonly used in the conventional selective catalytic reduction process. From the results, there exist broader regions of higher turbulent intensities for the multihole nozzle than for the conventional single-hole nozzle. These regions are well matched with the positions of high vorticity in the near upstream region of the jet flow issuing from the multiple holes of the nozzle. Consequently, the high turbulent intensities and vorticity magnitudes lead to intensified mixing between the flue gas and the reducing agent. Hence, the most suitable molar ratio between NOx and the reducing agent for the catalytic reaction can be easily obtained within a shorter physical mixing length as a result of the enhanced scalar mixing. Finally, the numerical results were applied to a trial design version of a multihole nozzle, and this nozzle was experimentally tested to confirm its mixing performance.     

Estimation of waste generation from floods

A framework of correlation for estimating the amount of waste generation from floods is developed. Flood waste data were collected from four recent typhoons in Taiwan. Parameters affecting the flood waste are analyzed. Population density, flooded area and amount of total rainfall are chosen as the correlating parameters for the model development, and regression diagnostics are performed to check the validity of the collected data. The simple linear model is shown to be incapable of correlating the flood waste data. An exponential model is proposed and shown to give acceptable correlation with the flood waste data spanning five orders of magnitude. The model can be useful in the planning of waste cleanup after floods.     

Numerical Simulation of Synoptic Condition on a Severe Sand Dust Storm

By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm.     

提高节理面c和Ψ对岩坡开挖变形的影响

为了反映岩质边坡在节理面注浆后的变形效应,首先,通过室内试验,分析注浆前后岩体变形和破坏的全过程,以探讨其抗剪性能(粘结力c和内摩擦角Ψ)的变化;然后,基于理想弹塑性本构模型的Mohr-Coulomb准则,运用拉格朗日元数值方法(FLAC3D),对岩坡注浆前后变形效应(水平位移、垂直位移、剪应变增量)进行模拟.结果表明:注浆加固后,岩体的位移场变得均匀和连续,节理面处的较大位移受到抑制,边坡的整体性得到提高,有利于边坡的稳定性.     

滚石灾害研究现状及发展趋势

滚石是我国西部山区常见的一种地质灾害,它分布范围极广,发生突然,频率高,严重威胁其周围的人类以及各种构筑物.目前,国内外有关滚石的理论研究比较薄弱,以致滚石灾害的防治工作受到严重的影响.基于对国内外大量滚石灾害研究资料的分析,将其研究现状概化为滚石风险分析、滚石运动轨迹、滚石冲击力以及滚石防护等4个方面.据此对滚石研究的发展趋势进行了探讨,以便为滚石灾害的机理研究和治理提供参考依据.