重庆市特大旱灾的自然与社会机制分析

文章针对2006年的特大旱灾探讨了2006年的特大旱灾的特征,分析了2006年特大旱灾的形成自然机制和社会机制,并提出了今后重庆市抗御旱灾的策略。认为2006年的特大旱灾是自然因素与社会因素叠加的结果,是人类社会经济系统自身易损性的体现。     

电子元器件的腐蚀

电子元器件在大气环境下,因潮湿及其它条件下会发生大气腐蚀,从而导致其材料产生腐蚀,电子结构系统发生故障如短路、点接触不良等.本文简单论述了因空气污染、塑料和有机物分解气体等导致的电子元器件的大气腐蚀原理及原因.     

系统动力学复杂性及其在海洋生态学中的研究进展

海洋生态系统具有开放性、耗散性和非线性等特点,可以借助于系统动力学方法对其研究.系统动力学研究一个不可回避的问题就是系统动力学复杂性.本文在简单介绍几种常见的系统动力学模型及其复杂性问题的基础上,系统阐述了当前系统动力学复杂性在海洋生物多样性的维持、海洋生态系统的物质循环、海洋生物群落结构稳定性、有害藻类的暴发、海洋污染物的扩散、海洋生态毒理动力学、海洋生物资源的开发与管理等方面的应用、研究进展及相关问题.在总结以上研究进展的基础上,本文对系统动力学复杂性在海洋生态学研究中的应用进行了展望.     

交通荷载作用下饱和软粘土孔压-应变分析模型

针对交通荷载的作用特点设计了循环三轴试验,进而对交通荷载作用下饱和软粘土的动力特件进行厂研究.结果表明:循环荷载作用下,饱和软粘土存在临界循环应力比,采用孔压曲线所得到的临界循环应力比要小于采用应变曲线所得到的临界循环应力比.当土样不存在初始剪应力时,随着循环次数的增加,土样的应力-应变关系曲线近似原点对称,但随着初始剪应力的增大,应力-应变关系曲线逐渐表现为一系列平行曲线,峰值孔压与循环孔压幅值均逐渐减少;同时,轴应变的发展加快,但循环应变幅值逐渐减小.当循环应力比小于临界循环应力比时,对于同一初始剪应力,不同循环应力比下的孔压比-动应变曲线近似集中在同一条曲线上.通过对试验数据进行回归分析,得到了交通荷载作用下饱和软粘土残余孔压-累积塑性应变关系模型.     

垃圾焚烧飞灰中重金属的分布规律及化学形态分析

研究了重庆市垃圾焚烧发电厂焚烧飞灰的粒径分布,分析了焚烧飞灰中重金属的含量、浸出特性和形态分布特征,讨论了不同粒径飞灰中重金属的分布特性.结果表明,大部分飞灰粒径集中在38～250 μm,其中粒径为38～100μm飞灰占总量的49.49%.飞灰浸出液中Pb和Zn的浓度均超出了<危险废物浸出毒性鉴别标准>(GB5085.3-2007),因此该焚烧飞灰被认定为危险废物.在＜250μm粒径范围内,Cd、Cr、Cu、Mn和Pb普遍表现出向小颗粒富集的趋势;Zn的粒径分布则与上述5种元素表现出相反的趋势;Ni的分布与粒径的相关性不大,在各粒径上的分布较均匀.除Ni元素外,用BCR法分析所得的其他6种重金属形态分析结果和总量测定的结果基本吻合.飞灰中Cr、Ni、Zn和Mn主要以稳定态存在,而Cd、Pb和Cu则主要以不稳定态存在.     

煤与瓦斯突出影响因素评价分析的模糊层次分析方法

在综合分析煤与瓦斯突出的影响因素的基础上,采用模糊层次分析法（FAHP）建立了煤与瓦斯突出模糊层次分析模型并进行了实例分析,确定了煤与瓦斯突出各影响因素的权重系数。评价结果表明：地应力、地质构造、瓦斯压力等是影响煤与瓦斯突出的主要因素。为制定相应的煤与瓦斯突出防治措施,提供了科学的理论依据和切合实际情况的评价方法。     

Emissions of SO2, NO and N2O in a circulating fluidized bed combustor during co-firing coal and biomass

This paper presents the experimental investigations of the emissions of SO2, NO and N2O in a bench scale circulating fluidized bed combustor for coal combustion and co-firing coal and biomass. The thermal capacity of the combustor is 30 kW. The setup is electrically heated during startup. The influence of the excess air, the degree of the air staging, the biomass share and the feeding position of the fuels on the emissions of SO2, NO and N2O were studied. The results showed that an increase in the biomass shares resulted in an increase of the CO concentration in the flue gas, probably due to the high volatile content of the biomass. In co-firing, the emission of SO2 increased with increasing biomass share slightly, however, non-linear increase relationship between SO2 emission and fuel sulfur content was observed. Air staging significantly decreased the NO emission without raising the SO2 level. Although the change of the fuel feeding position from riser to downer resulted in a decrease in the NO emission level, no obvious change was observed for the SO2 level. Taking the coal feeding position R as a reference, the relative NO emission could significantly decrease during co-firing coal and biomass when feeding fuel at position D and keeping the first stage stoichiometry greater than 0.95. The possible mechanisms of the sulfur and nitrogen chemistry at these conditions were discussed and the ways of simultaneous reduction of SO2, NO and N2O were proposed.     

Effects of long-term amendment of organic manure and nitrogen fertilizer on nitrous oxide emission in a sandy loam soil

To understand the effects of long-term amendment of organic manure and N fertilizer on N2O emission in the North China Plain, a laboratory incubation at different temperatures and soil moistures were carried out using soils treated with organic manure （OM）, half organic manure plus half fertilizer N （HOM）, fertilizer NPK （NPK）, fertilizer NP （NP）, fertilizer NK （NK）, fertilizer PK （NK） and control （CK） since 1989. Cumulative N2O emission in OM soil during the 17 d incubation period was slightly higher than in NPK soil under optimum nitrification conditions （25℃ and 60% water-filled pore space, WFPS）, but more than twice under the optimum denitrification conditions （35℃ and 90% WFPS）. N2O produced by denitrification was 2.1-2.3 times greater than that by nitrification in OM and HOM soils, but only 1.5 times greater in NPK and NP soils. These results implied that the long-term amendment of organic manure could significantly increase the N2O emission via denitrification in OM soil as compared to NPK soil. This is quite different from field measurement between OM soil and NPK soil. Substantial inhibition of the formation of anaerobic environment for denitrification in field might result in no marked difference in N2O emission between OM and NPK soils. This is due in part to more rapid oxygen diffusion in coarse textured soils than consumption by aerobic microbes until WFPS was 75% and to low easily decomposed organic C of organic manure. This finding suggested that addition of organic manure in the tested sandy loam might be a good management option since it seldom caused a burst of N2O emission but sequestered atmospheric C and maintained efficiently applied N in soil.     

盾构隧道施工对邻近建筑物差异沉降与扭曲变形影响分析∗

针对盾构隧道施工侧穿既有建筑物问题,结合南京地铁一号线北延段工程,以盾构隧道侧穿某浅基础建筑物为研究对象,通过对建筑物沉降实测数据进行分析,并利用Plaxis 3D 软件建立数值模型,研究了隧道距建筑物不同水平距离和盾构以不同角度穿越对建筑物差异沉降与扭曲变形特征的影响。结果表明：随着盾构开挖面逐渐接近建筑物,建筑物差异沉降及扭曲变形逐渐增大;差异沉降量在盾构机通过时达到最大值,之后趋于稳定,而扭曲变形峰值出现在盾构开挖面到达建筑物中点截面位置时,随后逐渐减小;当建筑物中心至隧道轴线的水平距离与隧道外径之比L/D=0.5~2 时,建筑物差异沉降量较大,在L/D=1.5 时达到峰值;当盾构穿越夹角从θ=0°增大至θ=90°时,建筑物最大差异沉降量不断增加,而最终扭曲变形值则先增大后减小,在θ=45°时扭曲变形达到峰值。研究结果可为盾构隧道侧穿浅基础建筑物时相关类似工程提供参考。     

环洱海地区气候变化特征研究

环洱海地区是云南省具有高原湖泊生态脆弱区、民族文化多元融合区和乡村经济发展活跃区等多重叠合特征的典型区域,是全球气候变化影响的敏感区和脆弱区。以环洱海地区1951~2014年6个基本站点的逐年平均气温、极端最高气温、极端最低气温、降水量、最大日降水量和日降水量≥0.1 mm日数资料为基础。采用线性倾向估计、Mann-Kendall趋势检验、Morlet小波分析和R/S分析等方法,研究了环洱海地区气候变化规律。结果发现:自1951年以来,环洱海地区年均气温和极端最低气温呈现出升高的趋势,而极端最高气温则呈现降低的趋势,变化速率分别为0.07℃/10 a、0.03℃/10 a和–0.14℃/10 a,对于年降水量、最大日降水量和降水日数而言,三者均为减少趋势,速率分别为–12.85 mm/10 a、–1.09mm/10 a和–1.73 d/10 a;环洱海地区年均气温、极端最高和极端最低气温均没有发生突变,年降水量和降水日数在2010年发生了一次减少突变,而最大日降水量则没有检测到突变的年份;环洱海地区年平均气温和年降水量在长时间尺度上的周期性变化最为显著,分别存在30 a和33 a左右的周期变化,并贯穿整个研究时段,而短时间尺度上的周期变化局域性特征突出;从未来演变趋势来看,年平均气温和极端最低气温将维持升温趋势,而极端最高气温则将持续降低趋势,年降水量继续减少的趋势未来将会逆转,但最大日降水量和降水日数两者将持续减少的概率更大。