利用SPAMS研究南宁市冬季单颗粒气溶胶化学成分

利用单颗粒气溶胶飞行时间质谱仪(SPAMS)对南宁市2015年冬季2月15~24日期间大气PM2.5进行观测.SPAMS所测得大气PM2.5数浓度与PM2.5质量浓度线性相关系数为0.76,在一定程度上颗粒物数浓度可反映大气污染状况.利用自适应共振神经网络分类方法(Art-2a)对PM2.5化学成分进行分类,确定PM2.5化学成分主要为元素碳、有机元素碳混合颗粒、有机碳、富钾颗粒、矿物质、富钠颗粒、二次无机颗粒、左旋葡聚糖以及其它重金属共9类.成分占比最高的是元素碳,其次是有机碳和富钾颗粒.监测到80%以上的PM2.5粒径主要集中在0.2~1.0μm之间,峰值出现在0.62μm处,各化学成分的粒径分布特征与总颗粒数粒径分布特征相似.各化学成分数浓度与PM2.5质量浓度随时间变化趋势较一致,化学成分数浓度占比变化在一定程度上可反映瞬时的污染来源.     

潜流人工湿地冬季运行的强化措施及效果分析

针对人工湿地在低温条件下处理效果较差的问题,为提高潜流人工湿地冬季运行效果。采用活性污泥挂膜和表面覆盖地膜的强化方式,开展冬季运行试验,分析试验人工湿地冬季运行经强化措施后的处理效果。结果表明,通过强化措施后,各指标平均去除效果都有较大提高,COD去除率由25%提升至49%、TN去除率由27%提升至45%、TP去除率由29%提升至51%。     

北京市典型绿化灌木阻滞吸附PM2.5能力研究

选取北京市典型绿化灌木物种大叶黄杨、小叶黄杨、紫叶小檗、矮紫杉,结合气室模拟与实地观测的方法,综合测定不同树种对PM2.5的吸附能力.同时,收集2012年12月~2013年5月间北京市区PM2.5浓度值,分析了北京市冬春季PM2.5污染特征.结果表明,由气室实验得到的4种植物对PM2.5阻滞吸附能力排序为:紫叶小檗>小叶黄杨>矮紫衫>大叶黄杨,其原因主要为叶片特征差异所致;室外测量结果表明,4种物种吸附能力排序为:小叶黄杨>紫叶小檗>矮紫衫>大叶黄杨.气室模拟与室外实测结果均表明,小叶黄杨和紫叶小檗具有较强的阻滞吸附PM2.5的能力;气室模拟与室外观测实验中植物阻滞吸附PM2.5能力的大小略有差异,其原因应与植物结构相关.同时,通过分析北京市PM2.5浓度的季节性变化,发现北京市冬季的PM2.5浓度值尤为高,且常绿灌木植物仍能表现出较好的阻滞吸附PM2.5的能力.     

RELATIONS BETWEEN COLOR AND SOME LIMNOLOGICAL CHARACTERISTICS OF FLORIDA LAKES1

Data obtained from a limnological survey of 165 Florida lakes were analyzed to determine regional differences in lake color (Pt-Co units) and relations between color and various physical, chemical, and biological parameters. Average color measurements for the different lakes ranged from 0 to 416 Pt-Co units with individual measurements being as high as 600 Pt-Co units. With the exception of extreme south Florida, lake color concentrations were found to increase from north to south and from inland highlands to lowlands. Central Florida had the greatest heterogeneity in lake color because of an extremely diverse geology and physiography. Color was inversely related to Secchi disc transparency and positively related to total iron concentrations. Color was not strongly related to pH, total alkalinity, nutrients, chlorophyll a, and many other limnological parameters. Although lakes having color concentrations greater than 20 Pt-Co units can often be visually identified as colored lakes, the limnological processes in these are not necessarily different from those of lakes having clear water.     

Assessing Potential for Recovery of Biotic Richness and Indicator Species due to Changes in Acidic Deposition and Lake ph in Five Areas of Southeastern Canada

Biological damage to sensitive aquatic ecosystems is among the most recognisable, deleterious effects of acidic deposition. We compiled a large spatial database of over 2000 waterbodies across southeastern Canada from various federal, provincial and academic sources. Data for zooplankton, fish, macroinvertebrate (benthos) and loon species richness and occurrence were used to construct statistical models for lakes with varying pH, dissolved organic carbon content and lake size. pH changes, as described and predicted using the Integrated Assessment Model (Lam et al., 1998; Jeffries et al., 2000), were based on the range of emission reductions set forth in the Canada/US Air Quality Agreement (AQA). The scenarios tested include 1983, 1990, 1994 and 2010 sulphate deposition levels. Biotic models were developed for five regions in southeastern Canada (Algoma, Muskoka, and Sudbury, Ontario, southcentral Québec, and Kejimkujik, Nova Scotia) using regression tree, multiple linear regression and logistic regression analyses to make predictions about recovery after emission reductions. The analyses produced different indicator species in different regions, although some species showed consistent trends across regions. Generally, the greatest predicted recovery occurred during the final phase of emission reductions between 1994 and 2010 across all taxonomic groups and regions. The Ontario regions, on average, were predicted to recover to a greater extent than either southcentral Québec or the Kejimkujik area of Nova Scotia. Our results reconfirm that pH 5.5–6.0 is an important threshold below which damage to aquatic biota will remain a major local and regional environmental problem. This damage to biodiversity across trophic levels will persist well into the future if no further reductions in sulphate deposition are implemented.     

黄河三角洲附近海域浮游动物多样性研究

以文献资料和定性调查相结合的方法，综合分析了黄河三角洲附近海域浮游动物物种多样性；以定量调查结果，探讨了浮游动物多样度以及与均度、单纯度之间的关系。结果表明： 该海域浮游动物物种占中国海的５－７ ％ ，占渤海的５１－７％ ；浮游动物多样度在０－１０ ～２－２８ 之间，均度在０－０２～０－９７ 之间，单纯度在０－１４ ～０－９９ 之间；多样度与均度呈显著的正相关，与单纯度呈显著的负相关。     

冬小麦灌溉减损经济效益的初步探讨

灌溉是获取作物高产的主要措施之一,灌溉减损经济效益与农民收入和生产经济效益密切相关.提出了从灌溉次数和灌溉量参数入手,根据灌溉投入和灌溉减损量来分析灌溉减损效益、减灾效益和生产经济效益;以华北冬麦区单点试验和调查结果为例,讨论了该方法在冬小麦减灾评估应用中的普适性和可行性.     

1961-2000年干旱对我国冬小麦产量的影响

假定在目前条件下的冬小麦作物品种、耕种措施和土壤特性不变,利用WOFOST作物模型,模拟了1961-2000年干旱对我国冬小麦产量的影响。模拟结果显示:1961-1980年干旱对我国冬小麦产量影响较为严重,干旱使整个麦区冬小麦平均减产4．6%,使北方麦区冬小麦平均减产12%。1981 -2000年,干旱对冬小麦产量的影响明显减轻。总体上,1961-2000年虽然冬小麦生育期内降水量持续减少,但干旱对冬小麦产量的影响没有加重的趋势。通过分析发现,我国北方地区冬小麦生育期内的降水和干旱与产量并没有显著相关关系,但春季降水和干旱则与产量显著相关,揭示了我国北方春季降水量对冬小麦产量影响的重要性。     

冬小麦旱灾风险评价的指标体系构建及应用——基于2009年北方春旱野外实地考察的认识

2009年2月初,我国北方冬麦区遭受了数十年未遇的严重干旱。基于野外实地考察,判断本次干旱对冬小麦造成的实际影响比气象统计与遥感监测结果要轻,同时因纬度、地貌类型、微地貌和田间管理水平的不同而呈现出明显的区域差异。在此基础上,提出应在已有的旱灾致灾指标（气象干旱）基础上,综合考虑地带性、地貌、水库等孕灾环境指标和田间管理水平等灾害适应指标来构建冬小麦旱灾风险的综合评价指标体系。并以北方冬麦区为例,选取SPI、地貌类型、DEM和水库缓冲区等指标得到的旱灾综合风险等级与实际旱情存在较高的吻合性。研究可为高风险区的冬小麦旱灾风险防范提供理论依据和案例支撑。     

Number concentration and size distributions of submicron particles in Jinan urban area： Characteristics in summer and winter

The aerosol number concentration and size distribution were measured with the newly developed Wide-range Particle Spectrometer in summer and winter of 2006 at the urban site of Jinan City.Here reported the characteristics of fine particles of the different observation seasons.Relative high number concentrations for the particles in the diameter range of 10-500 nm were observed in both seasons.It was found that the dominant number distributed in particle diameter smaller than 100 nm and the percentage over the number concentration of all air particles is much higher than what has been measured in other urban sites over the world.The number mean diameter in summer was much smaller than in winter,strongly suggesting the different origin of ultrafine particles in different seasons.That is, particles in ultrafine mode mainly came from nucleation and new particle formation in summer while from traffic emission in winter. The diurnal variation also supported this point.Number concentration in the diameter range of 10-200 nm got their peak values at noontime,well correlated with the mixing ratio of SO_2 and the intensity of solar radiation in summer.While in winter,those in the same diameter range showed the main peaks during the traffic hours happened in the morning and evening.