鄱阳湖水体颗粒物对3种典型藻类的生长及絮凝作用

研究了鄱阳湖水体颗粒物对3种典型藻类的生长及絮凝作用.以铜绿微囊藻(蓝藻)、四尾栅藻(绿藻)和菱形藻(硅藻)为研究对象,鄱阳湖采集沉积物为悬浮颗粒物,利用500 m L玻璃锥形瓶作为小型、光照均一体系,于此体系中研究了颗粒物对藻类生长的影响,使用混凝试验搅拌仪分别研究了颗粒物粒径、浓度和体系p H对颗粒物絮凝沉降藻细胞的影响.在小型光照均一体系中,20 mg·L-1(鄱阳湖悬浮颗粒物低浓度)和80 mg·L-1(鄱阳湖悬浮颗粒物高浓度)颗粒物对3种藻类的生长影响均较小.在颗粒物投加量为0.02 g·L-1时,60~300目颗粒物均促进藻类的絮凝沉降,并且随着颗粒物粒径(D50)的增大,藻细胞的絮凝沉降效率逐渐减小,而且粒径在1~25μm部分的颗粒在此过程中占主导地位.当颗粒物投加量由0.02 g·L-1升至1.28 g·L-1时,3种藻的絮凝沉降效率随之提高.在颗粒物投加量为0.02 g·L-1时,铜绿微囊藻、四尾栅藻和菱形藻的絮凝沉降效率仅为11.08%、15.87%和7.50%,当颗粒物浓度升至1.28 g·L-1时,3种藻的絮凝沉降效率分别达42.33%、41.72%、28.98%.在p H值6~10范围内,随着p H升高,颗粒物对蓝藻、绿藻的絮凝沉降作用逐渐减小,絮凝沉降效率分别从p H为6时的36.10%、35.07%降到p H为10时的16.25%、12.59%;而对硅藻的絮凝沉降作用不明显.由此可见,鄱阳湖水体颗粒物影响藻类的絮凝沉降过程,使藻类的群落结构发生变化.     

The concept of the Portuguese National Ecological Reserve: constraints and impossibilities in the Azores Archipelago

The biophysical features of small islands (SI) distinguish them from other territories; isolation, small size and several anthropogenic pressures reduce the resilience of ecosystems and increase their vulnerability to global changes. Many SI have a shortage of infrastructures, institutions and technical/financial resources that hinder planning and require different integrated solutions. In Portugal, the National Ecological Reserve (NER) is legally binding for spatial planning instruments. It aims to defend natural values and areas of ecological value, or sensibility, or susceptible to natural hazards. However, the criteria for the design of NER are strictly set for mainland territory, not taking into account specific features of small islands. A case study of the Azores Archipelago is used to demonstrate that spatial planning instruments should be adapted to island contexts. Such adaptation will increase the effectiveness of their implementation in relation to the protection of natural resources, stability of biophysical structures and prevention of natural hazards. Observing the main differences between mainland and the Azores Archipelago it is possible to define a methodological transposition of the NER aims and goals into an island context. This approach is an answer to the constraints in effective adaptation of spatial planning instruments for islands.     

有机化合物生物富集因子的计算机预测研究

有机化合物在生物体内的富集,通常用生物富集因子(bioconcentration factor,简称BCF)来表达,这是化合物生态环境毒性评估的重要指标。为合理预测有机化合物是否易于生物富集,首先从美国环保局网站收集了624个具有不同BCF值的化合物,然后采用7种分子指纹结合5种机器学习方法(包括支持向量机、C4.5决策树、k最近邻法、随机森林法和朴素贝叶斯法),构建了化合物BCF的分类预测模型,所有模型均采用独立外部验证集进行验证。其中,使用Chemo Typer分子指纹结合支持向量机方法得到的二分类模型,整体预测准确度最好,达到了85.4%。通过采用信息增益、频率分析等方法,进一步确定了化合物中易于引起生物富集的关键子结构,包括芳基氯、二芳基醚、氯代烷烃等。研究中所用到的方法为有毒化学品的生态风险评价提供了良好可靠的预测工具。     

公众对煤矿区地质灾害的感知与适应行为研究

煤矿区的地质灾害较为常见,而且随着开采时间的推移地质灾害问题日益严重。公众对煤矿区地质灾害的感知与适应行为直接与他们的生命财产相关,同时还关系到政策法规的制定。通过对煤矿区公众的问卷调查发现,公众对地质灾害的严重程度和灾害原因感知是比较准确的,但仍有相当比例的公众选择采取无效的紧急适应行为,有近三分之一的公众没有考虑采用迁移的适应行为。公众对煤矿区地质灾害适应行为的背后涉及利益相关方的博弈。     

“2014.5.10”云南怒江州福贡泥石流成因分析

2004年5月10日云南怒江州福贡县石月亮乡发生泥石流等地质灾害,造成人员、经济重大损失。分析了此次泥石流形成的条件,并着重探讨了天气学成因,结果表明:脆弱的地质环境、陡峻的迎风坡、便于集水、集物的地形地貌和丰富的松散物质是怒江贡山泥石流易发生的有利地质地貌条件;连续性累积降水及短时间暴雨的产生为泥石流提供了较好的水源条件;高原短波槽与孟加拉湾南支槽东移合并,中、低层槽前西偏南暖湿气流500 h Pa偏西北气流是形成怒江暴雨过程的大尺度天气环流背景;地面辐合线、干线、低层显著湿区、湿舌等是导致降水的中尺度系统;高能高湿的潜在不稳定及近地层的水汽辐合是暴雨发生的有利条件;多普勒雷达图10~20 d Bz分散的絮状回波、部分35 d Bz块絮状回波、卫星云图多絮状对流云、无强对流云团活动反映此次暴雨过程为非对流性暴雨。     

低分子量有机化合物对MnO_2和土壤氧化锰的还原溶解作用

为考察土壤锰氧化物的还原溶解行为,本文选取常见的根系分泌的8种有机酸(抗坏血酸、香草酸、柠檬酸、草酸、酒石酸、水杨酸、半胱氨酸和邻苯二甲酸)和1种酚类化合物(邻苯二酚),人工合成的Mn O2和5种富含氧化锰的土壤(广东徐闻的砖红壤、海南澄迈的砖红壤、云南昆明的砖红壤、浙江嵊县的红壤和江苏南京的黄棕壤),研究了有机化合物对氧化锰的还原溶解作用.结果表明,较低p H和较高温度有利于有机化合物对Mn O2的还原溶解.在p H 4.5—5.5和温度5—45℃范围内,不同有机化合物还原溶解Mn O2能力的大小顺序为:邻苯二酚半胱氨酸抗坏血酸香草酸柠檬酸草酸≈酒石酸水杨酸≈邻苯二甲酸.邻苯二酚、半胱氨酸和抗坏血酸对土壤中氧化锰也有较强的还原溶解能力.当5种土壤比较时,徐闻砖红壤中还原溶解出的锰量最高,其次为昆明砖红壤,嵊县红壤中还原溶解出的锰量最小.当有还原性有机化合物存在时徐闻砖红壤、昆明砖红壤和澄迈砖红壤中的氧化锰容易发生还原溶解反应,增加土壤中可溶态和交换态Mn2+的含量,并可能对植物产生锰毒害.     

Hydrogen peroxide (H2O2) requirement for the oxidation of crude oil in contaminated soils by a modified Fenton's reagent

The oxidation of soil organic matter (SOM) and total petroleum hydrocarbon were investigated in two soils at eight different hydrogen peroxide (H₂O₂) concentrations to determine the optimal H₂O₂ dosage for the efficient remediation of soils contaminated by crude oil with minimal SOM removal. In our study, H₂O₂ concentrations up to 1100 mM increased the SOM destruction up to 10%–15% in the two soils while no improvement of the crude oil removal efficiencies was observed. The results indicate that the destruction of SOM significantly limits the oxidation of crude oil because SOM might consume H₂O₂ more effectively than crude oil at H₂O₂ concentrations above 1100 mM. In addition, H₂O₂ concentrations higher than 1100 mM were not expected for both soils because of the extremely rapid H₂O₂ decomposition, and low H₂O₂ utilization, of both soils.     

Vertical distribution of aerosol optical properties based on aircraft measurements over the Loess Plateau in China

Vertical distributions of aerosol optical properties based on aircraft measurements over the Loess Plateau were measured for the first time during a summertime aircraft campaign, 2013 in Shanxi, China. Data from four flights were analyzed. The vertical distributions of aerosol optical properties including aerosol scattering coefficients (σ_sc), absorption coefficients (σ_ab), Angström exponent (α), single scattering albedo (ω), backscattering ratio (β_sc), aerosol mass scattering proficiency (Q_sc) and aerosol surface scattering proficiency (Q_sc^′) were obtained. The mean statistical values of σ_sc were 77.45 Mm^− 1 (at 450 nm), 50.72 Mm^− 1 (at 550 nm), and 32.02 Mm^− 1 (at 700 nm). The mean value of σ_ab was 7.62 Mm^− 1 (at 550 nm). The mean values of α, β_sc and ω were 1.93, 0.15, and 0.91, respectively. Aerosol concentration decreased with altitude. Most effective diameters (ED) of aerosols were less than 0.8 μm. The vertical profiles of σ_sc,, α, β_sc, Q_sc and Q_sc^′ showed that the aerosol scattering properties at lower levels contributed the most to the total aerosol radiative forcing. Both α and β_sc had relatively large values, suggesting that most aerosols in the observational region were small particles. The mean values of σ_sc, α, β_sc, Q_sc, Q_sc^′, σ_ab and ω at different height ranges showed that most of the parameters decreased with altitude. The forty-eight hour backward trajectories of air masses during the observation days indicated that the majority of aerosols in the lower level contributed the most to the total aerosol loading, and most of these particles originated from local or regional pollution emissions.     

长江流域沉积物中黑碳分布及其与多环芳烃的相关性研究

本文采用CTO-375法测定了长江流域主流及直流20个表层沉积物中黑碳的含量,探讨了沉积物中黑碳与粒度、总有机碳以及多环芳烃之间的关系。结果表明,长江流域沉积物中黑碳的含量范围在0.22~1.89mg/g之间,与粘土、粉砂及砂含量之间的相关性并不明显,说明粒度组成并不是控制BC分布的主要因素。BC与TOC之间的显著正相关性,表明BC与TOC有相似的来源,如人类活动、土壤流失。沉积物中BC与PAHs有较好的相关性,表明二者之间有相似的来源,同时也表明PAHs在研究区域沉积物中吸附主要由BC控制,这为研究多环芳烃在长江流域的环境归趋与影响因素等提供了新的信息。     

北运河流域(北京段)畜禽养殖污染现状及防治对策研究

畜禽养殖业产生的畜禽粪污对空气、土壤、地表水及地下水均会造成污染.调研了北运河流域(北京段)畜禽养殖业现状,分析了其污染空间分布及粪污处理方式,并提出了畜禽养殖存在的主要问题.结合国内外研究及北运河流域(北京段)概况,从布局、粪污处理、资金投入等方面提出了应对措施与建议,为环境管理部门开展畜禽养殖污染防治提供借鉴与参考.