伊犁河伊宁市段水质污染特征分析

在对伊犁河伊宁市段历年水质状况进行综合评价的基础上,探讨了城市河段水质的变化规律、污染特征和成因。     

Sorption of organic contaminants by biopolymers: role of polarity, structure and domain spatial arrangement

Sorption behavior of hydrophobic organic contaminants (HOCs) (i.e., pyrene, phenanthrene and naphthalene) by native and chemically modified biopolymers (lignin, chitin and cellulose) was examined. Lignins (native and treated) showed nonlinear sorption for all compounds studied, emphasizing their glassy character. Chitins and celluloses had linear isotherms for phenanthrene and naphthalene, illustrating the dominance of partitioning, while pyrene yielded nonlinear isotherms. Sorption capacity (K(oc)) of HOCs was negatively correlated with the polarity [(O+N)/C] of the biopolymers. Aromatic and alkyl+aromatic C percentages, rather than alkyl C content, demonstrated a better correlation with K(oc) values, indicating the importance of aromatic structures for HOC affinity. Hydrophobicity (K(ow))-normalized K(oc) values decreased sharply with increasing percentage of O-alkyl C versus total aliphatic C (O-alkyl C/total aliphatic C) or with polar C/(alkyl+aromatic C) ratio of the biopolymers until their values reached 80% and 4, respectively, illustrating the effect of surrounding polar groups on reducing affinity for HOCs. Overall, the results of this study highlight the role of spatial arrangement of domains within biopolymers in sorption of HOCs, and point to sorbent properties, such as functionality, polarity and structure, jointly regulating the sorption of HOCs in biopolymers.     

Zinc and cadmium accumulation and tolerance in populations of Sedum alfredii

To investigate the variation of Zn and Cd accumulation and tolerance of Sedum alfredii (a newly reported Zn/Cd hyperaccumulator), field surveys and hydroponic experiments were conducted among three populations of this species: two originating from old Pb/Zn mines in Zhejiang (ZJ) and Hunan (HN) Provinces and one from a "clean" site in Guangdong (GD) Province, China. Under field conditions, up to 12,524 and 12,253 mg kg(-1) Zn, and 1400 and 97 mg kg(-1) Cd in shoots of ZJ and HN plants were recorded respectively. Under hydroponic conditions, ZJ and HN plants accumulated significantly higher Zn and Cd in their leaves and stems, and possessed significantly higher Zn and Cd tolerance than GD plants. Among the two contaminated populations, ZJ plants showed higher Cd tolerance and accumulation (in leaves) than HN plants. The present results indicate that significant differences in Zn and Cd accumulation and tolerance exist in populations of S. alfredii.     

Remediation of soil contaminated with pyrene using ground nanoscale zero-valent iron

The sites contaminated with recalcitrant polycyclic aromatic hydrocarbons (PAHs) are serious environmental problems ubiquitously. Some PAHs have proven to be carcinogenic and hazardous. Therefore, the innovative PAH in situ remediation technologies have to be developed instantaneously. Recently, the nanoscale zero-valent iron (ZVI) particles have been successfully applied for dechlorination of organic pollutants in water, yet little research has investigated for the soil remediation so far. The objective in this work was to take advantage of nanoscale ZVI particles to remove PAHs in soil. The experimental factors such as reaction time, particle diameter and iron dosage and surface area were considered and optimized. From the results, both microscale and nanoscale ZVI were capable to remove the target compound. The higher removal efficiencies of nanoscale ZVI particles were obtained because the specific surface areas were about several dozens larger than that of commercially microscale ZVI particles. The optimal parameters were observed as 0.2 g iron/2 mL water in 60 min and 150 rpm by nanoscale ZVI. Additionally, the results proved that nanoscale ZVI particles are a promising technology for soil remediation and are encouraged in the near future environmental applications. Additionally, the empirical equation developed for pyrene removal efficiency provided the good explanation of reaction behavior. Ultimately, the calculated values by this equation were in a good agreement with the experimental data.     

灾难事件后继风险决策

对小概率/高风险的灾难事件的后继风险决策进行探讨,着重在决策的认知神经经济模型框架下,讨论灾难事件后继风险决策的影响因素。灾难事件后人们的风险觉知、信念和假定、经验等认知因素以及灾后情绪因素对于决策分别有不同的影响;人们灾后决策的特点为决策更多直觉化而较少运用理性分析;灾难后继决策有随时间变化的趋势,灾难事件后人们为寻求安全感而出现"损失偏差"(loss bias),该偏差在"获得"和"损失"两种条件下的影响是不同的。灾后风险决策的内在机制或可用思维和决策的双加工系统(dual-process)模型来解释。最后展望了灾难事件后继决策进一步的研究方向。     

基于社会科学统计程序(SPSS)回归性分析的尾矿库事故预测模型

基于社会科学统计程序(SPSS)软件的分析功能,对调查研究中获取的尾矿库案例进行数据提炼和分类编码,找出相关因子并进行回归性分析。最终目的是找出尾矿库各个因素的内在联系,建立简单的尾矿库事故模型,从而可以初步预测尾矿库事故发生的可能性。该预测模型为尾矿库事故的研究提出了新方法,对于防灾减灾以及保护人民生命财产安全起到了积极作用。     

废塑料处理技术进展与展望

文章介绍了解决废塑料污染的几种方法,分析了目前我国废塑料回收利用技术的现状,并介绍作者在这方面进行的一些新的研究工作：（1）使用自制的催化剂完成了聚烯烃类塑料催化热解回收燃料油的小试,获得了较好的效果;（2）通过实验对发泡聚苯乙烯热解回收苯乙烯单体的工艺流程提出了优化操作条件。根据国内外实际,文章最后对废塑料回收利用提出了几点建议。     

预测有机化合物对水蚤EC50值的片段常数法

根据217种化合物建立了估算有机化合物对水蚤EC50值（48h半数影响浓度）的片段常数模型,分析了模型的误差及稳健性。研究结果表明,有机化合物的片段常数和结构因子与水蚤的EC50值倒数的对数（lg1/EC50)显著相关,可以根据片段常数法估算有机化合物对水蚤的EC50。模型的可决系数为0.9687,平均绝对误差0.40个对数单位,其中68.7%化合物的误差小于0.5个对数单位。     

峡山地不同垂直带土壤层的水文功能及其影响因子

渗透性能和持水能力是土壤重要的水力学性质,是土壤调节径流、保持水土和涵养水源等水文功能的基础。以三峡库首的夷陵-大老岭山地为对象,采集亚高山棕壤针叶林地、中山黄棕壤针阔混交林与茶园地和低山黄壤针叶林地等4个样点剖面的土壤样品,在室内进行土壤饱和导水率、水分特征曲线和理化性质测定,量化了不同样地土壤渗透性能、持水能力和水分库容等水文功能参数,并明确了其主要影响因子。结果表明: 研究区山地土壤饱和导水率在0.06～14.78 mm/min之间,亚高山棕壤和中山黄棕壤林地土壤渗透性能较好,其平均饱和导水率在7.15～14.78 mm/ min之间,低山黄壤次之（1.3 9 mm/min）,中山黄棕壤茶园土壤渗透能力最差（1.17 mm/min）。不同类型土壤的饱和含水量、毛管含水量、田间持水量存在较大差异,凋萎含水量差异较小。同一类型土壤的不同发生层内,土壤饱和含水量随土壤深度的增加而递减,毛管持水量和田间持水量随土层深度的增加波动上升。不同样地间土壤水分总库容差异较大,随着海拔的升高,土壤水分总库容增加。土壤水分特征参数与土壤性质的相关分析表明,饱和导水率与土壤总孔隙度呈显著正相关,与容重呈显著负相关;饱和含水量、毛管持水量、田间持水量均与土壤总孔隙度、粘粒含量呈显著性正相关,与容重呈显著负相关;饱和含水量与根系重量呈显著正相关;毛管持水量、田间持水量与砂粒含量呈显著负相关。与中山茶园地和低山黄壤林地相比,亚高山棕壤和中山黄棕壤林地渗透性能较好且持水性更强,具有更好的调蓄径流和涵养水源的水文功能。 关键词： 山地土壤;土壤孔隙度;饱和导水率;持水能力;三峡库区     

近期长江张家洲南水道强冲刷机理与趋势分析

2016年9月利用多波束测深仪调查了张家洲河段河床微地貌的高分辨率形态与分布特征,结合1998年和2013年水下地形资料,分析了三峡截流以来该河段河槽的冲淤变化与演变趋势。结果表明：（1）张家洲河段整体呈冲刷状态,净冲刷量17.2×10.6 m³。其中,张家洲南水道是强冲刷区,最大冲刷深度约9 m;（2）河槽表层沉积物中值粒径为149.1~226.3 μm,与历史资料相比呈粗化趋势;（3）张家洲河段约82.9％的主航道发育了沙波,约14.0％的主航道发育了冲刷坑与冲刷槽,平床地形仅占3.1％。流域来沙量减少是张家洲河段整体冲刷的主要原因,而河流控制工程稳定了河势,迫使水流归槽,加剧了张家洲南水道的冲刷。随着流域来沙量持续减少,张家洲南水道主航道有可能进一步冲刷