大港地区大气颗粒物中多环芳烃分布及污染源识别的研究

多环芳烃（PAHs）是一类对人体危害较大的有机污染物。目前对大气环境中PAHs来源识别技术还处于探索与发展阶段。为了解天津大港油田地区大气环境中PAHs污染状况与来源,对天津市大港地区大气颗粒物中10种PAHs分布及污染源开展了调查。结果表明：大港地区10种PAHs总浓度平均为169ng/m3,比市区对照点的465ng/m³低63.7％,其中苯并（a）芘（BaP）平均浓度为13.6ng/m³,比市区对照点的41.1ng/m³低66.9％。实验结果经统计处理发现BaP浓度与其它9种PAHs浓度存在一定的相关性,相关系数均在0.60以上。利用比值法进行源识别得出：大港石化区PAHs主要来源为燃煤污染;而大港油田区PAHs主要来源为燃油污染。     

城市入河径流排放口总污染特征研究

流入城市雨源性河流的径流污染不容忽视,以我国南方典型城市深圳市的福田河流域为研究对象,经过18场典型降雨径流的测定,从污染过程线、径流初期效应识别和降雨事件平均浓度(EMC)等方面分析和讨论了城市河流入河径流排放口的总污染特征规律,有利于指导城市河流污染控制.结果表明,排放口地表径流浓度随时间变化历程中,COD、SS、TN、TP和BOD5普遍超出地表Ⅴ类水标准十多倍以上,某典型降雨场次的重金属(铬、镉、铜、砷和汞)污染较为严重,研究区排放口的浓度范围和平均值均高于重庆沙坪坝雨水口和加拿大Silerwood的雨水排放口,但低于武汉十里铺排放口.COD、SS、BOD5的初期效应尤为明显并且COD和SS冲刷强度较大,TN、TP初期效应不明显.COD、SS、TN、TP和BOD5的EMC浓度平均值分别为224.14、571.15、5.223、2.04、143.5 mg/L,在某种程度上,深圳市研究点的COD和SS的EMC值高于邻近的澳门、珠海,TN、TP值高于北京、广州、上海等城市,与国外的一些研究结果相比较,EMC值比韩国、美国及加拿大一些城市地表径流污染物浓度高得多,可见由排放口入河的径流总污染极其严重并需要治理.     

深冲钢板塑性变形形为研究

单相塑性材料的强度和塑性基本上是分别研究讨论的。此文以低碳深冲钢板为例,从能量观点出发,讨论了强度和塑性的内在制约关系,唯象地提出了单相塑性材料塑性破坏的判据,并解释了几个实验现象。此文的研究有助于加深对深冲钢塑性变形形为的理解。     

城市河道水质评价与研究

结合内梅罗指数法的原理,考虑金属毒性的积累效应,引入污染因子权重值,将权重值最大的评价指标纳入计算,采用改进的内梅罗指数法评价城市河道的水质污染状况。并对水质的划分标准临界值进行计算,以此作为评价水质污染状况的依据。研究结果表明,两种方法具有明显的差异,改进的内梅罗指数法对水质污染状况的评价结果较传统内梅罗指数法的辨识度更高,能够综合客观全面地体现城市河道水质状况,与真实情况较好的吻合,更为客观、合理。     

夏季渭河西安段溶解性有机质(DOM)的特征、分布及来源分析

通过紫外吸收光谱,三维荧光光谱结合平行因子分析(EEMs-PARAFAC)方法及主成分分析(PCA),研究了夏季渭河西安段水体中的溶解性有机质(DOM)的组成、来源,及其与水质指标的相关性.在研究区域共检出2种类别5个不同的DOM组分,分别为类腐殖质荧光组分C1、C2、C3、C5和1个类蛋白类荧光组分C4,5个组分具有...     

广州市农业环境污染及其对策

慨述了广州市农业环境污染状况，指出工业“三废”和城镇生活污水等外源污染是造成农业环境污染的主要因素，养殖业废水直接排放和频繁使用农用化学品也对农业环境造成一定程度的污染。提出了建立健全农业环境监控管理体系、推行农业生产许可制度、加强面源污染控制、推广无公害农产品生产技术、加大农业生态环境保护执法力度等污染控制对策。     

磷细菌筛选及其对苗期玉米生长的影响

从潮土、水稻土、砂姜黑土、石灰土上植物根际土壤和根中分离了86株磷细菌,通过NBRIP液体摇瓶培养3 d,培养液水溶磷质量浓度为4.2～387.3 mg.L^-1,水溶磷质量浓度与培养液pH呈显著负相关（r^2=0.621 6）。筛选出3株磷细菌进行玉米盆栽试验,结果表明,1株磷细菌处理的玉米干物质量和吸磷量与对照（处理4）相比无显著差异,2株磷细菌处理的玉米干物质量和吸磷量与对照相比有明显增加,干物质量增加了19.6%～37.5%,吸磷量增加了22.7%～40.2%,其中编号为HCW115解磷菌株的效果相当于施用无机磷（P）10 mg.kg^-1处理。     

Using hydrochemical signatures to characterize the long-period evolution of groundwater information in the Dagu River Basin,China

• The long-period groundwater evolution was identified by hydrochemical signatures. • The dominant processes in the groundwater evolution were verified. • Groundwater quality in the coastal areas was susceptible to deterioration due to SI. • Groundwater contamination arose from fertilizer, livestock manure & domestic sewage. The evolution of hydrochemical compositions influenced by long-period interactions between groundwater and the geo-environment is a fundamental issue for exploring groundwater quality and vulnerability. This study systematically investigated the hydrochemical processes and anthropogenic interference occurring in the river basin by bivariate plots, Gibbs diagrams, saturation index, and the major ions ratios. Apparent changes in groundwater hydrochemistry have been observed in the study area, illustrating the origins of major ions are affected by various internal and external factors. Results highlighted that TDS varied from freshwater to brackish water, ranging between 187.90 and 2294.81 mg/L. Ca²⁺ and HCO₃⁻ are the dominant ions in the studied samples. The results gained by Gibbs diagrams, bivariate plots, saturation index, and the major ions ratios demonstrated that minerals dissolution/precipitation, cation exchange, and human inputs play crucial roles in the unconfined aquifers. Moreover, the overuse of nitrogen fertilizer, livestock manure, and industrial/domestic sewage led to nitrate and nitrite contamination and brought significant challenges to the surrounding hydrogeo-environment. The present study could make an unambiguous identification of natural processes and anthropogenic interventions influencing groundwater hydrochemistry’s long-period evolution and create a preliminary strategy for groundwater resources management.     

Characteristics of plankton Hg bioaccumulations based on a global data set and the implications for aquatic systems with aggravating nutrient imbalance

• Hg bioaccumulation by phytoplankton varies among aquatic ecosystems. • Active Hg uptake may exist for the phytoplankton in aquatic ecosystems. • Impacts of nutrient imbalance on food chain Hg transfer should be addressed. The bioaccumulation of mercury (Hg) in aquatic ecosystem poses a potential health risk to human being and aquatic organism. Bioaccumulations by plankton represent a crucial process of Hg transfer from water to aquatic food chain. However, the current understanding of major factors affecting Hg accumulation by plankton is inadequate. In this study, a data set of 89 aquatic ecosystems worldwide, including inland water, nearshore water and open sea, was established. Key factors influencing plankton Hg bioaccumulation (i.e., plankton species, cell sizes and biomasses) were discussed. The results indicated that total Hg (THg) and methylmercury (MeHg) concentrations in plankton in inland waters were significantly higher than those in nearshore waters and open seas. Bioaccumulation factors for the logarithm of THg and MeHg of phytoplankton were 2.4–6.0 and 2.6–6.7 L/kg, respectively, in all aquatic ecosystems. They could be further biomagnified by a factor of 2.1–15.1 and 5.3–28.2 from phytoplankton to zooplankton. Higher MeHg concentrations were observed with the increases of cell size for both phyto- and zooplankton. A contrasting trend was observed between the plankton biomasses and BAF_MeHg, with a positive relationship for zooplankton and a negative relationship for phytoplankton. Plankton physiologic traits impose constraints on the rates of nutrients and contaminants obtaining process from water. Nowadays, many aquatic ecosystems are facing rapid shifts in nutrient compositions. We suggested that these potential influences on the growth and composition of plankton should be incorporated in future aquatic Hg modeling and ecological risk assessments.     

Microbial responses to the use of NaClO in sediment treatment

• Chlorine addition enhanced the release of TOC, TN from the sediment. • Chlorine has a long-term negative effect on microbial richness. • Usually enzymes lose activity, and expression of genes was downregulated. • Carbon degradation and nitrification might be strongly inhibited. Chlorine is often used in algal removal and deodorization of landscape waters, and occasionally used as an emergency treatment of heavily polluted sediments. However, the ecological impact of this practice has not been fully studied and recognized. In this study, NaClO at 0.1 mmol/g based on dry weight sediment was evenly mixed into the polluted sediment, and then the sediment was incubated for 150 days to evaluate its microbial effect. Results showed that NaClO addition enhanced the release of TOC, TN, Cr and Cu from the sediment. The microbial richness in the examined sediment decreased continuously, and the Chao1 index declined from 4241 to 2731, in 150 days. The microbial community composition was also changed. The abundance of Proteobacteria and Bacteroidetes increased to 54.8% and 4.2% within 7 days compared to the control, and linear discriminant analysis (LDA) showed gram-negative bacteria and aerobic bacteria enriched after chlorination. The functional prediction with PICRUSt2 showed the functions of the microbial community underwent major adjustments, and the metabolic-related functions such as carbon metabolism, including pyruvate and methane metabolisms were significantly inhibited; besides, 15 out of 22 analyzed key enzymes involved in C cycling and 6 out of 12 key enzymes or genes involved in N cycling were strongly impacted, and the enzymes and genes involved in carbon degradation and denitrification showed remarkable downregulation. It can be concluded that chlorination posed a seriously adverse effect on microbial community structure and function. This study deepens the understanding of the ecological effects of applying chlorine for environmental remediation.