初夏渤海湾营养盐结构特征及其限制状况分析

根据2016年初夏渤海湾营养盐、叶绿素a和相关水文参数等数据,利用浮游植物吸收营养盐最低阈值和化学计量关系作为判断依据对渤海湾营养盐限制状况进行分析.结果表明：受陆地径流和渤海中部冷水输入的影响,初夏渤海湾在近岸、中部和湾口呈现三个明显的温盐特征海区.溶解无机氮（DIN）和活性硅酸盐（SiO₃^2--Si）受陆源输入影响,呈现近岸高湾口低的特征;DIN平均浓度为（7.67±6.48）μmol/L,SiO₃^2--Si平均浓度为（5.44±3.01）μmol/L,在湾口表层,DIN含量较低仅为（2.21±2.94）μmol/L,其中50%站点含量低于阈值（1μmol/L）,58.3%的站点存在DIN限制.而活性磷酸盐（PO₄^3--P）受陆源输入和浮游植物吸收储存作用等因素影响,呈现西部和曹妃甸外近海高中部较低的分布特征,平均浓度为（0.07±0.07）μmol/L,近岸受陆源氮磷输入总量差异影响,表层存在磷潜在限制比例达100%,而中部表层受浮游植物消耗吸收的影响,PO₄^3--P含量较低,仅为（0.02±0.02）μmol/L （未检出设为0）,其中近74.3%的水样含量低于阈值（0.03μmol/L）,磷限制状况严重.随着渤海湾氮磷营养盐陆源输入总量差距不断扩大,磷限制状况必将会进一步发展.     

Investigation of interactions between surface water and petroleum-type pollutants

Background, Aims and Scope In oil spill investigations, one of the most important steps is a proper choice of approaches that imply an investigation of samples taken from different sedimentary environments, samples of oil contaminants taken in different periods of time and samples taken at different distances from the oil spill. In all these cases, conclusion on the influence of the environment, microorganisms or migration on the oil contaminants' composition can be drawn from the comparison of chemical compositions of the investigated contaminants. However, in case of water contaminants, it is very important to define which part of organic matter has been analyzed. Namely, previous investigations showed that there were some differences in chemical composition of the same oil contaminant depending on the intensity of its contact with ground water. The aim of this work is to define more precisely the interactions between oil contaminant and water, i.e. the influence of the intensity of interaction between the oil contaminant and water on its chemical composition. The study was based on a comparison of four fractionated extracts of an oil pollutant, after they had been analyzed in details. Methods Oil polluted surface water (wastewater canal, Pančevo, Serbia) was investigated. The study was based on a comparison of four extracts of an oil contaminant: extract 1 (decanted part), and extracts 2, 3 and 4 (extracted by shaking for 1 minute, 5 minutes and 24 hours, respectively). The fractionated extracts were saponified with a solution of KOH in methanol, and neutralized with 10% hydrochloric acid. The products were dissolved in a mixture of dichloromethane and hexane, and individually fractionated by column chromatography on alumina and silica gel (saturated hydrocarbon, aromatic, alcohol and fatty acid fractions). n-Alkanes and isoprenoid aliphatic alkanes, polycyclic alkanes of sterane and triterpane types, alcohols and fatty acids were analyzed using gas chromatography (GC) and gas chromatography-mass spectrometry (GC-MS). δ13CPDB values of individual n-alkanes in the aliphatic fractions were determined using gas chromatography-isotope ratio monitoring-mass spectrometry (GC-irmMS). Results and discussion. Extracts 1 and 2 are characterized by uniform distribution of n-alkanes, whereas extract 3 is characterized by an even-numbered members dominating the odd-ones, and extract 4 showed a bimodal distribution. Extract 1 is characterized by the least negative δ13CPDB values of C19-C26 n-alkanes. Sterane and triterpane analysis confirmed that all extracts originated from the same oil contaminant. n-Fatty acids, C19-C24, in all extracts are very low, being somewhat higher in extract 4. Even-numbered n-alcohols, C12–C16, were identified in the highest concentration in extract 3. It was assumed that algae were responsible for the composition of extract 3. Furthermore, a possible reason for higher concentrations of C19–C26 n-alkanes and C19–C24 fatty acids in extract 4 is the formation of inclusion compounds with colloidal micelles formed between the oil contaminant's NSO-compounds and water. Conclusion It was undoubtedly confirmed that there were specific differences in the compositions of the different extracts depending on the intensity of the interaction between the oil contaminant and the surface water. Recommendation and Outlook. When comparing the composition of oil contaminants from different water samples (regardless of the ultimate investigation goal) it is necessary to compare the extracts isolated under the same conditions, in other words, extracts that were in the same or very similar interaction with water.     

Length of index and ring fingers differentially influence sexual attractiveness of men’s and women’s hands

Humans show intra- and intersexual variation in second (2D) relative to fourth (4D) finger length, men having smaller 2D:4D ratio, possibly because of differential exposure to sex hormones during fetal life. The relations between 2D:4D and phenotypic traits including fitness components reported by several studies may originate from the organizational effects that sex hormones have on diverse organs and their concomitant effect on 2D:4D. Evolutionary theory posits that sexual preferences are adaptations whereby choosy individuals obtain direct or genetic indirect benefits by choosing a particular mate. Since sex hormones influence both fitness and 2D:4D, hand sexual attractiveness should depend on 2D:4D, a hypothesis tested only in one correlational study so far. We first presented hand computer images to undergraduates and found that opposite-sex hands with long 2D and 4D were considered more sexually attractive. When we experimentally manipulated hand images by increasing or decreasing 2D and/or 4D length, women preferred opposite-sex hands that had been masculinized by elongating 4D, whereas men avoided masculinized opposite-sex right hands with shortened 2D. Hence, consensus exists about which hands are attractive among different opposite-sex judges. Finger length may signal desirable sex hormone-dependent traits or genetic quality of potential mates. Psychological mechanisms mediating hand attractiveness judgments may thus reflect adaptations functioning to provide direct or indirect benefits to choosy individuals. Because the genetic mechanisms that link digit development to sex hormones may be mediated by Hox genes which are conserved in vertebrates, present results have broad implications for sexual selection studies also in nonhuman taxa.     

引起红土表层硅铝比值增大原因的可能性探讨

Si/Al或SiO2 /R2 O3 常常作为表生化学风化作用强度的重要指标。随着化学风化作用的进行 ,硅铝比或硅铝铁率表现出逐渐降低的演化趋势。中国南方的红土风化壳 ,是强烈化学风化作用的产物 ,被认为处于或经历了脱硅富铝化阶段。但是在红土剖面上部常常出现该比值不降反升的现象 ,给运用这一指标指示化学风化强度带来了困难。通过对贵州平坝、新蒲及花溪碳酸盐岩红色风化壳化学风化程度的研究 ,以及对中国南方几种不同结晶母岩上发育的红土的化学风化强度指标的对比讨论 ,探讨了产生这种现象的可能性原因。指出Fe、Al氧化物的下渗和淋失作用及其硅质的相对富集是引起中国南方红土表层出现Si/Al和SiO2 /R2 O3升高的主要原因。     

Seasonal and interannual variability of hydrology and nutrients in the Northeastern Black Sea

The main objective of this work was to investigate the temporal variability of hydrochemical parameters in two coastal regions of the Northeastern Black Sea: the Gelendzhik bay, influenced by anthropogenic activities and the Golubaya bay an open coastal region. Dissolved oxygen, biochemical oxygen demand, pH, alkalinity, phosphate, organic phosphorus, silicates, nitrates, nitrites, ammonia, organic nitrogen, oil products and heavy metals were measured. Si/P and Si/N ratios showed that the Gelendzhik bay waters were significantly enriched in nitrogen and phosphorus compounds. Unlike the Golubaya bay, phosphates were always present in the Gelendzhik bay, and development of photo-synthesis was not limited by these. Features of seasonal variability of nutrients in the Gelendzhik bay (increased concentrations and pronounced summer-autumn maximum) appeared to be a result of human impact—outflow of nutrients with shore input and recreational activities during the summer holiday season. The data obtained indicate that pollution from local spots from the coast of the Black Sea, related primarily to eutrophication, could play a large role in the nutrient balance of the sea and could affect its ecological state.     

Total Lead and Stable Lead Isotopes in Stockholm Sediments

Lead (Pb) in the environment is derived from both naturaland anthropogenic sources. The aim of this study is to estimate the isotopic signature of anthropogenic Pb in sediments from a highly contaminated area (Stockholm), to discuss the influence of different sources on this signature, and to suggest natural Pb background concentrations. Also distribution patterns and differences between different water areas in Stockholm have been studied, both by total Pb and stable Pb isotopes. In 1993, sediment samples were collected at 24 stations in the Stockholm area and analysed for total Pb, zirconium (Zr), scandium (Sc) and stable Pb isotopes (^{204, 206-208}Pb). Total Pb data show that the Stockholm sediments are severely contaminated by Pb. The contamination seems to be rather local since the small lakes surrounding the central parts of Stockholm are much less effected than the central parts. Stockholm is clearly influenced by anthropogenic and natural sources, but in some of the small lakes also by Pb in zircons from the geological basement. The anthropogenic Pb in Stockholm has typical ²⁰⁷Pb/²⁰⁶Pb ratios of 0.85–0.89 and ²⁰⁸Pb/²⁰⁴Pb ratios of 36–38, which are distinct from natural sources. Pb/Sc ratios suggest that the natural background Pb concentration is 10–20 mg kg^-1 d.w.     

后置缺氧UCT分段进水工艺处理低C/N城市污水

为处理低碳源生活污水,以内碳源反硝化途径为出发点,开发了后置缺氧UCT分段进水工艺.该工艺仅在UCT分段进水最后一好氧段末端增加了后置缺氧环节,以强化微生物内碳源储存能力.在低C/N水平（平均进水C/N=3.1±1.5）的生活污水条件下,后置缺氧UCT分段进水工艺实现了平均75.3%的TN去除率,运行61d后同步硝化反硝化去除的氮量高达31.5%;运行40d后污泥内碳源储存水平比原工艺污泥提高12.2%,9小时比内源反硝化速率由零提高至5.56mgN/（gVSS×d）,系统可通过好氧段同步硝化内源反硝化（SNED）提高TN去除率.污泥沉降性能有明显改善：SVI值由350mL/g降至97mL/g,而原UCT分段进水工艺污泥仍然膨胀.该工艺仅在原工艺基础上增加了一后置缺氧段,无需外加碳源和额外硝化液回流设施,有利于水厂升级改造.     

尼洋河流域水化学特征及其控制因素

为研究尼洋河流域水化学特征及其控制因素,2014年先后采集河水7组,井水13组,泉水10组,共计30组水样.综合运用数理统计、Piper三线图、Gibbs模型和离子比等方法,分析了尼洋河流域河水、泉水和井水的水文地球化学特征,并探讨了尼洋河流域的水化学演化规律.结果表明,河水、井水及泉水中阳离子均以Ca~(2+)、Mg~(2+)为主,占阳离子总量的84%以上;阴离子以HCO_3~-和SO_4~(2-)为主,占阴离子总量的97%以上;TDS介于79.11~290.48 mg·L~(-1)之间,平均值为165.21 mg·L~(-1),矿化度较低;水化学类型以HCO_3·SO_4(SO_4·HCO_3)-Ca·Mg(Mg·Ca)型水为主;水化学样品均分布在Gibbs模型左中部,说明该流域水化学离子组成受岩石风化作用控制;主成分分析及相关分析表明,尼洋河流域水化学组分受硅酸盐岩的溶解控制,碳酸盐岩的溶解也起到非常重要的作用.     

长江口及其邻近水域溶解无机氮的分布变化特征

根据2004年4个航次的调查资料,研究了长江口及其邻近水域溶解无机氮的分布变化特征。结果表明,高浓度溶解无机氮集中分布在河口附近。一般来讲,近岸硝酸盐浓度上层高于下层,远岸与之相反。由于生物和化学作用的影响,亚硝酸盐和铵盐垂直断面分布较为复杂。随着长江径流量的增加与减小、冲淡水势力范围的扩大与缩小,硝酸盐季节分布随之变化,然而,亚硝酸盐春季浓度较高,铵盐冬季浓度远大于其它季节。各月DIN/PO4-P比值远高于Redfield比值。与1985~1986年相比,20余年溶解无机氮增加了2.2倍,DIN/PO4-P比值升高了1.4倍,这主要取决于溶解无机氮浓度的增加。溶解无机氮在河口的转移除了生物活动的影响外,主要受海水稀释作用的控制。