河流汇合处水体磷素形态特征及紫外光照的影响：以渠江-嘉陵江、涪江-嘉陵江交汇为例

以渠江-嘉陵江、涪江-嘉陵江交汇处水体为研究对象,探究了河流交汇处水体磷素形态特征及紫外光照的影响.水体磷形态分析结果表明,研究的所有水体中总磷浓度均超过水体富营养化阈值(0.2 mmol·m-3),支流汇入干流前后,研究水体中总磷(TP)主要由总溶解性磷(TDP)组成,而溶解性无机磷(DIP)是TDP的主要组成部分.两支流汇入嘉陵江后,干流水体中各形态磷浓度均较干流汇合前升高,颗粒态磷(PP)增幅最大,达到129%.按水体相对分子质量(Mr)分级结果表明,溶解态高相对分子质量组分(0.5×103~10×103)中的磷为溶解性磷(DP,<0.22μm)主要成分,达到47%~61%,渠江和涪江两支流汇入干流后,嘉陵江水体不同相对分子质量组分中的磷含量并未发生较大变化.通过紫外光照后,游离态组分(<0.5×103)中的磷含量明显增加,增幅在10%~29%,其余两组分中磷含量均降低,和涪江-嘉陵江汇合处样本相比,渠江-嘉陵江汇合处水体胶体态组分(Mr10×103~0.22μm)中磷含量降幅大于前者.通过紫外光照实验,证明了紫外光照是影响水体中磷素地球化学过程的重要环境因素.     

Variations in stable hydrogen and oxygen isotopes in atmospheric water vapor in the marine boundary layer across a wide latitude range

The newly-developed cavity ring-down laser absorption spectroscopy analyzer with special calibration protocols has enabled the direct measurement of atmospheric vapor isotopes at high spatial and temporal resolution. This paper presents real-time hydrogen and oxygen stable isotope data for atmospheric water vapor above the sea surface, over a wide range of latitudes spanning from 38°N to 69°S. Our results showed relatively higher values of 8180 and 82H in the subtropical regions than those in the tropical and high latitude regions, and also a notable decreasing trend in the Antarctic coastal region. By combining the hydrogen and oxygen isotope data with meteoric water line and backward trajectory model analysis, we explored the kinetic fractionation caused by subsiding air masses and related saturated vapor pressure in the subtropics, and the evaporation-driven kinetic fractionation in the Antarctic region. Simultaneous observations of meteorological and marine variables were used to interpret the isotopic composition characteristics and influential factors, indicating that d-excess is negatively correlated with humidity across a wide range of latitudes and weather conditions worldwide. Coincident with previous studies, d-excess is also positively correlated with sea surface temperature and air temperature （Tair）, with greater sensitivity to Tair. Thus, atmospheric vapor isotopes measured with high accuracy and good spatial- temporal resolution could act as informative tracers for exploring the water cycle at different regional scales. Such monitoring efforts should be undertaken over a longer time period and in different regions of the world.     

Phosphorus speciation in the sediment profile of Lake Erhai, southwestern China: Fractionation and 31P NMR

The distribution characteristics of phosphorus(P) forms in the sediment profile of Lake Erhai,in southwestern China has been investigated by sequential extraction and 31P nuclear magnetic resonance spectroscopy(NMR) of NaOH extracts to understand P dynamics and its potential contribution to lake eutrophication.Contents of P fractions varied in the order of NH4Cl extracted P(NH4ClP) < bicarbonate-dithionite extracted P(BD-P) < HCl-P,Residual-P < NaOH extracted P(NaOH-P).The highly available NH4Cl-P represented less than 1% of total P(TP).BD-P and NaOH extracted reactive P(NaOH-rP) averaged 39%,while the ratio of Fe/P was higher than 15,indicating low P release from the sediments under permanent oxic condition.The less bio-available HCl-P,NaOH extracted nonreactive P(NaOH-nrP) and residual-P contributed 61% of TP.Regression analysis revealed that BD-P,NaOH-rP and HCl-P were positively correlated with the contents of Fe and Mn,Al and Fe,and Ca,respectively.The investigation of P compound groups in NaOH extracts by 31 P NMR showed that ortho-P and monoester-P were the largest two constituents of the P pool,followed by diester-P,phosphonate and pyro-P.A comparison of vertical variations of P groups in the sediment profile suggested that these compounds were involved in the P recycling to different extents in Lake Erhai.In particular,the lake exhibits high potential for labile P release from the surface sediments,which should be taken into consideration even after the outsourced P runoff ceased.     

Organic matter produced by algae and cyanobacteria: Quantitative and qualitative characterization

This work aims at characterizing organic matter produced by an alga Euglena gracilis and a cyanobacteria Microcystis aeruginosa and assessing the evolution of its characteristics during growth. A culture medium was optimized. The species growth phases were monitored using both visible spectrophotometry and flow cytometry cell counting. Organic matter fractionation according to hydrophobicity and specific UV absorbance (SUVA) index were used to specifically characterize the produced algal organic matter (AOM). The AOM characteristics were both growth phase and species dependent. However, a similar evolution was observed. The hydrophilic fraction (HPI) was the major fraction whatever the growth phases and was almost the only one produced during lag and exponential phases. It represented around 75% of AOM during exponential phase and then decreased when the stationary phase appeared. It represented 46% and 60% of the AOM during late decline phase for the cyanobacteria and the alga respectively. The hydrophobic (HPO) and transphilic (TPH) fractions started to appear from the beginning of the stationary phase with more hydrophobic compounds coming from intracellular organic material of dying cells. HPO and TPH percentages still increased during the decline phase probably because of two additional processes: photo-dissolution and leaching of particulate organic matter from cells fragments. A comparison of AOM during late decline phase and natural organic matter (NOM) from Glane River (France) underlined that AOM was more hydrophilic and presented a lower SUVA for each fractions than NOM. However, the difference between NOM and AOM hydrophobicity narrowed during decline phase.     

Individual stages of bacterial dichloromethane degradation mapped by carbon and chlorine stable isotope analysis

The fractionation of carbon and chlorine stable isotopes of dichloromethane(CH_2Cl_2,DCM)upon dechlorination by cells of the aerobic methylotroph Methylobacterium extorquens DM4 and by purified DCM dehalogenases of the glutathione S-transferase family was analyzed.Isotope effects for individual steps of the multi-stage DCM degradation process,including transfer across the cell wall from the aqueous medium to the cell cytoplasm,dehalogenase binding,and catalytic reaction,were considered.The observed carbon and chlorine isotope fractionation accompanying DCM consumption by cell supensions and enzymes was mainly determined by the breaking of C\Cl bonds,and not by inflow of DCM into cells.Chlorine isotope effects of DCM dehalogenation were initially masked in high density cultures,presumably due to inverse isotope effects of non-specific DCM oxidation under conditions of oxygen excess.Glutathione cofactor supply remarkably affected the correlation of variations of DCM carbon and chlorine stable isotopes(Δδ~(13)C/Δδ~(37)Cl),increasing corresponding ratio from 7.2–8.6 to 9.6–10.5 under conditions of glutathione deficiency.This suggests that enzymatic reaction of DCM with glutathione thiolate may involve stepwise breaking and making of bonds with the carbon atom of DCM,unlike the uncatalyzed reaction,which is a one-stage process,as shown by quantum-chemical modeling.     

采用电动修复增强技术去除电镀污泥中重金属

为提高电动修复技术去除电镀污泥中的重金属(Cu, Pb, Zn , Cr, Ni)的效率,采用污泥预酸化处理及阴极pH值控制处理2种途径进行强化,反应过程中电压为32V,处理时间为7d,结果表明,电镀污泥酸化pH值至4.5时,污泥中重金属的可移动性明显提高了,依次为Cr>Ni>Zn>Cu>Pb;污泥预酸化加阴极pH值控制处理能使电镀污泥中Zn、Ni、Cu和Pb交换态、碳酸盐结合态和有机硫化物态转化为可溶离子态,转化量大小依次为Ni>Zn>Cu>Pb,且该处理Zn、Ni、Cu和Pb的去除率分别达到74.02%、68.38%、39.22%、21.37%;但污泥预酸化及阴极pH值控制处理都不利于Cr的去除,对照处理Cr去除率为77.83%,污泥预酸化处理去除率降为40.65%,污泥预酸化加阴极pH值控制处理降至12.80%.     

溶解性有机物在土壤含水层处理系统中的变化

通过实验室模拟土壤含水层处理(SAT)的土壤柱系统研究了二级处理出水中溶解性有机物(DOM)的荧光特性在SAT系统中的变化.利用XAD树脂将二级处理出水中的DOM分为5个部分:疏水性有机酸(HPO-A),疏水性中性有机物(HPO-N),过渡亲水性有机酸(TPI-A),过渡亲水性中性有机物(TPI-N)和亲水性有机物(HPI).结果表明,TPI-N中的类芳香族蛋白质荧光物质在SAT系统中优先去除.经过SAT系统处理后,类芳香族蛋白质荧光物质和类溶解性微生物代谢产物荧光物质在HPO-A,HPO-N,TPI-A和HPI中的相对含量升高.各组分中带有3~5个稠合苯环的荧光物质,以及激发波长/发射波长(λex/λem)=390~410nm/456~476nm的类腐殖酸荧光物质在SAT系统中的去除率低于相应组分中以溶解性有机碳(DOC)表征的整体有机物的去除率.不同组分中的其他荧光物质在SAT系统中去除行为不同.     

Assessing the P fractionation in a tropical river-estuarine system of South India

Seasonal variations in dissolved and particulate P forms were assessed in the estuarine system of Chalakudy River, Kerala, South India – a tropical river having substantial relics of riparian vegetation. The contribution of the reactive P form extended to 84–96% compared with the residual fraction. Geographical and human activities have had effects on the phosphorus-loading capacity at various locations, which reveal pronounced variability in P distribution. Not all forms of phosphate in suspended particulate matter are likely to be released, and thus the nature of the P forms within the stock is a sensitive factor that can be utilised. Ca-bound P in suspensates increases to a highly significant level in the estuarine area, whereas Fe/Al-bound P predominates at the riverine and catchment areas during both the monsoon and non-monsoon seasons. Thus, calcium compounds determine the availability of P in the alkaline estuarine environment, whereas in the riverine environment, Al and Fe control P solubility. The comparatively low P load in upstream waters indicates that, under ambient situations, vegetative riparian zones can be very important P filters.     

Fractionation analysis of some heavy metals in sediments of the north-western part of the Red Sea,Egypt

Sequential extraction was used to study operationally determined chemical forms (exchangeable, carbonate, reducible metal, oxidisable metal and the residual fractions) of the metals Cd, Cu, Zn and Pb in sediments from 12 sample sites collected from the north-western part of the Red Sea, where improper recreational facilities have resulted in diverse impacts on the coastal environments fronting some of the recreation projects. The results showed that the average percentage of each phase was different among metal types; the residual binding fraction was the most important phase for binding Zn and to a lesser degree Cu. The reducible fraction was the second most important phase for Zn and Cu. For Pb, the fractions bounded to the residual fractions and the reducible phases are equal and exhibited the highest percentages. By contrast, the carbonate fraction was predominant for Cd. The percentages of Cd, Cu, Zn and Pb associated with the carbonate and exchangeable fractions, which are potentially the most harmful to the environment, were calculated and assessed at different sampling sites of the studied sediments. According to the Risk Assessment Code (RAC), the results reveal that Cd is the only metal that poses a high risk to the environment.     

淡水水体中氮污染源的识别——利用硝酸根中氮和氧同位素组成

氮营养盐污染在全球很多区域都是一个备受关注的环境问题,尤其是以农业为主的区域和人口密集的区域,因此,关于水体中氮污染源识别技术尤为重要.硝酸根离子中的氮、氧同位素组成在过去的十几年中频繁地应用于识别淡水水体中氮污染源的研究中.本文总结了已知氮污染源中氮、氧同位素组成的特征变化区间,阐述了影响氮、氧同位素组成的主要因素,描述了3种氮、氧同位素组成主流的测试方法,展望了未来定量测算各种氮污染源贡献比例的前景.在实际研究中,还将氮、氧同位素组成和水体化学特征结合,则可以有效地识别淡水水体的氮污染源.随着检测精度的不断提高,各种代表性端元污染物同位素值经验区间也变得更加准确.