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1.
七虎林河源头区地表腐殖质随着径流的冲刷进入水体,形成了天然有机质(NOM),其中,溶解性有机质(DOM)易对河流水质造成影响。为了研究七虎林河中DOM的时空分布特征及其对水质的影响,开展了6次采样,分析了水体及土壤吸收光谱和荧光光谱特征参数,利用平行因子(PARAFAC)算法解析了水体DOM的特性及来源。结果表明:七虎林河上游水体五日生化需氧量(BOD5)、高锰酸盐指数(CODMn)、化学需氧量(COD)、可溶性有机碳(DOC)的浓度分别为1.4 mg/L±0.2 mg/L、6.1 mg/L±3.0 mg/L、21 mg/L±8 mg/L、7.0 mg/L±3.2 mg/L,BOD5/COD平均值为0.08,说明流域内水体DOM的可生化性差,对水质影响较小。光谱特征参数紫外吸收系数(SUVA254)、荧光指数(FI)、腐殖化指数(HIX)、生物源指数(BIX)分析结果表明,七虎林河上游云山水库库上林区河段DOM的物质组成与水库及库下河段差异显著。库上河段DOM的芳香碳含量更高、分子量更大、自生源组分...  相似文献   

2.
焦化废水中的溶解性有机物(DOM)作为废水污染物和毒性的主要来源受到广泛关注。厌氧-缺氧-好氧(A-A-O)生物法联合混凝沉淀工艺在焦化废水处理中被广泛应用。于2018年4,7和11月分别采集4座焦化废水处理厂废水,采用光谱学分析手段和水生生物急性毒性试验对A-A-O联合混凝沉淀处理过程中焦化废水的DOM和毒性变化进行分析。结果表明,焦化废水中含有大量不饱和芳香性物质,其中类色氨酸、络氨酸物质占主导,其次为类溶解性微生物代谢产物、类富里酸物质和类腐殖酸类物质;未经处理的焦化废水对藻类和大型溞的急性毒性等级为中毒至高毒。A-A-O联合混凝沉淀处理可去除90%以上的类色氨酸、络氨酸和类富里酸物质,但对类腐殖酸类物质去除率相对较低,仅为约80%,关键去除段为缺氧段和好氧段;该工艺对焦化废水急性毒性削减率为80.51%~94.30%,关键削减段为厌氧段。Pearson相关性分析结果显示,焦化废水溶解性总有机碳(TOC)、类腐殖酸类物质荧光组分C1和类富里酸类物质荧光组分C4与废水急性毒性存在显著正相关关系,可利用其作为水样急性毒性初筛的指示性指标。可为焦化废水生化处理的效能优化和废水毒性控制及安全评估提供科学支撑。  相似文献   

3.
为研究邯郸市大气细颗粒物(PM_(2.5))中金属元素的污染特征,选取城区4个功能区(工业区、工业生活区、教学区和交通区)分别布设采样点位,采集2017年冬季PM_(2.5)样品。采用电感耦合等离子体质谱仪分析样品中11种金属元素(V、Cr、Mn、Fe、Ni、Co、Cu、As、Cd、Ba和Bi)的含量,对其空间污染特征进行比较,并运用主成分分析、聚类分析和绝对主成分得分-多元线性回归模型对金属元素的来源及其贡献率进行模拟计算,对Cr、Ni、Cu、As和Cd的潜在生态风险进行评估。研究结果表明,邯郸市冬季PM_(2.5)污染较为严重,4个功能区的PM_(2.5)日均值远超《环境空气质量标准》(GB 3095—2012)二级标准限值。对金属元素含量的分析表明,教学区大气PM_(2.5)中金属元素质量浓度的总和相对较低,尤其是Fe、Cr、Cd、Mn和Cu的含量均低于其他3个功能区,但是As的含量较高。富集因子计算结果显示,V、Co和Ba在邯郸市的富集系数小、污染程度低,其余金属元素尤其是As、Fe、Cd和Bi的富集系数大、污染程度高。对研究区大气PM_(2.5)金属元素的来源进行解析发现,金属元素的主要来源包括工业生产、自然源、化石燃料的燃烧及交通运输活动。其中,Cr、Mn、Fe、Cu、Cd和Ba主要来自工业活动,V、Co和Bi的主要来源是自然源,Ni和As主要来自化石燃料的燃烧及交通运输活动。潜在生态风险评估发现,邯郸市4个功能区金属元素的总生态风险指数均较高,尤其是As和Cd在各个功能区的潜在生态风险程度为极强,但Cr和Ni的潜在生态风险程度较低。  相似文献   

4.
应用地累积指数法对珠江(广州河段)表层沉积物中重金属污染程度进行了调查与评价.结果表明,其表层沉积物中重金属的地累积指数大小顺序为:Cu>Cd>Zn>Pb>As>Cr>Hg,其中Cu是主要污染物,Cd、Zn和Pb的地累积指数较高.在所有监测断面中,地累积级别达到4级(强污染)的有5个断面,即4#(雅瑶大桥)、5#(黄歧)、6#(黄沙)、7#(横滘)和16#(花地涌北出口).  相似文献   

5.
通过采集淮南市6个功能区四季的PM_(2.5)样品,运用GC-MS仪测定样品中PAHs含量并分析其主要来源。结果表明:该市PM_(2.5)中PAHs质量浓度年均值为31.06 ng/m~3,呈现冬季污染程度最重,夏季最轻,采矿区商业区工业区文教区居民区对照区的特征;夏季PAHs以3环和4环为主,春、秋、冬季以4环、5环和6环为主;6个功能区均以4环PAHs为主;PAHs主要来源为煤燃烧、机动车尾气排放、生物质燃烧及焦炉挥发,其中燃煤和机动车尾气污染贡献最大。  相似文献   

6.
选取昆明翠湖不同功能区表层沉积物,分析其氮的赋存形态与质量比分布特征,探讨上覆水、间隙水与沉积物各指标间的响应关系及污染现状分析评价。结果表明:翠湖表层沉积物总氮(TN)质量比为564 mg/kg~4 602 mg/kg,且沿水流方向增大;可转化态氮(TTN)含量变化差异性较小,以强氧化剂可提取态氮(SOEF-N)和强碱可提取态氮(SAEF-N)为主;上覆水溶解氧(DO)、氧化还原电位(ORP)、p H值、TN和间隙水p H值、氮盐、COD及沉积物氮赋存形态对翠湖表层沉积物中各形态氮的含量分布与变化存在响应关系。  相似文献   

7.
结合紫外可见吸收光谱与三维荧光光谱法,利用平行因子分析方法研究哈尔滨市磨盘山水库水体中的溶解性有机质(DOM)。结果表明,水体DOM吸收系数α355平均值为(4.71±0.66)m-1,表明水库中有色溶解性有机质(CDOM)较高;水库水体DOM存在3个荧光组分,分别为类腐殖质C1(345 nm、440 nm)、类腐殖质C2(285 nm、405 nm)和类富里酸组分C3(275 nm、475 nm);C1、C3呈现显著的正相关性,自生源指数与C1呈显著的负相关性;类腐殖质的荧光强度在深层水体中逐渐增加,且深层水体的腐殖化程度较高,较为稳定;水库中心水体中DOM的自生源特征较其他区域明显,浮游植物和细菌的有机体降解产物增加。  相似文献   

8.
应用模糊综合-加权模型,以及温州市3个典型湿地沉积物中7种重金属含量数据,对温瑞塘河重金属污染进行评价。模糊综合评价结果表明,温州市居民区河流三垟湿地沉积物属于Ⅴ级重金属污染水平,主要污染元素为Zn和Cd;山前上游河段卧龙河沉积物为Ⅲ级污染,主要污染物是Cd。工业区河流牛桥底河沉积物虽然也是Ⅴ级,但是Cu、Cr、Ni、Zn和Cd 5种重金属污染分值为1.0,小于前2个典型河段的1.2和3.3。内梅罗指数法和潜在生态危害系数法评价结果显示,沉积物的重金属污染程度为牛桥底河三垟湿地卧龙河,这与模糊综合评价结果相符。  相似文献   

9.
根据2010年3月(冬季)、5月(春季)、8月(夏季)、11月(秋季)对江苏省如东县贝类养殖区4次现场监测资料,着重对养殖区海水和表层沉积物中重金属的分布特征进行了分析,并对养殖区进行了生态环境质量评价及潜在生态风险评价。结果表明:海水中重金属污染程度顺序为Pb>Zn>Hg>Cu>As>Cd;表层沉积物中重金属的污染程度顺序依次为Zn>Pb>As>Cu>Hg>Cd;表层沉积物中重金属的潜在生态危害程度顺序依次为Hg>Cd>As>Pb>Cu>Zn。4次调查结果的多种重金属的潜在生态风险指数(RI)均低于140,表明这些重金属对海洋生态系统的潜在生态风险属于低潜在生态风险水平,养殖环境良好。  相似文献   

10.
开阳磷矿大规模采选矿活动对洋水河造成一定程度的重金属污染,为了解其污染状况,分析了洋水河水体中重金属Cd、U、Cu、Pb、Cr、Zn和类金属As等7种元素的含量,探讨其分布特征,并用地累积指数法和潜在生态危害指数法对沉积物中重金属污染程度及潜在生态危害进行了综合评价。结果表明,洋水河河水中重金属的浓度均低于中国地表水环境质量V类水质标准,沉积物中Cd、As和Zn的平均含量为1.27、50.28、151μg/g,分别高于贵州省土壤背景值6.05、3.14、2.26倍,高于中国水系沉积物背景值约9.07、5.53、2.89倍,其余元素均低于或接近贵州省土壤背景值和中国水系沉积物背景值,洋水河沉积物已不同程度受到Cd、As和Zn的污染;地累积指数评价结果表明,沉积物中Cd为中度污染,As属于轻度污染,其余元素均为无污染或轻度污染;潜在生态危害指数评价结果表明,单个重金属元素Cd的生态危害指数最大,其次是As,其余4种重金属均属于轻微生态风险,危害性小,综合潜在生态风险指数表明沉积物中重金属达到中等以上风险水平。  相似文献   

11.
In order to provide support for the discussion of the fate of organic matter in estuaries, a laboratory simulation was performed by changing freshwater ionic strength, pH and organic matter content. The change in spectroscopic characteristics caused by variations in salinity, pH and organic matter concentration in the filtered samples was observed by UV-Vis and fluorescence spectroscopy. The increase in emission fluorescence intensity of dissolved organic matter (DOM) due to increasing salinity (in the range 0 to 5 g l-1) is affected by the pH of the samples. The emission fluorescence intensity at the three maxima observed in the fluorescence spectra, is linearly correlated with dissolved organic carbon (DOC) concentration at several salinity values in the same sample. The increase in organic matter concentration caused a shift in the emission peak wavelength at 410 nm for several salinity values. We concluded that it is necessary to take into account the influence of salinity and pH on emission fluorescence of dissolved organic matter if it is to be used as a tracer in estuarine or near shore areas.  相似文献   

12.
This work investigated the effect of soil aquifer treatment (SAT) operation on the fluorescence characteristics of dissolved organic matter (DOM) fractions in soils through laboratory-scale soil columns with a 2-year operation. The resin adsorption technique (with XAD-8 and XAD-4 resins) was employed to characterize the dissolved organic matter in soils into five fractions, i.e., hydrophobic acid (HPO-A), hydrophobic neutral (HPO-N), transphilic acid (TPI-A), transphilic neutral (TPI-N), and hydrophilic fraction (HPI). The synchronous fluorescence spectra revealed the presence of soluble microbial byproduct- and humic acid-like components and polycyclic aromatic compounds in DOM in soils, and SAT operation resulted in the enrichment of these fluorescent materials in all DOM fractions in the surface soil (0–12.5 cm). More importantly, the quantitative method of fluorescence regional integration was used in the analysis of excitation–emission matrix (EEM) spectra of DOM fractions in soils. The cumulative EEM volume (Φ T, n ) results showed that SAT operation led to the enrichment of more fluorescent components in HPO-A and TPI-A, as well as the dominance of less fluorescent components in HPO-N, TPI-N, and HPI in the bottom soil (75–150 cm). Total Φ T, n values, which were calculated as $ {\Phi_{{T,n}}} \times {\mathrm{DOC}} $ , suggested an accumulation of fluorescent organic matter in the upper 75 cm of soil as a consequence of SAT operation. The distribution of volumetric fluorescence among five regions (i.e., P i, n ) results revealed that SAT caused the increased content of humic-like fluorophores as well as the decreased content of protein-like fluorophores in both HPO-A and TPI-A in soils.  相似文献   

13.
The potential biodegradation and subsequent transformation of 17β-estradiol (E2) to estrone (E1) were examined in the presence of various dissolved organic matter (DOM) isolated from effluent, river and lake waters. In addition, estrogenicity was estimated in association with the removal of E2 via its sorption onto DOM and biodegradation. The more biodegradable lake-derived DOM promoted more extensive transformation of E2 into E1 than the effluent organic matter through a biodegradation process. Overall, under all conditions, biodegradation dominated the removal of E2 in water. The increased dissolved organic carbon (DOC) concentrations in river and lake-derived DOM (e.g. 6.5 mg C L(-1)) reduced the removal of E2 by decreasing its biodegradation due to the moderate sorption of E2 onto DOM. The effluent organic matter showed greater removal of E2 via biodegradation, as well as significantly high sorption. This was associated with a large amount of hydrophobic fulvic acid (FA)- and humic acid (HA)-like organic components, as shown by the small increase in the specific UV absorbance at 254 nm (SUVA(254)). An increase in the DOC concentration reduced the removal of E2, resulting in high estrogenicity. The present study suggests that both organic composition and DOC concentration influenced the removal of E2 and, therefore, should be fully considered when assessing estrogenicity and its impacts on the aquatic environment.  相似文献   

14.
In contrast to extensive studies of dissolved organic matters (DOM) in natural lakes, the distributions and the characteristics of DOM in artificial dam reservoirs have not been well documented despite a growing demand for the construction worldwide. For this study, spatial variations in the concentrations and the characteristics of DOM in Lake Paldang, a large river-type dam reservoir, were investigated using the concentrations, the specific UV absorbance (SUVA), the synchronous fluorescence spectra and the molecular weight (MW(w)) values. In addition, environmental factors determining the DOM spatial distribution were examined based on a principal component analysis (PCA). Variations in the DOM characteristics were greater than those for the concentrations (1.1-2.4 mg C/L). In contrast to typical lakes, vertical variations with a depth were much smaller than those observed among horizontal sampling sites within the reservoir. Irrespective of the depth, four individual sampling locations were easily distinguished by comparison of some selected DOM characteristics. The protein-like fluorescence (PLF), MW(w) and SUVA values observed at the location near the dam exceeded the corresponding values for the sampling locations near major influent rivers, suggesting that, even for the river-type dam reservoir, the downstream DOM characteristics may be governed by in-lake DOM production processes such as the release from sediments and algal activities. The results of principal component analysis (PCA) revealed that approximately 61% of the variance in DOM distribution might be explained by allochthonous/autochthonous carbon sources and predominant presence of either total nitrogen or total phosphorous over the other.  相似文献   

15.
Spectroscopic characteristics of dissolved organic matter (DOM) in a large dam reservoir were determined using ultraviolet absorbance and fluorescence spectroscopy to investigate spatial distribution of DOM composition after turbid storm runoff. Water samples were collected along a longitudinal axis of the reservoir at three to four depths after a severe storm runoff. Vertical profiles of turbidity data showed that a turbid water layer was located at a middle depth of the entire reservoir. The spectroscopic characteristics of DOM samples in the turbid water layer were similar to those of terrestrial DOM, as demonstrated by the higher specific UV absorbance (SUVA) and the lower fluorescence emission intensity ratio (F 450/F 500) compared to other surrounding DOM samples in the reservoir. Synchronous fluorescence spectroscopy revealed that higher content of humic-like DOM composition was contained in the turbid water. Fluorescence excitation–emission matrix (EEM) showed that lower content of protein-like aromatic amino acids was present in the turbid water DOM. The highest protein-like fluorescence was typically observed at a bottom layer of each sampling location. The bottom water DOM exhibited extremely high protein-like florescence near the dam site. The particular observation was attributed to the low water temperature and the isolation of the local bottom water due to the upper location of the withdrawal outlet near the dam. Our results suggest that the distribution of DOM composition in a dam reservoir is strongly influenced by the outflow operation, such as selective withdrawal, as well as terrestrial-origin DOM inputs from storm runoff.  相似文献   

16.
Dissolved organic matter (DOM) in raw and treated wastewater from two breweries in Thailand was profiled and monitored for the purpose of water reclamation. The wastewater and the effluent from the use of an upflow anaerobic sludge blanket (UASB) and activated sludge (AS) were collected and analyzed through a resin fractionation method using the fluorescent excitation?Cemission matrix (FEEM) technique. The results revealed that the major organic fractions in the brewery wastewater were hydrophobic acid (HPOA) and hydrophilic base (HPIB), accounting for 65% of total dissolved organic carbon (DOC) mass for brewery A and 56% of total DOC mass for brewery B. The FEEM results indicated that the organic matter in the wastewaters of both breweries were mainly composed of tryptophan-like substances, represented by peaks C (230 nmEx/340?C365 nmEm) and D (265?C295 nmEx/315?C390 nmEm), and humic-like substances, represented by peaks E (290 nmEx/400 nmEm), F (330?C335 nmEx/395?C410 nmEm), and G (255?C265 nmEx/435?C455 nmEm). The analysis revealed that the reduction of DOM occurred mostly during the UASB treatment where most of the DOM reduction resulted from the removal of the HPOA and HPIB fractions. The HPOA fraction, a group of humic-like substances, is of particular concern when reclaiming treated brewery wastewater, and although it was reduced by more than 80% of its initial amount, it was still a dominant DOM fraction in the effluents.  相似文献   

17.
Diffusion is an important process for sediment-water exchange and plays a vital role in controlling water quality. Fugacity fraction (ff) was used to estimate the sediment-water diffusion of polycyclic aromatic hydrocarbons (PAHs) between seawater and surficial sediment. A total of 33 surface sediment and sea water samples were collected concurrently from the northeast coastal area in China and 25 PAHs were analyzed including the alkylated and chlorated PAHs. Fugacity fraction was calculated based on the PAH concentrations in water and sediment, octanol-water partition coefficient of PAHs, organic matter content in sediment, and density of sediment. The calculated results showed that ff increased with decreasing molecular weight of PAHs. The low molecular weight PAHs (2-3 rings) transferred from sediment to water and the sediment acted as a secondary source to the water. The medium molecular weight PAHs (4-5 rings) were close to the sediment-water equilibrium and the transfer tendency shifted between sediment and water. The high molecular weight PAHs (5-6 rings) transferred from water into sediment and the sediment acted as a sink. Soot carbon and the difference of PAH concentrations between sediment and water were found to be important factors affecting the sediment-water diffusion. This study provided new insight into the process of sediment-water diffusion, which has a great influence on the quality of water, especially in severely-polluted sediment areas.  相似文献   

18.
Conventionally, resin fractionation (RF) method has been widely used to characterize dissolved organic matter (DOM) found in different source waters based on general and broad DOM fractions grouping. In this study, a new refined method using multistep, microvolume resin fractionation combined with excitation emission matrix fluorescence spectroscopy (MSM-RF-EEMS) was developed for further isolation and characterization of subfractions within the primary DOM fractions separated from using the conventional RF method. Subsequently, its feasibility in indicating the occurrence of urban pollution in source waters was also assessed. Results from using the new MSM-RF-EEMS method strongly illustrated that several organic subfractions still exist within the regarded primary pure hydrophobic acid (HoA) fraction including the humic- and fulvic-like organic matters, tryptophan- and tyrosine-like proteins. It was found that by using the MSM-RF-EEMS method, the organic subfractions present within the primary DOM fraction could be easily identified and characterized. Further validation on the HoA fraction using the MSM-RF-EEMS method revealed that the constant association of EEM peak T1 (tryptophan) fraction could specifically be used to indicate the occurrence of urban pollution in source water. The correlation analysis on the presence of EEM peak T2 (tyrosine) fraction could be used as a supplementary proof to further verify the presence of urban pollution in source waters. These findings on using the presence of EEM peaks T1 and T2 within the primary HoA fraction would be significant and useful for developing a sensory device for online water quality monitoring.  相似文献   

19.
Concentrations of Cd, Co, Cu, Ni and Pb were measured in particulate and dissolved phases at 11 sites located upstream and near Athabasca oil sands development. The in situ discrimination between non-labile and labile dissolved metals was done using diffusive gradients in thin-films (DGT) devices. The DGT-labile fraction of Co and Ni was 30% lower near development sites whereas Cu, Cd and Pb showed minor changes spatially. It was found that an 8-fold increase in dissolved organic matter (DOM) near development induced a rapid decrease in DGT-labile metals. Dissolved metal concentrations were used along with DOM, major ions, nutrients, pH and conductivity to calculate the distribution of dissolved metal species using the speciation model WHAM. Labile-DGT metal concentrations agreed well with WHAM-predicted concentrations. It was also found that a significant amount of metals were associated with the non-DGT labile fraction (i.e. colloidal DOM) and colloid abundance was more important than suspended particulate matter abundance in influencing metal mobility near Athabasca oil soils development. Since changes in colloidal DOM levels are likely to be the result of surface mining activities, this confirms the serious effects of oil sands activities on metal biogeochemical cycles in the lower Athabasca River.  相似文献   

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