罗布泊“大耳朵”地区L07-10剖面沉积物重金属赋存形态研究

本研究以罗布泊"大耳朵"地区L07-10剖面沉积物中重金属Cu、Ni、Mn为研究对象,研究了重金属Cu、Ni、Mn的赋存形态,结果显示:Cu以残渣态和有机物结合态为主,可交换态和碳酸盐结合态较少;Ni以残渣态存在的比例较高,可交换态和有机物结合态含量较小;Mn以铁锰氧化物结合态和残渣态为主,可交换态和有机物结合态含量较少。重金属Cu、Ni和Mn的赋存形态在该剖面垂直方向上大部分呈波折多峰分布,其赋存形态与有机质也存在一定的相关性,但相关性有所不同。研究结果揭示了这3种重金属在罗布泊"大耳朵"地区L07-10剖面沉积物中赋存形态的分布规律,研究结果可为罗布泊干盐湖区重金属相关研究补充基础数据。     

落叶中DOM和NDOM对紫色土中Cu迁移的影响

以黄葛榕落叶中可溶性有机质(DOM)和不可溶性有机质(NDOM)为研究对象,分析用DOM、NDOM和DOM+NDOM改良碱性(Al-P)、中性(Ne-P)和酸性紫色土(Ac-P)后,土中Cu的形态变化。结果表明：随着老化时间的增加,各改良紫色土中离子交换态Cu含量均明显降低,碳酸盐结合态Cu含量基本保持不变,铁锰氧化物结合态和有机结合态Cu含量均逐渐增加。老化后,供试改良紫色土中Cu表现为有机结合态≈铁锰氧化物结合态＞碳酸盐结合态＞离子交换态的趋势,Cu迁移能力整体降低,降低幅度为44.22%~68.99%。     

河道沉积物中铅形态分布及影响因素分析

本文对二道坊河河道沉积物中铅的存在形态特征及其影响因素进行了研究。结果表明，铅各形态百分含量的顺序为铁锰氧化物相＞残渣相＞有机相＞碳酸盐结合相＞可交换相，并在水平分布、垂直方向呈现出一定的规律。每一形态铅与某些沉积物性质具有一定的相关性，并且建立了可信度较高的回归方程。     

室内尘埃中铅的赋存形态与儿童血铅的相关性研究

有关室内尘埃中铅的赋存形态与儿童血铅的相关性研究尚未见报道。在对某地儿童血铅进行调查期间,发现当地儿童血铅浓度与室内尘埃中铅的水溶态、离子交换态、腐殖酸结合态、铁锰氧化态、强有机结合态和残渣态呈正相关,但不显著,无统计学意义。但与总铅浓度呈显著正相关(R=0.447,P=0.032),与铅的碳酸盐结合态呈高显著相关(R=0.537,P=0.008)。在此基础上,将儿童血铅分别与尘埃中铅暴露量、摄入量和潜在剂量进行相关分析,结果表明,儿童血铅与室内尘总铅摄入量和总铅潜在剂量正相关但无统计意义,与尘总铅暴露量显著相关(R=0.431,P=0.040),与碳酸盐态的暴露量(R=0.537,P=0.008)、摄入量(R=0.538,P=0.008)和潜在剂量(R=0.540,P=0.008)高度显著相关。提示在土壤和尘埃中铅的碳酸盐态含量较高的地区,碳酸盐态铅可能是造成儿童血铅超标的主要原因。     

赤泥中氟的赋存状态

采用连续化学提取方法对赤泥中各形态的氟进行了提取,并对不同形态氟的迁移规律进行了研究.结果显示.从赤泥中可提取出五种形态的氟,即水溶态氟、可交换态氟、铁锰结合态氟、有机束缚态氟及残余态氟,其中残余态氟所占的比例最大,含量在60%～90%之间,然后依次是水溶态氟、可交换态氟、铁锰结合态氟、有机束缚态氟;赤泥的可给态氟化物(水溶态氟和可交换态氟)输出能力较强,对地下水影响较大,随着堆积时间的延长,赤泥的总氟含量有所降低,但可给态氟化物输出能力非但不减反而增强,赤泥堆放场对地下水的影响主要取决于赤泥中水溶态氟和可交换态氟含量的高低.     

粤北上坝村稻田土壤及间隙水中重金属污染研究

利用Tessier连续提取法对粤北上坝村稻田土壤中重金属化学形态分布特征进行研究,同时调查稻田间隙水中重金属的污染状况。结果表明,研究区域稻田土壤中Cu超标严重,主要以稳定态的形式存在,环境迁移量相对较少;土壤中Zn的生物有效性最低,Cd污染达到中等水平,其生物有效性最高;可交换态Mn,碳酸盐结合态Cd及铁锰氧化物结合态的Mn、Pb、Zn的占比较高,对农业生产环境具有一定的潜在威胁。稻田间隙水中Cd含量超标1.8倍。     

漳河上游流域沉积物中磷的空间分布特征及其影响因素

漳河上游地区众多的水利工程改变了流域水循环,同时也影响了河流泥沙和生源物质的循环过程。为揭示人类活动干扰下的沉积物中磷的赋存特征,采用改进后的连续化学萃取法分析了漳河上游沉积物中总磷(TP)和磷形态的空间分布特征及其影响因素。研究结果表明,漳河上游沉积物中的TP含量为405.94~899.98 mg/kg,低于我国其他主要河流,接近我国东部平原湖泊含量水平。漳河上游的TP富集指数(PEI)均值为1.15,表明漳河上游富营养化风险较高。可交换态磷(Ex-P)、铁锰螯合态磷(BD-P)、铁铝氧化态磷(NaOH-P)、钙结合态磷(HCl-P)分别占沉积物中TP含量的1.13%、33.96%、12.99%、35.05%。BD-P和HCl-P是沉积物中主要的磷形态,Ex-P的含量最低,NaOH-P的含量波动最大。漳河上游沉积物中,生物可利用磷(BAP)的含量约占TP含量的38.36%~52.04%,其中,清漳干流的BAP含量明显低于其他河段。清漳源头的水土流失及浊漳河的磷输入对漳河上游BAP含量的贡献较大。统计分析显示,漳河上游表层沉积物中,TP和磷形态的空间分布无显著差异,表明以水利工程建设为代表的强烈人类活动对漳河上游沉积物中磷的空间分布的影响不显著。相关性分析和冗余分析表明,沉积物中的NaOH-P含量与沉积物中黏土和粉土的占比有较高的相关性,BD-P和NaOH-P是控制沉积物中BAP构成的重要因素,Fe含量是沉积物中TP含量的主控因子。     

湘江干流沉积物中铅和镉的污染特征与评价

2007—2011年连续5 a采集了湘江干流水体沉积物,测定了沉积物样品中铅、镉的含量,同时对霞湾港沉积物中铅、镉的形态进行了分析,并利用地积累指数法、次生相与原生相比值法分别对沉积物中铅、镉的污染状况及生态风险进行了评价。结果表明:湘江水体沉积物中铅、镉的含量较高,其中松柏断面水体沉积物中的铅和镉最高;湘江霞湾港水体沉积物中镉以有机质和硫化物结合态为主;湘江松柏断面的地积累指数在时间上呈上升趋势,霞湾断面、马家河断面和昭山断面的地积累指数在时间上呈弱下降趋势,但松柏断面和霞湾断面沉积物中铅和镉的地积累指数较高,达到6级以上极强污染水平;生态风险评价结果显示,在湘江霞湾港沉积物中镉具有相对较高的生态风险指数,其潜在的生态风险应该引起重视。     

炭负载膨润土对河岸土铜迁移的影响模拟

采用质量分数为1%的生物炭(C)和生物炭负载膨润土( CB )改良嘉陵江、渠江和涪江(川渝段)8个不同河岸土样,并以土柱实验模拟铜在各改良土样中的迁移和形态变化特征(原土样作为对照)。结果表明：C和CB 的添加均有利于沿岸土对铜的吸附,吸附能力和穿透时间表现为CB 改良土样>C改良土样>原土样;各改良沿岸土样对铜吸附能力表现为上游土样强于下游。供试土柱中铜累积量为16.43 g/kg~56.54 g/kg,且表现为CB改良土样>C改良土样>原土样的趋势。铜结合形态以碳酸盐结合态比例最大,铁锰氧化态次之,可交换态和有机态较少。     

长江下游沉积物中重金属污染现状与特征

对长江下游沉积物中的重金属Co、Cr、Cu、Ni、Pb、Zn、Mn、Hg和As进行全量和醋酸提取态(包括水溶态、可交换态和碳酸盐结合态)分析.结果表明,大部分重金属主要来源于地壳元素的自然释放,但Cu、Zn、Hg和As在最近十几年因受到人为排放的影响质量比有所增加.长江江苏段的重金属质量比普遍高于入海口上海段;位于悬浮物易沉降地区的靖江重金属质量比明显偏高.Cu和Zn总体质量比较高,且醋酸提取态所占比例较大,对长江下游存在潜在的生态风险.     

城市空气质量周报效用分析

介绍了世界上一些发达国家的空气污染预报的做法和采取的措施,阐述了我国开展空气质量预报的方针和方法,指出了周报是预报的基础工作。叙述了我国空气质量周报的污染参数的选取、污染指数的分级及其浓度限值和污染指数计算及确定,分析并总结了开展城市空气质量周报所发挥的效用是提高公众的环保意识,加大了治理污染的力度,转变了环境监测的职能,促进了环境监测事业的发展     

锅炉烟尘测试中锅炉负荷率的计算方法探讨

GB5468 -91规定 ,锅炉烟尘测试时 ,必须对锅炉的运行负荷进行测试 ,而实际监测过程中 ,许多锅炉房不具备测试的计量条件 ,为了解决这一问题 ,文章提出利用烟气量和空气过剩系数计算锅炉负荷率。在实际监测工作中 ,该方法方便、易于操作 ,所得结果和标准规定方法所得结果有很好的一致性     

水中总硬度测量不确定度的评定

采用EDTA滴定法测定水质总硬度的测量不确定度评定。充分考虑测量重复性、标准溶液的配制、滴定等过程对测量的影响,计算水中总硬度的测量相对合成标准不确定度为1·81×10-3。     

实验室质量管理体系内部审核的实施

在实施GB/T15481-2000 idt ISO/IEC17025:1999标准《检测和校准实验室能力的通用要求》的过程中,通过实验室质量管理体系内部审核的实践与系统分析,识别出内部审核实施阶段的关键环节,提出召开首次会议、收集审核证据、确定审核发现和召开末次会议的技术方法,对提高内部审核的质量和有效性、获得可靠的审核结论具有重要意义。     

Fractionation of heavy metals and assessment of contamination of the sediments of Lake Titicaca

Chemical weathering is one of the major geochemical processes that control the mobilization of heavy metals. The present study provides the first report on heavy metal fractionation in sediments (8–156 m) of Lake Titicaca (3,820 m a.s.l.), which is shared by the Republic of Peru and the Plurinational State of Bolivia. Both contents of total Cu, Fe, Ni, Co, Mn, Cd, Pb, and Zn and also the fractionation of these heavy metals associated with four different fractions have been determined following the BCR scheme. The principal component analysis suggests that Co, Ni, and Cd can be attributed to natural sources related to the mineralized geological formations. Moreover, the sources of Cu, Fe, and Mn are effluents and wastes generated from mining activities, while Pb and Zn also suggest that their common source is associated to mining activities. According to the Risk Assessment Code, there is a moderate to high risk related to Zn, Pb, Cd, Mn, Co, and Ni mobilization and/or remobilization from the bottom sediment to the water column. Furthermore, the Geoaccumulation Index and the Enrichment Factor reveal that Zn, Pb, and Cd are enriched in the sediments. The results suggest that the effluents from various traditional mining waste sites in both countries are the main source of heavy metal contamination in the sediments of Lake Titicaca.     

“湖泛”恶臭物质分析及来源浅析

介绍了中国南方"湖泛"中的恶臭物质及检测情况,采用常规分析和气相色谱-质谱(GC-MS)对"湖泛"水样进行检测,认为"湖泛"恶臭物主要是氨和硫醚类物质。根据"湖泛"发生的时间及频次,结合南方地区农业水稻秧田的农药使用情况,推断氨基甲酸酯类农药的使用可能是"湖泛"发生的诱因。     

贵州黔东南州三板溪水库春季拟多甲藻水华特征

2011年3月13日对贵州省黔东南州三板溪水库进行春季浮游植物调查的结果表明,三板溪水库Ⅱ号采样点(下革东)发生以佩纳形拟多甲藻为优势种的拟多甲藻水华,细胞密度高达1.15×10⁷cell/L;板溪水库总氮的最低值为2.09 mg/L,总磷的最低值为0.95 mg/L,三板溪水库的总氮、总磷含量较丰富,不存在总氮或总磷是限制性因子;通过SPSS16.0统计软件分别进行Pearson 积距相关系数分析表明,氮磷比是三板溪水库发生拟多甲藻水华的主要影响原因。     

Environmental Assessment of the Impact of Ozone to the Neuston of the Sea-Surface Microlayer of the Gulf of Mexico

Substantial amounts of NOx (146 000 t/y) and total hydrocarbons (294 000 t/y) are released to the marine atmosphere by the large number of oil and gas operations over Federal waters of the Gulf of Mexico (GOM). Under appropriate meteorological conditions these emissions react to form ozone (0–54 g/m3 over-water) which can affect the marine environment. Using a dry deposition model, this work examines the amount of ozone derived from oil and gas offshore operations and deposited in the sea surface of the Gulf of Mexico, and assesses its impact on the neuston of the sea-surface microlayer. Surface integrated estimates of ozone deposited from oil and gas operations over the sea surface ranges from 400 kg to 1800 kg which results in sea surface concentrations of 15 g/m3. This estimate and the actual toxic ozone levels suggest no acute, toxic impacts to the neuston. However, indirect effects may occur through changes to the pelagic foodwebs and organic carbon pathways. Another potential pathway for ozone impacting the environment is through the production of bromate. Based on the concentrations and time scales (11–139 days) only sublethal effects appear to occur, but uncertainties associated with this assessment need to be further studied. From an ecological perspective, the environmental impacts and risks of NOx and VOC discharges from offshore platforms need to be assessed for neuston and other components of the marine ecosystem.     

Evaluation of method of preparation of passive diffusion tubes for measurement of ambient nitrogen dioxide

This study was carried out in response to suggestions that the measurement of NO(2) by Palmes-type passive diffusion tubes (PDT) is affected by the method of preparation of the triethanolamine (TEA) absorbent coating on the grids. The following combinations of factors were investigated: TEA solvent (acetone or water), volume composition of TEA in solvent (50% or 20%), and grid coating method (dipping in solution prior to assembly or pipetting solution on after assembly). Duplicate PDTs prepared by each of the 8 methods were exposed in parallel, in urban air, for a total of 80 separate 1 week exposures. NO(2) concentrations derived from PDTs prepared by pipetting methods were significantly less precise than concentrations from dipping methods, with mean RSDs for duplicate measurements of 13.8% and 8.5%, respectively (n= 316 each category). Pipetting methods using solutions of 50% TEA composition were particularly imprecise (mean RSD 17.2%). Data from PDTs prepared by pipetting methods were systematically more poorly correlated with each other and with data from co-located chemiluminescence analysers, than corresponding data from PDTs prepared by dipping methods, indicating that more consistent accuracy was also obtained by the latter PDTs. The statistical evidence suggested that PDTs prepared by pipetting 50% TEA in water generally gave lower NO(2) concentrations. Although this is in agreement with a previous study, it is also possible that such an observation here may be a statistical artefact given the demonstrably poorer precision of this method. The general tendency of PDTs to show positive bias in NO(2) measurement in urban air in 1 week exposures was again evident in this study (mean biases at roadside and urban centre locations of +35% (n= 475) and +18% (n= 112), respectively) consistent with augmentation of within-tube NO(2) flux by chemical reaction between co-diffusing NO and O(3). Overall, it is recommended that the pipetting method of PDT grid preparation is avoided, or at least investigated further, because of the apparent degradation in precision and accuracy of NO(2) measurement. Potential reasons for the effect are discussed.     

Monitoring of the functioning of ecosystems

The theoretical basis, the content and the possible applications of the program Monitoring of ecosystems are considered. A functional definition of ecosystem is proposed, and some features of ecosystems are defined on this basis. The program Monitoring of ecosystems is visualized as a large-scale program of simple measurements of the rates of the main ecosystem processes. The expected results can be utilized in two ways: (1) a comparative knowledge of ecosystem functioning provides the fundamentals of geography of ecosystems, and (2) the constant, repeatable evaluation of a given ecosystem function provides a basis for its rational management.