普者黑湿地小流域土壤总磷分布及污染风险评价

以普者黑湿地小流域为研究对象,分别采集农田0～5cm、草甸0～5cm及湖滨湿地0～5、5～10、10～15cm的土壤样品,分析干、湿季土壤总磷的分布特征。结果表明:(1)在水平分布上,干季表层土壤总磷含量为农田草甸湖滨湿地,湿季表层土壤总磷含量为农田湖滨湿地草甸;在垂向分布上,干、湿季土壤总磷含量分布一致,均为表层富集明显。(2)流域内土壤总磷含量均为湿季大于干季。(3)单因子指数评价结果显示,水平方向上,干、湿季农田与草甸表层土壤总磷均为重度污染,垂直方向上,干季湖滨湿地土壤总磷均为轻度污染,湿季均为重度污染。总体而言,普者黑流域湿季土壤磷污染程度较干季高。     

化学淋洗与生物质炭稳定化联合修复镉污染土壤

为探讨土壤淋洗与生物质炭稳定化联合修复技术对镉(Cd)污染黄棕壤修复效果的影响,研究通过振荡淋洗实验、BCR连续化学提取法和CaCl_2一次提取法,筛选确定污染土壤的最佳淋洗方案,并比较了淋洗修复、淋洗+稳定化修复技术对污染土壤中Cd生物有效性的影响。结果表明:3种淋洗剂的淋洗效率强弱顺序为EDTA-2NaHCl柠檬酸,最佳淋洗条件为0.12 mol·L~(-1)EDTA-2Na在固-液比1:4条件下振荡淋洗3 h,Cd的洗脱率为81.3%;淋洗后土壤中Cd的有效态(F1+F2)百分比减少了51.0%,显著降低了污染土壤的重金属总量及其环境风险;相比于单一淋洗修复技术,EDTA-2Na在添加体积(V_(添加))为最佳淋洗体积(V_(最优))的80%时,淋洗后再加入3%玉米秸秆炭稳定化15 d的联合修复技术能够将土壤中有效态Cd含量(CaCl_2-Cd)从8.13 mg·kg~(-1)降低到0.42 mg·kg~(-1)。因此,淋洗修复后施加玉米秸秆炭的联合修复技术,能够有效降低重金属污染土壤的生态环境风险,提高土壤环境质量。     

乌梁素海表层沉积物重金属分布特征及生态风险评价

采样分析了内蒙古乌梁素海表层沉积物中Cu、Zn、Pb、Cr、Cd、Hg和As的含量、分布特征和富集状况,分别以现代工业化前正常颗粒沉积物中重金属含量的最高背景值和河套地区土壤中重金属含量背景值为参照,采用瑞典科学家Lars Hakanson的潜在生态危害指数法对7种重金属的富集系数和生态危害系数以及各采样点的生态危害指数进行了评价。结果表明,乌梁素海表层沉积物中As和Pb的空间变异性较大;以2种背景值为参比得出的重金属污染水平顺序相近,Hg和As为对乌梁素海生态环境具有潜在影响的主要重金属元素;同时表明,以河套地区土壤重金属背景值为参照更能直观地反映出乌梁素海表层沉积物中重金属的污染程度。     

石油污染土壤胶体特征及其稳定性

采集辽河油田石油污染土壤样品并用离心法提取胶体,定性和定量研究了石油污染土壤胶体的主要物理化学性质,通过间歇实验研究了不同p H(p H=4~9)、不同价态阳离子(Na+、Ca2+和Fe3+)和不同价态阴离子(NO-3、SO2-4和PO3-4)存在下的胶体稳定性,比较了阳离子存在下石油污染土壤胶体和未受污染土壤胶体稳定性。研究结果表明,该石油污染土壤胶体总石油烃含量为123.24 mg/g,石油烃主要为直链烷烃和环烷烃。相同p H条件下石油污染土壤胶体Zeta电位负值比未受污染土壤胶体Zeta电位负值高。石油污染土壤胶体稳定性随p H值增加而增加,随着阳离子价数升高而减小,随阴离子价数升高而增大。Ca2+和Cu2+存在下,石油污染土壤胶体比未受污染土壤胶体稳定性更小。Na+和Fe3+存在下,石油污染土壤胶体比未受污染土壤胶体稳定性更大。     

百色市右江区大气PM10中水溶性无机离子的化学特征与来源

2010年10月至2011年9月采集百色市右江区大气PM10样品,分析PM10及其水溶性无机离子的化学特征与来源。结果表明:(1)百色市右江区大气PM10为13.89～319.44μg/m3,年均117.48μg/m3,年均值超过《环境空气质量标准》(GB 3095-2012)二级标准(100μg/m3)。百色市右江区大气可吸入颗粒物的污染主要出现在春冬季节。(2)水溶性无机离子浓度年均值依次为SO24->NO3->Cl->NH4+>K+>Na+>Mg2+>F-,SO24-、NO3-和Cl-浓度最高,分别占水溶性无机离子的57.7%、14.9%和14.5%。(3)百色市右江区大气PM10呈较强的酸性,高浓度的SO42-可能是导致百色市右江区大气PM10呈较强酸性的主要原因。(4)PM10的季节变化受气温和风速的影响极显著;气象因素对SO42-、NO3-、F-的影响不显著。(5)主因子分析表明,PM10中水溶性无机离子可能来自3个方面,Cl-和NO3-主要来自于当地低烟卤煤燃烧排放的烟气;Mg2+、K+和Na+主要来自于自然源;F-、SO24-和NH4+主要来自于混合源。     

苯并三唑在土壤中的吸附特性

为了解苯并三唑(BTA)在水-土系统中的迁移转化,通过批实验方法研究了BTA在华北平原土样(GSS13)中的吸附,考察了平衡时间、土壤投加量、溶液初始p H以及共存阳离子对吸附的影响。结果表明,在初始阶段,土壤对BTA的吸附速率较快,之后随着吸附点位的减少,吸附逐渐变慢;吸附过程符合准二级反应动力学方程。土壤对BTA的平衡吸附为非线性吸附,吸附等温线为Freundlich型;随着土壤投加量的增大,单位质量土壤吸附BTA的量减少,可能原因是所选土壤对BTA的吸附存在"固体浓度效应"。溶液的p H通过改变BTA的存在形式和土壤表面的带电性而影响吸附,当溶液p H在BTA的p Ka2(8.6)附近时,土壤对BTA的吸附效果最好。此外,溶液中共存阳离子对土壤吸附BTA有不同的影响,Na+对吸附影响不明显,而不同浓度Ca2+对BTA的吸附有不同程度的促进作用。     

硫化物沉淀法处理含铅废水

采用硫化物沉淀化处理含铅废水,考察了Na2S投加量、反应初始pH等操作条件对铅离子去除效果的影响,以及硫化铅沉淀反应过程的动力学特征,并采用激光粒度分析仪对反应生成的硫化铅沉淀的粒径分布进行了测定。实验结果表明,S2-与废水中Pb2+之间的沉淀反应能较好地符合一级反应动力学特征;Na2S与Pb2+的最佳物质的量之比为3;最佳的反应初始pH为6～9。在最佳操作条件下,Pb2+的平均去除率为99.60%,反应出水中Pb2+平均浓度为0.13 mg/L,低于污水综合排放标准(GB8978-1996)中铅的排放浓度限值。反应生成的硫化铅沉淀的平均粒径为2.62μm,具有较好的沉淀性能,能够通过沉淀的方式与废水分离。     

潜水丁坝在湖滨带生态恢复中的应用

为保护和稳固湖滨带,在太湖梅梁湾进行生态恢复研究,并成功地实施了示范工程.沿湖滨带共构筑14道潜水丁坝,每道长23～28 m,坝间距为40～80 m,坝上种植芦苇和菰.构筑的潜水丁坝能经受住太湖常见大风袭击和湖流淘蚀,芦苇和菰等长势良好,湖滨原有芦苇带在一定水深范围内每年向湖延伸2～5 cm,坝上其他水生植物和底栖动物螺蛳等自然繁衍.潜水丁坝所起作用为利用自然力改变岸边流场,使泥沙在湖滨带预定沉积区内沉积,减缓岸边侵蚀和降低沉积物再悬浮,从而为湖滨带水生植物生长创造良好的生境条件.研究发现,在微风条件下,潜水丁坝群能有效拦截麇集于岸边的蓝绿藻,并在湖滨带进行消化降解.研究提出的构筑潜水丁坝并种植水生植物的方案为湖滨带生态恢复提供了一种新的探索途径.     

斑马鱼对垃圾渗滤液胁迫的生物标志物响应

为了评价垃圾渗滤液的潜在生态风险和对水生动物的毒性,以斑马鱼(Danio rerio)为受试动物,探讨垃圾渗滤液对斑马鱼的急性毒性及其在亚致死浓度胁迫下鱼鳃、肝脏中的超氧化物歧化酶(SOD)、还原型谷胱甘肽(GSH)及Na+,K+-腺苷三磷酸(ATP)酶的变化.结果表明:(1)垃圾渗滤液对斑马鱼的24、48、72、96 h的半致死浓度(LC50)分别为25.58％(体积分数,下同)、24.28％、23.18％和22.51％.(2)斑马鱼肝脏和鱼鳃中的SOD活性、GSH含量和Na+,K+-ATP酶活性的变化可以反映垃圾渗滤液序列间歇式活性污泥法(SBR)出水对斑马鱼的肝脏和鳃都具有损伤作用.(3)斑马鱼鱼体的SOD、GSH和Na+,K+-ATP酶对外界污染物的生物影响是敏感的,可将其作为垃圾渗滤液慢性胁迫的有效生物标志物.     

MgCl2和脱水矿泥对赤泥盐碱性的调控

针对赤泥盐碱性过高造成资源化利用难的问题,采用MgCl2和氧化铝工业固体废物脱水矿泥对赤泥进行盐碱性调控,并依据赤泥的pH、电导率、碱性阴离子(OH-、CO32-、HCO3-、AlO2-)和可溶性盐分阳离子(K+、Ca2+、Na+、Mg2+)质量分数以及黑麦草种子发芽率结果表征盐碱性调控效果.结果表明,当赤泥投加7‰M...     

Impacts of simulated acid rain on recalcitrance of two different soils

Laboratory experiments were conducted to estimate the impacts of simulated acid rain (SAR) on recalcitrance in a Plinthudult and a Paleudalfs soil in south China, which were a variable and a permanent charge soil, respectively. Simulated acid rains were prepared at pH 2.0, 3.5, 5.0, and 6.0, by additions of different volumes of H₂SO₄ plus HNO₃ at a ratio of 6 to 1. The leaching period was designed to represent 5 years of local annual rainfall (1,200 mm) with a 33 % surface runoff loss. Both soils underwent both acidification stages of (1) cation exchange and (2) mineral weathering at SAR pH?2.0, whereas only cation exchange occurred above SAR pH?3.5, i.e., weathering did not commence. The cation exchange stage was more easily changed into that of mineral weathering in the Plinthudult than in the Paleudalfs soil, and there were some K⁺ and Mg²⁺ ions released on the stages of mineral weathering in the Paleudalfs soil. During the leaching, the release of exchangeable base cations followed the order Ca²⁺?>?K⁺?>?Mg²⁺?>?Na⁺ for the Plinthudult and Ca²⁺?>?Mg²⁺?>?Na⁺?>?K⁺ for the Paleudalfs soil. The SARs above pH?3.5 did not decrease soil pH or pH buffering capacity, while the SAR at pH?2.0 decreased soil pH and the buffering capacity significantly. We conclude that acid rain, which always has a pH from 3.5 to 5.6, only makes a small contribution to the acidification of agricultural soils of south China in the short term of 5 years. Also, Paleudalfs soils are more resistant to acid rain than Plinthudult soils. The different abilities to prevent leaching by acid rain depend upon the parent materials, types of clay minerals, and soil development degrees.     

非均相Fenton体系中无机助剂对亚甲基蓝脱色的影响

直接使用有机过渡金属化合物二茂铁作为催化剂，研究了非均相Fenton反应中亚甲基蓝的降解，并考虑了实际排放的印染废水中存在的无机助剂，进一步分析了典型无机助剂CuSO4、NaCl、Na2CO3、Na2SO4、Na2S的存在对该非均相Fenton体系的影响，结果表明：直接使用二茂铁做催化剂反应120min后，亚甲基蓝的剩余率为0．6％，羟基自由基的表观生成率为83．4％。NaCl、Na2CO3、Na2SO4、Na2S的加入会阻碍反应的进行，而CuSO4的加入会促进反应的进行。     

A 3 year study of the aerosol in northwest Saxony (Germany)

Over three years (1993–1995) daily PM-10 aerosol samples were collected at two locations in Saxony, at the rural measurement station Melpitz and at the north-eastern border of Leipzig. By using ion chromatography the water soluble ions Na⁺, NH⁺₄, K⁺, Mg²⁺, Ca²⁺, Cl^-, NO^-₃and SO^2-₄ were analysed daily. Soot was detected by reflectance measurement and gravimetric analysis. Major trends during this period were observed for soot, nitrate, sulphate and calcium. Some components had typical seasonal distributions, e.g. soot, nitrate and sulphate. The rural station Melpitz was influenced more strongly by the power plants at both sides of the Polish border than the urban area of Leipzig-Halle. During inversion periods, maxima of all aerosol components were measured. However, the highest concentrations during inversion periods decreased during the last years at both locations.     

Time Trends and Seasonal Variation of the Rainwater Chemical Composition in Spain

Abstract

A multiple regression model was used to describe temporal variations of the concentrations of H⁺, SO₄ ^{2 -}, NO₃ ^- and NH₄ ⁺ in Spanish rainwater. The model included the effects of linear trend, annual cycle, and precipitation quantity simultaneously.

The model fit very well for SO₄ ^{2 -} and NO₃ ^-, with statistical evidence of annual cycle and effect of precipitation quantity for these two ions and for NH₄ ⁺, but not for H⁺. There is no trend for any ion, with the single exception of a decreasing trend for H⁺ in one of the stations used.     

Some results of snow chemical surveys in the Kunnes River valley,East Tienshan mountains,China

Chemical surveys of snow were carried out in the upper reaches of the Kunnes River, a tributary of the Yili River in East Tienshan Mountains, China. Some surprisingly high values of sodium and potassium (K⁺+Na⁺) ranging from 4.44 to 8.99 mg/l compared with other data from neighboring areas are detected. Moreover, some relative high values of SO₄²⁻ with mean concentration 15.8 mg/l for new snow and 14.40 mg/l for deposited snow, ranging from 10.43 to 23.71 mg/l are also found. Therefore, it is inferred that the sodium and potassium (K⁺+Na⁺) are in the forms of sulfate and that the sources of the sulfate are deserts and some dried lakes in Central Asia. It is also found that there is obviously spatial variation of ions such as K⁺+Na⁺, Ca²⁺, SO₄²⁻ and HCO₃⁻. The concentrations of K⁺+Na⁺ and SO₄²⁻, and that of Ca²⁺ and HCO₃⁻ have similar spatial pattern. The temporal pattern of ion concentration of new snow is considered to be mainly controlled by the depth and area of snow cover in the study area and in the areas to the west.     

Seasonal variations of acidic air pollutants in Seoul,South Korea

The annular denuder system (ADS) was used to characterize seasonal variations of acidic air pollutants in Seoul, South Korea. Fifty- four 24 h samples were collected over four seasons from October 1996 to September 1997. The annual mean concentrations of HNO₃, HNO₂, SO₂ and NH₃ in the gas phase were 1.09, 4.51, 17.3 and 4.34 μg m^-3, respectively. The annual mean concentrations of PM_2.5(d_p≤2.5 μm in aerodynamic diameter, 50% cutoff), SO^2-₄, NO^-₃ and NH⁺₄ in the particulate phase were 56.9, 8.70, 5.97 and 4.19 μg m^-3, respectively. All chemical species monitored from this study showed statistical seasonal variations. Nitric acid (HNO₃) and ammonia (NH₃) exhibited substantially higher concentrations during the summer, while nitrous acid (HNO₂) and sulfur dioxide(SO₂) were higher during the winter. Concentrations of PM_2.5, SO^2-₄, NO^-₃ and NH⁺₄ in the particulate phase were higher during the winter months. SO^2-₄, NO^-₃ and NH⁺₄ accounted for 26–38% of PM_2.5. High correlations were found among PM_2.5, SO^2-₄, NO^-₃ and NH⁺₄. The mean H⁺ concentration measured only in the fall was 5.19 nmole m^-3.     

共存物质对重金属絮凝剂 MCC 除镉性能的影响简

为进一步拓展天然高分子絮凝剂壳聚糖的应用范围，以壳聚糖、L-半胱氨酸为原料，通过酰胺化反应制备一种具有重金属捕集功能的高分子重金属絮凝剂-2-氨基-3-巯基丙酰壳聚糖（MCC），研究了水体中常见的阴阳离子、有机配位剂及浊度对MCC除镉性能的影响，探讨了絮体形貌与絮体分形维数及絮凝除镉效果间的关系。结果表明，Na⁺、Cl^-、NO₃^-、F^-、SO₄^2-的存在对MCC除Cd²⁺均有促进作用，Ca²⁺表现为明显的抑制作用；低浓度的EDTA对除镉有促进作用，随着EDTA浓度的增大，逐渐转为抑制作用；低浓度的腐殖酸对MCC去除Cd²⁺有显著的促进作用；在一定范围内，浊度可促进 MCC对Cd²⁺的去除；絮体间空隙越多，絮体分形维数越小，除镉效果越好。     

Multivariate Space Analysis of the Major Precipitation Ions over Europe, 1986–1997

ABSTRACT

The annual average concentrations (1986–1997) of the major ions SO₄ ^2-, NO₃ ^-, Cl^-, NH₄+, Na+, Mg²+, Ca²+, and K+ in precipitation are analyzed for selected EMEP stations. The objective is to determine the ion patterns or typologies in precipitation by principal component analysis (PCA) combined with a cluster analysis. SO₄ ^2- and NO₃ ^- ions are predominant in central and eastern Europe. This area corresponds to high emissions of SO₂ and NO₂. Sea spray ions are predominant in coastal sites. The soil components show an important contribution in southern Europe, possibly due to the soil dust transported from northern Africa.     

几种试剂对硝酸根光催化脱色甲基橙的影响

以NO^-₃为光催化剂，在紫外灯照射下，对甲基橙溶液进行光催化脱色。结果表明，叔丁醇、甲醇和乙醇对催化脱色反应有抑制作用; KBr和Na₂SO₄对脱色反应均有促进作用;而且KBr的加入量存在最佳值; Na₂SO₄的促进作用随Na₂SO₄的量的增加逐渐增强。Na₂CO₃的存在对甲基橙的脱色反应没有影响。K₂S₃O₈和NO^-₃之间存在较强的协同作用；KIO₃和NO^-₃之间存在相加作用；KBrO₃和NO^-₃之间存在拮抗作用。     

Influence of meteorological factors and polluting environment on rain chemistry and wet deposition in a rural area near Chimay,Belgium

This paper focuses on a detailed analysis of the effects of meteorological factors explaining the variability of rain composition.Inorganic composition of 113 individual rain events was measured from May 2002 to October 2005 at a rural site near Chimay, in the western part of the Belgian Ardennes. Original models were fitted for each studied ion (H⁺, Mg²⁺, Ca²⁺, K⁺, NH₄⁺, Na⁺, Cl⁻, NO₃⁻ and SO₄²⁻) to relate rain event concentration or wet deposition to the rainfall volume (R), the length of the antecedent dry period (ADP), the volume of the previous event (R_prev) as well as to the mean wind speed and the prevailing wind direction during both the dry and the rainy periods. These variables explained from 32% (H⁺) to 69% (NO₃⁻) of rain concentration variability. Concentrations decreased logarithmically with increasing R values except in case of H⁺ for which a positive effect of rain volume on rain concentration was observed. ADP affected positively rain concentrations of all ions excluding K⁺ and H⁺ for which, respectively, a nonsignificant and a negative effect of this variable was observed. Increasing R_prev strengthened the effect of the variable R on H⁺, Mg²⁺, Ca²⁺, Na⁺, NH₄⁺ and SO₄²⁻ concentrations while it softened the effect of ADP on NO₃⁻ concentrations. Wind speed and direction during dry and rainy periods explained together from 8% (K⁺) to 38% (Na⁺) of rain concentration total variability. R² coefficients of the wet deposition models ranged from 0.51 (K⁺) to 0.79 (SO₄²⁻). For all ions, wet deposition increased significantly with increasing R values while the effects of the other variables were similar to those on concentrations. Wind conditions during dry and rainy periods explained from 4% (H⁺) to 24% (Na⁺) of wet deposition total variability. On an annual scale, the total dry period duration, the total rainfall volume as well as the shape of the distributions of the length of the antecedent dry periods and of the rain event volume are important parameters that influence annual wet deposition.