淀山湖上覆水与沉积物孔隙水中重金属的分布特征

研究了淀山湖上覆水和沉积物孔隙水中Pb ,Cd,Cr,Cu ,Fe和Mn的浓度及Eh 分布 ,分析了孔隙水中重金属的扩散通量 .结果表明 ,淀山湖中重金属的浓度由高到低依次为 :Mn >Fe >Cr,Cu ,Pb >Cd ;Fe和Mn在孔隙水中的浓度远远大于它们在上覆水中的浓度 ,表层沉积物孔隙水中Pb ,Cd ,Cr,Cu的浓度稍大于它们在上覆水中的浓度 ;沉积物中的重金属可能按照浓度梯度经孔隙水从沉积物向上覆水中扩散而最终影响上覆水的水质     

表面活性剂对可离子化有机化合物在黄土中吸附行为的影响

研究了2，4-二氯苯酚、2，4-二硝基苯酚和苯甲酸三种可离子化有机化合物在天然黄土和阳离子表面活性剂改性黄土中的吸附行为。讨论了DH值、离子强度和二价重金属阳离子对可离子化有机化合物在改性黄土中吸附的影响。提出了可离子化有机化合物在改性黄土中的吸附模型，吸附等温曲线可分解为两条分别代表离子和非离子形态的等温吸附曲线；其吸附行为可用双模式吸附理论来解释。在2，4-二硝基苯酚共存时，苯甲酸在改性黄土中的吸附量减小，证明竞争吸附的存在。     

Reconnaissance soil geochemical survey of Gibraltar

The extreme density of population of Gibraltar, situated at the southern tip of Spain, exerts considerable pressure on land use and thus future planning is of utmost importance. An initial reconnaissance soil geochemical survey of Gibraltar was based on 120 surface samples (0–15 cm) taken from a wide range of exposed, either bare soil or vegetated sites, to provide the optimum geographical distribution. The total elemental concentrations of 26 elements (Li, Na, K, Be, Mg, Ca, Sr, Ba, Al, La, Ti, V, Cr, Mo, Mn, Fe, Co, Ni, Cu, Ag, Zn, Cd, Pb, P, S, As) were determined by nitric/percholric acid digestion followed by inductively coupled plasma-atomic emission spectrometry (ICP-AES) analysis. The reconnaissance data shows that the spatial distribution of various elements depended on previous and present land use. Most elements (Ca, Cr, Mg and Mn excluded) exhibited relatively high concentrations in civilian and natural soils. Trends have been established for many elements, and concentrations exceeding guideline values have been found in certain areas of Gibraltar. This reconnaissance of Gibraltar is at present being followed by a more detailed baseline geochemical survey, which will establish the extent and magnitude of the variations in major and trace elements in soils and dusts, assess the impact of industrial, commercial and urban development on the geochemical landscape and to make recommendations concerning sustainable development.     

Heavy Metals in the Bed and Suspended Sediments of Anyang River, Korea: Implications for Water Quality

The objective of this study is to compare Anyang River bed sediments with water chemical composition and to assess the anthropogenic chemical inputs into the river system. Eight sampling locations were chosen along the river channel. Bed and suspended river sediments and water samples were collected, and analyzed for their chemical and physical composition. Data revealed that trace element concentrations in the river water were generally below world average, except for As, Mn, Ni and Cr. Among the three phases: water, bed and suspended sediment, more than 99% of the trace elements was associated with the bed sediment. Concentrations of trace elements in the sediment were a function a particle size distribution and organic content. The calculated degrees of enrichment based on the least influenced sample (ASD 1) indicated the river sediments were enriched with respect to background. The enrichment factors for Pb, Zn and As were relatively lower than for Cr, Co, Ni and Zn. The difference in the enrichment seems to reflect the human activities influence in the basin, and specially for Cd. Speciation of the elements in the five different chemical forms in the sediment by sequential extraction indicated that the reducible fraction was predominant for Fe, Zinc and Cu showed an irregular variation among the different fractions; whereas, Cd and Pb were more regular. Zinc and Cu highly existed mostly in exchangeable forms. Acid soluble and reducible forms were also important for most metals. The speciation implies that the metals associated with the sediment are subject to release into water bodies as goechemical variables (pH and Eh) change. Currently, the introduced metals are deposited near the source area and are mostly associated with the sediment, implying that the river bed sediment acts mainly as a sink, rather than a pool. The accumulated and enriched toxic trace elements can pose a potential pollution of river water.     

球衣菌对重金属离子的耐受性及其吸附能力

研究了球衣菌对重金属离子Ag 、Hg2 、Pb2 、Zn2 的耐受性及生物吸附情况,并着重对Pb2 的吸附行为及工艺条件进行了探讨.结果表明:球衣菌对 4种重金属离子均有不同程度的耐受性,其中对Pb2 具有较大的耐受力.不同生长阶段的菌体对重金属离子的敏感性也不同.球衣菌对Pb2 的吸附作用是一种快速而非依赖温度的过程.在ρi(Pb2 ) =5mg/L,菌体浓度ρb=0. 2g/L,θ=30 ~35℃,pH=6. 5,菌龄a=32h,吸附时间t=30min时,吸附率可达95. 6%,吸附量为 23. 9mg/g. 图 3参 10     

盾壳霉CCTCC M203020的生长特性及其应用潜力

以油菜菌核病病株菌核为诱饵，从油菜地中分离筛选得到一株盾壳霉(Coniothyrium minitans CCTCC M203020)．以生物防治能力好的CBS148．96为对照菌株，比较了两者在油菜叶上对油菜菌核病菌抑制作用和在土壤中对菌核的致腐能力及条件．结果表明：C．minitans CCTCC M203020对油菜菌核病菌的抑制作用及适用的pH范围(4．0～7．0)均优于CBS148．96，适片于油菜菌核病的生物防治．具体表现在：(1)C．minitans CCTCC M203020能够完全限制病原菌在叶面的进一步扩展(已萌发孢子率为800A时)，而CBS148．96则不能；(2)C．minitaras CCTCC M203020与CBS148．96的生长特性及培养条件相近，但其菌体生长和孢子产量分别高出60％和12％，并发现该菌株在PDA上产生孢子的最短周期是3．5～4d，较优培养条件为：20℃、初始pH5．0～6．2、空气湿度90％～97％；敛腐菌核的较优条件为：10^1～10^4孢子／菌核，土壤湿度80％～100％，pH4．0～7．0，图7参19     

丽水小盆地型城市酸雨现状及成因分析

根据浙江省丽水市 1 986— 2 0 0 2年酸雨监测数据 ,对该市酸雨污染的现状特征及成因进行了分析。结果表明 ,丽水市酸雨污染严重 ,并呈逐年加重的趋势。冬、春季酸雨率高 ,降水 pH值低 ;降水的主要离子SO42 -与NO-3比值逐年下降 ,说明大气污染有从煤烟型转为煤烟型与机动车尾气混合型的趋势 ;煤耗量、地型地貌特点、低空逆温层频率、地面弱风频率对酸雨率和降水 pH值有明显的影响。     

广州市蔬菜地土壤重金属污染状况调查及评价

探讨了广州市蔬菜地土壤重金属污染状况,测定了95份土壤样品中铅、镉、铬、砷、汞的含量水平。土壤中铅、镉、铬、砷、汞的含量分别在6.44～153.10mg/kg、0-0.682mg/kg、5.82～101.60mg/kg、0.04～45.36mg/kg、0.01～O.32mg/kg之间。就污染的普遍性而言,铅污染最为普遍,其次是砷污染;就污染的程度而言,镉污染最严重.其次为砷、汞。对比今昔污染变化.广州市土壤污染治理已取得显著成效,但仍需努力。土壤中镉、砷、汞三种元素的变异系数,特别是镉的变异系数较大,这可能预示着点源性污染的存在。     

微生物对土壤环境中重金属活性的影响

各种工农业生产和家庭消费引起的重金属在环境中的释放 ,以及由此带来的环境胁迫和破坏 ,呈加剧的趋势 .在全球范围内 ,人类活动引起的Ｐｂ ,Ｃｄ,Ｖ与Ｚｎ的释放量分别是自然情况下的 12 ,5 ,3和 3倍 .Ｓｂ ,Ａｓ ,Ｃｒ,Ｃｕ ,Ｈｇ,Ｎｉ,Ｓｅ等的人为释放量或超过自然释放量 ,或与自然释放量持平[1] .土壤是重金属离子的源和汇 ,土壤中的重金属离子可以多种形态存在 ,如可溶态、交换态以及与不同土壤固相组分如碳酸盐、铁锰氧化物、有机质、残渣物质结合的形态[2 ] .重金属在土壤中的活性和生物有效性受到多种因素的制约 ,特别是各种有机胶…     

东北过伐林灌木层物种多样性与林分因子的典型相关分析

研究林分特征尤其是经营上可以控制的因子对生物多样性的影响，将有助于制定合理的经营措施来维持和保护生物多样性，本文作者以我国东北过伐林区3种典型天然林类型为对象，采用典型相关分析方法，研究影响灌木层物种多样性的主要因子。结果表明：影响灌木层物种多样性的主要因子包括土壤含水率，树种多样性和林分密度；灌木层多样性组的变异被林分组第一典型变量解释的比例为68.32%,仍有31.68%的变异不能得到解释。