胡敏酸在土壤中的迁移

研究了不同条件下胡敏酸在土壤中的迁移过程.结果表明,其迁移过程表现出较大的差异,在溶液pH值、胡敏酸浓度和溶液流速均较高时,胡敏酸迁移的阻滞因子和在土壤中的吸附系数均较低,有利于胡敏酸在土壤中的迁移;在溶液pH值、胡敏酸浓度和溶液流速均较低时,土壤对胡敏酸迁移的阻滞作用较大.胡敏酸的迁移还与土壤性质有关,土壤黏粒含量和阳离子交换量越高,胡敏酸在土壤中吸附的越多,越不利于迁移.在土壤中的吸附是胡敏酸迁移的主要控制因素,在预测胡敏酸在水土环境中迁移时,应该充分考虑不同条件下胡敏酸在不同性质土壤中的吸附.     

沈阳市降雪中PFOS和PFOA污染现状调查

通过调查降雪中PFOS和PFOA的浓度,阐明了沈阳市大气中PFOS和PFOA的污染状况和污染规律.2006-02-06采集沈阳市区和郊区共计36个采样点的降雪样品,2006-02-25在其中5个采样点再次采集降雪样品.固相萃取融雪水中的PFOS和PFOA,利用LC-MS-SIM法测定样品中PFOS和PFOA浓度.全部样品中均检出PFOS和PFOA.2006-02-06降雪中PFOS和PFOA的浓度几何平均值分别为2.0 ng·L^-1（范围：0.4～46.2 ng·L^-1）和3.6 ng·L^-1（范围：1.6～22.4 ng·L^-1）,95%置信区间分别为1.5～2.8 ng·L^-1和3.1～4.2 ng·L^-1.PFOS和PFOA的最高浓度同时出现在郊区采样点朱尔屯,市中心区2种物质的浓度呈显著正相关.2006-02-25的5个采样点降雪中PFOS和PFOA的浓度几何平均值均为2.2 ng·L^-1.2次降雪中PFOS浓度差异不显著,2006-02-25降雪中PFOA浓度高于2006-02-06.结果表明,沈阳市区和郊区降雪中广泛存在PFOS和PFOA污染,局部区域可能存在共同的PFOS和PFOA污染来源;沈阳地区有较稳定的PFOS来源持续向大气中输送该类物质;PFOS和PFOA的环境行为可能不同.     

二级SBR系统处理染料废水长期运行的稳定性

考察了处理染料废水的二级SBR系统在连续运行120个周期过程中的稳定性.系统的运行先后经历了低染料浓度和高染料浓度2种情况.试验发现在长期运行过程中,二级SBR系统对进水水质及操作条件具有良好的适应性;能够有效去除废水中的污染物,对染料的平均去除率为81%～92.5%,对COD的平均去除率为89.4%～93.1%;出水水质比较稳定.在二级SBR系统中,厌氧污泥活性高,降解污染物能力强;好氧活性污泥形成团簇状结构,有利于稳定出水水质.     

重金属絮凝剂PEX对水中铅的去除性能研究

在合成高分子重金属絮凝剂聚乙烯亚胺基黄原酸钠(PEX)的基础上,研究了该絮凝剂处理含铅离子废水的效能,并对一些影响因素进行了考查。研究结果表明:高分子重金属絮凝剂PEX对铅离子的捕集效率较高,去除率可达90%以上;pH值对PEX去除铅离子有一定的影响,pH=5.0时去除效果最好;Mg2+﹑Ca2+、EDTA、柠檬酸、焦磷酸钠以及致浊物质的存在均能促进铅离子的去除;絮体残渣稳定性好,金属离子易回收,回收率可达到70.0%。     

滇池流域土壤活性腐殖质及其主要组分的紫外-可见与三维荧光光学特性

利用紫外-可见光谱和三维荧光光谱技术,结合土壤腐殖质及腐殖质组分(胡敏酸、富里酸)中的有机碳含量,研究了滇池流域土壤活性腐殖质及其组分胡敏酸和富里酸的光谱特征.结果表明,滇池流域土壤活性腐殖质中富里酸含量高于胡敏酸,流域范围内土壤活性腐殖质及其组分含量分布不均匀,活性腐殖质、胡敏酸和富里酸含量的变异系数分别达37.7%、36.4%、40.9%.土壤活性腐殖质及其组分胡敏酸和富里酸的碳含量均表现为菜地荒地草地湿地.光谱特征结果表明,滇池流域土壤活性腐殖质主要由自生源物质和经一定程度降解后的外源物质共同组成.此外,自生源性与光化学及生物活性具有正相关关系.因此,具有弱自生源性的滇池流域土壤活性腐殖质所具有的光化学和生物活性较弱.     

Adsorption mechanism of phenolic compounds from aqueous solution on hypercrosslinked polymeric adsorbent

The adsorption of two phenols, namely, phenol and salicylic acid(SA) onto a water-compatible hypercrosslinked polymeric resin (NJ-8) were studied in terms of pseudo-second-order and first order mechanisms for chemical sorption as well as an intraparticle diffusion mechanism process. Kinetic analysis showed that the intraparticle diffusion process was the essential rate-controlling step. The activation energies of sorption have also been evaluated with the pseudo-second-order and intraparticle diffusion constants, respectively. Adsorption equilibrium data were well fitted by the Langmuir, Freundlich and Redlich-Peterson isotherms. Adsorption was exothermic and basically of a type of transition between physical and chemical character. The sorption capacity was higher for SA due to its more hydrophobic. Phenol has a higher adsorption enthalpy since it could form stronger hydrogen bonding on NJ-8.     

华南地区高山酸沉降化学研究

1987—1989年春季,在华南地区衡山、狮子山、苗儿山和白云山观测到华南高山降水酸化,各测点降水pH<5.6的频率大于68％,平均pH值在3.56—4.85之间,分析了高山降水的化学特征,及其与高山的地理环境等因素的关系.结果表明,高山雨水与高空云水有相似性,狮子山和白云山的云雾水主要属地形云,受局地源的影响更为严重,化学性质更接近于地面雨水.     

镉铅在粘土上的吸附及受腐殖酸的影响

试验研究了镉和铅2种重金属在蒙脱土和高岭土上的吸附,以及外加腐殖酸的3种组分（富里酸、棕色胡敏酸和灰色胡敏酸）的影响。镉铅在粘土上的吸附随着介质pH的升高而增加。在pH4-8范围内的任意pH点,镉在高岭土上的吸附量因富里酸而降低,因2种胡敏酸而升高;当pH值高于6时,吸附量急剧增加。外加富里酸使得铅在粘土上的吸附在pH＞6时意外出现随着介质pH而降低的趋势。     

海南五指山和福建武夷山降水离子组成及来源

分析海南五指山及福建武夷山大气背景点2008年1月—2009年12月的降水pH及离子组成,并探讨离子来源. 结果表明:海南五指山监测点降水年均pH约为564,呈中性;武夷山监测点降水的年均pH约为530,呈弱酸性. 2个监测点降水中的SO₄2-、NO₃-和NH₄+的浓度和占总离子浓度的59%左右,表现出与城市相似的组成特征,表明这2个监测点的降水已经受到人类活动的影响. 降水酸度除受SO₄2-和NO₃-的影响外,还受到NH₄+、Ca2+和Mg2+等碱性物质的中和作用. 相对酸度和中和因子的计算表明,五指山和武夷山监测点降水酸度分别有85%和76%被碱性物质NH₄+和Ca2+中和. 富集因子计算及来源定量分析表明,这2个监测点已受到人为源的影响,人为源的贡献大于海洋源及地壳源. 武夷山监测点88%的Ca2+和56%的K+均来自人为源,主要是受人为污染物长距离传输及生物质燃烧的影响.      

An assessment of historical change in two northern Minnesota lakes

Two northern Minnesota lakes that had been studied in detail 22 years earlier (1958) were restudied to determine the extent of alteration in ecological conditions. Approximately one year after the original investigation, a coal-fired power plant, which incremented sulfate loading by about 6 kg/ha-yr, began operation nine miles away. These lakes lie within a region judged susceptible to acidic precipitation, though each lake, based on its buffering capacity, would be judged only moderately sensitive. In spite of the influence of this plant and other anthropogenic inputs, the change in lake ecology was apparently minimal. Water clarity decreased in both lakes and some alteration in zooplankton community structure was observed. The long-term utility of lake surveys depends upon how carefully and completely conditions can be reconstructed from records and reports. Past surveys generally omit measures of variability for the data, allowing only qualitative comparisons to be drawn. In order to judge the graded responses of aquatic ecosystems, necessary to sound management, quantitative measures are needed.Deceased.