酸化土壤活性铝溶出及形态变化的初步研究

用模拟酸雨酸化浙江省３种主要类型土壤，研究了酸化土壤活性铝的溶出和铝的形态变化。结果表明：酸雨对强酸性土壤（ｐＨ＜５）中活性铝的释出有一定促进作用，活性铝以Ａ１￣（３－）离子为主。当土壤ｐＨ值＞５时．活性铝以单聚羟基铝为主。酸化土壤中的活性铝主要是由土壤中固相的Ａｌ（ＯＨ）转化而来。     

聚硅氯化铝（PASC）的形态分布及转化规律：Ⅱ.^27Al—NMR法研究PASC溶 …

采用＾２７Ａｌ－ＮＭＲ法比较研究了ＰＡＳＣ与ＰＡＣ中铝的形态分布。实验结果表明,在ＰＡＳＣ中,由于聚硅酸与铝水解聚合物产物间的相互作用,使得铝的水解聚合形态分布及转化情况发生了变化。在相同Ｂ值条件下,ＰＡＳＣ中Ａｌ单和Ａｌ１３的含量低于ＰＡＣ中相应Ａｌ单和Ａｌ１３的含量,而ＰＡＳＣ中Ａｌ其它的含量大于ＰＡＣ中Ａｌ其它的含量,其差值随着碱化度（Ｂ）和Ａｌ／Ｓｉ摩尔比的减小而增大。     

Al—Ferron逐时络合比色法研究PACS中铝的水解聚合形态

制备了碱化度及不同Ａｌ＾３＋／ＳＯ＾２＝４摩尔比的系列ＰＡＣＳ，用Ａｌ－Ｆｅｒｒｏｎ逐时络合比色法研究了铝的形态分布，考察了碱化度，Ａｌ＾３＝／ＳＯ＾２＝４摩尔比，稀释作用及ｐＨ值对铝的形态分布的影响。     

Al13形态分离纯化方法的初步研究

对ＳＯ＾２－４／Ｂａ＾２＋法分离提纯Ａｌ１３形态的影响因素进行了研究,实验结果表明,聚合铝浓度、ＳＯ４／Ａｌ比、Ｂａ／ＳＯ４摩尔比、以及超声反应时间对分离效果上具有较大的影响。较高浓度的聚合铝利于沉淀的形成与分离。同时选用１：１的ＳＯ４／Ａｌ与Ｂａ＾２＋的共存对形态分析不产生影响,形态鉴定结果表明,经过上述分离条件所得产物形态为Ａｌ１３。     

聚硅氯化铝（PASC）的形态分布及转化规律：Ⅲ.Al—Ferron逐时络合比？…

本文对Ａｌ－Ｆｅｒｒｏｎ逐时络合比色法和＾２７Ａｌ－ＮＭＲ法对ＰＡＳＣ和ＰＡＣ中铝的形态分布测定结果进行了对比分析的讨论。结果表明。在ＰＡＣ中,Ａｌ１３和Ａｌｂｈ之间具有良好的对应关系。Ａｌ１３／Ａｌｂ比值为１．０左右。但对ＰＡＳＣ而言,情况有所不同,在低碱化度（Ｂ）和低Ａｌ／Ｓｉ摩尔比情况下,Ａｌ１３和Ａｌｂ之间的不存在对应关系,Ａｌ１３和Ａｌｂ比值远远小于１．０,随着Ｂ值和Ａｌ／Ｓｉ摩尔比的升     

土壤上铍的存在形态及提取研究

本文对三种不同类型土壤中铍的存在形态及提取进行了研究,并做了原土铍和外加铍形态提取对照试验,选择了各形态合适的提取剂,建立了土壤铍形态连续提取方法,对提取机理和形态分布规律进行了探讨。此外,还对土壤提取的有效铍与盆栽植物吸收铍量的相关性进行了初步研究。     

聚硅氯化铝（PASC）的形态分布及转化规律：Ⅰ.Al—Ferron逐时络合比色？…

采用Ａｌ－Ｆｅｒｒｏｎ逐时络合比色法比较研究了ＰＡＳＣ与ＰＡＣ中铝的形态分布及转化规律。实际结果表明,在ＰＡＳＣ中,由于聚硅酸与铝水解聚合产物的相互作用,使得铝的水解聚合形态分布及转化情况发生了变化。     

Al—Ferro络合比色动力学特征与聚合铝溶液形态

本文考察了Ａｌ－Ｆｅｒｒｏｎ逐时络合比色反应的假一级动力学特征,并探讨了其动力学参数的变化规律与聚合铝溶液形态分布和转化间的关系。结果表明。「Ａｌｂ」０与「Ａｌｂ」间的差值大小值ｒＯＨ的变化情况可反映Ａｌｂ的具体组分分布的复杂程度;Ｋｂ值的变化一定程度上可为Ａｌ１３是Ａｌｂ 态的主要组分提供佐证。     

土壤中铍的存在形态及提取研究

本文对三种不同类型土壤中铍的存在形态及提取进行了研究,并做了原土铍和外加铍形态提取对照试验,选择了各形态合适的提取剂,建立了土壤铍形态连续提取方法,对提取机理和形态分布规律进行了探讨。此外,还对土壤提取的有效铍与盆栽植物吸收铍量的相关性进行了初步研究。     

连续浸提技术测定土壤和沉积物中硒的形态

本文建立了土壤和沉积物中硒的形态分析方法，应用连续化学浸提技术将土壤和沉积物进行连续五次抽提，根据不同形态硒的溶解度，将土壤和沉积中的硒分为可溶态（水溶态）、可交换态及碳酸盐结合态、铁－锰氧化物结合态、有机物－硫化物结合态及元素态、残渣态五种结合形态。种形态硒分级浸提的相对标准偏差均小于４．０％，总回收率（即：五种形态和与总硒的比值）为９３．２－９４．４％。     

Distributions of heavy metals in the sediments of South Korean harbors

Mechanisms of natural attenuation of arsenic (As) by wetland plants may be classified by plant uptake and adsorption and/or co-precipitation by iron (oxy)hydroxide formed on the root surface of plants or in rhizosediment. A natural Cattail (Typha spp.) wetland impacted by tailings containing high levels of As from the Myungbong abandoned Au Mine, South Korea was selected, and the practical capability of this wetland to attenuate As was evaluated. The As concentrations in the plant tissues from the study wetland were several-fold higher than those from control wetland. SEM-EDX analyses demonstrated that iron plaques exist on the rhizome surface. Moreover, relatively high As contents bonded with hydrous iron oxides were found in the rhizosediments rather than in the bulk sediments. It was revealed through the leaching and sequential extraction analyses that As existed as more stable forms in the wetland sediment compared with adjacent paddy soil, which is also contaminated with As due to input of mine tailings. The As concentration ratios of extracted solution to sediment/soil represented that the wetland sediment showed significant lower values (10-fold) rather than the paddy soil with indicating high As stability. Also, As in the wetland sediment was predominantly bonded with residual phases on the basis of results from sequential extraction analysis. From these results, it is concluded that transformation of As contaminated agricultural field to wetland environment may be helpful for natural attenuation until active remediation action.     

Natural attenuation of arsenic in the wetland system around abandoned mining area

Mechanisms of natural attenuation of arsenic (As) by wetland plants may be classified by plant uptake and adsorption and/or co-precipitation by iron (oxy)hydroxide formed on the root surface of plants or in rhizosediment. A natural Cattail (Typha spp.) wetland impacted by tailings containing high levels of As from the Myungbong abandoned Au Mine, South Korea was selected, and the practical capability of this wetland to attenuate As was evaluated. The As concentrations in the plant tissues from the study wetland were several-fold higher than those from control wetland. SEM-EDX analyses demonstrated that iron plaques exist on the rhizome surface. Moreover, relatively high As contents bonded with hydrous iron oxides were found in the rhizosediments rather than in the bulk sediments. It was revealed through the leaching and sequential extraction analyses that As existed as more stable forms in the wetland sediment compared with adjacent paddy soil, which is also contaminated with As due to input of mine tailings. The As concentration ratios of extracted solution to sediment/soil represented that the wetland sediment showed significant lower values (10-fold) rather than the paddy soil with indicating high As stability. Also, As in the wetland sediment was predominantly bonded with residual phases on the basis of results from sequential extraction analysis. From these results, it is concluded that transformation of As contaminated agricultural field to wetland environment may be helpful for natural attenuation until active remediation action.     

Evaluating the respiratory bioaccessibility of nickel in soil through the use of a simulated lung fluid

Simulated lung fluids are solutions designed to mimic the composition of human interstitial lung fluid as closely as possible. Analysis of mineral dusts using such solutions has been used to evaluate the respiratory bioaccessibility of various elements for which solubility in the lungs is a primary determinant of reactivity. The objective of this study was to employ simulated lung fluid analysis to investigate the respiratory bioaccessibility of nickel in soils. Current occupational guidelines in Australia regulate nickel compounds in terms of water solubility, though this may not be an accurate estimation of the total nickel that will dissociate in the lungs. Surface soils were collected from the city of Kalgoorlie in Western Australia, the site of an operational nickel smelter and metal mining activities. The fraction of the samples less than 10 μm was extracted from the soil, and it was this sub-10-μm fraction that was found to hold most of the total nickel present in the soil. The fine fraction was analyzed using a simulated lung fluid (modified Gamble’s solution) to isolate the nickel phases soluble in the lungs. In addition, a sequential extraction was employed to compare the bioaccessible fraction to those dissolved from different binding forms in the soil. In all samples, the simulated lung fluid extracted more nickel than the two weakest leaches of the sequential extraction combined, providing a more representative nickel bioaccessibility value than the current water leach method.     

Simple assessment of the reactive aluminium in sediments

The mobility of aluminium in sediments was evaluated through a one-step extraction with a strong chelating agent. Single and sequential extraction procedures for the extraction of Al were applied to four sediments from a polluted region. A single-step extraction with 0.05 mol L⁻¹ ethylenediaminetetraacetic acid (EDTA) was used, and compared with a standardized SEP as reference. The Al contents extracted into Na₂EDTA were in good agreement with the sequential extraction that yeilds mobile and potentially mobile portion of Al. Extracted EDTA contents make up more than 70% of the first-three-step sum of the five-step extraction procedure. Thus, Na₂EDTA extraction of Al could be applied to assess aluminium mobility changes in sediments and soils.     

土壤中锰氧化物的形态及其化学提取方法综述

土壤中锰元素主要来自于成土母质,风化后的锰主要以锰氧化物形式存在于土壤中.锰氧化物因具有比表面积大、表面电荷低、对金属的亲合力强、氧化还原电位高等特性,对土壤中痕量金属的环境行为存在重要影响.化学提取方法是研究土壤中不同固相组分的重要手段.本文首先从土壤中锰的来源及主要存在形态出发,介绍了不同价态锰(+2、+3、+4)...     

土壤中锗的形态提取和形态分布研究

本文对不同类型土壤中锗的存在形态、开态分布和有效锗进行了研究,选择了合适的提取剂,建立了土壤中锗的形态连续提取方法。探讨了影响土壤中锗形态分布的因素。锗在土壤中主要以残渣态、酸可提态和有机结合态形式存在,土壤有机质能富集锗,此外,还试验了土壤有效锗与盆栽玉米吸收锗的相关性。     

外加锌在土壤中形态的研究

本文采用化学逐级提取法对吸附锌后的土壤分别提取了交换态、CaCO_3结合态、氧化物结合态和有机质结合态的锌量,并讨论pH、温度和溶液中锌离子浓度对不同形态锌分布的影响。实验结果表明:外加锌被石灰性土壤吸附后,高pH值(7.5)时形态分布为:CaCO_3结合态≥交换态>氧化物结合态>有机质结合态;低pH值(5.5)时则为:交换态>CaCO_3结合态>氧化物结合态>有机质结合态。各形态锌的分配系数还受到吸附时的温度和溶液中锌离子浓度的影响。     

Soil remediation using in situ immobilisation techniques

The main objective of this study was to investigate the efficiency of different substrates to reduce the extraction of heavy metals concentration in a heavily contaminated soil. Two contaminated soils by Cu and Zn were used to evaluate the effectiveness of eight substrates (calcium carbonate, bentonite, kaolinite, charcoal, manganese oxide, iron oxide, zeolite, phosphate) to reduce metal availability and to study the change of metals speciation in different forms using sequential extraction technique (single step). Sequential extraction technique (single step, 0.11 M acetic acid, HONH₃Cl, H₂O₂+NH₄OAc, Aqua regia) was applied on contaminated soils after and before treatment to evaluate metals speciation. Results indicate that the most effective treatments in decreasing available metal concentrations were calcium carbonate, zeolite and manganese or iron oxide. Metal sequential fractionations indicate that the exchangeable fraction of Cu and Zn in contaminated soils can be transformed into unavailable forms after chemical remediation.     

Modelling the concentrations of dissolved contaminants (Cd,Cu, Ni,Pb, Zn) in floodplain soils

Central European floodplain soils are often contaminated with potentially toxic metals. The prediction of their aqueous concentrations is a prerequisite for an assessment of environmental concerns. We tested the aqueous concentrations of cadmium (Cd), copper (Cu), nickel (Ni), lead (Pb) and zinc (Zn) derived from multi-surface adsorption modelling (on hydrous iron, aluminum and manganese oxides, clay and soil organic matter) against those analyzed in situ in the soil solution of four horizons of floodplain soils at the Elbe River, Germany. The input data for the reactive metals were derived from a seven-step sequential extraction scheme or from extraction with 0.43 M nitric acid (HNO₃) and evaluated in four modelling scenarios. In all scenarios, measured and modelled concentrations were positively related, except partially for Pb. Close reproduction of the measured data was obtained using measured data of accompanying cations and anions together with amounts of reactive metals from both the sequential extraction or from 0.43 M HNO₃ extraction, except for Cu, which was often strongly overestimated, and partially Cd. We recommend extraction with 0.43 M HNO₃ to quantify reactive metals in soil because the modelling results were metal-specific with better or equal results using the single extractant, the application of which is also less laborious. Approximations of ion concentrations and water contents yielded similar results. Modelled solid-phase speciation of metals varied with pH and differed from that from sequential extraction. Multi-surface modelling may be an effective tool to predict both aqueous concentrations and solid-phase speciation of metals in soil.