底泥中重金属毒性的室内孔隙水分析技术

根据孔隙水中重金属的浓度可以判定底泥中重金属的毒性但获得真正的底泥孔隙水十分困难。本文提供了一套简便易行的室内原状孔隙水取样技术,将碳化硅砂芯埋入底泥,添加表层水并静置９０ｄ,通过渗滤获得孔隙水,测定孔隙水中重的浓度,所得结果与微生态系统暴露试验中生物指示的重金属的毒性大小相吻合,与生物积累重金属的浓度显著正相关。     

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     

基于毒性效应的间隙水致毒物质鉴别技术进展

沉积物作为污染物迁移转化过程中重要的"源"和"汇",与整个生态系统及人类健康有着密切联系。间隙水很大程度上反映了水体沉积物的污染状况,同时可以真实反映生物的实际暴露情况,间隙水中关键致毒物质的鉴别是科学准确地评价间隙水及沉积物毒性与风险的重要基础。毒性鉴别评估(Toxicity Identification Evaluation,TIE)和效应引导的污染物识别(Effect Directed Analysis,EDA)技术作为致毒物质识别的主要方法,已在沉积物和间隙水的致毒物筛选中得到了初步的应用。本文介绍并比较了常用的间隙水提取方法,总结了TIE和EDA在间隙水致毒物质异位及原位鉴别方面的应用与发展,及鉴别过程中使用到的基本毒性量化方法与其适用条件。在当前间隙水关键致毒物质识别研究的基础上,指出了异位分析难以避免毒性损失和有机污染物鉴别方面的局限等问题,并提出应推广原位毒性试验技术且进一步发展有机物的精细分离技术和质谱识别技术等发展方向。     

3D geometric structures and biological activity: Application to microbial soil organic matter decomposition in pore space

During the past 10 years, soil scientists have started to use 3D Computed Tomography in order to gain a clearer understanding of the geometry of soil structure and its relationships with soil properties. We propose a geometric model for the 3D representation of pore space and a practical method for its computation. Our basic idea consists in representing pore space using a minimal set of maximal balls (Delaunay spheres) recovering the shape skeleton. In this representation, each ball could be considered as a maximal local cavity corresponding to the “intuitive” notion of a pore as described in the literature. The space segmentation induced by the network of balls (pores) was then used to spatialize biological dynamics. Organic matter and microbial decomposers were distributed within the balls (pores). A valuated graph representing the pore network, organic matter and distribution of micro-organisms was then defined. Microbial soil organic matter decomposition was simulated by updating this valuated graph. The method was implemented and tested using real CT images. The model produced realistic simulated results when compared with data in the literature in terms of the water retention curve and carbon mineralization. A decrease in water pressure decreased carbon mineralization, which is also in accordance with findings in the literature. From our results we showed that the influence of water pressure on decomposition is a function of organic matter distribution in the pore space. As far as we know, this is the approach to have linked pore space geometry and biological dynamics in a formal way. Our next goal will be to compare the model with experimental data of decomposition using different soil structures, and to define geometric typologies of pore space shape that can be attached to specific biological and dynamic properties.     

Influence of pore size of plankton nets and towing speed on the sampling performance of two high-speed samplers (Delfino I and II) and its consequences for the assessment of plankton populations

The sampling performance of two high-speed samplers, (Delfino I and II), fitted with a calibrated flow meter, was studied in the open Ligurian Sea using a battery comprising 6 such Delfinos linked together. Since, in plankton counts, only those organisms should be counted which are definitely retained in the nets, several techniques for the separation of the organisms which pass through the pore of a net of a given pore size and those which are safely retained were tested. Attempts to separate these two fractions by filtration of the fixed sample through nets of different pore sizes were not successful, as living organisms were able to pass through pore sizes which retained dead organisms. However, optical sizing under the dissecting microscope during counting gave reproducible results. Using this counting technique, the influence of the pore size of plankton nets on the reproducibility of sampling of natural populations was studied. The results obtained show that live plankton passes through the net pores at a size at which fixed plankton is retained. Hence, the minimum retention size for living and dead plankton is different. By comparing samples taken with nets of different pore sizes, and counting the organisms caught according to different sizes, it was possible to determine the minimum retention size of live plankton organisms for several different net pore-sizes. The minimum retention size is, therefore, the smallest pore size at which the organisms of a certain width cannot escape through the pores of the net and are, thus, quantitatively retained in the net. By applying the criterion of minimum retention size, the influence of speed towing on the number of plankton organisms caught was studied. It was shown that the number of organisms which are safely retained, i.e., do not escape through the pores, increased with speed, reaching a plateau at 5 to 7 knots.A contribution under the Association Contract CNEN-EURATOM. Contribution No. 668 of the Euratom Biology Division.     

用于研究土壤孔隙三维结构的连续数字图像的制备

主要介绍了一种用于分析土壤孔隙三维结构的连续数字图像的制备方法,内容包括土样的处理、不同格式图像之间的转换、孔隙结构分析指标等;对一类具体土壤的研究结果表明,在2cm的间距内,土壤孔隙结构仍存在较为明显的异质性。     

Synthesis and utilization of a mesoporous nickel oxide as a novel catalyst for degradation of phenol

Mesoporous nickel oxide (MNO) was synthesized by sol–gel method with saponificated chlorophyll-a (Chl-a) as template and Ni (II) acetate as starting material. XRD, surface area, pore volume, pore diameter and pore size distribution of MNO were determined. It exhibited high surface area and uniform pores with very sharp pore size distribution centered at 3.6 nm. High resolution transmission electron microscope images confirmed the results. MNO showed a high activity toward degradation of phenol at low temperature under atmospheric pressure of oxygen.     

Pillared interlayered clays: sustainable materials for pollution abatement

Environmental Chemistry Letters - Pillared interlayered clays have interesting properties such as high surface area, pore volume and extended pore size, high thermal stability, strong surface...     

Bewertung der potenziellen Grundwasserbelastung von deponierten Hochofengasschlämmen

Goal and Scope

Blast-furnace sludge is a waste originating from pig-iron production and contains contaminants such as lead, zinc, fluoride and cyanide assumably contaminating the groundwater by leaching.

Methods

We investigated the chemical composition of 27 samples of landfilled blast-furnace sludge in pore waters which were obtained by the centrifugation of fresh material and elution with water according to DIN 38414 part 4 (S 4).

Results

The pore waters as well as the eluates were neutral to alkaline (pH 7.3 to 10.7) and were dominated by alkali and alkaline-earth metals as well as sulphate and nitrate. The concentrations of all elements and compounds investigated were mostly clearly larger in the pore waters than in the eluates. The average concentrations of environmentally relevant constituents such as lead (0,18 mg?1), zinc (1,5 mg l?1), fluoride (10,6 mg l?1), and total cyanide (1.8 mg l?1) in the pore waters were distinctly larger than the inspection value of the German Federal soil Protection Ordinance for the pathway soil-groundwater. Lead, zinc, and total cyanide concentrations in the pore waters were largely underestimated by the eluates, as these concentrations were 70 to 90% lower in the eluates compared to the pore waters.

Conclusion

In the case of landfilled blast-furnace sludge, eluates according to DIN 38414 part 4 (S 4) provide low concentrations which are unrealistic to forecast concentrations in the seepage water.     

Direct measurement of pore-size distribution on artificial and natural deposits and prediction of pore space accessible to interstitial organisms

The pore spaces and particles comprising (a) 2 artificial sands consisting of uniform spherical particles and (b) 4 natural shell gravels from Church Island, Menai Strait, N. Wales, were observed directly in thin sections. Porosity and granulometry measurements made visually agreed with those obtained by traditional methods. Pore-size distributions could also be measured and always showed greater dispersion than particle-size distributions. In the almost monometric sands, the mean pore diameter was 30 to 40% of the mean particle diameter, in agreement with the Koseny-Carmen equation. In the polymorphic shell gravels, the mean pore size was only 15 to 20% of the mean particle size, and diminished with increased content of fine particles. A theoretical treatment is given, based on a model of interconnecting dilations and constrictions, to allow the proportion of total void space available to an organism of given diameter to be predicted.     

Specialized feeding mechanism in the pelagic copepod genus Heterorhabdus (Calanoida: Heterorhabdidae), with special reference to the mandibular tooth and labral glands

Scanning and transmission electron microscopy and gut-content analysis revealed the fine structure of the mandibular ventralmost tooth and labral glands of the carnivorous copepods Heterorhabdus spp. on the basis of the specimens collected in the waters near Nansei Islands, Southwestern Japan, in November 1993. The ventralmost tooth is hollow with a subterminal pore and a basal opening. The distal region of the tooth is like a hypodermic needle and is strengthened by opal layers. The tip of the tooth including the subterminal pore usually protrudes from between the labrum and the paragnath, while the basal region of the ventralmost tooth and the whole parts of the other teeth are semi-enclosed in the preoral food chamber formed by the labrum and the paragnath. There is a large glandular cell in the basal region of the mandibular gnathobase, but no direct connection exists between the gnathobasal cells and the tubular lumen of the ventralmost tooth. The posterior surface of the labrum carries a lateral pair of large glandular pores, which are located close to, and appear to fit exactly the basal openings of the ventralmost teeth. Each of these glands has two massive secretory cells, and the secretory materials from these cells appear to be mixed before discharge from the pore. A specialized feeding mechanism is proposed, wherein venom or anaesthetic is injected from the labral-gland pores into the tubular lumen of the mandibular ventralmost tooth, and then relcased into the prey from its subterminal pore immediately after capture using the stout maxillae of prey macrozooplankters such as copepodids and polychaetes.     

Metal partitioning in sediment pore water from the Ondo coastal region,Nigeria

Distribution and equilibrium partitioning of metals (Cd, Cu, Cr, Fe, Ni, Pb, Mn, and Zn) between pore water and surface sediments at the Ilaje coast of Ondo State, Nigeria, were studied. The Ilaje River can be one of the interesting research locations because of its economic nature and history of oil pollution. Seasonal variations were observed to investigate possible variations in the availability of metals for organisms throughout the year. The concentrations in both sediments and pore water during the dry and wet seasons were as follows: Cu?>?Fe???Mn?>?Pb?>?Ni?>?Cr?>?Cd?>?Zn. The pore water–sediment partition coefficient (K _p) showed that Zn and Cd were highly mobile while Fe and Cu have restricted mobility. Dissolved organic carbon (DOC) in pore water had a strong influence on mobility and bioavailability of all the metals (p?K _oc), increased levels of Fe and Cu were linked to lithological origin. Concentrations of Pb and Ni were associated with petroleum-related sources. The significance of the field-based techniques for ecotoxicological purposes is discussed.     

Influence of pore structure on biologically activated carbon performance and biofilm microbial characteristics

• Pore structure affects biologically activated carbon performance. • Pore structure determines organic matter (OM) removal mechanism. • Microbial community structure is related to pore structure and OM removal. Optimizing the characteristics of granular activated carbon (GAC) can improve the performance of biologically activated carbon (BAC) filters, and iodine value has always been the principal index for GAC selection. However, in this study, among three types of GAC treating the same humic acid-contaminated water, one had an iodine value 35% lower than the other two, but the dissolved organic carbon removal efficiency of its BAC was less than 5% away from the others. Iodine value was found to influence the removal of different organic fractions instead of the total removal efficiency. Based on the removal and biological characteristics, two possible mechanisms of organic matter removal during steady-state were suggested. For GAC with poor micropore volume and iodine value, high molecular weight substances (3500–9000 Da) were removed mainly through degradation by microorganisms, and the biodegraded organics (soluble microbial by-products,<3500 Da) were released because of the low adsorption capacity of activated carbon. For GAC with higher micropore volume and iodine value, organics with low molecular weight (<3500 Da) were more easily removed, first being adsorbed by micropores and then biodegraded by the biofilm. The biomass was determined by the pore volume with pore diameters greater than 100 μm, but did not correspond to the removal efficiency. Nevertheless, the microbial community structure was coordinate with both the pore structure and the organic removal characteristics. The findings provide a theoretical basis for selecting GAC for the BAC process based on its pore structure.     

Mobilization of heavy metals from contaminated paddy soil by EDDS,EDTA, and elemental sulfur

For enhanced phytoextraction, mobilization of heavy metals (HMs) from the soil solid phase to soil pore water is an important process. A pot incubation experiment mimicking field conditions was conducted to investigate the performance of three soil additives in mobilizing HMs from contaminated paddy soil (Gleyi-Stagnic Anthrosol): the [S, S]-isomer of ethylenediamine disuccinate (EDDS) with application rates of 2.3, 4.3, and 11.8 mmol kg⁻¹ of soil, ethylenediamine tetraacetate (EDTA; 1.4, 3.8, and 7.5 mmol kg⁻¹), and elemental sulfur (100, 200, and 400 mmol kg⁻¹). Temporal changes in soil pore water HM and dissolved organic carbon concentrations and pH were monitored for a period of 119 days. EDDS was the most effective additive in mobilizing soil Cu. However, EDDS was only effective during the first 24 to 52 days, and was readily biodegraded with a half-life of 4.1 to 8.7 days. The effectiveness of EDDS decreased at the highest application rate, most probably as a result of depletion of the readily desorbable Cu pool in soil. EDTA increased the concentrations of Cu, Pb, Zn, and Cd in the soil pore water, and remained effective during the whole incubation period due to its persistence. The highest rate of sulfur application led to a decrease in pH to around 4. This increased the pore water HM concentrations, especially those of Zn and Cd. Concentrations of HMs in the soil pore water can be regulated to a large extent by choosing the proper application rate of EDDS, EDTA, or sulfur. Hence, a preliminary work such as our pot experiment in combination with further plant experiments (not included in this study) will provide a good tool to evaluate the applicability of different soil additives for enhanced phytoextraction of a specific soil.     

沉积物间隙水溶解态磷和铁（Ⅱ）高分辨同步分析方法的研究

沉积物具有高度的空间异质性,尤其在沉积物-水界面附近的微环境中,溶质在微小尺度上可能存在强烈的浓度梯度分布,需要借助高分辨的获取技术才能表征。本研究发展了一种沉积物微界面溶解态反应性磷（Dissolved Reactive Phosphorus,DRP）和溶解态铁（Ⅱ）的同步分析方法。利用分辨率为4 mm、平衡时间仅为2 d的微型间隙水平衡装置（Peeper装置）获取微量间隙水（～100μL·样品-1）,采用384微孔板微量比色法分别测定同一间隙水样品中的DRP和溶解态铁（Ⅱ）的质量浓度,单一指标所消耗的间隙水体积由5 mL减少到仅～40μL,检出限分别为0.009和0.017 mg·L-1,精密度为1%～7%,均与常规方法相近。将该分析方法应用到太湖两个湖区的沉积物中,同步获得的微界面溶解态磷和铁（Ⅱ）的分布较好地反映了两者的关系。     

Geophysical investigations for evaluation of environmental pollution in a mine tailings area

Sulfide-containing mill wastes of the Komsomolsk ore processing plant situated in the Kemerovo region (Russia) were examined in 2013–2015. Multipurpose studies of the mine tailings determined the composition of waste, pore water, mine drainages, and affected groundwater. Electrical resistivity tomography was used to trace the geoelectric zoning of the waste samples. Layers with low resistivity indicated areas with pore spaces filled with highly mineralized solutions with Fe, Cu, Zn, Cd, As, and Sb at total concentrations of up to 50 g/L. Anomalous zones can be specified as ‘geochemical barriers’ – specific layers where the mobility of the elements is reduced due to pH conditions, redox potential, and Fe(III) hydroxide precipitation. The zones of increased conductivity in oxidized mine tailings indicated local areas with high acid production potential and coexisting acidic pore solution. In non-oxidized tailings, high conductivity of the mineral skeleton was observed. There was a migration of drainage outside the tailings, its direction monitored by geophysical data. Chemical analysis confirmed that the concentrations of As in groundwater samples were higher than the maximum permissible concentration.     

Determination of enzymatic activities for the characterization of sediments

In‐vivo enzymatic activity tests have been used for the characterization of sediments. Sediment samples representing three typical situations on the river Elbe and one reference site on the river Spree were investigated from March to October 1993. Fresh sediments and pore water were analyzed for their dehydrogenase and proteolytic enzymatic activities, respectively. The dehydrogenase and protease activities varied depending on sampling site, date and kind of sample. From the mean values of the dehydrogenase activities over the whole period of investigation significant differences between the sampling sites became evident. The dehydrogenase activity of pore water rather than that of the whole sediment is suitable to differentiate between anthropogenically influenced and not influenced sites. The dehydrogenase activities in the contaminated samples were extremly higher than those in the uncontaminated samples. In contrast to this, samples from the uncontaminated sites showed a considerably higher specific proteolytic activity. This fact is interpreted as a possible enzymatic inhibition.     

Sorption and bioavailability of arsenic in selected Bangladesh soils

The bioavailability of arsenic (As) in the soil environment is largely governed by its adsorption–desorption reactions with soil constituents. We have investigated the sorption–desorption behaviour of As in four typical Bangladeshi soils subjected to irrigation with As-contaminated groundwater. The total As content of soils (160 samples) from the Laksham district ranged from <0.03 to approximately 43 mg kg⁻¹. Despite the low total soil As content, the concentration of As in the pore water of soils freshly irrigated with As-contaminated groundwater ranged from 0.01 to 0.1 mg l⁻¹. However, when these soils were allowed to dry, the concentration of As released in the pore water decreased to undetectable levels. Remoistening of soils to field moisture over a 10-day period resulted in a significant (up to 0.06 mg l⁻¹) release of As in the pore water of soils containing >10 mg As kg⁻¹ soil, indicating the potential availability of As. In soils containing <5 mg As kg⁻¹, As was not detected in the pore water. A comparison of Bangladeshi soils with strongly weathered long-term As-contaminated soils from Queensland, Australia showed a much greater release of As in water extracts from the Australian soils. However, this was attributed to the much higher loading of As in these Australian soils. The correlation of pore water As with other inorganic ions (P, S) showed a strongly significant (P < 0.001) relationship with P, although there was no significant relationship between As and other inorganic cations, such as Fe and Mn. Batch sorption studies showed an appreciable capacity for both As^V and As^III sorption, with As^V being retained in much greater concentrations than As^III.     

Analysis of volatile fatty acids by ion-exclusion chromatography,with special reference to marine pore water

A method for measuring volatile fatty acids using ion-exclusion chromatography is presented. The system was found to be applicable to samples with high salt concentrations (e.g. seawater and marine pore water) when coupled with a vacuum distillation procedure. The method is straightforward, with no sample preconcentration and no introduction of external contamination. Calibration was found to be linear, with good reproducibility (coefficient of variation normally less than 5%) and the system was sufficiently sensitive to operate at the sub-ppm level (minimum detection limit for acetate and propionate was approximately 0.02 and 0.05 ppm, respectively). This technique was used to investigate the distribution of volatile fatty acids with sediment depth at Station E70 in Loch Eil, Scotland (sample was collected in March, 1983) and the results were in good agreement with recent publications. Although the system, at present, is limited in marine pore water to acetate and propionate, it has certain advantages over alternative systems and these are described.     

载铜活性炭纤维Cu-ACF的微观结构与表面形态

本文讨论了载铜活性炭纤维的制备过程与微观结构,表面形态的关系。