土壤轻组有机质

轻组有机质主要是由不同分解程度的植物残体和一些微生物结构体组成,它的改变可以用来指示土壤肥力的变化.本文综述了轻组的分离方法、轻组的组成、种植和施肥对轻组的影响、轻组在土壤团聚体和土壤剖面中的分布以及轻组的季节性变化.     

土壤轻组有机质

轻组有机质主要是由不同分解程度的植物残体和一些微生物结构体组成,它的改变可以用来指示土壤肥力的变化。本文综述了轻组的分离方法、轻组的组成、种植和施肥对轻组的影响、轻组在土壤团聚体和土壤剖面中的分布以及轻组的季节性变化。     

表面活性剂在北京碱性土壤中的吸附行为研究

通过静态吸附实验,研究了北京碱性土壤对阴离子表面活性剂SDS、阳离子表面活性剂CTAB和非离子表面活性剂Tween80的吸附行为,考察了温度对表面活性剂吸附的影响.结果表明:7种不同土样对SDS、CTAB和Tween80的吸附等温线均较好地符合Langmuir吸附模式,其吸附能力的大小顺序为2号轻壤土》轻粘土》中壤土》砂壤土》5号轻壤土》重壤土》紧砂土,这主要是由于7种土样的pH、有机质含量和机械组成不同的缘故;同一土壤中,CTAB的吸附量》Tween80的吸附量》SDS的吸附量;温度的升高,不利于SDS和CTAB在土壤中的吸附,而有利于Tween80的吸附.     

含磷材料对矿区铅镉污染土壤重金属形态转化的影响

以湖南郴州东江湖风景区矿区遗留地重金属污染土壤为研究对象,研究了3种含P材料,及其与蒙脱石的组合材料,对矿区土壤铅镉污染的修复效果.实验设6组处理,分别为P1组、P2组、P3组、P1 +M组、P2+M组、P3 +M组,通过添加5％的稳定剂,稳定2d后,分析土壤中铅镉的形态变化.实验结果表明:添加含P材料,及组合材料后,土壤中铅镉的离子交换态、铁锰结合态、有机结合态大幅度降低,残渣态显著升高.对Pb离子转化效果均在90.00％以上,Cd离子的转化效率相对较差,最优P1处理效果为74.20％.离子交换态的减少,有效地降低了重金属的生物有效性,有效地降低了环境风险.同时,含P材料均增加了土壤有效磷的含量,对矿区土壤的肥力也有一定提升.     

温度和表面活性剂对菲在土壤中吸附的影响

通过静态吸附实验,研究了北京地区土壤对菲的吸附行为,考察了温度和表面活性剂对菲吸附的影响.结果表明,6种土样对菲的吸附等温线均较好地符合Freundlich吸附模式,其吸附能力的大小顺序为:轻壤土>轻粘土>砂壤土>中壤土>重壤土>紧砂土;温度升高不利于菲在土壤中的吸附;十二烷基苯磺酸钠(LAS)和十六烷基三甲基澳化铵(CTAB)均利于菲在土壤表面的解吸,LAS和CTAB对菲的解吸率最高可达66.2%和31.8%,且LAS的解吸效果更好.     

基于地球化学标准化方法的平湖市农田土壤重金属污染评价

运用地球化学标准化方法评价浙江省平湖市农田土壤重金属污染状况.结果显示,约50%的农田土壤受到了重金属人为污染,其中除了5.6%的农田土壤受到了Hg中度人为污染外,其余均为轻微人为污染.每种重金属元素的地球化学基线值均可信,Cr、Pb、Cu、Zn、Ni和As与标准化元素Al线性相关性较好,而Hg和Cd与Al线性相关性不好,原因可能与后者受人类活动或土壤环境影响较大有关;多变量聚类分析结果表明,平湖市农田土壤重金属元素组成特征为Cd一族、Hg一族,而Cu、Pb、Ni、As、Cr和Zn为一组合族.     

广东省主要蔬菜产地土壤中重金属含量调查与评价

调查了广东省20个市(县)52个主要蔬菜产地土壤重金属含量,并以<土壤环境质量标准>(GB 15618-1995)二级标准为评价标准,采用单项污染指数法和综合污染指数法对其进行评价.结果表明,156个蔬菜产地土壤样品中Cd、Hg、As和Cr的超标率分别为9.62%、3.85%、0.64%和0.64%,Pb未出现超标;有8个蔬菜产地土壤重金属处于轻污染,13个蔬菜产地土壤重金属处于警戒限,其余蔬菜产地土壤重金属均在安全范围内.蔬菜产地土壤Cd污染最为普遍和严重,其次是Hg和As,且Cd的变异系数为103.67%,预示蔬菜产地土壤可能受到Cd的点源污染.珠江三角洲地区蔬菜产地土壤重金属含量普遍高于其他地区,粤西和粤北地区个别蔬菜产地土壤重金属超标.     

有机污染黏壤土热脱附后热导率的变化特性

为探究有机污染土壤热脱附后热导率的变化特性,采集了苏州市某原位热脱附修复场地编号为G01、G06和G09的示范区域深度为0～3 m的土壤(系黏壤土),并利用实验室的小型热脱附装置在350℃的条件下对污染土壤试样进行了1h热脱附;对其热脱附前后的粒径分布以及热脱附后的化学组成(矿物质和有机质的质量分数)进行了表征,并用探针式导热仪测试了其热导率.结果表明,在高温热脱附处理过程中,土壤颗粒的团聚作用比破碎作用更强,导致热脱附后土壤粒径增大;当密度、含水率和温度等条件保持一致时,热脱附后土壤的热导率较场地原位测试时无显著变化,平均值在1.4～1.5W·(m·℃)-1;随温度升高或干密度增大,土壤热导率均增大,且干密度对热导率的影响比温度更加显著.此外,3个采样区域的土壤热导率呈现一定的差异,其中,G06区域的热导率最大而G01区域最小,最多相差0.055W·(m·℃)-1,这主要是由不同区域土壤中矿物质(其热导率是有机质的3倍以上)质量分数的变化所致.本研究结果可为实际热修复场地的地层温升预测提供参考.     

矿区土壤中重金属元素含量异常的调查

对某金矿区下游土壤重金属元素含量异常区进行了调查,研究了异常元素的空间分布和相态组成.通过对土壤、水、农产品、大气沉降物等的采样分析表明,土壤中重金属元素含量异常是由于矿山开采,废水排放,下游引水灌溉造成的.对异常元素的环境影响进行了分析评价,并提出了土壤治理建议.     

白洋淀北岸农田土壤特性的表征

本文采用标准方法,测定了白洋淀北岸部分农田土壤的粒度组成、ｐＨ和有机碳含量等指标,对该地区土壤的特性进行了表征分析。结果表明,土壤的平均粒度分布大于２０μｍ的占５２．７３％,主要属于砂壤土。与１０年前相比,ｐＨ值变化不大;而有机碳含量是１０年前的１．２６倍。ｐＨ随土壤的垂直深度而略有增加,而有机碳含量则随土壤的垂直深度而减少。     

硫化钠对土壤中铅镉的固定效果简

研究了硫化钠用于固定土壤中铅镉的可行性,考察了硫化钠用量及土壤pH、有机质对固定过程中土壤铅、镉赋存形态及固定效果的影响。结果表明,添加硫化钠可改变土壤中铅镉的形态分布,明显降低可交换态铅镉的含量。条件适当时,铅镉可交换态下降值分别为63%和73%。硫化钠在固定铅的过程中,固定效率对土壤pH、有机质含量的变化较为敏感,在有机质含量较低或酸性土壤中,硫化钠对铅固定效率较高;相对于铅,有机质含量和pH变化对镉的固定效率影响不是很大。     

Sorption of polycyclic aromatic hydrocarbons (PAHs) to carbonaceous materials in a river floodplain soil

We report on sorption isotherm of phenanthrene (Phe) for river floodplain soil associated with carbonaceous materials, with particular attention being devoted to the natural loading of Phe. Our sorption experiments with original soil samples, size, and density sub-fractions showed that the light fraction had the highest sorption capacity comparable to low rank coals. In addition, the light fraction contributed most for the sorption of Phe in total soil samples. K_oc values for all fractions were in the same range, thus indicating that coal and coal-derived particles in all samples are responsible for the enhanced sorption for Phe. Sorption was strongly nonlinear and the combined partitioning and pore-filling model gave a better fit than the Freundlich sorption model. In addition, the spiked PAHs did not show the same behavior as the naturally aged ones, therefore the accessibility of indigenous background organic contaminants was reduced when coal and coal-derived particles are associated with the soils.     

Changes in soil organic matter chemical properties after organic amendments

Organic inputs are used to improve soil physical and chemical properties, but the corresponding changes in soil organic matter (SOM) chemical properties are not well known. In this study, we compared some characteristics of the SOM of a soil receiving either no organic inputs, or two different amendments during 15 years (straw or conifer compost). Quantities of organic carbon and C/N values were determined on particle size fractions after physical soil fractionation to localize changes due to amendments. Contents in reactive functional groups, acid-base properties and copper binding affinities were determined by titration experiments for the soluble fraction of SOM: the fulvic acid fraction (FA). Data of FA extracted from the bulk soil were compared to data of FA extracted from the <20 microm size fraction with the help of either a discrete or a continuous model (fit of data with FITEQL or NICA, respectively). Copper binding characteristics of FA extracted from the <20 microm size fraction did not change significantly after organic inputs, while those of FA extracted from the bulk organic-amended soils were found different from the ones with no amendment. Minor effects observed in the finer soil fractions were ascribed to their low turn-over of organic carbon and/or to a greater homogeneity in the nature of the organic carbon entering these fractions. Our results show major chemical changes in coarser soil organic fractions after organic amendments.     

EDTA强化电动力学修复重金属复合污染土壤

在自制的电动力学装置中,研究多种重金属复合污染土壤的电动力学修复,通过在阴极添加络合剂EDTA来提高修复效率。实验结果表明,EDTA的引入提高了修复过程中的电流值,且EDTA与重金属的络合提高了污染物向电极液的迁移效率,从而强化了电动力学修复效果。在设定的浓度(0、0.01、0.02、0.05和0.1 mol/L)中,0.1 mol/L的EDTA具有最佳的修复效率。在此实验条件下,污染土壤中的总铜、总铅和总镉的去除率分别为90.2%、68.1%和95.1%。电动力学修复后,对土壤重金属进行化学形态分析,发现电动力学修复显著改变了土壤重金属存在形态,修复后土壤中的铜、铅、镉主要以较稳定的有机态和残余态形式存在,显著降低了对周边生物和环境的毒害。     

Occurrence of coal and coal-derived particle-bound polycyclic aromatic hydrocarbons (PAHs) in a river floodplain soil

A PAH contaminated river floodplain soil was separated according to grain size and density. Coal and coal-derived particles from coal mining, coal industry and coal transportation activities were identified by organic petrographic analysis in our samples. Distinct concentrations of PAHs were found in different grain size and density fractions, however, similar distribution patterns of PAHs indicated similar sources. In addition, although light fractions had the mass fraction by weight of less than 5%, they contributed almost 75% of the total PAHs in the soil. PAH concentrations of all sub fractions showed positive correlation with their TOC contents. Altogether, coal and coal-derived particles that were abundant in light fractions could be the dominant geosorbents for PAHs in our samples.     

Multimedia fate of petroleum hydrocarbons in the soil: Oil matrix of constructed biopiles

A dynamic multimedia fugacity model was used to evaluate the partitioning and fate of petroleum hydrocarbon fractions and aromatic indicator compounds within the soil: oil matrix of three biopiles. Each biopile was characterised by four compartments: air, water, soil solids and non-aqueous phase liquid (NAPL). Equilibrium partitioning in biopile A and B suggested that most fractions resided in the NAPL, with the exception of the aromatic fraction with an equivalent carbon number from 5 to 7 (EC₅₋₇). In Biopile C, which had the highest soil organic carbon content (13%), the soil solids were the most important compartment for both light aliphatic fractions (EC₅₋₆ and EC₆₋₈) and aromatic fractions, excluding the EC₁₆₋₂₁ and EC₂₁₋₃₅. Our starting hypothesis was that hydrocarbons do not degrade within the NAPL. This was supported by the agreement between predicted and measured hydrocarbon concentrations in Biopile B when the degradation rate constant in NAPL was set to zero. In all scenarios, biodegradation in soil was predicted as the dominant removal process for all fractions, except for the aliphatic EC₅₋₆ which was predominantly lost via volatilization. The absence of an explicit NAPL phase in the model yielded a similar prediction of total petroleum hydrocarbon (TPH) behaviour; however the predicted concentrations in the air and water phases were significantly increased with consequent changes in potential mobility. Further comparisons between predictions and measured data, particularly concentrations in the soil mobile phases, are required to ascertain the true value of including an explicit NAPL in models of this kind.     

Bioavailability assessment and environmental fate of polycyclic aromatic hydrocarbons in biostimulated creosote-contaminated soil

When hydrocarbon-contaminated soil is subjected to bioremediation technology, hydrocarbon depletion is typically marked by an initially rapid reduction rate. This rate decreases over time and frequently a residual concentration remains in the soil. This kinetic has been attributed primarily to the enrichment of more recalcitrant fractions, as well as to the lack of resting hydrocarbon bioavailability. Thus, at the end of the bioremediation process, a part of the residual hydrocarbon soil concentration represents the non-bioavailable fraction, which is difficult to degrade by microbial populations and which poses a minor hazard. Therefore, determination of the bioavailable fraction in a bioremediation project represents both an estimation of the maximum level of achievable biodegradation, as well as an additional indication of the environmental health hazard. In the present study, aged creosote-contaminated soil was subjected to biostimulation processes, and the bioavailable fraction for several target polycyclic aromatic hydrocarbons (PAHs) was calculated using a mild extraction with cyclodextrines. The amount of PAH extracted corresponded to the desorbing fraction and can be regarded as the bioavailable fraction. The non-desorbing fraction data obtained from this procedure were compared to the remaining PAH concentrations following bioremediation treatment of soil microcosms. These results permitted the establishment of a theoretical biodegradation limit based on the desorbing fraction. In addition, neither accumulation of intermediate metabolites, nor the formation of bound-residues or reduced acute toxicity was observed.     

Thallium in fractions of soil formed on floodplain terraces

Two soils formed on the floodplain terrace of a rivulet flowing through the zinc-lead ore exploration area polluted with thallium and one soil from a floodplain terrace of the reference area were investigated in terms of thallium distribution between soil fractions. Such type of soil is formed on river floodplain terraces next to the main river channel and its composition records the history of river pollution. A sequential extraction of soil according to the BCR protocol was performed with an additional initial stage of extraction with water. Apart from labile thallium, thallium entrapped in the residual parent matter was also determined. Thallium was determined by flow-injection differential-pulse anodic stripping voltammetry. In all three cases, the major fraction is thallium entrapped in parent matter. Top soil from the polluted area contains 49.3% thallium entrapped in the residual parent matter, the bottom soil contains 41% while the reference soil contains 80% in this fraction. The major part of labile thallium is located in the reducible fraction (27.7% of total thallium in the top soil, 27% in the bottom soil and 12.4% of the reference soil). Second in terms of significance is the fraction of oxidizable thallium. The top soil contains 12% of total thallium concentration, the bottom soil contains 19% of total concentration, while the reference soil contains 4.1% of total concentration. The acid soluble/exchangeable fraction of thallium has almost the same significance as the oxidizable fraction. The top soil contains 10.4% of the total concentration, while the bottom soil contains 12% of the total concentration. Water soluble thallium concentration is very small. Comparison of the top and the bottom soil show that thallium has not been transported from the river channel onto the floodplain terrace over a long period.     

Seasonal variation of the distribution of PCBs in sediments and biota in a PCB-contaminated estuary

To elucidate the effects of seasonal variation of precipitation on the distribution of polychlorinated biphenyls (PCBs) in estuarine sediments and benthic feeders, PCB concentrations of river surface sediments and mullet fish (Liza macrolepis) were investigated in the estuary of Er-Jen River near former PCB contamination sites before and after each wet season from 2002 to 2004. Analyses of grain size distribution and organic matter revealed that the pre-existing surface sediments were covered by and mixed with the soil particulates brought by surface runoff after each wet season. Obvious increment of PCB content and significantly elevated fraction (p < 0.005) of light PCBs of the river mouth’s sediments after each wet season indicated that the invading particles were rich in unweathered PCBs. PCBs previously buried in the surface soil of heavily contaminated sites were flushed into this estuary through surface runoff. The precipitation altered the PCB patterns in sediment organic matter, the dietary source of mullet, and consequently changed that of mullets accordingly, which all possessed significant greater fraction of light PCBs. In this study, it was demonstrated that seasonal summer precipitation affected the distribution of PCBs on surface sediments and the mullets of this estuary. PCB residuals retained in this region still pose potential threats to biota resided here.     

Earthworms and radionuclides, with experimental investigations on the uptake and exchangeability of radiocaesium

The potential influence of earthworm activity on the mobility of radionuclides in soils and their subsequent availability for uptake by plants and transfer to higher trophic levels is briefly reviewed. The accumulation of caesium by the earthworm Aporrectodea longa from soil and from plant litter was investigated in laboratory experiments, as was the effect of reworking (through burrowing and ingestion) soil and soil with added organic material, on the extractability of caesium (ammonium acetate extraction). Soil was spiked with (134)Cs, organic matter with (137)Cs. In soil-fed worms, most of the radioactivity measured was eliminated with the gut contents; 5-25% of the ingested radioactivity was retained or assimilated. Loss of caesium from soil-fed worms followed a two component curve, with an initial rapid loss due to gut clearance (half-life of loss (Tb1/2) of about 0.2-0.6 days) and a slower loss of assimilated caesium (Tb1/2 of 15-26 days). Loss rates of assimilated caesium from worms fed on fragmented apple leaves were found to have half-lives of 18-54 days. Assimilation of caesium from apple leaves was higher than from soil, ranging from 55-100% of the activity measured before gut clearance. Dry weight transfer factors (concentration in worm tissue/concentration in substrate) for worms cleared of their gut contents were similar for the two substrates 0.04 and 0.04 for two loss experiments with worms fed on radioactive soil, and 0.03 and 0.05 for worms fed on apple leaves. After three months of reworking soil and soil/organic mixtures, A. longa was found to have no measurable effect on the extractable fraction of caesium. If earthworms have any subtle effects they were masked by changes in availability that occurred when the spiked soil and organic substrates were mixed together. Only about half of the extractable fraction in soil was recovered when soil was mixed with organic material suggesting that some of the labile fraction in soil had become complexed with organic material. This exchange occurred in substrate mixtures with and without worms. The limitation of chemical extraction procedures is discussed and suggestions for further work are presented.