土壤石油污染物生物通风修复的研究进展

生物通风是一种去污效果好、操作费用低的土壤原位修复技术。文章概述了生物通风系统的结构、设计目的、适用范围和优缺点，详细论述了生物通风的国内外研究现状，包括现场应用、影响因素和强化技术及理论研究，并展望了生物通风在我国的应用前景。     

土壤原位修复技术研究与应用进展

土壤原位修复技术是指不经挖掘,直接在污染场地就地修复污染土壤的土壤修复技术,具有投资低,对周边环境影响小的特点,是土壤修复的研究热点。土壤原位修复技术主要有淋洗,气相抽提（SVE）,多相抽提（MPVE）,气相喷射（IAS）,生物降解,原位化学氧化（ISCO）,原位化学还原,污染物固定,植物修复等。淋洗法主要用于治理高渗透性土壤中的重金属和难挥发降解的有机物。土壤气相抽提和喷射技术适用于处理土壤中的易挥发污染物,并有常与加热技术,生物处理技术等联用,可以起到促进污染物挥发,增氧促分解的作用。多相抽提法主要用于治理存在大量非水相流体的污染场地,可将土壤中有机相污染物直接抽出。生物降解有生物好氧降解、生物厌氧降解、生物还原降解多种,降解方式由污染物种类和地质条件决定。化学方法可将污染物氧化或还原为低毒无毒物质,周期一般较短。固定污染物可以直接加入药剂反应生成沉淀,也可制造合适条件使微生物生成可沉淀重金属的离子。植物修复主要用于富集重金属,成本低廉,但富集了重金属的植物体的有效利用尚待进一步研究。土壤原位修复需要因地制宜,灵活结合工期、污染情况、地质条件、地面设施等,得出最经济实用的修复方法,并在辅助提高技术上展开更多研究,使原位修复技术更经济有效。     

气相抽提去除红壤中挥发性有机污染物的去污机理探讨

通过探讨土壤气相抽提去除红壤中挥发性有机污染物的去污机理,建立了一维稳态条件下污染物在土壤多孔介质中传质的总微分方程,分别求出了平衡模型和动力学模型的解析解和数值解,并用实验结果对平衡模型和动力学模型进行了模拟和验证.实验结果和模型模拟结果表明理论模型与实验结果吻合良好,平衡模型和动力学模型在描述污染物在土柱通风过程中的传质时,分别适用于不同的阶段.在通风初期平衡模型能够很好地描述实验结果,而随着时间的推移,平衡模型的预测曲线逐渐偏离数据点,到了通风中后期,只有动力学模型才能够较好地描述和预测实验结果.     

农田土壤重金属污染状况及修复技术研究

重金属污染因具有毒性、易通过食物链在植物,动物和人体内累积,对生态环境和人体健康构成严重威胁。随着工业快速发展、农药及化肥的广泛使用,农田土壤重金属污染越来越严重,研究农田土壤重金属污染现状及修复技术对农产品安全具有重要意义。综合国内外农田土壤重金属污染状况,农田土壤重金属污染主要来源于固体废弃物堆放及处置、工业废物大气沉降、污水农灌和农用物质的不合理施用。该文综述了国内外有关农田重金属污染土壤修复技术（物理修复、化学修复、生物修复、农业生态和联合修复）的研究进展,并针对各种修复方法,阐述了其原理、修复条件、应用实例及其优缺点,重点论述了植物修复的机理和应用,提出了草本与木本联合修复可有效提高农田土壤重金属复合污染的修复效率,为农田土壤土壤重金属复合污染修复提出了新的途径。最后在对已有研究分析的基础上,提出了联合修复技术（如生物联合技术、物理化学联合技术和物理化学-生物联合技术）可以在一定程度上克服使用单一修复手段存在的缺点,可提高复合污染的修复效率、降低修复成本,未来应深入探索联合修复技术间的相互作用机理,以期为农田土壤重金属综合治理与污染修复提供科学依据。     

废铁屑修复汞污染土壤的实验研究

应用工厂废弃物—铁屑做原料,探讨不同铁屑投加量对修复不同土壤类型、不同程度汞污染土壤的能力,并与修复水体汞污染作了对比;另外,首次将淋滤法与国际上新兴的土壤、地下水修复技术-PRB技术结合,研究其修复土壤汞污染的效果。结果表明,废铁屑可很快去除水体中的汞,去除率可达93%;在铁屑存在下,能一定程度预防和修复土壤汞污染,在相同水体汞污染程度条件下,时间是影响土壤汞污染程度的主要因素;在CaCl2淋洗液作用下的模拟PRB实验中,土壤有效汞含量降低,同时淋洗液中汞质量浓度低于1μg·L-1。因此,用废铁屑能有效预防和修复土壤汞污染,且将淋滤法与PRB技术联用,与将铁屑直接撒入土壤中相比效果好得多,且不会引起后续的水体二次污染,是一种很有应用潜力、值得深入研究的土壤修复方法。     

土壤中微塑料污染现状与检测技术研究进展

微塑料一般是指粒径小于5 mm的塑料碎片,作为一种新污染物已经成为全球环境领域的研究热点.土壤作为环境中微塑料的最大储库,土壤中微塑料的污染逐渐引起重视并取得了一定的研究进展.本文系统了梳理了国内外土壤中微塑料的污染现状和污染特征,介绍了土壤中微塑料检测技术研究进展,重点探讨各类样品采集、前处理和和定性定量方法的优缺点以及对土壤中微塑料检测的适用性,分析了土壤中微塑料检测技术研究面临的主要挑战,提出未来土壤中微塑料污染调查与检测技术的研究方向,以期为科学开展土壤中微塑料污染风险治理与管控提供技术支撑.     

铬污染土壤的微生物修复工艺及中试

本研究利用土柱试验研究了铬污染土壤微生物修复的各工艺参数,结果表明:土壤粒径、喷淋强度、以及修复工艺对铬污染土壤的修复效果有很大的影响.最佳的工艺参数为:土壤粒径1～2 cm、喷淋强度在29.6～59.2 mL·min-1、工艺制度Ⅱ(先用自来水淋洗1 d,接着用菌液循环喷淋).在土柱试验的基础上开展了25吨/批的中试试验,铬污染土壤经过7～10 d的处理,土壤中Cr(Ⅵ)浸出毒性浓度由53.8 mg·L-1降低至0.4 mg·L-1,达到《铬渣污染治理环境技术规范》(HJ/T301～2007)中铬渣用作路基材料和混凝土骨料的标准限值,证明铬污染土壤微生物修复工业化具有可行性,为铬污染土壤工程化修复提供了技术支撑.     

化学强化植物修复复合污染土壤研究进展

近年来,土壤复合污染问题日趋严峻,且修复难度往往较大.在复合污染土壤众多修复技术中,植物修复因成本低、易实施、环境友好等特点而颇具潜力.然而植物修复存在周期长、效率低的局限性.因此,围绕植物开展的联合强化修复技术研究,成为复合污染土壤治理修复的新途径,其中化学强化植物修复技术研究备受关注.本文综述了化学强化植物修复3种复合污染土壤的效果,对比分析了不同化学强化措施的作用特点和异同,并对该技术的研究方向提出了展望.     

重金属污染土壤属性区间识别模型的赋权分析

土壤重金属污染评价为土壤重金属污染的及时防范和综合治理提供重要的理论依据。文章在属性区间识别理论的基础上,构建土壤重金属污染评价的属性区间识别模型：选取土壤重金属污染中普遍存在的Hg、Cd、As、Pb、Cu、Zn作为评价指标,采用均化系数将各评价指标的属性测度区间转化为综合属性测度;为避免主观因素,利用主成分分析法、熵权法、CRITIC法对各评价指标进行3次客观赋权;最后根据置信度准则和分级标准进行土壤重金属污染的综合评价。对3种赋权法得到的权重和评价结果进行比较,表明：属性识别模型在土壤重金属污染评价中适用且有利于评价结果准确性的提高;3种客观赋权法算得的权重合理,且其优异程度为主成分分析法〈熵权法〈CRITIC法。     

关于英国工矿区土壤重金属污染治理的考察报告

按照国家948项目规定,根据《引进国际先进技术工矿区土壤超富集植物材料选择及修复技术》项目合同要求,经国家林业局和省人民政府批准,省林业厅巡视员、高级工程师李定一同志率领队考察成员姚先铭、左家哺、童方平一行4人,前往英国考察工矿区土壤重金属污染治理以及商谈有关超富集植物材料与土壤改良剂引进问题．由于全世界英国最早开始采矿业,了解英国工矿区土壤重金属污染综合治理,引进有关超富集植物与土壤改良剂,对于解决我国目前工矿区土壤重金属污染问题具有重要意义．     

不同含水量细砂介质中挥发苯的有效扩散系数研究

挥发性有机污染物在土壤多孔介质中的有效扩散系数是土壤气相抽提(soil vapor extraction,SVE)传质过程中的一个重要参数.笔者以苯为研究对象,采用土柱扩散试验,对不同含水量条件下挥发苯在细砂介质中的有效扩散系数和扩散规律进行研究.结果表明,对于吸附型矿物含量少的细砂介质,含水量大小在一定程度上影响了挥发苯的扩散过程.含水量在50 g·kg-1时,扩散最快;低于50 g·kg-1时,随含水量增大扩散能力增强;高于50 g·kg-1时,扩散能力则随含水量增大而减弱.同一扩散柱中,随着扩散距离增加,挥发苯的有效扩散系数增大,这可能与其蒸汽分压降低有关.     

Carbonaceous resin capsule for vapor-phase monitoring of volatile hydrocarbons in soil: partitioning and kinetic model verification

The resin capsule system (RCS) was tested as a means of providing data on the presence and forms of volatile hydrocarbons. Results indicated that resin capsules provided data showing sensitivity to soil variables (texture and moisture content) and time. The objectives of this paper are to evaluate the RCS methodology and to determine whether carbonaceous resin capsules provide results that can be described by fundamental chemical partitioning and kinetic principles. Findings revealed a significant relationship between quantities of benzene, toluene, ethylbenzene, and xylene adsorbed on the capsule and quantities partitioned into the vapor phase. Kinetic evaluation indicated that the vapor adsorption by the resin capsule is regulated by diffusion processes. No verification of rate-limiting processes was possible due to limitations imposed by the experimental design, but it appears that during early stages, adsorption rate was limited by vapor diffusion through the soil. The resin capsule data also reflected differences that would be expected due to properties of the organic liquids present. These results provide further evidence that the RCS could be developed to suggest direct in situ monitoring to reveal quantities and nature of organic substances in soils.     

城市地下空间开发中的弃土管理和处置对策

城市地下空间的大规模开发利用将产生大量弃土。简要分析了弃土对环境的影响,介绍了弃土管理和处置的现状以及存在的问题,提出了加强立法和管理、优化施工方法和技术、对弃土进行资源化利用、妥善处置已污染的弃土等对策。     

Environmental impact of historical harbour city Zadar (Croatia) on the composition of marine sediments and soils

Large amounts of oyster shells are produced as a by-product of shellfish farming in coastal regions without beneficial use options. Accordingly, this study was conducted to evaluate the potential for the use of waste oyster shells (WOS) containing a high amount of CaCO₃ to improve soil quality and to stabilize heavy metals in soil. To accomplish this, an incubation experiment was conducted to evaluate the ability of the addition of 1–5 wt% WOS to stabilize the Pb (total 1,246 mg/kg) and Cd (total 17 mg/kg) in a contaminated soil. The effectiveness of the WOS treatments was evaluated using various single extraction techniques. Soil amended with WOS was cured for 30 days complied with the Korean Standard Test method (0.1 M·HCl extraction). The Pb and Cd concentrations were less than the Korean warning and countermeasure standards following treatment with 5 wt% WOS. Moreover, the concentrations of Cd were greatly reduced in response to WOS treatment following extraction using 0.01 M·CaCl₂, which is strongly associated with phytoavailability. Furthermore, the soil pH and exchangeable Ca increased significantly in response to WOS treatment. Taken together, the results of this study indicated that WOS amendments improved soil quality and stabilized Pb and Cd in contaminated soil. However, extraction with 0.43 M·CH₃COOH revealed that remobilization of heavy metals can occur when the soil reaches an acidic condition.     

Soil drying in a tropical forest: Three distinct environments controlled by gap size

Soil water and temperature regimes in the tropical moist forest on Barro Colorado Island, Panama, were simulated directly from meteorological data using the model SWEAT. Separate field observations from root-exclusion, litter-removal and control treatments in one small and one large forest gap were used for calibration and validation. After irrigating all treatments to field capacity, soil matric potential and temperature were measured over 17 days at four depths ≤50 mm using the filter-paper technique and bead thermistors. Understorey environments were also simulated under the same initial conditions. The results suggest that three distinct scenarios, controlled by gap size, describe how the above- and below-ground processes controlling soil drying are coupled: (1) in the large gap, root water extraction by surrounding trees is negligible so soil drying is dominated by evaporation from the soil surface. Soil temperature is dominated by direct solar heating and cooling due to evaporation. (2) In the small gap, root water extraction dominates soil drying with soil evaporation playing a minor role. Soil temperature is still dominated by direct sunlight with some cooling due to evaporation. (3) In the understorey, root water extraction dominates soil drying. Soil temperature is dominated by heat conduction from deep soil layers with some evaporation and sensible heat transfer. The contrasting soil drying regimes imposed by variation in canopy structure enhance micro-environmental heterogeneity and the scope for differential germination and seedling establishment in coexisting tropical tree species.     

Optimization of ecosystem model parameters using spatio-temporal soil moisture information

Parameters in process-based terrestrial ecosystem models are often nonlinearly related to the water flux to the atmosphere, and they also change temporally and spatially. Therefore, for estimating soil moisture, process-based terrestrial ecosystem models inevitably need to specify spatially and temporally variant model parameters. This study presents a two-stage data assimilation scheme (TSDA) to spatially and temporally optimize some key parameters of an ecosystem model which are closely related to soil moisture. At the first stage, a simplified ecosystem model, namely the Boreal Ecosystem Productivity Simulator (BEPS), is used to obtain the prior estimation of daily soil moisture. After the spatial distribution of 0–10 cm surface soil moisture is derived from remote sensing, an Ensemble Kalman Filter is used to minimize the difference between the remote sensing model results, through optimizing some model parameters spatially. At the second stage, BEPS is reinitialized using the optimized parameters to provide the updated model predictions of daily soil moisture. TSDA has been applied to an arid and semi-arid area of northwest China, and the performance of the model for estimating daily 0–10 cm soil moisture after parameter optimization was validated using field measurements. Results indicate that the TSDA developed in this study is robust and efficient in both temporal and spatial model parameter optimization. After performing the optimization, the correlation (r²) between model-predicted 0–10 cm soil moisture and field measurement increased from 0.66 to 0.75. It is demonstrated that spatial and temporal optimization of ecosystem model parameters can not only improve the model prediction of daily soil moisture but also help to understand the spatial and temporal variation of some key parameters in an ecosystem model and the corresponding ecological mechanisms controlling the variation.     

土壤宏蛋白质组学蛋白质提取方法及其应用

土壤宏蛋白质组学在揭示土壤微生物功能、代谢与环境相互作用方面具有广阔的应用前景,但由于土壤样品的特殊性,土壤蛋白质提取步骤是限制土壤宏蛋白质组学大规模应用的瓶颈之一.本文从样品制备、提取方法、影响因素等方面综述了土壤蛋白提取方面的研究进展.一般来说,根据实验目的、蛋白种类及后续研究方法设计相应的分组成收集策略才能取得较好的提取效果.土壤总蛋白、胞内蛋白与胞外蛋白分别有不同的提取方法.总蛋白提取一般采用直接提取法;胞外蛋白不需要裂解;胞内蛋白提取方法有直接提取法和间接提取法等.裂解、浓缩、去除腐殖质的方法以及提取液、pH值的选择等也会影响提取效果.此外,简单介绍了土壤宏蛋白质组学的应用,并对今后的研究工作提出展望.表1参36     

土壤汞污染研究进展

对国内外学者近些年来对土壤汞污染研究的工作进展作了系统的综述。主要包括土壤汞污染的途径、迁移方式和治理办法。其中重点介绍了大气汞的干湿沉降、土壤汞的释放及生物修复治理土壤汞污染。最后,还介绍了土壤汞形态的分析方法以及土壤挥发性汞释放通量的测量方法。     

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)...