修复 PAHs 复合污染体系的高效菌群构建及降解特性简

从污染环境分离和筛选得到了9株PAHs降解菌,以其为基本菌种,构建高效修复PAHs复合污染体系的菌群（D）。采用平板稀释涂布计数法对降解体系中菌群（D）的动态结构进行了解析,数据显示菌群内的微生物在降解过程中能相互协作,发挥稳定且高效的降解作用。实验进一步研究了菌群D对单一PAH和混合PAHs的降解特性,结果表明,无论对单一PAH还是混合PAHs,菌群D均具有较强的降解能力。当降解历时6 d,菌群D能使40 mg/L的单一PAH平均降解85.8%,使60 mg/L的混合PAHs平均去除89.4%。菌群D在多环芳烃复合污染体系的生物修复方面具有潜在的应用价值。     

洚解菌Pigmentiphagasp．strainD-2对啶虫脒污染土壤的生物修复作用

啶虫脒属于一种新型的氯化烟碱类杀虫剂,被认为是替代有机磷农药的重要品种之一,在世界范围内已经得到了广泛的应用,其在环境中的残留备受关注,利用微生物修复异源污染物是一种有效的措施。在实验室条件下,研究了高效降解菌D-2（噬染料菌属,Pigmentiphagasp．）对被啶虫脒污染土壤的修复作用及其影响因素。结果表明,降解菌株在未灭菌土壤中的降解效果要略好于灭菌土壤,在土壤外源添加降解菌2×10^8cfu／g,温度20～40℃,弱碱性（pH7．5）的条件下,该菌株能有效降解土壤中1～200mg／kg的啶虫脒。啶虫脒施用对土壤种群结构有一定的影响,可以刺激细菌和真菌的生长,从而使土壤微生物群落结构发生改变,而降解菌的施用可缓解啶虫脒对土壤微生物的影响,修复受污染土壤。因此,人工接种降解菌D-2可提高土壤中啶虫脒的降解率,有效降低其在土壤中的残留。     

Microbial changes in rhizospheric soils contaminated with petroleum hydrocarbons after bioremediation

Effects of bioremediation on microbial communities jn soils contaminated with petroleum hydrocarbons are a scientific problem to be solved. Changes in dominate microbial species and the total amount of microorganisms including bacteria and fungi in rhizospheric soils after bioremediation were thus evaluated using field bioremediation experiments. The results showed that there were changed dominant microorganisms including ] ] bacterial strains which are mostly Gram positive bacteria and 6 fungal species which were identified. The total amount of microorganisms including bacteria and fungi increased after bioremediation of microbial agents combined with planting maize. On the contrary, fungi in rhizospheric soils were inhibited by adding microbial agents combined with planting soybean.     

1株低温石油烃降解菌的分类鉴定及降解特性研究

从渤海油船泄漏区域的海底泥中筛选到1株能降解柴油的低温石油烃降解菌T7-2,初步鉴定为红平红球菌(Rhodococcus erythropolis).研究表明,利用工业乙醇无机盐培养基培养液体种子是适宜的,其最适温度和pH分别为15℃和7.8,工业乙醇最适加入量为0.5％,菌体浓度为10⁸ CFU/mL.接种人工海水烃降解培养基后,通过补加氮源 (NH₄)₂SO₄ 2.64　g/L、磷源Na₂HPO₄ 2.5 g/L和酵母粉 0.015 g/L后,15℃振荡培养7　d,降解率可以达到73.2％.该菌降解烷烃的范围很广泛,C12～C36均有不同程度的降解.     

含氟有机化合物的生态迁移及转化

含氟有机化合物的众多特性使得其在各方面得到越来越广泛的应用,同时也成为了一种较普遍的环境污染物。本文列举了含氟有机化合物的应用类型及相应的应用特点;指明其污染途径和毒性特征;从含氟有机物的分子结构特征、降解茵的类型、外部因素三方面阐明了其生物降解特性;总结了酶作用于碳氟键使得含氟有机物发生降解的四种作用;并介绍了含氟有机污染物的生物处理和生态修复的一般方法。     

黑麦草-不动杆菌组合体系对石油污染土壤的生物强化修复

以盆栽实验为基础,研究了植物（黑麦草,Lolium perenne L）-微生物（不动杆菌,Acinetobacter sp.）组合体系对石油污染土壤的修复效果。实验结果表明：在总石油烃含量为4 420.18 mg/kg、脱氢酶活性为230.52 μg/（g·d）、苯酚毒性当量浓度（TEQphenol）为1 633.21 mg/L的初始条件下,强化组总石油烃降解率最高为53.08%,是对照组的1.60倍;土壤的脱氢酶活性达到637.73 μg/（g·d）,是对照组的10.64倍;石油污染土壤的生物毒性大幅降低, TEQphenol最终降低至171.08 mg/L。说明该组合体系对石油污染土壤具有很好的修复作用,且微生物对土壤中有毒物质的降解起主要作用。     

秦皇岛地区土壤环境中六六六污染水平调查研究

通过对秦皇岛地区土壤环境中六六六残留量的调查监测,分析了秦皇岛地区土壤六六六污染现状和危害。建议应加强农药规范化管理,制定土壤生物修复计划,大力开发生物和物理防治技术以降低土壤环境中的六六六残留量,减少对人类和生物的影响。     

多环芳烃污染土壤的微生物修复技术

对生物修复技术中的微生物进行了分类,并阐述了微生物生物降解土壤中多环芳烃（PAHs）的基本原理。在此基础上,分析了国内外微生物生物修复技术的发展概况,采用图示法重点综述了原位处理技术和非原位处理技术的工艺流程,并列举了相应的工程应用实例。     

污染土壤生物修复中存在问题的探讨

污染物生物修复过程中存在着若干问题,其中包括引入外源微生物的条件与原则,生物修复过程中微生物的适应性机制与影响因素研究;污染物的浓度与生物修复之间的关系;有机污染物降解过程中的次生污染物问题;生物修复的现场放大技术;污染物的淋溶过程;对生物修复技术的生态毒理诊断与评价等.本文旨在提高对生物修复过程中存在的重要科学问题的认识,使生物修复技术的有效利用成为可能.     

Engineered in situ bioremediation of a petroleum hydrocarbon-contaminated aquifer: assessment of mineralization based on alkalinity, inorganic carbon and stable carbon isotope balances

A concept is proposed to assess in situ petroleum hydrocarbon mineralization by combining data on oxidant consumption, production of reduced species, CH₄, alkalinity and dissolved inorganic carbon (DIC) with measurements of stable isotope ratios. The concept was applied to a diesel fuel contaminated aquifer in Menziken, Switzerland, which was treated by engineered in situ bioremediation. In the contaminated aquifer, added oxidants (O₂ and NO₃⁻) were consumed, elevated concentrations of Fe(II), Mn(II), CH₄, alkalinity and DIC were detected and the DIC was generally depleted in ¹³C compared to the background. The DIC production was larger than expected based on the consumption of dissolved oxidants and the production of reduced species. Stable carbon isotope balances revealed that the DIC production in the aquifer originated mainly from microbial petroleum hydrocarbon mineralization, and that geochemical reactions such as carbonate dissolution produced little DIC. This suggests that petroleum hydrocarbon mineralization can be underestimated if it is determined based on concentrations of dissolved oxidants and reduced species.