多环芳烃降解菌的筛选与降解能力测定

从本溪多环芳烃(PAHs)污染土壤中经富集培养筛选出8株PAHs降解菌,研究了8株菌及其等比例混合培养对菲、芘和苯并[a]芘的降解能力。结果表明,在28℃,培养基中菲、芘和苯并[a]芘的浓度分别为50、50和5mg·L-1的复合底物条件下,培养28d后,菌株B3的降解效果最好,对菲、芘和苯并[a]芘的降解率分别为88.4%、54.0%和68.4%,8株菌的混合培养对菲、芘和苯并[a]芘的降解率分别为87.7%、35.3%和42.0%;经生理生化实验和16SrRNA序列比对,初步鉴定B3菌为假单胞菌属(Pseudomonas sp.)。     

煤矿污染土壤降解苯并(a)芘微生物多样性及降解能力研究

以苯并(a)芘(50 mg/L)为唯一碳源,对新疆芦草沟煤矿开采区土壤微生物进行3代胁迫培养(每代60 d);采用PCR-DGGE方法了解不同污染程度土样中降解苯并(a)芘的微生物类群和多样性特点;利用高效液相色谱(HPLC)测定胁迫培养每代培养物混合菌群对苯并(a)芘的降解能力。PCR-DGGE结果显示:不同污染程度原始样品与苯并(a)芘胁迫培养第3代培养物的微生物香浓指数(H)、丰度(S)和均匀度(E)有所不同,其中重度污染培养物降解苯并(a)芘的微生物类群最丰富。对优势条带进行克隆,其主要归属于变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)和放线菌门(Actinobacteria)。经HPLC检测发现重度污染样品中的群体微生物对苯并(a)芘的降解率明显高于轻度和中度污染样品,达到78.4%。研究表明新疆芦草沟煤矿开采区污染的土壤中可能蕴藏着降解苯并(a)芘的微生物资源。     

固定化微生物对多环芳烃污染土壤的降解

利用微生物固定化技术,研究了微生物固定化菌剂对土壤中菲、蒽、芘、(艹屈)和苯并(a)芘的降解动态,并且采用Michaelis-Menton和Monod动力学模型对结果进行拟合.结果显示,4种处理(TB02、TB07、TBB03、TBB08)均有降解菲、蒽、芘、(艹屈)和苯并(a)芘的能力.其中,处理TB02的降解能力强、降解速率快、半衰期短且处理成本低,而处理TB07则需要较长时间作用于PAHs污染土壤,其降解能力才能充分发挥出来.当菲、蒽、芘、(艹屈)和苯并(a)芘的初始浓度均为20 mg·kg-1时,42 d后,TB02对菲、蒽、芘、(艹屈)和苯并(a)芘的降解率分别为84.32%、85.24%、82.59%、43.75%和62.25%; 133 d后,TB07对5种污染物的降解率分别为95.00%、95.24%、90.93%、74.82%和72.20%.通过比较5种污染物半衰期,其可降解性由大到小依次为菲、蒽、芘、苯并(a)芘、(艹屈).     

芘降解菌群驯化过程中的演变

【目的】筛选、驯化获得芘的高效降解菌群,为利用其对多环芳烃污染土壤进行生物修复奠定理论基础。【方法】利用芘作为底物在矿物盐培养基(MSM)中富集驯化,得到了一个混合菌群PYR,利用分光光度计和HPLC测定混合菌群的生长与降解的关系,并对混合菌群降解多环芳烃底物的广谱性和降解芘性能的稳定性进行了测定;通过冷冻干燥的方法对菌群进行了保藏,通过HPLC的方法对保藏后复壮的菌群的降解性能进行了测定;通过培养和非培养方法对菌群的多样性进行了调查,通过构建16S rRNA基因文库的方法,分析焦化厂原始土壤中菌群组成和混合菌群转接3次(PYR-3)、6次(PYR-6)和9次(PYR-9)后的组成变化。【结果】该混合菌群可以利用芘作为唯一碳源和能源生长,12 d对芘的降解率为89%,对于菲(86%)及荧蒽(49%)也具有较高的降解率,但不能降解萘和茚并芘,并且该菌群的降解活性经过多次转接和冷冻干燥保藏保持稳定,从混合菌群中分离得到了9株菌,这9株菌分布在无色杆菌属(Achromobacter),芽胞杆菌属(Bacillus),节杆菌属(Arthrobacter),微小杆菌属(Exiguobacterium)和类土地杆菌属(Parapedobacter)。系统进化分析表明变形菌门是土壤原样(100%)及以芘为底物富集的混合菌群中的主要类群(PYR-3,83%),与原土壤样品相似,PYR-3中γ-Proteobacteria(占变形菌门的77%)中假单胞菌属的菌依然占主导地位,但由于菌群的多样性增加,假单胞菌属所占比例减少。随着富集代数的增加,菌群的多样性进一步增加,γ-Proteobacteria的比例在混合菌群中的比例下降(PYR-6中占变形菌门的33%,PYR-9中占变形菌门的18%),而β-Proteobacteria在混合菌群中的比例上升(PYR-3中占变形菌门的13%,PYR-6中占变形菌门的36%,PYR-9中占变形菌门的55%)。【结论】混合菌群具有很强的芘的降解性能,并且随着传代次数的增加,菌群的组成趋于稳定。     

污染土壤中苯并(a)芘的微生物降解途径研究进展

苯并(a)芘(BaP)是一种具有强致癌、致畸和致突变的多环芳烃(PAHs)。为了修复BaP污染的土壤,探索其降解途径是很重要的。为此,综述了国内外有关污染土壤中苯并(a)芘的微生物降解情况,对不同真菌、细菌降解苯并(a)芘的能力、代谢途径、共代谢底物以及环境影响因素进行了介绍和比较,提出了苯并(a)芘中间代谢产物的累积及其环境毒性方面的研究是修复苯并(a)芘污染土壤的重要方向。     

新疆石油污染土壤苯并(a)芘降解微生物多样性研究

为研究新疆石油开采区污染土壤中苯并(a)芘降解微生物的群落结构特点,采集克拉玛依石油开采区受污染程度不同的土壤样品, 以苯并(a)芘为唯一碳源、氮源的无机盐培养基五代富集培养, 采用PCR-DGGE 技术对第五代富集培养物的微生物群落结构开展研究, 根据DGGE 指纹图谱分析它们的遗传多样性。研究显示: 三个不同污染样品微生物多样性指数(H) 丰度(S)和均匀度(EH)均有所不同, 重度污染土样降解苯并(a)芘的微生物类群最为丰富, 其次是中度污染土样, 最少的是轻度污染土样; 并且三个样品微生物类群种类差异较大, 菌落相似性低。对 DGGE 的优势条带序列分析, 同源性最高的微生物分别属于变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)、放线菌门(Actinobacteria)和厚壁菌门(Firmicutes)。研究表明新疆石油开采区污染程度不同土壤中降解苯并(a)芘的微生物群落结构不同, 提示污染严重的环境里可能蕴藏着高效降解苯并(a)芘的微生物资源。     

高分子量多环芳烃降解菌筛选及在土壤电动-生物修复中应用

采用富集培养和多环芳烃双加氧酶基因检测方法,从焦化场地多环芳烃污染土壤分离筛选出9株PAHs降解菌。以高分子量多环芳烃芘为唯一碳源进行摇瓶降解实验,结果表明,J6、S5、S4、S2和B4对芘具有较好的降解能力,21 d时芘降解率均达55%以上,其中B4处理芘的降解率最高,达到70.2%。进一步研究了该5株菌及其混合菌对土壤中芘的降解效果,发现混合菌的降解效果高于单菌的降解效果,其中混合菌H4和单菌B4的降解效果较好,49 d时混合菌H4和单菌B4处理土壤中芘的降解率达29.3%和18.3%。经过16S rRNA基因序列比对,鉴定J6菌株为赤红球菌(Rhodococcus ruber),S5为芽孢杆菌属(Bacillus sp.),S4和S2是鞘脂单胞菌属(Sphingopyxis sp.),B4为假单胞菌属(Pseudomonas sp.)。在电场条件下,混合菌H4和单菌B4处理微生物数量及活性均显著提高,芘的降解率较单独H4和B4处理提高33.0%和20.1%,说明筛选出的5株高分子量多环芳烃降解菌具有较强的电场适应能力,可在高分子量多环芳烃污染土壤电动-微生物修复中应用。     

高环多环芳烃降解菌的筛选及其降解特性

通过富集培养及平板升华法从本溪钢铁公司周边多环芳烃(PAHs)污染土壤中分离出7株PAHs降解菌。以芘和苯并[a]芘为底物进行摇瓶降解实验,结果表明:G1、G2和G3菌株对高环PAHs芘和苯并[a]芘均具有较强的降解能力。进一步研究此3株菌及混合菌对原状污染土壤中PAHs的降解能力,发现80 d时对总PAHs的降解顺序依次为:混合菌G2G1G3,其中混合菌对PAHs降解率较单菌分别提高了9.17%、11.49%和16.11%;4个处理对4~6环PAHs的降解率较对照组相比提高的倍数随着环数增加而增大;总PAHs的降解率与脱氢酶的活性呈正相关。电场影响G1、G2和G3菌株对PAHs降解,在1.0 V·cm~(-1)电场条件下,4环、5环及6环PAHs降解率较单纯微生物修复提高12.13%、13.35%和14.52%,说明3株菌具有较强的电场适应能力,可在高环PAHs污染土壤的电动-微生物修复中应用。形态学观察及16S rRNA序列比对分析表明,G1、G2、G3菌株分别为鞘氨醇单胞菌属(Sphingomonas sp.)、苍白杆菌属(Ochrobactrum sp.)和无色杆菌属(Achromobacter sp.)。     

一株高分子量多环芳烃降解菌的筛选、鉴定及降解特性研究

采用富集培养方法从多环芳烃污染土壤中筛选分离得到1株能以苯并[a]芘(B[a]P)为唯一碳源和能源生长的菌株.形态特征观察和16S rDNA序列分析结果表明,该菌株为副球菌属(Paracoccus sp.),编号为HPD-2.HPD-2在3.0 mg/L的B[a]P液体培养基中生长较慢,培养5 d后B[a]P的降解率为89.7%.同时,该菌株对四环的芘和荧蒽也具有较好的降解能力,培养7 d后芘和荧蒽的降解率分别达到47.2%和84.5%.可见,该菌株对高分子量PAHs具有很好的降解潜力.     

芘降解菌Pseudomonas sp.PR3的植物促生特性及其对芘胁迫下水稻生长的影响北大核心CSCD

农田中不断积累的多环芳烃不仅严重影响作物生长,同时增加粮食安全风险。筛选兼具促进植物生长特性和降解污染物功能的微生物菌株是解决上述问题的一种有效手段。从油田附近生长的植物根表分离得到一株具有芘降解能力,同时还具有溶磷、产吲哚乙酸和铁载体等植物促生特性的菌株PR3,经16S rDNA序列同源性分析确定为假单胞菌(Pseudomonas sp.)。菌株PR3在无机盐培养液中生长14 d后,对芘(20 mg/L)的降解率可达94%,对萘(50 mg/L)、菲(50 mg/L)、苯并(a)芘(10 mg/L)的降解率也分别达到92%,84%和47%。同时,该菌株7 d内最大溶磷量为756.25 mg/L,2 d内IAA合成量可达14.46 mg/L,4 d内生成铁载体的活性单位可达58.53%。在不同芘污染浓度处理下的盆栽实验表明,接种PR3可有效促进水稻生长并提高根际土壤中芘的降解,去除率可达72.02%-86.22%,同时显著降低水稻根及地上部中的芘含量,分别为21.81%-53.01%和49.81%-57.17%。因此,菌株PR3有助于实现芘污染土壤的生态修复以及降低作物芘暴露的风险。     

Indigenous and enhanced mineralization of pyrene, benzo[a]pyrene, and carbazole in soils.

We studied the mineralization of pyrene, carbazole, and benzo[a]pyrene in soils obtained from three abandoned coal gasification plants in southern Illinois. The soils had different histories of past exposure to hydrocarbon contamination and different amounts of total organic carbon, microbial biomass, and microbial activity. Mineralization was measured by using serum bottle radiorespirometry. The levels of indigenous mineralization of 14C-labeled compounds ranged from 10 to 48% for pyrene, from undetectable to 46% for carbazole, and from undetectable to 25% for benzo[a]pyrene following long-term (greater than 180-day) incubations. Pyrene and carbazole were degraded with short or no lag periods in all soils, but benzo[a]pyrene mineralization occurred after a 28-day lag period. Mineralization was not dependent on high levels of microbial biomass and activity in the soils. Bacterial cultures that were capable of degrading pyrene and carbazole were isolated by enrichment, grown in pure culture, and reintroduced into soils. Reintroduction of a pyrene-degrading bacterium enhanced mineralization to a level of 55% within 2 days, compared with a level of 1% for the indigenous population. The carbazole degrader enhanced mineralization to a level of 45% after 7 days in a soil that showed little indigenous carbazole mineralization. The pyrene and carbazole degraders which we isolated were identified as a Mycobacterium sp. and a Xanthamonas sp., respectively. Our results indicated that mineralization of aromatic hydrocarbons can be significantly enhanced by reintroducing isolated polycyclic aromatic hydrocarbon-degrading bacteria.     

Indigenous and enhanced mineralization of pyrene, benzo[a]pyrene, and carbazole in soils.

We studied the mineralization of pyrene, carbazole, and benzo[a]pyrene in soils obtained from three abandoned coal gasification plants in southern Illinois. The soils had different histories of past exposure to hydrocarbon contamination and different amounts of total organic carbon, microbial biomass, and microbial activity. Mineralization was measured by using serum bottle radiorespirometry. The levels of indigenous mineralization of 14C-labeled compounds ranged from 10 to 48% for pyrene, from undetectable to 46% for carbazole, and from undetectable to 25% for benzo[a]pyrene following long-term (greater than 180-day) incubations. Pyrene and carbazole were degraded with short or no lag periods in all soils, but benzo[a]pyrene mineralization occurred after a 28-day lag period. Mineralization was not dependent on high levels of microbial biomass and activity in the soils. Bacterial cultures that were capable of degrading pyrene and carbazole were isolated by enrichment, grown in pure culture, and reintroduced into soils. Reintroduction of a pyrene-degrading bacterium enhanced mineralization to a level of 55% within 2 days, compared with a level of 1% for the indigenous population. The carbazole degrader enhanced mineralization to a level of 45% after 7 days in a soil that showed little indigenous carbazole mineralization. The pyrene and carbazole degraders which we isolated were identified as a Mycobacterium sp. and a Xanthamonas sp., respectively. Our results indicated that mineralization of aromatic hydrocarbons can be significantly enhanced by reintroducing isolated polycyclic aromatic hydrocarbon-degrading bacteria.     

Polycyclic aromatic hydrocarbon degradation by a Mycobacterium sp. in microcosms containing sediment and water from a pristine ecosystem

Microcosm studies were conducted to evaluate the survival and performance of a recently discovered polycyclic aromatic hydrocarbon (PAH)-degrading Mycobacterium sp. when this organism was added to sediment and water from a pristine ecosystem. Microcosms inoculated with the Mycobacterium sp. showed enhanced mineralization, singly and as components in a mixture, of 2-methylnaphthalene, phenanthrene, pyrene, and benzo[alpha]pyrene. Studies utilizing pyrene as the sole added PAH showed that the Mycobacterium sp. survived in microcosms for 6 weeks both with and without preexposure to PAH and mineralized multiple doses of pyrene. Pyrene mineralization rates for sterilized microcosms inoculated with the Mycobacterium sp. showed that competition with indigenous microorganisms did not adversely affect survival of or pyrene degradation by the Mycobacterium sp. Pyrene mineralization by the Mycobacterium sp. was not enhanced by inorganic nutrient enrichment and was hindered by organic nutrient enrichment, which appeared to result from overgrowth of indigenous bacteria. This study demonstrates the versatility of the PAH-degrading Mycobacterium sp. and expands its potential applications to include the degradation of two-, three-, four-, and five-ringed PAHs in sediments.     

Polycyclic aromatic hydrocarbon degradation by a Mycobacterium sp. in microcosms containing sediment and water from a pristine ecosystem.

Microcosm studies were conducted to evaluate the survival and performance of a recently discovered polycyclic aromatic hydrocarbon (PAH)-degrading Mycobacterium sp. when this organism was added to sediment and water from a pristine ecosystem. Microcosms inoculated with the Mycobacterium sp. showed enhanced mineralization, singly and as components in a mixture, of 2-methylnaphthalene, phenanthrene, pyrene, and benzo[alpha]pyrene. Studies utilizing pyrene as the sole added PAH showed that the Mycobacterium sp. survived in microcosms for 6 weeks both with and without preexposure to PAH and mineralized multiple doses of pyrene. Pyrene mineralization rates for sterilized microcosms inoculated with the Mycobacterium sp. showed that competition with indigenous microorganisms did not adversely affect survival of or pyrene degradation by the Mycobacterium sp. Pyrene mineralization by the Mycobacterium sp. was not enhanced by inorganic nutrient enrichment and was hindered by organic nutrient enrichment, which appeared to result from overgrowth of indigenous bacteria. This study demonstrates the versatility of the PAH-degrading Mycobacterium sp. and expands its potential applications to include the degradation of two-, three-, four-, and five-ringed PAHs in sediments.     

糙皮侧耳和鞘脂菌NS7对多环芳烃污染土壤的生物强化与协同作用

[背景] 真菌和细菌被认为在多环芳烃污染土壤生物修复过程中发挥协同作用,目前在真实土壤体系中开展真菌-细菌协同降解研究较少。[目的] 研究真菌和细菌对不同种类多环芳烃降解的差异及对蒽和苯并[a]蒽的生物强化与协同作用。[方法] 选用多环芳烃降解真菌和细菌各一株,在液体纯培养体系下分析它们对不同种类多环芳烃降解的差异,在土壤体系中采用放射性同位素示踪技术研究2种微生物对蒽和苯并[a]蒽的生物强化与协同作用。[结果] 供试细菌鞘脂菌NS7能够很好地降解低环种类多环芳烃,以蒽作为唯一碳源时可以将其完全降解,在复合污染条件下对菲、蒽、荧蒽、芘等降解效果突出（>90%）,对苯并[a]芘降解效果较差（9.76%）。相比而言,供试真菌糙皮侧耳菌对苯并[a]芘具有更好的降解效果（21.18%）,对低环多环芳烃降解效果明显不如降解菌NS7。在自然土壤中,蒽和苯并[a]蒽具有明显不同的矿化效率,分别为18.61%和4.28%,在蒽污染土壤中加入鞘脂菌NS7并未显著提高蒽的矿化率（P>0.05）,相比而言,苯并[a]蒽污染土壤中加入糙皮侧耳显著提高了污染物矿化效率（2.24倍）,表明真菌和细菌在土壤环境中的定殖存活能力可能影响了生物强化效果。采用灭菌土壤排除土著微生物的竞争排斥作用,研究了真菌菌丝对生物强化降解的影响,发现在蒽污染土壤中,真菌菌丝的迁移作用显著提高了细菌鞘脂菌NS7对污染物的矿化率,从1.75%提高到5.91%;而在苯并[a]蒽灭菌污染土壤中,接种糙皮侧耳却没有发现苯并[a]蒽矿化率提高的现象,表明自然土壤中真菌强化降解苯并[a]蒽的作用可能是源于真菌菌丝促进污染物和土著降解菌的接触,而非直接来自真菌本身。[结论] 细菌能够很好地降解低环种类多环芳烃,而真菌对高环种类多环芳烃降解效果较好。真菌可能通过菌丝促进土著微生物在土壤中的迁移,增大多环芳烃和土著降解菌的接触,从而促进了多环芳烃降解。研究加深了对多环芳烃污染土壤生物强化修复的认识,对发展基于真菌-细菌协同作用的生物强化与调控技术提供理论指导。     

Degradation and mineralization of high-molecular-weight polycyclic aromatic hydrocarbons by defined fungal-bacterial cocultures

This study investigated the biodegradation of high-molecular-weight polycyclic aromatic hydrocarbons (PAHs) in liquid media and soil by bacteria (Stenotrophomonas maltophilia VUN 10,010 and bacterial consortium VUN 10,009) and a fungus (Penicillium janthinellum VUO 10, 201) that were isolated from separate creosote- and manufactured-gas plant-contaminated soils. The bacteria could use pyrene as their sole carbon and energy source in a basal salts medium (BSM) and mineralized significant amounts of benzo[a]pyrene cometabolically when pyrene was also present in BSM. P. janthinellum VUO 10,201 could not utilize any high-molecular-weight PAH as sole carbon and energy source but could partially degrade these if cultured in a nutrient broth. Although small amounts of chrysene, benz[a]anthracene, benzo[a]pyrene, and dibenz[a,h]anthracene were degraded by axenic cultures of these isolates in BSM containing a single PAH, such conditions did not support significant microbial growth or PAH mineralization. However, significant degradation of, and microbial growth on, pyrene, chrysene, benz[a]anthracene, benzo[a]pyrene, and dibenz[a,h]anthracene, each as a single PAH in BSM, occurred when P. janthinellum VUO 10,201 and either bacterial consortium VUN 10,009 or S. maltophilia VUN 10,010 were combined in the one culture, i.e., fungal-bacterial cocultures: 25% of the benzo[a]pyrene was mineralized to CO(2) by these cocultures over 49 days, accompanied by transient accumulation and disappearance of intermediates detected by high-pressure liquid chromatography. Inoculation of fungal-bacterial cocultures into PAH-contaminated soil resulted in significantly improved degradation of high-molecular-weight PAHs, benzo[a]pyrene mineralization (53% of added [(14)C]benzo[a]pyrene was recovered as (14)CO(2) in 100 days), and reduction in the mutagenicity of organic soil extracts, compared with the indigenous microbes and soil amended with only axenic inocula.     

Removal of surfactant solubilized polycyclic aromatic hydrocarbons by Phanerochaete chrysosporium in a rotating biological contactor reactor

White rot fungi can oxidize surfactant solubilized polycyclic aromatic hydrocarbons (PAH). The objective of this study was to evaluate the performance of immobilized white rot fungus, Phanerochaete chrysosporium, to remove surfactant Tween 80 solubilized PAH i.e. phenanthrene, pyrene and benzo(alpha)pyrene in a rotating biological contactor (RBC) reactor. Results indicated that the immobilized P. chrysosporium in the RBC reactor system in continuous operation could effectively remove the three tested PAH at specific hydraulic loading rates and concentrations tested for each individual PAH. Batch operation of RBC reactor showed that the immobilized P. chrysosporium was stable and effective for the eight successive batch treatments of PAH in solution medium i.e. PAH removal was greater than 90% after 60 h, although only low levels of ligninolytic enzyme activity were detected. The removal of phenanthrene and pyrene in solution medium has been found to be a first order reaction in batch operation. A mass balance calculation indicated that biological oxidation was the main factor for removal of benzo(alpha)pyrene i.e. 95.7% in the RBC reactor. However, for phenanthrene and pyrene, both biological oxidation (i.e. 49 and 56%, respectively) and RBC disc foam adsorption (i.e. 44 and 34%, respectively) made a significant contribution to the removal of PAH.     

Bioassay-based screening of microorganisms that degrade dioxin using substrate-immobilized microtubes

In the current study, we attempted to develop a method for bioassay-based screening of microorganisms that degrade dioxin. However, a crucial problem encountered was that the standard dioxin 2,3,7,8-tetrachlorodibenzo-p-dioxin (TCDD) added to bacterial medium immediately disappeared from the liquid phase due to its adsorption onto polypropylene (PP) tubes. Among other aromatic hydrocarbons, adsorption onto PP tubes was also observed in beta-naphthoflavone but not in benzo[a]pyrene. Adsorption of TCDD was observed not only onto PP tubes but also onto polystyrene, glass, and PP tubes with low affinity for DNA or protein. Silanization was not effective at preventing adsorption of TCDD. TCDD immobilized onto PP tubes was recovered by organic solvents, including ethanol, methanol, and dimethyl sulfoxide (DMSO). The elution efficiency of the immobilized TCDD by DMSO was approximately 85%. Based on these findings, screening of bacteria that degrade dioxin was attempted as follows. First, TCDD was immobilized onto PP tubes. Second, bacterial suspension was added to the tubes and incubated for biodegradation of TCDD. Third, remaining, immobilized TCDD was eluted by DMSO and subjected to a reporter bioassay to evaluate the level of TCDD. Using this method, we demonstrated successful screening of bacteria that have the potential for degradation of dioxin.     

Fate of phenanthrene, pyrene and benzo[a]pyrene during biodegradation of crude oil added to two soils

The release of 14CO2 from 9-[14C]phenanthrene, 4,5,9,10-[14C]pyrene and 7-[14C]benzo[a]pyrene, added to Brent/Fortes crude oil and mixed into a pristine sand soil (0.40% organic C) and a pristine organic soil (22.9% organic C), was determined. After 244 days at 25 degrees C, 11.1 +/- 3.5% (sand) and 17.1 +/- 0.30% (organic) phenanthrene-14C and 9.77 +/- 2.8% (sand) and 5.86 +/- 1.4% (organic) benzo[a]pyrene-14C was released. After 210 days, 3.65 +/- 0.5% (sand) and 4.43 +/- 0.33% (organic) pyrene-14C was released. Inoculation of these two soils with DC1 and PD2 (bacteria capable of accelerating the phenanthrene and pyrene mineralisation in soil in the absence of crude oil) either at day 0 or after release as 14CO2 by indigenous degraders had ceased, failed to increase or initiate further mineralisation. Thus, aged PAH residues were non-bioavailable to these metabolically competent degrading microorganisms. At the end of the first period of incubation (210 days or 244 days), the total aromatic hydrocarbons recovered using Soxhlet extraction was 0.18% (sand) and 42.8% (organic) compared with approximately 100% from bio-inhibited soils. This confirmed that the indigenous microbiological activity not only caused a limited amount of PAH mineralisation but also reduced the extractability of residues, possibly due to the generation of metabolites which were chemisorbed and bound (and non extractable) in 'aged' soils.     

植物法生物修复PAHs和矿物油污染土壤的调控研究

选择苜蓿草为供试植物,以污染物含量水平、专性细菌和真菌及有机肥为调控因子,进行了植物法生物修复多环芳烃(PAHs)和矿物油污染土壤的调控研究。结果表明,PAHs和矿物油的降解率与有机肥含量呈正相关,增加有机肥5%,可提高矿物油降解率17.6%～25.6%,PAHs降解率9%.在植物存在条件下,土壤微生物降解功能增强。多环芳烃总量的平均降解率比无植物对照土壤提高2.0%～4.7%.投加特性降解真菌可不同程度地提高土壤PAHs总量和矿物油的降解率。真菌对萤蒽、芘和苯(a)蒽/(艹屈)的降解有明显促进作用。而细菌能明显提高苊稀/芴、蒽和苯(a)萤蒽/苯(k)萤蒽的降解率。