一株菲降解菌的分离鉴定及其降解条件研究

以菲为研究对象,从克拉玛依稠油污染土壤中筛选到1株对菲具有较好降解效果的菌株JZ3-21。通过形态观察、生理生化指标及16S rDNA序列分析对该菌株进行了鉴定。该株菌的16S rDNA序列与Pseudomonas属的相似性达99%,结合分离菌株的形态、生理生化特征和16S rDNA基因序列的分析结果,初步鉴定该菌株为恶臭假单胞菌（Pseudomonas putida.）。对其降解条件进行了研究,结果表明：在40℃,pH 8.0,接种量为1.5%的条件下,菌株对初始质量浓度为100 mg.L-1的菲在64 h内的降解率高达94.2%。该菌对高质量浓度菲有较好的耐受性,其最高耐受质量浓度可达2 000 mg.L-1。     

嗜铁细菌枯草芽胞杆菌Bs-15对辛硫磷的降解特性

为探讨嗜铁细菌对农药辛硫磷的降解及其土壤修复的潜能,采用改良定向培育法,对嗜铁细菌枯草芽胞杆菌(Bacillus subtilis)Bs-15进行驯化,摸索其降解条件,并测定其土壤修复能力.结果显示,菌株Bs-15对辛硫磷有较高的耐受性,在辛硫磷浓度达到800 mg L-1时仍可生长;可以以辛硫磷为唯一碳源生长,适合其降解的最佳外加营养物质为酵母粉,无机盐为MgCl2.最适辛硫磷降解浓度为≤100 mg L-1,浓度继续升高时降解效能明显降低;最适降解温度为35℃;对pH值有较广的适应范围,在pH 5-9时降解率较高;最适降解时间为24 h,振荡速率为150 r min-1,接种量为8%;土壤修复试验表明,此菌株在第20天时对土壤中辛硫磷的降解率接近50%.本研究结果说明枯草芽胞杆Bs-15对辛硫磷具有较好的降解作用,对辛硫磷污染的土壤具有良好的修复潜能.     

乐果降解菌LGX1的筛选及其降解特性研究

通过富集培养,从连续施用农药乐果的土壤中分离得到一株具有较强降解有机磷农药乐果能力的细菌菌株LGX1,通过菌落形态观察及细菌的16SrDNA测序,对其进行了鉴定,同时初步研究了其降解性能。结果表明：该菌株为蜡状芽孢杆菌（Bacillus cereus）,在接种量为20%,乐果初始质量浓度为100mg·L-1,外加碳源葡萄糖质量分数为2%,温度为35℃,初始pH值为4时该菌株对乐果的降解能力最强;并且能在以辛硫磷、毒死蜱和三唑磷为唯一碳源的基础盐培养基中生长,且均比在以乐果为唯一碳源的基础盐培养基中生长的OD600值要高,初步推断菌株LGX1对有机磷农药的降解有一定的广谱性。     

一株同时降解3种邻苯二甲酸酯降解菌的筛选鉴定及降解特性

选择邻苯二甲酸二甲酯(DMP)、邻苯二甲酸二丁酯(DnBP)和邻苯二甲酸二(2-乙基己基)酯(DEHP)作为目标污染物,采用富集驯化法从设施菜地土壤中筛选出1株可同时降解DMP、DnBP和DEHP的细菌MB1.经形态、生理生化特征及16S rDNA序列分析,初步鉴定为微杆菌属(Microbacterium sp.).通过正交试验研究了该菌株的最优降解条件以及最优条件下该菌株的生长曲线和降解曲线,最后在培养条件下研究了该菌株对人工污染土壤中邻苯二甲酸酯的降解特性.结果表明,菌株MB1的最优降解条件为:pH值为8,温度为25℃,接菌量为5%,每种邻苯二甲酸酯浓度为300 mg·L~(-1).在此最优条件下该菌株呈S型曲线增长,7 d后无机盐培养液中DMP、DnBP和DEHP的降解率分别为99.62%%、99.65%和55.26%.人工污染土壤中空白试验和投加菌株试验结果为:在不添加菌液的处理中,灭菌土壤21 d时DMP、DnBP和DEHP的降解率分别为3.86%、4.19%和2.01%;未灭菌土壤21 d时对DMP、DnBP和DEHP的降解率分别为4.82%、5.99%和3.44%.在添加菌液的处理中,21 d时土壤灭菌处理中DMP、DnBP和DEHP的降解率分别达94.45%、95.65%和39.21%;而土壤未灭菌处理中DMP、DnBP和DEHP的降解率分别达94.93%、95.99%和41.16%.该结果表明:土壤中土著微生物仅能降解微量PAEs,菌株MB1对土壤中DMP、DnBP和DEHP等3种PAEs污染物具有较为高效的降解能力,未灭菌土壤中邻苯二甲酸酯的降解效果略高于灭菌土壤.     

一株高效邻苯二甲酸二丁酯降解菌的筛选、鉴定及其降解特性研究

从活性污泥中分离出1株以邻苯二甲酸二丁酯(DBP)为碳源和能源生长的高效降解菌DP-2,经形态观察、生化鉴定及16S rDNA序列分析,鉴定该菌株为不动杆菌(Acinetobacter sp.).采用单因素试验研究了不同试验条件(接种量、DBP浓度、NaCl浓度和碳源)对菌株DBP降解特性的影响,结果表明:接种量大于10%时,菌株DP-2在3 d内对初始浓度为10 mg·L~(-1)的DBP降解率可达到90%以上;DBP初始浓度为5—50 mg·L~(-1)时,菌株在6 d内对DBP降解率均能达到90%以上,但高浓度DBP会影响菌株DP-2生长,DBP浓度为1000 mg·L~(-1)时,DBP降解率仅为26.88%;菌株降解DBP的最佳NaCl浓度范围为0—20 g·L~(-1);此外,醋酸钠、蔗糖、葡萄糖添加对于菌株降解DBP均有一定的促进作用,其中葡萄糖效果最为明显.在此基础上,采用响应曲面法优化了菌株降解DBP的培养条件并进行了试验验证,在盐度为5 g·L~(-1),接种量为17.14%,底物浓度为9.81 mg·L~(-1),菌株对DBP的降解率为85.86%.     

基于均匀设计优化新鞘氨醇菌US6-1对高分子量多环芳烃的降解条件

运用均匀设计优化一株新鞘氨醇菌Novosphingobium pentaromativorans stain US6-1对芘、荧蒽、苯并[a]芘等高分子量多环芳烃(High molecular weigh polycyclic aromatic hydrocarbons,HMW-PAHs)的降解条件.结果表明,在最适生长条件(30℃、pH 6.5及NaCl浓度为2.5%)下,接种量与底物浓度是影响该菌降解能力的关键因素.在接种量D660 nm为0.6、芘初始浓度56 mg L-1、培养时间5 d的情况下,菌株US6-1对芘的降解达到32.5 mg L-1,预测平均准确率达99.38%;在接种量D660 nm为0.6、荧蒽初始浓度48 mg L-1、培养时间5 d的情况下,对荧蒽的降解达到34.3 mg L-1,预测平均准确率达99.61%;在接种量D660 nm为0.1、苯并[a]芘初始浓度60 mg L-1、培养时间为5 d时,对苯并[a]芘的降解达到24 mg L-1,预测平均准确率达98.75%.菌株US6-1对芘及苯并[a]芘的降解能力比未优化前分别提高了29.2%与58%.     

一株除草剂氰氟草酯降解菌的分离鉴定与降解特性

氰氟草酯(Calofop-buty1)是一种芳氧苯氧羧酸酯类除草剂,其迁移、转化和分解等行为对环境及人类健康具有潜在危害.为了解其微生物代谢机制,从长期使用氰氟草酯的稻田土壤中分离到1株氰氟草酯降解菌株,命名为QDZ-B.菌株QDZ-B的16S rDNA基因序列长度为1 400 bp,在RDP数据库比对结果表明其与寡养食单胞菌属菌株的同源性最近,与模式菌株嗜麦寡养食单胞菌Stenotrophomonas maltophilia(AB008509)的同源性为99.8%.根据表型特征、生理生化特性和16S rDNA序列同源性分析,将菌株QDZ-B鉴定为寡养单胞菌属(Stenotrophomonas sp.).接种量为5%时,菌株QDZ-B在基础盐液体培养基中5 d对100 mg L-1氰氟草酯的降解率约为88.2%.菌株QDZ-B的降解效果与接种量成正相关,但接种量大于5%时,降解效率趋于平稳.菌株QDZ-B降解氰氟草酯的最适温度为30℃,最适pH为7.0.通过质谱分析鉴定了3个菌株QDZ-B降解氰氟草酯的代谢产物,分别为氰氟草酸、氰氟草酰胺和2-氟-3-对-乙氧基苯氧基苯酰胺.     

高效甲醛降解菌处理突发污染事故研究

通过选择培养,选育到1株能快速降解高浓度甲醛的菌株BZ-001H,经鉴定为Bacillus cereus,其最适降解条件是30℃和pH 7.0,最适浓度为8 000 mg L-1,最佳接种量为0.3‰,甲醛浓度越高时对pH的变化越敏感.用BZ-001H作为功能菌株对活性污泥系统强化后应急处理含2 035.67 mg L-1、4 155.63 mg L-1、8 099.27 mg L-1浓度甲醛的模拟废液,2.5h、6 h、14 h后去除率都能达到99%以上.模拟甲醛突发污染事故场景与应用条件,用BZ-001H强化常规SBR工艺应急处理4 073.65 mg L-1甲醛废液,经过8 h降解,可使出水甲醛达到《污水综合排放标准》(GB 8978-1996)一级标准.同时,考察了应急处理过程对应急系统和常规系统的影响,结果表明,应急处理结束后,应急SBR系统运行2周期后COD达标排放,6周期后氨氮达标排放;而对照系统受冲击明显,运行10周期后氨氮仍未达标,去处率仅为18.81%.     

一株微囊藻毒素-LR降解菌的降解特性

研究了从某人工湖底泥中筛选出的1株能够降解微囊藻毒素-LR(MC-LR)的菌株JM13的降解特性.实验结果表明,当加入50 mg·L-1淀粉作为外加碳源时,菌株对初始浓度为0.5 mg·L-1MC-LR的降解率可达44.5%;低浓度重金属Cu2+的加入可在一定程度上提高菌株对MC-LR的降解,降解率可达到44.8%;随着时间的延长,菌株对MC-LR的降解率不断增大,到第10天达到52.6%,当投入菌龄为36 h的菌悬液时,降解率可达到55.4%.对该菌株细胞表面疏水性(CSH)的测试结果显示,在菌JM13细胞表面疏水性最大的情况下(即有机∶相水相=3∶4时),添加淀粉及低浓度(0.5 mg·L-1)Cu2+可以在一定程度上抵御降解过程中细菌表面疏水性的降低,使菌体细胞能更好地同污染物接触,从而在一定程度上提高菌株对MC-LR的降解.     

一株菲降解菌的特性及相关降解基因的克隆

从石油污染土壤中分离到一株菲降解菌2F5-2.根据该菌株生理生化特征和16S rDNA序列相似性分析,将其初步鉴定为鞘氨醇杆菌属(Sphingobium sp.).该菌株在10 h内对100 mg/L的菲的降解率为100%.降解菲的最适温度为30℃,最适pH为7.对降解途径的初步研究显示,该菌株通过水杨酸途径降解菲.克隆了编码芳香烃双加氧酶α亚基的基因phdA,它与菌株Sphingomonas sp.P2、Sphingobium yanoikuyae B1、Sphingomonas sp.ZP1中phdA的同源性分别为97.9%、98%和100%,表明该基因具有保守性.图6参16     

涕灭威等三种农药在土壤中的移动性

涕灭威、呋喃丹和拉索三种农药在土壤中的淋溶结果表明，经过３０ｃｍ土柱下渗到收集器中的涕灭威为８８．０％，呋喃丹为６９．１％，拉索为１．８４％；农药在四种土壤中的淋溶速度，砂土＞砂壤土＞粘壤土＞粘土；土壤性质对农药移动的影响比农药自身性质的影响要小。     

林丹和呋喃丹对赤子爱胜蚓存活、生长和繁殖能力的影响

采用人工土培养法,通过急性和亚急性暴露实验,研究了林丹和呋喃丹对赤子爱胜蚓(Eisenia foetida)存活、生长和繁殖能力的影响.结果表明,1)林丹对蚯蚓14d LC50为162.09mg·kg-1,属低等毒性;呋喃丹对蚯蚓14d LC50为3.11mg·kg-1,属中等毒性.2)林丹在急性暴露期显著抑制蚯蚓的生长,在亚急性暴露期低浓度林丹对蚯蚓生长影响不显著,高浓度林丹则显著抑制蚯蚓的生长;呋喃丹在急性和亚急性暴露期对蚯蚓的生长均具有极显著的抑制作用.3)林丹和呋喃丹均可显著抑制蚯蚓的繁殖能力.4)林丹和呋喃丹均可对蚯蚓皮肤结构造成损伤,林丹的损伤程度较严重,呋喃丹相对较弱.5)LC50可以迅速有效地对农药的毒性进行初步判断,而生长抑制率和幼虫孵化数是更加敏感的评估农药对蚯蚓毒性的指标.     

The chemistry and parent material of urban soils in Bristol (UK): implications for contaminated land assessment

An earlier survey of topsoil from parks and allotment in the city of Bristol (UK) revealed the presence of relatively high levels of “pseudo-total” Cd, As, Cu, Pb and Zn, with Cd and As exceeding present UK soil guidelines. This follow-up work aimed at (1) estimating geochemical thresholds for these elements based on “near-total” soil, bedrock and sediment heavy metals and (2) determining the genetic relationship between soil and bedrock using rare earth elements (REEs or lanthanides) as tracers. “Near-total” concentration of 34 elements (Al, Ca, Fe, K, Mg, Na, As, Ba, Cd, Cr, Cu, Li, Mn, Ni, P, Pb, Sc, Ti, V, Zn, Y and the rare earth elements Ce, Dy, Er, Eu, Gd, Ho, La, Lu, Nd, Pr, Sm, Tb, Yb) were obtained by ICP-MS and ICP-OES. The results show that the soil composition is largely controlled by the soil parent material, though extreme outliers are indicative of contamination at a few sites of parkland and allotments. Cumulative frequency plots show the presence of different data sets for which separate “background” values should be determined. The REE data provide evidence that weathering of the underlying sandstone was a determinant factor leading to the relatively high heavy metal enrichment found in soil samples and sediments. Reference to UK soil guidelines to decide on possible remediation measures could be very misleading due to the natural high background levels of some elements in the underlying bedrock. Before defining land as “contaminated”, a thorough geochemical investigation is required at local scale in order to produce a more realistic and correct environmental assessment.     

基于RS-GIS的湖北丹江库区土壤水力侵蚀定量分析

湖北丹江库区是南水北调中线工程的主要淹没区和水源区,土壤水力侵蚀是影响水质安全和工程实施的重要因素。以1998年和2003年的TM遥感影像为主要信息源,建立了以植被覆盖度、坡度和土地利用为指标的水力侵蚀遥感分析方法,将水力侵蚀强度分为六级,并结合GIS的空间分析功能对1998年和2003年库区水力侵蚀强度变化及空间分布进行了划分。结果表明五年间库区微度侵蚀、中度侵蚀和强度侵蚀面积呈增加趋势,而轻度侵蚀和极强度侵蚀面积呈减少趋势;并将库区水力侵蚀空间分布划分为北部中低山丘陵中强度侵蚀区和中部河谷城区轻度流失区。分析结果对库区土壤侵蚀的治理和生态环境的改善具有指导意义。     

第四纪红壤不同熟化措施下的阴离子态养分含量及其剖面分布

本文对第四纪红壤及其发育的土壤中的６种必需阴离子态养分含量及其在土壤剖面中的分布进行了系统的讨论．结果表明，第四纪红壤中的各种必需阴离子态养分含量与土壤耕作熟化措施有关．荒地的ＮＯ、Ｃｌ－、Ｈ２ＢＯ较高，而开垦为旱地后，它们的含量下降；Ｈ２ＰＯ在土壤经过耕作熟化后有所提高；ＭｏＯ的含量则基本保持不变；与其它阴离子显著不同的是．经耕作熟化后，土壤有效性ＳＯ含量急剧增加，不同的阴离子态养分在土壤剖面中的分布特点不同．     

典型产业承接区土壤砷含量的空间分布特征及影响因素

本文以揭阳市为研究区域,采集了1330个表层土壤(0—20 cm)样品和331个深层土壤(150—200 cm)样品,利用富集因子法分析了表层土壤中As的污染状况,通过GIS空间分析技术以及单因素分析法探究了土壤As的空间分布特征以及影响因素.结果表明,研究区表层土壤As含量的均值为6.03 mg·kg^-1,低于该区土壤背景值(7.16 mg·kg^-1)及农用地土壤污染风险管控值(20 mg·kg^-1),大部分土壤为轻微污染和中度污染.揭阳市表层土壤As含量高值区分布于揭阳市东北部、中部和西南部地区,低值区分布于西北部和东南部地区.土壤类型、成土母质和土地利用类型是影响表层土壤As含量的重要因素,在不同土壤类型中,黄壤和赤红壤As含量相对较高;不同成土母质中,粉砂岩母质土壤As含量显著高于其他母质;在不同土地利用类型中,农用地土壤As含量最高.     

Effect of the nitrification inhibitor dicyandiamide on microbial communities and N<Subscript>2</Subscript>O from an arable soil fertilized with ammonium sulphate

Nitrous oxide (N₂O) affects climate change as a greenhouse gas and indirectly contributes to stratospheric ozone depletion. The main source of N₂O in soils is denitrification which requires high soil moisture, carbon and nitrate. Nitrification inhibitors can be used to mitigate emissions of N₂O from soils. In Portugal, fertilisers are often applied when soils are still relatively warm and moist conditions conducive to denitrification. A Portuguese arable soil was inhibited with dicyandiamide, a nitrification inhibitor and the effect on soil microbiological activity and composition was determined after 46 days. Soils were then incubated and received carbon and ammonium under high soil water conditions and mineral N and N₂O fluxes were measured during 22 days. We found that dicyandiamide decreased microbial populations and activity, but did not alter composition. Pre-conditioning of the soil with dicyandiamide was 80% more effective in reducing fluxes of N₂O than simultaneous application with fertiliser.     

Some observations on heavy metal concentrations in soils of the Mendip region of north Somerset

Topsoiis in the Mendip Hills of north Somerset are strongly enriched in Pb, Zn and Cd. While much of this enrichment is the result of pollution stemming from previous base metal mining, analyses of soil profile samples reveals that, in several cases, there is considerable enrichment of heavy metals with depth. This, together with relatively high levels of base metals in samples of the limestone and sandstone bedrocks, suggests that some of the enrichment in soil of heavy metals is due to natural processes.     

土壤磷素微生物作用的研究进展

土壤中许多微生物(包括菌根真菌)能够通过产生质子和有机酸溶解土壤不溶态无机磷，通过分泌磷酸酶水解有机磷，但微生物的这种作用受土壤供磷与植物对磷需求间平衡的控制。土壤微生物量中的磷是土壤有机磷最为活跃的部分，由于其周转快、极易矿化为植物有效磷而成为土壤有效磷的活性库。目前，测定土壤微生物量中的磷的方法并不统一，而熏蒸提取法的应用最为广泛。文章阐述了土壤微生物在提高土壤磷素有效性磷中所起的作用，介绍了土壤微生物量中的磷周转及其对土壤磷素有效性调节的重要性，并总结分析了熏蒸提取法测定土壤微生物量中的磷的实用性和局限性。     

Spatial variability in soil water and salinity in Tamarix community in a semiarid saline region of the upper Yellow River北大核心CSCD

Tamarix is widely distributed in semiarid saline regions of the upper Yellow River. The community of Tamarix affects the spatial distribution of soil water and salinity. It is important to explore the dynamic response relationship of Tamarix community and spatial distribution of soil water and salinity in order to evaluate the effects of vegetation community construction and ecological restoration in this region. The natural Tamarix community in the secondary saline-alkali land of the Ningxia Yellow River Irrigation Area was investigated in July 2016. Classical statistics and geostatistics were used to analyze the spatial distribution characteristics of soil water and salinity. The results showed that the soil water content was relatively low (1.98%-7.55%), whereas the soil salinity was high (average conductivity 10.28-25.38 mS/cm) in the study area. The variability coefficient range of soil water and salinity was 36.1%-83.7%, both with moderate variations. Furthermore, the variation degree of soil salinity decreased with the increase in soil depth. The soil water and salinity had obvious spatial structure characteristics, which was mainly affected by structural factors or structural factors associated with stochastic factors. The coefficients of nugget were 0.04%-49.88%, indicating the strong spatial correlation. The spatial distribution of soil water and salinity in Tamarix community showed a patchy pattern; the soil water and salinity distribution in the areas with high Tamarix growing density were considerably high. The correlation analysis showed that there was a positive correlation between soil water and salinity in the study area. In conclusion, soil water and salinity restrict the distribution and growth of Tamarix. Furthermore, the distribution and growth of Tamarix enhanced the spatial variability of soil water and salinity. Keywords. © 2018 Science Press. All rights reserved.