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1.
Bunge Michael Khknen Mika A. Rmisch Winfried Opel Matthias Vogler Susanne Walkow Fred Salkinoja-Salonen Mirja Lechner Ute 《Environmental science and pollution research international》2007,14(1):3-10
Background, Aims and Scope Sediments of the Spittelwasser creek are highly polluted with organic compounds and heavy metals due to the discharge of untreated
waste waters from the industrial region of Bitterfeld-Wolfen, Germany over the course of more than one century. However, relatively
few data have been published about the chloroorganic contamination of the sediment. This paper reports on the content of different
(chloro)organic compounds with special emphasis on polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/F), and chlorobenzenes. Existing concepts for the remediation of Spittelwasser sediment include
the investigation of natural attenuation processes, which largely depend on the presence of an intact microbial food web.
In order to gain more insight in terms of biological activity, we analyzed the capacity of sediment microflora to degrade
organic matter by measuring the activities of extracellular hydrolytic enzymes involved in the biogeochemical cycling of carbon,
nitrogen, phosphorus and sulfur. Furthermore, the detection of physiologically active bacteria in the sediment, particularly
of those known for their capability to reductively dehalogenate organochlorine compounds, illustrates the potential for intrinsic
bioremediation processes.
Methods PCDD/F and chlorobenzenes were analyzed by gas chromatography(GC)/mass spectrometry and GC/flame ionization detection, respectively.
The activities of hydrolytic enzymes were determined from freshly sampled sediment layers using 4-methylumbelliferyl (MUF)
or 7-amino-4-methylcoumarin-conjugated model compounds and kinetic fluorescence measurements. Physiologically active bacteria
from different sediment layers were microscopically visualized by fluorescence in situ hybridization (FISH). Specific bacteria were identified by 16S rRNA gene amplification and sequencing.
Results and Discussion The PCDD/F congener profile was dominated by dibenzofurans. In addition, the presence of specific tetra and pentachlorinated
dibenzofurans supported the assumption that extensive magnesium production was one possible source for the high contamination.
A range of other chloroorganic compounds, including several isomers of chlorobenzenes, hexachlorocyclohexane and 1,1,1-trichloro-2,2-bis
(p-chloro-phenyl)ethane (DDT), was present in the sediment. Activities of extracellular hydrolytic enzymes showed a strong
decrease in those sediment layers that were characterized by high contents of absorbable organic halogen (AOX), indicating
disturbed organic matter decay. Interestingly, an abnormal increase of cellulolytic enzyme activities below the organochlorine-rich
layers was observed, possibly caused by residual cellulose from discharges of sulfite pulping wastes. FISH revealed physiologically
active bacteria in most sediment layers from the surface down to the depth of about 60 cm, including members of Desulfitobacterium (D.) and Sulfurospirillum. The presence of D. dehalogenans was confirmed by its partial 16S rRNA gene sequence.
Conclusions Results of chemical sediment analyses demonstrated high loads of organochlorine compounds, particularly of PCDD/F. Several
years after stopping the waste water discharge to Spittelwasser creek, this sediment remains a main source for pollution of
the downstream river system by way of the ongoing mobilization of sediment during high floods. As indicated by our enzyme
activity measurements, the decomposition potential for organic matter is low in organochlorine-rich sediment layers. In contrast,
the comparably higher enzyme activities in less organochlorine-polluted sediment layers as well as the presence of physiologically
active bacteria suggest a considerable potential for natural attenuation.
Recommendations and Perspectives From our data we strongly recommend to explore the degradative capacity of sediment microorganisms and the limits for in situ activity towards specific sediment pollutants in more detail. This will give a sound basis for the integration of bioremediation
approaches into general concepts to reduce the risk that permanently radiates from this highly contaminated sediment.
Submission Editor: Dr. Henner Hollert (Henner.Hollert@urz.uniheidelberg.de) 相似文献
2.
本文利用统计分析和吸收系数描述了昆明西山土壤-植物系统中Fe,Mn,Ni分布特征。结果表明,受试植物在土壤-植物系统中对Ni元素均表现出相对的稀释和绥冲作用;对Mn元素,除了菊科夏田菊,山紫金子和牛旁外,均表现出相对富集作用。 相似文献
3.
本文研究了水深的变化以波高与周期联合概率密度分布造成影响。本文将236组实测数据按水深因子H的大小进行了分组,分别对其进行了谱分析和统计分析,得到了各组数据的联合分布图。利用数值模拟的方法扩大水深因子的变化幅度,得到了模拟联合分布图。研究发现,水深因子的改变不会对联合分布构成大的影响,因此得现一般水的波高与周期联合概率密度分布模式适用于浅海的结论。 相似文献
4.
5.
简要介绍了北京地热资源特点,分析了北京地热资源开发的时空演变规律.在搜集资料和实地调查的基础上,绘制出了北京城区地热井分布示意图,并针对其开发利用中可能出现的问题提出了对策. 相似文献
6.
7.
河南省旱涝灾害的地域分异规律和减灾对策研究 总被引:6,自引:0,他引:6
河南省地处我国南北气候过渡地带,自古以来就以旱涝灾害频繁而著称。根据旱涝灾害的地域分异特点,可将全省分为五个区。减轻旱涝灾害的主要措施是:加强水利建设,进一步开发地下水;扩大引黄灌溉、抗旱、补源面积;走旱作农业的道路,广泛提高农田抗灾水平。 相似文献
8.
氯氰菊酯降解菌的筛选鉴定及其降解特性研究 总被引:2,自引:0,他引:2
从农药厂废水排放口附近的污泥中分离到1株能降解氯氰菊酯的细菌LQ-3.根据其形态、生理生化特征和16S rDNA(GenBank Accession No.FJ222585)序列分析,将该菌株鉴定为Starkeya sp..LQ-3菌株只能以共代谢方式降解氯氰菊酯,在有酵母粉、蛋白胨、葡萄糖等营养物质存在的条件下,5 d内对20 mg·L-1氯氰菊酯的降解率达到72.1%.LQ-3菌株降解氯氰菊酯的最适温度为30 ℃左右,pH值为7~8.LQ-3菌株还能降解功夫菊酯、甲氰菊酯、联苯菊酯和溴氰菊酯.酶的定域试验表明,LQ-3菌株降解氯氰菊酯的酶属于胞外酶. 相似文献
9.
10.
分维数和稳定性指数是土壤空间分布的重要指数。通过建立安徽省土壤的空间数据库,运用分形理论,获得安徽省土壤类型周长与面积的关系,进而计算出各类土属在空间上的分维数和稳定性指数大小,得出如下结论:①安徽省土壤图斑的周长与面积之间存在双对数函数关系,相关性系数大部分在0.9以上,证明了安徽省土壤空间分形的客观存在。②安徽省各类土壤空间分维数大小在1.1375—1.9948之间,平均值为1.6138,最大的是泥质岩砾质土,最小的是脱青湖泥田。分维数在空间分布上存在差异,总的趋势是从西北向东南逐渐变大。③各种土属的稳定性指数在1.0252—0.0124之间,平均值约为0.2324,最大的是湿潮土,最小的是砂礓黄土。 相似文献