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联苯在各种稻田土壤和河流沉积物中的厌氧生物降解。

Anaerobic biodegradation of biphenyl in various paddy soils and river sediment.

作者信息

Yang Suyin, Yoshida Naoko, Baba Daisuke, Katayama Arata

机构信息

Graduate School of Engineering, Nagoya University, Furo-cho, Chikusa, Nagoya 464-8603, Japan.

出版信息

Chemosphere. 2008 Mar;71(2):328-36. doi: 10.1016/j.chemosphere.2007.09.002. Epub 2007 Oct 24.

DOI:10.1016/j.chemosphere.2007.09.002
PMID:17950776
Abstract

The anaerobic degradation of biphenyl was investigated in four uncontaminated Japanese paddy soils and one river sediment sample contaminated with benzene and chlorinated aliphatics. Two of the paddy soils and the sediment were capable of degrading biphenyl anaerobically without any additional medium or electron acceptors. The half-lives of biphenyl biodegradation in the three samples were 212 d in the Kuridashi soil, 327 d in the Kamajima soil, and 429 d in the river sediment. The Kuridashi soil metabolized 1+/-0.3% of [U-14C]-biphenyl into CO2 and 5+/-2% into water-soluble metabolites after 45 d of incubation. Submerged conditions, which result in lower nitrate and iron oxide contents, and neutral pH, appeared to be the common properties among the samples that influenced their degradation capacities. The addition of 10mM sulfate and 20mM Fe(III) as electron acceptors did not enhance the biphenyl degradation rate, whereas 10mM nitrate completely inhibited biphenyl degradation. The addition of different electron donors (lactate, acetate, or pyruvate) slightly slowed the degradation. Molybdate (an inhibitor of sulfate-reducing bacteria) had an inhibitory effect on biphenyl biodegradation, but bromoethanesulfonic acid (an inhibitor of methanogens) did not. Most biphenyl degradation was observed when only water was added, with no other electron acceptors or donors. These results suggest that sulfate-reducing bacteria and fermentative microbial populations play important roles in anaerobic biphenyl biodegradation in paddy soil.

摘要

在四种未受污染的日本稻田土壤和一个被苯及氯代脂肪烃污染的河流沉积物样本中,研究了联苯的厌氧降解情况。其中两种稻田土壤和沉积物能够在不添加任何额外培养基或电子受体的情况下厌氧降解联苯。在这三个样本中,联苯生物降解的半衰期分别为:栗田土壤中为212天,釜岛土壤中为327天,河流沉积物中为429天。在孵化45天后,栗田土壤将1±0.3%的[U-14C] - 联苯代谢为二氧化碳,5±2%代谢为水溶性代谢产物。淹水条件导致较低的硝酸盐和氧化铁含量以及中性pH值,这些似乎是影响样本降解能力的共同特性。添加10mM硫酸盐和20mM Fe(III)作为电子受体并没有提高联苯的降解速率,而10mM硝酸盐则完全抑制了联苯的降解。添加不同的电子供体(乳酸盐、乙酸盐或丙酮酸盐)会略微减缓降解。钼酸盐(硫酸盐还原菌的抑制剂)对联苯生物降解有抑制作用,但溴乙烷磺酸(产甲烷菌的抑制剂)则没有。当只添加水而不添加其他电子受体或供体时,观察到了大部分的联苯降解。这些结果表明,硫酸盐还原菌和发酵性微生物群体在稻田土壤厌氧联苯生物降解中起重要作用。

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