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BIODEGRADATION AND MINERALIZATION OF ISOTOPICALLY LABELED TNT AND RDX IN ANAEROBIC MARINE SEDIMENTS

机译:厌氧海洋沉积物中同位素标记的TNT和RDX的生物分解和成矿作用

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The lack of knowledge on the fate of explosive compounds 2,4,6-trinitrotoluene (TNT) and hexahydro-1,3,5-trinitro-1,3,5triazine (RDX), particularly in marine ecosystems, constrains the application of bioremediation techniques in explosive-contaminated coastal sites. The authors present a comparative study on anaerobic biodegradation and mineralization of N-15-nitro group isotopically labeled TNT and RDX in organic carbon-rich, fine-grained marine sediment with native microbial assemblages. Separate sediment slurry experiments were carried out for TNT and RDX at 23 degrees C for 16 d. Dissolved and sediment-sorbed fractions of parent and transformation products, isotopic compositions of sediment, and mineralization products of the dissolved inorganic N pool ((NH4+)-N-15, (NO3-)-N-15, (NO2-)-N-15, and N-15(2)) were measured. The rate of TNT removal from the aqueous phase was faster (0.75 h(-1)) than that of RDX (0.37 h(-1)), and N-15 accumulation in sediment was higher in the TNT (13%) than the RDX (2%) microcosms. Mono-aminodinitrotoluenes were identified as intermediate biodegradation products of TNT. Two percent of the total spiked TNT-N is mineralized to dissolved inorganic N through 2 different pathways: denitration as well as deamination and formation of NH4+, facilitated by iron and sulfate reducing bacteria in the sediments. The majority of the spiked TNT-N (85%) is in unidentified pools by day 16. Hexahydro-1,3,5trinitro- 1,3,5-triazine (10%) biodegrades to nitroso derivatives, whereas 13% of RDX-N in nitro groups is mineralized to dissolved inorganic N anaerobically by the end of the experiment. The primary identified mineralization end product of RDX (40%) is NH4+, generated through either deamination or mono-denitration, followed by ring breakdown. A reasonable production of N-2 gas (13%) was seen in the RDX system but not in the TNT system. Sixty-eight percent of the total spiked RDX-N is in an unidentified pool by day 16 and may include unquantified mineralization products dissolved in water. (C) 2016 SETAC
机译:缺乏对爆炸性化合物2,4,6-三硝基甲苯(TNT)和六氢-1,3,5-三硝基-1,3,5三嗪(RDX)的命运的了解,特别是在海洋生态系统中,限制了生物修复的应用爆炸物污染的沿海地区的技术。作者提出了在富含有机碳的细粒海洋沉积物和天然微生物组合物中,N-15硝基同位素标记的TNT和RDX进行厌氧生物降解和矿化的比较研究。在23摄氏度下对TNT和RDX分别进行了16 d的沉积物泥浆实验。母体和转化产物的溶解级分和沉积物级分,沉积物的同位素组成以及溶解的无机氮池((NH4 +)-N-15,(NO3-)-N-15,(NO2-)-N -15和N-15(2))。 TNT从水相中的去除速度(0.75 h(-1))比RDX(0.37 h(-1))更快,而TNT中沉积物中N-15的沉积率(13%)比RDX高。 RDX(2%)缩影。单氨基二硝基甲苯被鉴定为TNT的中间生物降解产物。 TNT-N加标总量的百分之二通过两种不同的途径矿化成溶解的无机N:脱氮,脱氨和NH4 +的形成,这是由沉积物中的铁和硫酸盐还原细菌促进的。到第16天,大多数加标的TNT-N(85%)都在未知池中。六水-1,3,5三硝基-1,3,5-三嗪(10%)生物降解为亚硝基衍生物,而RDX-N的13%在实验结束时,硝基中的N会厌氧矿化成溶解的无机N。 RDX(40%)的主要矿化终产物是NH4 +,它是通过脱氨或单硝化再环分解而产生的。在RDX系统中发现了合理的N-2气体产量(13%),而在TNT系统中却没有。到第16天,RDX-N加标总量中的68%位于一个不确定的池中,并且可能包括溶解在水中的未量化矿化产品。 (C)2016年SETAC

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