Nam K, Kim J Y, Oh D I
School of Civil, Urban & Geosystem Engineering, Seoul National University, Seoul, The Republic of Korea.
Environ Pollut. 2003;121(1):147-51. doi: 10.1016/s0269-7491(02)00181-1.
A study was conducted to determine the possible role of soil aggregates in the sequestration of phenanthrene and thus in the declined biodegradation of the hydrocarbon. Phenanthrene aged in Lima loam (2-mm aggregates) showed declined biodegradation with time of aging to the test bacterium P5-2 capable of using sorbed phenanthrene. In contrast, the compound aged in a soil reconstructed with 68% clay-silt and 32% sand that had been separated from the Lima loam was readily mineralized. The percentages of each fraction used were the same as those of the original soil. Biodegradation of aged phenanthrene was not affected significantly by varying the ratios of each fraction in reconstructed mixtures. In experiments with Lima loam, its clay-silt fraction, and its sand fraction, mineralization extent was much lower in soil aggregates compared with the other samples while all had similar organic carbon content of ca. 1.51%. This suggests that aggregation may be another important determinant in the reduced biodegradation of aged phenanthrene.
开展了一项研究,以确定土壤团聚体在菲的固存中以及因此在碳氢化合物生物降解能力下降方面可能发挥的作用。在利马壤土(2毫米团聚体)中老化的菲,随着老化时间的延长,对能够利用吸附态菲的测试细菌P5-2的生物降解能力下降。相比之下,在由从利马壤土中分离出的68%黏粒-粉粒和32%砂重建的土壤中老化的该化合物很容易被矿化。各组分的使用比例与原始土壤相同。通过改变重建混合物中各组分的比例,老化菲的生物降解没有受到显著影响。在用利马壤土、其黏粒-粉粒组分和砂组分进行的实验中,与其他样品相比,土壤团聚体中的矿化程度要低得多,而所有样品的有机碳含量都相似,约为1.51%。这表明团聚作用可能是老化菲生物降解减少的另一个重要决定因素。