Appl Environ Microbiol. 1995 Jan;61(1):27-33. doi: 10.1128/aem.61.1.27-33.1995.
One of the main factors impeding the bioremediation of polluted soils, sediments, and aquifers is the low bioavailability of chemicals which are sorbed by organic matter. To obtain more insight into the factors that control the degradation of sorbed compounds, we used a defined model system in which 3-chlorodibenzofuran (3CDF) was the organic contaminant, porous Teflon granules were the sorbent, and Sphingomonas sp. strain HH19k was the test organism. The sorption of 3CDF to Teflon reached equilibrium within 150 min. The curved shape of the sorption isotherm, the extent of sorption, and the desorption kinetics suggested that there was a surface interaction (adsorption) between 3CDF and Teflon which took place mainly inside the pores of the granules. The kinetics of desorption could be ascribed to sorption-retarded radial diffusion inside the granules since the desorption rate not only was correlated with the sorbed-phase concentration, but also depended on the equilibration status of sorption, since (i) the high initial desorption rate sharply declined because of the depletion of 3CDF in the outermost parts of the granules, but high rates were observed again after the system had been given time to reequilibrate, and (ii) the initial desorption rate was higher when the preceding contact time between sorbate and sorbent was shorter (i.e., most 3CDF was still located in the exterior parts of the granules). These characteristics were observed irrespective of whether the desorption was driven by percolating water through the sorbent or by attaching active bacteria to the sorbent. 3CDF consumption by attached cells drove 3CDF desorption to a considerable extent. The attached cells were thus efficiently supplied with desorbing 3CDF. On the basis of our results, we propose that the rate at which a sorbed substrate becomes available for organisms is influenced by (i) the specific affinity of the degrading organisms (i.e., their ability to reduce the aqueous substrate concentration) and (ii) the tendency of the organisms to adhere to the sorbent.
一种阻碍受污染土壤、沉积物和含水层生物修复的主要因素是化学物质的生物可利用性低,这些化学物质被有机物吸附。为了更深入地了解控制被吸附化合物降解的因素,我们使用了一个定义明确的模型系统,其中 3-氯二苯并呋喃(3CDF)是有机污染物,多孔聚四氟乙烯颗粒是吸附剂,鞘氨醇单胞菌 HH19k 菌株是测试生物。3CDF 对聚四氟乙烯的吸附在 150 分钟内达到平衡。吸附等温线的弯曲形状、吸附的程度和解吸动力学表明,3CDF 和聚四氟乙烯之间存在表面相互作用(吸附),主要发生在颗粒的孔隙内。解吸动力学可以归因于颗粒内部吸附延迟的径向扩散,因为解吸速率不仅与被吸附相的浓度相关,还取决于吸附的平衡状态,因为(i)高初始解吸速率由于颗粒最外层 3CDF 的耗尽而急剧下降,但在系统有时间重新平衡后又观察到高速率,以及(ii)当吸附质和吸附剂之间的先前接触时间较短时(即,大部分 3CDF 仍位于颗粒的外部部分),初始解吸速率更高。这些特征无论解吸是由渗透水通过吸附剂驱动还是通过将活性细菌附着在吸附剂上驱动都观察到。附着细胞消耗 3CDF 驱动 3CDF 解吸到相当大的程度。附着的细胞因此有效地供应了可解吸的 3CDF。根据我们的结果,我们提出,被吸附基质对生物体的可用性的速率受到以下因素的影响:(i)降解生物的特定亲和力(即,它们降低水溶液中基质浓度的能力)和(ii)生物附着在吸附剂上的倾向。