Schramm A, Santegoeds C M, Nielsen H K, Ploug H, Wagner M, Pribyl M, Wanner J, Amann R, de Beer D
Max Planck Institute for Marine Microbiology, D-28359 Bremen, Germany.
Appl Environ Microbiol. 1999 Sep;65(9):4189-96. doi: 10.1128/AEM.65.9.4189-4196.1999.
A combination of different methods was applied to investigate the occurrence of anaerobic processes in aerated activated sludge. Microsensor measurements (O(2), NO(2)(-), NO(3)(-), and H(2)S) were performed on single sludge flocs to detect anoxic niches, nitrate reduction, or sulfate reduction on a microscale. Incubations of activated sludge with (15)NO(3)(-) and (35)SO(4)(2-) were used to determine denitrification and sulfate reduction rates on a batch scale. In four of six investigated sludges, no anoxic zones developed during aeration, and consequently denitrification rates were very low. However, in two sludges anoxia in flocs coincided with significant denitrification rates. Sulfate reduction could not be detected in any sludge in either the microsensor or the batch investigation, not even under short-term anoxic conditions. In contrast, the presence of sulfate-reducing bacteria was shown by fluorescence in situ hybridization with 16S rRNA-targeted oligonucleotide probes and by PCR-based detection of genes coding for the dissimilatory sulfite reductase. A possible explanation for the absence of anoxia even in most of the larger flocs might be that oxygen transport is not only diffusional but enhanced by advection, i.e., facilitated by flow through pores and channels. This possibility is suggested by the irregularity of some oxygen profiles and by confocal laser scanning microscopy of the three-dimensional floc structures, which showed that flocs from the two sludges in which anoxic zones were found were apparently denser than flocs from the other sludges.
采用多种方法相结合来研究曝气活性污泥中厌氧过程的发生情况。对单个污泥絮体进行微传感器测量(O₂、NO₂⁻、NO₃⁻和H₂S),以在微观尺度上检测缺氧微环境、硝酸盐还原或硫酸盐还原情况。用¹⁵NO₃⁻和³⁵SO₄²⁻对活性污泥进行培养,以批量规模测定反硝化和硫酸盐还原速率。在所研究的六个污泥中,有四个在曝气过程中未形成缺氧区,因此反硝化速率非常低。然而,在两个污泥中,絮体中的缺氧情况与显著的反硝化速率同时出现。在微传感器或批量研究中,在任何污泥中均未检测到硫酸盐还原,即使在短期缺氧条件下也是如此。相比之下,通过与16S rRNA靶向寡核苷酸探针进行荧光原位杂交以及基于PCR检测异化亚硫酸盐还原酶编码基因,表明存在硫酸盐还原菌。即使在大多数较大的絮体中也没有缺氧现象的一个可能解释是,氧气传输不仅是扩散性的,而且通过平流得到增强,即通过孔隙和通道中的流动得以促进。一些氧分布的不规则性以及三维絮体结构的共聚焦激光扫描显微镜观察结果表明了这种可能性,这些观察结果显示,发现有缺氧区的两个污泥中的絮体明显比其他污泥中的絮体更致密。