AEM Accepts, published online ahead of print on 5 September 2014 Appl. Environ. Microbiol. doi:10.1128/AEM.02146-14 Copyright © 2014, American Society for Microbiology. All Rights Reserved.

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Stratified Microbial Structure and Activity in Sulfide- and

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Methane- Producing Anaerobic Sewer Biofilms

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Jing Sun1, Shihu Hu1, Keshab Raj Sharma1,2, Bing-Jie Ni1, Zhiguo Yuan1,2*

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Queensland, Australia;

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Advanced Water Management Center, The University of Queensland, St. Lucia, 4072,

CRC for Water Sensitive Cities, PO Box 8000, Clayton, Victoria, 3800, Australia

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*Corresponding author

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Email: [email protected]

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Phone: +61 (0)7 3365 4374

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Fax: +61 (0)7 3365 4726

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ABSTRACT

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Simultaneous production of sulfide and methane by anaerobic sewer biofilms has

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recently been observed, suggesting that sulfate-reducing bacteria (SRB) and

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methanogenic archaea (MA), microorganisms known to compete for the same substrates,

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can coexist in this environment. This study investigated the community structures and

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activities of SRB and MA in anaerobic sewer biofilms (average thickness of 800 μm)

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using a combination of microelectrode measurements, molecular techniques and

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mathematical modelling. It was seen that sulfide was mainly produced in the outer layer

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of the biofilm, between 0 - 300 μm, which is in good agreement with the distribution of

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SRB population as revealed by cryosection - fluorescence in situ hybridization (FISH). 1

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SRB have a higher relative abundance of 20% on the surface layer, which decreased

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gradually to below 3% at a depth of 400 μm. In contrast, MA mainly inhabited the inner

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layer of the biofilm. Their relative abundances increased from 10% to 75% at depths of

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200 μm and 700 μm, respectively, from the biofilm surface layer. High throughput

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pyrosequencing of 16S rRNA amplicons showed that SRB in the biofilm were mainly

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affiliated

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Desulfatiferula and Desulforegula, while about 90% of the MA population belonged to

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the genus Methanosaeta. The spatial organization of SRB and MA revealed by

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pryosequencing were consistent with the FISH results. A biofilm model was constructed

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to simulate the SRB and MA distributions in the anaerobic sewer biofilm. The good fit

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between model predictions and the experimental data indicates that the coexistence and

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spatial structure of SRB and MA in the biofilm resulted from the microbial types, their

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metabolic transformations and interactions with substrates.

with

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genera:

Desulfobulbus,

Desulfomicrobium,

Desulfovibrio,

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INTRODUCTION

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Sewer biofilms comprise complex multi-species microflora with a typical thickness of

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only about one millimeter (1). According to the electron donors and electron acceptors

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present in the wastewater, different carbon transformation processes can occur in close

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proximity in the sewer biofilms. Domestic wastewater normally contains a significant

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concentration of sulfate (ca. 100–1000 μM) but negligible nitrite and nitrate (2, 3).

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Therefore, under anaerobic conditions (normally occurs in pressure sewers fully filled

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with wastewater), sulfate reduction carried out by the sulfate-reducing bacteria (SRB)

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could be an important terminal electron accepting process in the sewer biofilms. The

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sulfate reduction activity in anaerobic sewers is important as the production of sulfide

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produced can be transferred to the gas phase of partially-filled gravity sewers and cause 2

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extensive corrosion of concrete sewer pipes (4, 5). Also, the emission of sulfide from

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sewers can cause odor problems to the surrounding area and pose health risks to sewer

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workers (6, 7). Apart from sulfate reduction, methanogenesis by the respiration of

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methanogenic archaea (MA) could also be a key terminal process in anaerobic sewer

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biofilms (8, 9). Guisasola and colleagues found that methanogenesis accounted for more

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than 70% of the chemical oxygen demand (COD) loss in laboratory anaerobic sewer

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biofilm reactors (9). A recent report suggests that methane emissions from sewers

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contribute significantly to the total greenhouse gas footprint of wastewater systems (10).

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Under anaerobic conditions, both sulfate reduction and methanogenesis can

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potentially occur in the same system while competing for the same electron donors,

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primarily hydrogen and acetate. In the presence of adequate sulfate concentrations, SRB

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will typically outcompete MA due to kinetic and thermodynamic advantages (11-13).

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However, the coexistence of SRB and MA has been observed in anaerobic sewer

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biofilms in the presence of sulfate. Guisasola et al. (9) hypothesized the coexistence of

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SRB and MA in sewer biofilms was due to the penetration limitation of sulfate into the

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biofilms, resulting in a stratified biofilm structure, with SRB being predominant in the

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outer zone, nearer to the wastewater, while MA inhabit the inner zone, nearer the sewer

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pipe. However, to date this hypothesis has not been verified. A few studies have

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investigated the veritical distribution of SRB in oxic-anoxic sewer biofilms (biofilms

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attached on gravity sewer pipe with the presence of oxygen or nitrate in wastewater), but

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studies on the SRB distribution in the anerobic sewer bioflims is scarce (14). In addition,

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the distubtion of MA in sewer biofilms and their interaction with SRB have not been

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explored yet. Similarly, the phylogenitic diversity of SRB and MA in the anaerobic

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sewer biofilms is rarelly reported. These fundamental information could provide a better

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understanding of the sulfate reduction and methanogenesis processes in sewer systems,

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which would be useful for sewer management. Therefore, the aims of this study are to

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investigate the community structures of both SRB and MA and to determine their spatial

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arrangement in anaerobic sewer biofilms.

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Both experimental investigations and modeling analyses were conducted to achieve

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the aims of this study. The experiments were carried out in an annular biofilm reactor

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mimicking anaerobic sewer conditions, which was fed with real domestic wastewater.

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Firstly, microelectrodes were applied to determine the spatial distribution of in situ

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sulfide production activity within the biofilms. Although it would have been ideal to

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determine the distribution of methane production activity using the same method, this

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was difficult to perform due to the lack of suitable microelectrodes (15). Secondly, the

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spatial distributions of the SRB and MA in the biofilms and their abundance at different

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depths were determined by fluorescence in situ hybridization (FISH) after

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cryosectioning the biofilm samples. This method has been used frequently to determine

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the spatial distributions of microbial communities in biofilms or granules. However,

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phylogenetic information is hardly revealed due to the limitation of oligonucleotide

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probes used in FISH (16). Therefore, 16S rRNA gene amplicon pyrosequencing was

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applied to further investigate the phylogenetic diversity. In previous studies of sewer

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biofilms, the phylogenetic analysis is performed on the entire biofilm, and information

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on the different genera at different biofilm depths is rarely reported (2, 14). In this study,

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we determined the phylogenetic diversity in different layers of the sewer biofilms by

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innovatively using pyrosequencing combined with cryosectioning. To our knowledge, to

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date, this method has not been applied in any other studies related to biofilms and

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granules. Finally, a mathematical model focusing on the interaction between SRB and

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MA in the sewer biofilm was developed to evaluate and interpret the experimental

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results.

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MATERIALS AND METHODS

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Reactor configuration, operation and monitoring. An annular biofilm reactor made

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of acrylonitrile butadiene styrene (ABS), one of the typical materials used for sewer

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pipes, was set up to mimic an anaerobic sewer pipe section (Fig. 1). The reactor

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consisted of an inner cylinder (of height 295 mm, and diameter of 130 mm) enclosed in

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an outer cylinder (of height 345 mm and inner diameter of 160 mm). Wastewater was

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filled in the gap between the two cylinders, with a volume of 3 L. Biofilms were grown

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on the walls of both cylinders in contact with the wastewater, resulting in a biofilm area

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to reactor volume (A/V) ratio of 119 m-1. Mixing was established by the rotation of the

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inner cylinder driven by a motor at a speed of 200 rpm. The mixing is expected to create

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a uniform shear stress on the reactor walls so that biofilms grow relatively evenly on the

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wall. The average shear stress provided by the mixing was 2.11 N/m2, which is typical in

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sewer systems (17). Eight removable ABS slides of width and length at 5 mm by 200

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mm were mounted in recessed slots on the inside of the outer cylinder. The slides were

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removable via ports on the top of the reactor for biofilm sampling. The reservoir on the

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top of the reactor was used to ensure the reactor was full of wastewater during sampling.

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The reactor was operated in a temperature-controlled room (20 ± 2 °C).Domestic

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sewage, collected on a weekly basis from a local wet well (Brisbane, Queensland), was

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used as the feed for the reactor. The sewage compositions varied to a certain extent in

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terms of sulfate, Volatile fatty acid (VFA), and COD concentrations. The sewage

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typically contained sulfate at concentrations of 10-25 mgS/L, sulfide at < 3 mgS/L,

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Soluble COD (sCOD) at 200-300 mg/L, 50-120 mgCOD/L of VFAs and approximately

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50 mgN/L of ammonium. Negligible amounts of sulfite, thiosulfate (

Stratified microbial structure and activity in sulfide- and methane-producing anaerobic sewer biofilms.

Simultaneous production of sulfide and methane by anaerobic sewer biofilms has recently been observed, suggesting that sulfate-reducing bacteria (SRB)...
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