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Nitrogen removal and NO accumulation during hydrogenotrophic denitrification: influence of environmental factors and microbial community characteristics Peng Li, Yajiao Wang, Jiane Zuo, Rui Wang, Jian Zhao, and Youjie Du Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b00071 • Publication Date (Web): 02 Aug 2016 Downloaded from http://pubs.acs.org on August 2, 2016
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Environmental Science & Technology
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Nitrogen removal and N2O accumulation during hydrogenotrophic
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denitrification: influence of environmental factors and microbial
3
community characteristics
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Peng Li1, Yajiao Wang1, Jiane Zuo*, Rui Wang, Jian Zhao, Youjie Du
5
State Key Joint Laboratory of Environmental Simulation and Pollution Control,
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School of Environment, Tsinghua University, Beijing 100084, China
7
*
8
(86)-10-62772455
9
1
Corresponding author, Email address:
[email protected], Phone number:
These authors contributed equally to this work.
10
Abstract
11
Hydrogenotrophic denitrification is regarded as an efficient alternative technology of
12
removing nitrogen from nitrate-polluted water that has insufficient organics material.
13
However, the biochemical process underlying this method has not been completely
14
characterized, particularly with regard to the generation and reduction of nitrous oxide
15
(N2O). In this study, the effects of key environmental factors on hydrogenotrophic
16
denitrification and N2O accumulation were investigated in a series of batch tests. The
17
results show that nitrogen removal was efficient with a specific denitrification rate of
18
0.66 kg N/(kg MLSSd), and almost no N2O accumulation was observed when the
19
dissolved hydrogen (DH) concentration was approximately 0.40 mg/L, the
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temperature was 30 °C and the pH was 7.0. The reduction of nitrate was significantly
21
affected by the pH, temperature, inorganic carbon (IC) content and DH concentration.
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A considerable accumulation of N2O was only observed when the pH decreased to 6.0
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and the temperature decreased to 15 °C, where little N2O accumulated under various
24
IC and DH concentrations. To determine the microbial community structure, the
25
hydrogenotrophic denitrifying enrichment culture was analyzed by Illumina
26
high-throughput sequencing, and the dominant species were found to belong to the
27
genera Paracoccus (26.1%), Azoarcus (24.8%), Acetoanaerobium (11.4%), Labrenzia
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(7.4%), and Dysgonomonas (6.0%).
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Key words: hydrogenotrophic denitrification; nitrous oxide accumulation; microbial
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community; high-throughput sequencing; kinetics
31 32 33
TOC art 1. Introduction
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Nitrate is one of the most critical pollutants in water and wastewater, and nitrate
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pollution of drinking water might increase the risk of non-Hodgkin's lymphoma and
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bladder and ovarian cancers in humans.1 Nitrate loading to surface water is commonly
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considered an important contributor to water quality deterioration and eutrophication.2
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Biological denitrification technologies have been widely applied for nitrogen removal
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because they provide efficient performance and low cost.3,4,5,6 Hydrogenotrophic
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denitrification is an innovative, effective and clean technology that has attracted
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considerable attention recently, and its main advantage over heterotrophic
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denitrification is that an additional dosage of
43
required.7,8
44
denitrification for the treatment of nitrate-polluted water with insufficient bioavailable
45
organics, such as groundwater, drinking water and secondary effluent of
46
wastewater.9,10
This
property
an organic carbon source is not
increases the effectiveness
of
hydrogenotrophic
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A variety of high-efficiency bioreactors of hydrogenotrophic denitrification have
48
been developed, such as fixed- and fluidized-bed reactors9,11, membrane biofilm
49
reactors and biofilm electrode reactors12,13. Because of the low solubility of hydrogen
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and the risk of explosion with escaped hydrogen gas, improving the efficiency and
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security of hydrogen delivery remains a major challenge. Therefore, many innovative
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hydrogen delivery systems have been developed along with membrane biofilm
53
reactors using gas-permeable membranes including hollow-fiber or silicon tubes.10
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In addition to the advancements in reactor configuration, a better understanding
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of the inherent biochemical process underlying hydrogenotrophic denitrification may
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also help promote the technology. Several kinetic models have been proposed to
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reveal the regularity of the process of hydrogenotrophic denitrification.14,15,16 In these
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studies, hydrogenotrophic denitrification was regarded as a two-step consecutive
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reduction of nitrate to nitrite and then to nitrogen gas. However, the complete process
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of hydrogenotrophic denitrification is actually a four-step process in which hydrogen
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supplies electrons for a stepwise reduction of nitrate to nitrite, nitric oxide (NO),
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nitrous oxide (N2O) and nitrogen gas through a series of reductases. When the
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production rate is higher than the consumption rate, N2O accumulates in the liquid
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phase, which causes the emission of N2O into the atmosphere. N2O is known as a
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main greenhouse gas, and biological denitrification during wastewater treatment is
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considered as one of the anthropogenic sources of N2O emission.
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evaluation of the characteristics of N2O accumulation, which depends on the
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microbial community and electron donor and environmental factors, is significant to
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mitigating N2O emissions from wastewater treatment. Although the characteristics of
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N2O accumulation during heterotrophic denitrification have been comprehensively
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investigated,18,19 related research on hydrogenotrophic denitrification is not available.
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This research deficit reduces our ability to understand the process of
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hydrogenotrophic denitrification.
18
Therefore, an
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To analyze the mechanisms underlying the hydrogenotrophic denitrification
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process, further studies are required, including investigations on N2O emissions, as
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well as on the effects of the environmental factors. Previous studies have indicated
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that the effectiveness of hydrogenotrophic denitrification is impacted by several
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crucial environmental factors, including the pH,14,20,21,22 temperature,10,11,20 inorganic
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carbon to nitrogen ratios (IC/N),13,22 dissolved hydrogen concentration (DH)13 and the
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nitrate concentration11,23Among these factors, pH has attracted the most interest, and
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the effects of pH in the range of 7.0 to 8.5 on nitrate removal have been
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studied.15,20,21,22 Although consensus on the optimal value has not been reached, the
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high dependency of pH on nitrate reduction and nitrite accumulation has been
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illustrated, which implies the significance of pH on N2O reduction and accumulation.
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In most cases, researchers investigating the nitrogen removal efficiency of
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hydrogenotrophic denitrification bioreactors have focused on the effects of the
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operational parameters, such as the hydrogen supply interval and the inorganic carbon
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dosage methods.13,21 Although the potential role of influential factors was indirectly
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suggested by these studies, the inherent effects of these factors on the biochemical
90
process were not revealed. In addition, because the microbial cultures utilized in
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various studies were different and the effects of multi factors were rarely involved in
92
one study, it is difficult to perform comparisons among factors across experiments.
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Therefore, a comprehensive study must be performed to unveil the effects of multi
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environmental factors on the biochemical process of hydrogenotrophic denitrification.
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The objectives of this paper are as follows: 1) to determine the rate of N2O
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reduction and accumulation in hydrogenotrophic denitrification; 2) to systemically
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investigate how the key environmental factors (i.e., pH, temperature, inorganic carbon
98
concentration and DH concentration) affect nitrate reduction, nitrite accumulation and
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N2O emission; and 3) to determine the microbial community of hydrogenotrophic
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denitrifiers by Illumina high-throughput sequencing. This study will help provide a
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better understanding of the hydrogenotrophic denitrification process, and the results
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will have important implications for the implementation and operation of
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hydrogenotrophic denitrification technology.
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2. Methods and Materials
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2.1 Bacteria acclimation and cultivation
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The initial inoculum of the hydrogenotrophic denitrifying culture was the
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activated sludge from the aerobic tank (Xiaojiahe Municipal Wastewater Treatment
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Plant, Beijing, China). After 60 days of constant feeding with H2 and synthetic
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nutrition, the denitrification rate remained constant. Therefore, it was confirmed to
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achieve a steady state for enrichment cultures. The enrichment culture was cultivated
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for 54 months continuously and then served as the stock culture. The acclimation and
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cultivation were conducted in batch mode at pH 7.0±0.5 at 30±1°C, with a cycle time
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of 12 h using three parallel parent reactors with a working volume of 2.0 L. Hydrogen
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gas was produced in situ through water electrolysis (HG-1805, Beijing, China).
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Synthetic water was used as feed, and it contained (per liter) 1.62 g KNO3, 0.5 g
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NaHCO3, 0.55 g NaH2PO4·2H2O, 2.11 g K2HPO4·3H2O and several other necessary
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nutrients, including 7.3 mg CaCl2·2H2O, 5.0 mg FeSO4·7H2O, 2.5 mg MnCl2·4H2O,
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0.5 mg CoCl2·6H2O, 0.5 mg (NH4)6Mo7O24·4H2O, 0.22 mgZnSO4·7H2O and 0.2 mg
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CuSO4·5H2O.
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2.2. Batch experiments
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2.2.1 Reactors
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Each batch test in this study was repeated three times in parallel. The batch
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reactor was sealable and the working volume of the reactor was 600 ml with 450 ml
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of headspace. The hydrogen was transferred from the headspace to the liquid bulk
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through a gas-liquid interface. At the beginning of a test, 140 ml of the synthetic feed
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water was added to each batch reactor, and then 10 ml of the centrifugal stock culture
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taken from the parent reactors was inoculated. The hydrogen gas produced by
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electrolysis was utilized to ensure that the volume percentage of the hydrogen in the
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headspace was 98~100% by alternating headspace evacuation of the reactor vacuum
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with hydrogen gas input.
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KNO3, KNO2 and N2O were used as substrates of denitrification, and NaHCO3
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was used as the inorganic carbon source at the given concentration. The synthetic
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contaminated water (per liter) also contained 0.55 g NaH2PO4·2H2O and 2.11 g
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K2HPO4·3H2O as buffers.26
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The pH was controlled during the tests by adding 0.2 M HCL and 0.2 M NaOH
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solutions to the set point ± 0.2. The temperature of the reaction system was
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maintained at the set point ± 0.5 °C by a temperature adjustable shaking incubator
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with a rotation speed of 130 r/min.
139 140
All of the batch tests conditions are listed in Table S1. 2.2.2 Batch test I: reduction performance of nitrate, nitrite and N2O
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Nitrate, nitrite and N2O were utilized as the sole electron acceptors with an
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adequate electron donor (hydrogen). The initial NO3--N and NO2--N concentrations
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were controlled at approximately 40 mg/L using KNO3 and KNO2. To control the
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initial N2O-N concentration, pure N2O gas (99.99%) was injected into the reactor to
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replace the volume of hydrogen gas to provide the initial nitrogen concentration of 60
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mg/L after normalizing to the liquid volume according to Henry’s Law. Batch test I
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was conducted under a pH of 7.0, a temperature of 30°C, an initial mass ratio of IC/N
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of 1.8 and a volume percentage of hydrogen gas at 100% in the headspace.
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The N2O-N concentration in this study indicates the sum of the N2O-N
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concentration in both the gaseous and liquid phases after normalizing to the liquid
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volume. The N2O-N or NO2--N accumulation during denitrification was estimated by
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the accumulation percentage, which is described as the ratio of the maximal
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accumulation concentration of nitrogen contained in N2O or NO2- to the initial
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nitrogen concentration.
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2.2.3 Batch test II: effects of pH, temperature, inorganic carbon concentration
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and DH concentration on hydrogenotrophic denitrification
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Batch test II was conducted to study the influence of the pH, temperature,
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inorganic carbon content and DH concentration on hydrogenotrophic denitrification
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with an initial NO3--N of approximately 40 mg/L.
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In the pH tests, the pH was maintained at 6.0, 6.5, 7.0, 7.5, 8.0, 8.5 and 9.0 under
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temperature of 30 °C, IC/N mass ratio of 1.8 and DH concentration of 0.40 mg/L. An
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overdose of inorganic carbon was used to ensure of a sufficient carbon supply. In the
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temperature tests, the temperature was maintained at 15, 20, 25, 30, 35, 40, 45 and
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50 °C under pH of 7.0, IC/N mass ratio of 1.8 and DH concentration of 0.40 mg/L. In
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the inorganic carbon concentration tests, the initial mass ratio of IC/N was adjusted to
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0, 0.18 and 1.8 under pH of 7.0, temperature of 30 °C, and DH concentration of 0.40
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mg/L. To study the effect of the hydrogen concentration, pure argon gas was used to
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replace the volume of hydrogen gas to adjust the initial gaseous volume percentage of
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hydrogen in the headspace to 10%, 50% and 100%, under pH of 7.0, temperature of
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30 °C and IC/N mass ratio of 1.8.
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approximately 0.02, 0.17 and 0.40 mg/L, respectively.
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2.3 Sampling and analytical methods
The DH concentrations were determined to reach
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The gaseous samples were collected in gasbags for further analysis of the
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gaseous N2O and H2. The liquor samples were used for the analyses of nitrite, nitrite,
175
dissolved N2O and DH after filtering through a disposable Millipore filter (0.45 µm
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pore size). MLSS samples were collected at the end of each experiment and
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determined by weighing the dry cell. The intervals of the sampling were between 10
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min to 3 h according to the rate of reaction.
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The gaseous hydrogen was analyzed by gas chromatography (GC) (Agilent 7890,
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USA) with a Carbonxen-1000 packed column (1.5 m×2.1 mm×60/80 mesh, Supelco)
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and a thermal conductivity detector (TCD). Gaseous N2O was measured by GC
182
(Agilent6890N, USA) using a
Porapak Q packed column (1.8 m×2.1 mm×80/100
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mesh, Supelco) and an electron capture detector (ECD).
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The DH concentration was measured by the headspace method.26Liquor samples
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were taken with headspace vials that were then immediately sealed and vigorous
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shaken and resting for more than 2 hours. Thus, the hydrogen in the gaseous and
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liquid phase almost achieved its equilibrium state. The hydrogen concentration in the
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headspace of the vial was measured by GC according to the methods described above.
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The liquor sample concentration would be calculated according to Henry’s Law. A
190
similar method was also utilized to measure the dissolved N2O concentration. The
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gaseous N2O concentration of the headspace inside the vial was measured by GC. The
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dissolved N2O concentration was calculated according to Henry’s Law and the Mass
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Conservation Law. The DH and dissolved N2O were calibrated according to the
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method of Lu et al.24 The detection limits for the DH and dissolved N2O were below
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0.001 mg/L and 0.002 mg/L, respectively, and the coefficients of variation were
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0.0056 and 0.0112, respectively.
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The nitrate, nitrite and MLSS were determined according to the standard
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methods of the Chinese NEPA.25 The pH was determined by portable meters (HQ40D,
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Hach, USA). All of the samples were analyzed in triplicate.
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2.4. Microbial community analysis
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2.4.1 DNA extraction and PCR amplification
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The genomic DNA of the enriched cultures of the hydrogenotrophic denitrifiers
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was extracted using the E.Z.N.A.Soil DNA Kit D5625-01 (OMEGA, USA). The
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purity and concentrations of the nucleic acids were accurately measured using a Qubit
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2.0 fluorometer (Life Tech, USA). The V3-V4 hypervariable regions of the bacterial
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16S
207
(5’-CCTACGGGNGGCWGCAG-3’)
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ATCC-3’).The PCR products were pooled and purified with a SanPrep Column DNA
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Gel Extraction Kit SK8192 (Sangon Biotech, China). The details of the PCR
210
amplification are available in the Supplemental Material.
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2.4.2 Illumina high-throughput sequencing and data analysis
rRNA
genes
were
amplified and
805R
with
the
primers
341F
(5’-GACTACHVGGGTATCTA
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The DNA library was prepared according to the MiSeqTM Reagent Kit
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Preparation Guide (Illumina, San Diego, CA, USA) and run on a MiSeq Illumina
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platform for sequencing (Sangon Tech, China). The read preprocessing, operational
215
taxonomic unit (OTU) generation and identification, and statistical analyses were
216
performed with Mothur, and the taxonomic classification was assigned using the RDP
217
Classifier. The OTUs were generated with an identity threshold of 97%.
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3. Results and Discussion
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3.1 Nitrate, nitrite and N2O reduction by hydrogenotrophic denitrifiers
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The reduction rates of nitrate and its intermediates were evaluated using nitrate,
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nitrite and N2O as the sole electron acceptor. As shown in Figure 1, all of the
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concentrations of NO3--N, NO2--N and N2O-N/L linearly declined to depletion. The
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specific reduction rates of NO3--N, NO2--N and N2O-N, were calculated to be 0.66,
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0.76 and 3.96 kg N/(kg MLSSd), respectively. The nitrate reduction rates were higher
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than those of previous studies under similar conditions, which were in the range from
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0.38 to 0.60 kg N/(kg MLSSd).14,15,20 The results indicated that the enriched cultures
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in this study were highly efficient in hydrogenotrophic denitrification. Although the
228
reference of N2O reduction rate from other research is still unavailable at present, it is
229
comparable with that in heterotrophic denitrification. 26
230
The specific reduction rate of NO2--N was determined to be higher than that of
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NO3--N. Theoretically, it is reasonable to anticipate that nitrite would not be observed
232
during the batch test. However, when using nitrate as the sole electron acceptor, a
233
slight nitrite accumulation was observed with a maximum of 5.0 mgN/L, which then
234
rapidly disappeared. Rezania et al. observed that the nitrite reduction rate declined in
235
the presence of nitrate.14 The reduction of both nitrate and nitrite is known to occur at
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the end of the respiratory chain. Thus, competition for the hydrogen carrier and
237
electron carrier might occur between nitrate reductase and nitrite reductase. Pan et al.
238
demonstrated the hypothesis of electron competition in heterotrophic denitrification
239
by methanol utilizing denitrifiers.27 The competitive inhibition is a reasonable
240
explanation of nitrite accumulation during nitrate reduction.
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When using nitrate as sole electron acceptor, N2O was detected at an extremely
242
low concentration of less than 0.018 mg N2O-N/L, which accounted for only 0.044%
243
of the initial NO3--N concentration. This result indicated that N2O accumulation could
244
be controlled at an extremely low level during hydrogenotrophic denitrification.
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When using nitrite as the sole electron acceptor, N2O accumulation was observed and
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achieved a maximum at the beginning of the reaction, and then gradually decreased to
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depletion. The maximum concentration of N2O-N accumulated was 0.27 mgN/L,
248
which accounted for 0.75% of the initial NO2--N concentration. Moreover, the N2O
249
accumulation was obviously higher than that when using nitrate as the sole electron
250
acceptor. Hence, it could be confirmed that N2O reduction would be inhibited in the
251
presence of nitrite with relative high concentration. Adverse impact of nitrite on N2O
252
reduction has been widely reported in the studies on heterotrophic denitrification.18
253
3.2 Effect of pH on denitrification and N2O production
254
Nitrate reduction and N2O generation were investigated at different pH values,
255
and the results are shown in Figure 2. The effects of pH on hydrogenotrophic
256
denitrification were significant. The specific nitrate reduction rate gradually increased
257
with the increase in the pH value from 6.0 to 8.0, and achieved at maximum of 0.90
258
kg N/(kg MLSSd) at pH 8.0, which gradually decreased when the pH increased from
259
8.0 to 9.0 (Figure 2(b)). The nitrite accumulation achieved a minimum at a pH of 8.0,
260
and gradually increased when the pH decreased from 8.0 to 6.0 or increased from 8.0
261
to 9.0. It achieved 13.6 and 8.4 mg/L at the pH of 6.0 and 9.0, respectively. The nitrite
262
reduction rate also achieved a maximum at pH 8.0, and declined when the pH
263
changed from this value. The results indicate that the pH dependency of nitrate is
264
similar to that of nitrite in the pH range of 6.0 to 9.0. There is an optimal pH value for
265
both of nitrate and nitrite reduction, and the reduction rates decrease when the pH
266
deviates from this value. Nitrite accumulation was likely caused by the lower
267
reduction rate of nitrite relative to that of nitrate. Hence, it could be inferred that
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nitrite reductase is more sensitive to pH variation than nitrate reductase. Similar
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results were reported by Ghafari et al., which demonstrated that the optimal pH value
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for nitrate reduction was in the range of 7.5 to 8.0 and the highest specific reduction
271
rate was 0.53 mg N/(g MLSSd).16 However, Rezania et al. obtained different results,
272
demonstrating that the specific nitrate and nitrite reduction rates gradually increased
273
as the pH increased and nitrite accumulation did not occur at pH value from 7.5 to
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9.5.14The inconsistency in the optimal pH for hydrogenotrophic denitrification might
275
have been related to the different cultures used in the experiments. The cultures
276
enriched under different cultivation conditions would form different microbial
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community structures, which result in different denitrification characteristics.
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The report on the N2O accumulation during hydrogenotrophic denitrification is
279
still unavailable at present. It was reported that for heterotrophic denitrification with
280
the initial ratio of organic carbon to nitrogen varying from 3.5 to 10 (mol/mol), the
281
concentration of N2O in liquid phase is in the range from 0.1 to 3.0 mg N/L
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What’s more, the conversion ratio of N2O-N concentration to initial NO3--N
283
concentration were reported in the range from 0 to 14% when organic carbon was
284
abundant for denitrification.
285
concentration accumulated in liquid phase was observed extremely low, less than
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0.022 mgN/L at pH in the range from 7.0 to 9.0, corresponding to only 0.056% of the
287
initial NO3--N concentration. Therefore, we can conclude that the N2O accumulation
288
during hydrogenotrophic denitrification was comparable with heterotrophic
30~33
28,29
.
As shown in Figure 2(C), maximal N2O
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denitrification, and the potential of N2O emission in practice would be acceptable.
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However, when the pH decreased to 6.5, N2O accumulation increased to 0.163 mg/L.
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Furthermore, N2O immensely accumulated and achieved 5.84 mg N2O-N/L at pH 6.0,
292
corresponding to 15.2% of initial NO3--N concentration. These results indicated that
293
the N2O reductase could keep highly active at neutral and slightly alkaline condition,
294
and in contrast, be inhibited at slightly acidic condition. It is generally considered that
295
the activity of enzyme will decrease when the pH value deviates from the suitable
296
range. Under slightly acidic condition, N2O massively accumulated during the batch
297
test, indicating that N2O reduction suffered a more serious decline than nitrite
298
reduction. A potential explanation was proposed that N2O reductase could be
299
significantly inhibited by free nitrous acids (FNA). Nitrous acid is a weak electrolyte.
300
Consequently, FNA would be formed in the presence of nitrite at acidic condition. In
301
contrary to none report on the characteristics of N2O accumulation during
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hydrogenotrophic denitrification, it has been observed that, for heterotrophic
303
denitrification, the amount of N2O accumulation would sharply increase when pH was
304
adjusted to lower than 7.0.34 It is reported that N2O reductase is more severely
305
inhibited than nitrite reductase even if the FNA concentration in solution is as low as
306
0.0007 mgHNO2-N/L.26 The proposed mechanisms of FNA inhibition include
307
uncoupling effect and competitive inhibition to the enzyme. FNA could increase the
308
proton permeability through cell membranes, so that proton motive force would
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collapse and the synthesis of adenosine triphosphate (ATP) would be inhibited.26
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Moreover, the active sites of N2O reductase is more easily combining with FNA rather
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than N2O. 26 As shown in Figure 2(b), the maximal concentration of NO2--N reached
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13.6 mg/L at pH 6.0. Based on theoretical calculation, FNA concentration would
313
achieve 0.032 mgHNO2-N/L. It is reasonable to conclude that FNA inhibition play an
314
importance role in the N2O accumulation at slightly acidic condition.
315
3.3 The effect of temperature on denitrification and nitrous oxide production
316
Temperature significantly affects the performance of heterotrophic denitrification
317
as demonstrated by extensive researches.35 The effect of temperature on
318
hydrogenotrophic denitrification has not yet been comprehensively evaluated. The
319
temperature dependency of hydrogenotrophic denitrification was investigated at
320
different temperatures in the range of 15.0 to 50.0 °C. The profiles of NO3--N, NO2--N
321
and N2O-N are shown in Figure 3. The apparent optimal temperature was 40 °C for
322
nitrate reduction, with a specific nitrate reduction rate of 2.49 kg N/(kg MLSSd). The
323
specific nitrate reduction rate decreased gradually when the temperature moved away
324
from the optimal value. At the temperature as high as 50 °C, the specific nitrate
325
reduction rate reached 1.29 kg N/(kg MLSSd). When the temperature dropped down
326
to 15 °C, the specific nitrate reduction rate decreased to 0.17 kg N/(kg MLSSd),
327
which corresponded to only 6.6% of that at the optimal temperature. The effect of
328
temperature from 15 °C to 30 °C was previously evaluated through continuous
329
operating bioreactor.10, 36 The results show that higher temperature led to a higher
330
denitrification rate in this range, and indicate that the temperature dependence of the
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denitrification rate could be described by an Arrhenius equation.10 A consensus has
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not been reached on the optimal temperature. Consistent with the results of this study,
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Kurt et al. found that the maximum denitrification rate could be obtained at 42 °C.20
334
However, Zhou et al. suggested the suitable temperature range was 30 °C to 35 °C.37
335
Nitrite accumulation was observed at all of the test temperatures. The maximum
336
nitrite accumulation concentration was relatively low at less than 6.5 mg/L, at the
337
temperatures from 20 °C to 35 °C. NO2--N accumulated to a great degree when the
338
temperature fell to 15 °C or exceeded 40 °C. The maximum accumulation
339
concentration of NO2--N achieved to 17.0 and 20.4 mg/L occurred at temperatures of
340
15 °C and 40 °C, respectively. If the nitrite reduction rate were lower than the nitrate
341
reduction rate, NO2--N accumulation would occur. The accumulation concentration of
342
NO2--N was observed increasing when the temperature was deviated from the
343
optimum, indicating that comparing with nitrate reduction rate, the nitrite reduction
344
rate was more affected by temperature. Rezania et al. compared the characteristics of
345
hydrogenotrophic denitrification at 12±1 °C and 25±1 °C and found that nitrate
346
reduction showed stronger competition ability for electron donors than nitrite
347
reduction at low temperatures, which caused unexpected nitrite accumulation at
348
12 °C.14
349
During the experiments at temperatures from 20 °C to 50 °C, the N2O
350
concentration was always maintained at a low level. The maximum N2O-N
351
concentrations at the different temperatures in this range were all below 0.06 mg/L.
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However, when the temperature fell to 15 °C, the maximum N2O accumulation
353
sharply increased to 2.48 mg N2O-N /L, which corresponded to 6.2% of the initial
354
NO3--N. When the temperature is lower than the suitable range, the activity of enzyme
355
that catalyzes biochemical reactions in microbial cells will decline rapidly. The
356
suitable ranges are different depending on the types of enzyme. As shown in Figure
357
3(C), when the temperature dropped to 15°C, an abrupt increase of N2O accumulation
358
was observed during hydrogenotrophic denitrification, indicating that N2O reduction
359
rate was lower than that of nitrite and nitrate. This result suggested that the
360
temperature of 15°C had been beyond the suitable range for N2O reductase. The
361
temperature ranges in which nitrite and nitrate reductases are active seem to be larger
362
than that for N2O reductase. Although references are not available for
363
hydrogenotrophic denitrification, N2O accumulation has been reported to significantly
364
increase at low temperatures during winter because of the low temperature.
365
3.4 Effect of the IC/N ratio on denitrification and N2O production
366
Hydrogenotrophic denitrifiers have been shown to use inorganic carbon to
367
synthesize their cells through an autotrophic pathway.8 To investigate the effect of the
368
inorganic carbon concentration on denitrification performance, the sequencing batch
369
tests were conducted with an IC/N mass ratio of 0, 0.18 and 1.8, which were roughly
370
equivalent to the stoichiometric amounts of 0, 1 and 10 times (Eq. 5), respectively.
371
The pH was adjusted and maintained at 7.0 for each test, so that the influence of pH
372
could be avoided. As shown in Figure 4, the denitrification performance was
373
promoted by an inorganic carbon source substrate. The specific nitrate reduction rates
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were determined to be 0.38, 0.51 and 0.66 kg N/(kg MLSSd), which corresponded to
375
IC/N mass ratios of 0, 0.18 and 1.8, respectively. Denitrification was not terminated
376
without a dose of the inorganic carbon source substrate, although carbon dioxide
377
could be fixed and utilized for assimilation, which may explain why the dissolution of
378
carbon dioxide in water supported the inorganic carbon requirement.22
379
Nitrite accumulation was observed in all of three tests. The maximum
380
accumulation concentration of NO2--N was 6.8 mgN/L, which occurred under an IC/N
381
mass ratio of 0.18. The nitrous oxide concentrations were all very low (less than 0.02
382
mgN/L, corresponding to 0.05% of the initial NO3--N) under the various IC/N ratios,
383
indicating that the concentration of inorganic carbon source substrate had little
384
influence on the N2O accumulation in hydrogenotrophic denitrification. Hence, the
385
results demonstrate that N2O reduction rate is always higher than nitrite reduction rate
386
under various IC/N ratios in this study.
387
3.5 Effect of the hydrogen concentration on denitrification and N2O production
388
The effect of the DH concentration on the denitrification performance was
389
evaluated by controlling the volume percentage of hydrogen in headspace. The
390
concentrations of DH, NO3--N, NO2--N and N2O-N during the batch tests are shown
391
in Figure 5. In each of the three batch tests, the DH concentration was maintained at a
392
relatively stable range before nitrate was depleted. DH concentrations of
393
approximately 0.02, 0.17 and 0.40 mg/L corresponded to volume percentage of
394
hydrogen in the headspace of 10%, 50% and 100%, the DH concentrations were
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determined to reach approximately 0.02, 0.17 and 0.40 mg/L, respectively. After
396
nitrate was reduced completely, the DH concentration gradually increased. The nitrate
397
reduction rate decreased with the hydrogen percentage in headspace decreasing from
398
100% to 10% (shown in Table S1). Similar observation was obtained by Karanasios et
399
al.
400
denitrification performance through continuous operation of bioreactors. With gas
401
flow of hydrogen decreasing, the DH concentration and the denitrification efficiency
402
both decreased.
38
who studied the effects of hydrogen gas supply on the hydrogenotrophic
403
In this study, even though the DH concentration was as low as 0.02 mg/L, the
404
nitrate reduction rate remained at 0.26 kg N/(kg MLSS·d). It was still acceptable in
405
practical application, comparing to the denitrification rates obtained in other studies.
406
39,40
407
very low DH concentration. This phenomenon could be explained by kinetic analysis
408
through a double Monod model. According to the approach described by Lu et al., the
409
hydrogen saturation constant was calculated to be 0.03 mg/L (R2 = 0.963). When DH
410
of 0.02 mg/L was close to saturation constant, the nitrate reduction rate was still
411
satisfactory although the corresponding hydrogen percentage in headspace was only
412
10%.
It is evident that hydrogenotrophic denitrification could be effectively operated at
413
Nitrite accumulation was observed in the batch tests with DH concentration of
414
0.17 and 0.40 mg/L. In hydrogenotrophic denitrification, various reductases of
415
nitrogen oxides could obtain electron from hydrogen. Although the characteristics of
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the electron distribution among different reductases has not been studied for
417
hydrogenotrophic denitrification, the electron competition among reductases of
418
nitrogen oxides in heterotrophic denitrification was observed by Pan et al. 27 They
419
found that when the electron donors were limited, the competition would be
420
intensified. If the reductase was more competitive, the reduction rate of the
421
corresponding nitrogen oxide would be higher. Therefore, it can be inferred that with
422
limited hydrogen supply, the nitrite reductase is more competitive comparing to
423
nitrate reductase.
424
As shown in Figure 5(d), the characteristics of N2O accumulation were similar at
425
the various DH concentrations, and all of the maximum concentrations were less than
426
0.03 mgN2O-N/L. This result indicated that N2O emission would not increase even if
427
the hydrogen were insufficient. Although limited information is available on the effect
428
of electron donor concentration on N2O reduction for the hydrogenotrophic
429
denitrification, the characteristics of N2O accumulation under electron donor
430
limitation for heterotrophic denitrification has been widely investigated.18 According
431
to the previous reports, when concentration of electron donor was lower than the
432
theoretical quantity demanded for heterotrophic denitrification, the N2O would
433
accumulate significantly in solution.
434
accumulated during hydrogenotrophic denitrification, although at most time, the DH
435
concentration was much lower than theoretical quantity demanded for denitrification
436
corresponding to the nitrate concentration in solution. Moreover, the decrease of DH
18
On the contrary, the N2O was not excessively
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437
concentration low to 0.02 mg/L would not cause excessive N2O accumulation. This
438
feature offers a unique advantage for hydrogenotrophic denitrification in reducing
439
N2O emission from nitrogen removal treatment.
440
3.6 Microbial community of hydrogenotrophic denitrifying culture
441
We obtained 84930 high quality sequences with the average length of 445 bps for
442
the analysis of the microbial community. The number of OTUs, Shannon-Weiner
443
Index, ACE and Chao1 richness estimators were 2493, 4.38, 2539.3 and 2495.9.
444
Rarefaction curve plotting OTUs numbers was shown in Supplementary Figure S1.
445
The phylogenetic structure of the hydrogenotrophic denitrifier community was
446
characterized at the phylum, class and genus level, respectively. The relative
447
abundances of the main phyla, classes and genera with sequence percentage more
448
than 0.5% are shown in Figure 6. At the phylum level, the culture was dominated by
449
Proteobacteria
450
Euryarchaeota (4.4%). As shown in Figure 6(b), the OTUs belonging to
451
Proteobacteria were mostly
affiliated to Alphaproteobacteria
452
Betaproteobacteria
although
453
Gammaproteobacteria (0.6%).
(64.0%),
Firmicutes
(25.4%),
(17.4%),
they
Bacteroidetes
were
rarely
(13.9%)
and
(37.9%) and affiliated
with
454
In total, 172 genera were identified, although only seven were predominant at
455
relative abundances of more than 4%. The sum of the sequence number belonging to
456
these seven genera accounted for 84.7% of the total sequences. As shown in Figure
457
6(c), the dominant genera (in order) were Paracoccus (26.1%), Azoarcus (24.8%),
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Acetoanaerobium
459
Geosporobacter (4.6%) and Methanobacterium (4.3%).
(11.4%),
Labrenzia
(7.4%),
Dysgonomonas
(6.0%),
460
The genus Paracoccus was the most abundant in this hydrogenotrophic
461
denitrifying culture, and is considered as metabolically versatile bacterium with
462
bioenergetic flexibility.41 Most of the species of Paracoccus use nitrate as an
463
alternative electron acceptor to oxygen with nitrogen gas as final reduction product. A
464
range of organic and inorganic compounds including hydrogen can be used as
465
electron donors by the Paracoccus species, which are frequently observed in
466
bioreactors that show nitrate reduction with hydrogen.42,43 In addition, Vasiliadou et al.
467
used a pure culture of Paracoccus sp. to investigate the hydrogenotrophic
468
denitrification process, and nitrite accumulation was not observed throughout the
469
batch test.16
470
The genus Azoarcus was another dominant genus with a relative abundance close
471
to that of Paracoccus. Species of this genus have been reported as denitrifying
472
bacteria,44and are regarded as important groups that play a role in denitrification in
473
sewage treatment.45
474
The genus Acetoanaerobium, which contains the single species Acetoanaerobium
475
noterae, is an anaerobic bacterium that forms acetate from H2 and CO2.46 This
476
bacteria was frequently found in microbial fuel cells (MFCs).47This is the first report
477
that bacteria affiliated with Acetoanaerobium are enriched in the hydrogenotrophic
478
denitrifying community. The production of acetate could conceivably serve as an
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479
electron donor and carbon source for the heterotrophic denitrification pathway that
480
might have occurred in this study. In the bioreactor, there are plenty of hydrogen as
481
electron donor and sodium bicarbonate as carbon source for hydrogenotrophic
482
denitrifier. The sodium bicarbonate could also serve as electron acceptor for
483
Acetoanaerobium to generate acetate and for Methanobacterium to generate methane.
484
Although the pathway of ecological interactions in the microbial community and the
485
contribution proportion of nitrogen removal are unavailable in this study, it can be
486
verified that there are a variety of metabolic types in such an ecological system with
487
hydrogen and inorganic carbon.
488
The genera Labrenzia, Dysgonomonas and Geosporobacter have never been
489
reported in hydrogenotrophic denitrifying culture in previous studies. However, they
490
were enriched in the bioreactor of this study. For the mechanism of significant
491
enrichment of these genera, it needs further investigation. Furthermore, the genus
492
Methanobacterium, which is hydrogenotrophic methanogenic archaea, was also
493
observed, suggesting that methanogenesis might also occur in this system.
494
Previous reports on the microbial community structure of hydrogenotrophic
495
denitrification are rare. Researchers have used denaturing gradient gel electrophoresis
496
and phylogenetic analysis to identify the dominant groups in hydrogenotrophic
497
denitrification cultures.23,48 In addition, studies have created clone libraries of the 16S
498
rRNA gene to reveal the microbial community structures.49 However, the information
499
obtained through these DNA fingerprinting analysis was too limited to reflect the
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completely microbial community, because of the finite quantity of clones. In order to
501
completely reflect the microbial community, Mao et al. applied high-throughput
502
sequencing to characterize microbial communities of enriched hydrogenotrophic
503
denitrifying cultures.42 In their study, the most dominant populations observed were
504
identified as Thauera species, which had a relative abundance of nealy 60%. Chen et
505
al. analyzed the microbial community of biofilm from a bio-ceramsite reactor of
506
hydrogenotrophic denitrifying through 454-pyrosequencing.
507
genus was found to be Acinetobacter when the bioreactor was operated at pH of 7.0,
508
while genus Planomicrobium was most dominant at pH of 9.0. Moreover, the genus
509
Thauera and Paracoccus were also observed in the bio-ceramsite reactor. Zhang et al.
510
analyzed the microbial community of a membrane-biofilm reactors (MBfR) of
511
hydrogenotrophic denitrifying through 454-pyrosequencing.51 The most abundant
512
genera in the MBfR feeding nitrate as the sole electron acceptor was found to be
513
denitrifying bacteria, including Stenotrophomonas and Dechloromonas.
50
The most dominant
514
3.7 Implications to the environmental application
515
The performances of hydrogenotrophic denitrification and characteristics of N2O
516
accumulation were investigated through a series of batch tests under various
517
environmental conditions. It has been confirmed that nitrate could be efficiently
518
removed through hydrogenotrophic denitrification under the general condition in
519
practical engineering, including the pH, temperature, inorganic carbon content and
520
hydrogen concentration. Among the batch tests, the N2O was only observed to
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521
massively accumulated under slightly acidic condition and temperature dropping to
522
15 °C. By contrast, the N2O accumulation was extremely low under other test
523
conditions that were common in practical engineering. This result indicated that
524
hydrogenotrophic denitrification is an adaptive and promising technology. Its
525
advantages are not only the efficient nitrogen removal performance but also the
526
mitigation potential of N2O emission. Although it was observed that the N2O
527
massively accumulated only under some specific conditions, the implications of this
528
finding was still significant for practice, considering there would be some nitrogen
529
removal requirement under such condition in engineering. For instance, in the winter
530
of cold region, the temperature of nitrate-polluted water may drop below 15 °C.
531
some region, the pH of nitrate-polluted water may be lower than 7.0.
532
results in this study, if the hydrogenotrophic denitrification were used in such
533
condition, the N2O emission would be concerned and mitigation measures should be
534
considered.
52
10
In
According to
535
The microbial community of hydrogenotrophic denitrification was revealed by
536
high throughput sequencing. The dominant species were found to belong to the genera
537
Paracoccus (26.1%), Azoarcus (24.8%), Acetoanaerobium (11.4%), Labrenzia (7.4%),
538
and Dysgonomonas (6.0%). These findings could contribute to the knowledge of the
539
hydrogenotrophic denitrifiers.
540
Acknowledgements
541
This work was financially supported by the National Water Pollution Control and
542
Treatment Science and Technology Major Project of China (No.2012ZX07205-001)
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and the China Postdoctoral Science Foundation (No.2014M560982).
544
Supporting Information Available
545
Relevant information on batch tests condition, nitrate reduction rate, maximal
546
NO2--N and N2O-N accumulation ratio; methods of PCR amplification, purification
547
and re-amplification; Rarefaction curve plotting OTUs numbers. This information is
548
available free of charge via the Internet at http://pubs.acs.org/
549
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(a) Phylum
0.4% 4.4%
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0.60% 0.70% 4.37% 6.66%
(b) Class
Betaproteobacteria
Proteobacteria 13.9%
Firmicutes
Clostridia
7.09% 37.89%
Bacteroidetes 17.4%
Euryarchaeota
Alphaproteobacteria
Bacteroidia Flavobacteria
17.25%
64.0%
Methanobacteria
Others
Gammaproteobacteria 25.44%
Others
(c) Genus 3.83% 0.57% 0.66% 8.08% 1.06% 1.09% 4.34%
26.11%
4.61% 5.97% 7.44% 11.40%
24.84%
Paracoccus Azoarcus Acetoanaerobium Labrenzia Dysgonomonas Geosporobacter Methanobacterium Proteiniphilum Dethiobacter Stappia Aquamicrobium Others Unclassified
Figure 6. The relative abundances of major bacterial groups at (a) Phylum, (b) Class and (c) Genus levels (sequence percentage >0.5%).
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