This study investigated the influences of aeration mode and influent carbon/nitrogen ratio on matrix oxygen concentration, pollutant removal, greenhouse gas emission, functional gene abundances and bacterial community in subsurface wastewater infiltration systems (SWISs). Intermittent or continuous aeration enhanced oxygen supply at 0.6 m depth in the matrix, which improved organics removal, nitrogen removal, the abundances of bacterial 16S rRNA, amoA, nxrA, narG, napA, nirK, nirS, norB, nosZ genes, bacterial community Alpha diversity, the relative abundances of Actinobacteria at 0.6 m depth, the relative abundances of Chloroflexi, Gemmatimonadetes, Bacteroidetes and Firmicutes at 0.9 and 1.2 m depth and reduced CH4 and N2O conversion efficiencies, the abundance of mcrA gene with carbon/nitrogen ratio of 12 and 16 compared with non-aeration. Increased carbon/nitrogen ratio resulted in higher TN removal efficiencies and lower CH4 and N2O conversion efficiencies in aeration SWISs than those in non-aeration SWIS. Intermittent aeration SWIS obtained high removal efficiencies of 83.2, 85.4 and 90.8% for TN, NH4+ -N and COD and low conversion efficiency of 0.21 and 0.65% for N2O and CH4 with optimal carbon/nitrogen ratio of 12. However, high TN (82.6%), NH4+ -N (84.9%) and COD (92.2%) removal efficiencies and low CH4 (0.67%) and N2O (0.23%) conversion efficiencies were achieved in continuous aeration SWIS with carbon/nitrogen ratio of 16.

  • Carbon/nitrogen ratio of 12 was recommended for intermittent aeration WSIS.

  • Carbon/nitrogen ratio of 16 was suggested for continuous aeration WSIS.

  • Aeration changed the abundances of bacterial 16S rRNA and functional genes.

  • Aeration could obtain high pollutant removal and low CH4 and N2O emission.

The discharge of decentralized domestic wastewater has resulted in the contamination of surface water and groundwater, causing ecological damage and exacerbating water scarcity in numerous countries (Yang et al. 2016). However, traditional centralized wastewater treatment technologies are unfit for decentralized domestic wastewater due to high construction, operation investment and complex maintenance (Ji et al. 2012). Subsurface wastewater infiltration system (SWIS) is a kind of low-construction cost and easy management ecological treatment method, which has been widely applied to treat decentralized domestic wastewater in many areas (Zheng et al. 2018). The construction cost of SWIS is one-half of the secondary biochemical treatment and the operating cost is one-fifth (Li et al. 2013). In subsurface wastewater infiltration systems (SWISs), wastewater is purified by physical, chemical and biochemical action after entering into the underground soil layer. The removal efficiency of COD and TP was more than 80 and 90%, respectively (Li et al. 2021). However, TN removal efficiency was only around 50% which limited its application (Li et al. 2020).

Biological nitrification and denitrification is the major nitrogen removal process in SWISs. The strategies widely adopted to strengthen nitrogen removal are: (1) amending the original soil with different materials, such as dewatered sludge, biochar and functional microorganisms (Sun et al. 2018; Jia et al. 2019; Liang et al. 2019); (2) increasing carbon source supply for denitrification process (Li et al. 2021); (3) improving soil oxygen environment for nitrification by aeration or intermittent operation (Pan et al. 2015; Chen et al. 2021b). Among these methods, aeration has been acknowledged as an effective and practical approach for enhancing the oxygen environment within the matrix and facilitating nitrogen removal (Fan et al. 2013; Liang et al. 2019). Aeration mode could be categorized into continuous aeration and intermittent aeration (IA), which could create different matrix oxygen environments and ultimately affect nitrogen and organics removal (Yang et al. 2016). The influent carbon/nitrogen ratio affected nitrogen removal in SWISs significantly (Li et al. 2018). Relevant studies have predominantly focused on the individual effects of aeration or carbon/nitrogen ratio on the removal of pollutants in SWISs (Zheng et al. 2018; Li et al. 2020).

The emissions of CO2, CH4 and N2O from SWISs are significant contributors to the greenhouse effect and have garnered increasing attention in recent years (Kong et al. 2016). CO2 is emitted from the aerobic degradation of organics. CH4 occurs in the anaerobic fermentation of organics and N2O is produced in the process of biological nitrification and denitrification. Many factors could affect greenhouse gas emissions in SWISs. Li et al. (2019) and Pang et al. (2020) found that influent hydraulic loading, pollutant loading and concentration affected N2O release in SWISs. CH4 and N2O emissions increased with the increase of influent carbon/nitrogen ratio, matrix oxidation reduction potential (ORP) and temperature in non-aeration SWISs, which was reported by Kong et al. (2016). Sun et al. (2018) and Zheng et al. (2018) concluded IA was a feasible strategy for SWISs to reduce N2O generation. However, there are few researches absorbed in the influence of influent carbon/nitrogen ratio and aeration mode on CO2, CH4 and N2O emission in SWISs synchronously.

In this study, series of laboratory-scale experiments in SWISs was carried out to (1) reveal the influences of influent carbon/nitrogen ratio and aeration mode on organic removal, nitrogen removal and CO2, CH4 and N2O emission; (2) explore bacterial community, vertical distribution and the abundances of functional genes involved in COD removal, removal, TN removal, three greenhouse gases emission with different influent carbon/nitrogen ratios and aeration modes; (3) achieve optimal operation parameters with which best pollutants removal were achieved and least greenhouse gases were produced.

Experimental SWISs

Three laboratory-scale SWISs made of perspex columns were used with 140 cm height and 30 cm internal diameter, which operated in the greenhouse laboratory of Shenyang Normal University in China with a temperature of 22 ± 1°C (Figure 1). The interior of three columns was packed with a two layer matrix. The upper layer consisted of 120 cm of meadow soil and coal-burning slag, mixed uniformly in a mass ratio of 9:1 to filter and purify wastewater. This layer had a surface area of 224.3 ± 2.7 m2/kg and contained total organics of 31.8 ± 1.3 g/kg, total nitrogen of 1.4 ± 0.5 g/kg, total phosphorus of 0.6 ± 0.05 g/kg and pH value at 7.2. The bottom layer was 20 cm of gravel (5–10 mm in diameter) to support the system and distribute water. Meadow brown soil was collected from field soil at Yuhong of Shenyang, China, which was the main soil type in plain areas. Coal-burning slag was gathered from Huanggu Heat Source Co., Ltd, Shenyang. Oxygen electrodes were installed in the middle of the matrix at 0.6, 0.9 and 1.2 m, respectively. Wastewater was distributed by a four-winged distributing pipe at 0.6 m and treated water was gathered at the outlet at the bottom. Black plastics are wrapped outside of each column to prevent light and algae breeding. Matrix sampling ports were at 0.6, 0.9 and 1.2 m on the right and left sides of each column.
Figure 1

Schematic diagram of three subsurface wastewater infiltration systems (SWISs) with intermittent aeration (IA-SWIS), continuous aeration (CA-SWIS) and without aeration (NA-SWIS).

Figure 1

Schematic diagram of three subsurface wastewater infiltration systems (SWISs) with intermittent aeration (IA-SWIS), continuous aeration (CA-SWIS) and without aeration (NA-SWIS).

Close modal

SWISs operation

Synthetic wastewater was continuously fed for each SWIS with 24 h hydraulic retention time. The carbon/nitrogen ratio of synthetic wastewater was adjusted by altering the content of sodium acetate (CH3COONa). Four different carbon/nitrogen ratios (a: 4; b: 8; c: 12; d: 16) were formulated. Synthetic wastewater also composed of 165 mg/L (NH4)2SO4; 15 mg/L KH2PO4; 8 mg/L NaNO3; 12 mg/L MgSO4; 12 mg/L MnSO4; 12 mg/L ZnSO4·7H2O; 12 mg/L FeSO4 and 12 mg/L CaCl2. The characteristics of the synthetic wastewater was shown in Table 1.

Table 1

The characteristics of the synthetic wastewater (mean ± SD)

Carbon/nitrogen ratio481216
COD (mg/L) 163.6 ± 8.9 324.4 ± 14.5 487.1 ± 10.7 658.9 ± 18.2 
(mg/L) 38.5 ± 0.6 39.2 ± 0.3 38.1 ± 0.5 38.7 ± 0.2 
TN (mg/L) 41.3 ± 0.3 41.7 ± 0.5 41.8 ± 0.6 41.1 ± 0.7 
(mg/L) 1.3 ± 0.6 1.2 ± 0.3 1.5 ± 0.2 1.1 ± 0.4 
TP (mg/L) 4.2 ± 0.4 4.1 ± 0.2 4.5 ± 0.3 4.4 ± 0.1 
Carbon/nitrogen ratio481216
COD (mg/L) 163.6 ± 8.9 324.4 ± 14.5 487.1 ± 10.7 658.9 ± 18.2 
(mg/L) 38.5 ± 0.6 39.2 ± 0.3 38.1 ± 0.5 38.7 ± 0.2 
TN (mg/L) 41.3 ± 0.3 41.7 ± 0.5 41.8 ± 0.6 41.1 ± 0.7 
(mg/L) 1.3 ± 0.6 1.2 ± 0.3 1.5 ± 0.2 1.1 ± 0.4 
TP (mg/L) 4.2 ± 0.4 4.1 ± 0.2 4.5 ± 0.3 4.4 ± 0.1 

Three laboratory-scale SWISs were named NA-SWIS, IA-SWIS and CA-SWIS, respectively. IA-SWIS and CA-SWIS contained aeration units which consisted of air pump, gas meter and aeration diffuser. The aeration diffuser was at 0.6 m below the surface matrix. Aeration diffusers and influent distributing pipes were wrapped in gravel with a diameter of 1–2 cm to prevent clogging. The airflow rate of 3.5 ± 0.2 L/min was applied in IA-SWIS and CA-SWIS, respectively. The cyclic aeration/non-aeration process was for IA-SWIS, which was 1 h for aeration and then 5 h without aeration. Continuous aeration was for CA-SWIS and non-aeration was for NA-SWIS. Before this experiment, three SWISs have been run for 45 days to allow microorganisms maturation. Four running plans were arranged in each SWIS with a carbon/nitrogen ratio gradually elevated from 4 to 8, 12 and 16. An increase in the influent carbon/nitrogen ratio also meant an increase in the organic loading rate. Each running plan lasted for 40 days. The experiment commenced in May of 2022 and spanned over a duration exceeding 5 months.

Sampling and analytical methods

Water samples and gas samples were collected after each SWIS had been run for 10 days under the experimental carbon/nitrogen ratio. The mature SWIS takes about a week to operate steadily under a new running parameter (Li et al. 2020).

Water samples were taken from the influent and outlet every 5 days. COD, , , , TOC and TN of the water samples were analyzed on the basis of water and wastewater standard analytical methods of China (Standard Method for the Examination of Water & Wastewater Editorial Board 2002).

Mixed gas samples were gathered every 5 days with the static stationary chambers during an aeration/non-aeration period. The detailed gas sampling operation was listed in the study of Zheng et al. (2018). The concentrations of CO2, CH4 and N2O in the gas samples were carried out by Agilent 6890N gas chromatography, respectively. CO2, CH4 and N2O emission rates and conversion efficiencies were calculated by (1)–(3) formulas (Li et al. 2020). Conversion efficiency is the mass percentage of CO2 and CH4 or N2O in removed TOC or TN, respectively.
(1)
(2)
(3)

ρ represents CO2, CH4 or N2O mass concentration, mg/m3; φv is the gas sample volume fraction; θ is the gas sample temperature, °C; M represents CO2, CH4 or N2O molar mass, g/mol; H is the height of gas collection unit, m; Δt is the sampling interval time; ρ2ρ1 represents CO2, CH4 or N2O mass concentrations in sampling interval, mg/m3; m1 represents CO2, CH4 or N2O emission in sampling interval, mg; m2 is the mass of TOC or TN removed in sampling interval, mg.

After each carbon/nitrogen ratio experiment, matrix samples were collected from sampling ports to analyze bacteria and functional genes by real-time quantitative polymerase chain reaction (qPCR) on 16S rRNA fragment of bacteria, the target fragment of ammonia monooxygenase (amoA) and nitrite oxidoreductase (nxrA), membrane-bound nitrate reductase (narG), periplasmic nitrate reductase (napA), nitrite reductase (nirS and nirK), nitric oxide reductase (norB), nitrous oxide reductase (nosZ) and Methyl Coenzyme M Reductase A (mcrA) genes which related to organics removal, nitrogen removal and CO2, N2O or CH4 production. The specific procedures of qPCR were referred to the study of Ji et al. (2012). In addition, the bacterial community of each sample was analyzed by high-throughput sequencing technology according to Chen et al. (2021a).

Matrix oxygen concentrations were recorded and stored in data collectors every 20 min. The average value of matrix oxygen concentrations was calculated as the mean of all data collected after each SWIS was run for 10 days under the experimental carbon/nitrogen ratio.

Each sample was analyzed three times and the mean value of the three analyses was reported. Statistical analysis was performed using SPSS 19.0 software. The significance level was set at P < 0.05 and differences were assessed using two-way ANOVA.

Oxygen concentrations in the matrix

Average matrix oxygen concentrations in an aeration/non-aeration cycle of this study under each carbon/nitrogen ratio are shown in Figure 2. Oxygen concentrations of NA-SWIS were lower than 0.96, 0.27 and 0.03 mg/L at 0.6, 0.9 and 1.2 m depths with carbon/nitrogen ratios of 4, 8, 12 and 16, respectively. Non-aeration SWIS was in anoxic or anaerobic condition because air diffused into the matrix was limited, which was in accordance with the reports of Li et al. (2021) and Pang et al. (2020). However, oxygen concentrations of CA-SWIS were more than 4.1 mg/L at 0.6 m depth and below 0.38 and 0.03 mg/L at 0.9 and 1.2 m depths with carbon/nitrogen ratios of 4, 8, 12 and 16, respectively. CA-SWIS was in aerobic condition (oxygen ≥ 2 mg/L) at 0.6 m and in anaerobic condition at 0.9 and 1.2 m. In IA-SWIS, oxygen concentrations at 0.6 m depth were higher than 4.0 mg/L with aeration and higher than 0.8 mg/L when aeration stopped with a carbon/nitrogen ratio of 4, 8, 12 and 16, respectively. Whether or not it was aerated, oxygen concentrations were lower than 0.3 and 0.04 mg/L at 0.9 and 1.2 m, respectively. In the non-aeration period of IA-SWIS, oxygen concentrations showed decreasing trends because nutrients and organics aerobic degradation consumed oxygen. With the same carbon/nitrogen ratio, oxygen concentrations of CA-SWIS and IA-SWIS at 0.6 m were significantly higher than those of NA-SWIS (P < 0.05), but they were not significantly different at 0.9 and 1.2 m (P > 0.05). Oxygen concentrations at 0.6 m depth decreased with the carbon/nitrogen ratio increasing in three SWISs. With a high carbon/nitrogen ratio, more organics aerobic degradation consumed more oxygen. Aeration enhanced the oxygen supply at 0.6 m depth, which did not change the matrix oxygen condition below 0.9 m depth.
Figure 2

Average matrix oxygen concentrations in an aeration/non-aeration cycle in IA-SWIS, CA-SWIS and NA-SWIS.

Figure 2

Average matrix oxygen concentrations in an aeration/non-aeration cycle in IA-SWIS, CA-SWIS and NA-SWIS.

Close modal

Effects of aeration mode and carbon/nitrogen ratio on organics and nitrogen removal

Average effluent concentrations and removal efficiencies of COD, and TN in three SWISs are shown in Figure 3. COD removal performances in aeration SWISs and non-aeration SWIS were significantly different. Average removal efficiencies of COD in CA-SWIS and IA-SWIS were significantly higher than those in NA-SWIS with the same carbon/nitrogen ratio (P < 0.05). Microbial aerobic degradation of organics is the major path for COD removal in SWISs (Yang et al. 2016). However, an anoxic or anaerobic matrix environment restricted COD removal in NA-SWIS. Aeration improved the oxygen supply of CA-SWIS and IA-SWIS, which promoted COD removal. COD removal efficiencies decreased with the influent carbon/nitrogen ratio increasing in NA-SWIS. More oxygen is required by the oxidation of more organics with a high carbon/nitrogen ratio. However, NA-SWIS could not provide sufficient oxygen with a high carbon/nitrogen ratio. COD removal efficiencies were not significantly different with a carbon/nitrogen ratio between 4 and 8 in IA-SWIS and CA-SWIS (P > 0.05), which was different from that in NA-SWIS. However, COD removal efficiencies decreased from 98.1 to 88.7% for IA-SWIS and from 98.2 to 92.2% for CA-SWIS as the carbon/nitrogen ratio increased from 8 to 16. Aeration with these experimental parameters could not provide adequate oxygen with a high carbon/nitrogen ratio of 16, which is accorded with the reports of Song et al. (2016), Zhou et al. (2017) and Li et al. (2018).
Figure 3

Average COD, , TN removal performance and , concentrations of the effluents in IA-SWIS, CA-SWIS and NA-SWIS.

Figure 3

Average COD, , TN removal performance and , concentrations of the effluents in IA-SWIS, CA-SWIS and NA-SWIS.

Close modal

In NA-SWIS, average removal efficiencies of were 84.7, 80.1, 47.7 and 15.6% with average effluent concentrations of 5.9, 7.6, 20.1 and 32.5 mg/L under carbon/nitrogen ratio of 4, 8, 12 and 16, respectively. Average effluent concentrations with carbon/nitrogen ratios of 12 and 16 exceeded the Class I of Municipal Sewage Treatment Plant Discharge Standard of China ( ≤ 15 mg/L) (GB18918-2002). removal efficiencies of NA-SWIS decreased with the carbon/nitrogen ratio increasing. Nitrification is an aerobic reaction, which is the first process for removal (Song et al. 2016). Non-aeration SWIS could not achieve this reaction efficiently due to a lack of oxygen (Yang et al. 2016; Li et al. 2021). More oxygen was required with carbon/nitrogen ratio increasing which inhibited ammonia oxidation microorganisms from oxidizing by oxygen competition. Average removal efficiencies of in IA-SWIS and CA-SWIS were significantly higher than those in NA-SWIS with the same carbon/nitrogen ratio (P < 0.05). Average removal efficiencies decreased when the carbon/nitrogen ratio increased from 8 to 16 in IA-SWIS and CA-SWIS. Aeration could not supply enough oxygen for nitrification with a high carbon/nitrogen ratio in this study. However, the average removal efficiency of in CA-SWIS was significantly higher than that in IA-SWIS with a carbon/nitrogen ratio of 16 (P < 0.05) because more oxygen was provided by continuous aeration.

In SWISs, denitrification is widely regarded as the main way to nitrogen removal, which needs anaerobic conditions and enough carbon source (Li et al. 2021). TN removal in SWISs with aeration and without aeration was significantly different. Average TN removal efficiencies decreased with the carbon/nitrogen ratio increasing in NA-SWIS, which was the same trend with removal. With a high carbon/nitrogen ratio, removal was restrained, which limited the denitrification reaction due to inadequate supply as electron acceptors. In NA-SWIS, average removal efficiencies of TN were 44.6 and 16.4% and average effluent TN concentrations were 22.7 and 34.6 mg/L with carbon/nitrogen ratio of 12 and 16, which exceeded the above-mentioned standard (TN ≤ 20 mg/L). The carbon/nitrogen ratio of 4 and 8 was recommended for non-aeration SWIS in this study. With carbon/nitrogen ratio of 4 and 8, average removal efficiencies of TN in IA-SWIS and CA-SWIS were significantly lower than those in NA-SWIS (P < 0.05), which were 23.3 and 53.1% for IA-SWIS and 22.8 and 52.6% for CA-SWIS, respectively. Moreover, was the main component of TN in the effluents in IA-SWIS and CA-SWIS. After effective organics oxidation and nitrification by aeration, the carbon source as electron donor was deficient, which led as electron accepters to be accumulated and not to be eliminated with a low carbon/nitrogen ratio. The results accorded with the report of Fan et al. (2013). With a carbon/nitrogen ratio of 12 and 16, the average removal efficiencies of TN in IA-SWIS and CA-SWIS were significantly higher than those in NA-SWIS (P < 0.05). After effective nitrification in aeration SWISs, a high carbon/nitrogen ratio provided more carbon sources for denitrification and resulted in less accumulation, which achieved high TN removal. The average TN removal efficiency of IA-SWIS was significantly higher than that of CA-SWIS with a carbon/nitrogen ratio of 12 due to more carbon sources obtained in IA-SWIS (P < 0.05). However, with a carbon/nitrogen ratio of 16, the average removal efficiency of TN in IA-SWIS was significantly lower than that in CA-SWIS because lower nitrification of IA-SWIS achieved compared with CA-SWIS and more carbon source provided after high efficient nitrification in CA-SWIS (P < 0.05). A carbon/nitrogen ratio of 12 and 16 was suggested for IA-SWIS and CA-SWIS separately.

Effects of aeration mode and carbon/nitrogen ratio on CO2, CH4 and N2O emission

As can be seen in Figure 4, average CO2 conversion efficiencies decreased with carbon/nitrogen ratio increasing in NA-SWIS, which were 80.1, 74.4, 61.2 and 47.5% with carbon/nitrogen ratios of 4, 8, 12 and 16. Air diffusion to the matrix was limited in non-aeration SWISs (Pan et al. 2015). Matrix oxygen concentrations decreased with the carbon/nitrogen ratio increasing at 0.6 m depth which caused organic matter aerobic oxidation to decrease and led to CO2 conversion efficiencies reduction. Average emission rates and conversion efficiencies of CO2 in IA-SWIS and CA-SWIS were significantly higher than those in NA-SWIS with the same carbon/nitrogen ratio (P < 0.05). Aeration supplied extra oxygen which greatly increased organics aerobic biochemical oxidation and improved CO2 generation. CA-SWIS obtained average CO2 emission rates of 8.5 and 10.6 g/(m2·day) with average conversion efficiencies of 89.3 and 82.6% under carbon/nitrogen ratio of 12 and 16, respectively, which were higher than those of IA-SWIS due to more oxygen provided by continuous aeration with high carbon/nitrogen ratios.
Figure 4

CO2, CH4 and N2O emission rates and conversion efficiencies with carbon/nitrogen ratio of 4, 8, 12, 16 in IA-SWIS, CA-SWIS and NA-SWIS.

Figure 4

CO2, CH4 and N2O emission rates and conversion efficiencies with carbon/nitrogen ratio of 4, 8, 12, 16 in IA-SWIS, CA-SWIS and NA-SWIS.

Close modal

CH4 conversion efficiencies of NA-SWIS enhanced with carbon/nitrogen ratio increasing, which were 0.82, 0.94, 1.12 and 1.35% with average CH4 emission rates of 9.4, 21.4, 37.5 and 58.2 mg/(m2·day) under carbon/nitrogen ratio of 4, 8, 12 and 16, respectively (in Figure 4). The increased carbon/nitrogen ratio meant more organic matter, which could expend more oxygen and supply more carbon source for the growth of anaerobic methanogen in non-aeration systems (Li et al. 2018). As a result, CH4 conversion efficiencies and emission rates increased with the influent carbon/nitrogen ratio increasing in NA-SWIS. Average CH4 conversion efficiencies were below 0.68% with carbon/nitrogen ratios of 4, 8, 12 and 16 in IA-SWIS and CA-SWIS, which were significantly lower than those in NA-SWIS with the same carbon/nitrogen ratio (P < 0.05). Low emission rates of CH4 in IA-SWIS and CA-SWIS were attributed to aeration, which improved organic aerobic oxidation and led to a decrease of available organics to methanogen. Wang et al. and Yang et al. reported the same result that aeration could reduce the abundance of methanogen and decrease CH4 production. Average CH4 conversion efficiencies of IA-SWIS and CA-SWIS were not significantly different (Yang et al. 2017). In aeration SWISs, there were no significant differences in CH4 conversion efficiencies among different carbon/nitrogen ratios in this study. It could be concluded that aeration mode and carbon/nitrogen ratio could hardly affect CH4 emission in aeration SWISs.

Average N2O emission rates were 5.2, 4.8, 3.2 and 2.4 mg/(m2 day) with conversion efficiencies of 0.89, 0.78, 0.55 and 0.41% when the carbon/nitrogen ratio was 4, 8, 12 and 16 in NA-SWIS, respectively (in Figure 4). Furthermore, average N2O conversion efficiencies decreased with the carbon/nitrogen ratio increasing, which was in agreement with the report of Li et al. (2018). A higher carbon/nitrogen ratio represents more organics, which might consume more available oxygen to oxide it and further constrain the autotrophic ammonia oxidation bacteria to oxidize due to oxygen competition. The final result was that denitrification as the next step of nitrification was also restricted in NA-SWIS. Therefore, N2O emission decreased. Jacobs and Harrison concluded when carbon source availability was high, nitrifying bacteria were poor competitors for compared with heterotrophic microbes (2014). Sabba et al. (2015) and Maucieri et al. (2017) also revealed that N2O conversion efficiency positively correlated with nitrification rate in low denitrification rate wastewater treatment systems. Average N2O emission rates and conversion efficiencies of CA-SWIS and IA-SWIS were more than 5.7 mg/(m2 day) and 0.97% with carbon/nitrogen ratios of 4 and 8, which were significantly higher than those of NA-SWIS because of high nitrification rates and low denitrification rates in aeration SWISs (P < 0.05). After efficient nitrification and aerobic oxidation of organics, the carbon source was not enough for the denitrification process which constrained N2O transforming to N2 in IA-SWIS and CA-SWIS with low carbon/nitrogen ratios of 4 and 8. Average N2O emission rates and conversion efficiencies with a carbon/nitrogen ratio of 12 and 16 were significantly lower than those with a carbon/nitrogen ratio of 4 and 8 in aeration SWISs (P < 0.05). Similar findings were reported by Li et al. (2018), Wang et al. (2014) and Zhou et al. (2017). A higher carbon/nitrogen ratio provided more organics for N2O to N2 transformation, which led to N2O emission reduction. The average emission rate of N2O in IA-SWIS was lower than that in CA-SWIS with a carbon/nitrogen ratio of 12 and was higher than that in CA-SWIS with a carbon/nitrogen ratio of 16. Compared with CA-SWIS, IA-SWIS could obtain more carbon sources with a carbon/nitrogen ratio of 12, which improved N2O transforming to N2. The concentrations of and TN in the effluent were 0.8 and 6.9 mg/L for IA-SWIS, which exhibited significantly lower than that in CA-SWIS (P < 0.05). The result indicated that denitrification converted more to N2 in IA-SWIS with a carbon/nitrogen ratio of 12. The effluent concentrations of and TN were 1.3 and 7.2 mg/L for CA-SWIS, which were significantly lower than those of IA-SWIS (P < 0.05) with a carbon/nitrogen ratio of 16. More carbon sources were provided after higher efficient nitrification in CA-SWIS with a carbon/nitrogen ratio of 16 in comparison with IA-SWIS, which reduced N2O emission and converted more to N2 in CA-SWIS.

A carbon/nitrogen ratio of 12 and 16 were separately proposed for IA-SWIS and CA-SWIS in consideration of CH4 and N2O emission.

Effects of aeration mode and carbon/nitrogen ratio on bacteria and functional genes

The primary degradation pathways of organics in SWISs involve bacterial oxidation and methanogenic anaerobic oxidation, resulting in the production of CO2 and CH4 as major end products (Chen et al. 2020). The abundances of bacterial 16S rRNA and mcrA gene could represent the richness of bacteria and methanogen, respectively (Jia et al. 2019). Nitrogen removal mainly depends on nitrification and denitrification processes, which are implemented by nitrifying bacteria and denitrifying bacteria, respectively (Pan et al. 2015). The amoA, nxrA genes are involved in the nitrification process and the narG, napA, nirS, nirK, norB, nosZ genes participate in the denitrification process (Pang et al. 2020). The abundances of bacterial 16S rRNA, mcrA and functional genes of nitrification and denitrification processes are taken as denary logarithms in order to distinguish conveniently, which are shown in Figure 5.
Figure 5

The abundances of bacterial 16S rRNA, mcrA, amoA, nxrA, narG, napA, nirS, nirK, norB and nosZ genes in IA-SWIS, CA-SWIS and NA-SWIS.

Figure 5

The abundances of bacterial 16S rRNA, mcrA, amoA, nxrA, narG, napA, nirS, nirK, norB and nosZ genes in IA-SWIS, CA-SWIS and NA-SWIS.

Close modal

In NA-SWIS, IA-SWIS and CA-SWIS, the bacterial 16S rRNA abundances decreased with matrix depth increasing, which complied with the same trend of matrix oxygen concentration. In NA-SWIS, the bacterial 16S rRNA abundances at 0.6 m depth decreased with the carbon/nitrogen ratio increasing because of insufficient oxygen supply. In contrast, the bacterial 16S rRNA abundances at 0.6 m depth increased with the carbon/nitrogen ratio increasing in IA-SWIS and CA-SWIS. With the same carbon/nitrogen ratio, the bacterial 16S rRNA abundances in IA-SWIS and CA-SWIS were significantly higher than those in NA-SWIS at 0.6 m depth (P < 0.05), which could interpret higher organics removal and more CO2 emission in aeration SWISs. Aeration supplied excess oxygen and a high carbon/nitrogen ratio provided more organic substrate for bacteria which promoted bacterial growth and reproduction (Pan et al. 2015). The bacterial 16S rRNA abundances in CA-SWIS were higher than those in IA-SWIS at 0.6 m depth because of more oxygen supplied by continuous aeration with carbon/nitrogen ratio of 12 and 16.

In aeration and non-aeration SWISs, the mcrA abundances increased with matrix depth increasing, which was opposite the tendency of matrix oxygen. The mcrA abundances at 0.6, 0.9 and 1.2 m depths increased with carbon/nitrogen ratio increasing in NA-SWIS. With carbon/nitrogen ratio increasing, methanogen could acquire more organics and the oxygen supply became insufficient, which helped to methanogen. The mcrA abundances in NA-SWIS were significantly higher than those in IA-SWIS and CA-SWIS with the same depth and carbon/nitrogen ratio (P < 0.05), which accorded with CH4 emission. CH4 emission rate was positively correlated with the mcrA abundance (Morris et al. 2014). There were no significant differences between the mcrA abundances in CA-SWIS and IA-SWIS with the same depth and carbon/nitrogen ratio in this study (P > 0.05).

In NA-SWIS, IA-SWIS and CA-SWIS, the amoA and nxrA abundances decreased with matrix oxygen decreasing. In NA-SWIS, the amoA and nxrA abundances at 0.6 m depth decreased with carbon/nitrogen ratio increasing because of insufficient oxygen supply, which was in accordance with removal. In IA-SWIS and CA-SWIS, the amoA and nxrA abundances were not significantly different with carbon/nitrogen ratio of 4 and 8 due to enough oxygen supply (P > 0.05). The amoA and nxrA abundances were hardly affected by aeration mode. However, the amoA and nxrA abundances decreased when carbon/nitrogen ratio increased from 8 to 12 and 16. High available organics restricted the nitrification process in SWISs with/without aeration (Song et al. 2016; Li et al. 2018). The amoA and nxrA abundances at 0.6 m depth of IA-SWIS and CA-SWIS were significantly higher than those of NA-SWIS (P < 0.05) due to aeration, which followed removal.

In NA-SWIS, the narG, napA, nirK, nirS, norB and nosZ abundances at 0.9 and 1.2 m depths decreased with carbon/nitrogen ratio increasing. Nitrification reaction was constrained with carbon/nitrogen ratio increasing, which led to insufficient for denitrification and decreased the enrichment of six functional genes of the denitrification process. When carbon/nitrogen ratios were 4 and 8, the abundances of six functional genes in NA-SWIS at 0.9 and 1.2 m depths were higher than those in IA-SWIS and CA-SWIS. Carbon source insufficient with low carbon/nitrogen ratio in aeration SWISs decreased the abundances of six functional genes. In aeration, SWISs, the abundances of six functional genes were significantly higher than those in NA-SWIS at 0.9 and 1.2 m depths with carbon/nitrogen ratio of 12 and 16 (P < 0.05), which could clarify excellent TN removal and N2O emission in IA-SWIS and CA-SWIS with high carbon/nitrogen ratio. In this study, aeration improved nitrification efficiency and a high carbon/nitrogen ratio provided more carbon source for denitrification, which enhanced the narG, napA, nirK, nirS, norB and nosZ abundances with carbon/nitrogen ratios of 12 and 16.

Effects of aeration mode and carbon/nitrogen ratio on bacteria community

Table 2 shows the alpha diversity of different depth matrices in three SWISs. The Chao1 and Shannon indexes reflected the bacterial species richness and bacterial community diversity, respectively (Chen et al. 2021b). The higher Chao1 and Shannon values indicated higher species richness and community diversity in matrix samples. The Chao1 and Shannon values of CA-SWIS and IA-SWIS were significantly higher than those of NA-SWIS, which indicated that higher bacterial species richness and community diversity were achieved in CA-SWIS and IA-SWIS. The facilitated proliferation of bacteria in CA-SWIS and IA-SWIS was attributed to aeration. The richness and diversity of bacteria decreased with the depth increasing in three SWISs. Yang et al. (2021) drew the same conclusion that more bacterial species and higher bacterial community diversity were found in aerobic conditions than anoxic/anaerobic conditions in SWISs.

Table 2

Alpha diversity of bacterial community in three SWISs with different carbon/nitrogen ratios

NA-SWIS
CA-SWIS
IA-SWIS
0.6 m0.9 m1.2 m0.6 m0.9 m1.2 m0.6 m0.9 m1.2 m
Chao1 
Carbon/nitrogen ratio 1,558.32 1,052.54 998.23 2,567.42 1,682.44 1,523.74 2,436.56 1,688.05 1,765.24 
1,306.58 1,123.02 1,002.56 2,483.96 1,776.23 1,504.36 2,561.08 1,700.98 1,605.07 
12 942.24 658.47 667.55 2,623.25 1,756.17 1,865.47 2,619.24 1,854.27 1,800.22 
16 516.41 642.11 634.82 2,778.64 1,825.05 1,707.24 2,596.13 1,788.24 1,658.15 
Shannon 
Carbon/nitrogen ratio 7.81 6.75 6.57 9.63 7.89 7.72 9.12 7.83 8.02 
7.45 6.81 6.40 9.26 7.96 7.68 9.54 7.92 7.95 
12 6.84 6.03 6.21 9.75 7.95 8.41 9.68 8.56 8.22 
16 6.52 5.94 5.75 9.81 8.28 7.92 9.59 8.07 7.86 
NA-SWIS
CA-SWIS
IA-SWIS
0.6 m0.9 m1.2 m0.6 m0.9 m1.2 m0.6 m0.9 m1.2 m
Chao1 
Carbon/nitrogen ratio 1,558.32 1,052.54 998.23 2,567.42 1,682.44 1,523.74 2,436.56 1,688.05 1,765.24 
1,306.58 1,123.02 1,002.56 2,483.96 1,776.23 1,504.36 2,561.08 1,700.98 1,605.07 
12 942.24 658.47 667.55 2,623.25 1,756.17 1,865.47 2,619.24 1,854.27 1,800.22 
16 516.41 642.11 634.82 2,778.64 1,825.05 1,707.24 2,596.13 1,788.24 1,658.15 
Shannon 
Carbon/nitrogen ratio 7.81 6.75 6.57 9.63 7.89 7.72 9.12 7.83 8.02 
7.45 6.81 6.40 9.26 7.96 7.68 9.54 7.92 7.95 
12 6.84 6.03 6.21 9.75 7.95 8.41 9.68 8.56 8.22 
16 6.52 5.94 5.75 9.81 8.28 7.92 9.59 8.07 7.86 

Figure 6 shows the relative abundance of bacterial species at different depths in three SWISs at the phylum level with influent carbon/nitrogen ratios of 4 (a), 8 (b), 12 (c) and 16 (d), respectively. The relative abundances over 1% were Proteobacteria, followed by Actinobacteria, Acidobacteria, Chloroflexi, Gemmatimonadetes, Planctomycetes, Bacteroidetes and Firmicutes, which accorded with previous reports (Jia et al. 2019; Chen et al. 2021b; Yang et al. 2021). Moreover, these eight phyla accounted for more than 95% at different depths in each SWIS when the influent carbon/nitrogen ratio was 4, 8, 12 and 16. Proteobacteria were the main bacteria in wastewater treatment systems, which played a key role in COD and nitrogen removal (Hassan et al. 2019). The relative abundance of Proteobacteria exhibited the highest proportion, surpassing 50% in this study. Actinobacteria had been deemed as a heterotrophic nitrifier which dominated in brown soil due to rich organic substances. The relative abundances of Actinobacteria at 0.6 m depth in CA-SWIS and IA-SWIS were significantly higher than those in NA-SWIS (P < 0.05), which could explain high removal in CA-SWIS and IA-SWIS. Aeration enhanced Actinobacteria relative abundance. Heterotrophic nitrifier positively correlated with removal and nitrifying enzyme activity (Pan et al. 2015; Sun et al. 2018). Acidobacteria as a representative taxonomic group in wastewater infiltration systems had no significant difference among the three SWISs. Chloroflexi, Gemmatimonadetes, Bacteroidetes and Firmicutes played an important role in the partial nitrification anammox and denitrification process (Jia et al. 2019). With carbon/nitrogen ratio was 12 and 16, the relative abundances of Chloroflexi, Gemmatimonadetes, Bacteroidetes and Firmicutes at 0.9 and 1.2 m depths in CA-SWIS and IA-SWIS were significantly higher than those in NA-SWIS (P < 0.05), which were in accordance with TN removal. Planctomycetes were a key population in the whole autotrophic deamination process (Delmont et al. 2018). The relative abundances of Planctomycetes were not significantly difference among the three SWISs.
Figure 6

Relative abundance of bacterial community at the phylum level in three SWISs with influent carbon/nitrogen ratio of 4 (a), 8 (b), 12 (c) and 16 (d)

Figure 6

Relative abundance of bacterial community at the phylum level in three SWISs with influent carbon/nitrogen ratio of 4 (a), 8 (b), 12 (c) and 16 (d)

Close modal

The aeration treatment effectively developed an aerobic environment in the matrix above 0.6 m, while maintaining an anoxic/anaerobic environment below 0.9 m. The aeration mode and carbon/nitrogen ratio exerted significant influences on the removal of organic compounds, nitrogen, CO2, CH4 and N2O emissions, as well as the composition of bacterial communities. COD, , TN removal efficiencies, CO2 and N2O conversion efficiencies decreased and CH4 emission increased with carbon/nitrogen ratio increasing in non-aeration SWIS. With high carbon/nitrogen ratio of 12 and 16, aeration improved COD, , TN removal, the bacterial 16S rRNA, amoA, nxrA, narG, napA, nirK, nirS, norB, nosZ abundances, bacterial community Alpha diversity, the relative abundances of Actinobacteria at 0.6 m depth, the relative abundances of Chloroflexi, Gemmatimonadetes, Bacteroidetes and Firmicutes at 0.9 and 1.2 m depths and decreased CH4 and N2O conversion efficiencies, the mcrA abundances in IA-SWIS and continuous aeration SWIS compared with those in non-aeration SWIS. In consideration of the removal efficiencies for organics, nitrogen and CH4 and N2O conversion, carbon/nitrogen ratios of 4 and 8 are recommended for non-aeration SWIS. For IA-SWIS and continuous aeration SWIS, carbon/nitrogen ratios of 12 and 16 are proposed, respectively.

We gratefully thank the financial support from the Applied Basic Research Plan of Liaoning (2023JH2/101300053); Science and Technology Plan of Shenyang (21-108-9-36), Basic Research Plan of Liaoning Education Department (2023), Major Original Program in Shenyang Normal University (ZD201904), and The Ninth Batch of Education and Teaching Reform Project of Shenyang Normal University (JG2021-YB099).

L. Z. investigated the work, wrote the article and prepared the original draft. Z. C. developed the methodology, investigated the article and rendered support in data curation. B. Y. investigated the work and revised the article. Z. L. investigated the article and rendered support in data curation. J. P. wrote the review and edited the article, rendered support in funding acquisition and visualized the article.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

Chen
H.
,
Gan
Q. L.
&
Fan
C. G.
2020
Methyl-coenzyme M reductase and its post-translational modifications
.
Frontiers in Microbiology
11
,
578356
.
Delmont
T. O.
,
Quince
C.
,
Shaiber
A.
,
Esen
O. C.
,
Lee
S. T. M.
&
Lucker
S.
2018
Nitrogen-fixing populations of Planctomycetes and Proteobacteria are abundant in surface ocean metagenomes
.
Nature Microbiology
3
,
804
813
.
Fan
J. L.
,
Zhang
B.
,
Zhang
J.
,
Ngo
H. H.
,
Guo
W. S.
&
Liu
F. F.
2013
Intermittent aeration strategy to enhance organics and nitrogen removal in subsurface flow constructed wetlands
.
Bioresource Technology
141
,
117
122
.
Jia
L. P.
,
Jiang
B. H.
,
Huang
F.
&
Hu
X. M.
2019
Nitrogen removal mechanism and microbial community changes of bioaugmentation subsurface wastewater infiltration system
.
Bioresource Technology
294
,
122
140
.
Li
Y. H.
,
Li
H. B.
,
Yang
L.
,
Xu
X. Y.
,
Wang
S. Q.
&
Su
F.
2019
Study on the contribution of different depth layers to N2O emission in subsurface wastewater infiltration system
.
Ecological Engineering
133
,
69
75
.
Li
Y. H.
,
Wang
S. Q.
,
Li
H. B.
,
Fang
Y. T.
,
Yang
L.
&
Su
F.
2020
Contribution of co-denitrification to nitrous oxide production from subsurface wastewater infiltration system
.
Ecological Engineering
151
,
105854
.
Maucieri
C.
,
Barbera
A. C.
,
Vymazal
J.
&
Borin
M.
2017
A review on the main affecting factors of greenhouse gases emission in constructed wetlands
.
Agricultural and Forest Meteorology
236
,
175
193
.
Pan
J.
,
Fei
H. X.
,
Song
S. Y.
,
Yuan
F.
&
Yu
L.
2015
Effects of intermittent aeration on pollutants removal in subsurface wastewater infiltration system
.
Bioresource Technology
191
,
327
331
.
Sabba
F.
,
Picioreanu
C.
,
Pérez
J.
&
Nerenberg
R.
2015
Hydroxylamine diffusion can enhance N2O emissions in nitrifying biofilms: A modeling study
.
Environmental Science and Technology
49
,
1486
1494
.
Song
S. Y.
,
Pan
J.
,
Wu
S. W.
,
Guo
Y. J.
,
Yu
J. X.
&
Shan
Q. X.
2016
Effects of COD/N ratios on pollutants removal in the subsurface wastewater infiltration systems with/without intermittent aeration
.
Water Science and Technology
187
,
14
22
.
Standard Method for the Examination of Water and Wastewater Editorial Board
.
2002
Standard Method for the Examination of Water and Wastewater
, 4th edn.
Environmental Science Press of China
,
Beijing, China
.
Sun
J.
,
Chen
L.
,
Rene
E. R.
,
Hu
Q.
,
Ma
W.
&
Shen
Z.
2018
Biological nitrogen removal using soil columns for the reuse of reclaimed water: Performance and microbial community analysis
.
Journal of Environmental Management
217
,
100
109
.
Yang
F.
,
Li
G. X.
,
Zang
B.
&
Zhang
Z. Y.
2017
The maturity and CH4, N2O, NH3 emissions from vermicomposting with agricultural waste
.
Compost Science and Utilization
25
,
262
271
.

Author notes

These authors contributed equally to this study and share first authorship.

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