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Article

Black Plastic Film Mulching Increases Soil Nitrous Oxide Emissions in Arid Potato Fields

1
Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
2
Center for Agricultural Water Research in China, China Agricultural University, Beijing 100083, China
3
China Institute of Water Resources and Hydropower Research, Beijing 100048, China
*
Author to whom correspondence should be addressed.
Int. J. Environ. Res. Public Health 2022, 19(23), 16030; https://doi.org/10.3390/ijerph192316030
Submission received: 5 November 2022 / Revised: 20 November 2022 / Accepted: 28 November 2022 / Published: 30 November 2022
(This article belongs to the Special Issue Greenhouse Gas Reduction)

Abstract

:
Black plastic film mulching is a common practice for potato production in the arid area of Northwest China. Many studies have reported the significant positive effect of black plastic film mulch on potato harvest, while the effect of black plastic film mulch treatment on soil nitrous oxide (N2O) emissions is still unclear. As a consequence, this study aimed to examine the effect of black plastic film mulch treatment on N2O emission from arid upland potato fields. With the static chamber-gas chromatography method, soil N2O emissions were measured. The results showed that black plastic film mulching treatment significantly increased cumulative soil N2O emissions by 21–26% compared with non-mulched treatment. Cumulative N2O emission positively correlated with soil temperature, soil moisture, soil CO2 concentration, and amoA-AOB abundance. This study indicated that black plastic film mulching, mainly through increasing soil temperature and soil moisture, increasing soil carbon dioxide (CO2) concentration, and promoting the abundance of nitrification-related functional gene of amoA-AOB, regulated N2O emissions. This study also highlighted that the specific soil environment under black plastic film mulch is conducive to N2O emissions and lay the foundation for settling the contradiction between food production and greenhouse gas mitigation in upland soils. The negative effects of black plastic film mulching on the environment should be considered in future applications in food production.

1. Introduction

Nitrous oxide (N2O), with 296 times the global warming potential of carbon dioxide within the 100-year time frame [1], has increased by 122% of the pre-industrial level to 329.9 ± 0.1 ppb [2]. Agricultural N2O emission is a tremendous global concern, given that agricultural soils contribute 60% of the global anthropogenic N2O emissions [3,4]. Potato is the fourth staple food with a 19.3 Mha harvest area worldwide [5]. Potato fields can potentially contribute to global N2O emissions.
Black plastic film mulching, a soil temperature retention soil surface management practice, has been widely used [6,7]. Mulching treatment can significantly enhance potato growth and harvest. One of our previous studies indicated that black plastic film mulch could enhance potato harvest by 6–30% [8], while few studies have paid attention to the effect of mulching on N2O emissions in arid and semi-arid potato fields. Soils covered with black plastic film mulch had higher soil temperatures compared to non-mulched soils in potato fields [9]. Mulching has been reported to significantly increase N2O emissions in the radish field owing to higher temperatures [10]. An exponential relationship between N2O flux and the soil temperature has been observed at 0 to 30 °C, while warming can also inhibit nitrification-induced N2O emission when soil temperature is over 30 °C [11]. Additionally, extremely high soil surface temperature (>30 °C) under plastic film mulching has been recorded from 10:00 a.m. to 6:00 p.m. during sprout development and vegetative growth stages in an arid potato field experiment [12]. Plastic film mulching could also reduce cumulative N2O emissions, which may contribute to the unsuitable soil temperature for N2O emission under mulching [13]. The uncertain effect of black plastic film mulching on N2O emission makes it urgent to investigate how this agronomic practice affects N2O emission in arid potato fields.
Compared to non-mulched treatment, black plastic film mulching could only insignificantly reduce N2O emissions owing to lower soil moisture if there is no irrigation during cultivation [10], while black plastic film mulching is always applied with drip irrigation in arid and semi-arid potato filed. In the black plastic film mulching–drip irrigation system, black plastic film mulch could maintain soil moisture at the 0–100 cm soil layer by reducing soil evaporation [14,15]. Topsoil moisture under black plastic film mulch was generally higher than that under non-mulched soil during the whole growing period [16,17]. On the other hand, nitrification and denitrification are two important pathways for N2O production and were mainly driven by nitrification-related microorganisms (amoA-AOA and amoA-AOB) and denitrification-related microorganisms (nirS and nirK) [18,19]. Soil moisture generally regulates the main microorganisms for N2O production. Nitrification can be an important pathway leading to N2O production when soils were incubated in 60% WFPS, and amoA-AOB would play a key role in N2O production [20]. Di suggested that soil moisture had a major influence on ammonia-oxidizing and denitrifying microbial communities and then regulating N2O emissions [19]. Denitrification-related communities (nirS and nirK) and amoA-AOB are reported to be able to grow under very wet soil conditions (130% field capacity) and produce N2O emissions [19]. Therefore, with a higher soil moisture condition under black plastic film, both nitrification and denitrification-related microorganisms may both play an important role in N2O, or denitrification-related microorganisms will dominate N2O emission. While previous studies paid more attention to the abiotic parameters regulating the effect of black plastic film mulch on soil N2O emissions, less attention has been paid to N2O-related microorganisms under plastic film mulch.
We hypothesized that black plastic film mulching could increase N2O emission by increasing soil temperature and moisture, as well as N2O-related microorganisms. We also hypothesized that both nitrification- and denitrification-related microorganisms will increase under mulching treatment leading to a higher N2O emission. This study aimed to (1) explore the effect of black plastic film mulching on soil N2O emission in the arid potato field, and (2) reveal the mechanisms of how black plastic film mulching affects soil N2O emission through regulating soil abiotic and biotic parameters.

2. Materials and Methods

2.1. Field Experimental Design

The field experiments were conducted in 2017 and 2018 at Shiyanghe Experimental Station in Gansu Province, China (37°52′ N, 102°50′ E, 1581 m a.s.l.). The region has a continental temperate climate. The mean annual temperature and precipitation are 8.8 °C and 164 mm, respectively. Daily air temperature and precipitation during the experiment are shown in Figure S1. The soil at the site is a sandy loam soil (9.1% clay, 31.3% silt, and 59.6% sand) with a pH of 8.2, a field capacity of 0.26 cm3/cm3, a bulk density of 1.56 g/cm3 and a total soil porosity of 41%. Other basic soil properties before the experiment are given in Table S1.
The experimental design was a randomized block design with three replicated plots (5 m × 5.6 m) for each treatment. Each plot had seven isosceles trapezoid ridges and each ridge had a length of 5 m, a width of 0.8 m, and a height of 0.3 m. Treatment of soil covered with (MC) or without (CK) black plastic mulch was settled. The black plastic film mulch was high-density and airtight with 0.008 mm in thickness, and covered soils before potato seeds plantation. The plastic film mulch was perforated for the transplantation of potato seeds. All plots were irrigated by an irrigation system as described in our previous studies [8,21]. Briefly, plots were irrigated when soil volumetric moisture content at 20 cm soil depth declined to 70% (v/v) of the field capacity [21]. Soil volumetric moisture contents were monitored by moisture sensors (introduced in Section 2.2). The amount of water irrigated for one irrigation event was 21 mm. Plots of MC treatment were irrigated 21 and 19 times in 2017 and 2018, respectively. Plots of CK treatment were irrigated 24 and 21 times in 2017 and 2018, respectively. All plots received the same fertilizer according to local management, and the fertilization strategies and other agronomic practices are shown in Table S2.

2.2. Soil Temperature and Moisture Measurement

Soil temperatures at 10 cm soil depth were monitored by thermal sensors (200TS, Irrometer Co., Inc., Riverside, CA, USA), and soil volumetric moisture at 20 cm soil depth was monitored by soil moisture sensors (200SS, Irrometer Co., Inc., Riverside, CA, USA). The data logger (900M, Irrometer Co., Ltd., Riverside, CA, USA) recorded the data every 10 min. The following equation calculated water-filled pore space (WFPS):
W F P S = v o l u m e t r i c   m o i s t u r e   c o n t e n t t o t a l   s o i l   p o r o s i t y
where total soil porosity is 41%.

2.3. N2O Flux Sampling

Fluxes of N2O were measured by a static opaque chamber-gas chromatography method (Supplementary Method). Briefly, a stainless-steel frame was inserted 5 cm into the soil of one ridge in each plot and included soil and two crops. An opaque polymethyl methacrylate chamber was placed on the pre-installed stainless-steel frames. Five gas samples were collected to calculate N2O flux around 9 a.m. after chamber closure, at a time interval of 4 min about every 5 days. Gas samples were then kept in pre-vacuumed plastic gasbags (Dalian Pulaite gas packing Co., Ltd., Dalian, China) and analyzed for the N2O concentration using a gas chromatograph (GC-2014 series, Shimadzu (China) Co., Ltd., Beijing, China) equipped with an electron capture detector (ECD). The column (SS-2 m × 4 mm Porapak Q (80/100)) and ECD temperatures were maintained at 60 °C and 300 °C, respectively.
Diurnal N2O flux samples were collected every 4–6 h over three days at early, middle, and later growth stages in both experimental years to identify the effect of MC treatment on N2O flux by alternating soil temperature (Supplementary Method). Flux samples between two irrigation events were also collected every day to identify the relationship between N2O flux and soil moisture (Supplementary Method).
Fluxes were calculated with linear function from the change of gas concentration in the chamber during the sampling period by the following equation [21]:
F = H m p R ( 273 + T ) C t
where F is the N2O flux (μg m−2 min−1); H is the height of chamber (m); m is the molecular weight of N2O (g mol−1); p is the atmospheric pressure (kPa); R is the value of the universal constant; T is the air temperature in the chamber (°C); C / t is the change of gas concentration in the chamber during the sampling period (μ mol min−1).
Cumulative N2O emissions were calculated by trapezoidal integration [22].

2.4. Soil Gas (CO2 and N2O) Sampling

A soil–air equilibration sampler was installed vertically in the soil to a soil depth of 15–20 cm (Supplementary Method and Figure S2). We extracted 20 mL of gas samples between 10:00 a.m. and 10:30 a.m. after soil N2O flux sampling, using a syringe through a three-way stopcock connecting with the silicon tube. Gas samples were then kept in pre-vacuumed plastic gasbags (Dalian Pulaite gas packing Co., Ltd., Dalian, China) and analyzed for the N2O concentration using a gas chromatograph. The three-way stopcock of the sampler was closed on non-sampling days to avoid the connection of soil air to atmospheric air.

2.5. DNA Extraction and Quantitative PCR

Soil samples were collected at the harvest time in 2018 and stored at −80 °C for subsequent DNA extraction and quantitative PCR analysis. Soil DNA was extracted using 0.5 g soil according to the manufactory’s protocol with a Fast DNA Spin Kit for Soil (MP Biomedicals, Eschwege, Germany). Copy numbers of amoA-AOA, amoA-AOB, nirS, and nirK genes were determined by quantitative PCR assays. The primers and thermal cycling conditions are given in Table S3.

2.6. Statistical Analysis

The effects of black plastic film mulching treatment on cumulative N2O emission, soil temperature, WFPS, and N2O-related gene numbers were analyzed by analysis of variance (ANOVA) for the least significant differences (LSD) at p < 0.05 level. Differences in cumulative N2O emission, soil temperature, WFPS, and N2O-related gene numbers between black plastic film mulching treatment and non-mulched treatment were analyzed by ANOVA for LSD at p < 0.05 level. The above statistical analyses were evaluated by SPSS (IBM SPSS statics version 24.0, SPSS Inc., Chicago, IL, USA). Graph drawing and regression models of soil N2O responding to soil abiotic and biotic parameters were performed by Origin and R language.

3. Results

3.1. N2O Flux and Soil Temperature

Nitrous oxide fluxes first increased and then decreased for both treatments from 8:00 a.m. to 8:00 a.m. on another day (Figure 1a–f). MC treatment significantly (p < 0.05) affected daily average N2O fluxes on all typical days, and significantly increased daily average N2O fluxes by 17–100% (Table S4).
Diurnal soil temperatures on typical days changed by a single-peak pattern (Figure 1g–l). MC treatment significantly (p < 0.05) promoted soil temperatures on typical days and significantly increased daily average N2O fluxes by 1.8–2.7 °C (Table S4).
There is a quadratic relationship between N2O emission rates and soil temperatures at the middle and later growth stages (Figure 1B,C). The N2O emission rate reached the greatest at about 25 and 29 °C at the middle and later growth stage, respectively. No significant relationship between N2O flux and soil temperature was found at the early growth stage (Figure 1A).

3.2. Soil N2O Flux Variation between Two Irrigation Events

Soil N2O fluxes changed with a decreasing trend after the irrigation event except fluxes measured on 26–30 July (Figure 2). N2O fluxes from 26 to 30 July changed with a flat trend.
WFPS reached the field capacity after the irrigation event and declined to about 70% (v/v) of the field capacity before the next irrigation event (Figure 2 and Figure S5). Meanwhile, WFPS in MC treatment declined slower than in CK treatment after irrigation (Figure S5).
Soil N2O flux had a positive linear correlation (p < 0.05) with WFPS (Figure 2c,f). Fluxes of N2O increased with the increase of WFPS when WFPS changed within a range of 39–62%.

3.3. Soil Gas Variation

Soil CO2 showed a firstly increasing and then decreasing pattern with two peaks during the experiments (Figure 3). Topdressing brought about a small CO2 peak in both experimental years. MC treatment had higher soil CO2 than CK treatment. Across two years, average soil CO2 concentrations were 5.3–5.9 × 103 and 3.5–4.0 × 103 ppm for MC and CK, respectively.
Soil N2O concentration variation for MC and CK treatments were similar during the experiment, with clear patterns of increasing occurring following the topdressing and decreasing after several days after topdressing (Figure 3). MC treatment had the higher average soil N2O concentrations than CK treatment, being 1.7 (MC) and 1.0 (CK) ppm in 2017 and 3.3 (MC) and 3.1 (CK) ppm in 2018, respectively.
Soil N2O concentrations increased as soil CO2 concentrations increased, and this response was best fitted by an exponential model (Figure 3). Soil CO2 could explain 44–92% of the variance in soil N2O concentrations regarding the correlations between soil C2O and soil N2O (Figure 3).

3.4. Soil N2O-Related Microbial Genes

Black plastic film mulching significantly affected amoA-AOB (Figure 4 and Table 1). The abundance of the amoA-AOB gene was 3.76 × 108 and 3.12 × 108 copies per gram of soil for MC and CK treatment, respectively. The abundance of amoA-AOB increased by 21% under MC treatment, compared with the value under CK treatment. No significant difference in the abundance of amoA-AOA, nirS, and nirK genes between MC and CK treatment.

3.5. Seasonal N2O Fluxes

Fluxes of N2O changed with fluctuations, and MC treatment had higher N2O fluxes than CK during the study periods (Figure 5). MC treatment significantly (p < 0.05) affected cumulative N2O fluxes (Figure 5 and Table 1). Over two study years, MC treatment increased cumulative N2O emission by 21–26%.
The cumulative N2O flux was positively correlated with soil temperature, soil WFPS, soil CO2 concentrations, soil N2O concentrations, and amoA-AOB gene abundance, while negatively correlated with irrigation times (Figure 6).

4. Discussion

The effect of black plastic film mulching (MC) treatment on N2O emission differs based on previous studies. Studies indicated that MC treatment increased [23], reduced [10,13], or did not affect [24,25] N2O emissions compared with non-mulched treatment. The influence of MC treatment on soil environmental conditions varying with the experimental sites could be the reason for the controversial results. Zhao [10] suggested MC treatment reduced N2O emissions in the hot pepper season owing to lower soil moisture. Reduction of the available mineral N due to the enhanced N uptake of plants would be another reason for the limiting of nitrification and denitrification processes under black plastic film mulching [13]. On the other hand, N2O emissions may not differ between the mulched and non-mulched fields, mainly because film mulching did not affect the soil temperature due to the cooling effect of irrigation [25]. While consistent with Yu [13] and Gao [26], our results showed that MC treatment significantly increased N2O emissions, mainly through regulating biotic (amoA-AOB) and abiotic (soil temperature, soil moisture, and soil CO2 concentrations) parameters (Figure 6).
In this study, N2O emissions had a quadratic relationship with soil temperatures during the 24-h measurement (Figure 1B,C), and cumulative N2O emissions also showed a positive relationship with average soil temperatures across two experimental years (Table 1, Figure S3 and Figure 6). Our results indicated that soil temperature was a vital abiotic regulator of soil N2O emission. The failure to find a correlation between N2O flux and soil temperature at the early growth stage (Figure 1A) may be attributed to the lower sensitivity of N2O-related microorganisms to soil temperature when sufficient nutrients in soils at the early growth stage [27]. Zhao [10] indicated that N2O emissions could increase with the increase of soil temperature (from 5 to 32 °C), while we found N2O emissions might decrease when soil temperature was above 25–29 °C at middle and later growth stages (Figure 1B,C). Similar results had been reported that N2O emissions would be inhibited when soil temperature was above 30 °C [11]. Soil N2O emissions could be potentially inhibited by black plastic film mulching for extremely high temperatures. Moreover, from the perspective of cumulative N2O emissions during the whole growing season, the positive effect outweighed the negative one of mulching–induced warming on cumulative N2O emissions. The positive linear correlation between cumulative N2O emission and average soil temperature (Figure 6) could support this inference.
Soil moisture was another primary factor affecting N2O emissions. MC treatment could significantly increase soil moisture, which has been reported by lots of studies [8,21]. We also found soil N2O emissions had a positive correlation with WFPS (from 39% to 62%) (Figure 2), which was consistent with that of Zhao [10]. Zhao indicated that the N2O emission rate was exponentially correlated with WFPS when WFPS varied from 20% to 80% [10]. Results also showed that average WFPS had a positive linear correlation with cumulative N2O emissions, which supports our inference that higher soil moisture under MC would be conducive to N2O production. On the other hand, soil moisture was observed to decrease more rapidly after irrigation under CK treatment (Figure S5), which indicated that soil humidity would retain at a higher level for N2O production for a longer time under MC treatment.
As reported that the denitrification process produced the greatest N2O at 70 to 90% WFPS [28], the nitrification process might domain N2O productions in this study (Figure S4). Ammonia oxidation is the first and rate-limiting step in nitrification, and it is catalyzed by an ammonia monooxygenase (AMO) encoded in gene amoA of AOA and AOB [29]. Although several studies have reported amoA-AOA to play an important role in nitrification [29,30], results in this study showed that MC treatment only significantly enhanced the abundance of amoA-AOB (Table 1 and Figure 4), and amoA-AOB abundances were positively correlated with cumulative N2O emissions (Figure 6). It was AOB, not AOA or other denitrification-related microorganisms, that induced the N2O emission under MC treatment. Previous studies also indicated that amoA-AOB-induced nitrification was regarded as the key pathway for N2O production [31]. Higher amoA-AOB–dependent N2O product stoichiometry than amoA-AOA was likely due to the incomplete NH2OH oxidation and nitrifier denitrification, as previously observed in neutral/alkaline soils [31,32]. Since some amoA-AOB had genes encoding a canonical hydroxylamine dehydrogenase and NO reductase and thus could conduct nitrifier denitrification, they played a more important role in these alkaline mulched soils (Figure 6). Notably, CO2 concentrations under MC treatment were higher than those under CK, which could be attributed to that MC treatment enhancing soil microbes’ activity [33,34]. We found significant exponential correlations between soil N2O and CO2 concentrations (Figure 3), and cumulative N2O emissions were significantly correlated with soil CO2 concentrations (Figure 6). As previous studies mentioned, elevated atmospheric CO2 increased soil nitrification rate and shifted ammonia-oxidizing community abundance and structure [35,36,37]. Elevated CO2 could both significantly shift amoA-AOB and amoA-AOA communities, and amoA-AOB was more sensitive to the rising CO2 concentration [35]. We infer that high CO2 concentration under black plastic film mulching might be conducive to the growth of amoA-AOB and promote N2O emissions.
From the above analyses, it can be seen that the MC treatment plays a primary role in regulating N2O emissions. This study showed a negative impact of MC treatment on greenhouse gas mitigation. On the other hand, studies have reported a significant positive effect of MC treatment on potato harvest [8]. Therefore, further research should be devoted to examining the impacts of MC treatment on both potato harvests and N2O emissions.

5. Conclusions

This study used the static chamber-gas chromatography method to evaluate the effect of black plastic film mulch treatment on soil N2O emission in the arid potato field. Our results demonstrated that black plastic film mulch treatment can significantly increase soil cumulative N2O emission. We identified that black plastic film mulching promoted soil N2O emissions mainly by altering abiotic parameters including increasing soil temperatures, soil moisture, and soil CO2 concentrations. We also highlighted that it was amoA-AOB, but not other N2O-related microorganisms that regulated N2O emission under plastic film mulching. Further research should be devoted to examining the impacts of black plastic film mulch treatment on greenhouse gas emissions apart from food production.

Supplementary Materials

The following supporting information can be downloaded at: https://www.mdpi.com/article/10.3390/ijerph192316030/s1, Supplementary Methods; Supplementary Results; Table S1: Soil properties of the top 20 cm soil before experiment; Table S2: Fertilization and agronomic practice in this study. Table S3: Primers and thermal cycling conditions used for quantitative PCR; Table S4: Daily average N2O fluxes and daily average soil temperatures as affected by black plastic film mulching treatment on typical days in 2017 and 2018; Figure S1: Dynamics of air temperature and precipitation during the experiment; Figure S2: Schematic diagram of the soil-air equilibration tube; Figure S3: Daily average soil temperature at 10 cm-depth of soils covered with (MC) or without (CK) black plastic film mulch; Figure S4: Variation of WFPS at 20 cm-depth of soils covered with (MC) or without (CK) black plastic film mulch; Figure S5: WFPS at 20 cm-depth of soils covered with (MC) or without (CK) black plastic film mulch between two irrigation events. References [38,39,40,41,42,43] are cited in Supplementary Materials.

Author Contributions

Conceptualization, C.M. and F.W.; data curation, C.M. and J.Z.; formal analysis, C.M. and K.Y.; funding acquisition, F.W.; investigation, C.M. and N.W.; methodology, C.M. and K.Y.; resources, F.W.; software, C.M. and J.Z.; supervision, F.W.; writing—original draft, C.M.; writing—review and editing, K.Y. and F.W. All authors have read and agreed to the published version of the manuscript.

Funding

Key Research Project of Science and Technology in Inner Mongolia Autonomous Region of China: NMKJXM202105-1, NMKJXM202004, and the National Natural Science Foundation of China: 52009142, 51579240.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The data presented in this study are available on request from the corresponding author.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. IPCC. Climate Change 2007: The Physical Science Basis; Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change; Solomon, S., Qin, D., Manning, M., Chen, Z., Marquis, M., Averyt, K.B., Tignor, M., Miller, H.L., Eds.; Cambridge University Press: Cambridge, UK; New York, NY, USA, 2007; 996p. [Google Scholar]
  2. WMO. WMO Greenhouse Gas Bulletin (GHG Bulletin)—No. 14: The State of Greenhouse Gases in the Atmosphere Based on Global Observations through 2017; WMO: Geneva, Switzerland, 2018. [Google Scholar]
  3. Reay, D.S.; Davidson, E.A.; Smith, K.A.; Smith, P.; Melillo, J.M.; Dentener, F.; Crutzen, P.J. Global agriculture and nitrous oxide emissions. Nat. Clim. Chang. 2012, 2, 410–416. [Google Scholar] [CrossRef]
  4. IPCC. Climate Change 2007: Mitigation; Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change; Metz, B., Davidson, O.R., Bosch, P.R., Dave, R., Meyer, L.A., Eds.; Cambridge University Press: Cambridge, UK; New York, NY, USA, 2007. [Google Scholar]
  5. FAO. FAOSTAT Online Database. Food and Agriculture Organization of the United Nations. Available online: http://www.fao.org/faostat/en/#data/RA (accessed on 3 November 2022).
  6. Li, Q.; Li, H.; Zhang, L.; Zhang, S.; Chen, Y. Mulching improves yield and water-use efficiency of potato cropping in China: A meta-analysis. Field Crop Res. 2018, 221, 50–60. [Google Scholar] [CrossRef]
  7. Ramakrishna, A.; Tam, H.M.; Wani, S.P.; Long, T.D. Effect of mulch on soil temperature, moisture, weed infestation and yield of groundnut in northern Vietnam. Field Crop Res. 2006, 95, 115–125. [Google Scholar] [CrossRef] [Green Version]
  8. Meng, C.; Wang, F.; Engel, B.A.; Yang, K.; Zhang, Y. Is Cattle Manure Application with Plastic-Film Mulch a Good Choice for Potato Production? Agronomy 2019, 9, 534. [Google Scholar] [CrossRef] [Green Version]
  9. Wang, F.; Feng, S.; Hou, X.; Kang, S.; Han, J. Potato growth with and without plastic mulch in two typical regions of Northern China. Field Crop Res. 2009, 110, 123–129. [Google Scholar] [CrossRef]
  10. Zhao, M.; Jiang, C.; Li, X.; He, X.; Hao, Q. Variations in nitrous oxide emissions as manipulated by plastic film mulching and fertilization over three successive years in a hot pepper-radish rotated vegetable production system. Agric. Ecosyst. Environ. 2020, 304, 107127. [Google Scholar] [CrossRef]
  11. Duan, P.; Wu, Z.; Zhang, Q.; Fan, C.; Xiong, Z. Thermodynamic responses of ammonia-oxidizing archaea and bacteria explain N2O production from greenhouse vegetable soils. Soil Biol. Biochem. 2018, 120, 37–47. [Google Scholar] [CrossRef]
  12. Zhang, Y.; Wang, F.; Shock, C.C.; Yang, K.; Kang, S.; Qin, J.; Li, S. Effects of plastic mulch on the radiative and thermal conditions and potato growth under drip irrigation in arid Northwest China. Soil Tillage Res. 2017, 172, 1–11. [Google Scholar] [CrossRef]
  13. Yu, Y.; Jia, H.; Zhao, C. Evaluation of the effects of plastic mulching and nitrapyrin on nitrous oxide emissions and economic parameters in an arid agricultural field. Geoderma 2018, 324, 98–108. [Google Scholar] [CrossRef]
  14. Ding, D.; Zhao, Y.; Feng, H.; Hill, R.L.; Chu, X.; Zhang, T.; He, J. Soil water utilization with plastic mulching for a winter wheat-summer maize rotation system on the Loess Plateau of China. Agric. Water Manag. 2018, 201, 246–257. [Google Scholar] [CrossRef]
  15. Zhao, Y.; Zhai, X.; Wang, Z.; Li, H.; Jiang, R.; Hill, R.L.; Si, B.; Hao, F. Simulation of soil water and heat flow in ridge cultivation with plastic film mulching system on the Chinese Loess Plateau. Agric. Water Manag. 2018, 202, 99–112. [Google Scholar] [CrossRef]
  16. Ma, D.; Chen, L.; Qu, H.; Wang, Y.; Misselbrook, T.; Jiang, R. Impacts of plastic film mulching on crop yields, soil water, nitrate, and organic carbon in Northwestern China: A meta-analysis. Agric. Water Manag. 2018, 202, 166–173. [Google Scholar] [CrossRef]
  17. Wang, X.; Li, Z.; Xing, Y. Effects of mulching and nitrogen on soil temperature, water content, nitrate-N content and maize yield in the Loess Plateau of China. Agric. Water Manag. 2015, 161, 53–64. [Google Scholar] [CrossRef]
  18. Liu, H.; Ding, Y.; Zhang, Q.; Liu, X.; Xu, J.; Li, Y.; Di, H. Heterotrophic nitrification and denitrification are the main sources of nitrous oxide in two paddy soils. Plant Soil 2019, 445, 39–53. [Google Scholar] [CrossRef]
  19. Di, H.J.; Cameron, K.C.; Podolyan, A.; Robinson, A. Effect of soil moisture status and a nitrification inhibitor, dicyandiamide, on ammonia oxidizer and denitrifier growth and nitrous oxide emissions in a grassland soil. Soil Biol. Biochem. 2014, 73, 59–68. [Google Scholar] [CrossRef]
  20. Shi, X.; Hu, H.; Zhu-Barker, X.; Hayden, H.; Wang, J.; Suter, H.; Chen, D.; He, J. Nitrifier-induced denitrification is an important source of soil nitrous oxide and can be inhibited by a nitrification inhibitor 3,4-dimethylpyrazole phosphate. Environ. Microbiol. 2017, 19, 4851–4865. [Google Scholar] [CrossRef]
  21. Meng, C.; Wang, F.; Yang, K.; Shock, C.C.; Engel, B.A.; Zhang, Y.; Tao, L.; Gu, X. Small wetted proportion of drip irrigation and non-mulched treatment with manure application enhanced methane uptake in upland field. Agric. For. Meteorol. 2020, 281, 107821. [Google Scholar] [CrossRef]
  22. Das, S.; Adhya, T.K. Dynamics of methanogenesis and methanotrophy in tropical paddy soils as influenced by elevated CO2 and temperature interaction. Soil Biol. Biochem. 2012, 47, 36–45. [Google Scholar] [CrossRef]
  23. Kim, G.W.; Das, S.; Hwang, H.Y.; Kim, P.J. Nitrous oxide emissions from soils amended by cover-crops and under plastic film mulching: Fluxes, emission factors and yield-scaled emissions. Atmos. Environ. 2017, 152, 377–388. [Google Scholar] [CrossRef]
  24. Liu, J.; Zhu, L.; Luo, S.; Bu, L.; Chen, X.; Yue, S.; Li, S. Response of nitrous oxide emission to soil mulching and nitrogen fertilization in semi-arid farmland. Agric. Ecosyst. Environ. 2014, 188, 20–28. [Google Scholar] [CrossRef]
  25. Li, Y.; Guan, K.; Peng, B.; Franz, T.E.; Wardlow, B.; Pan, M. Quantifying irrigation cooling benefits to maize yield in the US Midwest. Global Chang. Biol. 2020, 26, 3065–3078. [Google Scholar] [CrossRef]
  26. Guo, Z.; Zhang, Y.; Zhao, J.; Shi, Y.; Yu, Z. Nitrogen use by winter wheat and changes in soil nitrate nitrogen levels with supplemental irrigation based on measurement of moisture content in various soil layers. Field Crop Res. 2014, 164, 117–125. [Google Scholar] [CrossRef]
  27. Luo, G.; Kiese, R.; Wolf, B.; Butterbach-Bahl, K. Effects of soil temperature and moisture on methane uptakes and nitrous oxide emissions across three different ecosystem types. Biogeosci. Discuss. 2013, 10, 927–965. [Google Scholar] [CrossRef] [Green Version]
  28. Lark, R.M.; Milne, A.E. Boundary line analysis of the effect of water-filled pore space on nitrous oxide emission from cores of arable soil. Eur. J. Soil Sci. 2016, 67, 148–159. [Google Scholar] [CrossRef] [Green Version]
  29. Zhang, L.M.; Hu, H.W.; Shen, J.P.; He, J.Z. Ammonia-oxidizing archaea have more important role than ammonia-oxidizing bacteria in ammonia oxidation of strongly acidic soils. ISME J. 2012, 6, 1032–1045. [Google Scholar] [CrossRef] [Green Version]
  30. Baker, B.J.; De Anda, V.; Seitz, K.W.; Dombrowski, N.; Santoro, A.E.; Lloyd, K.G. Diversity, ecology and evolution of Archaea. Nat. Microbiol. 2020, 5, 887–900. [Google Scholar] [CrossRef]
  31. Hink, L.; Nicol, G.W.; Prosser, J.I. Archaea produce lower yields of N2O than bacteria during aerobic ammonia oxidation in soil. Environ. Microbiol. 2017, 19, 4829–4837. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  32. Hink, L.; Gubry-Rangin, C.; Nicol, G.W.; Prosser, J.I. The consequences of niche and physiological differentiation of archaeal and bacterial ammonia oxidisers for nitrous oxide emissions. ISME J. 2018, 12, 1084–1093. [Google Scholar] [CrossRef] [Green Version]
  33. Li, C.; Xiao, C.; Guenet, B.; Li, M.; Xu, L.; He, N. Short-term effects of labile organic C addition on soil microbial response to temperature in a temperate steppe. Soil Biol. Biochem. 2022, 167, 108589. [Google Scholar] [CrossRef]
  34. Hursh, A.; Ballantyne, A.; Cooper, L.; Maneta, M.; Kimball, J.; Watts, J. The sensitivity of soil respiration to soil temperature, moisture, and carbon supply at the global scale. Glob. Chang. Biol. 2017, 23, 2090–2103. [Google Scholar] [CrossRef]
  35. Nguyen, L.T.T.; Broughton, K.; Osanai, Y.; Anderson, I.C.; Bange, M.P.; Tissue, D.T.; Singh, B.K. Effects of elevated temperature and elevated CO2 on soil nitrification and ammonia-oxidizing microbial communities in field-grown crop. Sci. Total Environ. 2019, 675, 81–89. [Google Scholar] [CrossRef] [PubMed]
  36. Liu, Y.; Gao, K.; Guo, Z.; Liu, X.; Bian, R.; Sun, B.; Li, J.; Chen, J. An antagonistic effect of elevated CO2 and warming on soil N2O emissions related to nitrifier and denitrifier communities in a Chinese wheat field. Plant Soil 2022, 470, 97–110. [Google Scholar] [CrossRef]
  37. Shen, L.; Yang, Y.; Liu, J.; Hu, Z.; Liu, X.; Tian, M.; Yang, W.; Jin, J.; Wang, H.; Wang, Y.; et al. Different responses of ammonia-oxidizing archaea and bacteria in paddy soils to elevated CO2 concentration. Environ. Pollut. 2021, 286, 117558. [Google Scholar] [CrossRef] [PubMed]
  38. Song, X.; Ju, X.; Topp, C.F.E.; Rees, R.M. Oxygen Regulates Nitrous Oxide Production Directly in Agricultural Soils. Environ. Sci. Technol. 2019, 53, 12539–12547. [Google Scholar] [CrossRef]
  39. Shudan, B. Soil Agro-Chemistry Analysi; China Agriculture Press: Beijing, China, 2005. [Google Scholar]
  40. Francis, C.A.; Roberts, K.J.; Beman, J.M.; Santoro, A.E.; Oakley, B.B. Ubiquity and diversity of ammonia-oxidizing archaea in water columns and sediments of the ocean. Proc. Natl. Acad. Sci. USA 2005, 102, 14683–14688. [Google Scholar] [CrossRef] [Green Version]
  41. Rotthauwe, J.H.; Witzel, K.P.; Liesack, W. The ammonia monooxygenase structural gene amoA as a functional marker: Molecular fine-scale analysis of natural ammonia-oxidizing populations. Appl. Environ. Microb. 1997, 63, 4704–4712. [Google Scholar] [CrossRef] [Green Version]
  42. Throbäck, I.N.; Enwall, K.; Jarvis, Ã.S.; Hallin, S. Reassessing PCR primers targeting nirS, nirK and nosZ genes for community surveys of denitrifying bacteria with DGGE. Fems. Microbiol. Ecol. 2004, 49, 401–417. [Google Scholar] [CrossRef]
  43. Hallin, S.; Lindgren, P. PCR Detection of Genes Encoding Nitrite Reductase in Denitrifying Bacteria. Appl. Environ. Microb. 1999, 65, 1652–1657. [Google Scholar] [CrossRef]
Figure 1. Diurnal variation of N2O emission rates and soil temperatures on three typical days at early (a,d,g,j), middle (b,e,h,k), and later (c,f,i,l) growth stage, and relationship between N2O emission rate with soil temperature at early (A), middle (B), and later (C) growth stage. The date of the three growth stages is introduced in Supplementary Methods. MC and CK are abbreviations for treatments with or without mulching, respectively. Vertical bars are the standard error of the mean (n = 3).
Figure 1. Diurnal variation of N2O emission rates and soil temperatures on three typical days at early (a,d,g,j), middle (b,e,h,k), and later (c,f,i,l) growth stage, and relationship between N2O emission rate with soil temperature at early (A), middle (B), and later (C) growth stage. The date of the three growth stages is introduced in Supplementary Methods. MC and CK are abbreviations for treatments with or without mulching, respectively. Vertical bars are the standard error of the mean (n = 3).
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Figure 2. Variation of N2O emission rates and WFPS after irrigation under black plastic film mulching treatment in 2017 (a,b) and 2018 (d,e), and linear correlation between N2O emission rates and WFPS in 2017 and 2018 (c,f).
Figure 2. Variation of N2O emission rates and WFPS after irrigation under black plastic film mulching treatment in 2017 (a,b) and 2018 (d,e), and linear correlation between N2O emission rates and WFPS in 2017 and 2018 (c,f).
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Figure 3. Variation of soil CO2 and N2O concentrations in 2017 and 2018 and the relationship between soil CO2 and N2O concentrations.
Figure 3. Variation of soil CO2 and N2O concentrations in 2017 and 2018 and the relationship between soil CO2 and N2O concentrations.
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Figure 4. Soil N2Orelated gene abundances at the end of the experiment in 2018. Different letters above each bar indicate a significant difference between black plastic film mulching (MC) and non-mulched (CK) treatment at p < 0.05.
Figure 4. Soil N2Orelated gene abundances at the end of the experiment in 2018. Different letters above each bar indicate a significant difference between black plastic film mulching (MC) and non-mulched (CK) treatment at p < 0.05.
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Figure 5. Daily N2O emission rates and cumulative N2O emissions under the soil with (MC) and without (CK) black plastic film mulching. Different letters above each bar indicate a significant difference between MC and CK at p < 0.05. Values of the columns and standard errors are shown in Table 1. Vertical bars are the standard error of the mean (n = 3).
Figure 5. Daily N2O emission rates and cumulative N2O emissions under the soil with (MC) and without (CK) black plastic film mulching. Different letters above each bar indicate a significant difference between MC and CK at p < 0.05. Values of the columns and standard errors are shown in Table 1. Vertical bars are the standard error of the mean (n = 3).
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Figure 6. Correlations of cumulative N2O emission with soil temperature, WFPS, irrigation times, soil CO2 concentrations, soil N2O concentrations, and abundance of amoAAOA, amoAAOB, nirK, and nirS genes (a). Conceptual diagrams showing regulators and controls of black plastic film mulching effect on cumulative N2O emission (b).
Figure 6. Correlations of cumulative N2O emission with soil temperature, WFPS, irrigation times, soil CO2 concentrations, soil N2O concentrations, and abundance of amoAAOA, amoAAOB, nirK, and nirS genes (a). Conceptual diagrams showing regulators and controls of black plastic film mulching effect on cumulative N2O emission (b).
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Table 1. Cumulative N2O emissions, soil temperatures, WFPS, and soil N2O-related gene abundances as affected by black plastic film mulching treatment.
Table 1. Cumulative N2O emissions, soil temperatures, WFPS, and soil N2O-related gene abundances as affected by black plastic film mulching treatment.
YearParameterMC 1CKANOVA
2017Cumulative N2O emission (kg hm−2)5.56 ± 0.15 a4.58 ± 0.25 b*
Soil temperature (°C)20.7 ± 0.5 a18.2 ± 0.3 b*
WFPS (%)48.4 ± 0.446.1 ± 0.2*
2018Cumulative N2O emission (kg hm−2)5.77 ± 0.13 a4.57 ± 0.28 b*
Soil temperature (°C)21.6 ± 0.0 a19.6 ± 0.3 b*
WFPS (%)48.4 ± 0.146.7 ± 0.1*
amoA-AOA (107 g−1 soil)7.96 ± 0.507.80 ± 0.85ns
amoA-AOB (108 g−1 soil)3.76 ± 0.20 a3.12 ± 0.04 b*
nirK (105 g−1 soil)7.34 ± 0.077.51 ± 0.12ns
nirS (107 g−1 soil)4.91 ± 0.035.00 ± 0.02ns
1 Note: MC and CK are abbreviations for treatments with or without mulching, respectively. Different letters near the values indicate a significant difference between MC and CK at p < 0.05. Values are means ± SE (n = 3). *: difference between treatments was significant (p < 0.05); ns: there was no significant difference.
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Meng, C.; Zhao, J.; Wang, N.; Yang, K.; Wang, F. Black Plastic Film Mulching Increases Soil Nitrous Oxide Emissions in Arid Potato Fields. Int. J. Environ. Res. Public Health 2022, 19, 16030. https://doi.org/10.3390/ijerph192316030

AMA Style

Meng C, Zhao J, Wang N, Yang K, Wang F. Black Plastic Film Mulching Increases Soil Nitrous Oxide Emissions in Arid Potato Fields. International Journal of Environmental Research and Public Health. 2022; 19(23):16030. https://doi.org/10.3390/ijerph192316030

Chicago/Turabian Style

Meng, Chaobiao, Jianyu Zhao, Ning Wang, Kaijing Yang, and Fengxin Wang. 2022. "Black Plastic Film Mulching Increases Soil Nitrous Oxide Emissions in Arid Potato Fields" International Journal of Environmental Research and Public Health 19, no. 23: 16030. https://doi.org/10.3390/ijerph192316030

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