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Brief Report

Rice straw decomposition in paddy surface water potentially reduces soil methane (CH4) emission

[version 1; peer review: 1 approved with reservations, 1 not approved]
PUBLISHED 10 Mar 2022
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This article is included in the Agriculture, Food and Nutrition gateway.

Abstract

Background: Rice cultivation is a significant methane (CH4) emission source. Rice straw (RS) incorporation into the soil is a key factor that produces higher CH4 emission. The RS waterlogging approach on the soil surface possibly reduces CH4 emission due to not being buried into the soil. However, evaluation of CH4 emission by this approach has not been determined. The objective of this study was to examine CH4 emission under RS waterlogging on surface water compared with RS incorporation into the soil.
Methods: We carried out a microcosm experiment in a screen-house with two treatments, including (i) RS incorporation into the soil and (ii) RS waterlogging on the soil surface in triplicates. We compared the CH4 emissions and CH4 accumulation for the rice-growing and off-sowing periods. Yield-scaled CH4 emission was assessed based on total methane emission and rice yield.
Results: The results demonstrated that RS waterlogging reduced CH4 emission by 16.9% compared to RS incorporation into the soil. During the rice-growing period, total CH4 emission from RS waterlogging accounted for 36% of the incorporation treatment. However, RS waterlogging is caused by high emissions during the off-sowing stage. The difference between yield-scaled CH4 emissions was insignificant.
Conclusions: This study demonstrated that the treatment of RS by waterlogging is an appropriate alternative to conventional RS practices known as incorporation, which increases greenhouse CH4 emission. However, high CH4 emission during the off-sowing period, and RS accumulation in the field are key drivers that possibly contribute to greenhouse gas emissions. Therefore, further evaluation is needed to determine the long-term effects of this approach.

Keywords

greenhouse gas emission, rice straw incorporation, methane emission, organic rice, water management, the Vietnamese Mekong Delta

Introduction

The agricultural sector contributes approximately 10–12% of global anthropogenic emissions. Of these emissions, 47% of methane (CH4) emission has been attributed to agriculture production (Smith et al., 2007). Rice fields have been considered an important source of atmospheric CH4, accounting for 15–20% of the global total anthropogenic CH4 emission (Sass & Fisher, 1997). Rice straw (RS) plays a vital role in contributing to CH4 emission from paddy fields. Several field experiments have shown that RS incorporation significantly increases CH4 emissions in rice fields (Hoa et al., 2019; Jiang et al., 2019; Liu et al., 2015; Wang et al., 2019). In the Mekong Delta of Vietnam, the intensification of rice cultivation is a great contributor to CH4 emission (Oda & Chiem, 2019). Several studies have explored decomposing RS in paddy surface water as an effective pathway to reduce CH4 emission (Boateng et al., 2017; Oda & Chiem, 2019; Tariq et al., 2017). For example, Thao et al. (2019) demonstrated a field experiment on RS decomposing in field surface water 20 days before sowing as a suitable possibility for developing a double-cropping pattern in the Mekong Delta. However, the research did not determine how much this process reduced CH4 emissions. In addition, Oda & Chiem (2019) suggested that the strategy of decomposing RS on surface water effectively reduces CH4 emission from the paddies. To the best of our knowledge, CH4 emission from the RS decomposition process in water has not been thoroughly studied. Therefore, we conducted a microcosms experiment to clarify whether RS waterlogging reduces CH4 emission, and the results found that this approach did decrease the CH4 emission from the paddy field.

Methods

Study setting and materials

This study was conducted in an experimental screen house at Can Tho University (Cantho City, Vietnam) from April to August 2019. The screen-house consisted of a translucent white roof and rat-proof wire screens. The inner humidity in the experimental house is relatively similar compared with outdoors. We used plastic containers (38 cm × 58 cm × 30 cm high) filled to 20 cm with paddy field soil (10°18′N, 105°54′E). The soil was classified as Thionic Glycesol (International Union of Soil Sciences (IUSS) working group World Reference Base (WRB), 2015) (Dong et al., 2012).

Rice cultivation

Effects of RS waterlogging and RS incorporation into the soil on methane emission were evaluated following a conventional rice cultivation experiment (first crop). The first experiment set essential conditions (rice straw, soil) for implementing the second experiment. In the first crop, a short-duration variety of rice was used (IR50404 cultivar, 85–90 days) which is a typical rice variety of Vietnam, provided by Cuu Long Delta Rice Research Center (CLRRI). Pre-germinated seeds were sown at an equivalent rate of 250 kg ha-1 on wet-leveled soil. Water irrigation was managed as alternative wetting and drying (AWD) technology which reflood 5 cm when the surface water level naturally declined to 10 cm below the soil surface. The technology is known as multiple aerations developed by International Rice Research Institute (IRRI) to reduce water consumption for rice cultivation (Hoa et al., 2018). In the second crop, we used RS and soil from containers in the first crop to examine the effects of rice straw incorporation and waterlogging on methane emission. Fresh RS (above-surface biomass) in the first crop was collected and cut into 5 cm in length. Then it was immediately scattered onto the soil surface as well as incorporated into the soil, correspondingly. The IR50404 variety was also sown at a rate of equivalent to 250 kg ha-1. Water irrigation was managed as a continuously flooding management method during the rice-growing period. Fertilizers were not applied for either experiment.

Experimental design

There were two treatments, comprising (i) RS waterlogging on the soil surface and (ii) RS incorporation into the soil. Each treatment was set up in triplicate. A total of six microcosms were laid out closely in an array of two columns and three rows. Both treatments were performed one day after harvesting the first crop.

In the waterlogging treatment, RS was scattered on the soil surface and irrigated to 10 cm in-depth for the waterlogging treatment. Then, the RS was gently pressed into water. It was left for a 20-day stage without disturbing (off-sowing period). This timing was followed by a field demonstration recommended by Thao et al. (2019) that RS was well-fermented in water within 20 days, and the rice field has suitable conditions for broadcasting rice seeds. In the RS incorporation treatment, RS was incorporated into the soil by a shovel and immediately irrigated to 2 cm in-depth for a 5-day period (off-sowing period), a typical treatment pattern for a triple-cropping rice production system in the Vietnamese Mekong Delta.

On the sowing day, we drained the field and leveled it by hand. The soil was not reincorporated. We started irrigation on day 7 with 3–5 cm of water and maintained the water level during the rice-growing period. The water level was drained seven days before harvesting.

Measurements

The closed chamber method was used to measure CH4 following the guidelines recommended by Minamikawa et al. (2015). The chamber (58 cm in length × 38 cm in wide and 90 cm in height) was equipped with a vent to allow equilibration of the pressure, a thermometer, a sampling port, and a fan to ensure well-mixed air inside the chamber while taking the gas sample. Gas sampling was flushed five times with chamber air before collecting. Gas samples were collected with a propylene syringe 50mL at 3, and 23 min after the chamber placement, and each gas sample was immediately injected to 15 mL in vacuumed vials. During the off-sowing period (rice straw treated before harvesting), gas sampling was taken on days 3, 6, and 13 for the rice straw waterlogging treatment, while RS incorporation treatment was sampled on day 3. After sowing, sampling frequently intensified every three days during the first 21 days when the high fluxes were characteristically observed. Then, the process was carried out once a week until the day of harvest. All gas samples were taken between 07:00, and 10:00 am. The CH4 concentration was analyzed by gas chromatography (Shimadzu GC2014, Japan) equipped with a flame ionization detector, using 60/80 Carboxen® 1000 column at temperature 180 °C. Nitrogen (99.99%) as a carrier gas at a flow rate of 30 ml min−1.

Tap water was directly irrigated for rice containers. Water levels were checked by a 50-cm ruler (1-mm scale). Grain yield was detected by harvesting all rice in each pot and removing all unfilled grains using tap water. Grains were sundried at ambient temperature. The presented grain yield was adjusted to 14% of moisture by a grain moisture tester (Riceter f2, Kett Electric Laboratory, Tokyo, Japan).

Data processing

The cumulative CH4 emissions were calculated using a trapezoidal integration method with linear interpolation and numerical integration between sampling times. The calculation was done as follows: (i) calculate the daily gas flux by multiplying the daily mean hourly gas flux by 24, (ii) calculate the emission between every two consecutive measurements using the trapezoidal rule, and (iii) sum up the areas of all the trapezoids. Yield-scale CH4 emission was calculated by dividing total methane emission by grain yield. Detailed guidance can be found at Minamikawa et al. (2015). All measurements were carried out with three repetitions. Data processes were performed using Microsoft Excel 2019.

Analysis

Data analysis was performed using IBM SPSS Statistics 22.0 (RRID:SCR_016479). The independent sample t-test comparison was used to compare the CH4 emission in rice-growing and off-sowing periods as well as yield-scaled CH4 emission. The statistical significance was done with a confident level of 95%.

Results

Accumulative emission

We assessed the effects of rice straw management via waterlogging and incorporation on CH4 emission using a container experiment. The results showed that the CH4 emission from waterlogging accounted for 36% of the incorporation treatment during the rice-growing period (Figure 1a) (Oda et al., 2020). However, high emissions were found in the off-sowing stage (Figure 1b). The total CH4 emissions from the waterlogging and incorporation treatments were 502 ± 111.4 kgCH4.ha-1.crop-1 and 604 ± 41.9 kgCH4.ha-1.crop-1, respectively. In general, the magnitude of seasonal CH4 emission that was observed in our study was lower than what was found in previous studies on triple-cropping in the central Mekong Delta of Vietnam, which ranged between 710 and 1,789 kgCH4.ha-1.crop-1 (Oda & Chiem, 2019; Vo et al., 2018). The CH4 emission for the decomposing RS subject to waterlogging was 16.9% lower than that of the straw in the incorporation approach, even though the total timing of the off-sowing and rice-growing period was 30% longer. For the yield-scaled CH4 emission from straw, the waterlogging and incorporation models were 0.21 ± 0.02 kg CH4.kg grain-1 and 0.3 ± 0.08 kg CH4. kg grain-1, respectively. The difference between yield-scaled CH4 emissions was insignificant (P>0.05) (Figure 2).

c78678f9-39d5-48ce-9b57-dfe38ddc86b5_figure1.gif

Figure 1.

CH4 emission accumulation of rice strawy (RS) waterlogging and RS incorporation in the periods of rice-growing (a), and off-sowing (b).

c78678f9-39d5-48ce-9b57-dfe38ddc86b5_figure2.gif

Figure 2. Yield-scaled CH4 emission of rice straw (RS) waterlogging and RS incorporation.

Emission pattern

CH4 emission peaked one week after the prior crop's harvest. The peak of waterlogging was 3.82 times higher than the peak of the incorporation approach (Figure 3). After sowing, the CH4 emission of the incorporation approach was always higher when compared with the waterlogging method. The first peak was in line with a previous study (Oda & Chiem, 2019).

c78678f9-39d5-48ce-9b57-dfe38ddc86b5_figure3.gif

Figure 3. CH4 emission rate of rice straw (RS) waterlogging and RS incorporation.

Discussion

Conventional rice cultivation based on rice straw incorporation of paddy fields is a substantial source of CH4 emissions. Modification of rice straw practices is undoubtedly necessary to reduce CH4 flux when the rice straw incorporated into the soil. In other words, rice straw incorporation will be the most detectable substrate source to contribute to higher CH4 emission from rice paddy fields. Although rice straw amendment enriches soil organic carbon and improves soil fertility (Bjoern et al., 2014; Liu et al., 2014), it increases the availability of organic carbon and simultaneously intensifies strict anaerobic conditions to stimulate CH4 formation on the rice paddy field (Sass et al., 1991). Waterlogging rice straw management strategy instead of incorporation demonstrates less methane emission 12%, even though rice straw applied during the fallow period decreased CH4 emission by 11% compared to the same amount rice straw applied during rice filed preparation (Lu et al., 2000). In this study, we reached similar results in mitigation of emission from the rice straw practice with regards to non-incorporation reduced 16.9% for the whole period. The efficiency of CH4 emission from rice straw waterlogging on the field surface promotes aerobic decomposition, resulting in reducing CH4 emission.

This study showed the effects of rice straw management on CH4 emission in the rice-growing period. Total CH4 emission of rice straw after waterlogging was lower than that of the incorporation approach. These findings suggest that when rice straw was decomposed in water generated less CH4 emission than when it was buried in the soil. This can be explained by decomposition via soil-flooding management, which blocks oxygen penetration into the soil and creates a stable anaerobic condition, allowing bacteria capable of producing CH4 to thrive (Conrad, 2007). In the decomposition of rice straw in water, which is generally affected by dissolved oxygen, methanogenesis fermentation can be limited by high O2 concentrations (Jiang et al., 2019). In addition, the low yield-scaled CH4 emission from waterlogging demonstrates that this method effectively increases agricultural production and improves environmental protection.

As observed in this study, when waterlogging is used during the off-sowing period, CH4 emission is more concentrated than incorporation because the rice straw decomposition period is longer than that of rice straw incorporation treatment. Specifically, the off-sowing period was conducted for 20 days, while the rice straw incorporation treatment was performed for five days only. Subsequently, the total CH4 emission during the RS waterlogging is more significant than rice straw incorporation. Rice straw CH4 emission sources generate from rice straw decomposing. During off-sowing, rice straw waterlogging decomposes faster than incorporation and produces much more readily available carbon. The decomposing process consumes dissolved oxygen in the water, creating an anaerobic condition, contributing to the CH4 generation.

The development of agricultural technologies to reduce CH4 emission during off-sowing should be performed in future research. For instance, alternative wetting and drying (AWD) or intermittent irrigation could be a suitable option for reducing CH4 emission during the waterlogging period because it transmits the surface condition of the paddy field from reduction condition to oxidation condition by frequent contact with the air. Furthermore, the effects on the proportion of rice straw returning and seasonal carbon accumulation have not been deduced. Thus, future works should continuously examine their effects on CH4 emission in the long-term run.

Conclusions

We evaluated effects of RS treatment measures on CH4 emissions under waterlogging and incorporation. Our results indicated that RS decomposition under the waterlogging approach reduces CH4 emission compared to the incorporation approach, confirming the feasibility of rice straw waterlogging as a mitigation option for paddy CH4 emission in the Vietnamese Mekong Delta. However, waterlogging significantly contribute to CH4 emission during the off-sowing period. Thus, we recommend that reducing CH4 emission using RS decomposition during off-showing should be examined for further studies.

Data availability

Underlying data

Figshare: Methane emission in waterlogging double cropping. https://doi.org/10.6084/m9.figshare.11987628.v1 (Oda et al., 2020).

This project contains the following underlying data:

  • - Methane concentration and GHG_12 March 2020_17h25.xlsx (This file provides raw data that collected during experimental operation used for calculating CH4 emission (mgCH4.m-2.h-1) and cumulative methane emission (kgCH4.ha-1.crop-1), and yield-scaled CH4 emission (kg CH4 grain-1)).

Data are available under the terms of the Creative Commons Zero "No rights reserved" data waiver (CC0 1.0 Public domain dedication).

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Van Thao H, Oda M and Chiem NH. Rice straw decomposition in paddy surface water potentially reduces soil methane (CH4) emission [version 1; peer review: 1 approved with reservations, 1 not approved]. F1000Research 2022, 11:298 (https://doi.org/10.12688/f1000research.110326.1)
NOTE: If applicable, it is important to ensure the information in square brackets after the title is included in all citations of this article.
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ApprovedThe paper is scientifically sound in its current form and only minor, if any, improvements are suggested
Approved with reservations A number of small changes, sometimes more significant revisions are required to address specific details and improve the papers academic merit.
Not approvedFundamental flaws in the paper seriously undermine the findings and conclusions
Version 1
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PUBLISHED 10 Mar 2022
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Reviewer Report 23 May 2022
Azeem Tariq, Department of Plant and Environmental Sciences, University of Copenhagen, Copenhagen, Denmark 
Not Approved
VIEWS 17
The authors of 'Rice straw decomposition in paddy surface water potentially reduces soil methane (CH4) emission' present an effort in assessing the effects of two rice straw amendments on soil CH4 emissions during the crop growing period and during the ... Continue reading
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HOW TO CITE THIS REPORT
Tariq A. Reviewer Report For: Rice straw decomposition in paddy surface water potentially reduces soil methane (CH4) emission [version 1; peer review: 1 approved with reservations, 1 not approved]. F1000Research 2022, 11:298 (https://doi.org/10.5256/f1000research.121920.r129417)
NOTE: it is important to ensure the information in square brackets after the title is included in all citations of this article.
  • Author Response 17 Jun 2022
    Thao Huynh Van, College of Environment and Natural Resources, Can Tho University, Can Tho city, 900000, Vietnam
    17 Jun 2022
    Author Response
    Thank you very much for giving us constructive comments that helped us improve this paper immensely. All your comments have been carefully read and revised to elucidate underlying aspects. Our ... Continue reading
COMMENTS ON THIS REPORT
  • Author Response 17 Jun 2022
    Thao Huynh Van, College of Environment and Natural Resources, Can Tho University, Can Tho city, 900000, Vietnam
    17 Jun 2022
    Author Response
    Thank you very much for giving us constructive comments that helped us improve this paper immensely. All your comments have been carefully read and revised to elucidate underlying aspects. Our ... Continue reading
Views
32
Cite
Reviewer Report 16 May 2022
Yosei Oikawa, Department of International Innovative Agricultural Science, Tokyo University of Agriculture andTechnology, Tokyo, Japan 
Approved with Reservations
VIEWS 32
This study investigated the effects of rice straw waterlogging and rice straw incorporation into the soil on methane emission through a microcosm experiment. The results showed significant differences between those treatments and seem to contain some suggestive points to reduce ... Continue reading
CITE
CITE
HOW TO CITE THIS REPORT
Oikawa Y. Reviewer Report For: Rice straw decomposition in paddy surface water potentially reduces soil methane (CH4) emission [version 1; peer review: 1 approved with reservations, 1 not approved]. F1000Research 2022, 11:298 (https://doi.org/10.5256/f1000research.121920.r135051)
NOTE: it is important to ensure the information in square brackets after the title is included in all citations of this article.
  • Author Response 17 Jun 2022
    Thao Huynh Van, College of Environment and Natural Resources, Can Tho University, Can Tho city, 900000, Vietnam
    17 Jun 2022
    Author Response
    Thank you very much for giving us constructive comments that helped us improve this paper immensely. All your comments have been carefully read and revised to elucidate underlying aspects. Our ... Continue reading
COMMENTS ON THIS REPORT
  • Author Response 17 Jun 2022
    Thao Huynh Van, College of Environment and Natural Resources, Can Tho University, Can Tho city, 900000, Vietnam
    17 Jun 2022
    Author Response
    Thank you very much for giving us constructive comments that helped us improve this paper immensely. All your comments have been carefully read and revised to elucidate underlying aspects. Our ... Continue reading

Comments on this article Comments (0)

Version 2
VERSION 2 PUBLISHED 10 Mar 2022
Comment
Alongside their report, reviewers assign a status to the article:
Approved - the paper is scientifically sound in its current form and only minor, if any, improvements are suggested
Approved with reservations - A number of small changes, sometimes more significant revisions are required to address specific details and improve the papers academic merit.
Not approved - fundamental flaws in the paper seriously undermine the findings and conclusions
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