Research Article | Open Access
Can Chen, Deli Chen, Jianjun Pan, Shu Kee Lam, "Application of the Denitrification-Decomposition Model to Predict Carbon Dioxide Emissions under Alternative Straw Retention Methods", The Scientific World Journal, vol. 2013, Article ID 851901, 7 pages, 2013. https://doi.org/10.1155/2013/851901
Application of the Denitrification-Decomposition Model to Predict Carbon Dioxide Emissions under Alternative Straw Retention Methods
Straw retention has been shown to reduce carbon dioxide (CO2) emission from agricultural soils. But it remains a big challenge for models to effectively predict CO2 emission fluxes under different straw retention methods. We used maize season data in the Griffith region, Australia, to test whether the denitrification-decomposition (DNDC) model could simulate annual CO2 emission. We also identified driving factors of CO2 emission by correlation analysis and path analysis. We show that the DNDC model was able to simulate CO2 emission under alternative straw retention scenarios. The correlation coefficients between simulated and observed daily values for treatments of straw burn and straw incorporation were 0.74 and 0.82, respectively, in the straw retention period and 0.72 and 0.83, respectively, in the crop growth period. The results also show that simulated values of annual CO2 emission for straw burn and straw incorporation were 3.45 t C ha−1 y−1 and 2.13 t C ha−1 y−1, respectively. In addition the DNDC model was found to be more suitable in simulating CO2 mission fluxes under straw incorporation. Finally the standard multiple regression describing the relationship between CO2 emissions and factors found that soil mean temperature (SMT), daily mean temperature (), and water-filled pore space (WFPS) were significant.
Atmospheric concentrations have increased by approximately 35% and are predicted to reach 700 ppmv by the end of 20 century . Soils are the largest carbon pool in terrestrial ecosystem, containing more than two thirds of the total carbon and soil respiration, and contribute an annual atmospheric flux 10 times greater than fossil fuel combustion . Therefore, it is crucial to reduce emissions from agricultural land.
There are many factors affecting emissions, including soil temperature, soil moisture, and soil organic matter (SOM) . Schlesinger and Andrews  showed that soil emissions increase with soil temperature. La Scala et al.  reported that microbial activity, soil respiration, and enzymatic activity increased with rising temperature. Subke et al.  suggested that soil moisture was an important nonbiological factor affecting soil flux. Li  analyzed the sensitivity in predicting and flux emissions for a series of models and found that the amount of soil organic matter (SOM) was the most important factor.
Straw retention has been adopted worldwide to increase crop production. It has been shown to reduce but increase crop yield . Li et al.  considered that if the straw retention rate increased from 15 to 80% in China, the Chinese agricultural carbon budget should change from negative (emissions from soil of t y−1) to positive (soil absorbing t y−1). While the effects of different straw retention methods on emission flux have been studied in many continuous long-term experiments, information on the use of the DNDC model to simulate emission under different straw retention scenarios is lack. In particular information is required to predict the total variation of emission fluxes and the interrelation of important factors. The objective of this study was to simulate the daily rate of emissions in the straw retention and crop growth periods and study the annual amount of emission by the DNDC model for different straw retention treatments. The research analyzed the relationship of the major factors with path analysis and provided implications for the mitigation of emissions in the study area.
2. Materials and Methods
2.1. Study Site
Field experiments were conducted on a commercial farm in New South Wales (NSW) Australia, 34°30′S, 146°11′E, located approximately 30 km southeast of Griffith. Mean annual precipitation is 432 mm, and mean maximum and minimum temperatures are 23.0 and 10.3°C, respectively (measured at the nearest recording station, Leeton). The soil (0–20 cm) is classified as a Typic Natrixeralf and Mundiwa clay loam with clay particle content in 53.11% . The surface soil has a pH of 5.5 (soil : water = 1 : 5) of 0.03 kg carbon (C)/kg and soil bulk density of 1.37 g cm−3 (Table 1). WFPS is calculated as WFPS = (soil gravimetric water content × bulk density)/(1 − (bulk density/particle density)) . Maize was grown at the site on beds (two rows of plants per bed) and irrigated by furrow irrigation.
2.2. Experimental Design and Data Analysis
The field experiment began on 11 May 2010 (day 1) and ended on 10 May 2011 (day 365). There were two maize straw treatments in the field experiment. A randomized block design with three replicates was used in the 12 plots. The maize straw treatments were (1) application of 300 kg N ha−1, maize straw burnt and left on the field (300N-burn), and (2) application of 300 kg N ha−1, maize straw mulched (the amount of maize straw was 6750 kg ha−1) and incorporated into soil (5 cm) soon after harvest (300N-incorporated). The 300N-burn treatment used 6 plots and 300N-incorporated treatment used another 6 plots. The result of each treatment was the mean value. The two straw retention methods lasted for one maize season. Fertilizer was applied three times: 90 kg N ha−1 as on October 22, 2010 (day 165) three days before sowing, 10 kg N ha−1 as urea (mixed with the soil as seed manure) on October 25, 2010 (day 168) at sowing, and 200 kg N ha−1 as urea on December 6, 2010 (day 204). The area was flood irrigated ten times (Table 2). This study was divided into two periods. The first period, from May 11, 2010 to October 22, 2010 was called straw retention period. The second period, from October 22, 2010 to May 10, 2011 was called maize growth period.
The fluxes from the soil-plant system were measured on the basis of static transparent chamber and gas chromatography methods . The bottom chambers were empty and the top chambers were connected to an infrared analyzer via air pipes. Chambers were 43 cm × 43 cm × 110 cm and were adjusted according to the height of maize across time . This system measures fluxes integrated over 2 or 3 day intervals and avoids errors associated with manual flux chambers, when measurements are taken only at a particular time period. Each system was powered by a 12 V 120 amp-hour battery. The battery capacity was supplemented by an 80 W solar panel that extended the period between battery changeover to between 1 and 4 weeks. Soil temperature was measured using type K thermocouples and soil moisture was measured using time domain reflectometry (TDR) (Theta Probes ML2x, Delta-T Devices Ltd., Cambridge, UK). Both sets of sensors were logged by a controller/logger unit. Gas concentrations in the Tedlar sample bags were measured off-site at Aspendale. was measured using a Licor 6251 NDIR (Licor, Nebraska, USA). In addition concentration was measured directly in the field using a Gascard_II sensor (Edinburgh Instruments, Edinburgh, UK) incorporated into each chamber controller.
2.3. DNDC Model
In this study the DNDC model (version 9.5; http://www.dndc.sr.unh.edu/) was applied to simulate emission under different straw retention scenarios. The DNDC model has a relatively high level of complexity. The DNDC model can be used to simulate fluxes of , , , , , leaf area index (LAI) development, soil organic matter decomposition rate, nutrient leaching, change in soil organic carbon (SOC), and biomass production . DNDC contains four main submodels [7, 13]. The soil climate sub-model calculates hourly and daily soil temperature and moisture fluxes. The crop growth submodel simulates crop biomass accumulation and partitioning. The decomposition sub-model calculates decomposition, nitrification, volatilization and production. The input data are shown in Tables 1 and 2.
2.4. Data Analysis
The DNDC model was used to simulate fluxes under the different straw retention methods. Model accuracy and performance were evaluated by calculating the correlation coefficient and model efficiency (ME) . ME is calculated as where is observed values, is simulated values, is the total number of observations, is the mean of observed values, and is the current observation.
ME compares the squared sum of the absolute error with the squared sum of the difference between the observations and their mean value. It compares the ability of the model to reproduce the daily data variability with a much simpler model that is based on the arithmetic mean of the measurements. ME values close to 1 indicate a “near-perfect” fit [15, 16].
Five continuous long-term measurement factors were considered for the statistical analysis, namely, daily maximum temperature , daily minimum temperature, , daily mean temperature , soil mean temperature (SMT), and amount of irrigation. Irrigation was not a daily operation, but it had residual effects on soil water. Therefore, water-filled pore space (WFPS) was used to reflect the water dynamics following irrigation and rainfall events in soil. As a result, five factors which affected the emission were selected: , , , SMT, and WFPS.
Data were analyzed by correlation analysis and path analysis using SPSS 13.0. Path analysis can be used for the analysis of multiple variables and the linear relationship between variables. It was a development of regression analysis .
The straw retention period and crop growth period were studied separately because the sources of the were different in these two periods . The main sources of were straw decomposition, SOM decomposition, and microbial respiration during the straw retention period. Root respiration, SOM decomposition, and microbial respiration are the main sources during the crop growth period [19–21].
3.1. Simulation of Daily CO2 Emission during Straw Retention Period
The simulated and observed values of daily emission under different straw retention treatments during straw retention period are shown in Figure 1. The correlation coefficient between simulated and observed values for treatments 300N-burn and 300N-incorporation were 0.74 (Figure 1(a)) and 0.82 (Figure 1(b)), respectively, () and the ME values were 0.63 and 0.76.
3.2. Daily CO2 Emission during Crop Growth and Annual CO2 Emissions
The DNDC model was also used to simulate the daily fluxes during crop growth (Figure 2).
The correlation coefficients between the observed and simulated values of flux were 0.72 and 0.82 () for treatment 300N-burn and 300N-incorporation, respectively (Figure 2). The corresponding ME values were 0.63 and 0.79. The ME value of 300N-incorporation was higher than that of the 300N-burn. This indicates that the DNDC model was more suitable for simulating fluxes for the straw incorporation treatment than the straw burning treatment during the crop growth period.
The observed values of emissions during the maize growth season for 300N-Burn and 300N-incorporation were 4.7 t C ha−1 y−1 and 3.5 t C ha−1 y−1, respectively. The corresponding simulated values were 3.45 t C ha−1 y−1 and 2.13 t C ha−1 y−1, respectively (Table 3). The observed values were smaller than the observed values. This is because DNDC model could simulate the which is discharged by the microbial activities. The which produced though plant root respiration was ignored. This also suggested that the DNDC model might have underestimated the microbial activity and the rate of SOM decomposition . So it is necessary to improve the DNDC model to adjust microbial activity and the rate of SOM decomposition simulation and contain the plant root respiration simulation function.
3.3. Sensitive Analysis
Fixed factors (continuous long-term measurements) were used for the sensitivity analysis. Because the DNDC model was more suitable for the simulation of emissions under straw incorporation than the burning of straw, the reason is shown in Sections 3.1 and 3.2, the sensitivity analysis mainly focused on the relationship between different factors and emission for the straw incorporation treatment.
The emissions were significantly correlated with , , , WFPS, and SMT. The correlation coefficients were 0.5681, 0.5114, 0.5125, 0.5366, and 0.6729, respectively () (Table 4). Temperature, WFPS, and microbial activity can influence SOM decomposition and associated emissions [5, 6, 19].
|Correlation is significant at the 0.01 level-2-tailed).*Correlation is significant at the 0.05 level-2-tailed).|
Path analysis was used to analyze the relationship among these five factors (Tables 5 and 6). The results showed that SMT, , and WFPS were the main controlling factors of emissions. The standard multiple regression equation of the emission flux was (, , ), where is emission fluxes, is SMT, is , and is WFPS. The and were not chosen because of large diurnal fluctuation of temperature in the Griffith region. The daily maximum temperature and daily minimum temperature did not reach the optimum temperature for microbial activity.
4.1. The discussion of Daily CO2 Emission during Straw Retention Period
The observed and simulated emission decreased with time regardless of straw retention treatment (Figure 1). This was because the main source of emission was straw decomposition in the straw retention period . The straw decomposition rate decreased with time. The simulated and observed fluxes in the straw burnt treatment were higher than those under straw incorporation. The reason for the difference may be related to soil structural differences, particularly the reduced accessibility of by plant roots in the burned treatment . This difference may have contributed to the greater emissions from soil in our straw burn treatments. Perhaps the process was the same in the experiments. The change in soil structural in the straw burn treatment may allow microbes to obtain more mineral nutrition after straw burn and promote the formation of granular structure. Ruser et al.  investigated the impact of compaction on soils from a row cropping system and found that production has a sensitive influence on the soil compaction. The other reason is in agreement with the finding by Beer et al.  that more greenhouse gas was evolved from straw burn treatments monitored using automatic chambers over the whole season. Therefore the straw burn treatment discharged more than the straw incorporation treatment, so that the emissions were lower in the straw incorporation than in the straw burn .
The correlation coefficient between simulated and observed values and ME values implies that the DNDC model can be used to simulate daily fluxes in the straw retention period. The ME value for 300N-incorporation was higher than for 300N-burn, suggesting that the DNDC model was more suitable to simulate emission under straw incorporation than under the burning of straw.
4.2. The Discussion of Daily CO2 Emission during Crop Growth and Annual CO2 Emissions
Both the observed and simulated values for the treatment 300N-burn were higher than those for the 300N-incorporation. The result was the same as the straw retention method. Straw decomposition rate varies with the depth of incorporation . It has been shown that the straw decomposition rate during the 32 weeks of study was the highest at the 5 cm soil depth (decomposed > 65%), followed by the 15 cm soil depth (62%), the lowest for the straw materials left on the soil surface (50%) . Under the 300N-burn treatment, the maize straw was burnt and left on the field, and the main products of maize straw combustion were and plant ash. was emitted to the atmosphere directly. Plant ash was the main driver of microbial activity. Part of the plant ash was used by microbes in the straw retention period and the other part was used in the crop growth period. So increasing soil organic carbon associated with straw incorporation  would drive decreased emission. On the other hand, the base of plant ash contains substantial mineral nutrients, which could be used by the microbes directly for energy [27, 28]. Wakelin et al.  found that stubble burnt and incorporation led to totally dissimilar soil microbial populations. The straw, which was incorporated into the soil, might require a long organic matter decomposition process [7, 30]. The soil organic matter decomposition process is slow. Therefore, the soil microbes in the straw incorporated treatment might obtain less energy than in the soil burn treatment, so that straw incorporation discharges slower than straw burn.
The correlation coefficient between simulated and observed values and ME values indicates that the DNDC model was more suitable for simulating fluxes for the straw incorporation treatment than the straw burning treatment during the crop growth period.
4.3. The Discussion of Sensitive Analysis
SMT, , and WFPS showed a direct positive effect (the corresponding direct path coefficients were 0.8067, 0.6392, and 0.4014, resp.) and indirect positive effect (the total indirect path coefficients were 1.1016, 1.2499, and 1.0915, resp.) on emissions (Table 6). This indicates that SMT, , and WFPS could directly and indirectly affect the microbial activity and decomposition of straw and organic matter in soil and control emissions. The total indirect path coefficients of SMT, , and WFPS were greater than direct path coefficients. SMT, , and WFPS could influence the microbes in decomposing the organic matter and straw to release . The WFPS included irrigation and rainfall events in soil. So irrigation and rainfall events into soil may mainly indirectly affect emissions.
The DNDC model can be used to simulate emissions under different straw retention practices in the Griffith region, NSW, Australia. The results showed that the simulation values and trends were very close to the measured values of daily fluxes, annual emissions, and emission factors for all straw retention methods. The model accuracy for the 300N-incorporated treatment was higher than that for the 300N-burn treatment in both the straw retention period and the crop growth period. This implies that the DNDC model is more appropriate for simulation of emissions under straw incorporation treatment.
emissions were positively correlated with , , , WFPS, and SMT. The path analysis showed the standard multiple regression equation of the emission was . The SMT, , and WFPS were the main factors influencing emission under different straw retention methods. Management of these practices will help mitigate emissions in cropping systems
The authors thank Dr. Christopher Ogden (formerly of Weill Cornell Medical College in Qatar) for his check of English and comments on this paper. They also wish to express their thanks to anonymous reviewers for providing useful comments to improve the paper. This study was supported by the Australian Government Department of Agriculture, Forestry and Fisheries, and the Australian Research Council.
- IPCC, Changes in Atmospheric Constituents and in Radiative Forcing, Cambridge University Press, Cambridge, UK, 2007.
- M. Abdalla, S. Kumar, M. Jones, J. Burke, and M. Williams, “Testing DNDC model for simulating soil respiration and assessing the effects of climate change on the CO2 gas flux from Irish agriculture,” Global and Planetary Change, vol. 78, no. 3-4, pp. 106–115, 2011.
- H. Li, L.-G. Wang, and J.-J. Qiu, “Estimation of CO2 and N2O emissions from farmland soils in Hebei Province in Huang-Huai-Hai Plain,” Chinese Journal of Applied Ecology, vol. 18, no. 9, pp. 1994–2000, 2007 (Chinese).
- W. H. Schlesinger and J. A. Andrews, “Soil respiration and the global carbon cycle,” Biogeochemistry, vol. 48, no. 1, pp. 7–20, 2000.
- N. La Scala Jr., D. Bolonhezi, and G. T. Pereira, “Short-term soil CO2 emission after conventional and reduced tillage of a no-till sugar cane area in southern Brazil,” Soil and Tillage Research, vol. 91, no. 1-2, pp. 244–248, 2006.
- J.-A. Subke, M. Reichstein, and J. D. Tenhunen, “Explaining temporal variation in soil CO2 efflux in a mature spruce forest in Southern Germany,” Soil Biology and Biochemistry, vol. 35, no. 11, pp. 1467–1483, 2003.
- C. S. Li, “Biogeochemical concepts and methodologies: development of the DNDC model,” Quaternary Science Reviews, vol. 21, no. 2, pp. 89–99, 2001.
- J. J. Qiu, L. G. Wang, and H. J. Tang, “Studies on the situation of soil organic carbon storage in croplands in Northeast of China,” Scientia Agriculture Sinica, vol. 4, no. 8, pp. 594–600, 2005 (Chinese).
- C. S. Li, X. M. Xiao, and S. Frolking, “Green house gas emissions from croplands of China,” Quaternary Sciences, vol. 23, no. 5, pp. 493–404, 2003 (Chinese).
- D. M. Linn and J. W. Doran, “Effect of water-filled pore space on carbon dioxide and nitrous oxide production in tilled and nontilled soils,” Soil Science Society of America Journal, vol. 48, no. 6, pp. 1267–1272, 1984.
- X. B. Wang, G. Q. Liang, and W. Zhou, “Effect of optimized nitrogen application on denitrification losses and N2O emissions from soil in wheat/summer corn rotation system in North China,” Plant Nutrition and Fertilizer Science, vol. 15, no. 1, pp. 41–48, 2009 (Chinese).
- D. Dietiker, N. Buchmann, and W. Eugster, “Testing the ability of the DNDC model to predict CO2 and water vapour fluxes of a Swiss cropland site,” Agriculture, Ecosystems and Environment, vol. 139, no. 3, pp. 396–401, 2010.
- C. Li, S. Frolking, and T. A. Frolking, “A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications,” Journal of Geophysical Research, vol. 97, no. 9, pp. 9777–9783, 1992.
- J. E. Nash and J. V. Sutcliffe, “River flow forecasting through conceptual models part I: a discussion of principles,” Journal of Hydrology, vol. 10, no. 3, pp. 282–290, 1970.
- M. Abdalla, M. Jones, J. Yeluripati, P. Smith, J. Burke, and M. Williams, “Testing DayCent and DNDC model simulations of N2O fluxes and assessing the impacts of climate change on the gas flux and biomass production from a humid pasture,” Atmospheric Environment, vol. 44, no. 25, pp. 2961–2970, 2010.
- M. Wattenbach, O. Sus, N. Vuichard et al., “The carbon balance of European croplands: a cross-site comparison of simulation models,” Agriculture, Ecosystems and Environment, vol. 139, no. 3, pp. 419–453, 2010.
- T. W. Berger, C. Neubauer, and G. Glatzel, “Factors controlling soil carbon and nitrogen stores in pure stands of Norway spruce (Picea abies) and mixed species stands in Austria,” Forest Ecology and Management, vol. 159, no. 1-2, pp. 3–14, 2002.
- Y. Ouyang and C. Zheng, “Surficial processes and CO2 flux in soil ecosystem,” Journal of Hydrology, vol. 234, no. 1-2, pp. 54–70, 2000.
- X. J. Li, Z. G. Zhang, and Y. X. Li, “Effect of soil depth on decay speed of straw,” Acta Pedologia Sinica, vol. 38, no. 1, pp. 135–149, 2001 (Chinese).
- J. B. Yavitt, T. J. Fahey, and J. A. Simmons, “Methane and carbon dioxide dynamics in a northern hardwood ecosystem,” Soil Science Society of America Journal, vol. 59, no. 3, pp. 796–804, 1995.
- D. L. Kelting, J. A. Burger, and G. S. Edwards, “Estimating root respiration, microbial respiration in the rhizosphere, and root-free soil respiration in forest soils,” Soil Biology and Biochemistry, vol. 30, no. 7, pp. 961–968, 1998.
- R. B. Edis, D. Chen, G. Wang et al., “Soil nitrogen dynamics in irrigated maize systems as impacted on by nitrogen and stubble management,” Australian Journal of Experimental Agriculture, vol. 48, no. 3, pp. 382–386, 2008.
- R. Ruser, H. Flessa, R. Russow, G. Schmidt, F. Buegger, and J. C. Munch, “Emission of N2O, N2 and CO2 from soil fertilized with nitrate: effect of compaction, soil moisture and rewetting,” Soil Biology and Biochemistry, vol. 38, no. 2, pp. 263–274, 2006.
- T. Beer, M. Meyer, T. Grant, K. Russell, and C. Kirkby, “Life-cycle assessment of greenhouse gas emissions from agriculture in relation to marketing and development. Irrigate maize: from maize field to grocery store,” Final Report HQO6A/6/F3.5, CSIRO to the Australian Greenhouse Office, Grains Research and Development Corporation and CRC for Greenhouse Accounting, 2005.
- W. Wang, J. Guo, and T. Oikawa, “Contribution of root to soil respiration and carbon balance in disturbed and undisturbed grassland communities, Northeast China,” Journal of Biosciences, vol. 32, no. 2, pp. 375–384, 2007.
- C. A. Kirkby, A. Fattore, D. Smith, and C. P. Meyer, “Life cycle assessment of greenhouse gas emissions from irrigated maize stubble treatments and plant/soil responses,” in Proceedings of the Maize Association of Australia 6th Triennial Conference “Water to Gold”, pp. 177–184, Griffith, New South Wales, Australia, February 2006.
- N. Farahbakhshazad, D. L. Dinnes, C. Li, D. B. Jaynes, and W. Salas, “Modeling biogeochemical impacts of alternative management practices for a row-crop field in Iowa,” Agriculture, Ecosystems and Environment, vol. 123, no. 1–3, pp. 30–48, 2008.
- P. Falloon and P. Smith, “Simulating SOC changes in long-term experiments with rothC and CENTURY: model evaluation for a regional scale application,” Soil Use and Management, vol. 18, no. 2, pp. 101–111, 2002.
- S. Wakelin, M. Colloff, S. Rogers, and P. Harvey, “The effect of maize stubble and N management on ecologically-significant soil microbial communities,” in Maize Association of Australia 6th Triennial Conference “Water to Gold”, pp. 193–199, Griffith, NSW, Australia, February 2006.
- P. Smith, J. U. Smith, D. S. Powlson et al., “A comparison of the performance of nine soil organic matter models using datasets from seven long-term experiments,” Geoderma, vol. 81, no. 1-2, pp. 153–225, 1997.
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