Seasonal Dynamics of Soil Respiration of Quercus variabilis Plantation in Hilly Area of Xiaolangdi Reservoir of Yellow River

ZHAO Na; MENG Ping; ZHANG Jin-song; LU Sen; SONG Wen-chen

Volume 29 Issue 5

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Seasonal Dynamics of Soil Respiration of Quercus variabilis Plantation in Hilly Area of Xiaolangdi Reservoir of Yellow River

1.
Research Institute of Forestry, Chinese Academy of Forestry, State Key Laboratory of Tree Genetics and Breeding, Beijing 100091, China
2.
School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
3.
College of Forestry, Beijing Forestry University, Beijing 100083, China

Received Date: 2014-02-20

Abstract

[Objective] To separate and quantify the total, autotrophic and heterotrophic soil respiration. [Method] By the method of infrared gas exchange analyzer in trenching-plot, the total soil respiration (RS), autotrophic (RA) and heterotrophic respiration (RH) in a Quercus variabilis plantation were investigated in hilly area of Xiaolangdi Reservoir of Yellow River. The seasonal dynamics contribution rate and the environmental factors of RS, RA, and RH were determined. [Result] The results showed that the RS, RA and RH varied with the season, the maximum and the minimum were observed at summer and winter, respectively. Significant exponential relationships were obtained between RS, RA and RH and soil temperature at 5 cm (PRA, RH, and Rs, (Q10) were calculated as 3.40, 2.90 and 2.45 respectively. The RS, RA and RH were significantly lined with soil volumetric water content at 0~10 cm (PRs and RA had a linear correlation with soil pore water conductivity at 0~10 cm (PQ10 of Rs and RH had the highest value in summer and the lowest in winter. Compared with Q10 in Rs and RH, the seasonal variation in Q10 of RA presented opposite trend. The estimated contributions of RA and RH on Rs were 13.23%~37.33% and 62.67%~86.76%, respectively. The contribution of RA on Rs was consistent with soil temperature seasonally. In this study, the annual CO2 flux of Rs, RH and RA in the Q. variabilis plantation were 1 616.41, 1 199.39 and 417.02 g·m-2·a-1, respectively. [Conclusion] As the main component of total soil respiration, the heterotrophic respiration was significantly correlated with environmental factors, which could influence the overall emission from soil surface and provide theoretical support for further research about carbon cycle and energy exchange in forest ecosystems.
- Quercus variabilis,
- autotrophic respiration,
- heterotrophic respiration,
- Q₁₀,
- seasonal dynamics,
- trenching-plot method

References

[1]	Schlesinger W H, Andrews J A. Soil respiration and the global carbon cycle[J]. Biogeochemistry, 2000, 48(1):7-20.
[2]	Bond-Lamberty B, Thomson A M. Temperature-associated increases in the global soil respiration record[J]. Nature, 2010, 464(7288):579-582.
[3]	Luo Y Q, Zhou X H. Soil Respiration and the Environment[M]. New York:Academic Press, 2006:17-28.
[4]	Harmon M E, Bond-Lamberty B, Tang J, et al. Heterotrophic respiration in disturbed forests:A review with examples from North America[J]. Journal of Geophysical Research, 2011, 116(G4):1296-1300.
[5]	Schindlbacher A, Zechmeister-Boltenstern S, Jandl R. Carbon losses due to soil warming:do autotrophic and heterotrophic soil respiration respond equally?[J]. Global Change Biology, 2009, 15(4):901-913.
[6]	Maier M, Schack-Kirchner H, Hildebrand E E, et al. Pore-space CO₂ dynamics in a deep, well-aerated soil[J]. European Journal of Soil Science, 2010, 61:877-887.
[7]	Kuzyakov Y. Sources of CO₂ from soil and review of partitioning methods[J]. Soil Biology and Biochemistry, 2006, 38(3):425-448.
[8]	Hanson P J, Edwards N T, Garten C T, et al. Separating root and soil microbial contributions to soil respiration:A review of methods and observations[J]. Biogeochemistry, 2000, 48(1):115-146.
[9]	Subke J A, Inglima I, Francesca Cotrufo M F. Trends and methodological impacts in soil CO₂ efflux partitioning[J]. Global Change Biology, 2006, 12(6):921-943.
[10]	Bond-Lamberty B, Wang C, Gower S T. Contribution of root respiration to soil surface CO₂ flux in a boreal black spruce chronosequence[J]. Tree Physiology, 2004, 24(12):1387-1395.
[11]	Lee M S, Nakane K, Nakatsubo T, et al. Seasonal changes in the contribution of root respiration to total soil respiration in a cool-temperate deciduous forest[J]. Plant and Soil, 2003, 255:311-318.
[12]	王平, 张劲松, 孟平, 等. 华北低丘山地栓皮栎人工林土壤呼吸变化特征及其与撂荒地的差异[J]. 中国农业气象, 2011, 32(3):346-349.
[13]	王鹤松, 张劲松, 孟平, 等. 华北山区非主要生长季典型人工林土壤呼吸变化特征[J].林业科学研究, 2007, 20(6):820-825.
[14]	Xu M, Qi Y. Soil-surface CO₂ efflux and its spatial and temporal variations in a young ponderosa pine plantation in northern California[J]. Global Change Biology, 2001, 7(6):667-677.
[15]	Lloyd J, Taylor J A. On the temperature dependence of soil respiration[J]. Functional Ecology, 1994:315-323.
[16]	Nakane K, Kohno T, Horikoshi T. Root respiration rate before and just after clear-felling in a mature, deciduous, broad-leaved forest[J]. Ecological Research, 1996, 11(2):111-119.
[17]	Martin J G, Bolstad, P V. Annual soil respiration in broadleaf forests of northern Wisconsin:influence of moisture and site biological, chemical, and physical characteristics[J]. Biogeochemistry, 2005, 73(1):149-182.
[18]	罗璐, 申国珍, 谢宗强, 等. 神农架海拔梯度上4种典型森林的土壤呼吸组分及其对温度的敏感性[J]. 植物生态学报, 2011, 35(7):722-730.
[19]	汪金松, 范娟, 赵秀海, 等. 米槠和杉木人工林土壤呼吸及其组分分析[J]. 林业科学, 2013, 49(2):1-7.
[20]	Kuzyakov Y, Gabrichkova O. Time lag between photosynthesis and carbon dioxide efflux from soil:a review of mechanisms and controls[J]. Global Change Biology, 2010, 16(12), 3386-3406.
[21]	Burton A, Pregitzer K, Ruess R, et al. Root respiration in North American forests:effects of nitrogen concentration and temperature across biomes[J]. Oecologia, 2002, 131(4):559-568.
[22]	Lee N, Koo J W, Noh N J, et al. Autotrophic and heterotrophic respiration in needle fir and Quercus-dominated stands in a cool-temperate forest, central Korea[J]. Journal of plant research, 2010, 123(4):485-495.
[23]	Xu M, Qi Y. Spatial and seasonal variations of Q₁₀ determined by soil respiration measurements at a Sierra Nevadan forest[J]. Global Biogeochemical Cycles, 2001, 15(3):687-696.
[24]	Adviento-Borbe M A, Doran J W, Drijber R A, et al. Soil electrical conductivity and water content affect nitrous oxide and carbon dioxide emissions in intensively managed soils[J]. Journal of environmental quality, 2006, 35(6):1999-2010.
[25]	陈光水, 杨玉盛, 吕萍萍, 等. 中国森林土壤呼吸模式[J]. 生态学报, 2008, 28(4):1748-1761.
[26]	Curiel-Yuste J, Janssens I A, Carrara A, et al. Annual Q₁₀ of soil respiration reflects plant phenological patterns as well as temperature sensitivity[J]. Global Change Biology, 2004, 10(2):161-169.
[27]	Janssens I A, Pilegaard K I M. Large seasonal changes in Q₁₀ of soil respiration in a beech forest[J]. Global Change Biology, 2003, 9(6):911-918.
[28]	Tomotsune M, Yoshitake S, Watanabe S, et al. Separation of root and heterotrophic respiration within soil respiration by trenching, root biomass regression, and root excising methods in a cool-temperate deciduous forest in Japan cool-temperate deciduous forest in Japan[J]. Ecological research, 2013, 28(2):259-269.
[29]	Feng W, Zou X, Schaefer D. Above-and belowground carbon inputs affect seasonal variations of soil microbial biomass in a subtropical monsoon forest of southwest China[J]. Soil Biology and Biochemistry, 2009, 41(5):978-983.
[30]	Ngao J, Longdoz B, Granier A, et al. Estimation of autotrophic and heterotrophic components of soil respiration by trenching is sensitive to corrections for root decomposition and changes in soil water content[J]. Plant and Soil, 2007, 301(1-2):99-110.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Seasonal Dynamics of Soil Respiration of Quercus variabilis Plantation in Hilly Area of Xiaolangdi Reservoir of Yellow River

1. Research Institute of Forestry, Chinese Academy of Forestry, State Key Laboratory of Tree Genetics and Breeding, Beijing 100091, China

2. School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China

3. College of Forestry, Beijing Forestry University, Beijing 100083, China

Received Date: 2014-02-20

Abstract: [Objective] To separate and quantify the total, autotrophic and heterotrophic soil respiration. [Method] By the method of infrared gas exchange analyzer in trenching-plot, the total soil respiration (RS), autotrophic (RA) and heterotrophic respiration (RH) in a Quercus variabilis plantation were investigated in hilly area of Xiaolangdi Reservoir of Yellow River. The seasonal dynamics contribution rate and the environmental factors of RS, RA, and RH were determined. [Result] The results showed that the RS, RA and RH varied with the season, the maximum and the minimum were observed at summer and winter, respectively. Significant exponential relationships were obtained between RS, RA and RH and soil temperature at 5 cm (PRA, RH, and Rs, (Q10) were calculated as 3.40, 2.90 and 2.45 respectively. The RS, RA and RH were significantly lined with soil volumetric water content at 0~10 cm (PRs and RA had a linear correlation with soil pore water conductivity at 0~10 cm (PQ10 of Rs and RH had the highest value in summer and the lowest in winter. Compared with Q10 in Rs and RH, the seasonal variation in Q10 of RA presented opposite trend. The estimated contributions of RA and RH on Rs were 13.23%~37.33% and 62.67%~86.76%, respectively. The contribution of RA on Rs was consistent with soil temperature seasonally. In this study, the annual CO2 flux of Rs, RH and RA in the Q. variabilis plantation were 1 616.41, 1 199.39 and 417.02 g·m-2·a-1, respectively. [Conclusion] As the main component of total soil respiration, the heterotrophic respiration was significantly correlated with environmental factors, which could influence the overall emission from soil surface and provide theoretical support for further research about carbon cycle and energy exchange in forest ecosystems.

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Reference (30)

[1]	Schlesinger W H, Andrews J A. Soil respiration and the global carbon cycle[J]. Biogeochemistry, 2000, 48(1):7-20.
[2]	Bond-Lamberty B, Thomson A M. Temperature-associated increases in the global soil respiration record[J]. Nature, 2010, 464(7288):579-582.
[3]	Luo Y Q, Zhou X H. Soil Respiration and the Environment[M]. New York:Academic Press, 2006:17-28.
[4]	Harmon M E, Bond-Lamberty B, Tang J, et al. Heterotrophic respiration in disturbed forests:A review with examples from North America[J]. Journal of Geophysical Research, 2011, 116(G4):1296-1300.
[5]	Schindlbacher A, Zechmeister-Boltenstern S, Jandl R. Carbon losses due to soil warming:do autotrophic and heterotrophic soil respiration respond equally?[J]. Global Change Biology, 2009, 15(4):901-913.
[6]	Maier M, Schack-Kirchner H, Hildebrand E E, et al. Pore-space CO₂ dynamics in a deep, well-aerated soil[J]. European Journal of Soil Science, 2010, 61:877-887.
[7]	Kuzyakov Y. Sources of CO₂ from soil and review of partitioning methods[J]. Soil Biology and Biochemistry, 2006, 38(3):425-448.
[8]	Hanson P J, Edwards N T, Garten C T, et al. Separating root and soil microbial contributions to soil respiration:A review of methods and observations[J]. Biogeochemistry, 2000, 48(1):115-146.
[9]	Subke J A, Inglima I, Francesca Cotrufo M F. Trends and methodological impacts in soil CO₂ efflux partitioning[J]. Global Change Biology, 2006, 12(6):921-943.
[10]	Bond-Lamberty B, Wang C, Gower S T. Contribution of root respiration to soil surface CO₂ flux in a boreal black spruce chronosequence[J]. Tree Physiology, 2004, 24(12):1387-1395.
[11]	Lee M S, Nakane K, Nakatsubo T, et al. Seasonal changes in the contribution of root respiration to total soil respiration in a cool-temperate deciduous forest[J]. Plant and Soil, 2003, 255:311-318.
[12]	王平, 张劲松, 孟平, 等. 华北低丘山地栓皮栎人工林土壤呼吸变化特征及其与撂荒地的差异[J]. 中国农业气象, 2011, 32(3):346-349.
[13]	王鹤松, 张劲松, 孟平, 等. 华北山区非主要生长季典型人工林土壤呼吸变化特征[J].林业科学研究, 2007, 20(6):820-825.
[14]	Xu M, Qi Y. Soil-surface CO₂ efflux and its spatial and temporal variations in a young ponderosa pine plantation in northern California[J]. Global Change Biology, 2001, 7(6):667-677.
[15]	Lloyd J, Taylor J A. On the temperature dependence of soil respiration[J]. Functional Ecology, 1994:315-323.
[16]	Nakane K, Kohno T, Horikoshi T. Root respiration rate before and just after clear-felling in a mature, deciduous, broad-leaved forest[J]. Ecological Research, 1996, 11(2):111-119.
[17]	Martin J G, Bolstad, P V. Annual soil respiration in broadleaf forests of northern Wisconsin:influence of moisture and site biological, chemical, and physical characteristics[J]. Biogeochemistry, 2005, 73(1):149-182.
[18]	罗璐, 申国珍, 谢宗强, 等. 神农架海拔梯度上4种典型森林的土壤呼吸组分及其对温度的敏感性[J]. 植物生态学报, 2011, 35(7):722-730.
[19]	汪金松, 范娟, 赵秀海, 等. 米槠和杉木人工林土壤呼吸及其组分分析[J]. 林业科学, 2013, 49(2):1-7.
[20]	Kuzyakov Y, Gabrichkova O. Time lag between photosynthesis and carbon dioxide efflux from soil:a review of mechanisms and controls[J]. Global Change Biology, 2010, 16(12), 3386-3406.
[21]	Burton A, Pregitzer K, Ruess R, et al. Root respiration in North American forests:effects of nitrogen concentration and temperature across biomes[J]. Oecologia, 2002, 131(4):559-568.
[22]	Lee N, Koo J W, Noh N J, et al. Autotrophic and heterotrophic respiration in needle fir and Quercus-dominated stands in a cool-temperate forest, central Korea[J]. Journal of plant research, 2010, 123(4):485-495.
[23]	Xu M, Qi Y. Spatial and seasonal variations of Q₁₀ determined by soil respiration measurements at a Sierra Nevadan forest[J]. Global Biogeochemical Cycles, 2001, 15(3):687-696.
[24]	Adviento-Borbe M A, Doran J W, Drijber R A, et al. Soil electrical conductivity and water content affect nitrous oxide and carbon dioxide emissions in intensively managed soils[J]. Journal of environmental quality, 2006, 35(6):1999-2010.
[25]	陈光水, 杨玉盛, 吕萍萍, 等. 中国森林土壤呼吸模式[J]. 生态学报, 2008, 28(4):1748-1761.
[26]	Curiel-Yuste J, Janssens I A, Carrara A, et al. Annual Q₁₀ of soil respiration reflects plant phenological patterns as well as temperature sensitivity[J]. Global Change Biology, 2004, 10(2):161-169.
[27]	Janssens I A, Pilegaard K I M. Large seasonal changes in Q₁₀ of soil respiration in a beech forest[J]. Global Change Biology, 2003, 9(6):911-918.
[28]	Tomotsune M, Yoshitake S, Watanabe S, et al. Separation of root and heterotrophic respiration within soil respiration by trenching, root biomass regression, and root excising methods in a cool-temperate deciduous forest in Japan cool-temperate deciduous forest in Japan[J]. Ecological research, 2013, 28(2):259-269.
[29]	Feng W, Zou X, Schaefer D. Above-and belowground carbon inputs affect seasonal variations of soil microbial biomass in a subtropical monsoon forest of southwest China[J]. Soil Biology and Biochemistry, 2009, 41(5):978-983.
[30]	Ngao J, Longdoz B, Granier A, et al. Estimation of autotrophic and heterotrophic components of soil respiration by trenching is sensitive to corrections for root decomposition and changes in soil water content[J]. Plant and Soil, 2007, 301(1-2):99-110.

Seasonal Dynamics of Soil Respiration of Quercus variabilis Plantation in Hilly Area of Xiaolangdi Reservoir of Yellow River

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通讯作者: 陈斌, bchen63@163.com

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Seasonal Dynamics of Soil Respiration of Quercus variabilis Plantation in Hilly Area of Xiaolangdi Reservoir of Yellow River

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