Seasonal variations in soil respiration and temperature sensitivity under three land-use types in hilly areas of the Sichuan Basin
XiaoGuo Wang A C , Bo Zhu A , MeiRong Gao A , YanQiang Wang A and XunHua Zheng BA Institute of Mountain Hazards and Environment Research, Chinese Academy of Sciences, Chengdu, 610041, PR China.
B Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, PR China.
C Corresponding author. Email: xgwang@imde.ac.cn
Australian Journal of Soil Research 46(8) 727-734 https://doi.org/10.1071/SR07223
Submitted: 1 December 2007 Accepted: 1 August 2008 Published: 2 December 2008
Abstract
CO2 emissions from soils were measured under 3 land-use types at the adjacent plots of forest plantation, grassland, and cropland from January 2005 to December 2006. Mean soil CO2 efflux rates measured during the 2-year study varied from 59 to 527 mg CO2/m2.h in forest plantation, 37 to 498 mg CO2/m2.h in grassland, and 32 to 397 mg CO2/m2.h in cropland. Soil respiration in the 3 types of land-use showed a similar seasonal pattern in variation during both years, in which the single-peaked curve occurred in early summer and the minimum in winter. In particular, the date of maximum soil CO2 efflux rate in cropland occurred about 30 days earlier than in forest and grassland in both 2005 and 2006. The relationship of soil respiration rate (R) with soil temperature (T ) and soil moisture (W ) fitted well to the equation R = β0eβ1TW β2 (a, b, c were constants) than other univariate models which consider soil water content or soil temperature alone. Soil temperature and soil moisture together explained 69–92% of the temporal variation in soil respiration in the 3 land-use types. Temperature sensitivity of soil respiration (Q10) was affected positively by soil moisture of top 0.1 m layer and negatively by soil temperature at 0.05 m depth. The relationship between Q10 values and soil temperature (T ) or soil moisture (W ) indicated that a 1°C increase in soil temperature at 0.05 m depth will reduce the Q10 value by 0.07, 0.05, and 0.06 in forest, grassland, and cropland, respectively. Similarly, a 1% decrease in soil moisture of the top 0.1 m layer will reduce the Q10 value by 0.10, 0.09, and 0.11 in forest, grassland, and cropland.
Additional keywords: soil respiration, Q10 value, soil temperature, soil moisture.
Acknowledgments
This study was financially supported by the State Key & Basic Research Development Planning (No. 2005CB121108), National Natural Science Foundation of China (No. 40331014) and the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX1-SW-01-01B).
Boone RD,
Nadelhoffer KJ, Canary JD
(1998) Roots exert a strong influence on the temperature sensitivity of soil respiration. Nature 396, 570–572.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Borken W,
Xu YJ,
Brumme R, Lamersdorf N
(1999) A climate change scenario for carbon dioxide and dissolved organic carbon fluxes from a temperate forest soil: drought and rewetting effects. Soil Science Society of America Journal 63, 1848–1855.
|
CAS |
Bowden RD,
Newkirk KM, Rullo G
(1998) Carbon dioxide and methane fluxes by a forest soil under laboratory-controlled moisture and temperature conditions. Soil Biology & Biochemistry 30, 1591–1597.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Conant RT,
Klopatek JM,
Malin RC, Klopatek CC
(1998) Carbon pools and fluxes along an environmental gradient in northern Arizona. Biogeochemistry 43, 43–61.
| Crossref | GoogleScholarGoogle Scholar |
Cox PM,
Betts RA,
Jones CD,
Spall SA, Totterdel IJ
(2000) Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature 408, 184–187.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
PubMed |
Cramer W,
Kicklighter DW,
Bondeau A,
Moore B,
Churkina G,
Nemry B,
Ruimy A, Schloss A
(1999) Comparing global models of terrestrial net primary productivity (NPP): overview and key results. Global Change Biology 5(Suppl. 1), 1–15.
| Crossref | GoogleScholarGoogle Scholar |
Davidson EA,
Belk E, Boone RD
(1998) Soil water content and temperature as independent or confounded factors controlling soil respiration in a temperate mixed hardwood forest. Global Change Biology 4, 217–227.
| Crossref | GoogleScholarGoogle Scholar |
Davidson EA,
Trumbore SE, Amundson R
(2000) Soil warming and organic carbon content. Nature 408, 789–790.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
PubMed |
Del Grosso SJ,
Parton WJ,
Mosier AR,
Holland EA,
Pendall E,
Schimel DS, Ojima DS
(2005) Modeling soil CO2 emissions from ecosystems. Biogeochemistry 73, 71–91.
| Crossref | GoogleScholarGoogle Scholar |
Dörr H, Münnich KO
(1987) Annual variation in soil respiration in selected areas of the temperate forest. Tellus 39, 114–121.
Drewitt GB,
Black TA,
Nesic Z,
Humphreys ER,
Jork EM,
Swanson R,
Ethier GJ,
Griffs T, Morgenstern K
(2002) Measuring forest floor CO2 fluxes in a Douglas-fir forest. Agricultural and Forest Meteorology 110, 299–317.
| Crossref | GoogleScholarGoogle Scholar |
Fang C, Moncrieff JB
(2001) The dependence of soil CO2 efflux on temperature. Soil Biology & Biochemistry 33, 155–165.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Fernandez IJ,
Son Y,
Kraske CR,
Rustad LE, David MB
(1993) Soil carbon dioxide characteristics under different forest types and after harvest. Soil Science Society of America Journal 57, 1115–1121.
|
CAS |
Gulledge J, Schimel JP
(2000) Controls on soil carbon dioxide and methane fluxes in a variety of Taiga forest stands in interior Alaska. Ecosystems 3, 269–282.
| Crossref | GoogleScholarGoogle Scholar |
Howard DM, Howard PJA
(1993) Relationship between CO2 evolution, moisture content and temperature for a range of soil types. Soil Biology & Biochemistry 25, 1537–1546.
| Crossref | GoogleScholarGoogle Scholar |
Janssens IA, Pilegaard K
(2003) Large seasonal changes in Q10 of soil respiration in a beech forest. Global Change Biology 9, 911–918.
| Crossref | GoogleScholarGoogle Scholar |
Kirschbaum MIF
(1995) The temperature dependence of soil organic matter decomposition and effect of global warming on soil organic C storage. Soil Biology & Biochemistry 27, 753–760.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Kutsch WL, Kappen L
(1997) Aspects of carbon and nitrogen cycling in soils of the Bornhoved Lake district. II. Modeling the influence of temperature increase on soil respiration and organic carbon content in arable soils under different managements. Biogeochemistry 39, 207–224.
| Crossref | GoogleScholarGoogle Scholar |
Larionova AA,
Yermolayev AM,
Blagodatsky SA,
Rozanova LN,
Yevdokimov IV, Orlinsky DB
(1998) Soil respiration and carbon balance of gray forest soils as affected by land use. Biology and Fertility of Soils 27, 251–257.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Li HJ,
Yan JX,
Yue XF, Wang MB
(2008) Significance of soil temperature and moisture for soil respiration in a Chinese mountain area. Agricultural and Forest Meteorology 148, 490–503.
| Crossref | GoogleScholarGoogle Scholar |
Lisa JS,
Kurt J,
Tom S, Weinlang L
(2004) Intensive management modifies soil CO2 efflux in 6-year-old Pinus taeda L. stands. Forest Ecology and Management 200, 335–345.
| Crossref |
Liu H,
Zhao P,
Lu P,
Wang YS,
Lin YB, Rao XQ
(2007) Greenhouse gas fluxes from soils of different land-use types in a hilly area of South China. Agriculture, Ecosystems & Environment 124, 125–135.
| Crossref | GoogleScholarGoogle Scholar |
Lloyd J, Taylor JA
(1994) On the temperature dependence of soil respiration. Functional Ecology 8, 315–323.
| Crossref | GoogleScholarGoogle Scholar |
Lugo AE,
Sanchez AJ, Brown S
(1986) Land use and organic carbon content of some subtropical soils. Plant and Soil 96, 185–196.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
McGuire AD,
Melillo JM,
Kicklighter DW, Joyce LA
(1995) Equilibrium responses of soil carbon to climate change: Empirical and process-based estimates. Journal of Biogeography 22, 785–796.
| Crossref | GoogleScholarGoogle Scholar |
Motavalli P,
Discekici PH, Kuhn J
(2000) The impact of land clearing and agricultural practices on soil organic C fraction and CO2 efflux in the Northern Guamaquifer. Agriculture, Ecosystems & Environment 79, 17–27.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Orchard VA, Cook FJ
(1983) Relationship between soil respiration and soil moisture. Soil Biology & Biochemistry 15, 447–453.
| Crossref | GoogleScholarGoogle Scholar |
Paustian K,
Six J,
Elliott ET, Hunt HW
(2000) Management options for reducing CO2 emissions from agricultural soils. Biogeochemistry 48, 147–163.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Pavelka M,
Acosta M,
Marek MV,
Kutsch W, Janous D
(2007) Dependence of the Q10 values on the depth of the soil temperature measuring point. Plant and Soil 292, 171–179.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Post WM, Kwon KC
(2000) Soil carbon sequestration and land use change: processes and potential. Global Change Biology 6, 317–327.
| Crossref | GoogleScholarGoogle Scholar |
Powers JS,
Read JM,
Denslow JS, Guzman SM
(2004) Estimating soil carbon fluxes following land-cover change: a test of some critical assumptions for a region in Costa Rica. Global Change Biology 10, 170–181.
| Crossref | GoogleScholarGoogle Scholar |
Qi Y, Xu M
(2001) Separating the effects of moisture and temperature on soil CO2 efflux in a coniferous forest in the Sierra Nevada mountains. Plant and Soil 237, 15–23.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Qi Y,
Xu M, Wu JG
(2002) Temperature sensitivity of soil respiration and its effects on ecosystem carbon budget: non-linearity begets surprises. Ecological Modelling 153, 131–142.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Raich JW,
Rastetter EB,
Melillo JM,
Kicklighter DW,
Steudler PA,
Peterson BJ,
Grace AL,
Moore B, Vörösmarty CJ
(1991) Potential net primary productivity in South America: application of a global model. Ecological Applications 1, 399–429.
| Crossref | GoogleScholarGoogle Scholar |
Raich JW, Schlesinger WH
(1992) The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate. Tellus 44, 81–99.
Raich JW, Tufekcioglu A
(2000) Vegetation and soil respiration: Correlations and controls. Biogeochemistry 48, 71–90.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Schimel D,
Braswell BH, Vemap P
(1997) Continental scale variability in ecosystem processes: models, data, and the role of disturbance. Ecological Monographs 67, 251–271.
Schleser GH
(1982) The response of CO2 evolution from soils to global temperature changes. Zeitschrift fur Naturforschung. Section C. Biosciences 37a, 287–291.
|
CAS |
Schlesinger WH, Andrews JA
(2000) Soil respiration and the global carbon cycle. Biogeochemistry 48, 7–20.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Schwendenmann L,
Veldkamp E,
Brenes T,
O’Bien J, Mackensen J
(2003) Spatial and temporal variation in soil CO2 efflux in an old-growth neotropical rain forest, La Selva, Costa Rica. Biogeochemistry 64, 111–128.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Sparling GP,
West AW, Reynolds J
(1989) Influence of soil moisture regime on the respiration response of soils subjected to osmotic stress. Australian Journal of Soil Research 27, 161–168.
| Crossref | GoogleScholarGoogle Scholar |
Tjoelker MG,
Oleksyn J, Reich PB
(2001) Modeling respiration of vegetation: evidence for a general temperature-dependent Q10. Global Change Biology 7, 223–230.
| Crossref | GoogleScholarGoogle Scholar |
Trumbore SE,
Davidson EA,
Camargo PB,
Nepstad DC, Martinelli LA
(1995) Below-ground cycling of carbon in forests and pastures of eastern Amazonian. Global Biogeochemical Cycles 9, 515–528.
| Crossref | GoogleScholarGoogle Scholar |
CAS |
Xu M, Qi Y
(2001a) Soil-surface CO2 efflux and its spatial and temporal variations in a young ponderosa pine plantation in northern California. Global Change Biology 7, 667–677.
| Crossref | GoogleScholarGoogle Scholar |
Xu M, Qi Y
(2001b) Spatial and seasonal variations of Q10 determined by soil respiration measurements at a Sierra Nevadan forest. Global Biogeochemical Cycle 15, 687–696.
|
CAS |
Crossref |
Young R,
Wilson BR,
Malem M, Alston C
(2005) Carbon storage in the soils and vegetation of contrasting land uses in northern New South Wales, Australia. Australian Journal of Soil Research 43, 21–31.
| Crossref | GoogleScholarGoogle Scholar |
CAS |