Chow A T, Tanji K K, Gao S et al. Temperature, water content and wet-dry cycle effects on DOC production and carbon mineralization in agricultural peat soils[J]. Soil Biology & Biochemistry, 2006, 38(3): 477-488.
Von Lützow M, Kgel-Knabner I. Temperature sensitivity of soil organic matter decomposition — what do we know?[J]. Biology and Fertility of Soils, 2009, 46(1): 1-15.
[12]
Reth S, Reichstein M, Falge E. The effect of soil water content, soil temperature, soil pH-value and the root mass on soil CO2 efflux - a modified model[J]. Plant and Soil, 2005, 268(1): 21-33.
[13]
Wildung R E, Garland T R, Buschbom R L. The interdependent effects of soil temperature and water content on soil respiration rate and plant root decomposition in arid grassland soils[J]. Soil Biology & Biochemistry, 1975, 7(6): 373-378.
Fang C, Moncrieff J B. The dependence of soil CO2 efflux on temperature[J]. Soil Biology & Biochemistry, 2001, 33(2): 155-165.
[19]
Reichstein M, Bednorz F, Broll G et al. Temperature dependence of carbon mineralisation: conclusions from a long-term incubation of subalpine soil samples[J]. Soil Biology & Biochemistry, 2000, 32(7): 947-958.
[20]
Fierer N, Schimel J P. Effects of drying-rewetting frequency on soil carbon and nitrogen transformations[J]. Soil Biology & Biochemistry, 2002, 34(6): 777-787.
Giardina C P, Ryan M G. Evidence that decomposition rates of organic carbon in mineral soil do not vary with temperature[J]. Nature, 2000, 404(6780): 858-861.
Lundquist E J, Jackson L E, Scow K M. Wet-dry cycles affect dissolved organic carbon in two California agricultural soils[J]. Soil Biology & Biochemistry, 1999, 31(7): 1031-1038.