CO"2 emission in an intensively cultivated loam as affected by long-term application of organic manure and nitrogen fertilizer [An article from: Soil Biology and Biochemistry]
Description
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Description:
A long-term field experiment was conducted to examine the influence of mineral fertilizer and organic manure on the equilibrium dynamics of soil organic C in an intensively cultivated fluvo-aquic soil in the Fengqiu State Key Agro-Ecological Experimental Station (Fengqiu county, Henan province, China) since September 1989. Soil CO"2 flux was measured during the maize and wheat growing seasons in 2002-2003 and 2004 to evaluate the response of soil respiration to additions and/or alterations in mineral fertilizer, organic manure and various environmental factors. The study included seven treatments: organic manure (OM), half-organic manure plus half-fertilizer N (NOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (PK) and control (CK). Organic C in soil and the soil heavy fraction (organo-mineral complex) was increased from 4.47 to 8.61mgCg^-^1 and from 3.32 to 5.68mgCg^-^1, respectively, after the 13yr application of organic manure. In contrast, organic C and the soil heavy fraction increased in NPK soil to only 5.41 and 4.38mgCg^-^1, respectively. In the CK treatment, these parameters actually decreased from the initial C concentrations (4.47 and 3.32mgCg^-^1) to 3.77 and 3.11mgCg^-^1, respectively. Therefore, organic manure efficiently elevated soil organic C. However, only 66% of the increased soil organic C was combined with clay minerals in the OM treatment. Cumulative soil CO"2 emissions from inter-row soil in the OM and NPK treatments were 228 and 188gCm^-^2 during the 2002 maize growing season, 132 and 123gCm^-^2 during the 2002/2003 wheat growing season, and 401 and 346gCm^-^2yr^-^1 in 2002-2003, respectively. However, during the 2004 maize growing season, cumulative soil CO"2 emissions were as high as 617 and 556gCm^-^2, respectively, due to the contribution of rhizosphere respiration. The addition of organic manure contributed to a 16% increase in soil CO"2 emission in 2002-2003 (compared to NPK), where only 27%, 36% and 24% of applied organic C was released as CO"2 during the 2002 and 2004 maize growing seasons and in 2002-2003, respectively. During the 2002/2003 wheat growing season, soil CO"2 flux was significantly affected by soil temperature below 20^oC, but by soil moisture (WFPS) during the 2004 maize growing season at soil temperatures above 18^oC. Optimum soil WFPS for soil CO"2 flux was approximately 70%. When WFPS was below 50%, it no longer had a significant impact on soil CO"2 flux during the 2002 maize growing season. This study indicates the application of organic manure composted with wheat straw may be a preferred strategy for increasing soil organic C and sequestering C in soil.
Description:
A long-term field experiment was conducted to examine the influence of mineral fertilizer and organic manure on the equilibrium dynamics of soil organic C in an intensively cultivated fluvo-aquic soil in the Fengqiu State Key Agro-Ecological Experimental Station (Fengqiu county, Henan province, China) since September 1989. Soil CO"2 flux was measured during the maize and wheat growing seasons in 2002-2003 and 2004 to evaluate the response of soil respiration to additions and/or alterations in mineral fertilizer, organic manure and various environmental factors. The study included seven treatments: organic manure (OM), half-organic manure plus half-fertilizer N (NOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (PK) and control (CK). Organic C in soil and the soil heavy fraction (organo-mineral complex) was increased from 4.47 to 8.61mgCg^-^1 and from 3.32 to 5.68mgCg^-^1, respectively, after the 13yr application of organic manure. In contrast, organic C and the soil heavy fraction increased in NPK soil to only 5.41 and 4.38mgCg^-^1, respectively. In the CK treatment, these parameters actually decreased from the initial C concentrations (4.47 and 3.32mgCg^-^1) to 3.77 and 3.11mgCg^-^1, respectively. Therefore, organic manure efficiently elevated soil organic C. However, only 66% of the increased soil organic C was combined with clay minerals in the OM treatment. Cumulative soil CO"2 emissions from inter-row soil in the OM and NPK treatments were 228 and 188gCm^-^2 during the 2002 maize growing season, 132 and 123gCm^-^2 during the 2002/2003 wheat growing season, and 401 and 346gCm^-^2yr^-^1 in 2002-2003, respectively. However, during the 2004 maize growing season, cumulative soil CO"2 emissions were as high as 617 and 556gCm^-^2, respectively, due to the contribution of rhizosphere respiration. The addition of organic manure contributed to a 16% increase in soil CO"2 emission in 2002-2003 (compared to NPK), where only 27%, 36% and 24% of applied organic C was released as CO"2 during the 2002 and 2004 maize growing seasons and in 2002-2003, respectively. During the 2002/2003 wheat growing season, soil CO"2 flux was significantly affected by soil temperature below 20^oC, but by soil moisture (WFPS) during the 2004 maize growing season at soil temperatures above 18^oC. Optimum soil WFPS for soil CO"2 flux was approximately 70%. When WFPS was below 50%, it no longer had a significant impact on soil CO"2 flux during the 2002 maize growing season. This study indicates the application of organic manure composted with wheat straw may be a preferred strategy for increasing soil organic C and sequestering C in soil.
