Response of soil greenhouse gas emissions to temperature and moisture across different land-use types

doi:10.3969/j.issn.1000-5641.2021.04.013

Abstract

Abstract:

In this paper, soil samples were collected from the red soil region of southern China (namely, the Sunjiaba small watershed in Yingtan, Jiangxi) across four different land-use types. Laboratory incubation experiments were subsequently carried out from June 2019 to October 2019. We used a closed chamber to measure soil greenhouse gases (CO₂, CH₄, N₂O) simultaneously with the help of an advanced greenhouse gas analyzer (Picarro-G2508). The aim was to explore the response of soil greenhouse gas emissions across different land-use types to changes in temperature and soil moisture levels under the premise of global climate change. The results showed that the global warming potential (GWP) of the four land-use types increases with paddy, orangery, forest, and upland, respectively. This suggests that greenhouse gas emissions from paddy soils have the greatest relative impact on global warming. In a temperature-controlled experiment, soil CO₂ emissions were shown to have a significant positive correlation with soil temperature. The Q₁₀ values of soil respiration coefficients for the four land-use types were: 2.61 (forest), 2.51 (upland), 3.12 (orangery), and 3.17 (paddy). Thus, paddy soil respiration has the highest temperature sensitivity, indicating that paddy soil has a higher CO₂ emission potential. Correlations were not significant between CH₄ and N₂O emissions to soil temperature. In the moisture-controlled experiment, the results indicated that soil CO₂ emissions increased at the beginning and then decreased with increasing soil moisture, with the maximum emission rate at 20% GWC (gravity water content). CH₄ emissions from paddy soils increased with soil moisture (R² = 0.8875); CH₄ fluxes from the other three land-use types, however, were not significantly related to soil moisture. The soil N₂O emissions increased at the beginning and then decreased across the soil moisture range measured; all land-use types had the highest N₂O fluxes at 25% GWC.

Key words: land-use types, greenhouse gas, red soil, temperature, moisture

CLC Number:

S154.1

Wenxiu SANG, Hualei YANG, Jianwu TANG. Response of soil greenhouse gas emissions to temperature and moisture across different land-use types[J]. Journal of East China Normal University(Natural Science), 2021, 2021(4): 109-120.

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土地利用类型	粘粒度/%	土壤pH值	有机碳/%	总氮/%	电导率/(S·m^–1)	土壤容重/ (g·cm^–3)	土壤湿度/%
林地	48.685 ± 1.151	6.33 ± 0.039	10.304 ± 0.818	1.203 ± 0.114	0.037 ± 0.006	1.11 ± 0.048	16.56 ± 2.06
旱地	33.065 ± 1.117	6.83 ± 0.036	6.286 ± 0.701	0.842 ± 0.056	0.033 ± 0.005	1.06 ± 0.019	13.47 ± 1.70
橘园	19.057 ± 1.007	6.66 ± 0.037	8.301 ± 0.647	0.920 ± 0.107	0.027 ± 0.024	1.17 ± 0.045	14.38 ± 1.26
稻田	14.279 ± 0.509	5.50 ± 0.091	23.457 ± 1.020	0.685 ± 0.087	2.335 ± 0.086	1.02 ± 0.129	25.60 ± 1.11

土地利用类型	方程	R²	p值
林地	y = 0.0230e^0.0959x	0.833	p < 0.0001
旱地	y = 0.0179e^0.0920x	0.873	p < 0.0001
橘园	y = 0.0153e^0.1138x	0.864	p < 0.0001
稻田	y = 0.0221e^0.1154x	0.822	p < 0.0001

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