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

SANG Wenxiu; YANG Hualei; TANG Jianwu

doi:10.3969/j.issn.1000-5641.2021.04.013

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SANG Wenxiu, YANG Hualei, TANG Jianwu. Response of soil greenhouse gas emissions to temperature and moisture across different land-use types[J]. Journal of East China Normal University (Natural Sciences), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013

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SANG Wenxiu, YANG Hualei, TANG Jianwu. Response of soil greenhouse gas emissions to temperature and moisture across different land-use types[J]. Journal of East China Normal University (Natural Sciences), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013

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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

1.
State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai　200241, China
2.
Institute of Eco-Chongming, Shanghai　202162, China

Received Date: 2020-07-30
Publish Date: 2021-07-25

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.
- land-use types,
- greenhouse gas,
- red soil,
- temperature,
- moisture

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References

[1]	ZAVAREH K. Extreme precipitation events and the applicability of global climate models to the study of floods and droughts [J]. Mathematics and Computers in Simulation, 1997, 43(3): 261-268.
[2]	严中伟, 杨赤. 近几十年中国极端气候变化格局 [J]. 气候与环境研究, 2000, 5(3): 267-272.
[3]	GORNITZ V, COUCH S, HARTIG E K. Impacts of sea level rise in new york city metropolitan area [J]. Global and Planetary Change, 2001, 32(1): 61-88.
[4]	刘吉峰, 丁裕国, 江志红. 全球变暖加剧对极端气候概率影响的初步探讨 [J]. 高原气象, 2007, 26(4): 837-842.
[5]	BEIN T, KARAGIANNIDIS C, QUINTEL M. Climate change, global warming, and intensive care [J]. Intensive Care Medicine, 2019, 46(9): 485-487.
[6]	IPCC. Climate Change 2007: The Physical Science Basis [M]. Cambridge: Cambridge University Press, 2007.
[7]	DE J B, ANAYA C, MASERA O, et al. Greenhouse gas emissions between 1993 and 2002 from land-use change and forestry in Mexico [J]. Forest Ecology and Management, 2010, 260(10): 1689-1701.
[8]	WHALEN S C, REEBURGH W S. Moisture and temperature sensitivity of CH₄ oxidation in boreal soils [J]. Soil Biology and Biochemistry, 1996, 28(10/11): 1271-1281.
[9]	GUNTIÑASAABA M E. Effects of moisture and temperature on net soil nitrogen mineralization: A laboratory study [J]. European Journal of Soil Biology, 2012, 48(1): 73-80.
[10]	苏王娟, 李勇, 石辉, 等. 温度和水分对长沙市丘陵马尾松林红壤N₂O排放的影响—一个室内培养试验 [J]. 林业科学, 2013, 49(3): 152-158.
[11]	顾航, 肖凡书, 贺志理, 等. 湿地微生物介导的甲烷排放机制 [J]. 微生物学报, 2018, 58(4): 618-632.
[12]	LINDSEY E R, FERNANDEZ I J. Experimental soil warming effects on CO₂ and CH₄ flux from a low elevation spruce–fir forest soil in Maine, USA [J]. Global Change Biology, 1998, 4(6): 597-605.
[13]	XU L, BALDOCCHI D D, TANG J. How soil moisture, rain pulses and growth alter the response of ecosystem respiration to temperature [J]. Global Biogeochemical Cycles, 2004, 18(4): GB4002.
[14]	TANG J, BOLSTAD P V, DESAI A R, et al. Ecosystem respiration and its components in an old-growth northern forest in the Great Lakes region of the United States [J]. Agricultural and Forest Meteorology, 2008, 148(2): 171-185.
[15]	PAVELKA M, ACOSTA M, MAREK M V, et al. Dependence of the Q₁₀ values on the depth of the soil temperature measuring point [J]. Plant and Soil, 2007, 292(1/2): 171-179.
[16]	CAREY J C, TANG J, TEMPLER P H, et al. Temperature response of soil respiration largely unaltered with experimental warming [J]. Proceedings of the National Academy of Sciences of the USA (PNAS), 2016, 113(48): 13797-13802.
[17]	蒋高明, 黄银晓. 北京山区辽东栎林土壤释放CO₂的模拟实验研究 [J]. 生态学报, 1995, 17(5): 477-482.
[18]	LINN D M, DORAN J W. Effect of water-filled pore space on carbon dioxide and nitrous oxide production in tilled and nontilled soils [J]. Soil Science Society of America, 1984, 48(6): 1267-1272.
[19]	PATRICK M, ERIC F L. Global forest transition: Prospects for an end to deforestation, Michigan [J]. Annual Review of Environment and Resources, 2011, 36(1): 343-371.
[20]	BRUNN G J, HUDSON C C, SEKULI A, et al. Phosphorylation of the translational repressor PHAS-I by the mammalian target of rapamycin [J]. Science, 1997, 277(5322): 99-101.
[21]	YAN X, INDERWILDI O R, KING D A. Biofuels and synthetic fuels in the US and China: A review of Well-to-Wheel energy use and greenhouse gas emissions with the impact of land-use change [J]. Energy Environmental Science, 2010, 3(2): 190-197.
[22]	鲁江, 骆检兰, 苏正伟, 等. 亚热带红壤区不同土地利用方式土壤呼吸研究 [J]. 农业现代化研究, 2012, 33(6): 115-118.
[23]	伍玉鹏, 刘田, 彭其安, 等. 氮肥配施下不同C/N作物残渣还田对红壤温室气体排放的影响 [J]. 农业环境科学学报, 2014, 33(10): 2053-2062.
[24]	刘玲玲. 千烟洲红壤丘陵区土壤主要温室气体排放通量研究 [D]. 北京: 北京师范大学, 2007.
[25]	WANYAMA I, RUFINO M C, PELSTER D E, et al. Land use, land use history, and soil type affect soil greenhouse gas fluxes from agricultural landscapes of the east african highlands [J]. Journal of Geophysical Research: Biogeosciences, 2018, 123(3): 976-990.
[26]	ZHANG L H, SONG L P, WANG B C, et al. Co-effects of salinity and moisture on CO₂ and N₂O emissions of laboratory incubated salt-affected soils from different vegetation types [J]. Geoderma, 2018, 332(6): 109-120.
[27]	MA S S, XIONG J P, CUI R X, et al. Effects of intermittent aeration on greenhouse gas emissions and bacterial community succession during large-scale membrane-covered aerobic composting [J]. Journal of Cleaner Production, 2020, 266: 121551. doi: 10.1016/j.jclepro.2020.121551
[28]	MARTIN R M, MOSEMAN V S. Greenhouse gas fluxes vary between phragmites Australis and native vegetation zones in coastal wetlands along a salinity gradient [J]. Wetlands, 2015, 35(6): 1021-1031.
[29]	ZSCHORNACK T, DA ROSA C M, PEDROSO G M, et al. Mitigation of yield-scaled greenhouse gas emissions in subtropical paddy rice under alternative irrigation systems [J]. Nutrient Cycling Agroecosystems, 2016, 105(1): 61-73.
[30]	ROSENTRETER J A, MAHER D T, ERLER D V, et al. Seasonal and temporal CO₂ dynamics in three tropical mangrove creeks-A revision of global mangrove CO₂ emissions [J]. Geochimica et Cosmochimica Acta, 2018, 222(1): 729-745.
[31]	王巧环, 任玉芬, 孟龄, 等. 元素分析仪同时测定土壤中全氮和有机碳 [J]. 分析试验室, 2013(10): 41-45.
[32]	陈莹璐, 张玉柱, 谭子辉, 等. MS2000 和 LS13320 激光粒度仪测定沉积物粒度结果的差异 [J]. 中山大学学报(自然科学版), 2018(4): 48-55.
[33]	RISK D, KELLMAN L, BELTRAMI H. Carbon dioxide in soil profiles: Production and temperature dependence [J]. Geophysical Research Letters, 2002, 29(6): 1-4.
[34]	SCHǛTZ H, SEILER W, CONRAD R. Influence of soil temperature on methane emission from rice paddy fields [J]. Biogeochemistry, 1990, 11(2): 77-95.
[35]	丁维新, 蔡祖聪. 温度对甲烷产生和氧化的影响 [J]. 应用生态学报, 2003, 14(4): 604-608.
[36]	MAAG M, VINTHER F P. Nitrous oxide emission by nitrification and denitrification in different soil types and at different soil moisture contents and temperatures [J]. Applied Soil Ecology, 1996, 4(1): 5-14.
[37]	DORLAND S, BEAUCHAMP E G. Denitrification and ammonification at low soil temperatures [J]. Canadian Journal of Soil Science, 1991, 71(3): 293-303.
[38]	STOTTLEMYER R, TOCZYDLOWSKI D. Nitrogen mineralization in a mature boreal forest, Isle Royale, Michigan [J]. Journal of Environmental Quality, 1999, 28(2): 709-720.
[39]	郑循华, 王明星. 温度对农田N₂O产生与排放的影响 [J]. 环境科学, 1997, 18(5): 1-5.
[40]	CASTALDI S. Responses of nitrous oxide, dinitrogen and carbon dioxide production and oxygen consumption to temperature in forest and agricultural light-textured soils determined by model experiment [J]. Biology and Fertility of Soils, 2000, 32(1): 67-72.
[41]	高进长, 苏永红. 土壤呼吸对不同来源水分响应的研究进展 [J]. 干旱区研究, 2012, 29(6): 1014-1021.
[42]	戴万宏, 王益权, 黄耀, 等. 农田生态系统土壤CO₂释放研究 [J]. 西北农林科技大学学报(自然科学版), 2005, 32(12): 1-7.
[43]	邓东周, 范志平, 王红, 等. 土壤水分对土壤呼吸的影响 [J]. 林业科学研究, 2009, 22(5): 722-727.
[44]	王建林, 赵风华, 欧阳竹. 灌溉量对灌浆期麦田土壤呼吸的影响 [J]. 华北农学报, 2010, 25(3): 186-189.
[45]	PONNAMPERUMA F N. Organic matter and rice: Straw as source of nutrients for wetland rice [R]. Manila (Philippines): International Rice Research Institute Publication, 1984: 117-136.
[46]	KUCERA C L, KIRKHAM D R. Soil respiration studies in tall grassprairie in Missourt [J]. Ecology, 1971, 52: 912-915.
[47]	RUANE A C, ROSENZWEIG C. Agriculture & Food Systems to 2050: Climate Change Impacts on Agriculture [M]. Singapore: World Scientific Publishing, 2019: 161-184.
[48]	YAGI K. MINAMI K, OGAWA Y. Effects of water percolation on methane emission from paddy fields [J]. Res Rep Div Envrion Planning, 1990(6): 105-112.
[49]	YAGI K, MINAMI K, OGAWA Y. Effects of water percolation on methane emission from rice paddies: A lysimeter experiment [J]. Plant and Soil, 1998, 198(2): 193-200.
[50]	唐罗忠, 生原喜久雄, 户田浩人, 等. 湿地林土壤的Fe²⁺, Eh及pH值的变化 [J]. 生态学报, 2005, 25(1): 103-107.
[51]	侯会静, 杨士红, 徐俊增. 控制灌溉稻田CH₄排放的影响因子分析 [J]. 节水灌溉, 2016, 41(8): 70-75.
[52]	丁昌璞, 于天仁. 水稻土中氧化还原过程的研究: Ⅳ. 红壤性水稻土中铁锰的活动性 [J]. 土壤学报, 1958, 6(2): 99-107.
[53]	CASTRO M S, MELILLO J M, STEUDLER P A, et al. Soil moisture as a predictor of methane uptake by temperate forest soils [J]. Canadian Journal of Forest Research, 1994, 24(9): 1805-1810.
[54]	PALM C A, ALEGR J C, AREVALO L, et al. Nitrous oxide and methane fluxes in six different land use systems in the Peruvian Amazon [J]. Global Biogeochemical Cycles, 2002, 16(4): 21-22.
[55]	王连峰, 蔡祖聪. 水分和温度对旱地红壤硝化活力和反硝化活力的影响 [J]. 土壤, 2004, 36(5): 543-560.
[56]	谢勇, 荣湘民, 何欣, 等. 农田土壤N₂O排放的主要影响因素 [J]. 湖南农业科学, 2015(11): 92-97.
[57]	侯爱新, 王正平. 稻田CH₄和N₂O排放关系及其微生物学机理和一些影响因子 [J]. 应用生态学报, 1997, 8(3): 270-274.
[58]	熊莉, 徐振锋, 吴福忠, 等. 雪被斑块对川西亚高山冷杉林土壤氮转化酶活性的影响 [J]. 应用生态学报, 2014, 25(5): 1293-1299.
[59]	SCHAUFLER G, KITZLER B, SCHINDLBACHER A, et al. Greenhouse gas emissions from European soils under different land use: Effects of soil moisture and temperature [J]. European Journal of Soil Science, 2010, 61(5): 683-696.
[60]	李昌新, 黄山, 彭现宪, 等. 南方红壤稻田与旱地土壤有机碳及其组分的特征差异 [J]. 农业环境科学学报, 2009, 28(3): 606-611.
[61]	LIN S, JAVED L, HU G R, et al. Differences in nitrous oxide flfluxes from red soil under different land uses in mid-subtropical China [J]. Agriculture, Ecosystems and Environment, 2012, 146(1): 168-178.
[62]	BERGLUND Ö, BERGLUND K. Influence of water table level and soil properties on emissions of greenhouse gases from cultivated peat soil [J]. Soil Biology and Biochemistry, 2011, 43(5): 923-931.
[63]	林杉, 冯明磊, 阮雷雷, 等. 三峡库区不同土地利用方式下土壤氧化亚氮排放及其影响因素 [J]. 应用生态学报, 2008, 19(6): 1269-1276.
[64]	MOSIER A R, KROEZE C. Contribution of agroecosystems to the global atmospheric N₂O budget[C]// DESJARDINS R L, KENG J, HAUGEN K. Proceedings of international workshop on reducing N₂O emission from agroecosystems. Banff, Canada: Agriculture and Agri-Food Canada Research Branch & Alberta Agriculture, Food and Rural Development, Conservation and Development Branch, 1999: 3-15.