CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, China; School of Chemistry, Biology and Environment, Yuxi Normal University, Yuxi, China; Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Xishuangbanna, China; Xishuangbanna Station for Tropical Rain Forest Ecosystem Studies, Chinese Ecosystem Research Net, Mengla, China; University of Chinese Academy of Sciences, Beijing 100039, China.
CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, China; Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Xishuangbanna, China; Xishuangbanna Station for Tropical Rain Forest Ecosystem Studies, Chinese Ecosystem Research Net, Mengla, China; University of Chinese Academy of Sciences, Beijing 100039, China.
Sci Total Environ. 2022 Nov 25;849:157891. doi: 10.1016/j.scitotenv.2022.157891. Epub 2022 Aug 8.
Litter comprises a major nutrient source when decomposed via soil microbes and functions as subtract that limits gas exchange between soil and atmosphere, thereby restricting methane (CH4) uptake in soils. However, the impact and inherent mechanism of litter and its decomposition on CH4 uptake in soils remains unknown in forest. Therefore, to declare the mechanisms of litter input and decomposition effect on the soil CH4 flux in forest, this study performed a litter-removal experiment in a tropical rainforest, and investigated the effects of litter input and decomposition on the CH4 flux among forest ecosystems through a literature review. Cumulative annual CH4 flux was -3.30 kg CH4-C ha y. The litter layer decreased annual accumulated CH4 uptake by 8% which greater in the rainy season than the dry season in the tropical rainforest. Litter decomposition and the input of carbon and nitrogen in litter biomass reduced CH4 uptake significantly and the difference in CH4 flux between treatment with litter and without litter was negatively associated with N derived from litter input. Based on the literature review about litter effect on soil CH4 around world forests, the effect of litter dynamics on CH4 uptake was regulated by litter-derived nitrogen input and the amount soil inorganic nitrogen content. Our results suggest that nitrogen input via litter decomposition, which increased with temperature, caused a decline in CH4 uptake by forest soils, which could weaken the contribution of the forest in mitigating global warming.
当通过土壤微生物分解时,凋落物构成了主要的养分来源,并起到了抑制土壤与大气之间气体交换的作用,从而限制了土壤对甲烷(CH4)的吸收。然而,凋落物及其分解对森林土壤 CH4 吸收的影响和内在机制尚不清楚。因此,为了阐明凋落物输入和分解对森林土壤 CH4 通量的机制,本研究在热带雨林中进行了凋落物去除实验,并通过文献综述研究了凋落物输入和分解对森林生态系统 CH4 通量的影响。累积年 CH4 通量为-3.30 kg CH4-C ha y。凋落物层使年累积 CH4 吸收量减少了 8%,在热带雨林中雨季比旱季更为明显。凋落物分解和凋落物生物质中碳和氮的输入显著减少了 CH4 的吸收,有凋落物和无凋落物处理之间的 CH4 通量差异与来自凋落物输入的氮呈负相关。基于对世界各地森林凋落物对土壤 CH4 影响的文献综述,凋落物动态对 CH4 吸收的影响受凋落物衍生氮输入和土壤无机氮含量的调节。我们的研究结果表明,随着温度升高,通过凋落物分解增加的氮输入导致森林土壤 CH4 吸收减少,这可能削弱了森林在缓解全球变暖方面的贡献。