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西伯利亚桤木的入侵促进了北方泥炭地中溶解性有机碳的生物降解。

Alnus sibirica encroachment promotes dissolved organic carbon biodegradation in a boreal peatland.

机构信息

2011 Collaborative Innovation Center of Jiangxi Typical Trees Cultivation and Utilization, College of Forestry, Jiangxi Agricultural University, Nanchang 330045, China.

2011 Collaborative Innovation Center of Jiangxi Typical Trees Cultivation and Utilization, College of Forestry, Jiangxi Agricultural University, Nanchang 330045, China; Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.

出版信息

Sci Total Environ. 2019 Dec 10;695:133882. doi: 10.1016/j.scitotenv.2019.133882. Epub 2019 Aug 11.

Abstract

Symbiotic dinitrogen (N)-fixing trees have been expanding to boreal peatlands, yet its influence on dissolved organic carbon (DOC) biodegradation is unclear. Here, we measured DOC, ammonium‑nitrogen (NH-N), nitrate‑nitrogen (NO-N), dissolved inorganic nitrogen (DIN), and dissolved total nitrogen (DTN) concentrations, specific ultraviolet absorbance at 254 nm (SUVA), and humification index in the extracts obtained from peats in the 0-10 cm, 10-20 cm, and 20-40 cm depths in the open peatlands and Alnus sibirica islands in a boreal peatland, Northeast China. Afterwards, the peat extracts were used to assess the effect of N-fixing woody plant expansion on DOC biodegradation with a 42-day incubation experiment. The expansion of A. sibirica significantly increased NH-N, NO-N, DIN, and DTN concentrations, but did not produce a significant effect on SUVA and humification index in the extracts in each depth. Following A. sibirica expansion, DOC biodegradation was enhanced by 24.5%, 15.4%, and 38.3% at 0-10 cm, 10-20 cm, and 20-40 cm depths, respectively. Furthermore, DOC biodegradation was significantly and negatively correlated with DOC:DIN and DOC:DTN ratios, but exhibited no significant relationship with SUVA and humification index. This implied that improved N availability and associated shifts in C:N stoichiometry determined the increase in DOC biodegradation following A. sibirica expansion. Our findings suggest that N-fixing tree encroachment promotes microbial decomposition of DOC through improved N availability in boreal peatlands, which may cause organic C loss from soils in these C-enriched ecosystems.

摘要

共生固氮(N)树种不断向北方泥炭地扩展,但它对溶解有机碳(DOC)生物降解的影响尚不清楚。本研究中,我们测定了中国东北北方泥炭地开阔泥炭地和桤木岛(Alnus sibirica)0-10cm、10-20cm 和 20-40cm 土层中泥炭提取物的 DOC、铵态氮(NH-N)、硝态氮(NO-N)、溶解无机氮(DIN)和溶解总氮(DTN)浓度、254nm 处的特定紫外吸光度(SUVA)和腐殖化指数,随后使用这些泥炭提取物通过 42 天的培养实验来评估固氮木本植物扩展对 DOC 生物降解的影响。桤木的扩张显著增加了 NH-N、NO-N、DIN 和 DTN 浓度,但对各深度提取物的 SUVA 和腐殖化指数没有产生显著影响。桤木扩张后,0-10cm、10-20cm 和 20-40cm 土层的 DOC 生物降解分别增强了 24.5%、15.4%和 38.3%。此外,DOC 生物降解与 DOC:DIN 和 DOC:DTN 比值显著负相关,但与 SUVA 和腐殖化指数无显著关系。这表明,增加的 N 可用性和相关的 C:N 化学计量比的变化决定了桤木扩张后 DOC 生物降解的增加。我们的研究结果表明,固氮树种的入侵通过增加北方泥炭地的 N 可用性,促进了微生物对 DOC 的分解,这可能导致这些富含 C 的生态系统中土壤有机 C 的损失。

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