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中国西南云南省中部森林土壤-微生物-胞外酶化学计量特征对氮沉降的响应。

Response of soil-microbe-extracellular enzyme stoichiometric characteristics to nitrogen deposition in a forest in central Yunnan Province, Southwest China.

机构信息

College of Ecology and Environment, Southwest Forestry University, Kunming 650224, China.

Yunnan Yuxi Forest Ecosystem National Station, National Forestry and Grassland Administration, Yuxi 653100, Yunnan, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2024 Jul 18;35(7):1789-1798. doi: 10.13287/j.1001-9332.202407.010.

Abstract

To understand the effects of nitrogen deposition on element cycling and nutrient limitation status in forest ecosystems, we examined the effects of nitrogen deposition on the stoichiometric characteristics of forest soil-microbial-extracellular enzymes in forest. We conducted a field experiment with control (CK, 0 g N·m·a), low nitrogen (LN, 10 g N·m·a), medium nitrogen (MN, 20 g N·m·a) and high nitrogen (HN, 25 g N·m·a) since 2019. We collected soil samples (0-5 cm, 5-10 cm and 10-20 cm) at September 2022, and measured the contents of soil organic, total nitrogen, total phosphorus, microbial biomass carbon, nitrogen and phosphorus (MBC, MBN, MBP) and the activities of C, N, and P acquisition enzymes. The results showed that nitrogen deposition significantly reduced soil organic content, C:N and C:P by 6.9%-29.8%, 7.6%-45.2% and 6.5%-28.6%, and increased soil total N content and N:P by 10.0%-45.0% and 19.0%-46.0%, respectively. Nitrogen addition did not affect soil total P content. Except for soil C:N and C:P, soil nutrient content and stoichiometric ratio were highest in 0-5 cm soil layer. MN and HN treatments significantly decreased MBN by 11.0%-12.7%. MBC, MBP, and their stoichiometry did not change significantly under nitrogen deposition. Soil microbial nutrient content in 0-5 cm soil layer was significantly higher than that in other soil layers. Nitrogen deposition significantly decreased the activities of cellobiose hydrolase and leucine aminopeptidase (decreased by 14.5%-16.2% and 48.7%-66.3%). HN treatment promoted β-1,4-glucosidase activity (increased by 68.0%), but inhibited soil enzyme stoichiometric carbon to nitrogen ratio and nitrogen to phosphorus ratio (decreased by 95.4% and 88.4%). LN and MN treatment promoted β-1,4-N-acetylglucosaminidase activity (increased by 68.3%-116.6%), but inhibited enzyme stoichiometric carbon to phosphorus ratio (decreased by 14.9%-29.4%). Alkaline phosphatase activity had no significant change. Soil enzyme activities were significantly decreased with increasing soil depth. Soil total N and total P and microbial nutrients were negatively correlated with vector angle (representing microbial nitrogen or phosphorus limitation), while vector length (representing microbial carbon limitation) was consistently significantly positively correlated with vector angle, suggesting the synergistic promotion between microbial carbon limitation and phosphorus limitation. Nitrogen deposition gradually shifted to phosphorus limitation while alleviating microbial nitrogen limitation in forest. In addition, microbial activities in this region was limited by C availability, and the relationship between microbial C and P limitation was proportional.

摘要

为了了解氮沉降对森林生态系统元素循环和养分限制状态的影响,我们研究了氮沉降对森林土壤-微生物-胞外酶化学计量特征的影响。我们自 2019 年以来进行了对照(CK,0 g N·m·a)、低氮(LN,10 g N·m·a)、中氮(MN,20 g N·m·a)和高氮(HN,25 g N·m·a)的田间试验。我们于 2022 年 9 月采集了土壤样品(0-5 cm、5-10 cm 和 10-20 cm),并测量了土壤有机碳、总氮、总磷、微生物生物量碳、氮和磷(MBC、MBN、MBP)以及 C、N 和 P 获取酶的活性。结果表明,氮沉降显著降低了土壤有机碳含量、C:N 和 C:P,分别降低了 6.9%-29.8%、7.6%-45.2%和 6.5%-28.6%,同时增加了土壤总氮含量和 N:P,分别增加了 10.0%-45.0%和 19.0%-46.0%。氮添加对土壤总磷含量没有影响。除了土壤 C:N 和 C:P 外,0-5 cm 土层的土壤养分含量和化学计量比最高。MN 和 HN 处理显著降低了 11.0%-12.7%的 MBN。氮沉降对 MBC、MBP 及其化学计量比没有显著影响。0-5 cm 土层土壤微生物养分含量明显高于其他土层。氮沉降显著降低了纤维二糖水解酶和亮氨酸氨肽酶的活性(降低了 14.5%-16.2%和 48.7%-66.3%)。HN 处理促进了β-1,4-葡萄糖苷酶的活性(增加了 68.0%),但抑制了土壤酶化学计量碳对氮比和碳对磷比(降低了 95.4%和 88.4%)。LN 和 MN 处理促进了β-1,4-N-乙酰氨基葡萄糖苷酶的活性(增加了 68.3%-116.6%),但抑制了酶化学计量碳对磷比(降低了 14.9%-29.4%)。碱性磷酸酶活性没有明显变化。土壤酶活性随土壤深度的增加而显著降低。土壤总氮和总磷以及微生物养分与向量角(代表微生物氮或磷限制)呈负相关,而向量长度(代表微生物碳限制)与向量角呈一致的显著正相关,表明微生物碳限制和磷限制之间存在协同促进作用。氮沉降在缓解森林微生物氮限制的同时,逐渐向磷限制转变。此外,该地区的微生物活性受到碳可用性的限制,微生物 C 和 P 限制之间的关系是成比例的。

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