School of Geographical Science, Fujian Normal University, Fuzhou 350007, China.
Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China.
Ying Yong Sheng Tai Xue Bao. 2021 Feb;32(2):521-528. doi: 10.13287/j.1001-9332.202102.038.
The activity and stoichiometry of soil extracellular enzyme can provide a good indication for changes in soil nutrient availability and microbial demands for nutrients. However, it remains unclear how would nitrogen (N) deposition affect nutrient limitation of microbes in subtropical forest soils. We conducted a 5 years N addition experiment in a subtropical forest. The soil nutrients and enzyme activities associated with carbon (C), N, and phosphorus (P) cycles were measured. We also examined the nutrient distribution of microorganisms using enzyme stoichiometry and vector analysis. The results showed that N addition significantly decreased the contents of soil soluble organic C and available P and increased that of available N. Furthermore, N addition significantly decreased β-N-acetyl-glucosaminidase (NAG) activity and NAG/ microbial biomass carbon (MBC), and increased acid phosphatase (ACP) and ACP/MBC. The low and moderate N addition levels significantly increased enzyme C/P, vector length, and vector angle, but significantly decreased enzyme N/P. Results of redundancy analysis showed that the change in soil enzyme activity and enzymatic stoichiometry were mainly driven by soil available P content under N addition. In summary, N addition altered the microbial nutrient acquisition strategy, which increased nutrient allocation to P-acquiring enzyme production but reduced that to N-acquiring enzyme production. Moreover, N addition exacerbated the C and P limitation of soil microorganisms. Appropriate amount of P fertilizer could be applied to improve soil fertility of subtropical forest in the future.
土壤胞外酶的活性和化学计量可以很好地反映土壤养分供应的变化和微生物对养分的需求。然而,目前尚不清楚氮(N)沉降如何影响亚热带森林土壤中微生物的养分限制。我们在亚热带森林中进行了为期 5 年的 N 添加实验。测量了与碳(C)、N 和磷(P)循环相关的土壤养分和酶活性。我们还使用酶化学计量和向量分析检查了微生物的养分分布。结果表明,N 添加显著降低了土壤可溶性有机 C 和有效 P 的含量,增加了有效 N 的含量。此外,N 添加显著降低了β-N-乙酰-氨基葡萄糖苷酶(NAG)活性和 NAG/微生物生物量碳(MBC),并增加了酸性磷酸酶(ACP)和 ACP/MBC。低和中 N 添加水平显著增加了酶 C/P、向量长度和向量角度,但显著降低了酶 N/P。冗余分析的结果表明,在 N 添加下,土壤酶活性和酶化学计量的变化主要受土壤有效 P 含量的驱动。总之,N 添加改变了微生物的养分获取策略,增加了对 P 获取酶产生的养分分配,减少了对 N 获取酶产生的养分分配。此外,N 添加加剧了土壤微生物的 C 和 P 限制。未来可以施加适量的磷肥来提高亚热带森林的土壤肥力。