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秦岭不同海拔森林土壤-植物-凋落物化学计量特征对土壤氮组分的影响

马寰菲1,2,解梦怡1,2,胡汗1,2,郭垚鑫3,任成杰4,赵发珠1,2*   

  1. (1陕西省地表系统与环境承载力重点实验室, 西安 710127;2西北大学城市与环境学院, 西安 710127; 3西北大学生命科学学院, 西安710127;4西北农林科技大学农学院, 陕西杨凌 712100)
  • 出版日期:2020-03-10 发布日期:2020-03-10

Effects of stoichiometric characteristics of soil plantlitter on soil nitrogen components in different forests along an elevational gradient of Qinling Mountains.

MA Huan-fei1,2, XIE Meng-yi1,2, HU Han1,2, GUO Yao-xin3, REN Cheng-jie4, ZHAO Fa-zhu1,2*   

  1. (1Key Laboratory of Surface System and Environmental Carrying Capacity of Shaanxi Province, Xi’an 710127, China; 2College of Urban and Environmental Sciences, Northwest University, Xi’an 710127, China; 3College of Life Science, Northwest University, Xi’an 710127, China; 4College of Agronomy, Northwest A&F University, Yangling 712100, Shaanxi, China).
  • Online:2020-03-10 Published:2020-03-10

摘要: 为探究不同海拔森林土壤氮组分对土壤植物凋落物化学计量特征的响应规律,选取太白山1300~2600 m海拔范围内4种典型森林——锐齿栎林(Quercus alienavar. acuteserrata)、辽东栎林(Quercus liaotungensis)、红桦林(Betula albosinensis)、牛皮桦林(Betula albosinensisvar. septentrionalis)为研究对象,测定土壤、叶片、凋落物、根的碳(C)、氮(N)、磷(P)及土壤铵态氮、硝态氮、微生物生物量氮,分析不同森林土壤、植物、凋落物的化学计量比值的变化特征及其对氮组分的影响。结果表明:1)4种森林土壤C、N、P含量的变化范围分别为36.77~59.80、2.91~4.76、0.13~0.80 g·kg-1。C、N含量在不同森林间变化趋势基本一致,均表现为牛皮桦林>红桦林>辽东栎林>锐齿栎林;P含量的变化趋势表现为辽东栎林>牛皮桦林>红桦林>锐齿栎林;2)锐齿栎林叶片N∶P<14,表明锐齿栎林生长较大程度受N限制;辽东栎林、红桦林、牛皮桦林叶片N∶P>16,表明辽东栎林、红桦林、牛皮桦林生长较大程度受P限制;3)不同森林间微生物量氮差异显著(P<0.05),铵态氮含量无显著差异,硝态氮含量表现为锐齿栎林(0.33 mg·kg-1)>牛皮桦林(0.28 mg·kg-1)>辽东栎林(0.27 mg·kg-1)>红桦林(0.17 mg·kg-1);4)冗余分析结果表明,土壤-植物-凋落物N∶P值是影响土壤微生物量氮的重要因子,土壤C∶N是影响铵态氮、硝态氮含量的重要因子。本研究结果为太白山森林生态系统的保护和氮循环研究奠定基础。

关键词: 产量, 生理特性, 氮水平, 稗草, 水稻

Abstract: We examined the response of soil N components in forests along an elevational gradient to the stoichiometric characteristics of soilplantlitter with four typical forests Quercus aliena var. acuteserrata (QVA), Quercus liaotungensis (QW), Betula albo sinensis (BA), Betula albo sinensisvar.septentrionalis (BAV) in the range of 1300-2600 m elevation in Taibai Mountain. We measured the contents of organic C, total N, total P in soil, leaves, litter and roots, and soil ammonium N, nitrateN and microbial biomass N. We analyzed the stoichiometric characteristics of soil, plants, and litter in different forests and their effects on soil N components. The results showed that: (1) The variation ranges of soil C, N and P in the four forests were 36.77-59.80, 2.91-4.76 and 0.13-0.80 g·kg-1, respectively. The changes of soil C and N contents in different forests followed the same trend: BAV>BA>QW>QVA; the trend of change for soil P showed QW>BAV>BA>QVA. (2) The foliar N∶P ratio of QVA was lower than 14, indicating that plant growth in QVA was limited by N availability. Foliar N∶P ratio of QW, BA and BAV was above 16, indicating that plant growth in QW, BA and BAV were all limited by P. (3) Microbial biomass N varied significantly among different forests (P <0.05). There was no significant difference in ammoniumN content. The nitrateN content showed QVA (0.33 mg·kg-1)>BAV (0.28 mg·kg-1)>QW (0.27 mg·kg-1)>BA (0.17 mg·kg-1). (4) The results of redundancy analysis showed that the N∶P ratio of soilplantlitter was an important factor affecting microbial biomass N. Soil C∶N ratio was an important factor affecting ammonium N and nitrate N contents. Our results provide a basis for the rational management of major tree species and the study of nitrogen cycling in forest ecosystems of Taibai Mountain.

Key words: physiological characteristic., barnyardgrass, rice, nitrogen level, grain yield