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草业学报 ›› 2015, Vol. 24 ›› Issue (12): 1-9.DOI: 10.11686/cyxb2015019

• 研究论文 •    下一篇

东祁连山灌-草群落交错带土壤呼吸动态及影响因子分析

魏巍1,2,周娟娟1,2,曹文侠2,*,徐长林2   

  1. 1.西藏自治区农牧科学院草业科学研究所,西藏 拉萨 590000;
    2.甘肃农业大学草业学院,甘肃 兰州 730070
  • 收稿日期:2015-01-13 出版日期:2015-12-20 发布日期:2015-12-20
  • 通讯作者: caowx@gsau.edu.cn
  • 作者简介:魏巍(1986-),男,内蒙古乌兰察布人,助研。E-mail:weiweicc01@126.com
  • 基金资助:
    国家自然科学基金(31360569)和现代农业产业技术体系(CARS-35)资助

Soil respiration dynamics and impact factor analysis of a shrubland-grassland ecotone in the Eastern Qilian Mountains

WEI Wei1, 2, ZHOU Juan-Juan1, 2, CAO Wen-Xia2, *, XU Chang-Lin2   

  1. 1.Institute of Pratacultural Science, Tibet Academy of Agriculture and Animal Husbandry Science, Lhasa 590000, China;
    2.Grassland Science College of Gansu Agricultural University, Lanzhou 730070, China
  • Received:2015-01-13 Online:2015-12-20 Published:2015-12-20

摘要: 为探究高寒灌-草交错带土壤呼吸动态及影响因素,应用LI-8100A土壤呼吸自动测定系统,对东祁连山典型灌丛-草地交错带土壤呼吸动态及土壤因子进行测定,分析呼吸速率与土壤因子的相互关系。结果表明,整个交错带内土壤呼吸速率的均值介于2.3~7.2 μmol/(m2·s),各样地间土壤呼吸速率大小顺序为珠芽蓼草甸中心(S1)>草甸-金露梅灌丛交错区(MSC1)>金露梅灌丛中心(S2)>金露梅-杜鹃灌丛交错区(MSC2)>杜鹃灌丛中心(S3),S1和MSC1样地的土壤呼吸日变化呈单峰型,峰值出现在14:00,S2、MSC2、S3样地峰型不明显,且日变幅较小,仅为0.3~1.1 μmol/(m2·s);交错带内土壤物理性质和养分储量呈明显的垂直分异规律,土壤呼吸速率与土壤温度、全磷储量呈极显著的正相关(P<0.01),与土壤含水量极显著负相关(P<0.01),与0~20 cm土壤有机碳储量呈显著负相关(P<0.05);拟合分析显示,土壤温度、含水量和全磷储量是土壤呼吸速率的主要限制因子,土壤呼吸与土壤温度拟合系数最高,可解释土壤呼吸空间变异的79.9%。

Abstract: This research explored the factors influencing soil respiration dynamics of an alpine Shrubland-Grassland ecotone. The soil respiration dynamics were measured using a LI-8100A automated soil CO2 flux system, and relationship between soil respiration and soil factors was analysed for an eastern Qilian Mountain typical Shrubland-Grassland ecotone. The mean soil respiration rate was 2.3-7.2 μmol CO2/(m2·s). The rankings of soil respiration rate at different sampling points were: Polygonum viviparum meadow center (S1)>Polygonum viviparum meadow-Potentilla fruticosa shrub ecotone (MSC1)>Potentilla fruticosa shrub center (S2)>Potentilla fruticosa-Rhododendron shrub ecotone (MSC2)>Rhododendron shrub center (S3). The diurnal variation of soil respiration of S1 and MSC1 had a unimodal pattern, with the peak at 14:00. For S2, MSC2 and S3 respiration rates were only 0.3-1.1 μmol CO2/(m2·s) and the peak was not obvious. Soil physical properties showed a significant vertical gradation within ecotones. Soil respiration rate was significantly and positively correlated with soil temperature and total phosphorus (P<0.01), significantly negatively correlated with soil moisture (P<0.01), and significantly positively correlated with soil organic carbon in the 0-20 cm soil layer (P<0.05). Analysis of the relationship between soil respiration and soil temperature, soil moisture, total phosphorus, and organic carbon showed that soil temperature, soil moisture and total phosphorus were the main limiting factors for soil respiration rate. The highest fitted coefficient was soil temperature, which explained 79.9% of the spatial variability in soil respiration.