Welcome to Acta Prataculturae Sinica ! Today is Share:

Acta Prataculturae Sinica ›› 2015, Vol. 24 ›› Issue (12): 1-9.DOI: 10.11686/cyxb2015019

• Orignal Article •     Next Articles

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

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.