This study investigated the effect of the soil water holding capacity and permeability under different land use patterns in the Tianzhu alpine region of the Eastern Qilian Mountains,and four land use patterns were sel...This study investigated the effect of the soil water holding capacity and permeability under different land use patterns in the Tianzhu alpine region of the Eastern Qilian Mountains,and four land use patterns were selected,namely,natural grassland,rehabilitated land,oats land and perennial grassland. As time went by,different land use patterns imposed significant effects on the water holding capacity power and permeability. The soil bulk density was rehabilitated land(1. 104 g/cm3) > perennial grassland(1.061g/cm3) > oats land(1.011 g/cm3) > natural grassland(0. 781 g/cm3) ; the soil overall porosity was natural grassland(68.196%) > oats land(60.606%) > perennial grassland(58. 93%) > rehabilitated land(57. 5%) ; the natural grassland had the most water holding capacity power and soil steady infiltration rate(681. 966 t/hm 2 and 3. 02 mm/min) ,while the rehabilitated land had the least(575. 005 t/hm 2 and 1. 004 mm/min) . In terms of soil water-holding capacity and permeability,the natural grassland was the best out of these four use patterns while the rehabilitated land was the worst pattern. In other words,both oats land and perennial grassland had better water holding capacity power and permeability than the rehabilitated land.展开更多
In order to test whether the relationship between climate and the radial growth of trees is affected by altitude,altitude variability and time stability of climate-influenced radial growth of a dominant conifer,Chines...In order to test whether the relationship between climate and the radial growth of trees is affected by altitude,altitude variability and time stability of climate-influenced radial growth of a dominant conifer,Chinese pine(Pinus tabulaeformis),in the eastern Qilian Mountains were studied against the background of climate change using dendrochronology.Results show that 1)droughts at the end of the growing season of last year and during the early and middle growing season of the current year were the main limiting factors for the radial growth of Chinese pine at two altitude gradients;this was determined by analyzing the relationship between tree-ring width chronologies and climate factors.2)The sensitivity of the radial growth of trees to climate change gradually decreased and was affected more by drought stress at a lower altitude.3)An unstable divergence response was observed in the radial growth at the two altitudes,in response to controlling climatic factors;this observation was based on the moving correlation analysis of growth/climate relationships,and the aggravation of drought stress caused by increasing temperature was the main reason.4)The growth rate of Chinese pine at the two altitudes increased at first and then decreased,as measured by basal area increment(BAI)modeling.Future temperature rises may have significant effects on mountain forest ecosystems in arid and semi-arid regions.Effective management and protection measures should be taken,according to the response patterns of trees to climate change at different altitude gradients.展开更多
基金Supported by National Natural Science Fund Program (30960082)
文摘This study investigated the effect of the soil water holding capacity and permeability under different land use patterns in the Tianzhu alpine region of the Eastern Qilian Mountains,and four land use patterns were selected,namely,natural grassland,rehabilitated land,oats land and perennial grassland. As time went by,different land use patterns imposed significant effects on the water holding capacity power and permeability. The soil bulk density was rehabilitated land(1. 104 g/cm3) > perennial grassland(1.061g/cm3) > oats land(1.011 g/cm3) > natural grassland(0. 781 g/cm3) ; the soil overall porosity was natural grassland(68.196%) > oats land(60.606%) > perennial grassland(58. 93%) > rehabilitated land(57. 5%) ; the natural grassland had the most water holding capacity power and soil steady infiltration rate(681. 966 t/hm 2 and 3. 02 mm/min) ,while the rehabilitated land had the least(575. 005 t/hm 2 and 1. 004 mm/min) . In terms of soil water-holding capacity and permeability,the natural grassland was the best out of these four use patterns while the rehabilitated land was the worst pattern. In other words,both oats land and perennial grassland had better water holding capacity power and permeability than the rehabilitated land.
基金This research was supported by the National Natural Science Foundation of China(Grant No.41861006)Project/Supported by State Key Laboratory of Earth Surface Processes and Resource Ecology(Grant No.2020-KF04)the Research Ability Promotion Program for Young Teachers of Northwest Normal University(NWNU-LKQN2019-4).
文摘In order to test whether the relationship between climate and the radial growth of trees is affected by altitude,altitude variability and time stability of climate-influenced radial growth of a dominant conifer,Chinese pine(Pinus tabulaeformis),in the eastern Qilian Mountains were studied against the background of climate change using dendrochronology.Results show that 1)droughts at the end of the growing season of last year and during the early and middle growing season of the current year were the main limiting factors for the radial growth of Chinese pine at two altitude gradients;this was determined by analyzing the relationship between tree-ring width chronologies and climate factors.2)The sensitivity of the radial growth of trees to climate change gradually decreased and was affected more by drought stress at a lower altitude.3)An unstable divergence response was observed in the radial growth at the two altitudes,in response to controlling climatic factors;this observation was based on the moving correlation analysis of growth/climate relationships,and the aggravation of drought stress caused by increasing temperature was the main reason.4)The growth rate of Chinese pine at the two altitudes increased at first and then decreased,as measured by basal area increment(BAI)modeling.Future temperature rises may have significant effects on mountain forest ecosystems in arid and semi-arid regions.Effective management and protection measures should be taken,according to the response patterns of trees to climate change at different altitude gradients.
