Journal of Jilin University(Earth Science Edition) ›› 2024, Vol. 54 ›› Issue (2): 604-618.doi: 10.13278/j.cnki.jjuese.20220145

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Distribution Characteristics and Influencing Factors of Aboveground Biomass in Typical Grassland Ecosystem in Xilin River Basin

Liu Tingxi1,2,Zhao Xinyu1,Duan Limin1,2,Wang Yixuan1,2,Li Mingyang1,Li Yuankang1

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  1. 1. College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018,China

    2. Inner Mongolia Water Resource Protection and Utilization Key Laboratory, Hohhot 010018,China

  • Online:2024-03-26 Published:2024-04-09
  • Supported by:
    Supported by the National Natural Science Foundation of China (51939006, 51909122, 52269005), the Science and Technology Project of Inner Mongolia (2021GG0071, 2021GG0072), the Construction Project of Water Resources Protection and Utilization Key Laboratory of Inner Mongolia (2020PT0001), the Project of Ministry of Education Innovative Research Team (IRT_17R60), the Project of Innovation Team in Priority Areas Accredited by the Ministry of Science and Technology (2015RA4013) and the Project of Science and Technology Leading Talent Team of Inner Mongolia Autonomous Region (2022LRC0007)

Abstract:

In order to systematically quantify the synergistic relationship between environmental factors and their regulation of spatial and temporal patterns of biomass, taking the Xilin River basin as the study area, this study measured the aboveground biomass (AGB), soil water content, soil density, organic carbon mass fraction, total nitrogen mass fraction, soil pH and other environmental factors of the typical grassland ecosystem from May to September 2020. The relationship between AGB and driving factors were analyzed by using the geographic detector method. The results show that: 1) Watershed-level AGB increases stably at the beginning stage of the growing season, displays the highest increase rate in July, and reaches the maximum on September 3rd. AGB in the upstream and downstream is 209.12 and 147.19 g/m2, respectively. AGB in the upstream of the watershed is significantly higher than that in the downstream (significance level p<0.05), and the overall spatial pattern of AGB shows a decreasing trend from the southeast to the northwest in the watershed. 2) During the entire vegetation growing season, meteorological factors (precipitation and air temperature) are key factors driving the changes in AGB, with an explanation rate of more than 60.0% in the regression model. At the end of the growing season, in addition to meteorological factors, soil pH also significantly influences the dynamics of AGB in time and space. 3) At each stage of the growing season, the interaction between environmental factors shows nonlinear enhancement and double-factor enhancement. At the beginning of the growing season, the interaction between precipitation and  dry density of soil shows the most influential. When soil water content reaches a relatively high level, the interaction of soil dry density with other environmental factors (precipitation, air temperature, pH) exerts a significant impact on the AGB in the peak and late stages of the growing season vegetation growth in the basin.

Key words: Xilin River basin, grassland, aboveground biomass, environmental factors, geographic detectors

CLC Number: 

  • P339
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[3] ZHANG Zuo-lun, ZENG Qing-dong, YE Jie, JIA Chang-shun, LI Wen-Tao. Location Forecasting of Buried Metal Ore-body in Grasslands Covered Area-A Case of Lead-Zinc Mineral Occurrence in Middle-Southern Segment of Daxing’anling Mountains [J]. J4, 2007, 37(1): 38-0040.
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