LI Shaoning, LIU Yifei, ZHENG Jiayin, ZHAO Na, XU Xiaotian, LU Shaowei. Characteristics of precipitation water quality changes of four forest types in Songshan National Forest Park, Beijing[J]. Journal of Southwest Forestry University. DOI: 10.11929/j.swfu.202107045
Citation: LI Shaoning, LIU Yifei, ZHENG Jiayin, ZHAO Na, XU Xiaotian, LU Shaowei. Characteristics of precipitation water quality changes of four forest types in Songshan National Forest Park, Beijing[J]. Journal of Southwest Forestry University. DOI: 10.11929/j.swfu.202107045

Characteristics of precipitation water quality changes of four forest types in Songshan National Forest Park, Beijing

  • This study included four typical forest types in Beijing Songshan National Forest Park were selected as the research objects. According to the spatial order of atmospheric rainfall passing through forest ecosystem (forest canopy, litter layer and soil layer), the water quality effects of different forest types and different spatial levels were analyzed. The water quality characteristics and change mechanism were revealed. The results showed that: (1)The forest canopy exerted lympholysis on K+, Mg2+, NH4+ and Cl ions, and the forest penetration rain of each ion concentration increased by 0.01 to 2.88 times , and Ca2+, NO3, NO2, SO42− and F were mainly retained by adsorption, with a concentration decrease of 4.21% to 60.08%, compared with the large gas rainfall. (2)The litter layer mainly leached K+、Mg2+, Ca2+, NO3, F and Cl ions, increased the ion concentration by 0.27% - 58.81%, and adsorbed Na+, NH4+, NO2 and SO42− ions, decreased the ion concentration by 1.21% - 49.76%. (3)The four kinds of forest traveling ion concentration change trend of soil as follows. Na+, Mg2+ and Ca2+ concentrations increased gradually with the increase of soil depth. K + , NO3-, NO2-, SO42-, and F-concentrations showed a trend of rising first after decreasing from 0 c m~20 cm soil layers, and subsequently decreasing with soil depth. (4)The most of ions is strong dissolve in 0 c m~20 cm soil layer. The concentration of Na+, K+, Mg2+, Ca2+, NO3, NO2, SO42− and F ions in 0 cm - 20 cm soil layer increased by 10.14 times compared with that in dry water layer; The concentration of K+, NH4+, NO3, NO2, SO42−, F and Cl in the solution of 20 cm - 60 cm deep soil layer decreased gradually, ranging from 16.64% to 80.92%. The results of this study provide an important reference for improving the ecological environment in Beijing, and provide theoretical basis and data support for the environmental governance around the Winter Olympic Games.
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