鲁绍伟, 刘逸菲, 郑家银, 等. 北京松山国家森林公园4种林分类型降水水质变化特征[J]. 西南林业大学学报(自然科学), 2022, 43(0): 1–10 . DOI: 10.11929/j.swfu.202107045
引用本文: 鲁绍伟, 刘逸菲, 郑家银, 等. 北京松山国家森林公园4种林分类型降水水质变化特征[J]. 西南林业大学学报(自然科学), 2022, 43(0): 1–10 . DOI: 10.11929/j.swfu.202107045
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

本文排版定稿已在中国知网网络首发,如需阅读全文请打开知网首页,并搜索该论文题目即可查看。

北京松山国家森林公园4种林分类型降水水质变化特征

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

  • 摘要: 以北京松山国家森林公园4种典型林分类型为研究对象,按照大气降雨经过森林生态系统的空间顺序(林冠层、枯落物层和土壤层),分析不同林分类型下不同空间层次水质效应,探究大气降雨水质特征及变化规律。结果表明:林冠层对K+、Mg2+、NH4+和Cl离子起到淋溶作用,林分穿透雨较大气降雨各离子浓度增加了0.01~2.88倍,对Ca2+、NO3、NO2、SO42−和F主要起到吸附截留作用,浓度下降4.21%~60.08%。枯落物层对K+、Mg2+、Ca2+、NO3、F和Cl离子主要起到淋溶作用,枯透水较穿透雨各离子浓度增加了0.27%~58.81%,对Na+、NH4+、NO2和SO42−离子主要表现为吸附截留,离子浓度降低1.21%~49.76%。4种林分壤中流离子浓度变化趋势,Na+、Mg2+和Ca2+浓度呈现出随着土壤深度增加,离子浓度逐渐升高的趋势,NH4+和Cl浓度表现为随着土壤深度增加而逐渐下降的趋势;K+、NO3、NO2、SO42−和F浓度表现为0~20 cm土壤层先上升后降低的趋势,其后随土壤深度增加而降低。0~20 cm土壤层对大部分离子淋溶效果较强,该层溶液中Na+、K+、Mg2+、Ca2+、NO3、NO2、SO42−和F离子浓度较枯透水增加最高达10.14倍;20~60 cm的深层土壤对大部分离子起到吸附截留之作用,该层溶液中K+、NH4+、NO3、NO2、SO42−、F和Cl离子浓度逐渐下降,降幅为16.64%~80.92%。

     

    Abstract: 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.

     

/

返回文章
返回