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Analysis of factors controlling sediment phosphorus flux potential of wetlands in Hulun Buir grassland by principal component and path analysis method

机译:用主成分和路径分析法分析呼伦贝尔草原湿地泥沙磷通量潜力的控制因素。

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摘要

Phosphorus (P) flux potential can predict the trend of phosphorus release from wetland sediments to water and provide scientific parameters for further monitoring and management for phosphorus flux from wetland sediments to overlying water. Many studies have focused on factors affecting sediment P flux potential in sediment-water interface, but rarely on the relationship among these factors. In the present study, experiment on sediment P flux potential in sediment-water interface was conducted in six wetlands in Hulun Buir grassland, China and the relationships among sediment P flux potential in sediment-water interface, sediment physical properties, and sediment chemical characteristics were examined. Principal component analysis and path analysis were used to discuss these data in correlation coefficient, direct, and indirect effects on sediment P flux potential in sediment-water interface. Results indicated that the major factors affecting sediment P flux potential in sediment-water interface were amount of organophosphate-degradation bacterium in sediment, Ca-P content, and total phosphorus concentrations. The factors of direct influence sediment P flux potential were sediment Ca-P content, Olsen-P content, SOC content, and sediment Al-P content. The indirect influence sediment P flux potential in sediment-water interface was sediment Olsen-P content, sediment SOC content, sediment Ca-P content, and sediment Al-P content. And the standard multiple regression describing the relationship between sediment P flux potential in sediment-water interface and its major effect factors was Y = 5.849 -1.025X(1) -1.995X(2) + 0.188X(3) - 0.282X(4) (r = 0.9298, p 0.01, n = 96), where Y is sediment P flux potential in sediment-water interface, X-1 is sediment Ca-P content, X-2 is sediment Olsen-P content, X-3 is sediment SOC content, and X-4 is sediment Al-P content. Therefore, future research will focus on these sediment properties to analyze the interrelation among sediment properties factors, main vegetable factors, and environment factors which influence the sediment P flux potential in sediment-water interface.
机译:磷通量潜力可以预测磷从湿地沉积物向水的释放趋势,并为进一步监测和管理从湿地沉积物到上覆水的磷通量提供科学参数。许多研究集中于影响沉积物-水界面中沉积物P通量潜力的因素,但很少涉及这些因素之间的关系。本研究在中国呼伦贝尔草原的六个湿地上进行了沉积物-水界面中的沉积物P通量电势实验,得出了沉积物-水界面中的沉积物P通量电势,沉积物物理性质和沉积物化学特征之间的关系。检查。使用主成分分析和路径分析来讨论这些数据,包括相关系数,对沉积物-水界面中的沉积物P通量势的直接和间接影响。结果表明,影响沉积物-水界面中沉积物P通量潜力的主要因素是沉积物中有机磷酸盐降解细菌的数量,Ca-P含量和总磷浓度。直接影响沉积物P通量势的因素是沉积物Ca-P含量,Olsen-P含量,SOC含量和Al-P含量。沉积物-水界面中间接影响沉积物P通量的潜力是沉积物Olsen-P含量,沉积物SOC含量,Ca-P含量和Al-P含量。描述沉积物-水界面中的沉积物P通量势与其主要影响因子之间关系的标准多元回归为Y = 5.849 -1.025X(1)-1.995X(2)+ 0.188X(3)-0.282X(4) )(r = 0.9298,p <0.01,n = 96),其中Y是沉积物-水界面中的沉积物P通量势,X-1是沉积物Ca-P含量,X-2是沉积物Olsen-P含量,X- 3为沉积物SOC含量,X-4为沉积物Al-P含量。因此,未来的研究将集中在这些沉积物特性上,以分析影响沉积物-水界面中沉积物P通量潜力的沉积物特性因子,主要蔬菜因子和环境因子之间的相互关系。

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2017年第12期|617.1-617.9|共9页
  • 作者单位

    Beijing Forestry Univ, Grassland Resources & Ecol Res Ctr, 35 Qinghua East Rd, Beijing 100083, Peoples R China;

    Beijing Forestry Univ, Grassland Resources & Ecol Res Ctr, 35 Qinghua East Rd, Beijing 100083, Peoples R China;

    Chinese Res Inst Environm Sci, State Environm Protect Key Lab Reg Ecoproc & Func, Beijing 100012, Peoples R China;

    Chinese Res Inst Environm Sci, State Environm Protect Key Lab Reg Ecoproc & Func, Beijing 100012, Peoples R China;

    Chinese Res Inst Environm Sci, State Environm Protect Key Lab Reg Ecoproc & Func, Beijing 100012, Peoples R China;

    Chinese Res Inst Environm Sci, State Environm Protect Key Lab Reg Ecoproc & Func, Beijing 100012, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sediment P flux potential; Sediment-water interface; Principal component analysis; Path analysis; Determination coefficient;

    机译:沉积物P通量势沉积物-水界面主成分分析路径分析测定系数;
  • 入库时间 2022-08-17 13:25:54

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