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青藏高原不同草地利用方式对土壤粒径分形特征的影响
引用本文:宛倩,王杰,王向涛,刘国彬,张超.青藏高原不同草地利用方式对土壤粒径分形特征的影响[J].生态学报,2022,42(5):1716-1726.
作者姓名:宛倩  王杰  王向涛  刘国彬  张超
作者单位:西北农林科技大学水土保持研究所, 杨凌 712100;西藏农牧学院动物科学学院, 林芝 860000;中国科学院水利部水土保持研究所, 杨凌 712100
基金项目:国家自然科学基金(41761008);中国科学院战略性先导专项(XDA20040200);陕西省基础研究计划项目(2019KJXX-081,2021JM-605);中央高校基本科研业务费专项(2452018336)
摘    要:研究青藏高原草地土壤粒径结构分形特征,为该地区土壤质量评价和生态恢复提供科学依据。以青藏高原4种高寒草地(放牧、围栏禁牧、围栏禁牧+补植、未干扰)为对象,采用分形理论,研究不同利用方式对高寒草地土壤颗粒组成及分形特征的影响,明确土壤粒径分形特征的影响因素。结果表明:与放牧和围栏禁牧+补植相比,围栏禁牧草地中黏粒和粉粒体积分数分别增加了60%—91.1%、43.5%—80.1%,禁牧能够促进土壤砂粒向黏粒和粉粒转变。不同草地利用方式对分形维数有显著影响,单重分形维数D值依次为放牧草地<围栏禁牧+补植草地<未干扰草地=围栏禁牧草地,多重分形维数,包括信息维数D1、信息维数/容量维数比值D1/D0和关联维数D2依次为放牧草地<围栏禁牧+补植草地<围栏禁牧草地<未干扰草地。单重分形维数D与土壤黏粒、粉粒呈极显著正相关(P<0.01);砂粒、黏粒、粉粒、有机碳和全氮是多重分形维数的限制因素。信息维数D1、信息维数/容量维数比值D1...

关 键 词:草地类型  土壤颗粒组成  单重分形  多重分形
收稿时间:2020/12/4 0:00:00
修稿时间:2021/9/6 0:00:00

Effects of different meadow use types on the fractal characteristics of soil particle in the Qinghai-Tibet Plateau
WAN Qian,WANG Jie,WANG Xiangtao,LIU Guobin,ZHANG Chao.Effects of different meadow use types on the fractal characteristics of soil particle in the Qinghai-Tibet Plateau[J].Acta Ecologica Sinica,2022,42(5):1716-1726.
Authors:WAN Qian  WANG Jie  WANG Xiangtao  LIU Guobin  ZHANG Chao
Institution:Institute of Soil and Water Conservation, Northwest A & F University, Yangling 712100, China;College of Animal Science, Tibet Agriculture and Animal Husbandry College, Linzhi 860000, China;Institute of Soil and Water Conservation, Chinese Academy of Science & Ministry of Water Resources, Yangling 712100, China
Abstract:This study investigated the effect of different meadow use on the fractal characteristics of soil particle to provide the scientific basis for soil quality evaluation and ecological restoration of alpine grassland in the Tibetan Plateau. The soil particle composition and fractal characteristics were examined by the fractal theory in four alpine meadows (grazed meadow, fenced meadow, fenced+reseeded meadow, and undisturbed meadow) in the Tibetan Plateau, and their driving forces were clarified. The results showed that the volume fraction of clay and silt particles in fenced grazing grassland increased by 60%-91.1% and 43.5%-80.1%, respectively, compared with those in grazed meadow and fenced+reseeded meadow; grazing prohibition promotes the transformation of soil sand to clay and silt. Changes in meadow use type had significant effects on the soil fractal dimension. Single fractal dimension (D-value) was in the order of grazed meadowD1), entropy dimension/capacity dimension (D1/D0) and correlation dimension (D2), were in the order of grazed meadow < fenced+reseeded meadow < fenced meadow < undisturbed meadow. D-value of the single fractal dimension was positively correlated with the contents of clay and silt (P<0.01); the contents of sand, clay, silt, organic carbon and total nitrogen are the dominant factors affecting the multifractal parameters. D1, D1/D0 and D2 were positively correlated with the contents of soil organic carbon, total nitrogen, total phosphorus and nitrate nitrogen. In conclusion, multifractal dimension parameters can be used as indicators to evaluate the characteristics of soil fertility, and grazing prohibition can improve the soil texture in Tibetan Plateau.
Keywords:meadow type  soil particle composition  single fractal  multifractal dimension
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