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干旱区绿洲盐渍土粒径分布单重分形和多重分形特征
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  • 英文篇名:Fractal and Multifractal Analysis on Saline Soil Particle Size Distribution in Arid Oasis
  • 作者:张桉赫 ; 丁建丽 ; 王敬哲 ; 穆艾塔尔·赛地 ; 李艳菊
  • 英文作者:ZHANG An-he;DING Jian-li;WANG Jing-zhe;MUATTAR Saydi;LI Yan-ju;Key Laboratory of Smart City and Environment Modelling of Higher Education Institute,Xinjiang University;Collage of Resources and Environmental Sciences,Xinjiang University;Key Laboratory of Oasis Ecology under Ministry of Education,Xinjiang University;
  • 关键词:渭干河-库车河绿洲 ; 盐渍土 ; 土壤粒径 ; 单重分形 ; 多重分形 ; 干旱区
  • 英文关键词:Weigan-Kuqa River Oasis;;saline soil;;soil particle size;;fractal;;multifractal;;arid region
  • 中文刊名:GHQJ
  • 英文刊名:Arid Zone Research
  • 机构:新疆大学智慧城市与环境建模自治区普通高校重点实验室;新疆大学资源与环境科学学院;新疆大学绿洲生态教育部重点实验室;
  • 出版日期:2019-01-16 17:26
  • 出版单位:干旱区研究
  • 年:2019
  • 期:v.36
  • 基金:国家自然科学基金项目(41771470);; 新疆自治区重点实验室专项基金项目(2016D03001);; 自治区科技支疆项目(201591101);; 教育部促进与美大地区科研合作与高层次人才培养项目
  • 语种:中文;
  • 页:GHQJ201902006
  • 页数:9
  • CN:02
  • ISSN:65-1095/X
  • 分类号:49-57
摘要
为定量描述干旱区绿洲盐渍化土壤的粒径分布特征,对38个土壤样品的粒径分布与含盐量进行测定,并基于分形理论定量表征了研究区盐渍土和非盐渍土的土壤粒径分布特征。结果表明:粉粒的体积分数占主导地位,砂粒和黏粒次之;土壤含盐量与粉粒和黏粒体积分数呈正相关,而与黏粒呈负相关;单重分形维数D值介于1. 990~2. 349,且与土壤黏粒和粉粒含量成正比,相关系数分别为0. 81和0. 64(P <0. 01),与砂粒含量呈反比,相关系数为-0. 67(P <0. 01);土壤粒径分布具有多重分形特征,盐渍土(含盐量≥3 g·kg~(-1))的粒径分布较非盐渍土(<3 g·kg~(-1))更广,非均匀性更强;土壤含盐量与多重分形信息维D_1和D_1/D_0呈极显著负相关,相关系数分别为-0. 265(P <0. 01)和-0. 283(P <0. 01),与多重分形谱谱宽呈现极显著正相关,相关系数为0. 206(P <0. 01),而与D、容量维D_0和多重分形谱性状特性均没有显著相关性。
        In order to explore the relationship between salinization characters and soil particle size distribution( PSD) of soil in arid oasis,total 38 soil samples were collected from the Weigan-Kuqa River delta oasis in Xinjiang Uygur Autonomous Region in April 2016. And the characteristics of soil PSD of saline soil and non-saline soil in the study area were quantitatively based on the fractal theory. The results showed that the volumetric percentages of silt particles were dominated,followed by sand and clay particles. The volumetric percentages of silt and clay were positively correlated with soil salt content,while the volumetric percentage of sand was negatively correlated with soil salt content. The D value of the fractional dimension was ranged from 1. 990 to 2. 349,and the correlation coefficients between it and the volumetric percentages of clay and silt particles was 0. 81 and 0. 64,respectively,which passed the significance test at level of 0. 01. However,the correlation between D value and the volumetric percentage of sand particles was significantly negative with the correlation coefficient of-0. 67( P < 0. 01). The soil PSD had the multifractal characteristics,PSD range of the saline soil( salt content ≥3 g·kg~(-1)) was wider than that of the non-saline soil( salt content < 3 g·kg~(-1)),and which was more heterogeneous. Soil salt content was significantly negative correlation with the multifractal parameters D_1( the entropy dimension) and D_1/D_0 with the correlation coefficients of-0. 265( P < 0. 01) and-0. 283( P < 0. 01) respectively. The significantly positive correlation could be detected between soil salt content and Δa( the width of multifractal spectra) with a correlation coefficient of 0. 206( P < 0. 01). However,soil salt content had no significant correlation with D,D_0( capacity dimension) and Δf.
引文
[1]杨劲松.中国盐渍土研究的发展历程与展望[J].土壤学报,2008,45(5):837-845.[Yang Jingsong.Development and prospect of the research on salt-affected soils in China[J].Acta Pedologica Sinica,2008,45(5):837-845.]
    [2]Huang G,Zhang R.Evaluation of soil water retention curve with the pore-solid fractal model[J].Geoderma,2005,127(1):52-61.
    [3]王卫超,冯欢,王巍琦,等.开垦对盐渍化弃耕地土壤团聚体含量及稳定性的影响[J].土壤通报,2016,47(2):327-333.[Wang Weichao,Feng Huan,Wang Weiqi,et al.Change in content and characteristics of soil aggregates after reclamation of derelict salinized land[J].Chinese Journal of Soil Science,2016,47(2):327-333.]
    [4]Mandelbrot B B.The Fractal Geometry of Nature[M].New York:W.H.Freeman,1983.
    [5]Tyler S W,Wheatcraft S W.Fractal scaling of soil particle-size distributions:Analysis and limitations[J].Soil Science Society of A-merica Journal,1992,56(2):362-369.
    [6]杨培岭,罗远培.用粒径的重量分布表征的土壤分形特征[J].科学通报,1993,38(20):1 896-1 899.[Yang Peiling,Luo Yuanpei.Soil fractal characteristics characterized by weight distribution of particle size[J].Chinese Science Bulletin,1993,38(20):1 896-1 899.]
    [7]王敬哲,丁建丽,王飞,等.艾比湖湿地不同盐渍化土壤粒度组成及可蚀性研究[J].土壤,2018,50(3):589-605.[Wang Jingzhe,Ding Jianli,Wang Fei,et al.Particle size distribution(PSD)and erodibility of soils under different salinization degrees in Ebinur Lake Wetland[J].Soils,2018,50(3):589-605.]
    [8]Montero E.Rényi dimensions analysis of soil particle-size distributions[J].Ecological Modelling,2005,182(3-4):305-315.
    [9]Bittelli M,Campbell G S,Flury M.Characterization of particle-size distribution in soils with a fragmentation model[J].Soil Science Society of America Journal,1999,63(4):782-788.
    [10]代豫杰,郭建英,董智,等.不同沙生灌木下土壤颗粒及重金属空间分布特征[J].环境科学,2017(11):4 809-4 818.[Dai Yujie,Guo Jianying,Dong Zhi,et al.Soil particles and heavy metals spatial distribution under different psammophilic shrubs in Ulan Buh Desert[J].Environmental Science,2017(11):4 809-4 818.]
    [11]闵祥宇,李新举,李奇超.机械压实对复垦土壤粒径分布多重分形特征的影响[J].农业工程学报,2017,33(20):274-283.[Min Xiangyu,Li Xinju,Li Qichao.Influence of mechanical compaction on reclaimed soil particle size distribution multifractal characteristics[J].Transactions of the Chinese Society of Agricultural Engineering(Transactions of the CSAE),2017,33(20):274-283.]
    [12]王燕,斯庆毕力格,贾旭,等.基于多重分形的半干旱区弃耕农田土壤粒径分布特征[J].干旱区研究,2018,35(4):804-812.[Wang Yan,Siqingbilige,Jia Xu,et al.Soil particle size distribution characteristics of abandoned farmland based on multifractal in semiarid area[J].Arid Zone Research,2018,35(4):804-812.]
    [13]马成霞,丁建丽,杨爱霞,等.绿洲区域土壤盐渍化主要参数的空间异质性分析[J].干旱区资源与环境,2015,29(2):144-150.[Ma Chengxia,Ding Jianli,Yang Aixia,et al.Spatial variability of key parameters of soil salinization in oasis area[J].Journal of Arid Land Resources and Environment,2015,29(2):144-150.]
    [14]曹雷,丁建丽,玉米提·哈力克,等.基于国产高分一号卫星数据的区域土壤盐渍化信息提取与建模[J].土壤学报,2016,53(6):1 399-1 409.[Cao Lei,Ding Jianli,Umut Halik,et al.Extraction and modeling of regional soil salinization based on data from GF-1 satellite[J].Acta Pedologica Sinica,2016,53(6):1 399-1 409.]
    [15]乔木,周生斌,卢磊,等.新疆渭干河流域土壤盐渍化时空变化及成因分析[J].地理科学进展,2012,31(7):904-910.[Qiao Mu,Zhou Shengbin,Lu Lei,et al.Causes and spatial-temporal changes of soil salinization in Weigan River Basin,Xinjiang[J].Progress in Geography,2012,31(7):904-910.]
    [16]王家强,哈学萍.渭库绿洲土壤盐渍化遥感监测研究[J].农业系统科学与综合研究,2011,27(1):7-11.[Wang Jiaqiang,Ha Xueping.Remote sensing monitoring of soil salinization in the delta oasis of Weigan and Kuqa Rivers[J].System Sciences and Comprehensive Studies in Agriculture,2011,27(1):7-11.]
    [17]阿依图尔荪·哈力穆拉提.渭干河-库车河三角洲绿洲棉田表层土壤的理化特征研究[D].乌鲁木齐:新疆师范大学,2014.[Ayituersui Halimulati.The Research of the Topsoil Physical and Chemical Properties of Cotton Lands in Weigan and Kuqa Oasis[D].Urumqi:Xinjiang Normal University,2014.]
    [18]曹雷,丁建丽,于海洋.渭-库绿洲多尺度景观格局与盐度关系[J].农业工程学报,2016,32(3):101-110.[Cao Lei,Ding Jianli,Yu Haiyang.Relationship between multi-scale landscape pattern and salinity in Weigan and Kuqa rivers delta oasis[J].Transactions of the Chinese Society of Agricultural Engineering(Transactions of the CSAE),2016,32(3):101-110.]
    [19]新疆农业厅,新疆土壤普查办公室.新疆土壤[M].北京:科学出版社,1996:51-52.[Xinjiang Department of Agriculture,Office of Soil Survey of Xinjiang Uygur Autonomous Region.Xinjiang Soil[M].Beijing:Science Press,1996:51-52.]
    [20]白一茹,汪有科.黄土丘陵区土壤粒径分布单重分形和多重分形特征[J].农业机械学报,2012,43(5):43-48.[Bai Yiru,Wang Youke.Monofractal and multifractal analysis on soil particle distribution in Hilly and Gully areas of the Loess Plateau[J].Transactions of the Chinese Society for Agricultural Machinery,2012,43(5):43-48.]
    [21]管孝艳,杨培岭,吕烨.基于多重分形的土壤粒径分布与土壤物理特性关系[J].农业机械学报,2011,42(3):44-50.[Guan Xiaoyan,Yang Peiling,LüYe.Relationships between soil particle size distribution and soil physical properties based on multifractal[J].Transactions of the Chinese Society for Agricultural Machinery,2011,42(3):44-50.]
    [22]Paz Ferreiro J,Vidal Vázquez E.Multifractal analysis of Hg pore size distributions in soils with contrasting structural stability[J].Geoderma,2010,160(1):64-73.
    [23]胡宏昌,田富强,胡和平.新疆膜下滴灌土壤粒径分布及与水盐含量的关系[J].中国科学:技术科学,2011(8):13-20.[Hu Hongchang,Tian Fuqiang,Hu Heping.Soil particle size distribution and its relationship with soil water and salt under mulched drip irrigation in Xinjiang of China[J].Science China Technology Sciences,2011(8):13-20.]
    [24]王国梁,周生路,赵其国.土壤颗粒的体积分形维数及其在土地利用中的应用[J].土壤学报,2005,42(4):545-550.[Wang Guoliang,Zhou Shenglu,Zhao Qiguo.Volume fractal dimension of soil particles and its applications to land use[J].Acta Pedologica Sinica,2005,42(4):545-550.]
    [25]Evertsz C J G,Mandelbrot B B.Multifractal Measures,in Chaos and fractals[C]//Peitgen H O.New Frontiers of Science.New York:Springer Verlag,1992:921-953.
    [26]Grout H,Tarquis A M,Wiesner M R.Multifractal analysis of particle size distributions in Soil[J].Environmental Science&Technology,1998,32(32):1 176-1 182.
    [27]Pieri L,Bittelli M,Pisa P R.Laser diffraction,transmission electron microscopy and image analysis to evaluate a bimodal Gaussian model for particle size distribution in soils[J].Geoderma,2006,135(3):118-132.
    [28]方肖晨,王春红,张荣华,等.伏牛山区迎河小流域不同土地利用类型的土壤粒径分布特征[J].中国水土保持科学,2017,15(3):9-16.[Fang Xiaochen,Wang Chunhong,Zhang Ronghua,et al.Soil particle size distribution characteristics under different land use types in Yinghe Watershed of Funiu Mountain Area[J].Science of Soil and Water Conservation,2017,15(3):9-16.]
    [29]王德,傅伯杰,陈利顶,等.不同土地利用类型下土壤粒径分形分析---以黄土丘陵沟壑区为例[J].生态学报,2007,27(7):3 081-3 089.[Wang De,Fu Bojie,Chen Liding,et al.Fractal analysis on soil particle size distributions under different land-use type:A case study in the loess hilly areas of the Loess Plateau,China[J].Acta Ecologica Sinica,2007,27(7):3 081-3 089.]
    [30]张彩红,茹豪,武秀娟,等.庞泉沟流域土壤粒径分形维数特征[J].东北林业大学学报,2017(11):83-88.[Zhang Caihong,Ru Hao,Wu Xiujuan,et al.Fractal dimension characteristics of soil particle size in Pangquangou Watershed[J].Journal of Northeast Forestry University,2017(11):83-88.]
    [31]吴承祯,洪伟.不同经营模式土壤团粒结构的分形特征研究[J].土壤学报,1999,36(2):162-167.[Wu Chengzhen,Hong Wei.Study on fractal features of soil aggregate structure under different management patterns[J].Acta Pedologica Sinica,1999,36(2):162-167.]
    [32]黄冠华,詹卫华.土壤颗粒的分形特征及其应用[J].土壤学报,2002,39(4):490-497.[Huang Guanhua,Zhan Weihua.Fractal property of soil particle size distribution and its application[J].Acta Pedologica Sinica,2002,39(4):490-497.]
    [33]许婷婷,董智,李红丽,等.不同设障年限沙丘土壤粒径和有机碳分布特征[J].环境科学研究,2014,27(6):628-634.[Xu Tingting,Dong Zhi,Li Hongli,et al.Distributions of soil particle size and soil organic carbon in dunes of checkerboard barriers with different setting years[J].Research of Environmental Sciences,2014,27(6):628-634.]
    [34]杜金龙,靳孟贵,欧阳正平,等.焉耆盆地土壤盐分剖面特征及其与土壤颗粒组成的关系[J].地球科学:中国地质大学学报,2008,33(1):131-136.[Du Jinlong,Jin Menggui,Ouyang Zhengping,et al.Characteristics of soil salinity profiles and relationship between salinity and soil particle composition in Yanqi Basin of Xinjiang,China[J].Earth Science:Journal of China University of Geosciences,2008,33(1):131-136.]
    [35]孙梅,孙楠,黄运湘,等.长期不同施肥红壤粒径分布的多重分形特征[J].中国农业科学,2014,47(11):2 173-2 181.[Sun Mei,Sun Nan,Huang Yunxiang,et al.Multifractal characterization of soil particle size distribution under long-term different fertilizations in upland red soil[J].Scientia Agricultura Sinica,2014,47(11):2 173-2 181.]
    [36]李二焕,胡海波,鲁小珍,等.苏北滨海盐土区土壤盐分剖面特征及其理化特性[J].水土保持研究,2016,23(4):116-119.[Li Erhuan,Hu Haibo,Lu Xiaozhen,et al.Characteristics of soil salinity profiles and physical and chemical properties of coastal saline soil in the estuary of north Jiangsu[J].Research of Soil and Water Conservation,2016,23(4):116-119.]

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