中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Soil salinity distribution and its relationship with soil particle size in the lower reaches of Heihe River, Northwestern China

文献类型:期刊论文

作者Zhao, Yu1,2,3; Feng, Qi1; Yang, Huaide1,2
刊名ENVIRONMENTAL EARTH SCIENCES
出版日期2016-05-01
卷号75期号:9页码:18
ISSN号1866-6280
关键词Soil salinity Soil particle size distribution Fractal dimension Heihe River
DOI10.1007/s12665-016-5603-8
通讯作者Feng, Qi(qifeng@lzb.ac.cn)
英文摘要Recognition of the vertical and spatial distribution characteristics of soil salinity and its influencing factors have become a prerequisite for formulating strategies for the utilization and sustainable development of soil resources. The changes and characteristics of the particle size distribution (PSD) and its relationship with soil salinity were studied using the combined methods of laser diffraction analysis, the textural triangle and fractal analysis in the lower reaches of Heihe River, Northwestern China. The soil salinity showed clear surface accumulation characteristics. Soil salinity profiles in the area were classified into four types: Equably distribution profiles, bottom accumulation profiles, surface accumulation profiles, and oscillation profiles. In the study area, moderate salinized soil, heavy salinized soil and saline soil accounted for 5.71, 25.71, and 42.87 %, respectively. It was shown that soil salinization in the lower reaches of Heihe River is severe. Soil salinity and its spatial distribution is mainly controlled by SO42-, Cl-, Na+ + K+, Mg2+, and Ca2+. The soil texture of the topsoil can be classified as sand, sandy loam, silt loam, and silt. The silt and sand occupied the majority of the PDS at different soil depths. There was a decrease in soil salinity and soil particle size with increasing soil depth. The fractal dimension of PSD ranged from 2.503 to 2.555, the higher the sand content, the lower the fractal dimension. A considerable linear relationship also exists between the fractal dimension and the contents of soil clay, silt, sand and the soil salinity. Results show that the soil texture features dominated the soil salinity distribution.
收录类别SCI
WOS关键词SALT CONTENT ; GROUNDWATER ; SALINIZATION ; QUALITY ; DESERTIFICATION ; DIMENSIONS ; MOISTURE ; OASIS ; DELTA ; MODEL
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
语种英语
出版者SPRINGER
WOS记录号WOS:000376030100086
URI标识http://www.irgrid.ac.cn/handle/1471x/2557340
专题寒区旱区环境与工程研究所
通讯作者Feng, Qi
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Alashan Desert Ecohydrol Expt Res Stn, Lanzhou 730000, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Lanzhou Univ, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Zhao, Yu,Feng, Qi,Yang, Huaide. Soil salinity distribution and its relationship with soil particle size in the lower reaches of Heihe River, Northwestern China[J]. ENVIRONMENTAL EARTH SCIENCES,2016,75(9):18.
APA Zhao, Yu,Feng, Qi,&Yang, Huaide.(2016).Soil salinity distribution and its relationship with soil particle size in the lower reaches of Heihe River, Northwestern China.ENVIRONMENTAL EARTH SCIENCES,75(9),18.
MLA Zhao, Yu,et al."Soil salinity distribution and its relationship with soil particle size in the lower reaches of Heihe River, Northwestern China".ENVIRONMENTAL EARTH SCIENCES 75.9(2016):18.

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来源:寒区旱区环境与工程研究所

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