Arid
DOI10.1016/j.catena.2021.105373
Fractal and multifractal analysis of soil particle-size distribution and correlation with soil hydrological properties in active layer of Qinghai-Tibet Plateau, China
Gao, Zeyong; Niu, Fujun; Lin, Zhanju; Luo, Jing
通讯作者Niu, FJ (corresponding author), Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, 320 Donggang West Rd, Lanzhou 730000, Gansu, Peoples R China.
来源期刊CATENA
ISSN0341-8162
EISSN1872-6887
出版年2021
卷号203
英文摘要The soil hydrological properties (HPs) in active layers regulate soil water migration and affect the evolution of permafrost and biogeochemical cycles. There is relatively little understanding of the changes in soil HPs as a result of soil particle-size distribution (PSD) in the permafrost regions of the Qinghai-Tibet Plateau. In this study, different land-cover types, namely alpine wet meadow (AWM), extremely degraded wet meadow (EDWM), alpine meadow (AM), degraded alpine meadow (DAM), alpine steppe (AS), and alpine desert (AD), were used to determine the relationships between soil PSD and HPs. Soil HPs were determined using borehole nuclear magnetic resonance, and soil PSD (0-2 mm) was analyzed using fractal and multifractal theory. The results showed that vegetation degradation caused coarse soil particle accumulation in the root zone, reflected by the soil single-fractal dimension (D-v: 2.12-2.50). The D-v, values showed significant positive correlations with soil clay and silt content as well as a negative correlation with sand content. Results from the generalized fractal and singularity spectra suggested an even distribution of soil particles in the root zone of the AWM, AM, and AD sites. Vegetation degradation increased the soil PSD capacity dimension (D-0), information dimension (D-1), correlation dimension, D-1/D-0 ratio, and Holder exponent of order zero. This was indicative of a narrow soil PSD range and non-uniform soil texture in the root zone. Although capillary water dominated the total soil water content in the alpine soils, soil water composition was also dependent on the vegetation type and soil stratigraphic distribution. Soil particle composition and multifractal dimensions were found to be effective parameters for forecasting soil HPs in the non-mot zone of alpine soils. However, the presence of vegetation weakens the relationship between soil PSD and HPs. This study contributes to the accurate evaluation of hydrological and biogeochemical cycles in permafrost regions.
英文关键词Soil particle-size distribution Multifractal analysis Soil hydrological properties Alpine grasslands Qinghai-Tibet Plateau
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000654354000065
WOS关键词YELLOW-RIVER DELTA ; LAND-USE TYPES ; HYDRAULIC CONDUCTIVITY ; ORGANIC-MATTER ; WATER-RETENTION ; PERMAFROST REGIONS ; ALPINE GRASSLAND ; LOESS PLATEAU ; VEGETATION ; PATTERNS
WOS类目Geosciences, Multidisciplinary ; Soil Science ; Water Resources
WOS研究方向Geology ; Agriculture ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/349812
作者单位[Gao, Zeyong; Niu, Fujun; Lin, Zhanju; Luo, Jing] Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, 320 Donggang West Rd, Lanzhou 730000, Gansu, Peoples R China
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GB/T 7714
Gao, Zeyong,Niu, Fujun,Lin, Zhanju,et al. Fractal and multifractal analysis of soil particle-size distribution and correlation with soil hydrological properties in active layer of Qinghai-Tibet Plateau, China[J],2021,203.
APA Gao, Zeyong,Niu, Fujun,Lin, Zhanju,&Luo, Jing.(2021).Fractal and multifractal analysis of soil particle-size distribution and correlation with soil hydrological properties in active layer of Qinghai-Tibet Plateau, China.CATENA,203.
MLA Gao, Zeyong,et al."Fractal and multifractal analysis of soil particle-size distribution and correlation with soil hydrological properties in active layer of Qinghai-Tibet Plateau, China".CATENA 203(2021).
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