Wang Yueling, Wang Sicheng, Xu Hao, et al. Effects of Vegetation Restoration Methods on Soil Particle Size Characteristics in Loess Region of Southern Ningxia[J]. Bulletin of Soiland Water Conservation, 2021, 41(5): 83-91.
DOI:
Wang Yueling, Wang Sicheng, Xu Hao, et al. Effects of Vegetation Restoration Methods on Soil Particle Size Characteristics in Loess Region of Southern Ningxia[J]. Bulletin of Soiland Water Conservation, 2021, 41(5): 83-91. DOI: 10.13961/j.cnki.stbctb.2021.05.012.
Effects of Vegetation Restoration Methods on Soil Particle Size Characteristics in Loess Region of Southern Ningxia
[Objective] In order to provide a scientific basis for more effectively guiding the sustainable development of soil resources and ecological environmental protection in the loess region of Southern Ningxia Hui Autonomous Region
soil particle size characteristics under different vegetation recovery patterns were studied.[Methods] Field standardized soil samples (0-100 cm) were collected
and 216 samples from nine different vegetation restoration methods (Prunus armeniaca forest
Amygdalus davidiana forest
Hippophae rhamnoides forest
Caragana korshinskii forest
C. korshinskii×P. armeniaca forest
P. armeniaca×H. rhamnoides forest
dam land
alfalfa land
and abandoned land) were measured with a Mastersizer 3000 laser particle size analyzer. The average particle size (MZ)
standard deviation (δ)
skewness (SK)
and kurtosis (KG) were calculated by the Fokker and Ward formula.[Results] ① Under different vegetation recovery patterns
the main particle size components were silt (0.002~0.05 mm) and very fine sand (0.05~0.1 mm)
and the proportion of silt content in each particle size classification was the largest. The contents of clay
coarse sand
very coarse sand
and medium sand in different vegetation restoration methods tended to be stable
and changed little with increasing soil depth. The content of silt
very fine sand
and fine sand fluctuated greatly with increasing soil depth
and each layer showed different trends. ② The variation of the coefficient of variation of each particle size was basically the same under different vegetation restoration methods. The coefficient of variation of clay was the highest
followed by sand and silt. ③ The average soil particle size followed the order of P. armeniaca×C. korshinskii forest > H. rhamnoides forest > A. davidiana forest > C. korshinskii forest > P. armeniaca forest > alfalfa land > P. armeniaca×H. rhamnoides forest > abandoned land > dam land. The sorting ability of abandoned land
A. davidiana forest
and C. korshinskii forest was better than that of other sites
with H. rhamnoides forest being the worst.[Conclusion] Soil particle size distribution in different vegetation restoration methods was mainly affected by utilization mode
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Related Institution
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