JIANG Kun, QIN Hailong, LU Ying, et al. Fractal Dimension of Particle-Size Distribution for Soils Derived from Different Parent Materials in Guangdong Province[J]. 2016, 30(6): 319-324.
DOI:
JIANG Kun, QIN Hailong, LU Ying, et al. Fractal Dimension of Particle-Size Distribution for Soils Derived from Different Parent Materials in Guangdong Province[J]. 2016, 30(6): 319-324. DOI: 10.13870/j.cnki.stbcxb.2016.06.053.
Fractal Dimension of Particle-Size Distribution for Soils Derived from Different Parent Materials in Guangdong Province
were collected from profile horizons which derived from main parent materials (including basalt
sand-shale
Quaternary red soil and granite) in Guangdong Province
soil physico-chemical properties such as soil particle-size composition
organic matter
CEC
etc. were determined. The fractal dimension of particle-size distribution (PSD) for soils derived from different parent materials and its relationship with soil properties were studied. The results indicated that
the range of fractal dimension of PSD for soils derived from basalt
Quaternary red soil
granite and sand-shale were 2.923 9 to 2.981 2
2.858 8 to 2.937 7
2.769 3 to 2.923 1
and 2.544 6 to 2.885 6
respectively. The fractal dimension of PSD for soils derived from basalt
Quaternary red soil and sand-shale were significantly different. The fractal dimension of soil PSD showed an increasing trend with increasing soil depth
and the fractal dimension of soil PSD was almost the same in deep horizons of soils derived from the same parent material. The fractal dimension of soil PSD had smaller variation between soil at different depth in soil profiles derived from basalt and Quaternary red soil
however
the variation was larger for soils derived from sand-shale and granite. The fractal dimension of soil PSD was significantly negatively correlated with sand content
but was significantly positively correlated with clay content
soil total P
available K
total Fe
CEC
soil organic matter
total N
available N. The fractal dimension of soil PSD could be applied as a quantitative index reflecting soil fertility.