[1]XI Xiaokang,ZHU Zhongyuan,HAO Xiangyun.Spatial Variability of Soil Organic Carbon in Xilin River Basin[J].Research of Soil and Water Conservation,2017,24(06):97-104.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
24
Number of periods:
2017 06
Page number:
97-104
Column:
Public date:
2017-11-24
- Title:
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Spatial Variability of Soil Organic Carbon in Xilin River Basin
- Author(s):
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XI Xiaokang, ZHU Zhongyuan, HAO Xiangyun
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College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China
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- Keywords:
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soil organic carbon; spatial variability; geostatistics; anisotropy
- CLC:
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S153.6+21
- DOI:
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- Abstract:
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In order to explore the spatial variability of soil organic carbon in the Xilin River Basin, the variation characteristics and distribution pattern of 0-10 cm, 20-30 cm, 40-50 cm soil organic carbon were studied based on semivariance function theory and ordinary Kriging interpolation. The results showed that:(1) the best fitting models of soil organic carbon in 0-10 cm, 20-30 cm and 40-50 cm layers were Gaussian model, Gaussian model and Exponential model; (2) with the increase of soil depth, the spatial distribution of soil organic carbon increased, the spatial distribution of soil organic carbon in 0-10 cm layer was moderate, and the spatial distribution of soil organic carbon in 20-30 cm and 40-50 cm layers had a strong spatial distribution correlation and autocorrelation distances were 25.81 km, 20.26 km and 45.00 km, respectively; (3) anisotropy analysis showed that the variation degree of soil organic carbon in all directions was weakened with the increase of soil depth, and the half-variance of the same layer changed significantly in different directions, and the anisotropy was significant, the 45 ° direction from southwest to northeast and the southeast, the variance of the 45° direction showed the similarity; (4) the distribution of soil organic carbon in each layer was consistent; the soil organic carbon contents were higher in the southern part of the basin, in the north and north of the basin, and the middle and the south of the upper part of the basin. Soil organic carbon contents in the west and southwest was at the relatively moderate status, and topographic and vegetation distribution characteristics determine the distribution characteristics of soil organic carbon.