首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Fractal features of soil particle-size distribution and total soil nitrogen distribution in a typical watershed in the source area of the middle Dan River, China.
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Fractal features of soil particle-size distribution and total soil nitrogen distribution in a typical watershed in the source area of the middle Dan River, China.

机译:丹江中游典型流域土壤粒径分布和总氮分布的分形特征

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Fractal scaling theory was employed to analyze the fractal dimension of soil particle-size distribution (PSD) for different plant communities with similar soil types in a watershed in the middle Dan River Valley, China. A total of 296 soil samples were collected from 78 sites. PSD and total soil nitrogen (TSN) were determined in soil from depths of 0-60 cm in four soil horizons for different plant communities. Soils in this area typically comprise silt and fine sand. The fractal dimensions of the six selected plant communities ranged from 2.73-2.89, with fractal dimension (Dm) values of grassland and forestland being lower (2.73-2.78) than those of cropland (2.81 and 2.89). There was an obvious decreasing trend in TSN content with increasing depth under the various plant communities. Spatial patterns of TSN changed significantly with land-use types. Organic nitrogen was the main component of soil nitrogen. There was a strong positive correlation between the fractal dimension and the silt and clay content (n=78, R2=0.96, P<0.01), with increasing Dm values corresponding to higher silt and clay contents. The Dm value and TSN content both indicated positive correlations with silt and clay content at a depth of 20-60 cm. These results demonstrate that fractal dimension analysis offers a useful approach to quantify and assess the degree of soil degradation among similar soil types, but that anthropogenic disturbances can have a great impact on the fractal dimensions for different land-use types. Cropland was prone to soil degradation, especially on steep slopes. Consequently, improved conservation measures are needed to enhance and sustain soil and water quality, and to prevent further soil degradation in the middle Dan River.
机译:分形标度理论被用来分析中国中部丹河流域中具有相似土壤类型的不同植物群落的土壤粒径分布的分形维数。从78个地点总共采集了296个土壤样品。在不同植物群落的四个土壤层中,从0-60 cm的深度确定了土壤中的PSD和总土壤氮(TSN)。该地区的土壤通常包括淤泥和细砂。六个选定植物群落的分形维数在2.73-2.89之间,草地和林地的分形维数(D m )值比农田(2.81和2.89)低(2.73-2.78)。 。在不同植物群落下,随着土壤深度的增加,TSN含量呈明显下降趋势。 TSN的空间格局随土地利用类型而显着变化。有机氮是土壤氮的主要成分。随着D m 值的增加,分形维数与淤泥和黏土含量之间呈强正相关(n = 78,R 2 = 0.96,P <0.01)。对应较高的淤泥和粘土含量。 D m 值和TSN含量均与20-60 cm深度的粉砂和粘土含量呈正相关。这些结果表明,分形维数分析为量化和评估相似土壤类型之间的土壤退化程度提供了一种有用的方法,但是人为干扰会对不同土地利用类型的分形维数产生很大影响。农田易于土壤退化,特别是在陡坡上。因此,需要改善保护措施,以增强和维持土壤和水质,并防止丹河中游的土壤进一步退化。

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