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Spatial distribution characteristics of phaeozem in Songliao Plain based on RS
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Phaeozem is one kind of scarce resources on the earth. Due to the restrictions of natural factors and the influence of human activities over the years, phaeozem degradation has become increasingly serious. Based on images of the ASTER in 2006 and the ETM+ in 2000 in this paper, the phaeozem organic matter content which is greater than 2 % was obtained by using quantitative retrieval. Through the three-dimensional remote sensing image, terrain rendering and relevant information were analyzed. On the basis of the above, the spatial distribution characteristics of phaeozem in Songliao Plain were analyzed using DEM (digital elevation model) data. The results show that the total area of phaeozem in Songliao Plain is about 51360.15 km2, and the phaeozem organic matter content is gradually increasing along with the increasing latitude or longitude, and decreasing along with increasing slope. In addition, the soil organic matter content is lower in southern slopes than that in northern slopes.
Title: Spatial distribution characteristics of phaeozem in Songliao Plain based on RS
Description:
Phaeozem is one kind of scarce resources on the earth.
Due to the restrictions of natural factors and the influence of human activities over the years, phaeozem degradation has become increasingly serious.
Based on images of the ASTER in 2006 and the ETM+ in 2000 in this paper, the phaeozem organic matter content which is greater than 2 % was obtained by using quantitative retrieval.
Through the three-dimensional remote sensing image, terrain rendering and relevant information were analyzed.
On the basis of the above, the spatial distribution characteristics of phaeozem in Songliao Plain were analyzed using DEM (digital elevation model) data.
The results show that the total area of phaeozem in Songliao Plain is about 51360.
15 km2, and the phaeozem organic matter content is gradually increasing along with the increasing latitude or longitude, and decreasing along with increasing slope.
In addition, the soil organic matter content is lower in southern slopes than that in northern slopes.
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