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Updated: Apr 11, 2026

Use of Principal Components for Scaling Up Topographic Models to Map Soil Redistribution and Soil Organic Carbon
Published on: October 16, 2018
Three-Dimensional Mapping of Soil Organic Carbon by Combining Kriging Method with Profile Depth Function
Chong Chen1, Kelin Hu1, Hong Li2
1Department of Soil and Water Sciences, China Agricultural University, No 2, Yuan Ming Yuan Xi Lu, Beijing 100193, China.
This study maps soil organic carbon (SOC) in 3D using a novel kriging method. Results show SOC distribution is influenced by soil texture and land use, crucial for effective land management.
Area of Science:
- Soil Science
- Geospatial Analysis
- Environmental Science
Background:
- Spatial variation of soil organic carbon (SOC) is critical for land management.
- Vertical SOC distribution is complex due to soil texture and depth, challenging traditional 3D mapping.
- Existing 3D ordinary kriging methods are limited by the non-stationary nature of SOC in the vertical dimension.
Purpose of the Study:
- To develop and apply a 3D kriging method combined with profile depth function (KPDF) for regional SOC mapping.
- To investigate the influence of soil texture and land use on the vertical distribution of SOC.
- To create a 3D spatial distribution map of SOC in Quzhou County, China.
Main Methods:
- Collected 605 soil samples from 121 profiles (0.0-1.0 m depth) in Quzhou County.
- Applied the Kriging with Profile Depth Function (KPDF) method to model and map 3D SOC distribution.
- Analyzed correlations between SOC content, depth, soil texture, and land use type.
Main Results:
- The KPDF method accurately predicted SOC content, with R²=0.52 and RMSE=1.82 g kg⁻¹.
- An exponential equation effectively described the vertical distribution of mean SOC content.
- Surface SOC was high in the mid-west and south, low in the southeast; land use impacted surface SOC more than texture, while texture dominated deeper layers (0.2-0.4 m).
Conclusions:
- The KPDF method is suitable for generating 3D SOC distribution maps at a regional scale.
- Soil texture and land use significantly affect SOC spatial distribution, particularly in vertical profiles.
- Understanding these factors is essential for optimizing land use and soil management strategies.
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Topographic Surveying and Contours
Plotting of Topographic Maps
Levels of Use of a GIS
Profile Leveling and Cross Sections
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