Predictive Mapping of Topsoil Organic Carbon in an Alpine Environment Aided by Landsat TM

PLoS One. 2015 Oct 16;10(10):e0139042. doi: 10.1371/journal.pone.0139042. eCollection 2015.

Abstract

The objective of this study was to examine the reflectance of Landsat TM imagery for mapping soil organic Carbon (SOC) content in an Alpine environment. The studied area (ca. 3*104 km2) is the upper reaches of the Heihe River at the northeast edge of the Tibetan plateau, China. A set (105) of topsoil samples were analyzed for SOC. Boosted regression tree (BRT) models using Landsat TM imagery were built to predict SOC content, alone or with topography and climate covariates (temperature and precipitation). The best model, combining all covariates, was only marginally better than using only imagery. Imagery alone was sufficient to build a reasonable model; this was a bit better than only using topography and climate covariates. The Lin's concordance correlation coefficient values of the imagery only model and the full model are very close, larger than the topography and climate variables based model. In the full model, SOC was mainly explained by Landsat TM imagery (65% relative importance), followed by climate variables (20%) and topography (15% of relative importance). The good results from imagery are likely due to (1) the strong dependence of SOC on native vegetation intensity in this Alpine environment; (2) the strong correlation in this environment between imagery and environmental covariables, especially elevation (corresponding to temperature), precipitation, and slope aspect. We conclude that multispectral satellite data from Landsat TM images may be used to predict topsoil SOC with reasonable accuracy in Alpine regions, and perhaps other regions covered with natural vegetation, and that adding topography and climate covariables to the satellite data can improve the predictive accuracy.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Carbon / analysis*
  • Soil / chemistry*
  • Tibet
  • Tundra*

Substances

  • Soil
  • Carbon

Grants and funding

This work was supported by the National Natural Science Foundation of China (Nos: 41130530, 91325301, 41201207, 41571212, 41371224). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.