Abstract

Forest ecosystems play an important role in regional carbon and nitrogen cycling. Accurate and effective monitoring of their soil organic carbon (SOC) and soil total nitrogen (STN) stocks provides important information for soil quality assessment, sustainable forestry management and climate change policy making. In this study, a geographical weighted regression (GWR) model, a multiple stepwise regression (MLSR) model, and a boosted regression trees (BRT) model were compared to obtain the best prediction of SOC and STN stocks of the forest ecosystems in northeastern China. Five-hundred and thirteen topsoil (0–30 cm) samples (10.32 kg m−2 (±0.53) for SOC, 1.21 kg m−2 (±0.32) for STN), and 9 remotely-sensed environmental variables were collected and used for the model development and verification. By comparing with independent verification data, the best model (BRT) achieved R2 = 0.56 and root mean square error (RMSE) = 00.85 kg m−2 for SOC stocks, R2 = 0.51 and RMSE = 0.22 kg m−2 for STN stocks. Of all the remotely-sensed environment variables, soil adjusted vegetation index (SAVI) and normalized difference vegetation index (NDVI) are of the highest relative importance in predicting SOC and STN stocks. The spatial distribution of the predicted SOC and STN stocks gradually decreased from northeast to southwest. This study provides an attempt to rapidly predict SOC and STN stocks in the dense vegetation covered area. The results can help evaluate soil quality and facilitate land policy and regulation making by the government in the region.

Highlights

  • Carbon and nitrogen are two important chemical elements to maintain the structure and functioning of forest ecosystems [1]

  • Under the generalized skew distribution with skew coefficients of 0.54 and 0.63, the measured topsoil soil organic carbon (SOC) and soil total nitrogen (STN) stocks can be well described in this area

  • We found that the boosted regression trees (BRT) model had a lower uncertainty compared with geographical weighted regression (GWR) and multiple stepwise regression (MLSR) models

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Summary

Introduction

Carbon and nitrogen are two important chemical elements to maintain the structure and functioning of forest ecosystems [1]. Their cycling processes and interactions play a key role in regulating plant productivity, carbon sequestration potential, and stability of ecosystems [2]. Forest soil carbon stocks account for about 73% of global soil carbon, and have 3.5 × 105–5.5 × 105 Tg of nitrogen [1]. Climate can affect carbon and nitrogen changes in forest soils [5], plant distribution and productivity [6], and the change in soil organic carbon (SOC) and soil total nitrogen (STN) by changing the input of aboveground and underground litter [7]. Mapping soil carbon and nitrogen pools have become one of the core research topics in soil science, ecology and global climate change

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