Abstract

ABSTRACT Water erosion under tropical climate conditions is one of the main processes that change the balance between the inputs and outputs of soil organic carbon (SOC). Water erosion modeling using the Erosion Potential Method (EPM) can be used as an alternative to assist in understand soil carbon dynamics and its interaction with the erosive process. In this context, the objective of the study was to estimate carbon losses by water erosion in a watershed with a wide land-use diversity. The modelling was performed based on the soil organic matter content (SOM) of the area, and the estimated soil losses, according EPM. To the SOM determination, soil samples were collected 50 points (0-0.2 m) distributed in the watershed. The data analysis was performed using remote sensing techniques and a Geographic Information System, which was also used to interpolate the SOM content, through the use of the ordinary kriging. The results showed that from 126.53 Mg year-1 of the total eroded organic carbon estimated, 111.60 Mg year-1 were deposited in relief depressions, while 14.93 Mg year-1 reached the water body system. The applied methodology represents a cost-effective and relatively fast method to estimate the soil organic carbon loss by water erosion and allows the determination of the areas that most need intervention, aiming to decrease the impact of agriculture on greenhouse gas emissions. The main advantage of this method is the little input data requirement, which increases the possibility of application in poorly studied regions.

Highlights

  • The increased concentration of greenhouse gases in the atmosphere has drawn attention to soil organic carbon (SOC), as soils are the highest carbon reservoir of all terrestrial ecosystems (LAL, 2003)

  • Water erosion under tropical climate conditions is one of the main processes that change the balance between the inputs and outputs of soil organic carbon (SOC) (LAL, 2019)

  • The few studies found in the literature may be explicated to the fact of field assessments of soil organic carbon (SOC) loss by water erosion can be costly and consume much time

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Summary

Introduction

The increased concentration of greenhouse gases in the atmosphere has drawn attention to soil organic carbon (SOC), as soils are the highest carbon reservoir of all terrestrial ecosystems (LAL, 2003). Water erosion under tropical climate conditions is one of the main processes that change the balance between the inputs and outputs of soil organic carbon (SOC) (LAL, 2019). This process causes soil loss, exposing the stabilized organic carbon inside the aggregates to the climatic elements and the microbial enzymes (DECHEN et al, 2015). Data obtained from experimental plots are unable to represent an entire watershed due to the broad topographic and edaphic variations of the area (STARR et al, 2000) In this context, monitoring soil carbon removed by water erosion in the hydrographic basin scale can be realized using modeling techniques (HANCOCK et al, 2019; PARSONS, 2019; PRASANNAKUMAR et al, 2012)

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