Abstract

Abstract. In order to estimate a country-scale soil organic carbon (SOC) stock change in agricultural lands in Japan, while taking into account the effect of land-use changes, climate, different agricultural activities and the nature of soils, a spatially explicit model simulation system was developed using Rothamsted Carbon Model (RothC) with an integration of spatial and temporal inventories. Simulation was run from 1970 to 2008 with historical inventories. Simulated SOC stock was compared with observations in a nation-wide stationary monitoring program conducted during 1979–1998. Historical land-use change, characterized by a large decline in the area of paddy fields as well as a small but continuous decline in the area of orchards, occurred along with a relatively large increase in upland crop fields, unmanaged grasslands, and settlements (i.e. conversion of agricultural fields due to urbanization or abandoning). Results of the simulation on SOC stock change under varying land-use change indicated that land-use conversion from agricultural fields to settlements or other lands, as well as that from paddy fields to croplands have likely been an increasing source of CO2 emission, due to the reduction of organic carbon input to soils and the enhancement of SOC decomposition through transition of soil environment from anaerobic to aerobic conditions. The area-weighted mean concentrations of the simulated SOC stocks calculated for major soil groups under paddy fields and upland crop fields were comparable to those observed in the monitoring. Whereas in orchards, the simulated SOC stocks were underestimated. As the results of simulation indicated that SOC stock change under managed grasslands and settlements has been likely a major sink and source of CO2 emission at country-scale, respectively, validation of SOC stock change under these land-use types, which could not have been accomplished due to limited availability or a lack of measurement, remains a forthcoming challenge.

Highlights

  • Sequestration of soil organic carbon (SOC) in agricultural lands as an option to mitigate global climate change is considered to have significant technical potentials to reduce emission of CO2 or to act as CO2 sink at global scale (Lal, 2004; Smith et al, 2008)

  • We developed a system to perform estimation on SOC stock change in agricultural lands in Japan, with the objective (1) to provide useful information for decision support for policy making concerning a country-scale potential of soil carbon sequestration, as well as (2) to give estimates on a country-scale SOC stock change to be used in national green house gas inventory reporting to the United Nations Framework Convention on Climate Change (UNFCCC) for the sector of Land Use, Land Use Change and Forestry (LULUCF) or Agriculture, Forestry and Other Land Use (AFOLU), in accordance with Good Practice Guidance for Land Use, Land-Use Change and Forestry (GPG-LULUCF) (Intergovernmental Panel on Climate Change, 2003)

  • At country-level mean basis, the simulation indicated that managed grasslands have likely been sequestrating SOC (i.e. CO2 sink) with an influence of relatively greater rate of organic carbon input to soils estimated for this land-use type

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Summary

Introduction

Sequestration of soil organic carbon (SOC) in agricultural lands as an option to mitigate global climate change is considered to have significant technical potentials to reduce emission of CO2 or to act as CO2 sink at global scale (Lal, 2004; Smith et al, 2008). The SOC sequestration in agricultural lands has been attracting interest from international societies as Article 3.4 of Kyoto Protocol allows parties to include accounting on sinks or sources of CO2, due to SOC stock change in lands under cropland and grazing land management, to meet their target to reduce emissions of greenhouse gases (GHGs). Shirato : Rates and potentials of SOC sequestration in agricultural lands

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