Abstract

Conversion of agricultural lands to forest plantations to mitigate rising atmospheric carbon dioxide (CO2) has been proposed, but it depends on accurate estimation of the on-site carbon (C) stocks distribution. The use of aerial laser scanning (ALS) data is a rapidly evolving technology for the quantification of C stocks. We evaluated the use of allometric models together with high-density ALS data for the quantification of biomass and soil C stocks in a 14-year-old Quercus ilex and Q. suber plantation in Southwestern Spain. In 2010, a field survey was performed and tree dasometric and biomass variables were measured. Forty-five soil profiles (N = 180 soil samples) were taken systematically and the soil organic C content (SOC) was determined. Biomass and soil organic C values were regressed against individual dasometric variables and total tree height was used as a predictor variable. Aerial laser scanning data were acquired with a point density of 12 points m−2. Relationships among ALS metrics and tree height were determined using stepwise regression models and used in the allometric models to estimate biomass and SOC C stocks. Finally, a C stock map of the holm-cork oak cover in the study area was generated. We found a tree total biomass of 27.9 kg tree−1 for holm oak and 41.1 kg tree−1 for cork oak. In the holm oak plantation, the SOC content was 36.90 Mg ha−1 for the layer 0–40 cm (SOC40) under the tree crown and 29.26 Mg ha−1 for the inter-planted area, with significant differences from the reference agricultural land (33.35 Mg ha−1). Linear regression models were developed to predict the biomass and SOC at the tree scale, based on tree height (R2 > 0.72 for biomass, and R2 > 0.62 for SOC). The overall on-site C stock in the holm-cork oak plantation was 35.11 Mg ha−1, representing a net C stock rise of 0.47 Mg ha−1 yr−1. The ALS data allows a reliable estimation of C stocks in holm and cork oak plantations and high-resolution maps of on-site C stocks are useful for silvicultural planning. The cost of ALS data acquisition has decreased and this method can be generalised to plantations of other Mediterranean species established on agricultural lands at regional scales. However, an increase of filed data and the availability of local biomass and, in particular, SOC will improve accurate quantification of the C stocks from allometric equations, and extrapolation to large planted areas.

Highlights

  • Afforestation of set-aside agricultural lands was promoted by the European EconomicCommunity’s approval of the CEE 2080/92 directive, which established a Community aid scheme for forestry measures in agriculture to promote the transformation of agricultural lands into forest [1].The ecosystem importance of forests has long been recognised worldwide

  • The change from agricultural land to a forest plantation resulted in an increase in the biomass C stock

  • It resulted in a slight loss of soil organic C content (SOC) 14 years after afforestation

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Summary

Introduction

Afforestation of set-aside agricultural lands was promoted by the European EconomicCommunity’s approval of the CEE 2080/92 directive, which established a Community aid scheme for forestry measures in agriculture to promote the transformation of agricultural lands into forest [1].The ecosystem importance of forests has long been recognised worldwide. Afforestation of set-aside agricultural lands was promoted by the European Economic. Community’s approval of the CEE 2080/92 directive, which established a Community aid scheme for forestry measures in agriculture to promote the transformation of agricultural lands into forest [1]. From 1994 to 2006, an overall area of 232,858 ha of new forest plantations was established in Andalusia (Southwestern Spain), of which. Andalusia was the European region with the largest area of holm oak plantations in the Community forest plantation scheme due to the ecological and economic importance of this species in dehesa (savanna-type Mediterranean ecosystems). Carbon is stored in forest ecosystems in different fractions, in the biomass of living vegetation and in litter and forest soils [6]. Soils store three-times more CO2 than living biomass and two-times more than the atmosphere [9]

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