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Organic carbon in Icelandic Andosols: Geographical variation and impact of erosion

Research output: Contribution to journalArticlepeer-review

Abstract

The extensive soil erosion in Iceland during the past millennium has led to an irregular distribution of soil organic carbon (SOC). Intact and fully vegetated areas typically have Andosols with large amounts of organic carbon, whereas eroded areas are barren deserts with little organic carbon. We estimate the amount of organic carbon eroded during the past millennium is 120-500×106 t, whereas the total organic carbon in Icelandic soils is 2.1×109 t. Approximately half of the eroded organic carbon (60-250×106 t C) has been oxidized and released to the atmosphere. Current ongoing losses of SOC are estimated to be 50-100×103 t C yr-1. We also consider procedures for sequestering carbon to restore the carbon dynamics of denuded areas.

Original languageEnglish
Pages (from-to)225-238
Number of pages14
JournalCatena
Volume56
Issue number1-3
DOIs
Publication statusPublished - 21 Apr 2004

Bibliographical note

Funding Information: This paper is built on a synthesis of data derived from various studies and we gratefully acknowledge the work done by the following: Berglind Orradóttir, Elı́n Ásgeirsdóttir, Barbara Duran, Rannveig Guicharnaud and the staff of the Icelandic Soil Conservation Service. We are also grateful for the encouragement and inspiration of the European COST-622 group, and for permission to use their data. Some of the studies on which this paper is built were funded by grants from the National Power Company (Landsvirkjun) and Rala Government funds.

Other keywords

  • Andosol
  • Carbon sequestration
  • Erosion
  • Iceland
  • Soil organic carbon
  • Volcanic soils

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