Please use this identifier to cite or link to this item: http://dx.doi.org/10.14279/depositonce-6991
Main Title: Massive carbon addition to an organic-rich Andosol increased the subsoil but not the topsoil carbon stock
Author(s): Zieger, Antonia
Klaus, Kaiser
Ríos Guayasamín, Pedro
Kaupenjohann, Martin
Type: Article
Language Code: en
Abstract: Andosols are among the most carbon-rich soils, with an average of 254 Mg ha−1 organic carbon (OC) in the upper 100 cm. A current theory proposes an upper limit for OC stocks independent of increasing carbon input, because of finite binding capacities of the soil mineral phase. We tested the possible limits in OC stocks for Andosols with already large OC concentrations and stocks (212 g kg−1 in the first horizon, 301 Mg ha−1 in the upper 100 cm). The soils received large inputs of 1800 Mg OC ha−1 as sawdust within a time period of 20 years. Adjacent soils without sawdust application served as controls. We determined total OC stocks as well as the storage forms of organic matter (OM) of five horizons down to 100 cm depth. Storage forms considered were pyrogenic carbon, OM of < 1.6 g cm−3 density and with little to no interaction with the mineral phase, and strongly mineral-bonded OM forming particles of densities between 1.6 and 2.0 g cm−3 or > 2.0 g cm−3. The two fractions > 1.6 g cm−3 were also analysed for aluminium-organic matter complexes (Al–OM complexes) and imogolite-type phases using ammonium-oxalate–oxalic-acid extraction and X-ray diffraction (XRD). Pyrogenic organic carbon represented only up to 5wt% of OC, and thus contributed little to soil OM. In the two topsoil horizons, the fraction between 1.6 and 2.0 g cm−3 had 65–86wt% of bulk soil OC and was dominated by Al–OM complexes. In deeper horizons, the fraction > 2.0 g cm−3 contained 80–97 wt % of the bulk soil's total OC and was characterized by a mixture of Al–OM complexes and imogolite-type phases, with proportions of imogolite-type phases increasing with depth. In response to the sawdust application, only the OC stock at 25–50 cm depth increased significantly (α=0.05, 1−β=0.8). The increase was entirely due to increased OC in the two fractions > 1.6 g cm−3. However, there was no significant increase in the total OC stocks within the upper 100 cm. The results suggest that long-term large OC inputs cannot be taken up by the obviously OC-saturated topsoil but induce downward migration and gradually increasing storage of OC in subsurface soil layers. The small additional OC accumulation despite the extremely large OC input over 20 years, however, shows that long time periods of high input are needed to promote the downward movement and deep soil storage of OC.
URI: https://depositonce.tu-berlin.de//handle/11303/7816
http://dx.doi.org/10.14279/depositonce-6991
Issue Date: 7-May-2018
Date Available: 24-May-2018
DDC Class: 570 Biowissenschaften; Biologie
550 Geowissenschaften, Geologie
Subject(s): Andosol
organic carbon
Sponsor/Funder: DFG, TH 662/19-1, Open Access Publizieren 2017 - 2018 / Technische Universität Berlin
License: https://creativecommons.org/licenses/by/4.0/
Journal Title: Biogeosciences
Publisher: Copernicus Publications
Publisher Place: Göttingen
Volume: 15
Issue: 9
Publisher DOI: 10.5194/bg-15-2743-2018
Page Start: 2743
Page End: 2760
ISSN: 1726-4170
Appears in Collections:FG Bodenkunde » Publications

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