Biogeochemical factors related with organic matter degradation and C storage in agricultural volcanic ash soils

• Published in: Soil biology & biochemistry 2012-01, Vol.44 (1), p.130-142
• Main Authors: Hernández, Z., Almendros, G.
• Format: Article
• Language: English
• Subjects: Agronomy. Soil science and plant productions; Allophanic soils; Biochemistry and biology; Biological and medical sciences; C mineralization; Chemical, physicochemical, biochemical and biological properties; Fundamental and applied biological sciences. Psychology; Humic acid; Laboratory incubation; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Selective preservation; Soil science; Vineyards
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/j.soilbio.2011.08.009

Laboratory incubation experiments in addition to physicochemical analyses of volcanic ash soils were carried out in order to identify biogeochemical factors related with soil organic C (SOC) stabilization in the long term and with the potential for C sequestration of agroecosystems. Up to 24 vineyard plots under similar subtropical conditions in Tenerife Island (Spain) were sampled. Soil samples were incubated for 30 days in laboratory conditions (27 °C and 66% water holding capacity) and the CO2 released was periodically measured to plot C mineralization curves. Soil organic matter (SOM) with special emphasis paid on the humic acid (HA) was characterized by elemental composition, spectroscopic techniques: visible, infrared (IR) and 13C nuclear magnetic resonance (13C NMR) and analytical pyrolysis–gas chromatography/mass spectrometry (GC/MS). The dependent variables examined were either the total mineralization coefficient (TMC, g C · kg C soil−1 day−1) in laboratory incubations, or the SOC. A very significant negative correlation was found between SOC and TMC, i.e., in our soils, the higher the biodegradation rates under laboratory conditions, the lower the soil C sequestered in the corresponding plots. In it was also observed that the concentration of amorphous minerals (Alo + ½ Feo index) and the water holding capacity at 0.033 MPa were associated with lower CO2 release; the latter could suggest microanaerobic conditions hampering biodegradation in these thixotropic soils. Conversely, no correlation was found between SOC or TMC and typical soil physical and chemical factors, such as granulometric fractions or exchangeable calcium. The molecular characteristics of the HAs showed also predictive potential as regards SOC resilience, reflecting the comparatively fast biodegradation of SOM composed mainly of biomass constituents (prominent lignin signature and O-alkyl 13C NMR region). The poor correlation between total aromaticity of the HAs and SOM resistance against biodegradation could be explained by a dual origin of aromatic structures in HAs, either consisting of methoxyl-containing non-decomposed lignin structures or condensed black carbon-like polyaromatic structures. The results suggested the possibility of predicting the vulnerability of SOC to biodegradation from laboratory incubation experiments, which results of interest for modeling global change scenarios. ► The soil C mineralization under laboratory was a good predictor of C loss in field. ►