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RESEARCH ARTICLE

Role of root inputs from a dinitrogen-fixing tree in soil carbon and nitrogen sequestration in a tropical agroforestry system

Jorge Sierra A D and Pekka Nygren B C
+ Author Affiliations
- Author Affiliations

A Unité Agropédoclimatique de la Zone Caraïbe, INRA Antilles-Guyane, Domaine Duclos (Prise d’eau), 97170 Petit-Bourg, Guadeloupe (French Antilles), France.

B Center for Agroforestry, University of Missouri–Columbia, 203 Natural Resources Building, Columbia, MO 65211, USA.

C Present address: Department of Forest Ecology, PO Box 27, 00014 University of Helsinki, Finland.

D Corresponding author. Email: sierra@antilles.inra.fr

Australian Journal of Soil Research 43(5) 667-675 https://doi.org/10.1071/SR04167
Submitted: 16 November 2004  Accepted: 20 April 2005   Published: 8 August 2005

Abstract

Agroforestry is often mentioned as a suitable technology for land rehabilitation in the tropics and for mitigation of climate change because this land-use favours nutrient recycling and C sequestration. The aim of this work was to estimate soil C sequestration in a 12-year-old tropical silvopastoral system composed of a legume tree (Gliricidia sepium) and a C4 fodder grass (Dichanthium aristatum), and to link it with tree root biomass and N status in the soil. The site was under cut-and-carry management, i.e. tree pruning residues and cut grass were removed from the field and fed to stabled animals elsewhere. Thus, main sources for tree C and N inputs were root activity and turnover. Organic C derived from the trees and tree root biomass were determined based on natural 13C abundance. For the 0–0.2 m soil layer, the biomass of tree roots ≤2 mm diameter was 2.4 Mg/ha when the trees were pruned every 6 months (SS6), and 0.6 Mg/ha when pruned every 2 months (SS2). Both C (R2 = 0.39, P < 0.05) and N (R2 = 0.82, P < 0.05) sequestration were correlated with tree root biomass. The trees and grass contributed 18 and 8 Mg C/ha to soil, respectively, over the 12-year experiment in SS6. The net increase of 2.5 Mg N/ha in soil, originating from the trees, contributed to the net soil C sequestration. In SS2, trees contributed 16 Mg C/ha to soil over 12 years, but grass-derived C was reduced by 2 Mg C/ha because of the small amount of grass litter. The increase of 1.7 Mg N/ha in soil, derived from the trees, was not large enough to avoid C loss in this plot. Differences in soil C and N sequestration between plots were due to differences in system management, which affected the amount and the C/N ratio of inputs and outputs.

Additional keywords: natural 13C abundance, tree pruning, Vertisol, Vertosol.


Acknowledgments

We thank Saint-Ange Sophie (Agropedoclimatic Station) for skilful technical assistance and for the management of the experimental plots since 1989; Roxane Fagan (Stable Isotope Laboratory of the Kansas State University, USA) for carrying out the mass spectrometry of 13C samples; and Alan Scaife for reviewing the English manuscript. This work was financed by funds from the University of Missouri Life Sciences Mission Enhancement Programme (PN) and the Department Environment and Agronomy of the Institut National de la Recherche Agronomique, France (JS).


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