Abstract

Keynote paper presented at the International Leucaena Conference, 1‒3 November 2018, Brisbane, Queensland, Australia.The introduction of leucaena (Leucaena leucocephala), apart from increasing animal production, improves soil fertility through biological nitrogen (N) fixation and its deep-rooted system. There is limited information on carbon and N dynamics in hedgerow silvopastoral systems, particularly in the subsoil profile. The concentrations and vertical distribution of organic carbon (OC) and total N , and their fractions (particulate and associate forms) in the profile (0‒100 cm) of a 4-year-old leucaena stand in a Urochloa brizantha-Chloris gayana pasture were compared with those in the adjacent pure tropical grass (U. brizantha) pasture. Leucaena introduction increased the OC concentration in the subsoil (20‒100 cm) by 45%, particularly the stable form (associate OC) in the deepest horizon (50‒100 cm). This was attributed to a greater abundance of leucaena roots deeper in the profile than for grass. Leucaena also enhanced by 7.6% the N concentration (from 0.131 to 0.141%) in the topsoil (0‒20 cm) associated with an increment in the labile form (particulate organic N), due to leaf deposition, recycling of animal feces and nodule-N turnover from N fixation. Leucaena establishment has the potential to improve soil fertility and hence availability of N to companion grass growth, and can be utilized as a greenhouse gas mitigation strategy.

Highlights

  • Sustaining or enhancing soil organic carbon (OC) and total nitrogen (TN) in grazing systems is essential for maintaining the chemical, biological and physical properties of soils, as well as mitigating greenhouse gases emitted by agriculture (Franzluebbers and Stuedemann 2009)

  • This stratification was more pronounced in soil supporting pure grass pasture (PP) than in soil supporting leucaena-grass pasture (LP), since OC concentrations continued to decline with depth in PP but no differences were observed between subsoil depths in LP

  • OC concentrations were similar for LP and PP (1.25±0.05% vs. 1.31±0.06%, respectively)

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Summary

Introduction

Sustaining or enhancing soil organic carbon (OC) and total nitrogen (TN) in grazing systems is essential for maintaining the chemical, biological and physical properties of soils, as well as mitigating greenhouse gases emitted by agriculture (Franzluebbers and Stuedemann 2009). There is some information in the Chaco region on carbon sequestration in tropical grass pastures (Banegas 2014) and in silvopastoral systems (Corbella et al 2015), there is no published information on changes in soil OC and TN levels and their fractions (particulate and associate forms) under grazed leucaena pastures. Associate organic carbon (AOC) comprises OC particles

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