Abstract

Abstract. Urbanisation is becoming increasingly important in terms of climate change and ecosystem functionality worldwide. We are only beginning to understand how the processes of urbanisation influence ecosystem dynamics, making peri-urban environments more vulnerable to nutrient losses. Brisbane in South East Queensland has the most extensive urban sprawl of all Australian cities. This research estimated the environmental impact of land use change associated with urbanisation by examining soil nitrogen (N) turnover and subsequent nitrous oxide (N2O) emissions using a fully automated system that measured emissions on a sub-daily basis. There was no significant difference in soil N2O emissions between the native dry sclerophyll eucalypt forest and an extensively grazed pasture, wherefrom only low annual emissions were observed amounting to 0.1 and 0.2 kg N2O ha−1 yr−1, respectively. The establishment of a fertilised turf grass lawn increased soil N2O emissions 18-fold (1.8 kg N2O ha−1 yr−1), with highest emissions occurring in the first 2 months after establishment. Once established, the turf grass lawn presented relatively low N2O emissions for the rest of the year, even after fertilisation and rain events. Soil moisture was significantly higher, and mineralised N accumulated in the fallow plots, resulting in the highest N2O emissions (2.8 kg N2O ha−1 yr−1) and significant nitrate (NO3−) losses, with up to 63 kg N ha−1 lost from a single rain event due to reduced plant cover removal. The study concludes that urbanisation processes creating peri-urban ecosystems can greatly modify N cycling and increase the potential for losses in the form of N2O and NO3−.

Highlights

  • Global urbanisation processes are becoming increasingly important in terms of global warming and ecosystem functionality

  • The turf grass and fallow treatment were established within the pasture and share the same soil profile with its characteristics, except for bulk density in the A1 horizon, which changed after the turf grass establishment from 1.4 to 1.2 g cm−3

  • This study provides evidence that land use change associated with urbanisation accelerates N turnover and increases N2O emissions from soils by presenting the first high-temporalfrequency data set on peri-urban soils in the subtropics for a full year after land use change

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Summary

Introduction

Global urbanisation processes are becoming increasingly important in terms of global warming and ecosystem functionality. Urban sprawl and increasing population densities are causing severe land use changes from intact biomes and commercially focused agriculture into smaller residential properties with introduced species. This transition from rural to semi-rural, i.e. peri-urban, and urban environments is increasingly associated with development and construction processes and the extensive establishment of turf grass for residential backyards, public parks and sports grounds, and golf courses (IPCC, 2006). How these urbanisation processes influence ecosystem dynamics in biogeochemical cycling, and contribute to ecosystem vulnerability and global warming, is only beginning to be understood. On the other hand, changing soils from agricultural to residential use in temperate climates has shown the potential to improve critical ecosystem services by (i) providing stormwater treatment, (ii) acting as a sink for atmospheric nitrogen (N), and (iii) sequestering C (Golubiewski, 2006; Raciti et al, 2011)

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