Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa

Soils of arid and semi-arid ecosystems are important biogenic sources of atmospheric nitric oxide (NO), however, there is still a shortage of measurements from these systems. Here we present the results of a laboratory study of the biogenic emission of NO from four different landscape positions of t...

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Main Authors: G. T. Feig, B. Mamtimin, F. X. Meixner
Format: Article
Language:English
Published: Copernicus Publications 2008-12-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/5/1723/2008/bg-5-1723-2008.pdf
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spelling doaj-5a6d9fc90b3248708fbe322bd75f889b2020-11-24T23:30:21ZengCopernicus PublicationsBiogeosciences1726-41701726-41892008-12-015617231738Soil biogenic emissions of nitric oxide from a semi-arid savanna in South AfricaG. T. FeigB. MamtiminF. X. MeixnerSoils of arid and semi-arid ecosystems are important biogenic sources of atmospheric nitric oxide (NO), however, there is still a shortage of measurements from these systems. Here we present the results of a laboratory study of the biogenic emission of NO from four different landscape positions of the Kruger National Park (KNP), a large conservation area in a semi-arid region of South Africa. Results show that the highest net potential NO fluxes come from the low lying (footslope) landscape regions, which have the largest nitrogen stocks and highest rates of nitrogen input into the soil. Net potential NO fluxes from midslope and crest regions were considerably lower. The maximum release of NO occurred at fairly low soil moisture contents of 10%–20% water filled pore space. Using soil moisture and temperature data obtained in situ at the Kruger National Park flux tower site, net potential NO fluxes obtained in the laboratory were converted to field fluxes for each of the four landscape positions for the period 2003 to 2005. The highest field NO flux is from footslope positions, during each of these years and emissions ranged from 1.5–8.5 kg ha a (in terms of mass of nitrogen). Remote sensing and Geographic Information Systems techniques were used to up-scale field NO fluxes on a regional basis indicating that the highest emissions occurred from the midslope positions, due to their large geographical extent in the considered research area. Emissions for the KNP Skukuza land type (56 000 ha) ranged from 20×10<sup>3</sup> kg in 2004 to 34×10<sup>3</sup> kg in 2003. The importance of landscape characteristics in the determination of regional biogenic NO soil emission is emphasized. http://www.biogeosciences.net/5/1723/2008/bg-5-1723-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. T. Feig
B. Mamtimin
F. X. Meixner
spellingShingle G. T. Feig
B. Mamtimin
F. X. Meixner
Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
Biogeosciences
author_facet G. T. Feig
B. Mamtimin
F. X. Meixner
author_sort G. T. Feig
title Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
title_short Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
title_full Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
title_fullStr Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
title_full_unstemmed Soil biogenic emissions of nitric oxide from a semi-arid savanna in South Africa
title_sort soil biogenic emissions of nitric oxide from a semi-arid savanna in south africa
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2008-12-01
description Soils of arid and semi-arid ecosystems are important biogenic sources of atmospheric nitric oxide (NO), however, there is still a shortage of measurements from these systems. Here we present the results of a laboratory study of the biogenic emission of NO from four different landscape positions of the Kruger National Park (KNP), a large conservation area in a semi-arid region of South Africa. Results show that the highest net potential NO fluxes come from the low lying (footslope) landscape regions, which have the largest nitrogen stocks and highest rates of nitrogen input into the soil. Net potential NO fluxes from midslope and crest regions were considerably lower. The maximum release of NO occurred at fairly low soil moisture contents of 10%–20% water filled pore space. Using soil moisture and temperature data obtained in situ at the Kruger National Park flux tower site, net potential NO fluxes obtained in the laboratory were converted to field fluxes for each of the four landscape positions for the period 2003 to 2005. The highest field NO flux is from footslope positions, during each of these years and emissions ranged from 1.5–8.5 kg ha a (in terms of mass of nitrogen). Remote sensing and Geographic Information Systems techniques were used to up-scale field NO fluxes on a regional basis indicating that the highest emissions occurred from the midslope positions, due to their large geographical extent in the considered research area. Emissions for the KNP Skukuza land type (56 000 ha) ranged from 20×10<sup>3</sup> kg in 2004 to 34×10<sup>3</sup> kg in 2003. The importance of landscape characteristics in the determination of regional biogenic NO soil emission is emphasized.
url http://www.biogeosciences.net/5/1723/2008/bg-5-1723-2008.pdf
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