<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-25T02:27:23.526518791Z</responseDate><request verb="GetRecord" identifier="oai:repository.nwu.ac.za:10394/9513" metadataPrefix="dim">https://repository.nwu.ac.za/server/oai/request</request><GetRecord><record><header><identifier>oai:repository.nwu.ac.za:10394/9513</identifier><datestamp>2020-10-21T13:22:29Z</datestamp><setSpec>com_10394_26463</setSpec><setSpec>col_10394_26478</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Van Zyl, P.G.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Beukes, J.P.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Jaars, Kerneels</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="researchID">10710361 - Van Zyl, Pieter Gideon (Supervisor)</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="researchID">10092390 - Beukes, Johan Paul (Supervisor)</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2013-11-19T09:17:11Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="available">2013-11-19T09:17:11Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued">2012</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">http://hdl.handle.net/10394/9513</dim:field>
   <dim:field mdschema="dc" element="description">Thesis (MSc (Environmental Sciences))--North-West University, Potchefstroom Campus, 2013</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract" lang="en_US">Volatile organic compounds (VOCs) are emitted into the atmosphere from biogenic and&#xd;
anthropogenic sources with atmospheric lifetimes ranging from minutes to months,&#xd;
depending on the specific VOC compound considered. It is estimated that biogenic VOCs&#xd;
(BVOCs) (e.g. isoprenes, terpenes) make up 90% of the global atmospheric VOC budget.&#xd;
However, in highly industrialised regions, anthropogenic VOCs (e.g. benzene, toluene,&#xd;
ethylbenzene and xylene, combined abbreviated as BTEX) might dominate. VOCs have&#xd;
various reversible and irreversible effects on human health. They also have environmental&#xd;
impacts that range from changes in the population of terrestrial and aquatic ecosystems to the&#xd;
extinction of vulnerable species. VOCs are precursors for the formation of ozone (O3) during&#xd;
solar radiation initiated reactions in the presence of NOx. Tropospheric O3 is considered a&#xd;
pollutant, with negative impacts on human health, ecosystems and food security. O3 is also a&#xd;
short-lived greenhouse gas. Through reactions with radical species, VOCs lead to the&#xd;
formation of higher molecular weight organic compounds, which produce carbon monoxide&#xd;
(CO), peroxyacytyl nitrate (PAN) and ultimately secondary organic aerosol (SOA) particles.&#xd;
SOA particles impact directly on air quality and visibility, as well as directly and indirectly&#xd;
on the radiation balance of the earth that contributes to the regulation of climate.&#xd;
Notwithstanding the importance of atmospheric VOCs, limited data is available for VOCs in&#xd;
South Africa. In this study, a comprehensive dataset of BVOC and anthropogenic VOC&#xd;
species was obtained at the Welgegund measurement station in the North West Province,&#xd;
South Africa. Measurements were conducted from 9 February 2011 to 4 February 2012.&#xd;
Samples were collected on Tenax-TA and Carbopack-B adsorption tubes twice a week for&#xd;
two hours during day time and two hours during night time. The first 1.25m of the stainless&#xd;
steel sampling inlet was heated to 120ºC to remove O3 that could lead to sample degradation.&#xd;
Analyses of the sampled adsorption tubes were conducted by thermal desorption, cryofocusing,&#xd;
re-desorption, followed by gas chromatography separation and analysis with a mass&#xd;
selective detector (GC-MS).&#xd;
The results indicated that toluene was the most abundant aromatic hydrocarbon and heptane&#xd;
the most abundant alkane. Benzene is currently the only VOC listed as a criteria pollutant in&#xd;
the South African Air Quality Act with an annual average standard of 1.6ppb. The annual median benzene concentration was 0.13 ppb, while the highest daily benzene concentration&#xd;
measured was 8.7 ppb. No distinct seasonal cycles were identified for anthropogenic VOC&#xd;
species measured, i.e. aromatic hydrocarbons and alkanes. However, air mass history&#xd;
analysis indicated that air masses that passed over the Mpumalanga Highveld, the Vaal&#xd;
Triangle and the Johannesburg-Pretoria conurbation (collectively referred to as Area I) had&#xd;
significantly higher concentrations of these anthropogenic VOCs compared to air masses that&#xd;
passed over the western and eastern Bushveld Igneous Complex, and a region over which air&#xd;
masses typically followed an anti-cyclonic movement pattern (collectively referred to as Area&#xd;
II). Anthropogenic VOC levels in air masses that passed over the regional background (areas&#xd;
with no large point sources) had levels similar to air masses that had passed over Area II.&#xd;
Relatively good interspecies correlations (r > 0.8) between most of the aromatic&#xd;
hydrocarbons in air masses that had passed over Area I, with the exception of benzene,&#xd;
indicated that these species had common sources. Benzene, however, correlated well with&#xd;
CO, indicating that sources associated with incomplete combustion were most likely the&#xd;
origin of benzene in air masses that had passed over Area I.&#xd;
The interspecies concentration ratios for plumes passing over Area I indicated that this source&#xd;
region is relatively close to the Welgegund monitoring station and air masses that passed over&#xd;
this source region were substantially influenced by anthropogenic activities. The&#xd;
concentration ratios for plumes that passed over Area II and the Regional Background&#xd;
indicated that these were aged air masses. Furthermore, the concentration ratios of toluene,&#xd;
ethylbenzene and o,m,p-xylene (TEX) to the total aromatic concentration for air masses that&#xd;
passed over the various source regions showed a greater contribution to the total VOC&#xd;
concentration during periods of higher temperature, i.e. summer. This proved that the&#xd;
evaporation of solvents contributes significantly to VOC levels during the months with higher&#xd;
temperatures.&#xd;
The relative contribution of aromatic hydrocarbons to photochemical O3 formation in air&#xd;
masses that passed over the various source regions indicated the highest contribution was&#xd;
observed for air masses that passed over Area I, with Area II and the Regional Background in&#xd;
the same order of magnitude.&#xd;
The annual temporal variations of the measured BVOCs indicated that 2-methyl-3-buten-2-ol&#xd;
(MBO) and isoprene exhibited distinct seasonal patterns, i.e. higher values in summer and&#xd;
lower values in winter. The monoterpenes (MT) and the sesquiterpenes (SQT) did not follow distinct seasonal patterns. BVOC concentrations correlated relatively well to seasonal&#xd;
variations in temperature, photosynthetically active radiation (PAR), rainfall, relative&#xd;
humidity (RH) and CO2 flux. This proved that biogenic activity is responsible for BVOCs&#xd;
emitted. The most abundant MT was 􀄮-pinene, while 􀈕-caryophyllene was the most abundant&#xd;
SQT with annual median concentrations of 0.468 ppb and 0.022 ppb, respectively. Pollution&#xd;
roses for isoprene showed a dominance of sources from the north-west to the north-east, as&#xd;
well as the south-east. These directions correlated to areas where pockets of the savannah&#xd;
biome are located.</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="thesistype" lang="en_US">Masters</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso" lang="en_US">en</dim:field>
   <dim:field mdschema="dc" element="publisher">North-West University</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Volatile organic compounds (VOCs)</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Aromatic hydrocarbons</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Biogenic VOCs</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">BTEX</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Welgegund</dim:field>
   <dim:field mdschema="dc" element="title" lang="en">Temporal assessment of volatile organic compounds at a site with high atmospheric variability in the North–West Province</dim:field>
   <dim:field mdschema="dc" element="type" lang="en_US">Thesis</dim:field>
   <dim:field mdschema="others" element="access-status">open.access</dim:field>
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