Characterisation of spatial variability in water quality in the Great Barrier Reef catchments using multivariate statistical analysis
Introduction
Degradation of water quality is a global issue (Schwarzenbach et al., 2010). Human activities, such as agriculture and urbanisation, are major causes of water quality degradation (Zia et al., 2013). For example, Bricker et al. (2014) showed that the excess nutrient discharge to coastal waters in the Chesapeake Bay region of the USA over the past 200 years was linked to increased anthrophonic pressures, including discharge from sewage treatment plants, and runoff from urban and agricultural land uses.
In-stream surface water quality is important for the health of inland and coastal waters (De'ath et al., 2012; Harris, 2001; Packett et al., 2009). For instance, discharge of sediments and nutrients to marine ecosystems from inland catchments poses a threat to near-shore tropical coral reefs globally (Aronson et al., 2014; Ginsburg and Shinn, 1995). Coral reefs maintain not only environments with rich biodiversity, but they also provide economic benefits from tourism, fishing and aquaculture (Chabanet et al., 1997; Connell, 1978). The ecosystem in the Great Barrier Reef (GBR), Australia, has been deteriorating during recent decades (DeVantier et al., 2006). It is estimated that the GBR-wide coral cover has decreased by 50% since 1985, and the coral cover on inshore reefs has declined by 34% since 2005 (Brodie et al., 2013). De Valck and Rolfe (2018) estimated that failure to maintain water quality in GBR could result in substantial losses of local economic benefits associated with tourism.
While there are many reasons for the reduction in coral cover in the Great Barrier Reef, poor quality of the water discharging into the reef from the inland catchments is thought to be one major cause (Brodie et al., 2012; Hunter and Walton, 2008; McKergow et al., 2005). Suspended sediments (often derived from soil erosion) have resulted in a reduction in the light essential for organisms in marine ecosystems, including seagrass and coral. Sediments and organic rich flocculent masses can also smother marine organisms when particles settle out (Brodie et al., 2013; Haynes, 2001). Nutrients, especially nitrogen and phosphorus, have been closely linked to the observed decline in coral cover through these two mechanisms. Excessive nutrients have facilitated outbreaks of the crown-of-thorns starfish, a major coral predator (Brodie et al., 2005; Fabricius et al., 2010), and they have also been implicated in coral bleaching (Hoegh-Guldberg et al., 2007; Wooldridge and Done, 2009).
To protect aquatic environmental health and values in both rivers and bays, it is recognised that an improved water quality management strategy is essential (Lynam et al., 2010; Santhi et al., 2006; Sidle et al., 2006). This requires a sound understanding of the underlying reasons for water quality degradation in these rivers. However, constituent concentrations are highly variable in space and time due to hydrological variability (Allan et al., 1997), physical and bio-chemical processes (Ayers and Westcot, 1985; Letterman, 1999; Melching and Flores, 1999) and hydrological transport (Hrachowitz et al., 2016). Therefore, it is important to understand the spatial and temporal controls of water quality (Zhou et al., 2007b).
Previous studies of the Great Barrier Reef catchments using the water quality record have been conducted which either estimated the constituent loads (Kroon et al., 2012; Wallace et al., 2016), or focus on small scale or individual catchments land use effect of pollutant exports (Hunter and Walton, 2008; Packett et al., 2009; Stephen Lewis et al., 2014). Other efforts to understand variations in water quality in the Great Barrier Reef catchment have centred on modelling (Carroll et al., 2012; McCloskey et al., 2011; Waters et al., 2013). Through these earlier studies, a conceptual understanding of the role of different catchment characteristics in controlling differences in water quality between catchment is emerging. In addition, given the importance of catchment water quality to the Great Barrier Reef marine ecosystem, a detailed water quality monitoring system has been implemented by the Queensland Department of Science, Information and Innovation (DSITI). The detailed catchment scale monitoring data resulting from that monitoring system has not been systematically compared with catchment characteristics to date.
Most studies addressing the association between water quality and catchment characteristics have focused on temperate catchments in Asia, America and Europe (Ding et al., 2016; Donohue et al., 2006; Lowrance et al., 1997; Renard et al., 1997; Rice et al., 2015; Suif et al., 2016; Vrebos et al., 2017; Wu et al., 2015). Much less research has been undertaken in tropical catchments, like the Great Barrier Reef catchments. The key anthropogenic influences leading to water quality degradation in the Great Barrier Reef catchments have previously been studied at local scales. These include the relationship between sediment and particulate nutrients and erosion processes, and between non-point source dissolved nutrient and pesticide pollution from agricultural activities (Davis et al., 2016, Davis et al., 2017; Kroon et al., 2012; Kroon et al., 2016; Kuhnert et al., 2012; McKergow et al., 2005). These working hypotheses need continual testing as more detailed data emerge.
Multivariate statistical techniques can be used to explore the underlying patterns and potentially the processes affecting multi-site, multi-parameter water quality time-series data. Studies have used multivariate techniques such as cluster analysis and principal component analysis to interpret complex environmental monitoring data (Ouyang et al., 2014; Singh et al., 2004), identify sources of spatial variability in water quality (Mitra et al., 2018; Yang et al., 2010; Zhou et al., 2007a) and assessing monitoring networks (Shrestha and Kazama, 2007; Zhang et al., 2009). For instance, Li et al. (2011) used cluster analysis to detect the key groups of sites with similar water quality responses along the Middle Route of the South to North Water Transfer Project, China. They identified three groups of sites, reflecting the water quality responses of the sites, reflecting the main drivers of water quality: natural, agricultural and industrial sources.
It is well recognised that spatial and temporal dynamics in water quality are influenced by a wide range of natural and anthropogenic factors (Alberto et al., 2001; Kuhnert et al., 2012; Pratt and Chang, 2012; Singh et al., 2004). In this paper, serving as the initial part of a large study that aims to understand both spatial and temporal responses in water quality, we concentrate on the key catchment characteristics affecting spatial variability in stream water quality. We analysed water quality monitoring data from thirty-two sites using multivariate statistical analysis, over an 11-year period (2006–2016), using the time-averaged constituents concentrations (discussed in Section 2.4, Data preparation). The aim of the present study was to characterise spatial water quality variation, and to evaluate the relationships between spatial variations in water quality and catchment characteristics (e.g., land use, catchment geological, topographic and climatic conditions). The findings from the Great Barrier Reef catchments contribute to the growing understanding and knowledge of the key factors affecting spatial variability in water quality. In particular, this study addresses the following questions. (i) How strong is the spatial pattern in the concentration of water quality constituents across the Great Barrier Reef catchments? (ii) Are there groups of constituents with similar spatial behaviour? (iii) To what degree is the pattern in water quality associated with the catchment characteristics and what are they? (iv) What is the relative importance of anthropogenic controls and natural controls on water quality, and how these controls inform the management practices to improve water quality? The evaluation of the current conceptual understanding of catchment controls on water quality will further our understanding of spatial controls (e.g., catchment land use and hydrodynamic conditions) of water quality in the Great Barrier Reef catchments, so we can better manage our riverine water quality.
Section snippets
Study area
The Great Barrier Reef catchments are located in north-eastern Australia and encompass northern to southern coastal and inland Queensland. In total, the catchments have an area of 432,134 km2 and are divided into six Natural Resource Management (NRM) regions (Carroll et al., 2012; Waters et al., 2014) (Fig. 1). According to the Köppen-Geiger climate classification, the Great Barrier Reef catchment climates range from semi-arid tropical or thru warm oceanic to wet tropical (Fig. 2a) (Peel et
Cluster analysis
The cluster analyses of both the water quality and catchment characteristics suggested that the 32 sites can be grouped into two clusters (Fig. S-3a & b). There is good agreement between the two cluster analysis results (Fig. 3). Specifically, 8 out of the 32 sites are characterised as Cluster one in both analyses (blue round dots in Fig. 3), and 20 out of 32 sites are identified as Cluster two in both analyses (red triangles in Fig. 3). The clustering results differ for only 4 sites (blue
Spatial pattern in water quality responses
There are strong patterns in time-averaged water quality responses. Cluster analysis reveals that monitoring sites can be grouped based on similarity in their average water quality for each of the 9 constituents considered (Fig. 3, Fig. 4 and S-3a). Cluster one sites have lower average concentrations of all constituents except NOX (Fig. 4), with most of these sites are located in the northern region, where the converse is true for the Cluster two sites. This spatial pattern is evident when
Conclusions
This study applied multivariate statistical techniques to understand the spatial variability in stream water quality in the Great Barrier Reef catchments. We found that different catchment characteristics influenced the magnitude of concentration in varying ways in the Great Barrier Reef catchments. The influences of the key catchment characteristics depended on clusters of sites and their impacts differed for different constituents. Therefore, a comprehensive understanding of spatial
Acknowledgements
This study was supported by the Australian Research Council (LP140100495), the EPA Victoria, the Victorian Department of Environment, Land, Water and Planning, Bureau of Meteorology and Queensland Department of Natural Resources, Mines and Energy. The authors would like to acknowledge the efforts of the Queensland Department of Environment and Science who provided the water quality monitoring data. The author would also like to offer sincere gratitude to Ms. Jie Jian for her assistance in
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