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River and stream water quality and ecology - Greater Wellington ...

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<strong>River</strong> <strong>and</strong> <strong>stream</strong> <strong>water</strong> <strong>quality</strong> <strong>and</strong> <strong>ecology</strong> in the <strong>Wellington</strong> region: State <strong>and</strong> trends<br />

Figure 5.11: Periphyton <strong>quality</strong> classes for each of the 46 RSoE sites with hard<br />

substrate suitable for periphyton growth. Classes were assigned to each site<br />

according to compliance with MfE (2000) guidelines, based on both monthly<br />

assessments of periphyton cover <strong>and</strong> annual assessments of periphyton<br />

biomass made between July 2008 <strong>and</strong> June 2011<br />

a high degree of <strong>stream</strong> shade resulted in low periphyton growth despite<br />

exposure to moderate to high nutrient concentrations.<br />

Although formal monitoring of macrophyte cover was not undertaken during<br />

the reporting period at the nine RSoE sites dominated by soft substrate,<br />

observations recorded during other monitoring suggest that nuisance<br />

macrophyte growth regularly occurs at four of these sites. Nuisance<br />

macrophyte growth also occurs at a number of hard-bottomed sites<br />

characterised by small substrate <strong>and</strong>/or long accrual periods.<br />

Significant increases in periphyton cover <strong>and</strong>/or biomass were detected at 19<br />

RSoE sites while a significant decreasing trend was detected at one site. The<br />

magnitude of increasing trends was considerable at some sites – including<br />

many sites classified as ‘poor’ – <strong>and</strong> in some cases may have resulted in<br />

significant degradation of river <strong>and</strong> <strong>stream</strong> values. The reasons for these<br />

increasing trends are unclear. At many sites, the increasing trends have likely<br />

been influenced by unusually high river flows <strong>and</strong> short accrual periods at the<br />

start of the analysis period (summers of 2004 <strong>and</strong> 2005) which resulted in very<br />

low periphyton growth in these years. Further, at some sites, decreasing<br />

summer-time river flows over the duration of the trend period may also have<br />

influenced the observed trends.<br />

PAGE 74 OF 160 WGN_DOCS-#1100598-V3

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