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