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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25th percentile summer time flow m 3 /s<br />
25th percentile summer time flow m 3 /s<br />
14<br />
12<br />
10<br />
8<br />
6<br />
4<br />
2<br />
35<br />
30<br />
25<br />
20<br />
15<br />
10<br />
5<br />
2003/04 2004/05 2005/06 2006/07 2007/08 2008/09 2009/10 2010/11<br />
<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 />
Otaki <strong>River</strong> at Pukehinau<br />
Hutt <strong>River</strong> at Birchville<br />
Hutt <strong>River</strong> at Taita Gorge<br />
Waiohine <strong>River</strong> at Gorge<br />
Ruamahanga <strong>River</strong> at Waihenga<br />
2003/04 2004/05 2005/06 2006/07 2007/08 2008/09 2009/10 2010/11<br />
2003/04 2004/05 2005/06 2006/07 2007/08 2008/09 2009/10 2010/11<br />
WGN_DOCS-#1100598-V3 PAGE 73 OF 160<br />
25th percentile summer time flow m 3 /s<br />
25th percentile summer time flow m 3 /s<br />
0.35<br />
0.30<br />
0.25<br />
0.20<br />
0.15<br />
0.10<br />
0.05<br />
0.00<br />
0.12<br />
0.10<br />
0.08<br />
0.06<br />
0.04<br />
0.02<br />
0.00<br />
Pauatahanui Stream at Gorge<br />
Porirua Stream at Town Centre<br />
Waiwhetu Stream at Whites Line East<br />
Whangaehu <strong>River</strong> at Waihi<br />
Ruakokoputuna <strong>River</strong> at Iraia<br />
2003/04 2004/05 2005/06 2006/07 2007/08 2008/09 2009/10 2010/11<br />
Figure 5.10: 25 th percentile summer-time (November–April) flows between 2003/04<br />
<strong>and</strong> 2010/11 at ten flow monitoring sites across the <strong>Wellington</strong> region. Data from<br />
the Whangaehu <strong>and</strong> Ruakokoputuna river sites provided courtesy of NIWA<br />
5.3 Synthesis<br />
Both periphyton cover <strong>and</strong> biomass were lowest at RSoE sites with catchments<br />
dominated by forested areas of the Tararua, Rimutaka <strong>and</strong> Aorangi ranges.<br />
These sites rarely exceeded the MfE (2000) guidelines for protection of<br />
in<strong>stream</strong> values <strong>and</strong>, along with two highly shaded sites on <strong>stream</strong>s with<br />
pastoral catchments, were assigned an overall periphyton class of ‘excellent’<br />
(Figure 5.11).<br />
Periphyton growth was greatest at urban sites in <strong>Wellington</strong> <strong>and</strong> Porirua, as<br />
well as at pastoral sites in central <strong>and</strong> eastern Wairarapa (Figure 5.11). These<br />
sites frequently exceeded guidelines for protection of recreational, aquatic<br />
biodiversity <strong>and</strong> trout fishery/spawning values <strong>and</strong> were classed as ‘poor’.<br />
Several of these sites, including Taueru <strong>River</strong> at Gladstone, Kopuaranga <strong>River</strong><br />
at Stewarts, Mangatarere Stream at SH 2 <strong>and</strong> Huangarua <strong>River</strong> at Ponatahi<br />
Bridge, are listed in <strong>Greater</strong> <strong>Wellington</strong>’s existing Regional Fresh<strong>water</strong> Plan<br />
(WRC 1999) as supporting important trout habitat.<br />
Environmental variables that exhibited the strongest correlations with<br />
periphyton biomass <strong>and</strong>/or cover were nutrient concentrations <strong>and</strong> <strong>water</strong><br />
temperature. Many RSoE sites classified as having ‘poor’ compliance with the<br />
MfE (2000) periphyton guidelines recorded very high median concentrations of<br />
TN <strong>and</strong>/or TP, <strong>and</strong> high <strong>water</strong> temperatures. Some sites, such as those in<br />
eastern Wairarapa, recorded only low to moderate nutrient concentrations but<br />
high <strong>water</strong> temperatures. <strong>River</strong>s <strong>and</strong> <strong>stream</strong>s in these areas are subject to<br />
periods of extended low flow during summer <strong>and</strong> can support high periphyton<br />
biomass despite relatively low nutrient concentrations. Conversely, at two sites