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 />
3. <strong>River</strong>s <strong>and</strong> <strong>stream</strong>s in the <strong>Wellington</strong> region<br />
This section presents a brief overview of the natural diversity of river <strong>and</strong><br />
<strong>stream</strong> types/environments in the <strong>Wellington</strong> region, providing context for<br />
some of the natural differences in <strong>water</strong> <strong>quality</strong> <strong>and</strong> ecological health observed<br />
across the region’s rivers <strong>and</strong> <strong>stream</strong>s. Although <strong>Greater</strong> <strong>Wellington</strong>’s RSoE<br />
network focuses on permanently flowing <strong>water</strong> bodies, both permanently <strong>and</strong><br />
intermittently flowing <strong>stream</strong>s are outlined. This is consistent with the RMA<br />
(1991) definition of a river or <strong>stream</strong> as “a continually or intermittently flowing<br />
body of fresh <strong>water</strong>” that includes <strong>stream</strong>s <strong>and</strong> modified <strong>water</strong>courses. Some of<br />
the key anthropogenic activities that can affect <strong>stream</strong> <strong>water</strong> <strong>quality</strong> <strong>and</strong><br />
ecological health are also outlined, with a particular focus on l<strong>and</strong> use <strong>and</strong><br />
significant consented activities in the <strong>Wellington</strong> region.<br />
3.1 Permanently flowing rivers <strong>and</strong> <strong>stream</strong>s<br />
There are approximately 12,360 km of permanently flowing rivers <strong>and</strong> <strong>stream</strong>s<br />
in the <strong>Wellington</strong> region. These rivers <strong>and</strong> <strong>stream</strong>s range from the small-sized<br />
first order <strong>stream</strong>s, found in head<strong>water</strong>s <strong>and</strong> springheads, through to the larger<br />
lower reaches of major rivers such as the Otaki, Hutt <strong>and</strong> Pahaoa rivers (sixth<br />
order) <strong>and</strong> the Ruamahanga <strong>River</strong> (seventh order). First <strong>and</strong> second order<br />
<strong>stream</strong>s make up approximately 75% of the entire length of rivers <strong>and</strong> <strong>stream</strong>s<br />
in the region while rivers belonging to orders 5, 6 <strong>and</strong> 7 make up only 5% of<br />
total river <strong>and</strong> <strong>stream</strong> length (Table 3.1).<br />
Table 3.1: Approximate lengths of rivers <strong>and</strong> <strong>stream</strong>s belonging to each order in<br />
the <strong>Wellington</strong> region. Data obtained from REC (Snelder et al. 2004)<br />
Order Approximate length (km) <strong>River</strong>/<strong>stream</strong> length in the region (%)<br />
1 6,037 49<br />
2 3,130 25<br />
3 1,575 13<br />
4 928 8<br />
5 427 3<br />
6 174 1<br />
7 89 1<br />
Total 12,360 100<br />
Differences in geophysical characteristics of river <strong>and</strong> <strong>stream</strong> catchments, such<br />
as climate, topography <strong>and</strong> geology, result in natural differences in river <strong>and</strong><br />
<strong>stream</strong> characteristics (Snelder at al. 2004), including differences in flow,<br />
slope, temperature <strong>and</strong> substrate. This, together with down<strong>stream</strong> factors, such<br />
as distance from the coast, affect the composition of biological communities<br />
including in<strong>stream</strong> plants, macroinvertebrates <strong>and</strong> fish (Leathwick et al. 2008).<br />
<strong>River</strong>s <strong>and</strong> <strong>stream</strong>s in the <strong>Wellington</strong> region can be broadly grouped into three<br />
types based on their catchment geophysical characteristics:<br />
Steep gradients <strong>and</strong> hard sedimentary geology (Figure 3.1a <strong>and</strong> 3.1b) – these<br />
rivers <strong>and</strong> <strong>stream</strong>s are found in the Tararua, Aorangi <strong>and</strong> Rimutaka ranges as<br />
well as in moderately elevated areas around the <strong>Wellington</strong> coast <strong>and</strong> eastern<br />
Wairarapa. They have naturally high <strong>water</strong> clarity <strong>and</strong> low concentrations of<br />
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