Table 3 Summary of abstraction rate data for 2020-2021 11
Table 4 Limits for stormwater composition for each parameter (consents 3902, 3907, 4133) 16
Table 5 Sample results for the stormwater discharge to an unnamed tributary of the Tawhiti Stream 17
Table 6 Sample results for the stormwater discharge to an unnamed tributary of the Tangahoe River 18
Table 7 Sample results for the stormwater discharge to an unnamed coastal stream 19
Table 8 Summary of wastewater volume data for
an emerging ‘Great
Walk’ set to boost the region’s burgeoning reputation as a visitor destination.
The Council is also confident about its plans to build on recent gains in freshwater quality; to develop its
education programme; and to broaden and deepen its relationship with iwi and hapū.
Financially, the impact of our proposals is relatively minor. The Council is proposing an increase of 3.5 percent in
its general rates take for 2018/2019. In the last three years, the average
around the weir, one on the left abutment, and one on the right. The required minimum
compensatory flow is 400L/s.
page
Motukawa Race – Hydraulic and Geotechnical Assessment – Motukawa Hydro-Electric Power Scheme
RILEY Ref: 18MTK/ENH-C Page 7
25 November 2021
Riley Consultants Ltd
The current maximum consented take from the Manganui River into the race is 5.2m3/s. The
rate at which flow is abstracted from the river is controlled by two vertical gates at the intake
www.vote.nz
Ratepayer Roll: If a person is on the parliamentary roll in one area and
pays rates on a property in another area, this person may be eligible
to be enrolled on the non-resident ratepayer roll. A firm, company,
corporation or society paying rates on a property may nominate
one of its members or officers as a ratepayer elector (provided
the nominated person resides outside the area). Ratepayer Roll
enrolment forms are available from respective territorial authority
websites, or by
Walk’ set to boost the region’s burgeoning reputation as a visitor destination.
The Council is also confident about its plans to build on recent gains in freshwater quality; to develop its
education programme; and to broaden and deepen its relationship with iwi and hapū.
Financially, the impact of our proposals is relatively minor. There is an increase of 4.5 percent in the general
rates take for 2018/2019. In the last three years, the average general rates increase has been 0.97%. Over
emerging ‘Great
Walk’ set to boost the region’s burgeoning reputation as a visitor destination.
The Council is also confident about its plans to build on recent gains in freshwater quality; to develop its
education programme; and to broaden and deepen its relationship with iwi and hapū.
Financially, the impact of our proposals is relatively minor. The Council is proposing an increase of 3.5 percent in
its general rates take for 2018/2019. In the last three years, the average general rates
average. Base diagram source: IPCC.
Temperatures measured at climate stations across the
region show marked increases in air, water and soil
temperature, particularly over the past decade. Changes
in river water temperature are more subtle, while air and
soil temperatures have risen sharply, with soil temperature
increasing at a rate of around 1.4°C per decade. Changes
over 10 to 15 year periods are affected by long-term climate
trends as well as changes due to shorter
environmental performance
Besides discussing the various details of the performance and extent of compliance by the consent holders,
this report also assigns a rating as to each Company’s environmental and administrative performance during
the period under review. The rating categories are high, good, improvement required and poor for both
environmental and administrative performance. The interpretations for these ratings are found in
Appendix II.
For reference, in the 2021-2022 year, consent
studies undertaken in the late 1980s by
the Taranaki Catchment Commission showed that the entire Taranaki coastline is eroding at
long term average rates between 0.05 m/year and 1.89 m/year with exceptions at the Patea
and Stony (Hangatahua) river mouths where the coast was accreting. Erosion rates differ at
different locations, primarily due to differences around the coast in geology, coastal
orientation, proximity to river mouths and matters such as dune management.
Recalculating erosion
but not be limited to (tick all that apply): AEE Page Number Section
☐ The rate of discharge and hydrological effects
☐ Ecosystem health and potential disturbance
☐ Indigenous biodiversity
☐ Hydrological functioning
page
01/23 - Doc # 3095941 Page 6 of 17
☐ Cultural values
☐ Amenity
☐ Source control
☐ Treatment
☐ Site sediment and