Abstraction rate for the 2018-2019 period, with flow rates from 1 July 2018 to 19 January 2019,
from the Kahouri Stream (compliance limit red dashed line) 11
Figure 5 The irrigation areas, showing the cut and carry paddocks (green) and regular paddocks (blue)
(please note that the boundary lines are indicative only and may be subject to change) 12
page
iii
Figure 6 The volume of wastewater irrigated to land and discharged to water, compared with the
monthly rainfall totals 15
the garden of Lynn and Robin Bublitz, 27
Durham Avenue.
Bring your own food and a mug for lunch (tea
and coffee will be provided) + a bottle to finish
the day if you wish.(Glasses will be provided.)
page
page 3
R. ‘Gordon Collier’
Unnamed R. Vireya hybrid
R. arboreum This was grown from seed
collected by Ron Gordon.
R. protistum
The Weather
Weather always seems to be a talking
point. The high rainfall at Pukeiti,
usually over 4m per annum, when
relayed to
Executive Audit and Risk Agenda May 2023
Waitaha catchment consent monitoring report - Taranaki Regional Council.
Residual flow in race Retain a flow of at least 150 L/s, or a fish
salvage is to be undertaken
3371-Diversion of
water into race and
Lake Ratapiko
2 Maximum race water levels
Race water level:
Salisbury Rd: 205.20 m a.s.l
Mangaotea: 199.30 m a.s.l
Mangaotea Aqueduct: 199.25 m a.s.l
Lower Mangaotea: 199.15 m a.s.l
5 Recording of water levels and
rainfall
Water levels at the above sites to be
recorded, with the inclusion of rainfall at
the Mangaotea Aqueduct
‘Alert’ level for coastal waters (>140 cfu/100 ml). The 2014 E. coli counts for freshwater
Sites 1 and 2 were above the MfE ‘Alert’ level for freshwater (>260 cfu/100 ml).
The most likely explanation for the elevated counts is related to the high rainfall which
occurred prior to sampling. Under these circumstances, the sites can be influenced by
the Urenui River which drains from developed agricultural land. High counts recorded
at Site 1a, located upstream from the camp sewage
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25
Discussion 4.
The chemical composition of groundwater is determined by a number of influences.
These include the mineralogy of the soil and rock types forming catchments or
aquifers, aquifer structure, the source and volumes of recharge water, aquifer
residence times, overlying landuses and biochemical process.
Groundwater aquifers in Taranaki are predominantly recharged by rainfall falling on
the land surface, but recharge can also occur via infiltration from
STDC Kaponga, Manaia, Patea and Waverley WWTPs Monitoring Programme 2021-2022
meetings
and any points of interest be discussed in this item on the agenda. A template will be
issued prior to the next meeting. Members agreed that they will respond to these in future.
Item 10: Forthcoming Events (standing item)
Shared by Marcia that TRST have some events coming up that she is happy to share with
the minutes, but the main two are;
• They have four rural woman events coming up and one for migrant communities.
General Business
Shared that the region has a heavy rainfall