rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. THE PEOPLE Figures from the 2013 census show the total population of Taranaki stands at 109,608, an increase of 5.3% over the 2006 census figure. In the previous census period (2001-2006) the population of the region increased by 1.2%. Taranaki’s population accounts for 2.6% of New Zealand’s total population. Population changes have also varied
sulphide (H2S) was detected but the source could not be located. No odours were detected at the downwind boundary of the site. The cap on the closed areas of the landfill (stages 1 & 2) was in good condition and no issues were noted. The following action was to be undertaken: Continue with litter collection 8 September 2015 This site inspection was carried out in dry weather with light, variable wind conditions. There had been only 2.5 mm of rainfall within the previous two days.
Taranaki By-Products Ltd consent monitoring report - Taranaki Regional Council.
monitoring by OMV OMV monitors the combined stormwater discharge from the site, with sampling triggered by rainfall events. Table 3 shows the results obtained during the 2021-2022 monitoring year. There was no discharge at the time of scheduled sampling during April 2022. In all samples pH, hydrocarbons, and suspended solids levels were all within/below the limits set by consents 5997-1, 6269-1 and 10933-1, and were indicative of a consistently clean discharge. OMV initiated daily stormwater
National Survey of Pesticides and Emerging Organic Contaminants (EOCs) in Groundwater 2018 - ESR
Stream. Overflow due to rainfall entering this pond is discharged to land and to the Ngaere Stream to the north of the pond. Stormwater from the process areas is directed to a large separator system to the north east of the site. The effluent from this separator is discharged to a small unnamed tributary to the east which joins the Ngaere Stream approximately 40 metres above its confluence with the Patea River. 1 The Council has used
consents (7670- 1, 7884-1) being exercised, there were areas of pine which have been subsequently removed and processed. Average annual rainfall for the site is 1,383 mm (taken from nearby Motunui monitoring station). There are no significant surface water bodies located in the immediate vicinity of the areas that are landfarmed, other than small farm drains. Previous land use at the Wellington section of the landfarm has been a mixture of agriculture and small scale forestry. Further inland
Proposed Coastal Plan Schedule 5B - Sites of significance to Māori and associated values.
Average annual rainfall for the site is 1,043 mm (taken from the nearby Patea monitoring station). As with the other South Taranaki coastal sites, the Vanner site is subject to strong winds predominantly from the N-NW at average speeds of 10-20 knots (taken from Hawera automated weather station). The Mangaroa Stream runs through the northern extent of the site separating the stockpiling facilities and some of the available spreading area from the main spreading area at the southern end of
marginal coastal land situated on reworked dune fields. The predominant soil type has been identified as black loamy sand, and vegetation growth is primarily a mixture of pasture and dune grasses. Average annual rainfall for the site is 1,122 mm (taken from the nearby Glenn Road monitoring station). Two significant surface water bodies run adjacent to the spreading areas. The Waimate Stream flanks the north-western side of the main western site, whilst the Rawa Stream runs adjacent to the