Annual report 2016-2017
Tawhiti Catchment consent monitoring report 2016-2017.
Tawhiti Catchment consent monitoring report 2016-2017.
pH pH 6.7 6.5 6.4 6.4 6.5 - 8.5 Suspended solids g/m3 28 4 30 5 100 Turbidity NTU 16 - 4.8 - - page 15 2.1.3 Results of consent holder monitoring 2.1.3.1 Stormwater monitoring by SENZL SENZL monitors the combined stormwater discharge from the site, with sampling triggered by rainfall events. Table 3 shows the results obtained during the 2015-2016 monitoring year. Hydrocarbons, suspended solids and chloride levels were all below the limits set by consents
sampled, it was clear and slightly turbid with slight foaming visible in the stream. No sheen or odour was apparent. 18 March 2016 A total of 65.5 mm rainfall had been recorded in the previous week at NPWWTP, 58 mm of which fell during the day prior to the inspection. This had rapidly filled the site's stormwater ponds. While the water was being tested by DAS on the afternoon of the 17th March, permission was sought and given by the Council to allow the ponds to overflow to the
Greymouth Petroleum Kaimiro production station consent monitoring report - Taranaki Regional Council.
Trustpower Mangorei hydro scheme consent monitoring report - Taranaki Regional Council.
incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The Taranaki Region page 16 2017/2018 Annual Report 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
are few areas of sheltered water beyond the major estuaries such as the Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The
Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The Taranaki Region page 18 2016/2017 Annual Report THE PEOPLE
Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense 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
NPDC Colson Road Landfil consent monitoring report 2016-2017. l