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Summer 2015-2016

Stream, were due principally to resident wild fowl populations in the vicinity of recreational usage sites (as confirmed by inspections and more recently by DNA marker surveys). In terms of E. coli, bacteriological water quality in the latest survey period was similar in comparison with historical surveys. The total number of samples falling within the “Alert” or “Action” categories (28% of samples) was equal to the long-term average and was strongly influenced by samples at two urban sites

Annual report 2016-2017

sampled on 3 May 2017 31 Table 7 Chemical analysis of the Puremu Stream, sampled on 23 May 2017 33 Table 8 Results of metal analysis undertaken on 3 May 2017 34 Table 9 Results of metal analysis undertaken on 23 May 2017 35 Table 10 Results of rain event monitoring – discharge and Puremu Stream samples, 23 August 2016 37 Table 11 Results of rain event monitoring - Manganaha Stream, 23 August 2016 38 Table 12 Biomonitoring sites in the Puremu and Manganaha Streams related to the

Policy Planning Committee Agenda August 2022

reflect that rainfall at the coast is richer in chloride and sodium, compared to rainfall that falls inland. Nearly two thirds of GQMP sites plot below the SWDL, suggesting that much of the region’s groundwater is enriched with sodium from rock/water interactions with sodium rich source rocks. 26. An analysis of nitrate concentrations over the entire GQMP network suggests that there has been little change in groundwater nitrate levels over the last five years. There is weak statistical

The Taranaki Region

climate, with abundant rainfall and high sunshine hours, makes the region lush, green and fertile. Rainfall Annual rainfall varies throughout the region. Some coastal areas receive less than 1,400 mm annually, while the summit of Mount Taranaki receives around 7,500 mm. Heavy rainfall events do occur and there can be extremes. In 2012 heavy rain caused a number of slips on the coastal road around Mount Taranaki, including a large slip at Oākura that covered the road, burying a

Annual report 2013-2014

groundwater bore was in poor condition. All activity still appeared to have ceased at the Derby Road North site. 10 February 2014 Inspection was conducted in conjunction with groundwater sampling:- • No material had been stored or spread via this site for some years. • The old cells and stormwater ponds were full of rain water. • No sheen was evident, but some odour was observed immediately downwind of the cells during groundwater sampling. • No other issues were noted.

Inglewood WWTP monitoring report 2018-2019

was no sign of recent overflow discharges into the Kurapete Stream. The WWTP and facilities were operating satisfactorily, with the pond perimeter tracks recently mown. No odours were noted onsite. 20 May 2019 An inspection was conducted in fine weather with light wind. Rainfall of 276 mm of rain was recorded at the Inglewood WWTP Council weather station in the month prior. The primary screen was operating and wastes were fully contained. The primary aeration pond was a turbid brown

Annual report 2014-2015

Urenui & Onaero motor camps consent monitoring report - Taranaki Regional Council.

Oaonui Water Supply Ltd Annual Report 2022-2023

stream gaugings. The monitoring indicated that the operation of the sluicing of the weir has improved, with flows not falling below 151 L/s. There was one unauthorised incident recording non-compliance in respect to the water take consent between 30 July and 5 August 2022. Due to a lightning strike which destroyed the scheme’s electronics, OWSL were required to take water in manual operation mode, which resulted in a breach of abstraction rate until OWSL could fine-tune the process. The