Your search for 'River flow' returned 2604 results.

Summer 2014-2015

probably the main contributing factor to the high cyanobacteria levels. Exposed mats were caused by falling water levels during this long dry summer and/or the result of daily fluctuations in river flow caused by periodic releases of hydro scheme waters. Significant detaching or detached mats were often coincident with high levels of cyanobacteria present in the river. As a consequence of the presence of exposed and/or detaching mats, signage was erected at three sites advising recreational river

Annual report 2013-2014

trunk sewer. This chamber provided for splitting of the raw sewage influent to flow into either, or both ponds, but this provision was only intended for utilisation when excessive stormwater infiltration may have caused an overflow directly to the second pond. The final outfall (from the second pond) was to the Patea River. However, the connection between the two ponds and the outlet to the river were originally positioned directly opposite each other, thereby having the potential to

Summer 2010-2011

vi Figure 5 E. coli numbers for Lake Rotomanu for the 20 sample extended survey 12 Figure 6 River flow in the Waiwhakaiho River during the survey period (NOTE: Waiwhakaiho at Egmont Village Flow is unaudited data) 15 Figure 7 E. coli numbers for the Waiwhakaiho River at Merrilands Domain during the regular survey season 16 Figure 8 Box and whisker plots for all summer SEM surveys of E.coli bacteria numbers in the Waiwhakaiho River at Merrilands Domain 17 Figure 9

Fonterra Whareroa consent monitoring 2019-2020

Stream is less than 800 L/s, the rate of taking from the Tawhiti Stream shall not exceed 184 L/s, unless the turbidity of the Tangahoe River at the take site is greater than 850 NTU, and then the rate shall not exceed 347 L/s. In 2019-2020, the Tawhiti abstraction rate did not exceed 184 L/s at any time that the stream flow rate was less than 800 L/s. The maximum abstraction rate that occurred when the stream flow was below 800 L/s, was 171.7 L/s. The actual stream flow at this time was 795 …

Summer 2013-2014

6 Figure 2 E. coli numbers for Lake Rotomanu during the regular season 11 Figure 3 Box and whisker plots for all summer SEM surveys of E. coli bacteria numbers at Lake Rotomanu 13 page viii Figure 4 LOWESS trend plot of median E. coli numbers (per 100ml) at Lake Rotomanu for the 1996-2014 period 13 Figure 5 E. coli numbers for Lake Rotomanu for the 20 sample extended survey 14 Figure 6 River flow in the Waiwhakaiho River during the survey period 17

Form 300: Take and use surface water - general

scientific and amenity values  Ecology (e.g. river and lake habitat, vegetation, fish and fisheries, wildlife)  River flow _________________________________________________________________________________ _________________________________________________________________________________ _________________________________________________________________________________ _________________________________________________________________________________

Submission: Murray Dobbin

power generation. My application relates to the application to allow only 180 litres of water per second to flow into the river system below the weir (dam) located near S.H.45. Having observed the lower 2km of the Waiaua river for over 60 years from times of no residual flow, the 100 litres flow, the 180 litres of flow and since June 2018 of the full flow. This stretch of the river system now appears to be an alive, vibrant and fully functioning river. From these observations I would conclude that

Appendix 10H: Te Atiawa

reinforce Te Atiawa tribal identity. Papamoa (being Meeting of the Waters Scenic Reserve) (as shown on deed plan OTS-043-15) Papamoa is located on the banks of the Waiwakaiho River in the rohe of Ngati Te Whiti. The site is above a river bend which was later named the meeting of the waters because of the turbulent river flow at that point. The site was named Papamoa because the land around which it was located was as soft as a garden bed. Papamoa was also a nohoanga, a

Annual report 2013-2014

downstream of the oxidation ponds, and of the effluent from the oxidation ponds during late autumn under relatively low river flow conditions. This survey was delayed due to no discharge from the system under very dry late summer- autumn conditions. The sampling sites are shown in Figure 2 (Section 3) of this report. The samples were analysed for temperature, pH, conductivity, chloride, dissolved oxygen, total and filtered uninhibited biochemical oxygen demand, turbidity, suspended solids, dissolved

Assessment of environmental effects

concentration measured downstream compared to that upstream of the plant’s discharge (24% increase in faecal coliform concentration). The downstream concentrations are still well within the National Objective Framework bottom line value of 1,000 cfu/100mL. Visual Appearance There is some discolouration in the Patea River beyond the permitted mixing zone (50 m) of the plant’s discharge. This is most likely a result of the potential algae solids in the discharge and low flow conditions.