title: "Kia Mauri Tau!" Narratives of recovery from disabling mental health problems

authors: Lapsley, Hilary

subjects: Maori

abstract: A bicultural research team at the University of Waikato successfully applied for funding from the Health Research Council to do a qualitative research project in the area of ‘pathways to wellness’. The Mental Health Narratives Project set out to gather forty narratives of mental ill health, recovery and life after recovery by interviewing Maori and non-Maori women and men who once had a disabling mental health problem. We aimed to describe journeys to mental health, identify key themes in accounts of the recovery process and describe the impact of the experience of mental ill health on life after recovery.

text: "Kia Mauri Tau!" Narratives of recovery from disabling mental health problems A bicultural research team at the University of Waikato successfully applied for funding from the Health Research Council to do a qualitative research project in the area of ‘pathways to wellness’. The Mental Health Narratives Project set out to gather forty narratives of mental ill health, recovery and life after recovery by interviewing Maori and non-Maori women and men who once had a disabling mental health problem. We aimed to describe journeys to mental health, identify key themes in accounts of the recovery process and describe the impact of the experience of mental ill health on life after recovery.

year: 2002

title: Place imaginaries: Photography and place-making at Te Awa River Ride

authors: Hill, Rodrigo

subjects: photography

abstract: Contemporary photographic practice has evolved into a field of possibilities, which includes a flux of representational modes that depict experiences, feelings and emotions. This PhD with Creative Practice Components investigates how photography is embedded within ways of knowing, experiencing and making places and the subsequent visual constructions of place imaginaries.  Drawing on contemporary photographic practice and theory, I position myself as a qualitative researcher engaged in creative practice, specifically lens-based approaches and modes of photographic representation. In contrast to photography’s dominant discourse centred on indexical and objective assumptions, I understand photographic practices and images as constructions of multiple meanings.

I use Te Awa River Ride as my research locale, a place where different practices and discourses entangle, forming a diverse set of dynamic and intersecting meanings. Te Awa River Ride is a shared pathway, with a planned total length of 70 kilometres, that edges the banks of the Waikato River from Ngāruawāhia to Cambridge, in the central North Island of Aotearoa New Zealand. I understand Te Awa River Ride as a place-composite, layered by multiple place imaginaries, including indigenous Māori, Pākehā and European ways of meaning and place-making. In this thesis I draw upon place imaginaries as a way of expressing visual possibilities, constructions and affective responses to my own and others’ experiences at this unique research location. 

My photography practice aims to actualise particular place imaginaries through curation and sequencing of lens-based explorations of light, movement and water. This process and the compilation of imagery into curatorial products, such as photography installations, generate novel ways of perceiving the Waikato River and Te Awa River Ride, revealing the centrality of photography in place-making processes.

text: Place imaginaries: Photography and place-making at Te Awa River Ride Contemporary photographic practice has evolved into a field of possibilities, which includes a flux of representational modes that depict experiences, feelings and emotions. This PhD with Creative Practice Components investigates how photography is embedded within ways of knowing, experiencing and making places and the subsequent visual constructions of place imaginaries.  Drawing on contemporary photographic practice and theory, I position myself as a qualitative researcher engaged in creative practice, specifically lens-based approaches and modes of photographic representation. In contrast to photography’s dominant discourse centred on indexical and objective assumptions, I understand photographic practices and images as constructions of multiple meanings.

I use Te Awa River Ride as my research locale, a place where different practices and discourses entangle, forming a diverse set of dynamic and intersecting meanings. Te Awa River Ride is a shared pathway, with a planned total length of 70 kilometres, that edges the banks of the Waikato River from Ngāruawāhia to Cambridge, in the central North Island of Aotearoa New Zealand. I understand Te Awa River Ride as a place-composite, layered by multiple place imaginaries, including indigenous Māori, Pākehā and European ways of meaning and place-making. In this thesis I draw upon place imaginaries as a way of expressing visual possibilities, constructions and affective responses to my own and others’ experiences at this unique research location. 

My photography practice aims to actualise particular place imaginaries through curation and sequencing of lens-based explorations of light, movement and water. This process and the compilation of imagery into curatorial products, such as photography installations, generate novel ways of perceiving the Waikato River and Te Awa River Ride, revealing the centrality of photography in place-making processes.

year: 2019

title: Ecological monitoring of artificial destratification effects in Lake Rotoehu: 2014-2015

authors: Tempero, Grant Wayne

abstract: Lake Rotoehu is a shallow (mean depth 8 m), polymictic eutrophic lake in the Rotorua lakes district. Catchment land use intensification has contributed to a decline in water quality and persistent cyanobacterial algal blooms for the past 20 years and combines with a background of nutrient-rich geothermal inflows. Two artificial mixing devices were deployed in Lake Rotoehu in the spring of 2012 by the Bay of Plenty Regional Council with the aim of preventing lake thermal stratification. They were previously operated over the summer-autumn periods of 2012-13 and 2013-14 and their effects were monitored on a monthly basis until June 2014. The devices force compressed air through a diffuser near the lake bottom, and into three large vertical cylinders. Buoyancy, caused by the rising bubbles, draws water from the bottom of the lake up through the vertical cylinders and directs it horizontally into the surface mixed layer (epilimnion). This causes mixing of thermally distinct layers of the water column, and is designed to inhibit stratification and prevent hypolimnetic deoxygenation. Results from previous monitoring indicate that the mixing devices produced a limited, localised mixing effect, but had no influence on whole lake ecology. With a view to improving performance, modifications, including channelling all air through a single mixing device and increasing compressor output, were effected in preparation for the 2014-15 summer-autumn seasons. The University of Waikato was contracted by the Bay of Plenty Regional Council to conduct a monitoring programme to ascertain the effect of these modifications.
Three sites within Lake Rotoehu were sampled monthly at similar depths from October 2014 to May 2015. Sites 1 and 3 were located approximately 30 m from a mixing device and Site 2 acted as a control site as it was considered to be unaffected by the direct effects of the mixing. Zooplankton, phytoplankton and nutrient samples (total nitrogen, total phosphorus, nitrate, ammonium and dissolved phosphorus) were collected at two different depths (0.5 m and 9.0 m), at each site. In addition, CTD (conductivity, temperature, depth) vertical profiles were also taken at each site. Temperature data were also obtained from a fixed-sensor, high-frequency monitoring buoy deployed in the lake and used to determine lake stability.
The summer of 2014-15 produced conditions favourable for the formation of prolonged lake stratification. This resulted in a marked decline in water quality during January-May 2015 in comparison to the previous three years of monitoring data. Evidence of localised homogenisation by the mixing device of the dominant phytoplankton and zooplankton taxonomic groups demonstrated notable improvement in mixing device performance. Temperature profile data were more equivocal, with no clear observations of the effects of artificial mixing over an extended area of the lake. However, supplemental profiles taken from within the discharge plumes (approximately 30 m from the mixing device) demonstrated evidence of hypolimnetic water being discharged to the epilimnion.
It is concluded that the current design and configuration of the artificial mixing devices is effective in drawing water from the hypolimnion into the epilimnion. However, it appears that the thermal mass of Lake Rotoehu is too large for a single mixing device to overcome and there appears to be no substantial ecological benefit in continuing to operate the devices without substantial modification. If significant, sustained improvements in water quality are to be achieved using these devices, further capital investment will be required. Further research investigating the efficiency and area of influence of the mixing devices may help to improve their design and operation.

text: Ecological monitoring of artificial destratification effects in Lake Rotoehu: 2014-2015 Lake Rotoehu is a shallow (mean depth 8 m), polymictic eutrophic lake in the Rotorua lakes district. Catchment land use intensification has contributed to a decline in water quality and persistent cyanobacterial algal blooms for the past 20 years and combines with a background of nutrient-rich geothermal inflows. Two artificial mixing devices were deployed in Lake Rotoehu in the spring of 2012 by the Bay of Plenty Regional Council with the aim of preventing lake thermal stratification. They were previously operated over the summer-autumn periods of 2012-13 and 2013-14 and their effects were monitored on a monthly basis until June 2014. The devices force compressed air through a diffuser near the lake bottom, and into three large vertical cylinders. Buoyancy, caused by the rising bubbles, draws water from the bottom of the lake up through the vertical cylinders and directs it horizontally into the surface mixed layer (epilimnion). This causes mixing of thermally distinct layers of the water column, and is designed to inhibit stratification and prevent hypolimnetic deoxygenation. Results from previous monitoring indicate that the mixing devices produced a limited, localised mixing effect, but had no influence on whole lake ecology. With a view to improving performance, modifications, including channelling all air through a single mixing device and increasing compressor output, were effected in preparation for the 2014-15 summer-autumn seasons. The University of Waikato was contracted by the Bay of Plenty Regional Council to conduct a monitoring programme to ascertain the effect of these modifications.
Three sites within Lake Rotoehu were sampled monthly at similar depths from October 2014 to May 2015. Sites 1 and 3 were located approximately 30 m from a mixing device and Site 2 acted as a control site as it was considered to be unaffected by the direct effects of the mixing. Zooplankton, phytoplankton and nutrient samples (total nitrogen, total phosphorus, nitrate, ammonium and dissolved phosphorus) were collected at two different depths (0.5 m and 9.0 m), at each site. In addition, CTD (conductivity, temperature, depth) vertical profiles were also taken at each site. Temperature data were also obtained from a fixed-sensor, high-frequency monitoring buoy deployed in the lake and used to determine lake stability.
The summer of 2014-15 produced conditions favourable for the formation of prolonged lake stratification. This resulted in a marked decline in water quality during January-May 2015 in comparison to the previous three years of monitoring data. Evidence of localised homogenisation by the mixing device of the dominant phytoplankton and zooplankton taxonomic groups demonstrated notable improvement in mixing device performance. Temperature profile data were more equivocal, with no clear observations of the effects of artificial mixing over an extended area of the lake. However, supplemental profiles taken from within the discharge plumes (approximately 30 m from the mixing device) demonstrated evidence of hypolimnetic water being discharged to the epilimnion.
It is concluded that the current design and configuration of the artificial mixing devices is effective in drawing water from the hypolimnion into the epilimnion. However, it appears that the thermal mass of Lake Rotoehu is too large for a single mixing device to overcome and there appears to be no substantial ecological benefit in continuing to operate the devices without substantial modification. If significant, sustained improvements in water quality are to be achieved using these devices, further capital investment will be required. Further research investigating the efficiency and area of influence of the mixing devices may help to improve their design and operation.

year: 2015