title: Theorising teaching

authors: Bell, Beverley

subjects: theorising

abstract: Theorising of teaching is not limited to the major theorists, as researchers and teachers also theorise teaching. This article explores theorising by researchers and a teacher in two ways: firstly, an overview or framework from the research literature on teaching as a sociocultural practice is developed, and secondly, the framework is tested by analysing the transcripts of a beginning teacher talking about her teaching.

text: Theorising teaching Theorising of teaching is not limited to the major theorists, as researchers and teachers also theorise teaching. This article explores theorising by researchers and a teacher in two ways: firstly, an overview or framework from the research literature on teaching as a sociocultural practice is developed, and secondly, the framework is tested by analysing the transcripts of a beginning teacher talking about her teaching.

year: 2010

title: The presence, speciation, and movement of arsenic in Lake Tarawera

authors: Cochrane, Kirstie-Lee May Nicole

subjects: Arsenic, Lake Tarawera, rhizons

abstract: Arsenic is a naturally occurring element with potential toxicity to humans depending on concentration and chemical state. Contamination of freshwater environments by arsenic has been seen globally, occurring through both natural and anthropogenic sources. This thesis explores the presence, speciation, and movement of arsenic within Lake Tarawera, including the related physical and biogeochemical processes that control the movement and state of arsenic within the water body and from inlet sources. 
Lake Tarawera, in the Bay of Plenty Region, North Island, New Zealand is a large deep-water lake in an active volcanic region. Field measurements taken from Lake Tarawera were targeted towards a known localised geothermal area to explore spatial heterogeneity. The results show how the monomictic cycling regime of Lake Tarawera contributes to the retention of arsenic in the water column through increasing concentrations of benthic arsenic during the period of stratification across five open-water sites (196% difference between surface and benthic water As concentrations in March 2020), and homogenous distribution through winter overturning (10% maximum difference in As concentrations, statistically insignificant). The physical and chemical conditions of the lake (temperature and pH) and high solubility of arsenic retain dissolved species in the water column. Oxygen depletion is observed in the deepest part of the lake (2.3 mg L⁻¹ at 79 m depth) which corresponds with increased benthic arsenic concentrations (126 µg L⁻¹).  
Inlets in the southern arm of the lake (Wairua Arm) are higher sources of arsenic into the water body than inlets in the main body of the lake, with arsenic concentrations from all sampled Wairua Arm inlets exceeding the World Heath Organisation 10 µg L⁻¹ drinking water standard; dissolved concentrations ranging from 41.0-947 µg L⁻¹. One high volume waterfall (Rotomahana WateArsenic is a naturally occurring element with potential toxicity to humans depending on concentration and chemical state. Contamination of freshwater environments by arsenic has been seen globally, occurring through both natural and anthropogenic sources. This thesis explores the presence, speciation, and movement of arsenic within Lake Tarawera, including the related physical and biogeochemical processes that control the movement and state of arsenic within the water body and from inlet sources.  Lake Tarawera, in the Bay of Plenty Region, North Island, New Zealand is a large deep-water lake in an active volcanic region. Field measurements taken from Lake Tarawera were targeted towards a known localised geothermal area to explore spatial heterogeneity. The results show how the monomictic cycling regime of Lake Tarawera contributes to the retention of arsenic in the water column through increasing concentrations of benthic arsenic during the period of stratification across five open-water sites (196% difference between surface and benthic water As concentrations in March 2020), and homogenous distribution through winter overturning (10% maximum difference in As concentrations, statistically insignificant). The physical and chemical conditions of the lake (temperature and pH) and high solubility of arsenic retain dissolved species in the water column. Oxygen depletion is observed in the deepest part of the lake (2.3 mg L⁻¹ at 79 m depth) which corresponds with increased benthic arsenic concentrations (126 µg L⁻¹).  Inlets in the southern arm of the lake (Wairua Arm) are higher sources of arsenic into the water body than inlets in the main body of the lake, with arsenic concentrations from all sampled Wairua Arm inlets exceeding the World Heath Organisation 10 µg L⁻¹ drinking water standard; dissolved concentrations ranging from 41.0-947 µg L⁻¹. One high volume waterfall (Rotomahana Waterfall) provides a per second arsenic loading of 16,400 ± 2,660 µg As s⁻¹. The more toxic form of arsenic (AsIII) was only detected in one instance, from a warm water stream inlet. Iron and manganese concentrations and the partitioning of these transition metals indicates the ratio of arsenic to these binding elements is not of the right order of  magnitude to remove substantial arsenic from the water column, as dissolved arsenic concentrations exceed that of both iron and manganese. 
Water isotope ratios and dissolved arsenic concentrations from Rotomahana Waterfall show a complicated mixing regime, including influences such as wind, rainfall, other inlets, and opposing water flows coming from the main water and the high flow waterfall. High temperature and low flow waters from Hot Water Beach demonstrates the influence of inlet water temperature because they alter the movement and concentrations of arsenic heading out towards the open-water inlets. The high temperature of Hot Water Beach creates a localised area of thermal stratification, which causes surface mixing and dilution of the inlet waters with the nearest open-water site. Mixing then occurs with depth closer to the open-water site, passed the point of the hot water induced thermocline. These targeted samples highlight how well arsenic is diluted and buffered by such a large volume of water, and demonstrate the importance of stratification, temperature, and flow rate on the movement of As.  
Laboratory and field studies attempted to minimise oxygen introduction to pore water samples using rhizons (pore water filters) and vacutainers. Arsenic speciation was retained in field samples in the vacutainers for up to three months, with concentrations of up to 2,230 µg L-1 of AsIII measured; this result which led to laboratory experiments on the long-term storage and retention of AsIII. However, the data from these laboratory studies were inconclusive for over-time analyses of two experiments; days 2, 26, and 55 after sample spiking for the first experiment, and days 2 and 29 for the second experiment. Vacutainers and rhizons extracted pore waters in-situ in attempt to minimise oxygen introduction to low dissolved oxygen samples; however, the methodology for long-term storage requires further research.  
Speciation of arsenic occurs in the sediments due to the highly anoxic environment, with pore water AsIII concentrations ranging exceeding 2,000 µg L⁻¹ in the surface sediments and decreasing with depth. Sediment concentrations show distinct accumulation boundaries which are indicative of redox boundaries over time. rfall) provides a per second arsenic loading of 16,400 ± 2,660 µg As s⁻¹. The more toxic form of arsenic (AsIII) was only detected in one instance, from a warm water stream inlet. Iron and manganese concentrations and the partitioning of these transition metals indicates the ratio of arsenic to these binding elements is not of the right order of  magnitude to remove substantial arsenic from the water column, as dissolved arsenic concentrations exceed that of both iron and manganese. Water isotope ratios and dissolved arsenic concentrations from Rotomahana Waterfall show a complicated mixing regime, including influences such as wind, rainfall, other inlets, and opposing water flows coming from the main water and the high flow waterfall. High temperature and low flow waters from Hot Water Beach demonstrates the influence of inlet water temperature because they alter the movement and concentrations of arsenic heading out towards the open-water inlets. The high temperature of Hot Water Beach creates a localised area of thermal stratification, which causes surface mixing and dilution of the inlet waters with the nearest open-water site. Mixing then occurs with depth closer to the open-water site, passed the point of the hot water induced thermocline. These targeted samples highlight how well arsenic is diluted and buffered by such a large volume of water, and demonstrate the importance of stratification, temperature, and flow rate on the movement of As.  Laboratory and field studies attempted to minimise oxygen introduction to pore water samples using rhizons (pore water filters) and vacutainers. Arsenic speciation was retained in field samples in the vacutainers for up to three months, with concentrations of up to 2,230 µg L⁻¹ of AsIII measured; this result which led to laboratory experiments on the long-term storage and retention of AsIII. However, the data from these laboratory studies were inconclusive for over-time analyses of two experiments; days 2, 26, and 55 after sample spiking for the first experiment, and days 2 and 29 for the second experiment. Vacutainers and rhizons extracted pore waters in-situ in attempt to minimise oxygen introduction to low dissolved oxygen samples; however, the methodology for long-term storage requires further research.  Speciation of arsenic occurs in the sediments due to the highly anoxic environment, with pore water AsIII concentrations ranging exceeding 2,000 µg L⁻¹ in the surface sediments and decreasing with depth. Sediment concentrations show distinct accumulation boundaries which are indicative of redox boundaries over time.

text: The presence, speciation, and movement of arsenic in Lake Tarawera Arsenic is a naturally occurring element with potential toxicity to humans depending on concentration and chemical state. Contamination of freshwater environments by arsenic has been seen globally, occurring through both natural and anthropogenic sources. This thesis explores the presence, speciation, and movement of arsenic within Lake Tarawera, including the related physical and biogeochemical processes that control the movement and state of arsenic within the water body and from inlet sources. 
Lake Tarawera, in the Bay of Plenty Region, North Island, New Zealand is a large deep-water lake in an active volcanic region. Field measurements taken from Lake Tarawera were targeted towards a known localised geothermal area to explore spatial heterogeneity. The results show how the monomictic cycling regime of Lake Tarawera contributes to the retention of arsenic in the water column through increasing concentrations of benthic arsenic during the period of stratification across five open-water sites (196% difference between surface and benthic water As concentrations in March 2020), and homogenous distribution through winter overturning (10% maximum difference in As concentrations, statistically insignificant). The physical and chemical conditions of the lake (temperature and pH) and high solubility of arsenic retain dissolved species in the water column. Oxygen depletion is observed in the deepest part of the lake (2.3 mg L⁻¹ at 79 m depth) which corresponds with increased benthic arsenic concentrations (126 µg L⁻¹).  
Inlets in the southern arm of the lake (Wairua Arm) are higher sources of arsenic into the water body than inlets in the main body of the lake, with arsenic concentrations from all sampled Wairua Arm inlets exceeding the World Heath Organisation 10 µg L⁻¹ drinking water standard; dissolved concentrations ranging from 41.0-947 µg L⁻¹. One high volume waterfall (Rotomahana WateArsenic is a naturally occurring element with potential toxicity to humans depending on concentration and chemical state. Contamination of freshwater environments by arsenic has been seen globally, occurring through both natural and anthropogenic sources. This thesis explores the presence, speciation, and movement of arsenic within Lake Tarawera, including the related physical and biogeochemical processes that control the movement and state of arsenic within the water body and from inlet sources.  Lake Tarawera, in the Bay of Plenty Region, North Island, New Zealand is a large deep-water lake in an active volcanic region. Field measurements taken from Lake Tarawera were targeted towards a known localised geothermal area to explore spatial heterogeneity. The results show how the monomictic cycling regime of Lake Tarawera contributes to the retention of arsenic in the water column through increasing concentrations of benthic arsenic during the period of stratification across five open-water sites (196% difference between surface and benthic water As concentrations in March 2020), and homogenous distribution through winter overturning (10% maximum difference in As concentrations, statistically insignificant). The physical and chemical conditions of the lake (temperature and pH) and high solubility of arsenic retain dissolved species in the water column. Oxygen depletion is observed in the deepest part of the lake (2.3 mg L⁻¹ at 79 m depth) which corresponds with increased benthic arsenic concentrations (126 µg L⁻¹).  Inlets in the southern arm of the lake (Wairua Arm) are higher sources of arsenic into the water body than inlets in the main body of the lake, with arsenic concentrations from all sampled Wairua Arm inlets exceeding the World Heath Organisation 10 µg L⁻¹ drinking water standard; dissolved concentrations ranging from 41.0-947 µg L⁻¹. One high volume waterfall (Rotomahana Waterfall) provides a per second arsenic loading of 16,400 ± 2,660 µg As s⁻¹. The more toxic form of arsenic (AsIII) was only detected in one instance, from a warm water stream inlet. Iron and manganese concentrations and the partitioning of these transition metals indicates the ratio of arsenic to these binding elements is not of the right order of  magnitude to remove substantial arsenic from the water column, as dissolved arsenic concentrations exceed that of both iron and manganese. 
Water isotope ratios and dissolved arsenic concentrations from Rotomahana Waterfall show a complicated mixing regime, including influences such as wind, rainfall, other inlets, and opposing water flows coming from the main water and the high flow waterfall. High temperature and low flow waters from Hot Water Beach demonstrates the influence of inlet water temperature because they alter the movement and concentrations of arsenic heading out towards the open-water inlets. The high temperature of Hot Water Beach creates a localised area of thermal stratification, which causes surface mixing and dilution of the inlet waters with the nearest open-water site. Mixing then occurs with depth closer to the open-water site, passed the point of the hot water induced thermocline. These targeted samples highlight how well arsenic is diluted and buffered by such a large volume of water, and demonstrate the importance of stratification, temperature, and flow rate on the movement of As.  
Laboratory and field studies attempted to minimise oxygen introduction to pore water samples using rhizons (pore water filters) and vacutainers. Arsenic speciation was retained in field samples in the vacutainers for up to three months, with concentrations of up to 2,230 µg L-1 of AsIII measured; this result which led to laboratory experiments on the long-term storage and retention of AsIII. However, the data from these laboratory studies were inconclusive for over-time analyses of two experiments; days 2, 26, and 55 after sample spiking for the first experiment, and days 2 and 29 for the second experiment. Vacutainers and rhizons extracted pore waters in-situ in attempt to minimise oxygen introduction to low dissolved oxygen samples; however, the methodology for long-term storage requires further research.  
Speciation of arsenic occurs in the sediments due to the highly anoxic environment, with pore water AsIII concentrations ranging exceeding 2,000 µg L⁻¹ in the surface sediments and decreasing with depth. Sediment concentrations show distinct accumulation boundaries which are indicative of redox boundaries over time. rfall) provides a per second arsenic loading of 16,400 ± 2,660 µg As s⁻¹. The more toxic form of arsenic (AsIII) was only detected in one instance, from a warm water stream inlet. Iron and manganese concentrations and the partitioning of these transition metals indicates the ratio of arsenic to these binding elements is not of the right order of  magnitude to remove substantial arsenic from the water column, as dissolved arsenic concentrations exceed that of both iron and manganese. Water isotope ratios and dissolved arsenic concentrations from Rotomahana Waterfall show a complicated mixing regime, including influences such as wind, rainfall, other inlets, and opposing water flows coming from the main water and the high flow waterfall. High temperature and low flow waters from Hot Water Beach demonstrates the influence of inlet water temperature because they alter the movement and concentrations of arsenic heading out towards the open-water inlets. The high temperature of Hot Water Beach creates a localised area of thermal stratification, which causes surface mixing and dilution of the inlet waters with the nearest open-water site. Mixing then occurs with depth closer to the open-water site, passed the point of the hot water induced thermocline. These targeted samples highlight how well arsenic is diluted and buffered by such a large volume of water, and demonstrate the importance of stratification, temperature, and flow rate on the movement of As.  Laboratory and field studies attempted to minimise oxygen introduction to pore water samples using rhizons (pore water filters) and vacutainers. Arsenic speciation was retained in field samples in the vacutainers for up to three months, with concentrations of up to 2,230 µg L⁻¹ of AsIII measured; this result which led to laboratory experiments on the long-term storage and retention of AsIII. However, the data from these laboratory studies were inconclusive for over-time analyses of two experiments; days 2, 26, and 55 after sample spiking for the first experiment, and days 2 and 29 for the second experiment. Vacutainers and rhizons extracted pore waters in-situ in attempt to minimise oxygen introduction to low dissolved oxygen samples; however, the methodology for long-term storage requires further research.  Speciation of arsenic occurs in the sediments due to the highly anoxic environment, with pore water AsIII concentrations ranging exceeding 2,000 µg L⁻¹ in the surface sediments and decreasing with depth. Sediment concentrations show distinct accumulation boundaries which are indicative of redox boundaries over time.

year: 2020

title: The presence of the past: Maori history in contemporary reflection

authors: Mahuika, Nepia

abstract: This is the opening line of a famous saying in my tribe. For our people - Ngāti Porou - these words have become embedded in our tribal identity as important directives that we are encouraged to aspire to. In the “days destined to you”, Ngata reminds us that each generation has its own mana (or authority), our own responsibilities and challenges, our own dreams and destinies to fulfil, and our own histories to tell about Ngāti Porou: who we are, our past, present, and future. If we consider this expectant, and I think hopeful, affirmation as a gift and responsibility, then taking real ownership of the “days destined to us” requires us to know what our forebears have entrusted us with. What are those historical gifts that we might use to “centre” and assert ourselves as Māori, as Ngāti Porou? We might look at this directly, i mua: the past before us because it is our history that is so crucial to us as we walk consciously, and with determination, into the future. Our past before us helps us to know where we are going, it helps us correc our course when we stray, keeps us mindful of the “kaupapa”: whatever that might be in our generation and corner of the Maori universe. We’ve heard already today from both Enoka and Arini how Māori, in our own ways, are engaging with our past, drawing on our korero tuku iho (our oral histories passed down across the generations), on our whakairo (our carving), to illuminate the many ways Māori do, and think about, the past.

text: The presence of the past: Maori history in contemporary reflection This is the opening line of a famous saying in my tribe. For our people - Ngāti Porou - these words have become embedded in our tribal identity as important directives that we are encouraged to aspire to. In the “days destined to you”, Ngata reminds us that each generation has its own mana (or authority), our own responsibilities and challenges, our own dreams and destinies to fulfil, and our own histories to tell about Ngāti Porou: who we are, our past, present, and future. If we consider this expectant, and I think hopeful, affirmation as a gift and responsibility, then taking real ownership of the “days destined to us” requires us to know what our forebears have entrusted us with. What are those historical gifts that we might use to “centre” and assert ourselves as Māori, as Ngāti Porou? We might look at this directly, i mua: the past before us because it is our history that is so crucial to us as we walk consciously, and with determination, into the future. Our past before us helps us to know where we are going, it helps us correc our course when we stray, keeps us mindful of the “kaupapa”: whatever that might be in our generation and corner of the Maori universe. We’ve heard already today from both Enoka and Arini how Māori, in our own ways, are engaging with our past, drawing on our korero tuku iho (our oral histories passed down across the generations), on our whakairo (our carving), to illuminate the many ways Māori do, and think about, the past.

year: 2016