title: Kia rehe te matau, kia rehe te maui

authors: Winiata, Te Whatanui Huia

subjects: Taiaha, Maori business, maori development

abstract: The theory of applying successful military strategy to the world of business is not a new concept.  The connection between these two environments has often been explored, and works by Sun Tzu and others promote the connection between the battlefield and the boardroom.  The cut and thrust of the business realm is often likened to combat, and the guiding principles and beliefs that influence Generals and Field Commanders are in many ways identical to those of executives and Chief Executive Officers.

This thesis is interested in exploring the interconnectedness between battle and business from a Māori perspective.  In particular, this study explores the link between the Māori weapon known as the taiaha, and Māori business, in the belief that the lessons learnt from the various taiaha schools can be transferred to Māori business.  Likewise, the beliefs, principles and philosophies that are instilled within warriors while training with the taiaha have a valid place within Māori business, and when applied to the Māori business arena, have beneficial outcomes for those involved.

This study highlights fundamental taiaha principles that are applicable to the Māori business world.  These beliefs have been identified by a number of taiaha experts as well as successful Māori business operators.  The long term purpose of this thesis is to support Māori entering into business, by highlighting traditional values that are taught through the medium of taiaha, and showing how they can be applied to business.

text: Kia rehe te matau, kia rehe te maui The theory of applying successful military strategy to the world of business is not a new concept.  The connection between these two environments has often been explored, and works by Sun Tzu and others promote the connection between the battlefield and the boardroom.  The cut and thrust of the business realm is often likened to combat, and the guiding principles and beliefs that influence Generals and Field Commanders are in many ways identical to those of executives and Chief Executive Officers.

This thesis is interested in exploring the interconnectedness between battle and business from a Māori perspective.  In particular, this study explores the link between the Māori weapon known as the taiaha, and Māori business, in the belief that the lessons learnt from the various taiaha schools can be transferred to Māori business.  Likewise, the beliefs, principles and philosophies that are instilled within warriors while training with the taiaha have a valid place within Māori business, and when applied to the Māori business arena, have beneficial outcomes for those involved.

This study highlights fundamental taiaha principles that are applicable to the Māori business world.  These beliefs have been identified by a number of taiaha experts as well as successful Māori business operators.  The long term purpose of this thesis is to support Māori entering into business, by highlighting traditional values that are taught through the medium of taiaha, and showing how they can be applied to business.

year: 2013

title: Mouri Tu, Mouri Moko, Mouri Ora! Moko as a wellbeing strategy

authors: Penehira, Mera

subjects: Maori

abstract: This research has been undertaken within the Health Research Council funded International Collaborative Indigenous Health Research Partnership (ICIHRP) program, “The role of resiliency in responding to blood borne viral and sexually transmitted infections in Indigenous communities”. Some Indigenous communities in Australia, New Zealand and Canada have been shown to experience higher rates of blood borne viral infections. There are a number of categories of health intervention that have been shown to be effective in prevention and enhancing access to treatment for blood borne viral infections, including various forms of health promotion, enhanced diagnostic and treatment services, and harm reduction measures related to injecting drug use. The present research was undertaken with the understanding that development of effective responses of this kind among Indigenous people would benefit from a better understanding of the social and cultural factors that might protect against these infections and their consequences. It is argued that such factors are linked in various ways to Indigenous resistance and resiliency, which is described as the means by which people choose to make use of individual and community strengths to protect themselves against adverse health outcomes and enhance their health and wellbeing.

In this thesis I explore how people and their identity are affected when you are part of a marginalised or vulnerable population – namely, Māori women who have contracted the Hepatitis C Virus (HCV). I argue that traditional knowledge and healing practices are central to Māori getting well and keeping well, and that the use of cultural frameworks and practices have potentially restorative, therapeutic and healing values that are not yet researched or understood by the health field. I argue that a Māori framework of wellbeing, namely ‘Mana Kaitiakitanga’, provides the context in which tā moko (Māori traditional tattoo) fits naturally as a healing intervention. I share the stories of Māori women with HCV who have applied this (tā moko and other forms of tattoo) in their lives and in their journeys back to wellness. Tā moko is a process that penetrates the flesh and marks the skin; it is a process that involves both blood and pain, which may seem incongruous with healing. It is argued however that through pain comes understanding; through pain comes a RE-membering of strength; through pain comes joy; and finally through marking comes identity of who we are and how well we have been and can be again.

Issues and intersections of identity, marginalisation, gender, health, and wellbeing are at the forefront of this research story and of the journeys of the three women whose case studies are presented in this thesis. What makes this thesis unique is that it researches all three of these potential cornerstones of health: identity; wellbeing (spiritual and emotional), and physical wellbeing, in relation to a specific health problem, namely HCV. It is intended that this work will add power to what might be viewed as a particularly Indigenous solution to a virus that disproportionately affects our Indigenous population. This is not about rejecting Western health solutions, but it is about recognising and returning to Indigenous health solutions.

text: Mouri Tu, Mouri Moko, Mouri Ora! Moko as a wellbeing strategy This research has been undertaken within the Health Research Council funded International Collaborative Indigenous Health Research Partnership (ICIHRP) program, “The role of resiliency in responding to blood borne viral and sexually transmitted infections in Indigenous communities”. Some Indigenous communities in Australia, New Zealand and Canada have been shown to experience higher rates of blood borne viral infections. There are a number of categories of health intervention that have been shown to be effective in prevention and enhancing access to treatment for blood borne viral infections, including various forms of health promotion, enhanced diagnostic and treatment services, and harm reduction measures related to injecting drug use. The present research was undertaken with the understanding that development of effective responses of this kind among Indigenous people would benefit from a better understanding of the social and cultural factors that might protect against these infections and their consequences. It is argued that such factors are linked in various ways to Indigenous resistance and resiliency, which is described as the means by which people choose to make use of individual and community strengths to protect themselves against adverse health outcomes and enhance their health and wellbeing.

In this thesis I explore how people and their identity are affected when you are part of a marginalised or vulnerable population – namely, Māori women who have contracted the Hepatitis C Virus (HCV). I argue that traditional knowledge and healing practices are central to Māori getting well and keeping well, and that the use of cultural frameworks and practices have potentially restorative, therapeutic and healing values that are not yet researched or understood by the health field. I argue that a Māori framework of wellbeing, namely ‘Mana Kaitiakitanga’, provides the context in which tā moko (Māori traditional tattoo) fits naturally as a healing intervention. I share the stories of Māori women with HCV who have applied this (tā moko and other forms of tattoo) in their lives and in their journeys back to wellness. Tā moko is a process that penetrates the flesh and marks the skin; it is a process that involves both blood and pain, which may seem incongruous with healing. It is argued however that through pain comes understanding; through pain comes a RE-membering of strength; through pain comes joy; and finally through marking comes identity of who we are and how well we have been and can be again.

Issues and intersections of identity, marginalisation, gender, health, and wellbeing are at the forefront of this research story and of the journeys of the three women whose case studies are presented in this thesis. What makes this thesis unique is that it researches all three of these potential cornerstones of health: identity; wellbeing (spiritual and emotional), and physical wellbeing, in relation to a specific health problem, namely HCV. It is intended that this work will add power to what might be viewed as a particularly Indigenous solution to a virus that disproportionately affects our Indigenous population. This is not about rejecting Western health solutions, but it is about recognising and returning to Indigenous health solutions.

year: 2011

title: Sensitive soils of the Puketoka Formation, Hamilton, New Zealand

authors: Kitchen, Emily

subjects: Puketoka Formation

abstract: Sensitive soils are known to cause significant issues in the infrastructure and civil engineering industry, and are prone to sudden, oftentimes catastrophic failures following long periods of stability. 
The Walton Subgroup soils deposited through volcanic activity and partially reworked by the ancestral Waikato River are identified within the Hamilton Basin. These materials are of interest to the engineering community, and consultancy groups in the Hamilton area, due to their identified sensitivity. The Puketoka Formation was focused on in this study.
Sampling of material was undertaken at two active construction sites in Hamilton: Dixon Road Roundabout, and Temple View Urban Development. A series of classification tests were completed to determine the samples’ mineralogical and geotechnical characteristics. 
Mineralogical testing found that all the materials were silt dominated (55.06 – 81.12 %), with sub-ordinate clay (13.10 – 18.85 %) and sand (5.56 – 25.35 %) fractions. The moisture contents were variable (49 – 65 %). The field moist bulk density varied throughout the samples (1069 – 1576 kg/m3), as did the oven dry bulk densities (645 – 1057 kg/m3). The porosity as a result also varied (36 – 51 %). The void ratios followed the same trend as the porosity values (0.56 – 0.88). The particle densities of the materials also showed variation (1935 – 2487 kg/m3). The activities of all three samples were variable, ranging from inactive (0.60) to active (1.79). The X-Ray Diffraction (XRD) analysis determined that the main clay mineral present within the samples was a kaolinite group clay, either halloysite or kaolinite. The Fieldes & Perrott NaF test to determine the presence of allophane was also completed on the samples. Both tests were negative, confirming the dominance of halloysite. Bulk analysis also determined other constituents of the samples to include quartz, plagioclase, augite and volcanic glass. Scanning Electron Microscopy (SEM) indicated the main halloysite morphologies present to be a combination of short and long tubules, spheroids, plates and book formations. The microstructure was analysed, and the main clay minerals, grains, microaggregates, and pores within the materials described. The microfabric was consistent for all three samples, with each showing an abundance of small pores (< 20 µm). These pores hold significant amounts of water in not readily accessible locations, leading to the highly porous, but poorly permeable nature of the materials. DRAB1 and TV1 showed microstructures consistent with Huppert (1986) and Beattie’s (1990) ‘matrix’ structures, whilst TV2 showed a more dominant ‘skeletal’ to ‘matrix’ structure. 
Atterberg limits testing found that the samples had a high liquid limit (59 – 75 %) and plastic limit (41 – 53 %), but a variable plasticity index (8 – 34 %) and liquidity index (0.1 – 2). This placed all three samples within the high plasticity “MH” category upon the Casagrande chart. Consolidated undrained triaxial testing of DRAB1 and TV1 indicated a characteristic normally consolidated response to shear, with the majority of cores showing shear band formation. Only TV1 at 170 kPa displayed an intermediate failure type, potentially occurring due to a combination of material being tested, confining pressure, and the low shear rate allowing time for pressure dissipation. The percentage of axial strain the cores failed at varied (1.81 – 16.35 %), and the peak deviator stress (129 – 277 kPa) and pore water pressure values (717.2 – 879.7 kPa) tended to increase as the confining pressures increased. Graphical outputs show a moderate strain, contractive (MSC) style of failure. The effective shear strength values produced were in keeping with the varying ranges of previously published values (effective cohesion: 0 – 37 kPa, effective friction angle: 27 - 38°). The permeability for all three samples was estimated to be ~10-9 – 10-10. Thin section analyses of failed core sections for DRAB1 at 270 kPa confining pressure and TV1 at 130 and 230 kPa confining pressures found that some degree of shear formation and propagation occurred. The calculated R’ angle for DRAB1 was closely observed in the thin section, however was not for TV1. This was hypothesised to have occurred due to a true shear band failure not occurring, rather the development of intermediate to juvenile shear bands within the soil. 
The sensitivity of the Puketoka Formation and wider Walton Subgroup is hypothesised to have been derived from the reworking and weathering the materials experienced. This in turn influenced the porosity and permeability of the materials, which I believe govern the sensitivity of the soils to a degree. Therefore, I believe the Puketoka Formation materials are representative of a silt-dominated, minimally reworked deposit of volcanic origin, that showed appreciable differences compared with the previously studied Tauranga soils. 
The remediation strategies used in the engineering industry were also analysed, and the suitability of the strategies in the context of the Puketoka Formation discussed. This assessment provides an overview of why traditional strategies for remediation may not be beneficial in some cases for the Walton Subgroup materials, which could be of benefit to key engineering groups that encounter these soil materials.
The results of this study provide a set of data which can be used as an initial reference point. The findings and hypotheses made could be of use to key groups including local engineering consultancies, who handle these materials regularly.

text: Sensitive soils of the Puketoka Formation, Hamilton, New Zealand Sensitive soils are known to cause significant issues in the infrastructure and civil engineering industry, and are prone to sudden, oftentimes catastrophic failures following long periods of stability. 
The Walton Subgroup soils deposited through volcanic activity and partially reworked by the ancestral Waikato River are identified within the Hamilton Basin. These materials are of interest to the engineering community, and consultancy groups in the Hamilton area, due to their identified sensitivity. The Puketoka Formation was focused on in this study.
Sampling of material was undertaken at two active construction sites in Hamilton: Dixon Road Roundabout, and Temple View Urban Development. A series of classification tests were completed to determine the samples’ mineralogical and geotechnical characteristics. 
Mineralogical testing found that all the materials were silt dominated (55.06 – 81.12 %), with sub-ordinate clay (13.10 – 18.85 %) and sand (5.56 – 25.35 %) fractions. The moisture contents were variable (49 – 65 %). The field moist bulk density varied throughout the samples (1069 – 1576 kg/m3), as did the oven dry bulk densities (645 – 1057 kg/m3). The porosity as a result also varied (36 – 51 %). The void ratios followed the same trend as the porosity values (0.56 – 0.88). The particle densities of the materials also showed variation (1935 – 2487 kg/m3). The activities of all three samples were variable, ranging from inactive (0.60) to active (1.79). The X-Ray Diffraction (XRD) analysis determined that the main clay mineral present within the samples was a kaolinite group clay, either halloysite or kaolinite. The Fieldes & Perrott NaF test to determine the presence of allophane was also completed on the samples. Both tests were negative, confirming the dominance of halloysite. Bulk analysis also determined other constituents of the samples to include quartz, plagioclase, augite and volcanic glass. Scanning Electron Microscopy (SEM) indicated the main halloysite morphologies present to be a combination of short and long tubules, spheroids, plates and book formations. The microstructure was analysed, and the main clay minerals, grains, microaggregates, and pores within the materials described. The microfabric was consistent for all three samples, with each showing an abundance of small pores (< 20 µm). These pores hold significant amounts of water in not readily accessible locations, leading to the highly porous, but poorly permeable nature of the materials. DRAB1 and TV1 showed microstructures consistent with Huppert (1986) and Beattie’s (1990) ‘matrix’ structures, whilst TV2 showed a more dominant ‘skeletal’ to ‘matrix’ structure. 
Atterberg limits testing found that the samples had a high liquid limit (59 – 75 %) and plastic limit (41 – 53 %), but a variable plasticity index (8 – 34 %) and liquidity index (0.1 – 2). This placed all three samples within the high plasticity “MH” category upon the Casagrande chart. Consolidated undrained triaxial testing of DRAB1 and TV1 indicated a characteristic normally consolidated response to shear, with the majority of cores showing shear band formation. Only TV1 at 170 kPa displayed an intermediate failure type, potentially occurring due to a combination of material being tested, confining pressure, and the low shear rate allowing time for pressure dissipation. The percentage of axial strain the cores failed at varied (1.81 – 16.35 %), and the peak deviator stress (129 – 277 kPa) and pore water pressure values (717.2 – 879.7 kPa) tended to increase as the confining pressures increased. Graphical outputs show a moderate strain, contractive (MSC) style of failure. The effective shear strength values produced were in keeping with the varying ranges of previously published values (effective cohesion: 0 – 37 kPa, effective friction angle: 27 - 38°). The permeability for all three samples was estimated to be ~10-9 – 10-10. Thin section analyses of failed core sections for DRAB1 at 270 kPa confining pressure and TV1 at 130 and 230 kPa confining pressures found that some degree of shear formation and propagation occurred. The calculated R’ angle for DRAB1 was closely observed in the thin section, however was not for TV1. This was hypothesised to have occurred due to a true shear band failure not occurring, rather the development of intermediate to juvenile shear bands within the soil. 
The sensitivity of the Puketoka Formation and wider Walton Subgroup is hypothesised to have been derived from the reworking and weathering the materials experienced. This in turn influenced the porosity and permeability of the materials, which I believe govern the sensitivity of the soils to a degree. Therefore, I believe the Puketoka Formation materials are representative of a silt-dominated, minimally reworked deposit of volcanic origin, that showed appreciable differences compared with the previously studied Tauranga soils. 
The remediation strategies used in the engineering industry were also analysed, and the suitability of the strategies in the context of the Puketoka Formation discussed. This assessment provides an overview of why traditional strategies for remediation may not be beneficial in some cases for the Walton Subgroup materials, which could be of benefit to key engineering groups that encounter these soil materials.
The results of this study provide a set of data which can be used as an initial reference point. The findings and hypotheses made could be of use to key groups including local engineering consultancies, who handle these materials regularly.

year: 2021