title: Learning through 'being' and 'doing'

authors: Grant, Suzanne Lisa Parker

subjects: first-person action research

abstract: Our research may not emerge in the tidy, linear manner often described in research papers, and hoped for outcomes may never eventuate. Amid this seeming confusion, researchers may experience personal discomfort and perceptions of failure. Drawing on my experiences as a doctoral candidate I address two of the areas for which my own reading of literature left me ill-prepared. I focus first on the emergent nature of action research, and second on the contributions reflection can make to our development as action researchers. Students and teachers of action research are encouraged to appreciate the richness and variety of experiences which interaction and engagement in the research process may bring, for it is these activities which shape our development as researchers.

text: Learning through 'being' and 'doing' Our research may not emerge in the tidy, linear manner often described in research papers, and hoped for outcomes may never eventuate. Amid this seeming confusion, researchers may experience personal discomfort and perceptions of failure. Drawing on my experiences as a doctoral candidate I address two of the areas for which my own reading of literature left me ill-prepared. I focus first on the emergent nature of action research, and second on the contributions reflection can make to our development as action researchers. Students and teachers of action research are encouraged to appreciate the richness and variety of experiences which interaction and engagement in the research process may bring, for it is these activities which shape our development as researchers.

year: 2007

title: Fluxes of Energy and Water Vapour from Grazed Pasture on a Mineral Soil in the Waikato

authors: Kuske, Tehani Janelle

subjects: eddy covariance

abstract: The eddy covariance (EC) technique was used to measure half hourly fluxes of energy and evaporation from 15 December 2007 to 30 November 2008 at the Scott Research Farm, located 7 km east of Hamilton. Many other supporting measurements of climate and soil variables were also made. The research addressed three objectives:
1. To examine the accuracy of the eddy covariance measurement technique.
2. Understand the surface partitioning of energy and water vapour on a diurnal to annual timescale.
3. Compare measurements of evaporation to methods of estimation.
Average energy balance closure at Scott Farm was deficient by 24%, comparable to published studies of up to 30%. Three lysimeter studies were carried out to help verify eddy covariance data. These resulted in the conclusions that; 1) lysimeter pots needed to be deeper to allow for vegetation rooting depths to be encompassed adequately; 2) forcing energy balance closure was not supported by two of the studies (summer and winter); 3) latent heat flux (λE) gap filling of night time EC data during winter over estimated values by about 10 W m-2; and 4) the spring lysimeter study verified eddy covariance measurements including the closure forcing method. Some uncertainty still exists as to the accuracy of both lysimeter and EC methods of evaporation measurement because both methods still have potential biases, however for the purpose of this study, it would appear data are sufficiently accurate to have confidence in results. Energy and water vapour fluxes varied on both a diurnal and seasonal timescale. Diurnally, fluxes were small or negative at night and were highest during the day, usually at solar noon. Seasonally, spring and summer had the highest energy and evaporation fluxes and winter rates were small but tended to exceed available energy supply. Evaporation was constrained by soil moisture availability during summer and by energy availability during winter. Estimated annual evaporation at Scott Farm was 755 mm, 72% of precipitation. Two evaporation models were compared to eddy covariance evaporation (EEC) measurements; the FAO56 Penman-Monteith model (Eo) and the Priestley-Taylor model (EPT). Both models over estimated evaporation during dry conditions and slightly under estimated during winter. The α coefficient that is applied to EPT was not constant and a seasonally adjusted value would be most appropriate. A crop coefficient of 1.13 is needed for Eo measurements during moist conditions. Eo began over estimating evaporation when soil moisture contents dropped below ~44%. A water stress adjustment was applied to both models which improved evaporation estimates, however early onset of drying was not able to be adjusted for. The adjusted Eo model is the most accurate overall, when compared to EEC.

text: Fluxes of Energy and Water Vapour from Grazed Pasture on a Mineral Soil in the Waikato The eddy covariance (EC) technique was used to measure half hourly fluxes of energy and evaporation from 15 December 2007 to 30 November 2008 at the Scott Research Farm, located 7 km east of Hamilton. Many other supporting measurements of climate and soil variables were also made. The research addressed three objectives:
1. To examine the accuracy of the eddy covariance measurement technique.
2. Understand the surface partitioning of energy and water vapour on a diurnal to annual timescale.
3. Compare measurements of evaporation to methods of estimation.
Average energy balance closure at Scott Farm was deficient by 24%, comparable to published studies of up to 30%. Three lysimeter studies were carried out to help verify eddy covariance data. These resulted in the conclusions that; 1) lysimeter pots needed to be deeper to allow for vegetation rooting depths to be encompassed adequately; 2) forcing energy balance closure was not supported by two of the studies (summer and winter); 3) latent heat flux (λE) gap filling of night time EC data during winter over estimated values by about 10 W m-2; and 4) the spring lysimeter study verified eddy covariance measurements including the closure forcing method. Some uncertainty still exists as to the accuracy of both lysimeter and EC methods of evaporation measurement because both methods still have potential biases, however for the purpose of this study, it would appear data are sufficiently accurate to have confidence in results. Energy and water vapour fluxes varied on both a diurnal and seasonal timescale. Diurnally, fluxes were small or negative at night and were highest during the day, usually at solar noon. Seasonally, spring and summer had the highest energy and evaporation fluxes and winter rates were small but tended to exceed available energy supply. Evaporation was constrained by soil moisture availability during summer and by energy availability during winter. Estimated annual evaporation at Scott Farm was 755 mm, 72% of precipitation. Two evaporation models were compared to eddy covariance evaporation (EEC) measurements; the FAO56 Penman-Monteith model (Eo) and the Priestley-Taylor model (EPT). Both models over estimated evaporation during dry conditions and slightly under estimated during winter. The α coefficient that is applied to EPT was not constant and a seasonally adjusted value would be most appropriate. A crop coefficient of 1.13 is needed for Eo measurements during moist conditions. Eo began over estimating evaporation when soil moisture contents dropped below ~44%. A water stress adjustment was applied to both models which improved evaporation estimates, however early onset of drying was not able to be adjusted for. The adjusted Eo model is the most accurate overall, when compared to EEC.

year: 2009

title: Whānau mentoring, Māori youth and crime

authors: Joseph, Robert

abstract: This article will discuss how the whänau was the traditional institution for teaching and nurturing children through (among other things) effective mentoring, and how children were taught tikanga, or the ‘right way’ to think, speak, act and become. Traditional leadership development, whänau dysfunction and whänau renewal are also discussed, followed by my conclusions. This article will not be discussing the place of colonisation, high unemployment, lower education rates and other socio-economic disparities among Mäori that play a part in the causes and perpetuation of Mäori youth and crime. A discussion on the Treaty of Waitangi, indigenous rights, and Mäori development is also omitted although the importance of each of these areas is acknowledged. As the theme of this issue of Childrenz Issues is ‘seeking pathways beyond colonisation’, the focus of this article is on Mäori dealing appropriately with the problems of Mäori youth and crime through effective mentoring within the institution of the whänau.

text: Whānau mentoring, Māori youth and crime This article will discuss how the whänau was the traditional institution for teaching and nurturing children through (among other things) effective mentoring, and how children were taught tikanga, or the ‘right way’ to think, speak, act and become. Traditional leadership development, whänau dysfunction and whänau renewal are also discussed, followed by my conclusions. This article will not be discussing the place of colonisation, high unemployment, lower education rates and other socio-economic disparities among Mäori that play a part in the causes and perpetuation of Mäori youth and crime. A discussion on the Treaty of Waitangi, indigenous rights, and Mäori development is also omitted although the importance of each of these areas is acknowledged. As the theme of this issue of Childrenz Issues is ‘seeking pathways beyond colonisation’, the focus of this article is on Mäori dealing appropriately with the problems of Mäori youth and crime through effective mentoring within the institution of the whänau.

year: 2007-01