Effect of soil moisture stress on uptake and recovery of tagged nitrogen by wheat

Includes bibliographical references (pages 42-43).Labelled 15NH4NO3 was used in a growth chamber to study the effect of moisture stress on the utilization of nitrogen by wheat. This made it possible to determine the recovery of nitrogen (N) in the soil-plant system of two Chernozemic soils. Moisture stress effects were less evident in a clay soil than in a loam. Approximately 55% of the N utilized by the growing plants came from organic soil-N mineralized during the growing period. From 59 to 71% of the initial fertilizer plus soil mineral-N was utilized by the plants. Twenty to 36% remained in the soil, and 1 to 17% was lost. Losses were greatest in soils exposed to high moisture stress and were related to the residual NO3-N levels in the soil. They were attributed to denitrification. Immobilization of N was highest at low moisture stress where plant growth was the greatest, but mineralization was unaffected by the moisture stress applied. It was estimated that 5.0 to 6.2 kg N were required to produce 100 kg of wheat, the highest efficiency of N utilization being obtained at low soil moisture stress

Tachyons, Supertubes and Brane/Anti-Brane Systems

We find supertubes with arbitrary (and not necessarily planar) cross section; the stability against the D2-brane tension is due to a compensation by the local momentum generated by Born-Infeld fields. Stability against long-range supergravity forces is also established. We find the corresponding solutions of the infinite-N M(atrix) model. The supersymmetric D2/anti-D2 system is a special case of the general supertube, and we show that there are no open-string tachyons in this system via a computation of the open-string one-loop vacuum energy.Comment: 1+23 pages, 2 figures, LaTeX. V2, 1+28 pages: Further generalization to non-planar cross-sections and addition of an entirely new section with the explicit supergravity solutions. V3, 1+30 pages: Bound on the angular momentum added, other minor changes in Section

Psychological type and attitude towards Celtic Christianity among committed Churchgoers in the United Kingdom: an empirical study

This article takes the burgeoning interest in Celtic Christianity as a key example of the way in which churches may be responding to the changing spiritual and religious landscape in the United Kingdom today and examines the power of psychological type theory to account for variation in the attitude of committed churchgoers to this innovation. Data provided by a sample of 248 Anglican clergy and lay church officers (who completed the Francis Psychological Type Scales together with the Attitude toward Celtic Christianity Scale) demonstrated that intuitive types, feeling types, and perceiving types reported a more positive attitude towards Celtic Christianity than sensing types, thinking types, and judging types. These findings are interpreted to analyse the appeal of Celtic Christianity and to suggest why some committed churchgoers may find this innovation less attractive

M2-Branes and Background Fields

We discuss the coupling of multiple M2-branes to the background 3-form and 6-form gauge fields of eleven-dimensional supergravity, including the coupling of the Fermions. In particular we show in detail how a natural generalization of the Myers flux-terms, along with the resulting curvature of the background metric, leads to mass terms in the effective field theory.Comment: 19 page

The Vulnerability of Groundwater Resources to Climate Change in Timor-Leste. Prepared for the Australian Government Department of Climate Change and Enerfy Efficiency by B. Mayers, R. Fisher, T. Paul P. Wurm. A. Campbell, Research Institute for the Enviro

This report is part of a two part study of the vulnerability of Timor-Leste’s ground water resources, and those who use them, to predicted climate change.In this part of the study by Charles Darwin University (CDU) we focus on potential impact and adaptive capacity to address the vulnerability of Districts to water availability, and provide recommendations for water management. The second part of the study, by Geosciences Australia and presented separately, investigates the biophysical vulnerability of Timor Leste (of the aquifers) to climate change.This report uses a mixed methods approach including:• Review of current climate change predictions• Review of information about aquifer characteristics, provided by the GA study• Assessment of exposure of aquifers to pressure by groundwater users, by reviewing population distribution and growth• Evaluation of adaptive capacity of groundwater users, using census data on indicators of wealth, and field interviews about use and management of water resources.Using these methods we identify priority areas for action in water management and current and potential adaptation options. These options link readily to the National Adaptation Programmes of Action for Timor-Leste (NAPA), and we have also ranked them broadly in terms of predicted cost of implementation.Timor-Leste is a small island developing state, located in the eastern part of the lesser Sunda Islands archipelago. Topography is rugged, with the central mountains of the island reaching altitudes of almost 3000m. The climate is monsoonal, and annual rainfall varies with elevation and aspect, from less than 1000mm in some coastal areas to over 2500mm in the wettest high altitude areas. Timor-Leste has a complex geology and much of the bedrock is sedimentary calcareous rock with shallow soils of low water holding capacity, high alkalinity and low nutrient content.According to the national census, in 2010 Timor-Leste had a population of 1.07 million. Population growth is high (2.4%), fertility rate is high (5.7 births for each fertile aged woman) and the population is relatively young (41% under 14 years, 54% between 15-66 years, and about 5% over 65 years).Already, water insecurity is widespread in Timor-Leste and is a major limitation of food security and livelihoods. Low-input agriculture is the main economic activity in Timor-Leste, with over 86% of households involved in subsistence farming. The main staple crops are rice, maize and cassava, with the limited rice production on the coastal plains fed by gravity irrigation and maize widely grown on the uplands.Geoscience Australia has classified aquifer types in Timor-Leste according to geology and “prospectivity”, i.e. potential flow rates or yields. The major aquifer types in Timor-Leste are:• Sedimentary aquifers with intergranular porosity, which have potential to hold large amounts of groundwater. Alluvial sedimentary aquifers have potential to be high yielding aquifers, with higher yield associated with greater porosity where sediments are more well-sorted (e.g. Dili).• Limestone karstic aquifers with fissured porosity are associated with many springs fed by groundwater and are sensitive to rainfall. In limestone areas, groundwater recharge, storage and yield are affected by the age of the system which determines whether fissures and channels have formed (e.g. in and around Baucau).• Fractured rock aquifers with localised porosity are low yielding and usually only sufficient for household use and animal watering. There is little or no porosity and groundwater is stored in existing fractures, with new channels not becoming larger with time (e.g. Lequidoe in Aileu District).A substantial proportion (about 33%) of the population live on high yielding sedimentary aquifers, particularly on the coast, such as in Dili District, however, most of the population (44%) live on localised aquifers in the highlands (approximately equally on high yielding karst and low yielding localised fractured rock aquifers aquifers).Uncertainty in climate change projections for Timor-Leste is relatively high because Timor-Leste is a similar in size to the grid cells of the models used for projections, has variable topography and little climatic data with which to test the validity of the models that underpin the projections.The most recent climate projections for Timor-Leste have been published by the Pacific Climate Change Science Program (www.pacificclimatechangescience.org). These projections include:• warming of average air and sea temperatures (by 0.4-1.0oC by 2030 under a high emissions scenario);• decrease in dry season and increase in wet season rainfall;• extreme rainfall events to occur more frequently;• decrease in frequency and increase in high intensity cyclones;• sea level rise will continue (by 6-15cm by 2030 under a high emissions scenario)• ocean acidification will continue.Impacts of climate change are discussed within the following framework:Exposure of groundwater resources to climate change were derived from prospectivity of aquifers as determined by Geoscience Australia. Sensitivity of groundwater resources was mapped by overlaying relative aquifer yield and modelled annual rainfall. Areas along the central northern coast and in Oecussi are expected to be particularly sensitive. Sensitivity was also considered in terms of population pressures, both density and rate of change.Potential impacts of climate change were a function of expected exposure to climate change and sensitivity to those changes. High potential impact was identified in several areas on low yielding, localised aquifers: Liquica District, with low rainfall west of Dili; the Districts of Ainaro, Aileu, Bobonaro, and Ermera, with high and rapidly growing populations; Oecussi District, with high population growth and low rainfall. The major towns of Dili and Baucau can also be considered sites of high potential impacts because of high population densities and high population growth rates. This is despite having relatively high yielding aquifers: high yielding sedimentary aquifer in the case of Dili and high yielding fissured aquifer in the case of Baucau. In addition, the surrounding hills are underlain by low yielding fractured rock aquifers.Vulnerability to climate change is a product of potential impacts and adaptive capacity.High adaptive capacity can minimise the vulnerability of a community or nation in the face of high potential impacts. Adaptive capacity is influenced by many factors, including poverty, education, health and social capital. We derived some possible indicators of adaptive capacity using data from the national census and Demographic and Health Survey, and from field surveys at sites representing the main aquifer types. This investigation indicated higher vulnerability due to potentially low adaptive capacity in some Districts. Dili is wealthy compared with other Districts and this may represent relatively high capacity for adaptation. Other factors, such as implementation of some health programs and evidence of community management bodies, suggest high adaptive capacity in other Districts. Current adaptation strategies in some sites included cooperative management of water resources, moving temporarily when water sources became unavailable, carrying water, and collecting rainwater.In summary, the following adaptation options are recommended:1. Documentation and monitoring of ground water resources – to improve understanding of water availability;2. Integrated water harvesting and storage, and irrigation maintenance – to build local resilience and adaptive capacity;3. Agricultural diversification - to build resilience and adaptive capacity;4. Improving governance (policy and regulation) – to reduce waste and over use, to secure availability and access, and to increase adaptive capacity.The people of Timor-Leste face substantial challenges in coping with the variability of the current climate, and further challenges regarding the expected changes to climate and water availability. Options for adaptations to climate change should be considered in the context of food security and sustainable agriculture and natural resource management practices at community, landscape and national scales. The need for this broader framework is stipulated in the National Adaptation Programmes of Action for Timor-Leste (NAPA)

GW Librae: Still Hot Eight Years Post-Outburst

We report continued Hubble Space Telescope (HST) ultraviolet spectra and ground-based optical photometry and spectroscopy of GW Librae eight years after its largest known dwarf nova outburst in 2007. This represents the longest cooling timescale measured for any dwarf nova. The spectra reveal that the white dwarf still remains about 3000 K hotter than its quiescent value. Both ultraviolet and optical light curves show a short period of 364-373 s, similar to one of the non-radial pulsation periods present for years prior to the outburst, and with a similar large UV/optical amplitude ratio. A large modulation at a period of 2 h (also similar to that observed prior to outburst) is present in the optical data preceding and during the HST observations, but the satellite observation intervals did not cover the peaks of the optical modulation so it is not possible to determine its corresponding UV amplitude. The similarity of the short and long periods to quiescent values implies the pulsating, fast spinning white dwarf in GW Lib may finally be nearing its quiescent configuration.Comment: 6 figures, accepted in A