735 research outputs found
Confocal measurement of the three-dimensional size and shape of plant parenchyma cells in developing fruit tissue
Gray, John D. ; Kolesik, Peter ; Høj, Peter B. ; And Coombe, Bryan G
Where not to have a heart attack in Australia!: The Cardiac ARIA Index
abstract onlyAbstract not availableR. Clark, N. Coffee, K. Eckert, D. Turner, D. Coombe, J. Lawrence, S. Stewart, D. van Gaans, D. Wilkinson, A. Tonki
The origin and development of brown earths on clay-with-flints and coombe deposits
Summary Field investigation of the origin and development of three brown-earth (sol Zessiwk) profiles has been supplemented by mechanical and mineralogical analyses and micromorphological studies. Two profiles, representative of the Batcombe and Winchester series, were on Clay-with-flints and the third, of the Charity series, on a Coombe deposit. Particle-size distribution and petrographic data strongly suggest that all three soils are derived in part from loess. The Charity is interpreted as an autoch- thonous profile formed in a Head deposit composed of chalky and flinty detritus mixed with loess by soliflwion, whereas the Batcombe and Winchester are two- stage profiles, formed in composite (non-uniform) parent materials resulting from the superficial incorporation of loess with the truncated or redeposited remains of previously weathered horizons with rotlehm and/or braunlehm fabrics. These Clay-with-flint substrata contain materials derived from Chalk and Eocene beds in varying proportions, weathered in Tertiary or interglacial periods and rearranged by periglacial agencies. Clay-with-flints sensu stricto, as represented in the Win- chester subsoil, has distinctive physical, mineralogical, and micromorphological characteristics, and appears to have originated by sub-surface solution of the Chalk and illuvial accumulation of clay derived for the most part from overlying deposits. The land surfaces concerned have probably been subjected to at least one alternation of periglacial and temperate conditions after the addition of loess. Hence the extent to which either profile reflects the influence of the contemporary environment is not readily assessed, but evidence is adduced that the upper horizons of each profile bear the impress of similar pedogenic processes, including eluviation of clay-size material and acidic weathering leading to the accumulation of vermiculite, modified in the Winchester by the effects of erosion and soil creep
Cardiac ARIA: a geographic accessibility model to cardiac services in Australia
PowerPoint Presentation.
Spatial Information Committee (SICOM), Surveying and Spatial Sciences Institute (SSSI) and Spatial industries Business Association (SIBA)Turner D, Coffee N, Clark RA, Eckert K, Coombe D, Lawrence J, Astles P, Stewart S, van Gaans D, Hugo G, Bamford E, Wilkinson D, Tonkin A.
On behalf of the CARDIAC-ARIA project grou
Where not to have a heart attack in Australia!
Poster - Subtitle: The Cardiac ARIA Index: Measuring accessibility to cardiac services in urban, rural and remote Australia using GISClark RA, Coffee N, Turner D, Eckert K, Coombe D, Bamford Errol, Hugo Graeme, Lawrence J, Stewart S, van Gaans D, Wilkinson D, Tonkin A., On behalf of the Cardiac ARIA project
Mapping services to support a patient's journey through evidence-based care pathways after a cardiac event
Conference paper abstractAbstract not availableR.A. Clark, D. Wilkinson, N. Coffee, K. Eckert, P. Astles, M. Milligan, G. Pearce, S. Stewart, D. van Gaans, D. Turner, D. Coombe, C. Aroney, D. Chew, H. Grantham, P. Macdonald, A. MacIsaac, P. Thompson, W.Walsh, A. Tonkin, Onbehalf of the CARDIAC-ARIA project grou
sj-docx-1-hpp-10.1177_15248399231206088 – Supplemental material for The Measurement Approaches to Partnership Success (MAPS) Questionnaire and Facilitation Guide: A Validated Measure of CBPR Partnership Success
Supplemental material, sj-docx-1-hpp-10.1177_15248399231206088 for The Measurement Approaches to Partnership Success (MAPS) Questionnaire and Facilitation Guide: A Validated Measure of CBPR Partnership Success by Barbara L. Brush, Barbara Israel, Chris M. Coombe, Shoou-Yih D. Lee, Megan Jensen, Eliza Wilson-Powers, Adena Gabrysiak, P. Paul Chandanabhumma, Elizabeth Baker, Marita Jones and Laurie Lachance in Health Promotion Practice</p
sj-docx-2-hpp-10.1177_15248399231206088 – Supplemental material for The Measurement Approaches to Partnership Success (MAPS) Questionnaire and Facilitation Guide: A Validated Measure of CBPR Partnership Success
Supplemental material, sj-docx-2-hpp-10.1177_15248399231206088 for The Measurement Approaches to Partnership Success (MAPS) Questionnaire and Facilitation Guide: A Validated Measure of CBPR Partnership Success by Barbara L. Brush, Barbara Israel, Chris M. Coombe, Shoou-Yih D. Lee, Megan Jensen, Eliza Wilson-Powers, Adena Gabrysiak, P. Paul Chandanabhumma, Elizabeth Baker, Marita Jones and Laurie Lachance in Health Promotion Practice</p
sj-docx-2-heb-10.1177_10901981231213352 – Supplemental material for Validation of the Measurement Approaches to Partnership Success (MAPS) Questionnaire
Supplemental material, sj-docx-2-heb-10.1177_10901981231213352 for Validation of the Measurement Approaches to Partnership Success (MAPS) Questionnaire by Laurie Lachance, Barbara L. Brush, Graciela Mentz, Shoou-Yih D. Lee, P. Paul Chandanabhumma, Chris M. Coombe, Ricardo DeMajo, Adena Gabrysiak, Megan Jensen, Angela G. Reyes, Zachary Rowe, Amy J. Schulz, Eliza Wilson-Powers and Barbara A. Israel in Health Education & Behavior</p
Measurement of the D+/- production asymmetry in 7 TeV pp collisions
The asymmetry in the production cross-section \sigma of D+/- mesons, A_P = (\sigma(D+) - \sigma(D-))/(\sigma(D+) + \sigma(D-)), is measured in bins of pseudorapidity \eta and transverse momentum p_T within the acceptance of the LHCb detector. The result is obtained with a sample of D+ -> K_S pi+ decays corresponding to an integrated luminosity of 1.0 fb^-1, collected in pp collisions at a centre of mass energy of 7 TeV at the Large Hadron Collider. When integrated over the kinematic range 2.0 K_S pi+ decay is negligible. No significant dependence on \eta or p_T is observed
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