128,051 research outputs found
The William G. Sutherland, D.O. Collection
No full textFinding aid for The William G. Sutherland, D.O. CollectionWilliam Garner Sutherland, D.O. (1872-1954), a Minnesota Osteopathic physician and student of Andrew Taylor Still, discovered the field of cranial osteopathy. Dr. Sutherland referred to his discovery as "Osteopathy in the Cranial Field" (OCF). He founded the Osteopathic Cranial Association in 1946 (which changed its name to the Cranial Academy when it became a component of the American Academy of Osteopathy in 1960). He also founded the Sutherland Cranial Teaching Foundation in 1953 to guide the training of physicians in cranial osteopathic techniques.The Sutherland Collection contains the writings, memorabilia, recorded lectures and voluminous correspondence of Dr. Sutherland, tracing the growth of the Sutherland Cranial Teaching Foundation as well as documenting the spread of the cranial concept as a viable specialty within the osteopathic profession. Included are the unofficial papers of the Sutherland Cranial Teaching Foundation (1950-1971) and the Moorestown Cranial Study Group. The papers were gathered by Anne L. Wales, D.O., an early faculty member of the Sutherland Cranial Teaching Foundation. The Moorestown Cranial Study Group was created by and met in the home/office of Rebecca Conrow Lippincott, D.O. and Howard A. Lippincott, D.O. for the further study and review of cranial procedures and advancements. Materials from the New England Cranial Study Group are also included. The collection contains transcriptions and slides from lectures by Dr. Sutherland, et al (1947-48), a manuscript copy of his seminal work, The Cranial Bowl (1939), photographs of Dr. Sutherland and many other early pioneers in the field, and audio and video presentations of classroom and conference lectures by Dr. Sutherland and other leading cranial experts of the time. Also included in the collection are personal items belonging to Dr. Sutherland and correspondence from Dr. and Mrs. Sutherland to Drs. Chester Handy and Anne Wales
graig-sutherland/transport-miz-tc: Software and Data for MIZ Transport by Sutherland et al. , TC, 2022
No full textSoftware and data assoicated with:
Sutherland, G., Aguiar, V., Hole, L.-R., Rabault, J., Dabboor, M., and Breivik, Ø.: Determining an optimal transport velocity in the marginal ice zone using operational ice-ocean prediction systems, The Cryosphere Discuss. [preprint], https://doi.org/10.5194/tc-2021-289, in review, 2021
Sutherland, L, VX28325
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/420059Surname: SUTHERLAND. Given Name(s) or Initials: L. Military Service Number or Last Known Location: VX28325. Missing, Wounded and Prisoner of War Enquiry Card Index Number: 40884.244639
Item: [2016.0049.52320] "Sutherland, L, VX28325
Windsurfer fin hydrodynamics
No full textFin hydrodynamics of a windsurferL. Sutherland & R.A. Wilson Department of Ship Science, University of Southampton 1 Introduction Windsurfing is a relatively new technical sport and has advanced rapidly in the quality of equipment, with the consequent increase in speed and technique that only time can allow. The initial developments were aimed at the obvious components such as the sail rig and the shape of the board itself. The remaining item of the windsurfer, the fin, was initially thought of as providing a control surface for directional stability, similar to the effects of a tail fin of an aeroplane. Of course this is far from the truth, since the driving force derived from the sail rig, has to be resisted by the fin. Thus the windsurfer must be thought of as a combined system of a board, rig and the fin. This paper will concentrate on the fin geometry and our ability to derive design force estimates, so that suitable matching of board to fin
Correspondence to Robert L. Sutherland
No full textUnsigned letter to Robert L. Sutherland, Director of the Hogg Foundation thanking him for a copy of "The Hogg Foundation Reports
A Viking burial at Balnakeil, Sutherland
No full textA full discussion of a young Viking male pagan grave with full consideration of its context and broader significance in the context of the Norse in the British Isles
Structural and Functional features of the CD34 antigen: an update
No full textCD34 is a heavily glycosylated type I transmembrane molecule, that can be phoshorylated by a variety of kinases including Protein kinase C and Tyrosine kinases. The classification of epitopes detected by different CD34 MAbs has aided the selection of appropriate antibodies for use in specific clinical and research laboratory settings. Detailed structural analyses and cloning studies have confirmed that CD34 is a sialomucin, and have suggested that the fine composition of the carbohydrate moieties contained in its extended N-terminal region is important in determining its interactions with a variety of different ligands. For high endothelial venules (HEV) CD34 to serve as a ligand for L-selectin, the O-linked glycans of HEV CD34 are modified in an exquisitely specific manner with a variety of sialyl- and sulfo-transferases. In contrast, CD34 is not the ligand for L-selectin in hematopoietic stem/progenitor cells (HSPCs) and despite much endeavour, ligands for hematopoietic CD34 remain to be identified
Structural and Functional features of the CD34 antigen: an update
No full textCD34 is a heavily glycosylated type I transmembrane molecule, that can be phoshorylated by a variety of kinases including Protein kinase C and Tyrosine kinases. The classification of epitopes detected by different CD34 MAbs has aided the selection of appropriate antibodies for use in specific clinical and research laboratory settings. Detailed structural analyses and cloning studies have confirmed that CD34 is a sialomucin, and have suggested that the fine composition of the carbohydrate moieties contained in its extended N-terminal region is important in determining its interactions with a variety of different ligands. For high endothelial venules (HEV) CD34 to serve as a ligand for L-selectin, the O-linked glycans of HEV CD34 are modified in an exquisitely specific manner with a variety of sialyl- and sulfo-transferases. In contrast, CD34 is not the ligand for L-selectin in hematopoietic stem/progenitor cells (HSPCs) and despite much endeavour, ligands for hematopoietic CD34 remain to be identified
An in situ assessment of seabed stability in Baynes Sound, British Columbia, Canada
No full textSutherland, T.F. and Amos, C.L., 2020. An in situ assessment of seabed stability in Baynes Sound, British Columbia, Canada. Journal of Coastal Research, 36(3), 472-486. Coconut Creek (Florida), ISSN 0749-0208. The Sea Carousel, an annular flume, was deployed to examine (in situ) fundamental parameters of seabed stability in Baynes Sound, British Columbia, Canada. Sediment grain size, water and organic contents, and chlorophyll and phaeopigment concentrations were collected to establish a hierarchy of factors associated with seabed stability. Sediment stability increased toward the Sound entrance in concert with decreases in water, organic, and silt-clay contents and a transition from cohesive to noncohesive properties. Bed-stress estimates, based on the quadratic stress law and turbulent kinetic energy (TKE) methods, showed a decrease in the drag coefficient from the inner (0.04) to the outer (0.0015) Sound. Surface erosion thresholds ranged between 0.04 to 0.28 Pa, whereas the friction coefficients (e.g., the failure envelop) were on average 12°, representing normally consolidated sediments. Type I (floc) erosion occurred at low shear stresses, whereas type II (mass) erosion happened at higher values. Erosion rates (E, for type I erosion) fitted a power function of excess shear stress (E
m = τ0 - τcrit,z)m with zero offset, where 0.81 < m < 2.32. The lowest and highest values for a given excess-shear stress occurred in the inner Sound and outer Sound, respectively. Settling of (resuspended) sediment after an exponential decay law [d(SSC)/dt] = SSC0 (expkt), where k fell within that of published values (3 < k < 539). Higher values of k (fastest settling) were observed in the inner Sound relative to the outer Sound. The sedimentation diameter (ds) fell in a coarse-silt to fine-sand range and was larger in the outer Sound, reflecting a coarsening of bed sediments.
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Robert E. Lee Sutherland
No full textFrom the Fant Memorial Library Photographs Collection. R. E. L. Sutherland, university president 1930-1932https://athenacommons.muw.edu/mdl-1900-1949/1094/thumbnail.jp
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