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Full-Text Articles in Entire DC Network
Building Strong Brands: An Examination Of The Ubt Brand Building Experience, Metihe Kastrati
Building Strong Brands: An Examination Of The Ubt Brand Building Experience, Metihe Kastrati
Theses and Dissertations
No abstract provided.
Volume 12, No. 2 (Winter 2008), Office Of University Advancement, Bryant University
Volume 12, No. 2 (Winter 2008), Office Of University Advancement, Bryant University
Bryant Magazine (1997-2019)(2024-present)
No abstract provided.
Put Another Way…, Dewey I. Dykstra
Put Another Way…, Dewey I. Dykstra
Physics Faculty Publications and Presentations
No abstract provided.
References For Time In Archaeology: Time Perspectivism Revisited, Simon J. Holdaway, Luann Wandsnider
References For Time In Archaeology: Time Perspectivism Revisited, Simon J. Holdaway, Luann Wandsnider
Department of Anthropology: Faculty Publications
22 pages of reference bibliography for the 2008 anthology of articles on archeology, methodology, and time.
Evaluation And Application Of The Cpm Dairy Nutrition Model, L. O, Tedeschi, W. Chalupa, E. Janczewski, D. G. Fox, C. Sniffen, R. Munson, Paul J. Kononoff, R. Boston
Evaluation And Application Of The Cpm Dairy Nutrition Model, L. O, Tedeschi, W. Chalupa, E. Janczewski, D. G. Fox, C. Sniffen, R. Munson, Paul J. Kononoff, R. Boston
Department of Animal Science: Faculty Publications
The Cornell-Penn-Miner (CPM) Dairy is an applied mathematical nutrition model that computes dairy cattle requirements and the supply of energy and nutrients based on characteristics of the animal, the environment and the physicochemical composition of the feeds under diverse production scenarios. The CPM Dairy was designed as a steady-state model to use rates of degradation of feed carbohydrate and protein and the rate of passage to estimate the extent of ruminal fermentation, microbial growth, and intestinal digestibility of carbohydrate and protein fractions in computing energy and protein post-rumen absorption, and the supply of metabolizable energy and protein to the animal. …
Asynchronous Learning Networks: Policy Implications For Minority Serving Institutions And For Leaders Addressing Needs Of Minority Learners, Janet K. Poley
Asynchronous Learning Networks: Policy Implications For Minority Serving Institutions And For Leaders Addressing Needs Of Minority Learners, Janet K. Poley
Department of Agricultural Leadership, Education, and Communication: Faculty Publications
For minority serving institutions, policies that support learners call for decisions about equity, quality, cost, impact on national economic performance and international global relationships.
Changing U.S. demographics and globalization factors of the type described by Thomas Friedman in The World Is Flat (rapidly expanding technology infrastructure, politics, innovation) [1] are creating the environment within which policies in this country and around the world are and will be developed well into the first 25 years of the century. This paper is focused on the Minority Serving Institutions including formally designated MSIs as well as other public and private institutions desiring to …
Principles Of Normative Integration And The Allocation Of International Authority: The Wto, The Vienna Convention On The Law Of Treaties, And The Rio Declaration, Tomer Broude
Loyola University Chicago International Law Review
No abstract provided.
Doha Round Schisms: Numerous, Technical, And Deep, Raj Bhala
Doha Round Schisms: Numerous, Technical, And Deep, Raj Bhala
Loyola University Chicago International Law Review
No abstract provided.
Palaeomagnetism Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, G. Acton, F. Florindo, L. Jovane, B. Lum, C. Ohneiser, L. Sagnotti, E. Strada, K. L. Verosub, G. S. Wilson, Andrill-Sms Science Team
Palaeomagnetism Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, G. Acton, F. Florindo, L. Jovane, B. Lum, C. Ohneiser, L. Sagnotti, E. Strada, K. L. Verosub, G. S. Wilson, Andrill-Sms Science Team
ANDRILL Research and Publications
We conducted initial palaeomagnetic studies on cores from site AND-2A (77°45.488’S, 165°16.605’E, ~383.57 metres water depth). A total of 813 samples were collected that span from the top of the section down to the base at 1138.54 metres below sea floor (mbsf). Samples were collected every one or two metres down the core, with paired (pilot) samples being collected about every ten to twenty metres to allow us to assess the demagnetisation behaviour of the samples using either alternating field (AF) or thermal demagnetisation. With the exception of only a few intervals, AF demagnetisation was observed to resolve a characteristic …
Preliminary Integrated Chronostratigraphy Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, G. Acton, J. Crampton, G. Di Vincenzo, Christopher R. Fielding, F. Florindo, M. Hannah, D. M. Harwood, S. Ishman, K. Johnson, L. Jovane, Richard Levy, B. Lum, M. C. Marcano, S. Mukasa, C. Ohneiser, M. P. Olney, C. Riesselman, L. Sagnotti, C. Stefano, E. Strada, M. Taviani, E. Tuzzi, K. L. Verosub, G. S. Wilson, M. Zattin, Andrill-Sms Science Team
Preliminary Integrated Chronostratigraphy Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, G. Acton, J. Crampton, G. Di Vincenzo, Christopher R. Fielding, F. Florindo, M. Hannah, D. M. Harwood, S. Ishman, K. Johnson, L. Jovane, Richard Levy, B. Lum, M. C. Marcano, S. Mukasa, C. Ohneiser, M. P. Olney, C. Riesselman, L. Sagnotti, C. Stefano, E. Strada, M. Taviani, E. Tuzzi, K. L. Verosub, G. S. Wilson, M. Zattin, Andrill-Sms Science Team
ANDRILL Research and Publications
We use all available chronostratigraphic constraints – biostratigraphy, magnetostratigraphy, radioisotopic dates, strontium-isotope stratigraphy, and correlation of compositional and physical properties to well-dated global or regional records – to construct a preliminary age model for ANDRILL SMS Project’s AND-2A drillcore (77°45.488’S, 165°16.605’E, 383.57 m water depth). These diverse chronostratigraphic constraints are consistent with each other and are distributed throughout the 1138.54 m-thick section, resulting in a well-constrained age model. The sedimentary succession comprises a thick early and middle Miocene section below 224.82 mbsf and a condensed middle/late Miocene to Recent section above this. The youngest sediments are Brunhes age (<0.781 Ma), as confirmed by a radioisotopic age of 0.691±0.049 Ma at 10.23 mbsf and the occurrence of sediments that have normal magnetic polarity down to ~31.1 mbsf, which is interpreted to be the Brunhes/Matuyama reversal (0.781 Ma). The upper section is punctuated by disconformities resulting from both discontinuous deposition and periods of extensive erosion typical of sedimentary environments at the margin of a dynamic ice sheet. Additional breaks in the section may be due to the influence of tectonic processes. The age model incorporates several major hiatuses but their precise depths are still somewhat uncertain, as there are a large number of erosional surfaces identified within the stratigraphic section. One or more hiatuses, which represent a total 7 to 8 million years of time missing from the sedimentary record, occur between about 50 mbsf and the base of Lithostratigraphic Unit (LSU) 3 at 122.86 mbsf. Similarly, between about 145 mbsf and the base of LSU 4 at 224.82 mbsf, one or more hiatuses occur on which another 2 to 3 million years of the sedimentary record is missing. Support for the presence of these hiatuses comes from a diatom assemblage that constrains the age of the core from 44 to 50 mbsf to 2.06-2.84 Ma, two radioisotopic dates (11.4 Ma) and a Sr‑isotope date (11.7 Ma) that indicate the interval from 127 to 145 mbsf was deposited between 11.4 and 11.7 Ma, and three diatom occurrence datums from between 225.38 and 278.55 mbsf that constrain the age of this upper part of Lithostratigraphic Unit (LSU) 5 to 14.29 - 15.89 Ma. Below the boundary between LSU 5 and 6 sedimentation was relatively continuous and rapid and the age model is well-constrained by 9 diatom datums, seven 40 …0.781>
Physical Properties Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, Gavin B. Dunbar, C. Atkins, D. Magens, F. Niessen, Andrill-Sms Science Team
Physical Properties Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, Gavin B. Dunbar, C. Atkins, D. Magens, F. Niessen, Andrill-Sms Science Team
ANDRILL Research and Publications
Whole-core measurements of Wet Bulk Density (WBD), compressional (P)-wave velocity (Vp), and Magnetic Susceptibility were measured at a sampling interval of 1 or 2 centimetres (cm) throughout the AND-2A drill core for initial core characterisation and on-site correlation with seismic modeling to predict target-reflector depth. Measurements were made using a GEOTEK (Multi-Sensor-Core-Logger MSCL). Density and velocity standards were measured together with core runs of 3-6 metres (m) (and occasionally up to 18 m) throughout the entire depth range to monitor data quality. Drift of the magnetic susceptibility sensor was also monitored and corrected where necessary. These physical properties show a …
Operations Overview For The Andrill Southern Mcmurdo Sound Project, Antarctica, T. Falconer, A. Pyne, D. Wilson, Richard Levy, S. Nielsen, S. Petrushak, Andrill-Sms Science Team
Operations Overview For The Andrill Southern Mcmurdo Sound Project, Antarctica, T. Falconer, A. Pyne, D. Wilson, Richard Levy, S. Nielsen, S. Petrushak, Andrill-Sms Science Team
ANDRILL Research and Publications
During the austral spring of 2007-08, a 1138 metre (m)-long rock and sediment core (ANDRILL [AND]-2A) was recovered from beneath the land-fast sea-ice in southern McMurdo Sound (SMS) in 384 m of water. A custom-built drilling system comprising an UDR-1200 rig, jack-up platform, hot water drill, sea riser, and diamond-bit wireline coring string was set up on the sea-ice approximately 32 kilometres (km) from Scott Base (NZ) and McMurdo Station (USA). The drilling system employed technology developed to handle challenging environmental conditions, including drilling from an 8 metre-thick sea-ice ‘platform’ that moved both laterally and vertically, tidal currents, and high …
Sedimentology And Stratigraphy Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, Christopher R. Fielding, C. B. Atkins, K. N. Bassett, G. H. Browne, G. B. Dunbar, B. D. Field, Tracy D. Frank, L. A. Krissek, K. S. Panter, S. Passchier, S. F. Pekar, S. Sandroni, F. Talarico, Andrill-Sms Science Team
Sedimentology And Stratigraphy Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, Christopher R. Fielding, C. B. Atkins, K. N. Bassett, G. H. Browne, G. B. Dunbar, B. D. Field, Tracy D. Frank, L. A. Krissek, K. S. Panter, S. Passchier, S. F. Pekar, S. Sandroni, F. Talarico, Andrill-Sms Science Team
ANDRILL Research and Publications
During the 2007 – 2008 austral spring season, the ANDRILL Southern McMurdo Sound Project recovered a core 1138 metres long (AND-2A) from a location in the southern McMurdo Sound near the Dailey Islands. This core contains a range of lithologies, including various types of terrigenous clastic diamictite, conglomerate and breccia, sandstone and mudrocks, volcanic lava, pyroclastic and reworked volcanic sedimentary rocks, and diatomite. The succession is divided into fourteen lithostratigraphic units (LSUs), two of which (LSUs 1 and 8) are further subdivided into three and four sub-units, respectively, based on changes in abundance of lithologies. Thirteen lithofacies are recognized, ranging …
Background To The Andrill Southern Mcmurdo Sound Project, Antarctica, F. Florindo, D. M. Harwood, F. Talarico, Richard Levy
Background To The Andrill Southern Mcmurdo Sound Project, Antarctica, F. Florindo, D. M. Harwood, F. Talarico, Richard Levy
ANDRILL Research and Publications
During the austral spring of 2007, the Southern McMurdo (SMS) Project recovered a 1138.54 meter long drill core (AND-2A) from a 8.5 m thick floating seaice platform (~8.5 meters thick) over approximately 380 meters of water (77°45.488S; 165°16.613E) (Fig. 1). This demonstrated the ANDRILL Program’s continuing success in recovering high quality marine and glacimarine sedimentary drill core (> 98% core recovery) from high latitude ice-covered areas. A primary goal of the SMS Project, the second drillhole
of the McMurdo Sound Portfolio (Harwood et al., 2006), was to recover an Antarctic marine sediment record depositied during the middle Miocene, which has …
Explanatory Notes For The Andrill Southern Mcmurdo Sound Project, Antarctica, F. Florindo, D. M. Harwood, Richard Levy, G. Acton, Christopher R. Fielding, K. Panter, T. Paulsen, F. Sangiorgi, F. Talarico, M. Taviani, V. Willmott, Andrill-Sms Science Team
Explanatory Notes For The Andrill Southern Mcmurdo Sound Project, Antarctica, F. Florindo, D. M. Harwood, Richard Levy, G. Acton, Christopher R. Fielding, K. Panter, T. Paulsen, F. Sangiorgi, F. Talarico, M. Taviani, V. Willmott, Andrill-Sms Science Team
ANDRILL Research and Publications
This Explanatory Notes section complements and supports four other documents, which collectively describe the process and procedures of scientific investigations employed during the ANDRILL SMS Project: (1) ANDRILL Southern McMurdo Sound Project - Scientific Prospectus (ANDRILL contribution 5 - Harwood et al., 2005); (2) a Science Plan summary of SMS Project research compiled from research proposals of Science Team menbers (available on the SMS Project ‘Science Drive’ – Harwood et al., 2007); (3) SMS Project Science Logistics Implementation Plan (SLIP) - draft documents developed and distributed to SMS team members prior to deployment; (4) Operations overview – Falconer et al., …
Late Cenozoic Climate History Of The Ross Embayment From The And-1b Drill Hole: Culmination Of Three Decades Of Antarctic Margin Drilling, T. R. Naish, R. D. Powell, Peter J. Barrett, R. H. Levy, S. Henrys, G. S. Wilson, L. A. Krissek, F. Niessen, M. Pompilio, J. Ross, R. Scherer, F. Talarico, A. R. Pyne, Andrill-Mis Science Team
Late Cenozoic Climate History Of The Ross Embayment From The And-1b Drill Hole: Culmination Of Three Decades Of Antarctic Margin Drilling, T. R. Naish, R. D. Powell, Peter J. Barrett, R. H. Levy, S. Henrys, G. S. Wilson, L. A. Krissek, F. Niessen, M. Pompilio, J. Ross, R. Scherer, F. Talarico, A. R. Pyne, Andrill-Mis Science Team
ANDRILL Research and Publications
Because of the paucity of exposed rock, the direct physical record of Antarctic Cenozoic glacial history has become known only recently and then largely from offshore shelf basins through seismic surveys and drilling. The number of holes on the continental shelf has been small and largely confined to three areas (McMurdo Sound, Prydz Bay, and Antarctic Peninsula), but even in McMurdo Sound, where Oligocene and early Miocene strata are well cored, the late Cenozoic is poorly known and dated. The latest Antarctic geological drilling program, ANDRILL, successfully cored a 1285-m-long record of climate history spanning the last 13 m.y. from …
Petrologic And Geochemical Composition Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, K. Panter, F. Talarico, K. Bassett, P. Del Carlo, B. Field, T. Frank, S. Hoffmann, G. Kuhn, L. Reichelt, S. Sandroni, M. Taviani, L. Bracciali, G. Cornamusini, H. Von Eynatten, S. Rocchi, Andrill-Sms Science Team
Petrologic And Geochemical Composition Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, K. Panter, F. Talarico, K. Bassett, P. Del Carlo, B. Field, T. Frank, S. Hoffmann, G. Kuhn, L. Reichelt, S. Sandroni, M. Taviani, L. Bracciali, G. Cornamusini, H. Von Eynatten, S. Rocchi, Andrill-Sms Science Team
ANDRILL Research and Publications
The compositional record of the AND-2A drillcore is examined using petrological, sedimentological, volcanological and geochemical analysis of clasts, sediments and pore waters. Preliminary investigations of basement clasts (granitoids and metasediments) indicate both local and distal sources corresponding to variable ice-volume and ice-flow directions. Low abundance of sedimentary clasts (e.g., arkose, litharenite) suggests reduced contributions from sedimentary covers while intraclasts (e.g., diamictite, conglomerate) attest to intrabasinal reworking. Volcanic material includes pyroclasts (e.g., pumice, scoria), sediments and lava. Primary and reworked tephra layers occur within the Early Miocene interval (1093 to 640 metres below sea floor). …
Palaeontological Characterisation And Analysis Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, M. Taviani, M. Hannah, D. M. Harwood, S. E. Ishman, K. Johnson, M. Olney, C. Riesselman, E. Tuzzi, A. G. Beu, S. Blair, V. Cantarelli, A. Ceregato, S. Corrado, B. Mohr, S. H.H. Nielson, D. Persico, S. Petrushak, J. I. Raine, S. Warny, Andrill-Sms Science Team
Palaeontological Characterisation And Analysis Of The And-2a Core, Andrill Southern Mcmurdo Sound Project, Antarctica, M. Taviani, M. Hannah, D. M. Harwood, S. E. Ishman, K. Johnson, M. Olney, C. Riesselman, E. Tuzzi, A. G. Beu, S. Blair, V. Cantarelli, A. Ceregato, S. Corrado, B. Mohr, S. H.H. Nielson, D. Persico, S. Petrushak, J. I. Raine, S. Warny, Andrill-Sms Science Team
ANDRILL Research and Publications
The palaeontological yield of the 1138.54 metre-long AND-2A sedimentary rock core provides unique documentation of Neogene environments in the Ross Sea region of Antarctica. Especially important is the biological legacy of the climatically crucial ‘mild’ middle Miocene phase. Diatom-bearing units provide key information for stratigraphic intervals never previously recovered from locations proximal to the Antarctic continent and constrain the age model for the AND-2A core. Benthic calcareous (and agglutinated) foraminifera were present at many levels; remarkable is the occurrence of planktonic taxa only seldom found in the Neogene nearshore record of the Ross Sea region. The sporadic occurrence of calcareous …
Downhole Measurements In The And-2a Borehole, Andrill Southern Mcmurdo Sound Project, Antarctica, T. Wonik, T. Grelle, D. Handwerger, R. D. Jarrard, A. Mckee, T. Patterson, T. Paulsen, S. Pierdominici, D. R. Schmitt, H. Schröder, M. Speece, T. J. Wilson, Andrill-Sms Science Team
Downhole Measurements In The And-2a Borehole, Andrill Southern Mcmurdo Sound Project, Antarctica, T. Wonik, T. Grelle, D. Handwerger, R. D. Jarrard, A. Mckee, T. Patterson, T. Paulsen, S. Pierdominici, D. R. Schmitt, H. Schröder, M. Speece, T. J. Wilson, Andrill-Sms Science Team
ANDRILL Research and Publications
Under the framework of the ANDRILL Southern McMurdo Sound (SMS) Project successful downhole experiments were conducted in the 1138.54 metre (m)-deep AND-2A borehole. Wireline logs successfully recorded were: magnetic susceptibility, spectral gamma ray, sonic velocity, borehole televiewer, neutron porosity, density, calliper, geochemistry, temperature and dipmeter. A resistivity tool and its backup both failed to operate, thus resistivity data were not collected. Due to hole conditions, logs were collected in several passes from the total depth at ~1138 metres below sea floor (mbsf) to ~230 mbsf, except for some intervals that were either inaccessible due to bridging or were shielded by …
2008 Bird Strike Committee–Usa/Canada Meeting Program
2008 Bird Strike Committee–Usa/Canada Meeting Program
Bird Strike Committee-USA/Canada Joint Annual Meeting: 10th (2008)
No abstract provided.
Using Chemigation Safely And Effectively: Training Manual
Using Chemigation Safely And Effectively: Training Manual
University of Nebraska-Lincoln Extension: Historical Materials
Table of Contents
Acknowledgements
Introduction
Factors Affecting Chemigation Practice
Irrigation Systems
Chemigation Equipment and Safety Devices
Calibration Procedures
Management
Laws and Regulations
Appendix A Summary - Nebraska Chemigation Act
Appendix B NDEQ Rules and Regulations Pertaining to Chemigation
Appendix C Leakage Test
Appendix D Certified Chemigation Check Valve Models
Appendix E Calculating Irrigated Acreages
Appendix F Fertilizer and Pesticide Containment
Appendix G Disposing of Livestock Waste Through an Irrigation Distribution System
Appendix H Nebraska Natural Resources Districts
UNL Extension Publications
Focus Emu, September 30, 2008, Office Of Public Information
Focus Emu, September 30, 2008, Office Of Public Information
Focus EMU
No abstract provided.
Focus Emu, March 25, 2008, Office Of Public Information
Focus Emu, March 25, 2008, Office Of Public Information
Focus EMU
No abstract provided.
Focus Emu, March 11, 2008, Office Of Public Information
Focus Emu, March 11, 2008, Office Of Public Information
Focus EMU
No abstract provided.
Focus Emu, January 15, 2008, Office Of Public Information
Focus Emu, January 15, 2008, Office Of Public Information
Focus EMU
No abstract provided.
Focus Emu, December 2, 2008, Office Of Public Information
Focus Emu, December 2, 2008, Office Of Public Information
Focus EMU
No abstract provided.
Winter Commencement, December 14, 2008, Eastern Michigan University
Winter Commencement, December 14, 2008, Eastern Michigan University
Commencement Programs and Materials
No abstract provided.
Spring Commencement, April 27, 2008, Eastern Michigan University
Spring Commencement, April 27, 2008, Eastern Michigan University
Commencement Programs and Materials
No abstract provided.
Pm Ceremonial Script, April 27, 2008, Eastern Michigan University
Pm Ceremonial Script, April 27, 2008, Eastern Michigan University
Commencement Programs and Materials
No abstract provided.
Am Ceremonial Script, April 27, 2008, Eastern Michigan University
Am Ceremonial Script, April 27, 2008, Eastern Michigan University
Commencement Programs and Materials
No abstract provided.