The Coming Millennium: Enduring Issues Confronting Catholic Health Care

Professor Singer and Ms. Johnson Lantz provide a cogent overview of Catholic health care in the United States and address the key issues affecting Catholic health care in the coming years. In particular, (1) clarity in canonical and ethical interpretation; (2) industry consolidation; and (3) next generation sponsorship and the impact of these issues are discussed in detaiL The authors conclude that successful Catholic health care organizations must maintain strong mission and business fundamentals in an increasingly competitive reimbursement and regulatory environment

High Pressure Cyclic Triaxial Tests

Shear modulus and damping from high pressure (up to 500 psi) cyclic triaxial tests of soils are presented. The test results are compared with published models where low confining pressures were used. The apparatus and test setup for the high pressure tests are also discussed

Medium development strategies and scale down models for a high density high productivity cell line

Medium Development at Regeneron continues to enhance fed batch culture productivity. These efforts have been enabled through the development of high throughput scale down models in shake flasks and the ambr® 250. Design of Experiment (DOE) approaches have been applied to optimize the operating conditions in the small scale models leading to performance for growth and titer that match benchtop bioreactor with no off-set. The development of these representative scale down models and our approach to medium development will be described. A medium development case study will be presented from a recent Regeneron fed batch process with a cell line achieving high cell densities and depleting the culture of key amino acids. The traditional medium development approach of supplementing the culture with the depleted nutrients was unsuccessful: high amino acid consumption rates required large amounts of amino acids resulting in significantly increased culture osmolality and reduced productivity. Leveraging high throughput culture systems and multifactor DOEs, multiple medium composition factors in combination were rapidly evaluated. Mathematical models relating medium input factors to process outputs are generated that allow for process optimization. Using this approach, a new feeding strategy was developed that limits increases in osmolality and yields titers approaching 10g/L in both the scale down systems and a process that has been implemented for clinical scale manufacturing of a monoclonal antibody

Who should we hire?: Examining coaching succession in NCAA Division I women’s basketball

The purpose of this study was to evaluate the performance of newly hired coaches in relation to their predecessors, and utilize the analysis to provide guidance to decision makers in college athletic departments. This study examined 185 coaching changes in Division I women’s basketball in 16 conferences between 2000 and 2009. Data were collected from online sources including institutional websites, media guides, and media articles. Latent class analysis was employed to reduce the data to one item per factor. Factors included demographics, coaching ability, coaching experience, past team performance, hiring factors (coaching level change, inside/outside hire, interim, conference affiliation), and institutional factors (public/private, demographic market area, enrollment, budget, and National Association of Collegiate Directors of Athletics standings). Mixed models analysis was performed to identify which categories have a relationship with changes in the number of wins following a coaching change. Results suggest that past team performance was the strongest indicator of future performance after a coaching change

Theology, News and Notes - Vol. 56, No. 02

Theology News & Notes was a theological journal published by Fuller Theological Seminary from 1954 through 2014.https://digitalcommons.fuller.edu/tnn/1165/thumbnail.jp

TECHNOLOGY-BASED FINANCIAL SERVICES DELIVERY AND CUSTOMER SATISFACTION: A STUDY OF THE NIGERIAN BANKING SECTOR

This study was designed to identify the extent to which technology has impacted customer satisfaction in the Nigerian banking sector. Data analysis was based on responses obtained from 120 customers of three Deposit Money Banks within Ogun and Lagos States of Nigeria. Features of bank service evaluated in the study are time saving, convenience, crime reduction, reliability, risk reduction, and ease of use. The result showed significant positive impact of all the above service features on customer satisfaction, an indication that electronic-based banking has enhanced customer satisfaction in Nigeria. It is recommended that more service points and user-friendly customer-oriented financial products be provided to support this initiative

Hydrogeology and Geochemistry of Glacial Deposits in Northeastern Kansas

Twelve counties (Atchison, Brown, Doniphan, Douglas, Jackson, Jefferson, Johnson, Leavenworth, Nemaha, Shawnee, Wabaunsee, and Wyandotte) in northeastern Kansas were glaciated during the Pleistocene Epoch. The glacial deposits consist of till, fluvial, loess, and lacustrine deposits locally totalling thicknesses of 400 ft (120 m). A major buried valley 3 mi (5 km) wide, 400 ft (120 m) deep, and 75 mi (120 km) long trends eastward across southern Nemaha, northern Jackson, and central Atchison counties. Several smaller tributary valleys can be identified in Atchison, Nemaha, Brown, Jackson, and Jefferson counties. Other buried valleys generally trend southward to the Kansas River valley or northward into Nebraska and Missouri. The glacial deposits filling the buried valleys locally are clayey. However, most valleys contain at least some water-bearing sand and gravel. Wells drilled into the best water-bearing sand and gravel deposits may yield as much as 900 gallons per minute (gpm; 0.06 m3/sm3/s), but less than 500 gpm (0.03 m3/s) is more common. The alluvial deposits of the Kansas and Missouri river valleys are the major sources of ground water in northeastern Kansas. Wells in these aquifers may have yields of 5,000 gpm (0.3 m3/s), but yields are more commonly less than 3,000 gpm (0.2 m3/s). We analyzed data from 80 pump tests using computer programs to find the best fit for transmissivity (1) and storage (S) values on glacial, alluvial, and bedrock aquifers. Transmissivities in the Missouri River valley alluvium ranged from 200,000 gallons per day per foot (gpd/ft) to 600,000 gpd/ft (2,000-7,000 m2/d), and storage values were between 0.001 and 0.0004. Tests in the Kansas River valley alluvium indicated transmissivities in the range 50,000-600,000 gpd/ft (600-7,000 m2/d) and storage values of 0.03. In the main buried valley across northeastern Kansas, the glacial deposits had T and S values of 2,500-25,600 gpd/ft (31.0-318 m2/d) and 0.00002-0.002, respectively. In the smaller buried valleys the glacial deposits had T values ranging from 1,500 gpd/ft to 100,000 gpd/ft (19-1,200 m2/d). Because of increasing population size in northeastern Kansas, appropriations of water for public and industrial water supplies have been increasing. Most of the pumpage comes from wells in the Kansas and Missouri river valleys. However, in 1981 the Division of Water Resources reported allocations of 1,466 acre-ft of water from wells tapping glacial aquifers associated with the main buried channel across Nemaha, Jackson, and Atchison counties and an additional 837 acre-ft from tributaries associated with the main buried channel. Nemaha County has the largest appropriation of water from the glacial aquifer (1,549 acre-ft/yr in 1983), and Wyandotte County has the largest appropriation of water from the alluvial aquifers (54,250 acre-ft/yr in 1983). Shawnee County has the largest number of ground-water appropriation rights (217). In 1981, for the 12-county study area, the Division of Water Resources found that 773 wells have ground-water appropriation rights. These 773 wells have appropriation rights for 140,484 acre-ft of water from alluvial aquifers, 5,290 acre-ft from glacial aquifers, and 2,146 acre-ft from Pennsylvanian and Permian rock aquifers. Maps for each county show the depth to bedrock, total thickness of Pleistocene sand and gravel deposits, estimated yield of wells, depth to water in wells and test holes, and the saturated thickness of Pleistocene deposits. A bedrock topographic map for the twelve counties was prepared from outcrop data and information from more than 5,000 water well, oil and gas, and test-hole logs. Ground waters from alluvial deposits are hard calcium bicarbonate waters that may have iron concentrations of several milligrams per liter. Sand and gravel associated with the glacial deposits generally yield hard calcium bicarbonate waters and may contain appreciable amounts of iron, manganese, sulfate, and chloride locally. Nitrate concentrations above 45 mg/L are noted in a number of wells of varying depth and aquifer source

Hydrogeology and Geochemistry of Glacial Deposits in Northeastern Kansas

Twelve counties (Atchison, Brown, Doniphan, Douglas, Jackson, Jefferson, Johnson, Leavenworth, Nemaha, Shawnee, Wabaunsee, and Wyandotte) in northeastern Kansas were glaciated during the Pleistocene Epoch. The glacial deposits consist of till, fluvial, loess, and lacustrine deposits locally totalling thicknesses of 400 ft (120 m). A major buried valley 3 mi (5 km) wide, 400 ft (120 m) deep, and 75 mi (120 km) long trends eastward across southern Nemaha, northern Jackson, and central Atchison counties. Several smaller tributary valleys can be identified in Atchison, Nemaha, Brown, Jackson, and Jefferson counties. Other buried valleys generally trend southward to the Kansas River valley or northward into Nebraska and Missouri. The glacial deposits filling the buried valleys locally are clayey. However, most valleys contain at least some water-bearing sand and gravel. Wells drilled into the best water-bearing sand and gravel deposits may yield as much as 900 gallons per minute (gpm; 0.06 m3/sm3/s), but less than 500 gpm (0.03 m3/s) is more common. The alluvial deposits of the Kansas and Missouri river valleys are the major sources of ground water in northeastern Kansas. Wells in these aquifers may have yields of 5,000 gpm (0.3 m3/s), but yields are more commonly less than 3,000 gpm (0.2 m3/s). We analyzed data from 80 pump tests using computer programs to find the best fit for transmissivity (1) and storage (S) values on glacial, alluvial, and bedrock aquifers. Transmissivities in the Missouri River valley alluvium ranged from 200,000 gallons per day per foot (gpd/ft) to 600,000 gpd/ft (2,000-7,000 m2/d), and storage values were between 0.001 and 0.0004. Tests in the Kansas River valley alluvium indicated transmissivities in the range 50,000-600,000 gpd/ft (600-7,000 m2/d) and storage values of 0.03. In the main buried valley across northeastern Kansas, the glacial deposits had T and S values of 2,500-25,600 gpd/ft (31.0-318 m2/d) and 0.00002-0.002, respectively. In the smaller buried valleys the glacial deposits had T values ranging from 1,500 gpd/ft to 100,000 gpd/ft (19-1,200 m2/d). Because of increasing population size in northeastern Kansas, appropriations of water for public and industrial water supplies have been increasing. Most of the pumpage comes from wells in the Kansas and Missouri river valleys. However, in 1981 the Division of Water Resources reported allocations of 1,466 acre-ft of water from wells tapping glacial aquifers associated with the main buried channel across Nemaha, Jackson, and Atchison counties and an additional 837 acre-ft from tributaries associated with the main buried channel. Nemaha County has the largest appropriation of water from the glacial aquifer (1,549 acre-ft/yr in 1983), and Wyandotte County has the largest appropriation of water from the alluvial aquifers (54,250 acre-ft/yr in 1983). Shawnee County has the largest number of ground-water appropriation rights (217). In 1981, for the 12-county study area, the Division of Water Resources found that 773 wells have ground-water appropriation rights. These 773 wells have appropriation rights for 140,484 acre-ft of water from alluvial aquifers, 5,290 acre-ft from glacial aquifers, and 2,146 acre-ft from Pennsylvanian and Permian rock aquifers. Maps for each county show the depth to bedrock, total thickness of Pleistocene sand and gravel deposits, estimated yield of wells, depth to water in wells and test holes, and the saturated thickness of Pleistocene deposits. A bedrock topographic map for the twelve counties was prepared from outcrop data and information from more than 5,000 water well, oil and gas, and test-hole logs. Ground waters from alluvial deposits are hard calcium bicarbonate waters that may have iron concentrations of several milligrams per liter. Sand and gravel associated with the glacial deposits generally yield hard calcium bicarbonate waters and may contain appreciable amounts of iron, manganese, sulfate, and chloride locally. Nitrate concentrations above 45 mg/L are noted in a number of wells of varying depth and aquifer source

A Post-Succession Analysis of Factors Influencing Coaching Success in NCAA Division I Men’s Basketball – Journal of Issues in Intercollegiate Athletics

Based on the reciprocal determinism component of social learning theory, a total of 736 men’s NCAA Division I basketball coaching changes between 1999 and 2014 were examined to establish which factors were related to conference success following a coaching change. Results from an exploratory latent class analysis indicated that many demographic, environmental, and experiential variables assumed to be important in hiring a new coach are insignificant. However, a program’s previous success, individual coaching ability, and previous coach vacancy circumstance are all significantly related to conference winning differential after a coaching change. Results also indicated a regression to the mean occurs after most coaching changes except for the most elite programs. Pragmatically, however, findings show relatively small increments in winning or losing following a coaching change, suggesting that the impact of a coach is often overstated. Stakeholders can use this information to evaluate coaches, programs, and hiring practices in men’s Division I basketball