Bringing Anglo-governmentality into public management scholarship : the case of evidence-based medicine in UK health care

The field of public administration and management exhibits a limited number of favored themes and theories, including influential New Public Management and Network Governance accounts of contemporary government. Can additional social science–based perspectives enrich its theoretical base, in particular, analyzing a long-term shift to indirect governance evident in the field? We suggest that a variant of Foucauldian analysis is helpful, namely “Anglo-governmentality.” Having reviewed the literatures, we apply this Anglo-governmentality perspective to two case studies of “post hierarchical” UK health care settings: first, the National Institute for Health and Clinical Excellence (NICE), responsible for producing evidence-based guidelines nationally, and the second, a local network tasked with enacting such guidelines into practice. Compared with the Network Governance narrative, the Anglo-governmentality perspective distinctively highlights (a) a power–knowledge nexus giving strong technical advice; (b) pervasive grey sciences, which produce such evidence-based guidelines; (c) the “subjectification” of local governing agents, herein analyzed using Foucauldian concepts of the “technology of the self” and “pastoral power”; and (d) the continuing indirect steering role of the advanced neoliberal health care State. We add to Anglo-governmentality literature by highlighting hybrid “grey sciences,” which include clinical elements and energetic self-directed clinical–managerial hybrids as local governing agents. These findings suggest that the State and segments of the medical profession form a loose ensemble and that professionals retain scope for colonizing these new arenas. We finally suggest that Anglo-governmentality theory warrants further exploration within knowledge-based public organizations

Geochemistry and Stable Isotopes of Surface Water and Groundwater in the Continental Pit in Butte, Montana, USA

The Continental porphyry Cu‐Mo mine, located 2 km east of the famous Berkeley Pit lake of Butte, Montana, contains two small lakes that vary in size depending on mining activity. In contrast to the acidic Berkeley Pit lake, the Continental Pit waters have near-neutral pH and relatively low metal concentrations. The main reason is geological: whereas the Berkeley Pit mined highly‐altered granite rich in pyrite with no neutralizing potential, the Continental Pit is mining weakly‐altered granite with lower pyrite concentrations and up to 1‐2% hydrothermal calcite. The purpose of this study was to gather and interpret information that bears on the chemistry of surface water and groundwater in the active Continental Pit. Pre‐existing chemistry data from sampling of the Continental Pit were compiled from the Montana Bureau of Mines and Geology and Montana Department of Environmental Quality records. In addition, in March of 2013, new water samples were collected from the mine’s main dewatering well, the Sarsfield well, and a nearby acidic seep (Pavilion Seep) and analyzed for trace metals and several stable isotopes, including dD and d18O of water, d13C of dissolved inorganic carbon, and d34S of dissolved sulfate. In December 2013, several soil samples were collected from the shore of the frozen pit lake and surrounding area. The soil samples were analyzed using X‐ray diffraction to determine mineral content. Based on Visual Minteq modeling, water in the Continental Pit lake is near equilibrium with a number of carbonate, sulfate, and molybdate minerals, including calcite, dolomite, rhodochrosite (MnCO3), brochantite (CuSO4·3Cu(OH)2), malachite (Cu2CO3(OH)2), hydrozincite (Zn5(CO3)2(OH)6), gypsum, and powellite (CaMoO4). The fact that these minerals are close to equilibrium suggests that they are present on the weathered mine walls and/or in the sediment of the surface water ponds. X‐Ray Diffraction (XRD) analysis of the pond “beach” sample failed to show any discrete metal‐bearing phases. One of the soil samples collected higher in the mine, near an area of active weathering of chalcocite‐rich ore, contained over 50% chalcanthite (CuSO4·5H2O). This water‐soluble copper salt is easily dissolved in water, and is probably a major source of copper to the pond and underlying groundwater system. However, concentrations of copper in the latter are probably controlled by other, less‐soluble minerals, such as brochantite or malachite. Although the acidity of the Pavilion Seep is high (~ 11 meq/L), the flow is much less than the Sarsfield Well at the current time. Thus, the pH, major and minor element chemistry in the Continental Pit lakes are buffered by calcite and other carbonate minerals. For the Continental Pit waters to become acidic, the influx of acidic seepage (e.g., Pavilion Seep) would need to increase substantially over its present volume

Studying Invasive Species Using GIS

Students will search GIS databases for information. (Guided by the teacher modeling the method and the sites, using a Smartboard or LCD projector.) Students will use the information gathered from GIS data sites to create a GIS map. (Guided by the teacher modeling the methods needed to use the program, using a Smartboard or LCD projector.) Students will interpret the data from the map to determine relationships between invasive species and biotic or abiotic factors in the surrounding environment. Students will answer questions about the data they collected

Exploring Energy, Motion and Forces with Interactive Physics

Students will use the Interactive Physics program to create a simple machine. Students will create a lever and a ball that will fall onto it and changed the direction of the force