The EU and Bosnia and Herzegovina: Democracy promotion within the limits of the "ethnic conflict" paradigm

Seeking to contribute to the emerging debate about the substance of EU democracy promotion policies, this paper takes as its focus Bosnia and Herzegovina, where the EU‟s current democracy promotion efforts are primarily focused on reform of the country‟s constitution. Bosnia‟s current constitution, established by the 1995 Dayton Agreement, provides for consociational power-sharing and extensive territorial decentralisation. While EU officials have stressed the inadequacies of the present constitutional arrangements, over time the reforms demanded have become more limited in scope. As such, I suggest that the outcome of any successful constitutional reform negotiations will be technical fixes to the present constitution, allowing the country to meet the obligations of future EU membership, rather than its wholesale redesign. Rather than promoting liberal democracy as it has elsewhere, then, in Bosnia the EU supports the perpetuation of consociational structures, which EU officials regard as the most realistic option given the country‟s post-conflict political context. Faced with the lack of a constitutional norm within the Union, let alone a consociational one, EU policy-makers have instead chosen to refer to a particular reading of the history of the European integration project itself in order to lend support to their approach in Bosnia, which continues to privilege group over individual rights. I highlight how notions of a „union of diversity‟ or a „union of minorities‟ are used to legitimise an approach to democracy promotion that is predicated on a view of Bosnia as composed of a patchwork of ethnic groups with discrete and discernable interests and identities

The effect of varying sea coal fineness on sea coal activity in molding sands

An experiment was conducted in an attempt to establish a relation between sea coal activity in a facing sand and the particle size of the sea coal added to the sand. It was felt that if a sufficient difference in distribution of volatiles was detected, a correlation between particle size and activity of the sea coal within the test specimens might be established. The lack of positive evidence to support such a relationship is indicative that a variation in particle size does not promote volatile re-deposition within the range of particle sizes investigated for the particular weight per cent of sea coal added --Abstract, page [ii]

Design of a building and stack for a power plant

Thesis (BS)--University of Illinois, 1913Typescript and m

A High-Resolution Airborne Color-Infrared Camera Water Mask for the NASA ABoVE Campaign

The airborne AirSWOT instrument suite, consisting of an interferometric Ka-band synthetic aperture radar and color-infrared (CIR) camera, was deployed to northern North America in July and August 2017 as part of the NASA Arctic-Boreal Vulnerability Experiment (ABoVE). We present validated, open (i.e., vegetation-free) surface water masks produced from high-resolution (1 m), co-registered AirSWOT CIR imagery using a semi-automated, object-based water classification. The imagery and resulting high-resolution water masks are available as open-access datasets and support interpretation of AirSWOT radar and other coincident ABoVE image products, including LVIS, UAVSAR, AIRMOSS, AVIRIS-NG, and CFIS. These synergies offer promising potential for multi-sensor analysis of Arctic-Boreal surface water bodies. In total, 3167 km2 of open surface water were mapped from 23,380 km2 of flight lines spanning 23 degrees of latitude and broad environmental gradients. Detected water body sizes range from 0.00004 km2 (40 m2) to 15 km2. Power-law extrapolations are commonly used to estimate the abundance of small lakes from coarser resolution imagery, and our mapped water bodies followed power-law distributions, but only for water bodies greater than 0.34 (±0.13) km2 in area. For water bodies exceeding this size threshold, the coefficients of power-law fits vary for different Arctic-Boreal physiographic terrains (wetland, prairie pothole, lowland river valley, thermokarst, and Canadian Shield). Thus, direct mapping using high-resolution imagery remains the most accurate way to estimate the abundance of small surface water bodies. We conclude that empirical scaling relationships, useful for estimating total trace gas exchange and aquatic habitats on Arctic-Boreal landscapes, are uniquely enabled by high-resolution AirSWOT-like mappings and automated detection methods such as those developed here