The Climate of Opinion in Illinois 2008- 2016: Roots of Gridlock

Since January 1, 2015, Illinois has been frozen in a governmental and political gridlock that has dominated the state’s political discourse, consumed the energies of all involved, and created chaos in governmental and non-profit agencies that normally deliver state services. It has also created untold hardship and suffering among those who are most dependent on state services. The conflict has especially threatened to drastically reduce the quality and missions of the institutions of public higher education in Illinois, a state system that was widely recognized as one of the best in the nation and the world

Hydrogeology and Hydrochemistry of the Falls City Uranium Mine Tailings Remedial Action Project, Karnes County, Texas

Oxidized uranium ore deposits were discovered in the Deweesville sandstone (also referred to as the Stones Switch; Bunker and MacKallor [1973]) in the Falls City region in the 1950s. Uranium was mined and milled in the small community of Deweesville by Susquehanna-Western, Inc. (SWI) from April 1961 to August 1973. Tailings composed of sediment residue from the sulfuric acid milling process and residual sulfuric acid solutions were disposed of in six ponds on the outcrop of the Deweesville, within the mined-out uranium pits in the Deweesville, and on the outcrop of the Conquista, creating a set of large tailings impoundments (figs. 1.1 and 1.2). From 1978 to 1982 Solution Engineering, Inc. (SEI) conducted a secondary recovery of the remaining uranium in the tailings piles by in situ leaching. In 1984, the ponds on top of two of the tailings piles were spray evaporated and a clay cap was placed over the piles to prevent additional percolation of water through the piles and into the underlying aquifers. Acidic tailings solutions have been recharging the underlying aquifers since initial tailings disposal and may still be leaking into these aquifers. Several hydrogeologic investigations have been conducted to assess whether there has been groundwater contamination from the tailings. Early studies were conducted by Turk, Kehle and Associates (1976), and Ford, Bacon & Davis Utah (1978, 1981). Each of these studies included only minor investigations of the hydrogeology and hydrochemistry of the site and, in general, underestimated the extent of contamination from the site. Investigations conducted by the U.S. Department of Energy (DOE) from 1985 to 1991 have since revealed the true extent of contamination (U.S. Department of Energy, 1991).Bureau of Economic Geolog

Gravitational Lenses With More Than Four Images: I. Classification of Caustics

We study the problem of gravitational lensing by an isothermal elliptical density galaxy in the presence of a tidal perturbation. When the perturbation is fairly strong and oriented near the galaxy's minor axis, the lens can produce image configurations with six or even eight highly magnified images lying approximately on a circle. We classify the caustic structures in the model and identify the range of models that can produce such lenses. Sextuple and octuple lenses are likely to be rare because they require special lens configurations, but a full calculation of the likelihood will have to include both the existence of lenses with multiple lens galaxies and the strong magnification bias that affects sextuple and octuple lenses. At optical wavelengths these lenses would probably appear as partial or complete Einstein rings, but at radio wavelengths the individual images could probably be resolved.Comment: 30 pages, including 12 postscript figures; accepted for publication in Ap

Hydrogeologic Characterization of the Saline Aquifers, East Texas Basin- Implications to Nuclear Waste Storage in East Texas salt Domes

Groundwaters in the deep aquifers (Nacatoch to Travis Peak) range in salinity from 20,000 to over 200,000 mg/L. Based on their isotopic compositions, they were originally recharged as continental meteoric waters. Recharge probably occurred predominantly during the Cretaceous time; therefore, the waters are very old. Because the basin has not been uplifted, there are no extensive recharge or discharge zones. The flanks of domes and radial faults associated with domes may function as localized discharge points. Both the water chemistry and the hydraulic pressures for the aquifers suggest that the basin can be subdivided into two major aquifer systems: (1) the upper Cretaceous aquifers (Woodbine and shallower) which are hydrostatic and (2) the deep lower Cretaceous and deeper formations (Glen Rose, Travis Peak, and older units), which are slightly overpressured. The source of sodium and chloride in the saline waters is considered to be from salt dome dissolution. Most of the dissolution occurred during the Cretaceous. Chlorine-36 analyses suggest that dome solution is not presently occurring. Salinity cross sections across individual domes do not indicate that ongoing solution is an important process. The major chemical reactions in the saline aquifers are dome dissolution, albitization, and dedolomitization. Albitization and dedolomitization are important only in the deeper formations. The high Na concentrations in the deeper aquifer system result in the alteration of plagioclase to albite and the release of Ca into solution. The increase in Ca concentrations causes a shift in the calcite/dolomite equilibrium. The increase in Mg results from dissolution of dolomite.Bureau of Economic Geolog

A response to “Likelihood ratio as weight of evidence: a closer look” by Lund and Iyer

Recently, Lund and Iyer (L&I) raised an argument regarding the use of likelihood ratios in court. In our view, their argument is based on a lack of understanding of the paradigm. L&I argue that the decision maker should not accept the expert’s likelihood ratio without further consideration. This is agreed by all parties. In normal practice, there is often considerable and proper exploration in court of the basis for any probabilistic statement. We conclude that L&I argue against a practice that does not exist and which no one advocates. Further we conclude that the most informative summary of evidential weight is the likelihood ratio. We state that this is the summary that should be presented to a court in every scientific assessment of evidential weight with supporting information about how it was constructed and on what it was based

Panel. Community Engagement and Interpreting Slavery in North Mississippi

The “Behind the Big House” Project / Jodi Skipper, University of Mississippi and Suzanne DavidsonBehind the Big House is a slave dwelling interpretation program in Holly Springs, Mississippi. The program offers a counter-narrative to the Holly Springs Annual Pilgrimage Tour of Historic Homes and Churches, the city’s main tourist attraction which has historically neglected the contributions of enslaved persons. Behind the Big House was initiated by several private property owners who understood that interpreting the structures which housed enslaved persons could help to remedy such omissions. In addition to discussing how historical memory impacts the functions of these sites in the present, Skipper will discuss her role as a Behind the Big House tour guide, and how she incorporates the tour as an applied component in her courses. Slavery and Its Descendants / W. Ralph Eubanks, University of MississippiThe legacy of slavery and its impact across generations of African Americans is often ignored or overlooked, particularly by institutions that benefited from enslaved labor. The University of Mississippi is no exception. Payment records from the 1840s in the archives of the University of Mississippi indicate that Robert Sheegog—who once owned Faulkner’s home Rowan Oak—along with other local slave owners, loaned slaves to the University. This connection between the slaves of Rowan Oak and the building of the University of Mississippi holds the potential to redefine the idea of legacy connections to the University, since inevitably the descendants of several of those slaves are among the university’s alumni. This paper will discuss the on-going work of the University of Mississippi’s slavery research group and the possible outcomes of planned genealogical research to find the descendants of the slaves from Faulkner’s Rowan Oak who built the university.The University of Mississippi Slavery Research Group / Jeffrey Jackson and Charles K. Ross, University of MississippiIn this presentation, we present the story of the University of Mississippi Slavery Research Group focusing on its origins and the various factors that led to its formation. We highlight some of the groups’ most significant recent efforts to better understand how antebellum slavery shaped the formation of the University of Mississippi and life in North Mississippi generally and we discuss some of our initial projects and initiatives that seek to remember, memorialize and interpret the lives of enslaved people for our students, our local community, and our nation.Interpreting Slavery at Burns Belfry and Rowan Oak / George McDaniel, Burns-Belfry African American History MuseumCaroline Barr was a foundational figure in the life of William Faulkner. As he called her, “Mammy Callie,” she had worked for the Falkner family since he was a young boy. Her house and her story demand a further interpretation beyond the gates of Rowan Oak. Using her as a point of departure, this talk will explore African American history within the larger context of the town of Oxford. It will also look at the ways in which that history is being interpreted today and how that interpretation can be improved through building connections between different historical sites. This connectivity allows for a deeper understanding of African American history in Oxford and the world in which Faulkner lived and wrote