HYDROGEOLOGY OF THE THERMAL LANDSLIDE

The large Thermal Landslide overlies the initial area of geothermal development at The Geysers. The landslide is waterbearing while the underlying Franciscan formation bedrock units are essentially non-waterbearing except where affected by hydrothermal alteration. Perched ground water moving through the landslide is heated prior to discharge as spring flow

Periodic boundary conditions in a 3D hydro code

We have modified a 3D hydrodynamics code so that it has the capability to impose periodic boundary conditions on the problem being considered. This capability allows it to treat only a basic symmetry unit of the problem when translational or rotational periodic symmetries are present. The code has been run successfully for two test problems involving rotational symmetries

Senate \u27libelously\u27 labeled by Campus

Letter to the editor of The Maine Campus. We feel it necessary to take issue with your recent editorial, entitled, Elected Cowardice. The seven authors of the letter express support for the decision made by the University Senate to deny finding to the Wilde-Stein club and vow, ...if they successfully obtain travel funds, we intend to approach the senate with the idea of one of our classmates and form a Happy Hetero Club, and [ask] for funds to travel [to] prime chick locations

Hugoniots of aerogels involving carbon and resorcinol formaldehyde

Recently, a first-order phase transition is predicted in liquid carbon using atomistic simulation and Brenner's bond order potential. There are also experimental data suggesting a possibility for a first-order phase transition. In light of this, a thermochemical equilibrium code (CHEQ) is used to provide guidance to experiments to find a liquid-liquid phase change in carbon foam and carbon-rich aerogel, resorcinol formaldehyde. Isotherms and Hugoniots were computed based on the previous analysis by van Thiel and Ree. The present calculations predict the liquid-liquid-graphite triple point to be at 5000 K and 5.2 GPa and its critical point to be at 6000 K and 8.8 GPa. The present Hugoniot calculations suggest that the liquid-liquid phase transition may be detected by performing a shock experiment with initial density of approximately 0.15 gm/cm{sup 3}