Biennial report /

Title from cover.

LLW : the Illinois approach : site identification plan and status report /

Cover title.

Statutes and regulations : (32 Illinois Administrative Code, chapter II) /

Cover title.

Environmental assessment : reference repository location, Hanford site, Washington.

"DOE/RW-0070."

Status report[s] on Clinch River Study.

UC-70

Environmental assessment, Davis Canyon Site, Utah.

At head of title: Nuclear Waste Policy Act (Section 112).

An Investigation of the destruction of ion exchange resins

Ion exchange resins are used for many purposes in various areas of science and commerce. One example is the use of cation exchange resins in the nuclear industry for the clean up of radioactively contaminated water (for example the removal of 137Cs). However, during removal of radionuclides, the resin itself becomes radioactively contaminated, and must be treated as Intermediate Level Waste. This radioactive contamination of the resin creates a disposal problem. Conventionally, there are two main avenues of disposal for industrial wastes, landfill burial or incineration. However, these are regarded as inappropriate for the disposal of the cation exchange resin involved in this project. Thus, a method involving the use of Fenton's Reagent (Hydrogen Peroxide/soluble Iron catalyst) to destroy the resin by wet oxidation has been developed. This process converts 95% of the solid resin to gaseous CO2, thus greatly reducing the volume of radioactive waste that has to be disposed of. However, hydrogen peroxide is an expensive reagent, and is a major component of the cost of any potential plant for the destruction of ion exchange resin. The aim of my project has been to discover a way of improving the efficiency of the destruction of the resin thus reducing the cost involved in the use of hydrogen peroxide. The work on this problem has been concentrated in two main areas:-1) Use of analytical techniques such as NMR and IR to follow the process of the hydrogen peroxide destruction of both resin beads and model systems such as water soluble calixarenes. 2) Use of various physical and chemical techniques in an attempt to improve the overall efficiency of hydrogen peroxide utilization. Examples of these techniques include UV irradiation, both with and without a photocatalyst, oxygen carrying molecules and various stirring regimes.

Experimental investigation of the fuel properties of glidfuel, palm oil mill effluent biodiesel and blends

Biofuels derived from industry waste have potential to substitute fossil fuels (Diesel and Gasoline) in internal combustion (IC) engines. Use of waste streams as fuels would help to reduce considerably life-cycle greenhouse gas emissions and minimise waste processing costs. In this study an investigation into the fuel properties of two waste derived biofuels were carried out, they are: (i) Glidfuel (GF) biofuel - a waste stream from paper industry, and (ii) Palm Oil Mill Effluent (POME) biodiesel - biodiesel produced from palm oil industry effluent through various treatment and transesterification process. GF and POME was mixed together at various proportions and separately with fossil diesel (FD) to assess the miscibility and various physical and chemical properties of the blends. Fuel properties such as kinematic viscosity, higher heating value, water content, acid number, density, flash point temperature, CHNO content, sulphur content, ash content, oxidation stability, cetane number and copper corrosion ratings of all the fuels were measured. The properties of GF, POME and various blends were compared with the corresponding properties of the standard FD. Significance of the fuel properties and their expected effects on combustion and exhaust emission characteristics of the IC engine were discussed. Results showed that most properties of both GF and POME biodiesel were comparable to FD. Both GF and POME were miscible with each other, and also separately with the FD. Flash point temperatures of GF and POME biodiesel were 40.7°C and 158.7°C respectively. The flash point temperature of GF was about 36% lower than corresponding FD. The water content in GF and FD were 0.74 (% wt) and 0.01 (% wt) respectively. Acidity values and corrosion ratings of both GF and POME biodiesel were low compared to corresponding value for FD. The study concluded that optimum GF-POME biofuel blends can substitute fossil diesel use in IC engines.

The Study of Sonar for Imaging of the Solid-Liquid Interface Inside Large Tanks

Retrieval, treatment, and disposal of high-level radioactive waste (HLW) is expected to cost between 100 and 300 billion dollars. The risk to workers, public health, and the environment are also a major area of concern for HLW. Visualization of the interface between settled solids and the optically opaque liquid is needed for retrieval of the waste from underground storage tanks. A Profiling sonar selected for this research generates 2-D image of the interface. Multiple experiments were performed to demonstrate the effectiveness of sonar in real-time monitoring the interface inside HLW tanks. First set of experiments demonstrated that objects shapes could be identified even when 30% of solids entrained in liquid, thereby mapping the interface. Simulation of sonar system validated these results. Second set of experiments confirmed the sonar’s ability in detecting the solids with density similar to the immersed liquid. Third set of experiments determined the affects of near by objects on image resolution. Final set of experiments proved the functional and chemical capabilities of sonar in caustic solution.

Data and Documentation

The primary aims of this survey were to assess household waste management practices; participation in waste diversion practices; knowledge of local waste management politics; willingness to participate in local decision making regarding the development of a local waste processing facility; attitudes and perceptions of waste, waste management policies, and waste management technologies.

Probleme und Risiken bei der geplanten Einlagerung radioaktiver Abfälle in einen nordwestdeutschen Salzstock

Der Plan, große Mengen radioaktiver Materialien in Salinar- gesteine von Salzstöcken einzulagern, schließt die Rück- holbarkeit praktisch aus. Bei der Abschätzung des Langzeitverhaltens der Gesteine, der Grubenbaue und des gesamten Diapirs sind - wie auch beim Einlagerungsvorgang selbst - Fehler nicht auszuschließen und nicht korrigierbar. Die Antragsteller behandeln die geowissenschaftlichen Aspekte der Einlagerung (Teilprojekt 6) nicht qualifiziert und widmen den damit verbundenen Problemen eine unangemessen geringe Aufmerksamkeit. Sie lassen die einem solchen Projekt adäquate planerische Sorgfalt vermissen, gehen mit den zur Verfügung stehenden Daten in ihrer Argumentation ungenau oder selektiv um und erwecken den Eindruck, unter der Erdoberfläche nach dem 'trial-and-error'-Prinzip Vorgehen zu wollen. Salzstöcke sind tektonisch grundsätzlich instabile Gesteinskörper. Die an ihrem Aufbau überwiegend beteiligten Gesteine sind die wasserlöslichsten der Erdkruste; sie reagieren am empfindlichsten auf mechanische und thermische Beanspruchung und sind am reaktionsfähigsten bei möglichen Interaktionen zwischen Einlagerungsmaterial und Einlagerungsmedium. Salzstöcke sind die auf bergtechnische Eingriffe am sensibelsten reagierenden Gesteinskörper, insbesondere, wenn der am Salzspiegel herrschende Lösungszustand gestört wird, wenn durch künstliche Hohlräume im Innern Kriechbewegung (Konvergenz) des gesamten Salinars ausgelöst wird und wenn mit der Einlagerung thermische Belastungen einhergehen, welche höher sind als die mit der Gesteinsbildung und -Umbildung verbundenen Temperaturen es jemals waren. Daß trotz dieser Empfindlichkeit Gewinnungsbergbau in Diapiren möglich ist, ist kein Beleg für ihre Eignung als Endlager. Die Geowissenschaften verfügen über Modellvorstellungen zur Deutung der Salinargenese, des Salzaufstiegs und des gebirgsmechanischen Verhaltens. Diese Modelle sind teils als 'Lehrbuchwahrheit1 allgemein akzeptiert, werden z.T. aber auch als Hypothesen kontrovers diskutiert. Langzeitprognosen über das Verhalten von Gesteinen sind nicht verläßlich, wenn sie auf widersprochenen Modellvorstellungen über das Wesen von Gesteinen und Gesteinsverhalten beruhen. Die Salzstockauswahl ging der geowissenschaftlichen Erkundung voraus. Die wenigen publizierten Daten zur regionalen Geologie lassen nicht auf einen bergbautechnisch besonders leicht zu beherrschenden Salzstock schließen. Die Lage des Diapirs im Verbreitungsgebiet wasserreicher quartärzeitlicher Rinnensysteme spricht genauso gegen die Standortwahl wie die zu erwartende komplizierte Interntektonik und die politisch bedingte Unerforschbarkeit der Gesamtstruktur Gorleben-Rambow. Als Fehlentscheidung ist die durch Landkäufe am Standort Gorleben vorweggenommene Auswahl des Fabrikgeländes einschließlich Schachtanlage und Tritiumwasser-Verpressung auf dem Salzstock zu werten. Der nicht auszuschließende "Störfall Wassereinbruch" kann sich über Tage auf die Standsicherheit der riesigen Gebäude und Lagerbecken zerstörerisch auswirken und so Kontamination der Umgebung verursachen. Geowissenschaftliche Gründe, Erfahrungen aus der Bergbaukunde und die Erwartung, daß man fehlerhaftes Handeln nicht ausschließen kann, führen den Verfasser zu der Überzeugung, daß die Endlagerung radioaktiver Abfälle im Salz nicht zu empfehlen und nicht zu verantworten ist.

Quantifizierung postholsteinzeitlicher Subrosionen am Salzstock Gorleben durch statistische Auswertung von Bohrergebnissen

The Gorleben salt dome is actually investigated for its suitability as a repository for radioactive waste. It is crossed by a subglacial drainage channel, formed during the Elsterian glaciation (Gorleben channel). Some units of its filling vary strongly in niveau and thickness. Lowest positions and/or largest thickness are found above the salt dome. This is interpreted as a result of subrosion during the Saalean glaciation. The rate can be calculated from niveau differences of sediments formed during the Holsteinian interglacial. However, their position might have been influenced by other factors also (relief of the channel bottom, glacial tectonics, settlement of underlying clay-rich sediments). Their relevance was estimated applying statistical techniques to niveau and thickness data from 79 drillings in the Gorleben channel. Two classes of drillings with features caused by either Saalean subrosion or sedimentary processes during the filling of the Gorleben channel can be distinguished by means of factor and discriminant analysis. This interpretation is supported by the results of classwise correlation and regression analysis. Effects of glacial tectonics on the position of Holsteinian sediments cannot be misunderstood as subrosional. The influence of the settlement of underlying clay sediments can be estimated quantitatively. Saalean subrosion rates calculated from niveau differences of Holsteinian sediments between both classes differ with respect to the method applied: maximum values are 0,83 or 0,96 mm/a, average values are 0,31 or 0,41 mm/a.