Status of highly enriched uranium processing capability at Building 9212 Oak Ridge Y-12 Plant.

"December 8, 1995."

Y-12 plant site - Oak Ridge, Tennessee.

Supt. of Docs. no.: E 1.20/2:0182

Problems of physics in the ion source /

"The Y-12 Plant of the Clinton Engineer Works was operated by the Tennessee Eastman Corporation under Contract No. W-7401-eng-23 from Januaury 1943 until May 4, 1947, at which time operations were taken over by Carbide and Carbon Chemicals Corporation for the U.S. Atomic Energy Commission under Contract No. W-7405-eng-26"--Page 2 of cover.

Microbiological characteristics in a zero-valent iron reactive barrier

Zero-valent iron (Fe0)-based permeable reactive barriertreatment has been generating great interest for passivegroundwater remediation, yet few studies have paid particularattention to the microbial activity and characteristics withinand in the vicinity of the Fe0-barrier matrix. The presentstudy was undertaken to evaluate the microbial population andcommunity composition in the reducing zone of influence byFe0 corrosion in the barrier at the Oak Ridge Y-12 Plantsite. Both phospholipid fatty acids and DNA analyses were usedto determine the total microbial population and microbialfunctional groups, including sulfate-reducing bacteria,denitrifying bacteria, and methanogens, in groundwater andsoil/iron core samples. A diverse microbial community wasidentified in the strongly reducing Fe0 environment despitea relatively high pH condition within the Fe0 barrier (up topH 10). In comparison with those found in the backgroundsoil/groundwater samples, the enhanced microbial populationranged from 1 to 3 orders of magnitude and appeared to increase from upgradient of the barrier to downgradient soil. Inaddition, microbial community composition appeared to change overtime, and the bacterial types of microorganismsincreased consistently as the barrier aged. DNA analysisindicated the presence of sulfate-reducing and denitrifyingbacteria in the barrier and its surrounding soil. However, theactivity of methanogens was found to be relatively low,presumably as a result of the competition by sulfate/metal-reducing bacteria and denitrifying bacteria because of the unlimited availability of sulfate and nitrate in the site groundwater. Results of this study provide evidenceof a diverse microbial population within and in the vicinity ofthe iron barrier, although the important roles of microbial activity, either beneficially or detrimentally, on the longevityand enduring efficiency of the Fe0 barriers are yet to be evaluated.

Distribution of Uranium and Thorium in Dolomitic Gravel Fill and Shale Saprolite

The objectives of this study were to examine (1) the distribution of U and Th in dolomitic gravel fill and shale saprolite, and (2) the removal of uranium from acidic groundwater by dolomitic gravel through precipitation with amorphous basaluminite at the U.S. DOE Oak Ridge Integrated Field Research Challenge (ORIFRC) field site west of the Oak Ridge Y-12 National Security Complex in East Tennessee. Media reactivity and sustainability are a technical concern with the deployment of any subsurface reactive media. Because the gravel was placed in the subsurface and exposed to contaminated groundwater for over 20 years, it provided a unique opportunity to study the solid and water phase geochemical conditions within the media after this length of exposure. This study illustrates that dolomite gravel can remove U from acidic contaminated groundwater with high levels of Al3+, Ca2+, NO3−, and SO42− over the long term. As the groundwater flows through high pH carbonate gravel, U containing amorphous basaluminite precipitates as the pH increases. This is due to an increase in groundwater pH from 3.2 to ∼6.5 as it comes in contact with the gravel. Therefore, carbonate gravel could be considered as a possible treatment medium for removal and sequestration of U and other pH sensitive metals from acidic contaminated groundwater. Thorium concentrations are also high in the carbonate gravel. Thorium generally shows an inverse relationship with U from the surface down into the deeper saprolite. Barite precipitated in the shallow saprolite directly below the dolomitic gravel from barium present in the acidic contaminated groundwater.

The acute radiation syndrome : a medical report on the Y-12 accident, June 16, 1958 /

"Contract No. AT(40-1)-Gen-33."

Performance evaluation of a zerovalent iron reactive barrier: Mineralogical characteristics

There is a limited amount of information about the effects of mineral precipitates and corrosion on the lifespan and long-term performance of in situ Fe° reactive barriers. The objectives of this paper are (1) to investigate mineral precipitates through an in situ permeable Fe° reactive barrier and (2) to examine the cementation and corrosion of Fe° filings in order to estimate the lifespan of this barrier. This field scale barrier (225' long x 2' wide x 31' deep) has been installed in order to remove uranium from contaminated groundwater at the Y-12 plant site, Oak Ridge, TN. According to XRD and SEM-EDX analysis of core samples recovered from the Fe° portion of the barrier, iron oxyhydroxides were found throughout, while aragonite, siderite, and FeS occurred predominantly in the shallow portion. Additionally, aragonite and FeS were present in up-gradient deeper zone where groundwater first enters the Fe° section of the barrier. After 15 months in the barrier, most of the Fe° filings in the core samples were loose, and a little corrosion of Fe° filings was observed in most of the barrier. However, larger amounts of corrosion (~10-150 µm thick corrosion rinds) occurred on cemented iron particles where groundwater first enters the barrier. Bicarbonate/ carbonate concentrations were high in this section of the barrier. Byproducts of this corrosion, iron oxyhydroxides, were the primary binding material in the cementation. Also, aragonite acted as a binding material to a lesser extent, while amorphous FeS occurred as coatings and infilings. Thin corrosion rinds (2-50 µm thick) were also found on the uncemented individual Fe° filings in the same area of the cementation. If corrosion continues, the estimated lifespan of Fe° filings in the more corroded sections is 5 to 10 years, while the Fe° filings in the rest of the barrier perhaps would last longer than 15 years. The mineral precipitates on the Fe° filing surfaces may hinder this corrosion but they may also decrease reactive surfaces. This research shows that precipitation will vary across a single reactive barrier and that greater corrosion and subsequent cementation of the filings may occur where groundwater first enters the Fe° section of the barrier.

Field observation of sequestration of uranium in iron-rich sediments under sequential reduction-oxidation conditions at the DOE Oak Ridge IFRC

At the U.S. DOE Oak Ridge Integrated Field Research Challenge (ORIFRC) site, the iron content of shallow subsurface materials (i.e. weathered saprolite) is relatively high (up to 5-6% as w/w), and therefore, the forms of the iron species present plays a critical role in the long-term sequestration of uranium. A long term pilot-scale study of the bioreduction and reoxidation of uranium conducted at the ORIFRC area 3 site, adjacent to the former S-3 disposal ponds (source zone), has provided us with the opportunity to study the impact of iron species on the sequestration of U(VI). The aqueous U(VI) concentrations at the site were decreased to below the EPA MCL through the intermittent injection of ethanol as the electron donor. Previous field tests indicated that both oxygen and nitrate could oxidize the bioreduced U(IV) and cause a short-term rebound of aqueous phase uranium concentration after the oxidative agents were delivered directly to the bioreduced zone.

A field test has been conducted to examine the long-term effect of exposure of bioreduced sediments to nitrate in contaminated groundwater for more than 1,380 days at the Area 3 site. Contaminated groundwater was allowed to invade the previously bioreduced zone via the natural groundwater gradient after an extended period in which reducing conditions were maintained and the bioreduced zone was protected from the influx of upgradient contaminated groundwater. The geochemical response to the invasion of contaminated groundwater was dependent on whether the monitoring location is in the middle or the fringe of the previously bioreduced zone. In general, the nitrate concentrations in the previously bioreduced area, increased gradually from near zero to ~50-300 mM within 200 days and then stabilized. The pH declined from bioreduced levels of 6.2-6.7 to below 5.0. Uranium concentrations rebounded in all monitoring wells but at different rates. At most locations U concentrations rebounded, declined and then rebounded again. Methane gas disappeared while a significant level (20,000 to 44,000 ppmv) N2O was found in the groundwater of monitoring wells after three years of reoxidization.

The U(IV) in sediments was mainly reoxidized to U(VI) species. Based on XANES analysis, the predominate uranium in all samples after re-oxidation was similar to a uranyl nitrate form. But the U content in the sediment remained as high as that determined after bioreduction activates were completed, indicating that much of the U is still sequestrated in situ. SEM observations of surged fine sediments revealed that clusters of colloidal-sized (200-500nm) U-containing precipitates appeared to have formed in situ, regardless from sample of FW106 in non-bioactivity control area or of pre-bioreduced FW101-2 and FW102-3. Additionally, SEM-EDS and microprobe analysis, showed that the U-containing precipitates (~1% U) in FW106 are notably higher in Fe, compared to the precipitates (~1-2.5% U) from FW101-2 and FW102-3. However, XRF analysis indicated that the U content was remained as high as 2180 and 1810 mg/kg with U/Fe ratio at 0.077 and 0.055 vs 0.037 g/g, respectively in pre-bioreduced FW101-2 and FW102-3, suggesting more U sequestrated by Fe in pre-bioreduced sediments.

Autoconcepto y calidad de vida en niños entre 8 y 12 años que concurren a los hogares de tránsito de la ciudad de Concepción del Uruguay, Entre Ríos

Resumen: La presente investigación, de tipo descriptiva-correlacional y transversal, se centró en conocer la relación que existe entre el autoconcepto y la calidad de vida de los niños entre 8 y 12 años que concurren a los hogares de tránsito, en la ciudad de Concepción del Uruguay, Entre Ríos. La muestra (no probabilística, intencional) estuvo conformada por 64 niños, de ambos sexos, 33 varones y 31 mujeres. Los mismos tenían entre 8 y 12 años. Los individuos evaluados eran asistentes a los hogares de tránsito mencionados anteriormente. Las técnicas de recolección de datos utilizadas fueron las siguientes: la Escala Verbal para Niños y Adolescentes del Autoconcepto de Martina Casullo, adaptación de Piers-Harris (1964) y el Cuestionario para Calidad de Vida Kidscreen-27. La Escala Verbal para Niños y Adolescentes del Autoconcepto (Casullo, 1990), cuenta con seis dimensiones: comportamiento, estatus intelectual y escolar, imagen corporal, sentimientos de ansiedad, percepciones acerca del reconocimiento que otros hacen de la propia conducta (popularidad) y bienestar y satisfacción personal. El cuestionario Kidscreen-27 (Quintero, Lugo, García, y Sánchez, 2011) consta de cinco dimensiones: actividad física y salud, estado de ánimo y sentimientos, vida familiar y tiempo libre, apoyo social y amigos, y entorno escolar. Los datos fueron recabados por medio de la concurrencia a ambos hogares, solicitando previamente las autorizaciones correspondientes a los directivos, como así también a los padres y/o tutores de los niños. Respecto a los procedimientos de análisis de los datos, se utilizó el programa estadístico informático SPSS (Statistical Package for the Social Sciences) versión 15.0 para Windows. Se realizó un análisis descriptivo de las dos variables principales de esta investigación (autoconcepto y calidad de vida) con el objetivo de conocer los niveles con que se presentan en niños. Además, para conocer la relación entre ambas variables, se llevó a cabo el análisis de correlación de Pearson. Para estudiar si existe diferencia en el autoconcepto y la calidad de vida en función del sexo de los niños, se realizó análisis multivariados de varianza (MANOVA). Los resultados obtenidos indicaron niveles elevados en la mayoría de las dimensiones de las variables estudiadas (autoconcepto y calidad de vida). En cuanto a las distinciones según el sexo en dichas variables, no se encontraron diferencias significativas, sólo una variación mínima en dos dimensiones del autoconcepto, donde se visualiza que el comportamiento social y la popularidad es más elevada en los niños que en las niñas.Se hallaron, por otro lado, correlaciones estadísticamente significativas en la mayoría de las dimensiones de ambas variables, las mismas son: entre comportamiento y actividad física/salud; entre comportamiento y apoyo social/amigos; entre comportamiento y entorno escolar; entre estatus intelectual/escolar y actividad física/salud; entre estatus intelectual/escolar y estado de ánimo/sentimientos; entre estatus intelectual/escolar y entorno escolar; entre imagen corporal con apoyo social/amigos; entre sentimientos de ansiedad y actividad física/salud; entre sentimientos de ansiedad y estado de ánimo/sentimientos; entre sentimientos de ansiedad y apoyo social/amigos; entre popularidad y estado de ánimo/sentimientos; entre popularidad y apoyo social/amigos; entre bienestar/satisfacción vital y actividad física/salud; entre bienestar/satisfacción vital y estado de ánimo/sentimientos; entre bienestar/satisfacción vital y apoyo social/amigos; entre bienestar/satisfacción vital y entorno escolar; entre el total global del autoconcepto y actividad física/salud; entre el total global del autoconcepto y estado de ánimo/sentimientos; entre el total global del autoconcepto y apoyo social/amigos; entre el total global del autoconcepto y entorno escolar. Sólo una dimensión de la calidad de vida no se relaciona con ninguna de las dimensiones del autoconcepto, a saber, vida familiar/tiempo libre. En lo que respecta a las conclusiones, puede considerarse que los resultados de esta investigación verifican que existe correlación entre el autoconcepto y la calidad de vida de los niños concurrentes a los hogares de tránsito Santa Clara de Asís y la Casa del Menor

imátgenes 10, 11 y 12

Fue el último en poseerla quien, instantes antes de perderla para siempre y movido por una presunción ya del todo instintiva, bautizó la ciudad con el nombre de Memoria grafiando esa palabra en las fachadas de las avenidas. Presumió que en un futuro, muy lejano quizá pero alcanzable, y a pesar de los trazos ya inseguros de su escritura afectada, alguien podría leerla y recobrar la lucidez.

Soil-Landscape relationships at the lower reaches of a watershed at Bear Creek near Oak Ridge, Tennessee

The watersheds at Bear Creek, Oak Ridge, TN, have similar soil–landscape relationships. The lower reaches of many of these watersheds consist of headwater riparian wetlands situated between sloping non-wetland upland zones. The objectives of this study are to examine the effects of (i) slope and geomorphic processes, (ii) human impacts, and (iii) particular characteristics of soils and saprolite that may effect drainage and water movement in the wetlands and adjacent landscapes in one of these watersheds. A transect was run from west to east in a hydrological monitored area at the lower reaches of a watershed on Bear Creek. This transect extended from a steep side slope position across a floodplain, a terrace, and a shoulder slope. On the upland positions of the Nolichucky Shale, mass wasting, overland flow and soil creep currently inhibit soil formation on the steep side slope position where a Typic Dystrudept is present, while soil stability on the shoulder slope has resulted in the formation of a well-developed Typic Hapludult. In these soils, argillic horizons occur above C horizons on less sloping gradients in comparison to steeper slopes, which have Bw horizons over Cr (saprolite) material. A riparian wetland area occupies the floodplain section, where a Typic Endoaquept is characterized by poorly drained conditions that led to the development of redoximorphic features (mottling), gleying, organic matter accumulation, and minimal development of subsurface horizons. A thin colluvial deposit overlies a thick well developed Aquic Hapludalf that formed in alluvial sediments on the terrace position. The colluvial deposit from the adjacent shoulder slope is thought to result from soil creep and anthropogenic erosion caused by past cultivation practices. Runoff from the adjacent sloping landscape and groundwater from the adjacent wetland area perhaps contribute to the somewhat poorly drained conditions of this profile. Perched watertables occur in upland positions due to dense saprolite and clay plugging in the shallow zones of the saprolite. However, no redoximorphic features are observed in the soil on the side slope due to high runoff. Remnants of the underlying shale saprolite, which occur as small discolored zones resembling mottles, are also present. The soils in the study have a CEC of