Alien Registration- Newman, Lavina S. (Gorham, Cumberland County)

https://digitalmaine.com/alien_docs/31669/thumbnail.jp

Perbedaan Efektivitas Zeolit Dan Manganese Greensand Untuk Menurunkan Kadar Fosfat Dan Chemical Oxygen Demand Limbah Cair “Laundry Zone” Di Tembalang

Laundry business is a business in clothes washing services. Preliminary test results show that the levels of phosphate and COD laundry liquid wastes is 12,36 mg/l and 5.920 mg/l. These levels exceeded the water quality standard of waste that phosphate concentration of 2 mg/l and COD concentration of 100 mg/l. This research aimed to determine the difference effectiveness of zeolite and manganese greensand to decrease phosphate and chemical oxygen demand on waste "laundry zone" in Tembalang. This research uses Quasi-Experimental with pretest - posttest design. The sample used is wastewater from the washing machine outlet of "laundry Zone". Analysis data used to test hypothesis is by one way anova test with 95% significance level. Research result show that phosphate levels before treatment is 12,36 mg/l and COD levels is 5.920 mg/l. After treatment with zeolite and manganese greensand in diameter 0,25 mm, 0,5 mm, 0,75 mm and 1 mm showed that the levels of phosphate and COD decreased. From one way anova got the difference at significant of α = 0,05 decreased levels of phosphate and COD after media zeolite by p-value = 0,001, the difference at significant of α = 0,05 decreased levels of phosphate and COD after media manganese greensand by p-value = 0,01, and the difference at significant of α = 0,05 decreased levels of phosphate and COD after media zeolit and manganese greensand by p-value = 0,0001. Effectiveness of the highest decline in phosphate and COD reached 73,30 % dan 71,68% occurred in treatment with zeolite diameter of 0,25 mm

Estratigrafía de alta resolución de depósitos de flujos gravitacionales de la Formación Los Molles (Grupo Cuyo - Jurásico) en la región de La Jardinera, cuenca Neuquina

El Grupo Cuyo en el área del arroyo La Jardinera (Pliensbachiano a Caloviano Temprano) refleja una fisiografía de cuenca de plataforma y talud. Una discordancia de orden mayor define la culminación de una espesa sucesión de turbiditas y representa un límite de secuencia de 2do orden. La más antigua secuencia de 2do orden comprende el tramo basal de la Formación Los Molles e incluye un ciclo transgresivo-regresivo asignado a estratos de base de talud y fondo de cuenca. La secuencia más joven, que incluye el resto del Grupo Cuyo, consiste de una sucesión regresiva puntuada por varios desplazamientos abruptos de elementos fisiográficos (límites de secuencia de 3er orden). Las secuencias depositacionales de 3er orden incluyen depósitos de talud y de base de talud del Aaleniano de la Formación Los Molles, facies de plataforma del Bajociano Temprano en la transición entre las formaciones Los Molles y Lajas, y sedimentitas de plataforma interna a nearshore del Bajociano medio a tardío de la Formación Lajas, que es a su vez cubierta por depósitos del Bathoniano aluvial de la Formación Challacó. Ciclos de más alta frecuencia alternan en la sucesión y han controlado el origen, depositación y abandono de los elementos arquitecturales. Análisis de facies y de elementos arquitecturales indican que los depósitos gravitatorios densos de la Formación Los Molles encuadran en un modelo de rampa submarina. Los tres tipos de flujos gravitacionales (GF) han sido relacionados a caídas del nivel del mar de 4to orden. Los GF1 fueron asignados a flujos hiperpícnicos producidos durante un cortejo temprano de mar bajo de 4to orden, coevo con incisión fluvial en la plataforma, que evolucionaran a flujos turbidíticos en el talud, produciendo cargas de pulsos depositacionales cuya signatura composicional es fluvial. El sistema de GF1 incluye canales relativamente pequeños sobre el talud, lóbulos bien desarrollados en la base del talud y la planicie de fondo de cuenca proximales, así como lóbulos adventicios en la planicie del fondo de cuenca. Los estratos GF2 fueron asignados a flujos hiperpícnicos influenciados por un componente oscilatorio y relacionados a cortejos tardíos de mar bajo de 4to orden, que también incluyen relleno de canales incididos. Ellos están caracterizados en el talud por areniscas onduladas y laminadas ampliamente distribuidas y facies heterolíticas, que incluyen scours de bajo relieve en sus porciones centrales. Ellos representan flujos densos más diluidos y de grano más fino con respecto a los GF1. Los GF3, también asociados con cuñas de mar bajo de 4to orden, comprenden depósitos de flujos en masa y debris de talud y de base de talud, que representan clásicos surges de corta duración causados por debilidades en taludes relativamente abruptos. Los cortejos transgresivos y de mar alto de 4to orden llevaron al abandono de la etapa turbidítica y extensiva depositación de fango.The Pliensbachian to Early Callovian Cuyo Group in the Arroyo La Jardinera area reflects a shelf-slope-basin plain physiography. A major unconformity defines the onset of a thick turbidite succession and represents a 2nd order sequence boundary. The older 2nd order depositional sequence comprises the base of Los Molles Formation and includes a transgressive-regressive cycle ascribed to basin plain and slope rise strata. The younger one, which includes the rest of the Cuyo Group, consists of a regressive succession punctuated by several abrupt shifts of physiographic elements (3rd order sequence boundaries). The 3rd order depositional sequences include Aalenian slope rise and slope deposits in the Los Molles Formation, Early Bajocian shelfal facies at the transition of the Los Molles and Lajas formations, and Middle to Late Bajocian inner shelf to nearshore strata in the Lajas Formation that are overlain by Bathonian alluvial deposits of the Challacó Formation. Higher frequency cycles punctuate the succession and have controlled the origin, deposition and abandonment of the architectural elements. Facies and architectural elements analyses indicate that gravity flow deposits in the Los Molles Formation fit in a submarine ramp model. The three identified gravity flow (GF) types have been related to 4th order relative sea-level falls. The GF1 was ascribed to hyperpycnal flows produced during 4th order early lowstand, coeval to fluvial incision on the shelf, which were ignited in the slope and produced depletive depositional pulses with a fluvial compositional signature. The GF1 system includes relatively small channels in the slope, well-developed lobes in the slope rise and proximal basin plain, and lobe fringes in the basin plain. The GF2 strata were ascribed to hyperpycnal flows influenced by an oscillatory component and related to the 4th order late lowstand systems tract that also includes the incised channels fill. They are characterized in the slope by widespread, undulating and laminated sandstone and heterolithic facies, which include low relief scours at their central portions. They represent more diluted and finer-grained density flows relative to the GF1. The GF3, also associated with the 4th order lowstand wedge, comprises mass and debris flow deposits in the slope and slope rise that represent classical, short-lived surges caused by slope failures on relatively steep slopes. The 4th order transgressive and highstand systems tracts led to the abandonment of the turbidite stages and widespread mud deposition.Fil: Paim, Paulo S. G.. Universidad de Vale do Rio dos Sinos; BrasilFil: Silveira, Ariane. Universidad de Vale do Rio dos Sinos; BrasilFil: Lavina, Ernesto L. C.. Universidad de Vale do Rio dos Sinos; BrasilFil: Faccini, Ubiratan F.. Universidad de Vale do Rio dos Sinos; BrasilFil: Leanza, Hector Armando. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina. Universidad Nacional de La Plata; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; ArgentinaFil: Teixeira de Oliveira, J. M. M.. Universidad de Vale do Rio dos Sinos; BrasilFil: D'Avila, Roberto S. F.. Universidad de Vale do Rio dos Sinos; Brasil. Petrobras Argentina S.a; Argentin

EUROnu-WP6 2010 Report

This is a summary of the work done by the Working Package 6 (Physics) of the EU project "EUROnu" during the second year of activity of the project.Comment: 82 pages, 51 eps figure

Study of the eightfold degeneracy with a standard β\beta-Beam and a Super-Beam facility

The study of the eightfold degeneracy at a neutrino complex that includes a standard $\beta$-Beam and a Super-Beam facility is presented for the first time in this paper. The scenario where the neutrinos are sent toward a Megaton water Cerenkov detector located at the Fr\'{e}jus laboratory (baseline 130 Km) is exploited. The performance in terms of sensitivity for measuring the continuous ($\theta_{13}$ and $\delta$) and discrete (${sign} [ \Delta m^2_{23} ]$ and ${sign} [\tan (2\theta_{23}) ]$) oscillation parameters for the $\beta$-Beam and Super-Beam alone, and for their combination has been studied. A brief review of the present uncertainties on the neutrino and antineutrino cross-sections is also reported and their impact on the discovery potential discussed

A Beta Beam complex based on the machine upgrades for the LHC

The Beta Beam CERN design is based on the present LHC injection complex and its physics reach is mainly limited by the maximum rigidity of the SPS. In fact, some of the scenarios for the machine upgrades of the LHC, particularly the construction of a fast cycling 1 TeV injector (``Super-SPS''), are very synergic with the construction of a higher $\gamma$ Beta Beam. At the energies that can be reached by this machine, we demonstrate that dense calorimeters can already be used for the detection of $\nu$ at the far location. Even at moderate masses (40 kton) as the ones imposed by the use of existing underground halls at Gran Sasso, the CP reach is very large for any value of $\theta_{13}$ that would provide evidence of $\nu_e$ appearance at T2K or NO$\nu$A ($\theta_{13}\geq 3^\circ$). Exploitation of matter effects at the CERN to Gran Sasso distance provides sensitivity to the neutrino mass hierarchy in significant areas of the $\theta_{13}-\delta$ plane