136 research outputs found

    On Disjoint hypercubes in Fibonacci cubes

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    The {\em Fibonacci cube} of dimension nn, denoted as Γ_n\Gamma\_n, is the subgraph of nn-cube Q_nQ\_n induced by vertices with no consecutive 1's. We study the maximum number of disjoint subgraphs in Γ_n\Gamma\_n isomorphic to Q_kQ\_k, and denote this number by q_k(n)q\_k(n). We prove several recursive results for q_k(n)q\_k(n), in particular we prove that q_k(n)=q_k1(n2)+q_k(n3)q\_{k}(n) = q\_{k-1}(n-2) + q\_{k}(n-3). We also prove a closed formula in which q_k(n)q\_k(n) is given in terms of Fibonacci numbers, and finally we give the generating function for the sequence {q_k(n)}_n=0\{q\_{k}(n)\}\_{n=0}^{ \infty}

    Perceived Influence and Response of River Users to Invasive Bighead and Silver Carp in the Illinois River

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    Two United States federally injurious fishes, bighead(Hypophthalmichthys nobilis)and silver carp(H. molitrix),are established in the Mississippi River Basinand have the potential tocolonize the Laurentian Great Lakes. Given this imminentthreat, a critical need for stakeholders is an understanding ofthe potential social influences of this invasion oncommunities that rely upon the ecosystems bighead and silvercarp now inhabit; influences so far unstudied. Using intercept surveys (n= 469), we tested forthe potential social influencesof bighead and silvercarp in four river communities;three in which they haveestablishedpopulations(test, Illinois River, Illinois) and one in which they have not(control, Mississippi River, Iowa). Reported principal differences between test and control sites were observed for recreational fishing, aestheticappreciation of the river, and experience with bighead and silvercarp. Our exploratory results indicate that bighead and silvercarp may have a negative influence on river usage.Illinois Natural History Surveyunpublishednot peer reviewedOpe

    Maturation of the Vaca Muerta and Agrio Formations due to the emplacement of magmatic intrusive complexes in the southern Men-doza region of the Neuquén Basin

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    La existencia de complejos intrusivos en cuencas sedimentarias ha sido documentada en varias cuencas en distintas partes delmundo. Generalmente se emplazan en rocas ricas en materia orgánica, produciendo la maduración de la misma. Además, el emplazamientopuede generar vías de migración de fluidos, estructuras que pueden ser posibles trampas de hidrocarburos, y pueden serreservorios fracturados. Este trabajo se focalizará en el impacto térmico y la consecuente generación de hidrocarburos producidospor el emplazamiento de un complejo intrusivo. Para ello se escogió el sector surmendocino de la Cuenca Neuquina, dónde existengran cantidad de intrusiones ígneas emplazadas en las rocas generadoras del Grupo Mendoza (Formaciones Vaca Muerta y Agrio)y en sedimentitas continentales del Grupo Neuquén. Se realizó la identificación de intrusivos mediante datos de sísmica y pozos. Seconfeccionó una sección estructural de la zona de estudio, para luego realizar los modelos termales. Los resultados de las modelizacionesmuestran que el emplazamiento de intrusivos genera la maduración de las Formaciones Vaca Muerta y Agrio, especialmentedonde se produce una clusterización de los intrusivos. Éste efecto está regulado por la temperatura de la roca de caja al tiempo delemplazamiento, la edad del emplazamiento y el solapamiento de las intrusiones. Se concluye que en la región surmendocina de laCuenca Neuquina, las Formaciones Vaca Muerta y Agrio se encuentran maduradas por el impacto térmico de un complejo intrusivo,pudiendo llegar a generar cantidades considerables de hidrocarburos.The existence of intrusive-complexes in sedimentary basins has been documented in many basins all around the world. Generally, they are emplaced in organic rich rocks, producing their maturation. Also, the emplacement can generate fluid's migration conduits, structures that can be hydrocarbon traps, and fractured reservoirs. This paper will focus on the thermal impact and the consequent hydrocarbon generation produced by the emplacement of an intrusive-complex. For that aim, we have chosen the southern Mendoza area of the Neuquén Basin, where a great quantity of igneous intrusions are emplaced in the source rocks of the Mendoza Group (Vaca Muerta and Agrio Formations), and in continental sedimentites of the Neuquén Group. The identification of the intrusives was made based on seismic and borehole data. We produced a structural section of the study area, which was used afterwards to make the thermal models. The results of our modellings show that the emplacement of intrusives generates the maturation of the Vaca Muerta and Agrio Formations, especially where a clustering of the intrusions is produced. This effect is regulated by the temperature of the host rock at the time of emplacement, the age of the emplacement, and the clustering of intrusions. We conclude that in the southern Mendoza region of the Neuquén Basin, the Vaca Muerta and Agrio Formations were matured because of the thermal impact of an intrusive complex, being able to generate considerable amount of hydrocarbons.Fil: Spacapan, Juan Bautista. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”; Argentina. YPF - Tecnología; ArgentinaFil: Palma, Joaquín Octavio. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. YPF - Tecnología; ArgentinaFil: Rocha Vargas, Marcelo Emilio. YPF - Tecnología; ArgentinaFil: Leanza, Hector Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”; ArgentinaFil: D'Odorico, Alejandro. YPF - Tecnología; ArgentinaFil: Rojas Vera, Emilio Agustin. YPF - Tecnología; ArgentinaFil: Manceda, René Enrique. YPF - Tecnología; ArgentinaFil: Galland, Olivier. University of Oslo; NoruegaFil: Medialdea, Adrián. YPF - Tecnología; ArgentinaFil: Cattaneo, Diego Matias. YPF - Tecnología; Argentin
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