Aproximaciones al estudio de la interacción individuo-paisaje a modo de evocacion comunicativa intrapersonal (2a. parte)

El análisis de la interacción individuo-paisaje presenta numerosas perspectivas de estudio vinculadas a la generación e interpretación de simbolismos e imaginarios. La capacidad significante y/o de evocación comunicativa del paisaje encuentra, en la comunicación intrapersonal, una argumentación relevante en el proceso de construcción de un aparato teórico que permita estudiar el proceso de apropiación y vivencia del paisaje en términos de manifestación comunicativa. El despliegue de un aparato teórico que permita interpretar el mensaje del paisaje así como descodificar su discurso intangible, representa el objetivo principal de la investigación que se presenta a continuación.

Aproximaciones al estudio de la interacción individuo-paisaje a modo de evocación comunicativa intrapersonal (1a. parte)

El análisis de la interacción individuo-paisaje presenta numerosas perspectivas de estudio vinculadas a la generación e interpretación de simbolismos e imaginarios. La capacidad significante y/o de evocación comunicativa del paisaje encuentra, en la comunicación intrapersonal, una argumentación relevante en el proceso de construcción de un aparato teórico que permita estudiar el proceso de apropiación y vivencia del paisaje en términos de manifestación comunicativa. El despliegue de un aparato teórico que permita interpretar el mensaje del paisaje así como descodificar su discurso intangible, representa el objetivo principal de la investigación que se presenta a continuación.

Metallogenic model of the Trepca Pb-Zn-Ag skarn deposit, Kosovo: Evidence from fluid inclusions, Rare Earth Elements, and stable isotope data

The Trepca Pb-Zn-Ag skarn deposit (29 Mt of ore at 3.45% Pb, 2.30% Zn, and 80 g/t Ag) is located in the Kopaonik block of the western Vardar zone, Kosovo. The mineralization, hosted by recrystallized limestone of Upper Triassic age, was structurally and lithologically controlled. Ore deposition is spatially and temporally related with the postcollisional magmatism of Oligocene age (23-26 Ma). The deposit was formed during two distinct mineralization stages: an early prograde closed-system and a later retrograde open-system stage. The prograde mineralization consisting mainly of pyroxenes (Hd(54-100)Jo(0-45)Di(0-45)) resulted from the interaction of magmatic fluids associated with Oligocene (23-26 Ma) postcollisional magmatism. Whereas there is no direct contact between magmatic rocks and the mineralization, the deposit is classified as a distal Pb-Zn-Ag skarn. Abundant pyroxene reflects low oxygen fugacity (<10(-31) bar) and anhydrous environment. Fluid inclusion data and mineral assemblage limit the prograde stage within a temperature range between 390 degrees and 475 degrees C. Formation pressure is estimated below 900 bars. Isotopic composition of aqueous fluid, inclusions hosted by hedenbergite (delta D = -108 to -130 parts per thousand; delta O-18 = 7.5-8.0 parts per thousand), Mn-enriched mineralogy and high REE content of the host carbonates at the contact with the skarn mineralization suggest that a magmatic fluid was modified during its infiltration through the country rocks. The retrograde mineral assemblage comprises ilvaite, magnetite, arsenopyrite, pyrrhotite, marcasite, pyrite, quartz, and various carbonates. Increases in oxygen and sulfur fugacities, as well as a hydrous character of mineralization, require an open-system model. The opening of the system is related to phreatomagmatic explosion and formation of the breccia. Arsenopyrite geothermometer limits the retrograde stage within the temperature range between 350 degrees and 380 degrees C and sulfur fugacity between 10(-8.8) and 10(-7.2) bars. The principal ore minerals, galena, sphalerite, pyrite, and minor chalcopyrite, were deposited from a moderately saline Ca-Na chloride fluid at around 350 degrees C. According to the isotopic composition of fluid inclusions hosted by sphalerite (delta D = -55 to -74 parts per thousand; delta O-18 = -9.6 to -13.6 parts per thousand), the fluid responsible for ore deposition was dominantly meteoric in origin. The delta S-31 values of the sulfides spanning between -5.5 and +10 parts per thousand point to a magmatic origin of sulfur. Ore deposition appears to have been largely contemporaneous with the retrograde stage of the skarn development. Postore stage accompanied the precipitation of significant amount of carbonates including the travertine deposits at the deposit surface. Mineralogical composition of travertine varies from calcite to siderite and all carbonates contain significant amounts of Mn. Decreased formation temperature and depletion in the REE content point to an influence of pH-neutralized cold ground water and dying magmatic system.

Origin of siderite mineralisation in Petrova and Trgovska Gora Mts., NW Dinarides

The Petrova and Trgovska Gora Mts. (Gora=Mountain) are Variscan basement units incorporated into the northwestern Dinarides during the Alpine orogeny. They host numerous siderite-quartz-polysulphide, siderite-chalcopyrite, siderite-galena and barite veins, as well as stratabound hydrothermal-replacement ankerite bodies within carbonates in non-metamorphosed, flysch-like Permo-Carboniferous sequences. The deposits have been mined for Cu, Pb, Ag and Fe ores since Medieval times. Fluid inclusion studies of quartz from siderite-polysulphide-quartz and barite veins of both regions have shown the presence of primary aqueous NaCl-CaCl(2)+/- MgCl(2)-H(2)O +/- CO(2) inclusions. The quartz-sulphide stage of both regions show variable salinities; 2.7-26.2 wt% NaCl eq. for the Trgovska Gora region and 3.4-23.4 wt% NaCl eq. for the Petrova gora region, and similar homogenisation temperatures (100-230A degrees C). Finally, barite is precipitated from low salinity-low temperature solutions (3.7-15.8 wt % NaCl equ. and 115-145A degrees C). P-t conditions estimated via isochore construction yield formation temperatures between 180-250A degrees C for the quartz-sulphide stage and 160-180A degrees C for the barite stage, using a maximum lithostatic pressure of 1 kbar (cc. 3 km of overburden). The sulphur isotope composition of barite from both deposits indicates the involvement of Permian seawater in ore fluids. This is supported by the elevated bromium content of the fluid inclusion leachates (120-660 ppm in quartz, 420-960 ppm in barite) with respect to the seawater, indicating evaporated seawater as the major portion of the ore-forming fluids. Variable sulphur isotope compositions of galena, pyrite and chalcopyrite, between -3.2 and +2.7aEuro degrees, are interpreted as a product of incomplete thermal reduction of the Permian marine sulphate mixed with organically- and pyrite-bound sulphur from the host sedimentary rocks. Ore-forming fluids are interpreted as deep-circulating fluids derived primarily from evaporated Permian seawater and later modified by interaction with the Variscan basement rocks. (40)Ar/(39)Ar data of the detrital mica from the host rocks yielded the Variscan age overprinted by an Early Permian tectonothermal event dated at 266-274 Ma. These ages are interpreted as those reflecting hydrothermal activity correlated with an incipient intracontinental rifting in the Tethyan domain. Nevertheless, 75 Ma recorded at a fine-grained sericite sample from the alteration zone is interpreted as a result of later resetting of white mica during Campanian opening/closure of the Sava back arc in the neighbouring Sava suture zone (Ustaszewski et al. 2008).

Evidence for two different bonding mechanisms of Al on Si(111)

By means of the ab initio cluster-model approach, we present theoretical evidence for two different mechanisms of bonding of atomic Al to Si(111). On the atop site (T1) the interaction of atomic Al to Si(111) is characteristic of an ionic bond whereas interaction above the threefold eclipsed site (T4) leads to the formation of a typical covalent bond. Moreover, both sites have a similar interaction energy if electronic correlation effects are included. While the conclusions regarding the nature of the chemisorption bond in the two sites do not depend either on the cluster-model size, the kind of embedding hydrogen atoms used, or the quality of the wave function (Hartree-Fock or configuration interaction), the chemisorption energy depends strongly on the wave function used. In fact, inclusion of correlation energy is necessary to properly describe the interaction energies.

Functional interaction between peroxisome proliferator-activated receptors-alpha and Mef-2C on human carnitine palmitoyltransferase 1beta (CPT1beta) gene activation

Muscle-type carnitine palmitoyltransferase 1 (CPT1β) is considered to be the gene that controls fatty acid mitochondrial β-oxidation. A functional peroxisome proliferator-activated receptor (PPAR) responsive element (PPRE) and a myocite-specific (MEF2) site that binds MEF2A and MEF2C in the promoter of this gene had been previously identified. We investigated the roles of the PPRE and the MEF2 binding sites and the potential interaction between PPARα and MEF2C regulating the CPT1β gene promoter. Mutation analysis indicated that the MEF2 site contributed to the activation of the CPT1β promoter by PPAR in C2C12 cells. The reporter construct containing the PPRE and the MEF2C site was synergistically activated by co-expression of PPAR, retinoid X receptor (RXR) and MEF2C in non-muscle cells. Moreover, protein-binding assays demonstrated that MEF2C and PPAR specifically bound to one another in vitro. Also for the synergistic activation of the CPT1β gene promoter by MEF2C and PPARα-RXRα, a precise arrangement of its binding sites was essential.

Investigation of interaction between native and impurity defects in ZnSe

Zinc selenide is a prospective material for optoelectronics. The fabrication of ZnSe­based light-emitting diodes is hindered by complexity of p-type doping of the component materials. The interaction between native and impurity defects, the tendency of doping impurity to form associative centres with native defects and the tendency to self-compensation are the main factors impeding effective control of the value and type of conductivity. The thesis is devoted to the study of the processes of interaction between native and impurity defects in zinc selenide. It is established that the Au impurity has the most prominent amphoteric properties in ZnSe among Cu, Ag and Au impurities, as it forms a great number of both Au; donors and Auz„ acceptors. Electrical measurements show that Ag and Au ions introduced into vacant sites of the Zn sublattice form simple single-charged Agz„+ and Auzn+ states with d1° electron configuration, while Cu ions can form both single-charged Cuz„ (d1) and double-charged Cuzr`+ (d`o) centres. Amphoteric properties of Ag and Au transition metals stimulated by time are found for the first time from both electrical and luminescent measurements. A model that explains the changes in electrical and luminescent parameters by displacement of Ag ions into interstitial sites due to lattice deformation forces is proposed. Formation of an Ag;-donor impurity band in ZnSe samples doped with Ag and stored at room temperature is also studied. Thus, the properties of the doped samples are modified due to large lattice relaxation during aging. This fact should be taken into account in optoelectronic applications of doped ZnSe and related compounds.

Isótopos estables aplicados al estudio de los sistemas paleoagrícolas mediterráneos

El origen y progresivo desarrollo de la agricultura es probablemente el primer ejemplo de interacción recíproca a gran escala entre la humanidad y el medio ambiente. Por tanto, reconstruir las condiciones ambientales que caracterizaron la adopción de la agricultura es de gran interés de cara a conocer sus causas potenciales, así como para comprender los efectos a largo plazo de la economía agrícola sobre el ambiente. En este trabajo presentamos la metodología desarrollada por nuestro equipo para reconstruir las condiciones climáticas y de cultivo en la agricultura primitiva, basada en el análisis de la composición isotópica de carbono (enriquecimiento en 13C) y nitrógeno (enriquecimiento en 15N) en restos vegetales recuperados de yacimientos arqueológicos. El análisis de 13C en cariópsides de cereales carbonizadas ha permitido cuantificar la disponibilidad hídrica de los cultivos en diversos yacimientos de la Península Ibérica y el Creciente Fértil, así como estimar su rendimiento en el pasado, mientras que el análisis de 15N, nos aporta información cualitativa sobre las condiciones nutricionales. Por otro lado, el análisis de 13C en restos forestales (carbones) ha permitido cuantificar las condiciones climáticas (precipitación y déficit hídrico) en los mismos yacimientos, aportando así información sobre el marco climático en el que se desarrollaron los cultivos.

Usabilidad en sitios web orientados al comercio electrónico y a los servicios: www.renfe.com

Este trabajo evalúa la usabilidad de la web de Renfe, comparándola con sitios de características similares, particularmente en Francia y Alemania. Para este análisis se efectúa un test de usuario con personas enmarcadas dentro de las características de los usuarios potenciales.

Social network extraction and analysis based on multimodal dyadic interaction

Social interactions are a very important component in people"s lives. Social network analysis has become a common technique used to model and quantify the properties of social interactions. In this paper, we propose an integrated framework to explore the characteristics of a social network extracted from multimodal dyadic interactions. For our study, we used a set of videos belonging to New York Times" Blogging Heads opinion blog. The Social Network is represented as an oriented graph, whose directed links are determined by the Influence Model. The links" weights are a measure of the"influence" a person has over the other. The states of the Influence Model encode automatically extracted audio/visual features from our videos using state-of-the art algorithms. Our results are reported in terms of accuracy of audio/visual data fusion for speaker segmentation and centrality measures used to characterize the extracted social network.

Aproximaciones al estudio de la interacción individuo-paisaje a modo de evocacion comunicativa intrapersonal (2a. parte)

El análisis de la interacción individuo-paisaje presenta numerosas perspectivas de estudio vinculadas a la generación e interpretación de simbolismos e imaginarios. La capacidad significante y/o de evocación comunicativa del paisaje encuentra, en la comunicación intrapersonal, una argumentación relevante en el proceso de construcción de un aparato teórico que permita estudiar el proceso de apropiación y vivencia del paisaje en términos de manifestación comunicativa. El despliegue de un aparato teórico que permita interpretar el mensaje del paisaje así como descodificar su discurso intangible, representa el objetivo principal de la investigación que se presenta a continuación.

Aproximaciones al estudio de la interacción individuo-paisaje a modo de evocación comunicativa intrapersonal (1a. parte)

The analysis of the individual-landscape interaction presents different perspectives of study related to the generation and interpretation of symbolisms and imaginary. The significant capability and/or of communicative evocation of the landscape finds, in the intrapersonal communication, a relevant argumentation in the process of construction of a theoretical device. This question allows to study the process of appropriation and experience of the landscape in terms of communicative action. The development of a theoretical device that allows to interpret the message of the landscape as well as to decode its intangible speech, represents the main aim of the research that appears next.

Moderate-Vigorous physical activity across Body Mass Index in females: moderating effect of endocannabinoids and temperament

Background: Endocannabinoids and temperament traits have been linked to both physical activity and body mass index (BMI) however no study has explored how these factors interact in females. The aims of this cross-sectional study were to 1) examine differences among distinct BMI groups on daytime physical activity and time spent in moderate-vigorous physical activity (MVPA), temperament traits and plasma endocannabinoid concentrations; and 2) explore the association and interaction between MVPA, temperament, endocannabinoids and BMI. Methods: Physical activity was measured with the wrist-worn accelerometer Actiwatch AW7, in a sample of 189 female participants (43 morbid obese, 30 obese, and 116 healthy-weight controls). The Temperament and Character Inventory-Revised questionnaire was used to assess personality traits. BMI was calculated by bioelectrical impedance analysis via the TANITA digital scale. Blood analyses were conducted to measure levels of endocannabinoids and endocannabinoid-related compounds. Path-analysis was performed to examine the association between predictive variables and MVPA. Results: Obese groups showed lower MVPA and dysfunctional temperament traits compared to healthy-weight controls. Plasma concentrations of 2-arachidonoylglyceryl (2-AG) were greater in obese groups. Path-analysis identified a direct effect between greater MVPA and low BMI (b = −0.13, p = .039) and high MVPA levels were associated with elevated anandamide (AEA) levels (b = 0.16, p = .049) and N-oleylethanolamide (OEA) levels (b = 0.22, p = .004), as well as high Novelty seeking (b = 0.18, p<.001) and low Harm avoidance (b = −0.16, p<.001). Conclusions: Obese individuals showed a distinct temperament profile and circulating endocannabinoids compared to controls. Temperament and endocannabinoids may act as moderators of the low MVPA in obesity.

Estudo da influência de adições de prata na resistividade elétrica da liga Cu-5%Al

Estudou-se a influência de adições de 2, 6 e 8% Ag, em peso, na resistividade elétrica da liga Cu-5%Al, utilizando-se o método dos quatro pontos e um sistema de registro contínuo de variação da resistividade elétrica com a temperatura. Os resultados obtidos indicaram que a resistividade elétrica da liga aumenta com o aumento da concentração de prata e que as inflexões observadas nas curvas de variação da resistividade com a temperatura de aquecimento podem ser atribuídas à solubilização da prata na matriz de Cu-Al. Observou-se também que a velocidade de aquecimento da amostra é um fator importante na intensidade e forma dos eventos observados.

Determinação das energias de ativação para nucleação de precipitados e difusão da prata na liga cu-2%al com adições de prata

As energias de ativação para nucleação de precipitados ricos em prata e de difusão da prata no cobre, em ligas de Cu-2%Al contendo 2, 4, 6, 8, 10 e 12%Ag, em peso, foram determinadas utilizando-se medidas de variação da microdureza com a temperatura e o tempo de envelhecimento. Os resultados indicaram que, com o método utilizado, é possível obter valores para as energias de ativação para nucleação da fase rica em prata e de difusão da prata no cobre bastante próximos daqueles citados na literatura.