Climatic records over the past 30 ka from temperate Australia – a synthesis from the Oz-INTIMATE workgroup

Temperate Australia sits between the heat engine of the tropics and the cold Southern Ocean, encompassing a range of rainfall regimes and falling under the influence of different climatic drivers. Despite this heterogeneity, broad-scale trends in climatic and environmental change are evident over the past 30 ka. During the early glacial period (∼30–22 ka) and the Last Glacial Maximum (∼22–18 ka), climate was relatively cool across the entire temperate zone and there was an expansion of grasslands and increased fluvial activity in regionally important Murray–Darling Basin. The temperate region at this time appears to be dominated by expanded sea ice in the Southern Ocean forcing a northerly shift in the position of the oceanic fronts and a concomitant influx of cold water along the southeast (including Tasmania) and southwest Australian coasts. The deglacial period (∼18–12 ka) was characterised by glacial recession and eventual disappearance resulting from an increase in temperature deduced from terrestrial records, while there is some evidence for climatic reversals (e.g. the Antarctic Cold Reversal) in high resolution marine sediment cores through this period. The high spatial density of Holocene terrestrial records reveals an overall expansion of sclerophyll woodland and rainforest taxa across the temperate region after ∼12 ka, presumably in response to increasing temperature, while hydrological records reveal spatially heterogeneous hydro-climatic trends. Patterns after ∼6 ka suggest higher frequency climatic variability that possibly reflects the onset of large scale climate variability caused by the El Niño/Southern Oscillation.

Analysis and modelling of the hydraulic conductivity in aquitards : application to the Galilee Basin and the Great Artesian Basin, Australia

In large sedimentary basins with layers of different rocks, the groundwater flow between aquifers depends on the hydraulic conductivity (K) of the separating low-permeable rocks, or aquitards. Three methods were developed to evaluate K in aquitards for areas with limited field data: • Coherence and harmonic analysis: estimates the regional-scale K based on water-level fluctuations in adjacent aquifers. • Cokriging and Bayes' rule: infers K from downhole geophysical logs. • Fluvial process model: reproduces the lithology architecture of sediment formations which can be converted to K. These proposed methods enable good estimates of K and better planning of further drillholes.

Periglasiaalisten ilmiöiden alueellinen mallintaminen subarktisessa ympäristössä

Periglacial processes act on cold, non-glacial regions where the landscape deveploment is mainly controlled by frost activity. Circa 25 percent of Earth's surface can be considered as periglacial. Geographical Information System combined with advanced statistical modeling methods, provides an efficient tool and new theoretical perspective for study of cold environments. The aim of this study was to: 1) model and predict the abundance of periglacial phenomena in subarctic environment with statistical modeling, 2) investigate the most import factors affecting the occurence of these phenomena with hierarchical partitioning, 3) compare two widely used statistical modeling methods: Generalized Linear Models and Generalized Additive Models, 4) study modeling resolution's effect on prediction and 5) study how spatially continous prediction can be obtained from point data. The observational data of this study consist of 369 points that were collected during the summers of 2009 and 2010 at the study area in Kilpisjärvi northern Lapland. The periglacial phenomena of interest were cryoturbations, slope processes, weathering, deflation, nivation and fluvial processes. The features were modeled using Generalized Linear Models (GLM) and Generalized Additive Models (GAM) based on Poisson-errors. The abundance of periglacial features were predicted based on these models to a spatial grid with a resolution of one hectare. The most important environmental factors were examined with hierarchical partitioning. The effect of modeling resolution was investigated with in a small independent study area with a spatial resolution of 0,01 hectare. The models explained 45-70 % of the occurence of periglacial phenomena. When spatial variables were added to the models the amount of explained deviance was considerably higher, which signalled a geographical trend structure. The ability of the models to predict periglacial phenomena were assessed with independent evaluation data. Spearman's correlation varied 0,258 - 0,754 between the observed and predicted values. Based on explained deviance, and the results of hierarchical partitioning, the most important environmental variables were mean altitude, vegetation and mean slope angle. The effect of modeling resolution was clear, too coarse resolution caused a loss of information, while finer resolution brought out more localized variation. The models ability to explain and predict periglacial phenomena in the study area were mostly good and moderate respectively. Differences between modeling methods were small, although the explained deviance was higher with GLM-models than GAMs. In turn, GAMs produced more realistic spatial predictions. The single most important environmental variable controlling the occurence of periglacial phenomena was mean altitude, which had strong correlations with many other explanatory variables. The ongoing global warming will have great impact especially in cold environments on high latitudes, and for this reason, an important research topic in the near future will be the response of periglacial environments to a warming climate.

Tectono-geomorphic and environmental set-up deduced during deposition of Mio-Pleistocene sediments in NW Himalaya, India

Detailed pedofacies characterization along-with lithofacies investigations of the Mio-Pleistocene Siwalik sediments exposed in the Ramnagar sub-basin have been studied so as to elucidate variability in time and space of fluvial processes and the role of intra- and extra-basinal controls on fluvial sedimentation during the evolution of the Himalayan foreland basin (HFB). Dominance of multiple, moderately to strongly developed palaeosol assemblages during deposition of Lower Siwalik (similar to 12-10.8 Ma) sediments suggest that the HFB was marked by Upland set-up of Thomas et al. (2002). Activity of intra-basinal faults on the uplands and deposition of terminal fans at different times caused the development of multiple soils. Further, detailed pedofacies along-with lithofacies studies indicate prevalence of stable tectonic conditions and development of meandering streams with broad floodplains. However, the Middle Siwalik (similar to 10.8-4.92 Ma) sub-group is marked by multistoried sandstones and minor mudstone and mainly weakly developed palaeosols, indicating deposition by large braided rivers in the form of megafans in a Lowland set-up of Thomas et al. (2002). Significant change in nature and size of rivers from the Lower to Middle Siwalik at similar to 10 Ma is found almost throughout of the basin from Kohat Plateau (Pakistan) to Nepal because the Himalayan orogeny witnessed its greatest tectonic upheaval at this time leading to attainment of great heights by the Himalaya, intensification of the monsoon, development of large rivers systems and a high rate of sedimentation, hereby a major change from the Upland set-up to the Lowland set-up over major parts of the HFB. An interesting geomorphic environmental set-up prevailed in the Ramnagar sub-basin during deposition of the studied Upper Siwalik (similar to 4.92 to <1.68 Ma) sediments as observed from the degree of pedogenesis and the type of palaeosols. In general, the Upper Siwalik sub-group in the Ramnagar sub-basin is subdivided from bottom to top into the Purmandal sandstone (4.92-4.49 Ma), Nagrota (4.49-1.68 Ma) and Boulder Conglomerate (<1.68 Ma) formations on the basis of sedimentological characters and change in dominant lithology. Presence of mudstone, a few thin gravel beds and dominant sandstone lithology with weakly to moderately developed palaeosols in the Purmandal sandstone Fm. indicates deposition by shallow braided fluvial streams. The deposition of mudstone dominant Nagrota Fm. with moderately to some well developed palaeosols and a zone of gleyed palaeosols with laminated mudstones and thin sandstones took place in an environment marked by numerous small lakes, water-logged regions and small streams in an environment just south of the Piedmont zone, perhaps similar to what is happening presently in the Upland region/the Upper Gangetic plain. This area is locally called the `Trai region' (Pascoe, 1964). Deposition of Boulder Conglomerate Fm. took place by gravelly braided river system close to the Himalayan Ranges. Activity along the Main Boundary Fault led to progradation of these environments distal-ward and led to development of on the whole a coarsening upward sequence. (C) 2014 Elsevier B.V. All rights reserved.

Estrategias de muestreo para la determinación de las propiedades hidráulicas del suelo en dos unidades cartográficas

Cuando se usan los mapas de suelos para estimar las propiedades hidráulicas del suelo, éstos presentan diversas limitaciones debidas a varios factores, entre los cuales podemos citar, la falta de información a cerca de su variabilidad espacial a escala detallada (finca). En estos casos se hace necesario el muestreo adicional de estas propiedades para obtener una mejor estimación de su variabilidad espacial de cara la planificación y ejecución del riego. Con el objetivo de conocer los requerimientos de muestreo de la conductividad hidráulica saturada y la sorptividad (el horizonte Ap y sobre la superficie del suelo) fueron muestreadas dos unidades cartográficas de suelos a escala 1:25000 del área de influencia del canal Segarra-Garrigues, en Cataluña (NE de España) a través de un muestreo anidado. Los semivariogramas muestran un patrón de variabilidad acorde al tamaño modal de las fincas del área (a nivel de serie) con manejo homogéneo de la superficie del suelo. La sorptividad es la propiedad menos afectada por este factor (manejo del suelo). La distancia optima de muestreo y el número de muestras necesarias para obtener un buen resultado en la estimación de la Ks en el horizonte Ap es impracticable en ambas unidades. Para el resto de las propiedades la distancia de muestreo está dentro del tamaño modal de las fincas (100 m). Únicamente se puede obtener una buena estimación de la Ks y la sorptividad en el orden de magnitud del logaritmo de los datos obtenidos con un número de muestras considerablemente baja.

Evaluación de la producción de biogás y porcentaje de descontaminación de dos biodigestores tubulares plásticos alimentados con estiércol porcino y bovino en la Hacienda Santa Rosa, UNA-Managua

La presente investigación se efectuó en la Hacienda Santa Rosa Facultad de Ciencia Animal (FACA) de la Universidad Nacional Agraria (UNA-Managua) localizada en el Km 13 carretera norte, desvío a la comunidad de Sabana Grande, Managua, Nicaragua; ubicada a los 86º09'36'' longitud oeste y los 12º 08' 15''latitud norte con una altitud de 56 msnm con precipitación anual de 1,132.07 mm,temperatura anual de 27.08 ºC, una humedad relativa de 73.2%.La finalidad de esta investigación fue evaluar la producción de biogás en Biodigestores tubulares plásticos alimentados con estiércol porcino y bovino respectivamente y el porcentaje de descontaminación del efluente.Este estudio se inició en el mes de noviembre del año 2008 y finalizó en enero del 2009. Para este experimento se utilizaron dos Biodigestores tubulares plásticos, para instalarlos previamente se excavó una fosa en suelo firme tomando como dato un total de 20 cerdos distribuidos en dos corrales, los cuales tenían un peso entre 20 a 30 kg, y 10 bovinos con un peso promedio de 400 kg. Durante el desarrollo del experimento se midieron las variables. Cantidad de materia orgánica,Adición de agua, Producción de biogás,Producción de bioabono (efluente),eficiencia del sistema de reciclaje, temperatura del material en ambas cajas, oxígeno disuelto en el agua(DBO5) del material en caja de entrada y salida, pH del material. Para las variables producción de biogás, cantidad de estiércol y agua (afluente) y (efluente) producido se realizó una prueba de “tstudent” Una vez instalado los biodigestores, se iniciaron todas las mediciones dando seguimiento para determinar el tiempo de retención hidráulica.

Dessalinização de água do mar no litoral nordestino e influência da transposição de água na vazão do Rio São Francisco

Consultoria Legislativa - Área XI - Meio Ambiente e Direito Ambiental, Organização Territorial, Desenvolvimento Urbano e Regional.

La máquina de Marly

Duración (en horas): De 21 a 30 horas. Destinatario: Estudiante y Docente

De La navigation de l'Amazone : reponse a un memoire de M. Maury, officier de la marine des Etats-Unis

Pedro de Ângelis, militar e político italiano, nasceu em Nápolis, em 1784, e morreu em Buenos Aires, em 1854. Acompanhou o Rei Murat no exílio, após sua queda, e o preceptor de seus filhos. Retornou à Itália no regime constitucionalista, exilando-se novamente com o estabelecimento do absolutismo. A convite de Rivadavia, fixou-se em Buenos Aires, participando com destaque da política da República do Prata, contrária aos direitos do Brasil. Tornou-se, todavia, profundo conhecedor da história e da política da história e da política da América do Sul. De la navigation de l’Amazone, publicação em francês, editada em Montevidéu, segundo Borba de Moraes, “foi escrita a pedido do Governo brasileiro”, que foi o financiador da obra, em resposta aos planos de Maury para colonizar o Vale do Amazonas com afro-norte-americanos. “Apesar da sua parcialidade, a obra pode ser considerada valiosa contribuição para o conhecimento do Brasil”, como afirma Palau. Foi, também, publicada em espanhol, francês e português.

Spatial distribution of Chlorpyrifos and Endosulfan in USA coastal waters and the Great Lakes

Between 1994 and 1997, 258 tissue and 178 sediment samples were analyzed for chlorpyrifos throughout the coastal United States and the Great Lakes. Subsequently, 95 of the 1997 tissue samples were reanalyzed for endosulfan. Tissue chlorpyrifos concentrations, which exceeded the 90th percentile, were found in coastal regions known to have high agricultural use rates but also strongly correlated with sites near high population. The highest concentrations of endosulfans in contrast, were generally limited to agricultural regions of the country. Detections of chlorpyrifos at several Alaskan sites suggest an atmospheric transport mechanism. Many Great Lakes sites had chlorpyrifos tissue concentrations above the 90th percentile which decreased with increasing distance from the Corn Belt region (Iowa, Indiana, Illinois, and Wisconsin) where most agriculturally applied chlorpyrifos is used. Correlation analysis suggests that fluvial discharge is the primary transport pathway on the Atlantic and Gulf of Mexico coasts for chlorpyrifos but not necessarily for endosulfans. (PDF contains 28 pages)

Diário da Constituinte [gravação de vídeo] : [programa n. 716]

Trata da votação dos últimos pontos polêmicos das disposições transitórias. Foi votada a licença paternidade de cinco dias. A constituinte também aprovou o compromisso do Brasil de lutar pela instalação de um Tribunal Internacional dos Direitos Humanos. A última emenda aprovada suprimiu o artigo 23 das disposições transitórias. Ficou definido que as atuais empresas brasileiras, que fazem pesquisas e lavra de recursos minerais e de aproveitamento de potências de energia hidráulica, terão sua autorização quatro anos após a promulgação da nova Carta. Foi assegurado aos médicos a acumulação de dois cargos exercidos na Administração Pública Direta e Indireta

Um protesto : resposta ás pretenções da França a uma parte do Amazonas manifestadas por Mr. Deloncle

Dado de responsabilidade pesquisado no Lello Universal em 2 volumes, 19-? v. 2 p. 192.

Respuesta a la sequía de Pinus radiata D. Don y su implicación en los procesos de tolerancia

160 p. (Bibliogr. 141-160)

Diário da Constituinte [gravação de vídeo] : [programa n. 536]

Apenas empresas nacionais poderão explorar mineração em áreas de fronteiras, estratégicas e em territórios indígenas. Também foram discutidas outras emendas que propõem a nacionalização total do subsolo brasileiro serão decididas no voto. Lei complementar definirá as áreas estratégicas. Empresas nacionais terão preferência no transporte de cabotagem e no transporte marítimo internacional. O governo brasileiro deverá comprar navios nos estaleiros brasileiros. É função do Estado incentivar a organização dos garimpeiros em cooperativas. Lei Ordinária disporá sobre a política tarifária de serviços públicos. A seguir foi votada o artigo 205. Estabelece que jazidas, minas, recursos minerais e potenciais recursos energia hidráulica são propriedades da União.

Diário da Constituinte [gravação de vídeo] : [programa n. 462]

O líder do PMDB, senador Mário Covas reuniu hoje os vice-líderes do partido para repassar o acordo feito com o Centrão em torno do capítulo 2, do título 3. Este capítulo trata da competência e dos bens da União. Pertencem à União por exemplo, o mar territorial, os recursos minerais, lagos, ilhas e rios, além do subsolo e das terras indígenas. Pelo acordo, esse bens continuam de posse da União, que dará concessões à iniciativa privada para a sua exploração. Os recursos minerais e os recursos do subsolo são bens da União. Uma emenda que concede royalties aos estados e municípios pela exploração de petróleo, energia hidráulica e elétrica e gás natural em seus territórios foi aprovada. Foi aprovada também a emenda que suprimiu do texto do Centrão a expressão "posse imemorial das terras indígenas", para que o texto ficasse de acordo com a realidade brasileira.