Left to right: Oliva, Laura, and Damon at TS/Ph-1b, Taylor Slough

This material is based upon work supported by the National Science Foundation through the Florida Coastal Everglades Long-Term Ecological Research program under Cooperative Agreements #DBI-0620409 and #DEB-9910514. This image is made available for non-commercial or educational use only.

Oliva collecting periphytometer slides at TS/Ph-2, Taylor Slough

This material is based upon work supported by the National Science Foundation through the Florida Coastal Everglades Long-Term Ecological Research program under Cooperative Agreements #DBI-0620409 and #DEB-9910514. This image is made available for non-commercial or educational use only.

Eficacia del aceite de oliva en la prevención de úlceras por presión en pacientes inmovilizados en atención primaria. Ensayo clínico aleatorizado, multicéntrico, paralelo, triple ciego, de no inferioridad

Las úlceras por presión representan un importante problema de salud pública y tienen un importante impacto económico en los sistemas de salud. La mayoría de los estudios para prevenir las úlceras por presión se han llevado a cabo en contextos hospitalarios, usando ácidos grasos hiperoxigenados (AGHO) y hasta la fecha, no se ha realizado ningún estudio específico con aceite de oliva virgen extra (AOVE) en el entorno domiciliario. Material y método Objetivo principal: evaluar si la utilización de AOVE no es inferior a los AGHO en la prevención de úlceras por presión (UPP) en pacientes inmovilizados en el entorno domiciliario. Diseño: Ensayo clínico aleatorizado multicéntrico, paralelo, a triple ciego, de no inferioridad. Ámbito: Población consultante de centros de salud andaluces. Muestra: 831 pacientes inmovilizados en riesgo de padecer UPP. Resultados El período de seguimiento fue de 16 semanas. En el análisis por protocolo, ninguna de las zonas evaluadas presentó diferencias de riesgo de incidencia de las úlceras por presión que superasen el valor delta establecido (10%). Sacro: AOVE 8 (2,55%) vs AGHO 8 (3,08%), RAR 0,53 (-2,2 a 3,26). Talón derecho: AOVE 4 (1,27%) vs AGHO 5 (1,92)%, RAR 0,65 (-1,43 a 2,73). Talón izquierdo: AOVE 3 (0,96%) vs AGHO 3 (1,15%), RAR 0.2 (-1,49 a 1,88). Trocánter Derecho: AOVE 0 (0%) vs AGHO 4 (1,54%), RAR 1,54 (0,04-3,03). Trocánter izquierdo: AOVE 1 (0,32%) vs AGHO 1 (0,38%), RAR 0.07 (-0,91 a 1,04). Discusión Este ensayo clínico pretendía evaluar si la prevención de las UPP usando una fórmula de AOVE no era inferior a la prevención de UPP con el uso AGHO, en el entorno domiciliario y con pacientes inmovilizados de alto riesgo. Los resultados han mostrado esta no inferioridad al no observarse diferencias que hayan superado el límite inferior del intervalo de confianza y convierte al aceite de oliva en un producto eficaz para la prevención de UPP en este tipo de pacientes. Se necesitan más estudios para investigar el mecanismo de acción del AOVE en la prevención de las UPP y relacionarlo con la etiopatogenia de éstas. Bibliografía 1. Gorecki C, Brown JM, Nelson EA, Briggs M, Schoonhoven L, Dealey C, et al. Impact of pressure ulcers on quality of life in older patients: a systematic review. J Am Geriatr Soc. 2009 Jul;57(7):1175–83. 2. Yamamoto Y, Hayashino Y, Higashi T, Matsui M, Yamazaki S, Takegami M, et al. Keeping vulnerable elderly patients free from pressure ulcer is associated with high caregiver burden in informal caregivers. J Eval Clin Pract. 2010 Jun;16(3):585–9. 3. Hanson D, Langemo DK, Anderson J, Thompson P, Hunter S. Friction and shear considerations in pressure ulcer development. Adv Skin Wound Care. 2010 Jan;23(1):21–4. 4. Soldevilla Agreda JJ, Torra i Bou J-E, Verdú Soriano J, López Casanova P. 3.er Estudio Nacional de Prevalencia de Úlceras por Presión en España, 2009: Epidemiología y variables definitorias de las lesiones y pacientes. Gerokomos. 2011 Jun;22(2):77–90. 5. Kottner J, Lahmann N, Dassen T. [Pressure ulcer prevalence: comparison between nursing homes and hospitals]. Pflege Z. 2010 Apr;63(4):228–31. 6. Wilborn D, Halfens R, Dassen T, Tannen A. [Pressure ulcer prevalence in German nursing homes and hospitals: what role does the National Nursing Expert Standard Prevention of Pressure Ulcer play?]. Gesundheitswesen Bundesverb Ärzte Öffentl Gesundheitsdienstes Ger. 2010 Apr;72(4):240–5. 7. Tubaishat A, Anthony D, Saleh M. Pressure ulcers in Jordan: a point prevalence study. J Tissue Viability. 2011 Feb;20(1):14–9. 8. James J, Evans JA, Young T, Clark M. Pressure ulcer prevalence across Welsh orthopaedic units and community hospitals: surveys based on the European Pressure Ulcer Advisory Panel minimum data set. Int Wound J. 2010 Jun;7(3):147–52. 9. Defloor T, Schoonhoven L, Katrien V, Weststrate J, Myny D. Reliability of the European Pressure Ulcer Advisory Panel classification system. J Adv Nurs. 2006 Apr;54(2):189–98

Factores determinantes del uso de Internet en la comercialización del aceite de oliva. Análisis del sector en Cataluña

Las cooperativas son entidades con una gran presencia económica y social en España, y tienen una gran influencia en la economía rural de las zonas donde están ubicadas. El principal objetivo del presente trabajo es el análisis del uso de las nuevas tecnologías por parte de las cooperativas agroalimentarias, centrándose en las productoras de aceite de oliva para determinar los principales factores que condicionan su comportamiento en la Red. En el presente estudio se analizan sus sitios web y se determina qué tipo de información aporta, tanto datos generales como datos de comercialización. A partir de los resultados obtenidos, se busca la relación que pueda existir entre el tamaño de la cooperativa, su actividad exportadora o la actividad de comercio electrónico con la presencia online, mediante una regresión logística. De esta manera podremos conocer si realmente la implantación de nuevas tecnologías en las cooperativas permite desarrollar una óptima actividad económica.

RELAZIONE TRA IL CONSUMO DI OLIO EXTRAVERGINE DI OLIVA E I CASI DI DECESSO PER MALATTIA DI ALZHEIMER IN SPAGNA

In the chemical composition of olive oil (Olea europaea L.) it is emphasized the massive presence of oleic acid (over 70%), monounsaturated fatty acid part of the family of omega 9, a 7-8% linoleic acid (omega 6) and a small presence (0.5-1%) of linolenic acid (omega 3). For its high content of monounsaturated fatty acids, olive oil is the most stable and therefore the most suitable for heating, compared to oils with a dominance of polyunsaturated fatty acids. Interest in vitamin E has increased in recent years, thanks to its high antioxidant power and its role against related diseases with age-related, visual, dermatological, cardiovascular disorders Alzheimer’s disease and more. Vegetable oils are a major source of vitamin E through diet (Sayago et al., 2007), especially with the variety of olives “Hojiblanca”. Thanks to unsaturated fatty acids cell oxidation can be prevented: this helps prevent many illness, and even premature aging. So far, the advantages acknowledged to olive oil are those of lowering cholesterol, preventing cardiovascular disease, diabetes and cancer. Among the most recent researches it is important to distinguish the studies carried out on their contribution to the prevention and treatment of breast cancer and Alzheimer’s disease. Researchers found that in addition to the benefi ts that give monounsaturated fats, in extra virgin olive oil, there is a substance called “oleocanthal”, which helps protect nerve cells damaged in Alzheimer’s disease. The importance of this discovery is enormous when one considers that only Alzheimer’s disease affects 30 million people around the world, with a different distribution depending on the type of oil in the diet (Olguín Cordero, 2012). The latest research endorses that oleocanthal works by destroying cancer cells without affecting the healthy ones, as it is stated in the Molecular and Cellular Oncology Journal. Studies carried out in different Spanish universities have concluded that thanks to the antioxidant power of olive oil, a disease such as Alzheimer can be prevented. In conclusion, we can say that the Mediterranean diet rich in extra virgin olive oil greatly infl uences on human health, reducing, delaying or even eliminating several diseases.

“Cultura y clase trabajadora, a propósito de ‘Artesanos y obreros costarricenses 1880- 1914', de Mario Oliva Medina”

Introducción:Si la historia económica se ha venido desarrollando sistemáticamente en nuestro país desde hace poco más de una década, no es menos cierto que la historia socual recién comienza a dar sus primeros pasos. Una de sus vertienetes, aquella relacionada con la historia del movimiento obrero, viene tomando un auge inusitado. Es indudable que le fomento sistemático de la investigación y de medios de difusión de pensamiento histórico producido, son factores que han contribuido decisivamente a acelerar este proceso...

Use of Bayesian geostatistical prediction to estimate local variations in Schistosoma haematobium infection in western Africa

Objective We aimed to predict sub-national spatial variation in numbers of people infected with Schistosoma haematobium, and associated uncertainties, in Burkina Faso, Mali and Niger, prior to implementation of national control programmes. Methods We used national field survey datasets covering a contiguous area 2,750 × 850 km, from 26,790 school-aged children (5–14 years) in 418 schools. Bayesian geostatistical models were used to predict prevalence of high and low intensity infections and associated 95% credible intervals (CrI). Numbers infected were determined by multiplying predicted prevalence by numbers of school-aged children in 1 km2 pixels covering the study area. Findings Numbers of school-aged children with low-intensity infections were: 433,268 in Burkina Faso, 872,328 in Mali and 580,286 in Niger. Numbers with high-intensity infections were: 416,009 in Burkina Faso, 511,845 in Mali and 254,150 in Niger. 95% CrIs (indicative of uncertainty) were wide; e.g. the mean number of boys aged 10–14 years infected in Mali was 140,200 (95% CrI 6200, 512,100). Conclusion National aggregate estimates for numbers infected mask important local variation, e.g. most S. haematobium infections in Niger occur in the Niger River valley. Prevalence of high-intensity infections was strongly clustered in foci in western and central Mali, north-eastern and northwestern Burkina Faso and the Niger River valley in Niger. Populations in these foci are likely to carry the bulk of the urinary schistosomiasis burden and should receive priority for schistosomiasis control. Uncertainties in predicted prevalence and numbers infected should be acknowledged and taken into consideration by control programme planners.

Efficient content-based image retrieval based on multi-feature fusion

The increased availability of image capturing devices has enabled collections of digital images to rapidly expand in both size and diversity. This has created a constantly growing need for efficient and effective image browsing, searching, and retrieval tools. Pseudo-relevance feedback (PRF) has proven to be an effective mechanism for improving retrieval accuracy. An original, simple yet effective rank-based PRF mechanism (RB-PRF) that takes into account the initial rank order of each image to improve retrieval accuracy is proposed. This RB-PRF mechanism innovates by making use of binary image signatures to improve retrieval precision by promoting images similar to highly ranked images and demoting images similar to lower ranked images. Empirical evaluations based on standard benchmarks, namely Wang, Oliva & Torralba, and Corel datasets demonstrate the effectiveness of the proposed RB-PRF mechanism in image retrieval.

Ferrolysis induced soil transformation by natural drainage in Vertisols of sub-humid South India

In sub-humid South India, recent studies have shown that black soil areas (Vertisols and vertic Intergrades), located on flat valley bottoms, have been rejuvenated through the incision of streambeds, inducing changes in the pedoclimate and soil transformation. Joint pedological, geochemical and geophysical investigations were performed in order to better understand the ongoing processes and their contribution to the chemistry of local rivers. The seasonal rainfall causes cycles of oxidation and reduction in a perched watertable at the base of the black soil, while the reduced solutions are exported through a loamy sand network. This framework favours a ferrolysis process, which causes low base saturation and protonation of clay, leading to the weathering of 2:1 then 1:1 clay minerals. Maximum weathering conditions occur at the very end of the wet season, just before disappearance of the perched watertable. Therefore, the by-products of soil transformation are partially drained off and calcareous nodules, then further downslope, amorphous silica precipitate upon soil dehydration. The ferrolysed area is fringing the drainage system indicating that its development has been induced by the streambed incision. The distribution of C-14 ages of CaCO3 nodules suggests that the ferrolysis process started during the late Holocene, only about 2 kyr B.P. at the studied site and about 5 kyr B.P. at the watershed outlet. The results of this study are applied to an assessment of the physical erosion rate (4.8x10(-3) m/kyr) since the recent reactivation of the erosion process. (C) 2010 Elsevier B.V. All rights reserved.

Modelling the chemical weathering fluxes at the watershed scale in the Tropics (Mule Hole, South India): Relative contribution of the smectite/kaolinite assemblage versus primary minerals

We investigate the chemical weathering processes and fluxes in a small experimental watershed (SEW) through a modelling approach. The study site is the Mule Hole SEW developed on a gneissic basement located in the climatic gradient of the Western Ghats, South India. The model couples a lumped hydrological model simulating the water budget at the watershed scale to the WITCH model estimating the dissolution/precipitation rates of minerals using laboratory kinetic laws. Forcing functions and parameters of the simulation are defined by the field data. The coupled model is calibrated with stream and groundwater compositions through the testing of a large range of smectite solubility and abundance in the soil horizons. We found that, despite the low abundance of smectite in the dominant soil type of the watershed (4 vol.%), their net dissolution provides 75% of the export of dissolved silica, while primary silicate mineral dissolution releases only 15% of this flux. Overall, smectites (modelled as montmorillonites) are not stable under the present day climatic conditions. Furthermore, the dissolution of trace carbonates in the saprolitic horizon provides 50% of the calcium export at the watershed scale. Modelling results show the contrasted behavior of the two main soil types of the watershed: red soils (88% of the surface) are provider of calcium, while black soils (smectite-rich and characterized by a lower drainage) consumes calcium through overall carbonate precipitation. Our model results stress the key role played by minor/accessory minerals and by the thermodynamic properties of smectite minerals, and by the drainage of the weathering profiles on the weathering budget of a tropical watershed. (C) 2010 Elsevier B.V. All rights reserved.

Formation and preservation of pedogenic carbonates in South India, links with paleo-monsoon and pedological conditions: Clues from Sr isotopes, U-Th series and REEs

The influence of the pedogenic and climatic contexts on the formation and preservation of pedogenic carbonates in a climosequence in the Western Ghats (Karnataka Plateau, South West India) has been studied. Along the climosequence, the current mean annual rainfall (MAR) varies within a 80 km transect from 6000 mm at the edge of the Plateau to 500 mm inland. Pedogenic carbonates occur in the MAR range of 500-1200 mm. In the semi-arid zone (MAR: 500-900 mm), carbonates occur (i) as rhick hardpan calcretes on pediment slopes and (ii) as nodular horizons in polygenic black soils (i.e. vertisols). In the sub-humid zone (MAR: 900-1500 mm), pedogenic carbonates are disseminated in the black soil matrices either as loose, irregular and friable nodules of millimetric size or as indurated botryoidal nodules of centimetric to pluricentimetric size. They also occur at the top layers of the saprolite either as disseminated pluricentimetric indurated nodules or carbonate-cemented lumps of centimetric to decimetric size. Chemical and isotopic (Sr-87/Sr-86) compositions of the carbonate fraction were determined after leaching with 0.25 N HCl. The corresponding residual fractions containing both primary minerals and authigenic clays were digested separately and analyzed. The trend defined by the Sr-87/Sr-86 signatures of both labile carbonate fractions and corresponding residual fractions indicates that a part of the labile carbonate fraction is genetically linked to the local soil composition. Considering the residual fraction of each sample as the most likely lithogenic source of Ca in carbonates, it is estimated that from 24% to 82% (55% on average) of Ca is derived from local bedrock weathering, leading to a consumption of an equivalent proportion of atmospheric CO2. These values indicate that climatic conditions were humid enough to allow silicate weathering: MAR at the time of carbonate formation likely ranged from 400 to 700 mm, which is 2- to 3-fold less than the current MAR at these locations. The Sr, U and Mg contents and the (U-234/U-238) activity ratio in the labile carbonate fraction help to understand the conditions of carbonate formation. The relatively high concentrations of Sr, U and Mg in black soil carbonates may indicate fast growth and accumulation compared to carbonates in saprolite, possibly due to a better confinement of the pore waters which is supported by their high (U-234/U-238) signatures, and/or to higher content of dissolved carbonates in the pore waters. The occurrence of Ce, Mn and Fe oxides in the cracks of carbonate reflects the existence of relatively humid periods after carbonate formation. The carbonate ages determined by the U-Th method range from 1.33 +/- 0.84 kyr to 7.5 +/- 2.7 kyr and to a cluster of five ages around 20 kyr, i.e. the Last Glacial Maximum period. The young occurrences are only located in the black soils, which therefore constitute sensitive environments for trapping and retaining atmospheric CO2 even on short time scales. The maximum age of carbonates depends on their location in the climatic gradient: from about 20 kyr for centimetric nodules at Mule Hole (MAR = 1100 mm/yr) to 200 kyr for the calcrete at Gundlupet (MAR = 700 mm/yr, Durand et al., 2007). The intensity of rainfall during wet periods would indeed control the lifetime of pedogenic carbonates and thus the duration of inorganic carbon storage in soils. (C) 2010 Elsevier Ltd. All rights reserved.