987 resultados para nutrition transition


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General information on the Council Bluffs Youth Connections prototype under Improving Transition Outcomes with Iowa Vocational Rehabilitation Services.

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General information on the Henry County Transition Partners community prototype under Improving Transition Outcomes with Iowa Vocational Rehabilitation Services.

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Henry County's Transition Partners' youth focus group interview invitation.

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Henry County's Transition Partners' focus group invitation specifically for teachers.

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Interview questions used by Henry County Transition Partners during focus groups and individual interviews.

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Information gleaned from the focus groups and individual interviews with educators, youth and parents.

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Résumé L'ostéoporose est une maladie systémique du squelette caractérisée par une fragilité osseuse augmentée avec pour conséquence une augmentation de la susceptibilité aux fractures. C'est actuellement un important problème de santé publique avec des conséquences majeures pour les systèmes de soins tant d'un point de vue médical que financier. Les projections mondiales prévoient une augmentation significative du nombre de fractures de la hanche d'ici 2050. Cette étude vise à analyser l'influence des apports nutritionnels par rapport à celle de la condition physique sur le risque de fracture ostéoporotique en reprenant les données évaluant la consommation de produits laitiers au sein du collectif de l'étude SEMOF («Evaluation suisse de méthodes de mesure du risque de fracture ostéoporotique»). Nous avons d'abord montré que les apports moyens en calcium des 7788 femmes âgées de 70 ans et plus ayant participé à l'étude sont inférieurs aux recommandations suisses et internationales. Des trois régions étudiées, la Suisse romande est celle où les apports quotidiens moyens en calcium et en protéines provenant des produits laitiers sont les plus faibles et où l'incidence des fractures de la hanche secondaires à l'ostéoporose est la plus élevée. Les apports en calcium et en protéines sont également plus élevés à la campagne par rapport à la ville alors que l'incidence des fractures de la hanche n'est pas significativement différente entre ville et campagne. De plus, nous avons montré que les apports quotidiens moyens en calcium et en protéines provenant des produits laitiers ne diffèrent pas significativement entre les femmes avec ou sans fracture de la hanche pendant le suivi. En revanche, la condition physique des femmes qui ont présenté une fracture de la hanche est significativement moins bonne. Sur la base de données anamnestiques concernant les facteurs de risque de chute et la mobilité, nous avons développé un score permettant d'identifier les femmes les plus à risque de chute. La condition physique de ces femmes, attestée par le test de la chaise et la mesure de la force de préhension est la moins bonne. Toutefois, leurs apports quotidiens moyens en calcium et en protéines provenant des produits laitiers ne diffèrent pas significativement par rapport aux femmes à faible risque de chute. En conclusion, le risque de fracture de la hanche liée à l'ostéoporose est plus élevé chez les femmes de plus de 70 ans vivant en Suisse romande que dans les deux autres régions linguistiques. Il est déterminé avant tout par le risque de chute et par la condition physique. Les apports en calcium et en protéines provenant des produits laitiers, tels que nous les avons évalués ne semblent pas déterminants.

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Asymmetric fiscal decentralization, by which we mean different fiscal arrangements between the central government and different groups of, or individual, lower-level governments, may be justified from an economic efficiency perspective. As argued by Tiebout (1956), Oates (1972) and others, a decentralized system of regional and local governments is better able to accommodate differences in tastes for public goods and services. This efficiency argument calls for decentralization of fiscal authority to regional and local governments, but not necessarily asymmetric decentralization. However, when the differences in tastes for public goods and services arise out of differences in history, culture and language across regions of a country, asymmetric treatment may be justified. History, culture and language may influence how a group of people (a region) views autonomy, independence and fiscal authority. Some regions may have had experience with autonomous government in the past, they may have a culture that is strongly reliant upon (or leery of) the central government, or they may be fearful of losing their separate languages if they do not have special arrangements. To accommodate differences in taste for independence, autonomy, and fiscal authority, it may be necessary to have different fiscal arrangements between the central government and the different regions comprising the country.

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Some biochemical functions of vitamin C make it an essential component of parenteral nutrition (PN) and an important therapeutic supplement in other acute conditions. Ascorbic acid is a strong aqueous antioxidant and is a cofactor for several enzymes. The average body pool of vitamin C is 1.5 g, of which 3%-4% (40-60 mg) is used daily. Steady state is maintained with 60 mg/d in nonsmokers and 140 mg/d in smokers. Shocked surgical, trauma, and septic patients have a drastic reduction of circulating plasma ascorbate concentrations. These low concentrations require 3-g doses/d to restore normal plasma ascorbate concentrations, questioning the recommended PN dose of 100 mg/d. Determination of intravenous requirements is usually based on plasma concentrations, which are altered during the inflammatory response. There is no clear indicator of deficiency: serum or plasma ascorbate concentrations <0.3 mg/dL (20 micromol/L) indicates inadequate vitamin C status. On the basis of available pharmacokinetic data the 100 mg/d dose for patients receiving home PN and 200 mg/d for stable adult patients receiving PN are adequate, but requirements have been shown to be higher in perioperative, trauma, burn, and critically ill patients, paralleling oxidative stress. One recommendation cannot fit all categories of patients. Large vitamin C supplements may be considered in severe critical illness, major trauma, and burns because of increased requirements resulting from oxidative stress and wound healing. Future research should distinguish therapeutic use of high-dose ascorbic acid antioxidant therapy from nutritional PN requirements.

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The case of two transition tables is considered, that is two squareasymmetric matrices of frequencies where the rows and columns of thematrices are the same objects observed at three different timepoints. Different ways of visualizing the tables, either separatelyor jointly, are examined. We generalize an existing idea where asquare matrix is descomposed into symmetric and skew-symmetric partsto two matrices, leading to a decomposition into four components: (1)average symmetric, (2) average skew-symmetric, (3) symmetricdifference from average, and (4) skew-symmetric difference fromaverage. The method is illustrated with an artificial example and anexample using real data from a study of changing values over threegenerations.

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Stable isotopes of carbonates (delta(13)C(carb), delta(18)O(carb)), organic matter (delta(13)C(org), delta(15)N(org)) and major, trace and rare earth element (REE) compositions of marine carbonate rocks of Late Permian to Early Triassic age were used to establish the position of the Permian-Triassic boundary (PTB) at two continuous sections in the Velebit Mountain, Croatia. The chosen sections - Rizvanusa and Brezimenjaca - are composed of two lithostratigraphic units, the Upper Permian Transitional Dolomite and the overlying Sandy Dolomite. The contact between these units, characterized by the erosional features and sudden occurrence of ooids and siliciclastic grains, was previously considered as the chronostratigraphic PTB. The Sandy Dolomite is characterized by high content of non-carbonate material (up to similar to 30 wt.% insoluble residue), originated from erosion of the uplifted hinterland. A relatively rich assemblage of Permian fossils (including Geinitzina, Globivalvulina, Hemigordius, bioclasts of gastropods, ostracods and brachiopods) was found for the first time in Sandy Dolomite, 5 m above the lithologic boundary in the Rizvanusa section. A rather abrupt negative delta(13)C(carb) excursion in both sections appears in rocks showing no recognizable facies change within the Sandy Dolomite, -2 parts per thousand at Rizvanusa and -1.2 parts per thousand at Brezimenjaca, 11 m and 0.2 m above the lithologic contact, respectively. This level within the lower part of the Sandy Dolomite is proposed as the chemostratigraphic PTB. In the Rizvanusa section, the delta(13)C(org) values decline gradually from similar to-25 parts per thousand in the Upper Permian to similar to-29 parts per thousand in the Lower Triassic. The first negative delta(13)C(org) excursion occurs above the lithologic contact, within the uppermost Permian deposits, and appears to be related to the input of terrigenous material. The release of isotopically light microbial soil-biomass into the shallow-marine water may explain this sudden decrease of delta(13)C(org) values below the PTB. This would support the hypothesis that in the western Tethyan realm the land extinction, triggering a sudden drop of woody vegetation and related land erosion, preceded the marine extinction. The relatively low delta(15)N(org) values at the Permian-Triassic (P-Tr) transition level, close to approximate to 0 parts per thousand, and a secondary negative delta(13)C(org) excursion of -0.5 parts per thousand point to significant terrestrial input and primary contribution of cyanobacteria. The profiles of the concentrations of redox-sensitive elements (Ce, Mn, Fe, V), biogenic or biogenic-scavenged elements (P, Ba, Zn, V), Ce/Ce* values, and normalized trace elements, including Ba/Al, Ba/Fe, Ti/Al, Al/(Al + Fe + Mn) and Mn/Ti show clear excursions at the Transitional Dolomite-Sandy Dolomite lithologic boundary and the chemostratigraphic P-Tr boundary. The stratigraphic variations indicate a major regression phase marking the lithologic boundary, transgressive phases in the latest Permian and a gradual change into shallow/stagnant anoxic marine environment towards the P-Tr boundary level and during the earliest Triassic. (C) 2010 Elsevier B.V. All rights reserved.