953 resultados para Tibi reservoir
Resumo:
The multiscale finite-volume (MSFV) method has been derived to efficiently solve large problems with spatially varying coefficients. The fine-scale problem is subdivided into local problems that can be solved separately and are coupled by a global problem. This algorithm, in consequence, shares some characteristics with two-level domain decomposition (DD) methods. However, the MSFV algorithm is different in that it incorporates a flux reconstruction step, which delivers a fine-scale mass conservative flux field without the need for iterating. This is achieved by the use of two overlapping coarse grids. The recently introduced correction function allows for a consistent handling of source terms, which makes the MSFV method a flexible algorithm that is applicable to a wide spectrum of problems. It is demonstrated that the MSFV operator, used to compute an approximate pressure solution, can be equivalently constructed by writing the Schur complement with a tangential approximation of a single-cell overlapping grid and incorporation of appropriate coarse-scale mass-balance equations.
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Q fever is a zoonosis caused by an intracellular Gram-negative bacteria, Coxiella burnetii. Animals are the main reservoir and transmission to men generally is occurring by inhalation of contaminated aerosols. Acute Q fever generally is benign and usually resolves spontaneously. When symptomatic, the clinical presentation typically includes one of the following three syndromes: a flu-like illness, a granulomatous hepatitis or an atypical pneumonia. Individuals presenting risk factors such as patients with valvular heart diseases and vascular prostheses, as well as pregnant women and immuno-suppressed patients represent a population at risk of chronic infection, with endocarditis as the most common clinical form.
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BACKGROUND: Complications associated with intrathecal pumps may be linked to the surgical procedure, the implanted device, or the medication itself.¦CASE REPORTS: Three patients treated chronically with intrathecal clonidine presented with clonidine overdose due to inadvertent extravasation during the refilling procedure. All patients experienced loss of consciousness and severe systemic hypertension that required aggressive parenteral treatment.¦DISCUSSION: Clonidine is an alpha-2 agonist with a nearly 100% bioavailability after oral or rectal administration. With high plasma concentration secondary to massive systemic overdose, the specificity for the alpha-2 receptor is lost and an alpha-1 agonist activity predominates and causes marked hypertension. Management of clonidine overdose consists of supportive therapy guided by signs and symptoms.¦CONCLUSION: Inadvertent injection into the subcutaneous pocket rather than the reservoir is rare but very dangerous as the drug cannot be retrieved and massive doses are involved. Signs and symptoms of systemic overdose with drugs commonly used in implanted drugs delivery system should be well known to ensure early diagnosis and treatment.
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The development of new drug delivery systems to target the anterior segment of the eye may offer many advantages: to increase the biodisponibility of the drug, to allow the penetration of drug that cannot be formulated as solutions, to obtain constant and sustained drug release, to achieve higher local concentrations without systemic effects, to target more specifically one tissue or cell type, to reduce the frequency of instillation and therefore increase the observance and comfort of the patient while reducing side effects of frequent instillation. Several approaches are developed, aiming to increase the corneal contact time by modified formulation or reservoir systems, or by increasing the tissue permeability using iontophoresis. To date, no ocular drug delivery system is ideal for all purposes. To maximize treatment efficacy, careful evaluation of the specific pathological condition, the targeted Intraocular tissue and the location of the most severe pathology must be made before selecting the method of delivery most suitable for each individual patient.
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En la literatura sobre creació d’empreses, les dones empresàries són considerades un re· servori de desenvolupament econòmic i un model de gestió empresarial alternatiu. D’al· tra banda, els immigrants posseeixen un fort esperit emprenedor. El paper de les adminis· tracions locals per donar suport a aquests col· lectius en la creació d’empreses és rellevant. L’intens procés migratori viscut a Osona en els darrers anys mereix una anàlisi des de la perspectiva de l’emprenedoria de gènere. Aquest estudi fa una comparació de les em· presàries autòctones i immigrades de la co· marca, així com de les polítiques de suport realitzades pels ajuntaments.
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We study energy relaxation in thermalized one-dimensional nonlinear arrays of the Fermi-Pasta-Ulam type. The ends of the thermalized systems are placed in contact with a zero-temperature reservoir via damping forces. Harmonic arrays relax by sequential phonon decay into the cold reservoir, the lower-frequency modes relaxing first. The relaxation pathway for purely anharmonic arrays involves the degradation of higher-energy nonlinear modes into lower-energy ones. The lowest-energy modes are absorbed by the cold reservoir, but a small amount of energy is persistently left behind in the array in the form of almost stationary low-frequency localized modes. Arrays with interactions that contain both a harmonic and an anharmonic contribution exhibit behavior that involves the interplay of phonon modes and breather modes. At long times relaxation is extremely slow due to the spontaneous appearance and persistence of energetic high-frequency stationary breathers. Breather behavior is further ascertained by explicitly injecting a localized excitation into the thermalized arrays and observing the relaxation behavior.
Resumo:
In conventional construction practices, a longitudinal joint is sawed in a PCC (Portland Cement Concrete) pavement to control concrete shrinkage cracking between two lanes of traffic. Sawing a joint in hardened concrete is an expensive and time consuming operation. The longitudinal joint is not a working joint (in comparison to a transverse joint) as it is typically tied with a tie bar at 30 inch spacing. The open joint reservoir, left by the saw blade, typically is filled or sealed with a durable crack sealant to keep incompressibles and water from getting into the joint reservoir. An experimental joint forming knife has been developed. It is installed under the paving machine to form the longitudinal joint in the wet concrete as a part of the paving process. Through this research method, forming a very narrow longitudinal joint during the paving process, two conventional paving operations can be eliminated. Joint forming eliminates the need of the joint sawing operation in the hard concrete, and as the joint that is formed does not leave a wide-open reservoir, but only a hairline crack, it does not need the joint filling or sealing operation. Therefore, the two conventional longitudinal joint sawing and sealing operations are both being eliminated by this innovation. A laboratory scale prototype joint forming knife was built and tested, initially forming joints in small concrete beams. The results were positive so the method was proposed for field testing. Initial field tests were done in the construction season of 2001, limited to one paving contractor. A number of modifications were made to the knife throughout the field tests. About 3000 feet of longitudinal joint was formed in 2001. Additional testing was done in the 2002 construction season, working with the same contractor. About 150,000 feet of longitudinal joint was formed in 2002. Evaluations of the formed joints were done to determine longitudinal joint hairline crack development rate and appearance. Additional tests will be done in the next construction season to improve or perfect the longitudinal joint forming technique.
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Simulated-annealing-based conditional simulations provide a flexible means of quantitatively integrating diverse types of subsurface data. Although such techniques are being increasingly used in hydrocarbon reservoir characterization studies, their potential in environmental, engineering and hydrological investigations is still largely unexploited. Here, we introduce a novel simulated annealing (SA) algorithm geared towards the integration of high-resolution geophysical and hydrological data which, compared to more conventional approaches, provides significant advancements in the way that large-scale structural information in the geophysical data is accounted for. Model perturbations in the annealing procedure are made by drawing from a probability distribution for the target parameter conditioned to the geophysical data. This is the only place where geophysical information is utilized in our algorithm, which is in marked contrast to other approaches where model perturbations are made through the swapping of values in the simulation grid and agreement with soft data is enforced through a correlation coefficient constraint. Another major feature of our algorithm is the way in which available geostatistical information is utilized. Instead of constraining realizations to match a parametric target covariance model over a wide range of spatial lags, we constrain the realizations only at smaller lags where the available geophysical data cannot provide enough information. Thus we allow the larger-scale subsurface features resolved by the geophysical data to have much more due control on the output realizations. Further, since the only component of the SA objective function required in our approach is a covariance constraint at small lags, our method has improved convergence and computational efficiency over more traditional methods. Here, we present the results of applying our algorithm to the integration of porosity log and tomographic crosshole georadar data to generate stochastic realizations of the local-scale porosity structure. Our procedure is first tested on a synthetic data set, and then applied to data collected at the Boise Hydrogeophysical Research Site.
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The purpose of this study was to evaluate the efficacy of a Coulomb Controlled Iontophoresis system (CCI) in the local delivery of corticosteroids for the treatment of uveitis. The therapeutic efficacy of Dexamethasone (Dex) administered by CCI was compared to systemic injection and to topical application with the iontophoresis apparatus in the absence of electrical current. The evaluation was done in the treatment of the endotoxin-induced uveitis (EIU) model, and in the effect on TNF gene expression in the iris/ciliary body as well as in the retina and on TNF levels in aqueous humor and vitreous. Dex was administered either at the time of LPS injection or 5 hours later. For iontophoresis, we used a 1 ml reservoir-electrode covering the cornea, the limbus, and the first millimeter of the sclera. The applied electrical current was of 400 microA during four minutes with a total surface charge of 0.4 C cm-2. EIU was evaluated by clinical examination, by counts of intraocular inflammatory cells on histological sections, and by measuring the protein levels in the aqueous humor and in the vitreous. The TNF-alpha gene expression in the iris and ciliary body, and in the retina was evaluated by RT-PCR. The systemic effect of Dex delivered by CCI was evaluated on the level of serum TNF-alpha in EIU. Our results demonstrated that local administration of Dex by CCI inhibited anterior and posterior signs of intraocular inflammation as effectively as systemic administration, with no effect on systemic level of TNF. In the anterior and posterior segments of the eye, the protein exudation. TNF levels and the cellular infiltration were inhibited. The TNF-alpha gene expression was inhibited in the anterior as well as the posterior segment of the eye. No clinical nor histological damage were caused by the CCI apparatus. In conclusion, CCI administration of Dex allows for a therapeutic effect on the posterior as well as the anterior segment of the eye, and may present a viable alternative to systemic administration of glucocorticoids in severe ocular inflammations.
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The main geothermal reservoir of Acqui Terme-Visone hosts Na-Cl waters, which are in chemical equilibrium at 120-130 degrees C with typical hydrothermal minerals including quartz, albite, K-feldspar, illite, chlorite (or smectite), anhydrite, calcite and an unspecified Ca-Al-silicate. In the Acqui Terme-Visone area, these geothermal waters ascend along zones of high vertical permeability and discharge at the surface almost undiluted or mixed with cold, shallow waters. To the SW of Acqui Terme, other ascending geothermal waters, either undiluted or mixed with low-salinity waters, enter relatively shallow secondary reservoirs, where they reequilibrate at 65-70 degrees C. Both chemical and isotopic data indicate that bacterial SO4 reduction affects all these waters, especially those discharged by the secondary reservoirs. Therefore, geothermal waters must get in contact with oil, acquiring the relatively oxidized organic substances needed by SO4-reducing bacteria. This oil-water interaction process deserves further investigations, for potential economic implications. (C) 2000 Elsevier Science Ltd. All rights reserved.
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The objective of this work was to test a closed soilless growing system for producing bare root transplants and runner tips of two strawberry clones, using two categories of substrates. The system used corrugated roofing panels of fiber-cement, over which a substrate layer was used as a growing bed. The nutrient solution was pumped from a reservoir toward the upper end of the roofing panels and drained back to a reservoir. Plant growth and development were determined for two advanced strawberry clones, grown in sand or in Plantmax organic substrate. Growth of the stock plants and the number and dry mass of bare root transplants were similar in the substrates, but bare roots differed in their crown diameters by substrate. For number of runner tips, no significant differences were found in total, small, and medium categories in the substrates. A mean production of about 590 runner tips per square meter and 145 bare root transplants per square meter was obtained. For both clones, a large number of bare root transplants and runner tips of adequate size were produced in the closed soilless growing system using sand or organic substrate.
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The Mississippi Valley-type (MVT) Pb-Zn ore district at Mezica is hosted by Middle to Upper Triassic platform carbonate rocks in the Northern Karavanke/Drau Range geotectonic units of the Eastern Alps, northeastern Slovenia. The mineralization at Mezica covers an area of 64 km(2) with more than 350 orebodies and numerous galena and sphalerite occurrences, which formed epigenetically, both conformable and discordant to bedding. While knowledge on the style of mineralization has grown considerably, the origin of discordant mineralization is still debated. Sulfur stable isotope analyses of 149 sulfide samples from the different types of orebodies provide new insights on the genesis of these mineralizations and their relationship. Over the whole mining district, sphalerite and galena have delta(34)S values in the range of -24.7 to -1.5% VCDT (-13.5 +/- 5.0%) and -24.7 to -1.4% (-10.7 +/- 5.9%), respectively. These values are in the range of the main MVT deposits of the Drau Range. All sulfide delta(34)S values are negative within a broad range, with delta(34)S(pyrite) < delta(34)S(sphalerite) < delta(34)S(galena) for both conformable and discordant orebodies, indicating isotopically heterogeneous H(2)S in the ore-forming fluids and precipitation of the sulfides at thermodynamic disequilibrium. This clearly supports that the main sulfide sulfur originates from bacterially mediated reduction (BSR) of Middle to Upper Triassic seawater sulfate or evaporite sulfate. Thermochemical sulfate reduction (TSR) by organic compounds contributed a minor amount of (34)S-enriched H(2)S to the ore fluid. The variations of delta(34)S values of galena and coarse-grained sphalerite at orefield scale are generally larger than the differences observed in single hand specimens. The progressively more negative delta(34)S values with time along the different sphalerite generations are consistent with mixing of different H(2)S sources, with a decreasing contribution of H(2)S from regional TSR, and an increase from a local H(2)S reservoir produced by BSR (i.e., sedimentary biogenic pyrite, organo-sulfur compounds). Galena in discordant ore (-11.9 to -1.7%; -7.0 +/- 2.7%, n=12) tends to be depleted in (34)S compared with conformable ore (-24.7 to -2.8%, -11.7 +/- 6.2%, n=39). A similar trend is observed from fine-crystalline sphalerite I to coarse open-space filling sphalerite II. Some variation of the sulfide delta(34)S values is attributed to the inherent variability of bacterial sulfate reduction, including metabolic recycling in a locally partially closed system and contribution of H(2)S from hydrolysis of biogenic pyrite and thermal cracking of organo-sulfur compounds. The results suggest that the conformable orebodies originated by mixing of hydrothermal saline metal-rich fluid with H(2)S-rich pore waters during late burial diagenesis, while the discordant orebodies formed by mobilization of the earlier conformable mineralization.
Resumo:
Sur le feuillet de garde A, cette note autographe de Mabillon : « Hic codex optimae notae scriptus est ante annos circiter octingentos. Multa scitu digna continet, maxime in triduo ante Pascha. In litaniis sabbati sancti fit supplicatio pro congregatione S. Petri, quem patronum habet Pictavensis ecclesia. Invocantur etiam in iisdem sanctus Hilarius et sancta Radegundis, qui praecipue ad ecclesiam Pictavensem pertinent ; sed nulla mentio de aliis sanctis ejusdem dioecesis. Haec scripsi XI kal. decembris an. 1695. — F. J. M. » Fol. 1 : « Benedictio episcoporum. — Consecratio ». Fol. 2 : « Oratio ad ordinandum praesbiterum. — Consecratio. ». Fol. 3 : « Oratio ad ordinandum diaconum. — Consecratio. » Fol. 4 : « Ordo qualiter in Romana ecclesia praesbiteri, diaconi, subdiaconi ordinandi sunt. » Fol. 5 : « Ordinatio subdiaconi ». Fol. 5v° : « Ordinatio ostiarii. » Fol. 6 : « Ordinatio lectoris ». Fol. 6v° : « Ordinatio exorcistae ». Fol. 7 : « Ordinatio acoliti ». Fol. 7v° : « Incipit ordo qualiter publice vel specialiter agitur modus paenitentiae secundum censuram ecclesiasticam, quod quarta feria quinquagesime inchoatur ». Fol. 8v° : « Confessio pura coram Deo et angelis et coram omnibus sanctis » : — de superbia (fol. 12) ; de inani gloria (fol. 13) ; de invidia (fol. 13 vo) ; de ira (fol. 14 vo) ; de tristitia (fol. 15) ; de avaricia (fol. 16) ; de ventris ingluvie (fol. 20) ; de luxuria (fol. 23). Fol. 40v° : « Missa pro paenitentibus et confitentibus, sive unus sive plures fuerint ». Fol. 43 : « Denunciatio scrutinii quod tertia ebdomada in quadragesima secunda feria iniciatur ». Fol. 43v° : « Oratio super electos ad catecuminum faciendum ». Fol. 44 : « Benedictio salis dandi caticuminis. » — Prières et exhortations aux catéchumènes. Explication des évangiles. Fol. 54-56 : Le Credo, en grec avec traduction latine au-dessus. La traduction est faite de mot à mot. Pour l'article grec, le traducteur s'est contenté de mettre au-dessus, dans le texte latin, ces lettres ar. (articulus). Fol. 58v° : Explication du Pater. Fol. 60v° : « Incipit missa primi scrutinii ». Fol. : 63 : « Alia missa de secundo scrutinio ». Fol. 66v° : « Missa de tertio scrutinio ». Fol. 70 : « Sabbato ante diem Palmarum ». Fol. 72 : « Dominica indulgentiae quae est dies Palmarum ». Fol. 73 : Les 36 premiers vers de la pièce Gloria, laus de Théodulfe, évêque d'Orléans (Henry Martin signale l'éd. qu'en a fait Duemmler dans les Poetae latini aevi carolini, t. I, p. 558 : « Gloria, laus et honor tibi sit, Christe redemptor, Cui puerile decus promsit osanna pium. Israhel es tu rex Davidis et inclita proles, Nomine qui in Domini, rex benedicte, venis... » Fol. 95 :« Feria II post Palmas ». Fol. 98v° : « Feria tertia ». Fol. 130 : « Feria V, quae est cena Domini ». Fol. 141v° : « Alia missa eodem die, si plures ad reconciliandum venerint ». Fol. 154 : « Missa chrismalis ». Fol. 160 : Litanies. A noter : SS. Denys, Quentin, Julien, Géréon, Hilaire, Martin, Aignan, Benoît, Cloud [Clodoald], Ste Geneviève. Fol. 170v° : « Benedictio chrismatis principalis ». Fol. 171 : « Exorcismus olei ad baptizandos ». Fol. 173v° : In cena Domini de Flavius, évêque: « Versus Flavii episcopi ad mandatum in cena Domini ». « Tellus a cethra jubilent in magni cena principis, Que protoplasti pectora vite purgavit ferculo ; Hac nocte factor omnium potenti sat mysterio Carnem suam cum sanguine in escam transfert anime. — Tellus. » Fol. 174 : « Item versus Bedae » (Bède). « Fuit Domini dilectus languens a Bethania Lazarus beatus sacris olim cum sororibus quas Jhesus eternus Amor diligebat plurimum Martham simul et Mariam, felices per secula. » Fol. 174v° : « Feria VI quae est Parasceve ». Fol. 192v° : « Pange lingua gloriosi Proelium certaminis ». Fol. 193 : « Incipit de sabbato sancto. — Ordo baptisterii ». Fol. 200v° : Litanies. A noter : SS. Quentin, Cucuphat, Julien, Lucien, Hilaire, Martin, Benoît, Germain, Columban, Samson ; SStes Geneviève, Brigitte, Colombe, Radegonde, Aldegonde. — A noter aussi (fol. 201 vo) : « Ut exercitum Francorum conservare digneris. — Ut illum abbatem et cunctam congregationem sancti illius in tuo apto servitio conservare digneris... » Fol. 202 : « Benedictio cerei. — Exultet jam angelica turba coelorum. Exultent divina mysteria... », avec neumes. Fol. 208 : Litanies. A noter : SS. Hilaire, Martin, Ambroise, Maur, Maurille, Lezin, évêque d'Angers ; SStes Blandine, Nathalie. Fol. 210 : « Inde canitur hic versus : »« Urbs beata Hierusalem, dicta pacis visio, que construitur in celis vivis ex lapidibus... » Fol. 210v° : « Benedictio fontis ». Fol. 213 : vers « Tibi laus perennis auctor baptismatis... » Fol. 213v° : Litanies. A noter : SS. Martin, Brice, Médard, Vaast, Germain, Marcel, Hilaire ; SStes Reine, Julienne, Gertrude, Colombe, Geneviève, Afre, Radegonde, Aldegonde, Darie, Brigitte, Paule. — A noter (fol. 215) : « Ut exercitum Francorum conservare digneris. — Ut congregationem sancti Petri in tuo apto servitio conservare digneris ». Fol. 223 : « Finit ordo baptisterii ». Fol. 227 : Le jour de Pâques. Fol. 230v° : « Feria II ». Fol. 241 : « Feria quinta ». Fol. 245v° : « Feria VI ». Fol. 248 : « Sabbato ». Fol. 252v° : « In octavis Paschae ». Fol. 256v° : « Missa in octavis Paschae pro baptizatis ». Fol. 257v° : « Missa pro parroechias in diebus paschalibus... ». Fol. 258v° : « Fides catholica continens credulitatem... » Fol. 269 : « Missa pro conjugibus sterilitate infecundis in procreatione prolis ». Fol. 273v° : « Orationes ad benedicendam aquam aspergendam in domo. — Exorcismus salis ». Fol. 274 : « Benedictio salis. — Exorcismus aque. — Benedictio aque ». Fol. 274v° : « Benedictio salis et aquae... » etc. Fol. 275 : « Exorcismus salis et aquae contra fulgura ». Fol. 276 : « Benedictio salis ad pecora. — Orationes ad clericum faciendum ». Fol. 276v° : « Benedictio putei ». Fol. 277 : « Benedictio frugum novarum ». Fol. 277v° : « Benedictio panis. — Oratio ad capillarum (sic). — Alia ad tonsorandum puerum ». Fol. 278 : « Oratio post tonsionem. — Oratio ad barbas tondendas ». Fol. 278 : « lncipit actio pontificalis ad... » . Le verso du feuillet 279 est tout à fait effacé. Neumes français, du IXe s., aux f. 202-204 (l'Exultet) ; addition du Xe s. au f. 203 v° (Bernard).
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This work presents geochemistry and structural geology data concerning the low enthalpy geothermal circuits of the Argentera crystalline Massif in northwestern Italian Alps. I n this area some thermal springs (50-60 degreesC), located in the small Bagni di Vinadio village, discharge mixtures made up of a Na-Cl end-member and a Na-SO4 component. The latter is also discharged by the thermal springs of Terme di Valdieri located some kilometres apart within the same tectonic complex. Both end-members share the same meteoric origin and the same reservoir temperature, which is close to 150 degreesC. Explanations are thus required to understand how they reach the surface and how waters of the same origin and circulating in similar rocks can attain such different compositions. Sodium-sulphate waters discharged at both sites, likely represent the common interaction product of meteoric waters with the widespread granitic-migmatitic rocks of the Argentera Massif, whereas Na-CI waters originate through leaching of mineralised cataclastic rocks, which are rich in phyllosilicatic minerals and fluid inclusions, both acting as Cl- sources. Due to the relatively low inferred geothermal gradient of the region, -25C/km, meteoric waters have to descend to depths of 5.5-6 km to attain temperatures of similar to 150 degreesC. These relevant depths can be reached by descending meteoric waters, due to the recent extensional stress field, which allows the development of geothermal circulations at greater depths than in other sectors of the Alps by favouring a greater fractures aperture. The ascent of the thermal waters rakes place along brittle shear zones. In both sites, the thermal waters emerge at the bottoms of the valleys, close to either the lateral termination of a brittle shear zone at Terme di Valdieri, or a step-over between two en-echelon brittle shear zones at Bagni di Vinadio. These observations attest to a strong control operated on the location of outlet regions by both brittle tectonics and the minima in hydraulic potential inside the fractured massif.
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As a result of the construction of the Saylorville Dam and Reservoir on the Des Moines River, six highway bridges crossing the river were scheduled for removal. One of these, an old pinconnected high-truss single-lane bridge, was selected for a testing program which included ultimate load tests. The purpose of the ultimate load tests, which are summarized in this report, was to relate design and rating procedures presently used in bridge design to the field behavior of this type of truss bridge. The ultimate load tests consisted of ultimate load testing of one span of the bridge, of two I-shaped floorbeams, and of two panels of the timber deck. The theoretical capacity of each of these components is compared with the results from the field tests.