Time transcendence, metadata and future utilization in 3D models of point clouds for heritage elements

Contributed to: Virtual Retrospect 2007 (Pessac, France, Nov 14-16, 2007)

Shoreline erosion due to extreme storms and sea level rise

A summary is presented of research conducted on beach erosion associated with extreme storms and sea level rise. These results were developed by the author and graduate students under sponsorship of the University of Delaware Sea Grant Program. Various shoreline response problems of engineering interest are examined. The basis for the approach is a monotonic equilibrium profile of the form h = Ax2 /3 in which h is water depth at a distance x from the shoreline and A is a scale parameter depending primarily on sediment characteristics and secondarily on wave characteristics. This form is shown to be consistent with uniform wave energy dissipation per unit volume. The dependency of A on sediment size is quantified through laboratory and field data. Quasi-static beach response is examined to represent the effect of sea level rise. Cases considered include natural and seawalled profiles. To represent response to storms of realistic durations, a model is proposed in which the offshore transport is proportional to the "excess" energy dissipation per unit volume. The single rate constant in this model was evaluated based on large scale wave tank tests and confirmed with Hurricane Eloise pre- and post-storm surveys. It is shown that most hurricanes only cause 10% to 25% of the erosion potential associated with the peak storm tide and wave conditions. Additional applications include profile response employing a fairly realistic breaking model in which longshore bars are formed and long-term (500 years) Monte Carlo simulation including the contributions due to sea level rise and random storm occurrences. (PDF has 67 pages.)

Beach monitoring project Sand Key Phase II Beach nourishment program (North Redington Beach and Redington Shores) Post-Nourishment Report Part II Offshore Profiles and Wave Data

This study presents the third post-nourishment survey (January 1989) results for the Sand Key Phase II beach nourishment project carried out in June, 1988. The monitoring program to this beach nourishment project is a joint effort between the University of South Florida and University of Florida. The field surveys include a total of 26 profiles, encompassing approximately 3 miles of shoreline extending from DNR R-96 to R-1ll. The total calculated volume loss of sand in the nourished segment (from R-99G to R-107) between the July 88 and January 89 surveys is 51,113 cubic yards, which is a loss about 9.7 percent of 529,150 cubic yards actually placed in the nourishment project. The total loss of sand computed in the entire survey area is 26,796 cubic yards, which is only 5.1 percent of the sand placed in the nourishment project. It is stressed that a part of these net volume reductions is due to the background erosion and not due to spreading losses induced by the nourishment project. (PDF contains 168 pages.)

Antioxidant defense system and family environment in adolescents with family history of psychosis

[EN] Our objective was to determine antioxidant defence activity in healthy controls (HC) and healthy unaffected second-degree relatives of patients with early onset psychosis (HC-FHP),and to assess its relationship with familiar environment measured using the Family Environment Scale (FES). Methods: We included 82 HC and 14 HC-FHP aged between 9 and 17 years. Total antioxidant status,lipid peroxidation, antioxidant enzyme activities and glutathione levels were determined in blood samples. Results:There was a significant decrease in the total antioxidant level in the HC-FHP group compared with the HC group (OR = 2.94; p = 0.009), but no between-group differences in the Global Assessment of Functioning (GAF) scale scores. For the FES, the HC-FHP group had significantly higher scores in the cohesion (p = 0.007) and intellectual-cultural dimensions (p=0.025). After adjusting for these two FES dimensions, total antioxidant status remained significantly different between groups (OR = 10.86, p = 0.009).

Community structure in real-world networks from a non-parametrical synchronization-based dynamical approach

[EN]This work analyzes the problem of community structure in real-world networks based on the synchronization of nonidentical coupled chaotic Rössler oscillators each one characterized by a defined natural frequency, and coupled according to a predefined network topology. The interaction scheme contemplates an uniformly increasing coupling force to simulate a society in which the association between the agents grows in time. To enhance the stability of the correlated states that could emerge from the synchronization process, we propose a parameterless mechanism that adapts the characteristic frequencies of coupled oscillators according to a dynamic connectivity matrix deduced from correlated data. We show that the characteristic frequency vector that results from the adaptation mechanism reveals the underlying community structure present in the network.

Alternative income in Kainji Lake area: introduction of improved cocks to fisherfolk

Details are given of a study conducted in the framework of the Kainji Lake Fisheries Promotion Project to boost income from alternative sources. The project identified 'improved poultry keeping' as suitable for introduction around the Kainji Lake area. In the long term, the programme will assist increasing especially the income of female members of fishing families, since poultry is kept in the villages mainly by women. (PDF contains 35 pages)

Evaluation of the body burdens of heavy metals in five commercially important fishes from different locations in Kainji Lake

The level and distribution of some heavy metals viz Cadmium, Lead, Copper Zinc, and Cobalt in five commercially important fishes, water and sediments at three different locations in Kainj Lake were determined using standard methods. The results show that the ranges of heavy metals mu g/g in fishes in Dam site Laotian are: Cd (0.05~c0.01-20~c01), (Pb(ND-1.12 plus or minus )1), Cu (0.81~c25-2.93~c06), Zn (20.89 arrow right .15-36.78~c2.97), Co(0.08~c01-0.27~c02); in cover Dam, the ranges are Cd (0.04~c02-0.16~c0.2), Pb (nd-02~c01), Cu(0.75~c05-2.61~c13), Zn(15.70~c1.55-32.23~c2.70), Co(0.04~c02-0.25~c0.01) and in Yuna they are Cd (0.05~c01-0.14~c02), Pb (nd-0.32~c01), Cu (0.23~c07-2.70~c05), Zn(15.50 plus or minus `.35-25.62~c2.47), Co(0.07~c02-23~c0.01). The metals concentration (mg/l) in the water sample from Dam site, cover dam and Yuna respectively are Cd(0.007~c001,. 004~c001 and 0.005~001), Pb(013~c001, ND and ND), Cu(.055~c008.030~c007, 05 plus or minus .010), Zn(0.13~c01, 0.060 plus or minus .0055) and Co (.026 plus or minus .022 plus or minus .004, .024 plus or minus .004), while the metals concentration ( mu g/g) in sediments sample from Dam site, cover dam and Yuna are respectively Cd(.05 plus or minus .01, .02 plus or minus .01), Pb(16.00~c1.00, ND and 9.33~c1.01), Cu(24.00~c1.34, 4.26 plus or minus .91 and 11.08~c1.32), Zn(42.00~c1.00, 35~c10 and 38.00 plus or minus .45), Co(15.00~c1.17, 8.69~c1.21 and 10.91~c44). The concentrations of the tested heavy metals are within the acceptable standards of WHO (1987a)

Padrões de consumo alimentar e índice de massa corporal nas regiões nordeste e sudeste do Brasil

O presente estudo avaliou os padrões de consumo alimentar entre adultos brasileiros e a sua associação com o Índice de Massa Corporal (IMC). Em 1996/1997, o Instituto Brasileiro de Geografia e Estatística (IBGE), coletou dados antropométricos, de consumo alimentar e socioeconômicos de 9351 indivíduos entre 20 e 60 anos, moradores das áreas urbanas e rurais das regiões Nordeste e Sudeste do Brasil. Através da análise de componentes principais foram identificados os padrões de consumo alimentar. A associação entre os padrões de consumo alimentar e o IMC foi avaliado através de regressão linear. A prevalência de obesidade (IMC >= 30 kg/rn2) foi de 2,7% entre homens moradores das áreas rurais e em torno de 8,0% para os moradores da área urbana, em ambas as regiões. Entre as mulheres, esta prevalência na área rural foi de 6,5% no Nordeste, 14,3% no Sudeste e em torno de 12% nas áreas urbanas. A prevalência de sobrepeso (IMC>= 25 kg/m2) na área rural foi, aproximadamente, 20,0%para o sexo masculino e 24,0% para o sexo feminino, ficando ao redor de 30% nas áreas urbanas. Identificou-se três padrões de consumo: o padrão 1 (misto), com o consumo de quase todos os alimentos, o padrão 2, um padrão a base de arroz, farinha e feijão, composição característica da dieta tradicional do brasileiro, e o padrão 3, onde poucos alimentos explicaram a variação de consumo, contudo, estes alimentos variaram nas quatro áreas. Ajustando-se para idade, renda, escolaridade e atividade física, o padrão misto associou-se positivamente com o IMC (p<0,003), exceto no Sudeste rural (p=016). A dieta tradicional no Sudeste rural (p=0,007) e o padrão 3, composto por tubérculos, farinha e carne, no Nordeste urbano (p=O,0004), associaram-se negativamente com o IMC. Concluiu-se que o padrão misto se associou positivamente ao IMC, sugerindo que o consumo calórico total, mais do que o padrão da dieta, explicaria o aumento da obesidade observado no Brasil.

Excitation energies and decay properties of T = 3/2 states in ^(17)O, ^(17)F and ^(21)Na

The two lowest T = 3/2 levels in ²¹Na have been studied in the ¹⁹F(³He, n), ²⁰Ne (p,p) and ²⁰Ne (p,p’) reactions, and their excitation energies, spins, parities and widths have been determined. In a separate investigation, branching ratios were measured for the isospin-nonconserving particle decays of the lowest T = 3/2 levels in ¹⁷O and ¹⁷F to the ground state and first two excited states of ¹⁶O, by studying the ¹⁵N(³He,n) ¹⁷F*(p) ¹⁶O and ¹⁸O(³He, α)¹⁷O*(n) ¹⁶O reactions.

The ¹⁹F(³He,n) ²¹Na reaction was studied at incident energies between 4.2 and 5.9 MeV using a pulsed-beam neutron-time-of-flight spectrometer. Two T = 3/2 levels were identified at excitation energies of 8.99 ± 0.05 MeV (J > ½) and 9.22 ± 0.015 MeV (J ^π = ½⁺, Γ ˂ 40 keV). The spins and parities were determined by a comparison of the measured angular distributions with the results of DWBA calculations.

These two levels were also obsesrved as isospin-forbidden resonances in the ²⁰Ne(p,p) and ²⁰Ne(p,p’) reactions. Excitation energies were measured and spins, parities, and widths were determined from a single level dispersion theory analysis. The following results were obtained:

E_x = 8.973 ± 0.007 MeV, J ^π = 5/2 ⁺ or 3/2⁺, Γ ≤ 1.2 keV,

^Γp_o = 0.1 ± 0.05 keV; E_x = 9.217 ± 0.007 MeV, J^π = ½ ⁺,

Γ = 2.3 ± 0.5 keV, ^Γp_o = 1.1 ± 0.3 keV.

Isospin assignments were made on the basis of excitation energies, spins, parities, and widths.

Branching ratios for the isospin-nonconserving proton decays of the 11.20 MeV, T = 3/2 level in ¹⁷F were measured by the ¹⁵N(³He,n) ¹⁷ F*(p) ¹⁶O reaction to be 0.088 ± 0.016 to the ground state of ¹⁶O and 0.22 ± 0.04 to the unresolved 6.05 and 6.13 MeV levels of ¹⁶O. Branching ratios for the neutron decays of the analogous T = 3/2 level, at 11.08 MeV in ¹⁷O, were measured by the ¹⁶O(³He, α)¹⁷O*(n)¹⁶O reaction to be 0.91 ± 0.15 to the ground state of ¹⁶O and 0.05 ± 0.02 to the unresolved 6.05 and 6.13 MeV states. By comparing the ratios of reduced widths for the mirror decays, the form of the isospin impurity in the T = 3/2 levels is shown to depend on T_z.

A study of T=1, T=3/2, and T=2 states in some light nuclei using (He^3,n) reactions

The (He³, n) reactions on B¹¹, N¹⁵, O¹⁶, and O¹⁸ targets have been studied using a pulsed-beam time-of-flight spectrometer. Special emphasis was placed upon the determination of the excitation energies and properties of states with T = 1 (in Ne¹⁸), T = 3/2 (in N¹³ and F¹⁷) and T = 2 (in Ne²⁰). The identification of the T = 3/2 and T = 2 levels is based on the structure of these states as revealed by intensities and shapes of angular distributions. The reactions are interpreted in terms of double stripping theory. Angular distributions have been compared with plane and distorted wave stripping theories. Results for the four reactions are summarized below:

1) O¹⁶ (He³, n). The reaction has been studied at incident energies up to 13.5 MeV and two previously unreported levels in Ne¹⁸ were observed at E_x = 4.55 ± .015 MeV (Γ = 70 ± 30 keV) and E_x = 5.14 ± .018 MeV (Γ = 100 ± 40 keV).

2) B¹¹ (He³, n). The reaction has been studied at incident energies up to 13.5 MeV. Three T = 3/2 levels in N¹³ have been identified at E_x = 15.068 ± .008 MeV (Γ ˂ 15 keV), E_x = 18.44 ± .04, and E_x 18.98 ± .02 MeV (Γ = 40 ± 20 keV).

3) N¹⁵ (He³, n). The reaction has been studied at incident energies up to 11.88 MeV. T = 3/2 levels in F¹⁷ have been identified at E_x = 11.195 ± .007 MeV (Γ ˂ 20 keV), E_x = 12.540 ± .010 MeV (Γ ˂ 25 keV), and E_x = 13.095 ± .009 MeV (Γ ˂ 25 keV).

4) O¹⁸ (He³, n). The reaction has been studied at incident energies up to 9.0 MeV. The excitation energy of the lowest T = 2 level in Ne²⁰ has been found to be 16.730 ± .006 MeV (Γ ˂ 20 keV).

Angular distributions of the transitions leading to the above higher isospin states are well described by double stripping theory. Analog correspondences are established by comparing the present results with recent studies (t, p) and (He³, p) reactions on the same targets.

Solubility and Diffusivity of Water in Lunar Basalt, and Chemical Zonation in Olivine-Hosted Melt Inclusions

I report the solubility and diffusivity of water in lunar basalt and an iron-free basaltic analogue at 1 atm and 1350 °C. Such parameters are critical for understanding the degassing histories of lunar pyroclastic glasses. Solubility experiments have been conducted over a range of fO₂ conditions from three log units below to five log units above the iron-wüstite buffer (IW) and over a range of pH₂/pH₂O from 0.03 to 24. Quenched experimental glasses were analyzed by Fourier transform infrared spectroscopy (FTIR) and secondary ionization mass spectrometry (SIMS) and were found to contain up to ~420 ppm water. Results demonstrate that, under the conditions of our experiments: (1) hydroxyl is the only H-bearing species detected by FTIR; (2) the solubility of water is proportional to the square root of pH₂O in the furnace atmosphere and is independent of fO₂ and pH₂/pH₂O; (3) the solubility of water is very similar in both melt compositions; (4) the concentration of H₂ in our iron-free experiments is <3 ppm, even at oxygen fugacities as low as IW-2.3 and pH₂/pH₂O as high as 24; and (5) SIMS analyses of water in iron-rich glasses equilibrated under variable fO₂ conditions can be strongly influenced by matrix effects, even when the concentrations of water in the glasses are low. Our results can be used to constrain the entrapment pressure of the lunar melt inclusions of Hauri et al. (2011).

Diffusion experiments were conducted over a range of fO₂ conditions from IW-2.2 to IW+6.7 and over a range of pH₂/pH₂O from nominally zero to ~10. The water concentrations measured in our quenched experimental glasses by SIMS and FTIR vary from a few ppm to ~430 ppm. Water concentration gradients are well described by models in which the diffusivity of water (D^*_water) is assumed to be constant. The relationship between D^*_water and water concentration is well described by a modified speciation model (Ni et al. 2012) in which both molecular water and hydroxyl are allowed to diffuse. The success of this modified speciation model for describing our results suggests that we have resolved the diffusivity of hydroxyl in basaltic melt for the first time. Best-fit values of D^*_water for our experiments on lunar basalt vary within a factor of ~2 over a range of pH₂/pH₂O from 0.007 to 9.7, a range of fO₂ from IW-2.2 to IW+4.9, and a water concentration range from ~80 ppm to ~280 ppm. The relative insensitivity of our best-fit values of D^*_water to variations in pH₂ suggests that H₂ diffusion was not significant during degassing of the lunar glasses of Saal et al. (2008). D^*_water during dehydration and hydration in H₂/CO₂ gas mixtures are approximately the same, which supports an equilibrium boundary condition for these experiments. However, dehydration experiments into CO₂ and CO/CO₂ gas mixtures leave some scope for the importance of kinetics during dehydration into H-free environments. The value of D^*_water chosen by Saal et al. (2008) for modeling the diffusive degassing of the lunar volcanic glasses is within a factor of three of our measured value in our lunar basaltic melt at 1350 °C.

In Chapter 4 of this thesis, I document significant zonation in major, minor, trace, and volatile elements in naturally glassy olivine-hosted melt inclusions from the Siqueiros Fracture Zone and the Galapagos Islands. Components with a higher concentration in the host olivine than in the melt (MgO, FeO, Cr₂O₃, and MnO) are depleted at the edges of the zoned melt inclusions relative to their centers, whereas except for CaO, H₂O, and F, components with a lower concentration in the host olivine than in the melt (Al₂O₃, SiO₂, Na₂O, K₂O, TiO₂, S, and Cl) are enriched near the melt inclusion edges. This zonation is due to formation of an olivine-depleted boundary layer in the adjacent melt in response to cooling and crystallization of olivine on the walls of the melt inclusions concurrent with diffusive propagation of the boundary layer toward the inclusion center.

Concentration profiles of some components in the melt inclusions exhibit multicomponent diffusion effects such as uphill diffusion (CaO, FeO) or slowing of the diffusion of typically rapidly diffusing components (Na₂O, K₂O) by coupling to slow diffusing components such as SiO₂ and Al₂O₃. Concentrations of H2O and F decrease towards the edges of some of the Siqueiros melt inclusions, suggesting either that these components have been lost from the inclusions into the host olivine late in their cooling histories and/or that these components are exhibiting multicomponent diffusion effects.

A model has been developed of the time-dependent evolution of MgO concentration profiles in melt inclusions due to simultaneous depletion of MgO at the inclusion walls due to olivine growth and diffusion of MgO in the melt inclusions in response to this depletion. Observed concentration profiles were fit to this model to constrain their thermal histories. Cooling rates determined by a single-stage linear cooling model are 150–13,000 °C hr^-1 from the liquidus down to ~1000 °C, consistent with previously determined cooling rates for basaltic glasses; compositional trends with melt inclusion size observed in the Siqueiros melt inclusions are described well by this simple single-stage linear cooling model. Despite the overall success of the modeling of MgO concentration profiles using a single-stage cooling history, MgO concentration profiles in some melt inclusions are better fit by a two-stage cooling history with a slower-cooling first stage followed by a faster-cooling second stage; the inferred total duration of cooling from the liquidus down to ~1000 °C is 40 s to just over one hour.

Based on our observations and models, compositions of zoned melt inclusions (even if measured at the centers of the inclusions) will typically have been diffusively fractionated relative to the initially trapped melt; for such inclusions, the initial composition cannot be simply reconstructed based on olivine-addition calculations, so caution should be exercised in application of such reconstructions to correct for post-entrapment crystallization of olivine on inclusion walls. Off-center analyses of a melt inclusion can also give results significantly fractionated relative to simple olivine crystallization.

All melt inclusions from the Siqueiros and Galapagos sample suites exhibit zoning profiles, and this feature may be nearly universal in glassy, olivine-hosted inclusions. If so, zoning profiles in melt inclusions could be widely useful to constrain late-stage syneruptive processes and as natural diffusion experiments.

Mortalidade por asma no município do Rio de Janeiro no período de 2000 2009: análise de causas múltiplas

O estudo das causas múltiplas de óbitos permite conhecer a extensão real das estatísticas de mortalidade, minimizando a subestimação dos dados de mortalidade por asma. O objetivo desta pesquisa foi avaliar a tendência das taxas de mortalidade por asma informada em qualquer linha ou parte do atestado médico da declaração de óbito, no município do Rio de Janeiro, no período de 2000-2009. Os dados foram obtidos no Sistema de Informações de Mortalidade (SIM), no período de 2000 a 2009, nas Declarações de Óbitos (DO) registradas com CID-10 J45 e J46, de residentes do município do Rio de Janeiro, com um ano ou mais de idade. Foram calculadas taxas de mortalidade padronizadas por idade, nas seguintes faixas etárias: 1-4 anos, 5-34 anos, 35-59 anos, 60 e mais anos, considerando-se asma como causa básica e como causas múltiplas, segundo gênero para cada ano do período. Para análise de dados foi utilizado a técnica de regressão linear. No período de 10 anos a asma foi causa básica em 67,2% dos óbitos que mencionaram asma. A subestimação da mortalidade por asma como causa básica, foi igual a 48,7%. A taxa de mortalidade padronizada por asma como causa básica declinou de 2000 a 2009 de 2,22 para 1,72/100.000 habitantes em 2009, (β= -0.06, p=0.017) e como causas múltiplas passou de 3,45 para 2,82/100.000 habitantes (β= -0.11, p=0.005). A análise segundo gênero evidenciou um declínio mais acentuado entre os homens, cuja taxa de mortalidade por asma como causa básica padronizada passou de 1,58/100.000 em 2000 para 0,59/100.000 em 2009 (β= -0.08, p=0.007); como causa múltipla a taxa diminuiu de 2,49/100.000 em 2000 para 1,11/100.000 em 2009 (β= -0.14, p<0.00001). Entre as mulheres a taxa de mortalidade passou de 2,79/100.000 em 2000 para 2,72/100.000 em 2009 como causa básica e de 4,29/100.000 em 2000 para 4,32/100.000 em 2009. A regressão linear segmentada, realizada em dois períodos, de 2000 a 2004 e 2004 a 2009, não foi estatisticamente significativa (2000 a 2004: β= -0,16, p=0,131 e 2004 a 2009: β= 0,04, p=0,630). Do total de óbitos nos quais a asma foi mencionada como causa múltipla 2,8% ocorreram na idade de 1 a 4 anos e 61% na faixa de 60 anos e mais. Quando a asma foi causa básica, as causas associadas mais frequentes foram as doenças do aparelho respiratório e nos óbitos em que foi classificada como causa associada destacaram-se como causas básicas as doenças do aparelho respiratório e circulatório. A magnitude das taxas de mortalidade por asma foi sempre maior nas mulheres comparado aos homens. A série histórica mostrou tendência ao declínio nas taxas de mortalidade, segundo causas básicas e múltiplas, com declínio entre os homens e estabilidade entre as mulheres. A mortalidade por asma foi subestimada quando considerada apenas como causa básica, o que poderia ser evitado com a utilização da metodologia de causas múltiplas nas estatísticas de mortalidade da asma.

Determinação de clorobenzenos em água por cromatografia de fase gasosa com headspace

As preocupações com o meio ambiente em particular com a água, adquirem especial importância, porque as demandas estão se tornando cada vez maiores, sob o aspecto crescente da população e das atividades industriais. Quando se fala em água subterrânea, a primeira ideia que surge é que ela seja potável. Mas nem sempre isso é uma verdade. Em área urbana, os crescentes números de problemas devido a contaminação, na maioria das vezes por vazamentos de combustíveis oriundos dos tanques de armazenamento dos postos de gasolina. Sem falar nas indústrias que também oferecem potencial risco de contaminação para esses corpos hídricos e são pouco divulgadas. O presente trabalho tem como foco determinar os compostos clorobenzenos por cromatografia de fase gasosa com headspace (CG-HS) em matriz água e validar a metodologia. A metodologia usada neste estudo foi cromatografia de fase gasosa com headspace (CG HS), por ser uma técnica excelente e sensível e é utilizada para determinar compostos voláteis em baixas concentrações. Os dados obtidos foram tratados estatisticamente de modo avaliar a seletividade, os limites de detecção e quantificação, a faixa linear de trabalho, a linearidade e a recuperação. As recuperações variam de 80 a 110%, os coeficientes de variação obtidos foram menor que 20%, todas as substâncias estudadas apresentaram linearidade na faixa de trabalho de 0,8 a 100g.L-1. Foram estudadas 10 amostras de água subterrânea do Município do Rio de Janeiro e nas amostras analisadas foram encontrados todos os compostos em estudo, com faixa de concentração: monoclorobenzeno (<0,8 a 2,988g.L-1); 1,3-diclorobenzeno (<0,8 a 23,067g.L-1); 1,4-diclorobenzeno (nd a 16,160g.L-1); 1,2-diclorobenzeno (<0,8 a 48,685g.L-1); 1,3,5-triclorobenzeno (<0,8 a 21,900g.L-1); 1,2,4-triclorobenzeno (1,007 a 183,808g.L-1) e 1,2,3-triclorobenzeno (<0,8 a 126,886g.L-1)

Fatores associados a óbito e hospitalizações em uma clínica de insuficiência cardíaca

Trata-se de um estudo descritivo, retrospectivo, com abordagem quantitativa cujo objetivo geral foi descrever e analisar o perfil epidemiológico dos pacientes com Insuficiência Cardíaca atendidos pela Clinica de IC de um Hospital Universitário. Os objetivos específicos orientam-se para:(a)Caracterizar os casos de Insuficiência Cardíaca segundo variáveis demográficas, variáveis clínicas, de diagnóstico e co morbidades;(b)Comparar as características clínicas e demográficas dos pacientes conforme grupos etiológicos identificados e fração de ejeção;(c)Determinar a taxa de mortalidade e hospitalização dos pacientes acompanhados pela clínica. Os dados analisados neste estudo são oriundos de um banco de dados onde são alocadas informações dos pacientes em atendimento ambulatorial da referida clinica.Para a análise dos dados foi utilizada a estatística descritiva, freqüências e porcentagens assim como tabelas e gráficos para a demonstração dos dados levantados.Os mesmos foram analisados através do software SPSS v.18.0, no qual se utilizou a estatística multivariada e curvas de sobrevida de Kaplan-Meyer.Os resultados apontam para uma predominância masculina de 60,1%, com idade de 63,5 anos. Na caracterização quanto à classe funcional observa-se que a predominante é a classe funcional I e II com 73,6% do total. Os pacientes assistidos apresentam uma média de 42% da fração de ejeção do ventrículo esquerdo e 61,7% possuem etiologia não isquêmica. Em nosso estudo, descrevemos 71,8% de portadores de disfunção sistólica. Os pacientes com etiologia isquêmica tinham predomínio do sexo masculino(70,7%), e a etiologia não isquêmica com uma prevalência maior do sexo feminino(45,5%vs 29,3%;p<0,001). Além disso, os pacientes isquêmicos eram mais idosos (p<0,001), com historia familiar de DAC(p<0,041), presença de diabetes (p<0,001). A disfunção sistólica(FE<50%) era predominante no grupo de pacientes isquêmicos(77%vs 69%; p=0,048).As classes funcionais mais avançadas(III e IV) foram menos predominantes nos indivíduos isquêmicos(32,5%) em relação aos não isquêmicos(41,3%;p=0,041).O paciente de etiologia isquêmica recebeu tratamento farmacológico semelhante ao não isquêmico com exceção do uso de AAS(p<0,001).Esses indivíduos cursaram com maior numero de internações por outras causas exceto IC(p<0,001) e maior numero de óbitos(p=0,007).Em relação à fração de ejeção, observou-se que indivíduos com FE>50% tinham predomínio do sexo feminino(p=0,006),mais idosos(p<0,001),de etiologia não isquêmica(p=0,048) e classes funcionais I e II(p=0,025).Indivíduos com FE<50% eram mais graves, apresentando maior número de internações por IC(37,8%vs20%;p<0,001), e internações por outras causas(27,2%vs17,5%;p=0,018) e maior número de óbitos (18%vs8,4%;p=0,005) do que os com fração de ejeção preservada. O resultado desse estudo teve como finalidade o conhecimento do perfil de uma população própria, com o objetivo de aprimorar a assistência prestada a ela. Os enfermeiros de Clínicas de IC, juntos com os profissionais da equipe multidisciplinar, desempenham papel fundamental no acompanhamento, orientação e educação desses pacientes.