O crescimento no primeiro ano de vida e o excesso de peso no início da idade escolar

INTRODUÇÃO - A obesidade é uma preocupação de saúde pública cada vez mais importante, em todo o mundo. A obesidade infantil, por sua vez, vem sendo associada a um alto risco de agravos infantis e de obesidade e doenças crônicas não transmissíveis na fase adulta. Admite-se que o início da vida seja um momento crítico e determinante para o risco do indivíduo desenvolver sobrepeso ou obesidade. Entretanto, não está definido se existe algum período de maior vulnerabilidade na fase pós-natal e qual seria o melhor marcador do crescimento da criança para indicar uma possível intervenção precoce que possa minimizar o risco de desenvolver excesso de peso ou obesidade. OBJETIVO - Analisar as relações existentes entre indicadores antropométricos de crescimento no primeiro ano de vida e o desenvolvimento de excesso de peso no início da idade escolar. MÉTODOS - Estudo de uma coorte histórica de uma unidade básica de saúde em São Paulo, Brasil. Os momentos analisados foram aos três, seis e doze meses e aos sete anos de idade. Avaliou-se a velocidade de crescimento e o crescimento alcançado durante o primeiro ano de vida frente aos desfechos: excesso de peso e obesidade aos sete anos de idade. As variáveis foram analisadas estatisticamente através do Coeficiente de Correlação de Pearson e das curvas ROC, além de terem sido estimadas a sensibilidade, a especificidade e o risco relativo. RESULTADOS - Os Coeficientes de Correlação de Pearson do ganho de peso por ganho de comprimento nos períodos de 0 a 3 meses, 0 a 6 meses e 0 a 12 meses foram, respectivamente, 0,23 (IC 95 por cento : 0,13 a 0,33), 0,29 (IC 95 por cento : 0,19 a 0,39) e 0,34 (IC 95 por cento : 0,24 a 0,43), todos significantes estatisticamente. Os Coeficientes de Correlação de Pearson do escore z do Índice de Massa Corpórea (IMC) para 3, 6 e 12 meses foram, respectivamente, 0,39 (IC 95 por cento : 0,29 a 0,48), 0,41 (IC 95 por cento : 0,32 a 0,50) e 0,42 (IC 95 por cento : 0,33 a 0,51). Para excesso de peso na idade escolar, a utilização do marcador escore z do IMC aos 12 meses maior que 0,49 apresentou sensibilidade de 68,29 por cento (IC 95 por cento : 59,3 por cento a 76,4 por cento ), especificidade de 63,51 por cento (IC 95 por cento : 56,6 por cento a 70,0 por cento ) e risco relativo estimado de 2,31 (IC 95 por cento : 1,69 a 3,17). Para obesidade, o mesmo marcador apresentou sensibilidade de 76,47 por cento (IC 95 por cento : 62,5 por cento a 87,2 por cento ), especificidade de 56,89 por cento (IC 95 por cento : 50,9 por cento a 62,7 por cento ) e risco relativo estimado de 3,49 (IC 95 por cento : 1,90 a 6,43). CONCLUSÕES - O primeiro trimestre de vida se revelou como sendo o período mais crítico, entre os estudados, para o desenvolvimento de sobrepeso ou obesidade no início da idade escolar. No entanto, o escore z do IMC acima de 0,49 aos 12 meses de vida se mostrou como o melhor marcador para esses dois desfechos.

Procedure for calculating the chloride diffusion coefficient and surface concentration from a profile having a maximum beyond the concrete surface

Chlorides induce local corrosion in the steel reinforcements when reaching the bar surface. The measurement of the rate of ingress of these ions, is made by mathematically fitting the so called “error function equation” into the chloride concentration profile, obtaining so the diffusion coefficient and the chloride concentration at the concrete surface. However, the chloride profiles do not always follow Fick’s law by having the maximum concentration at the concrete surface, but often the profile shows a maximum concentration more in the interior, which indicates a different composition and performance of the most external concrete layer with respect to the internal zones. The paper presents a procedure prepared during the time of the RILEM TC 178-TMC: “Testing and modeling chloride penetration in concrete”, which suggests neglecting the external layer where the chloride concentration increases and using the maximum as an “apparent” surface concentration, called C max and to fit the error function equation into the decreasing concentration profile towards the interior. The prediction of evolution should be made also from the maximum.

An R script to plot the conditioned Gini (or skewness) coefficient in the bivariate case

In the cs.index.zip file we provide an R script which let us plot the conditioned Gini (or skewness) coefficient used in the working paper entitled "On conditional skewness with applications in environmental data" submitted to Environmental and Ecological Statistics. On the other hand, the ReadMe.pdf explains how to use the cs.index.R script.

Heat flow and heat conductivity coefficient measured in bottom sediments collected in Cruise 13 of R/V Akademik Sergey Vavilov in the Pechora Sea

In Cruise 13 of R/V Akademik Sergey Vavilov in the Pechora Sea, six heat flow varied from 50 to 75 mW/m**2. Deep heat flow in the Pechora Sea was calculated equal to 45 mW/m**2, which is confirmed by results of geological and geophysical studies and corresponds to Middle Baikal age of the basement. A model of structure of the lithosphere in the Pechora Sea is suggested. Total thickness of the lithosphere in the basin (190 km) determined from geothermal data agrees well with that in transition zones from the continent to the ocean. According to estimates of deep heat flow in the region obtained, thickness of the mantle (160 km), of the basaltic (15 km), and of the granitic (15 km) layers of the lithosphere were also evaluated. Temperature values at boundaries of the sedimentary layers were calculated over a geological and geophysical profile crossing the Pechora Sea basin. Temperatures obtained agree with the temperature interval of hydrocarbon generation and correspond to Permian-Triassic sedimentary sequences, which are the most productive ones in the Pechora Sea region from the point of view of oil and gas potential.

(Table 1) Magnetic viscosity coefficient, VRM and NRM of DSDP Hole 6-57

THE magnetic properties of the basalts which form layer 2 of the oceanic lithosphere are important because of their relevance to the hypothesis (Vine and Matthews, 1963, doi:10.1038/199947a0) of seafloor spreading. Most studies of these magnetic properties have been carried out on basalts obtained from dredge hauls taken predominantly from ocean ridge systems and fracture zones. These constitute special areas of the oceanic crust where the sediment cover is negligible. It is of interest to compare the magnetic properties of the dredged basalts with samples recovered from holes drilled through the overlying sediments into the basaltic layer at places distant from ridge axes. Samples obtained from the abandoned Mohole project and, more recently, from the Deep Sea Drilling Project (DSDP) possessed magnetic properties similar to those of dredged basalts (Cox and Doell, 1962, doi:10.1029/JZ067i010p03997; Lowrie et al., 1973, doi:10.1016/0012-821X(73)90198-2). Here I describe highly unstable magnetic characteristics found in basalts from DSDP hole 57.

Effects of internal gain assumptions in building energy calculations /

The utilization of direct solar gains in buildings can be affected by operating profiles, such as schedules for internal gains, thermostat controls, and ventilation rates. Building energy analysis methods use various assumptions about these profiles. This paper describes the effects of typical internal gain assumptions in energy calculations. The results of this study indicate that calculations of annual heating and cooling loads are sensitive to internal gains, but in most cases are relatively insensitive to hourly variation in internal gains.

Determining discharge-coefficient ratings for selected coastal control structures in Broward and Palm Beach counties, Florida /

Shipping list no.: 99-0001-P.

Effect of rate of change of slip on the peak braking coefficient of passenger car tires. Technical report.

Mode of access: Internet.

Zoune chez sa ninnaine : fan'm gain sept sauts pou li passé /

Reprint of the Port-au-Prince 1906 ed.

Coefficient generator and cursor for the stereomatrix 3-D display system,

"Supported in part by contract no. Atomic Energy Commission AT(11-1)1469."

System and circuit design of the transformatrix coefficient processor and output data channel,

Vita.

Path integral calculation of the three-particle direct and exchange contributions to the pair distribution function and of the third virial coefficient for He4 gas /

Thesis--Illinois.