991 resultados para Mu Us sand land


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OBJECTIVE Because there is discordance between different immunoassay values for serum hGH, and because clinical state may not correlate with immunoreactive hGH, we have developed an assay to accurately measure serum hGH somatogenic bioactivity. The results of this assay were compared with the Elegance two-site ELISA assay across 135 patient samples in a variety of clinical states. DESIGN The somatogenic assay was based on stable expression of hGH receptor in the murine BaF line, allowing these cells to proliferate in response to hGH. To eliminate interference by other growth factors in serum, we created a specific antagonist of the hGH receptor (similar to Trovert or Pegvisomant) which allowed us to obtain a true measure of hGH somatogenic activity by subtraction of the activity in the presence of the antagonist. The assay was carried out in microtiter plates over 24 h, with oxidation of a chromogenic tetrazolium salt (MTT) as the endpoint. PATIENTS These encompassed a number of different clinical conditions related to short stature, including idiopathic short stature, neurosecretory dysfunction and renal failure, as well as obese patients on dietary restriction and normal volunteers. MEASUREMENTS In addition to the colourimetric (MTT) response to hGH, we measured free hGH by stripping out GHBP-bound hGH using beads coupled to a monoclonal antibody to the GHBP (GH binding protein). All samples were measured in both bioassay and ELISA assay. RESULTS This bioassay was sensitive (5 mU/l or 2 mug/l) and precise, and not subject to interference by the GHBP. There was a good correlation (r = 0.95) between bioactivity and immunoactivity across clinical states. There was, however, an increased bioactivity during secretory peaks (over 25 mU/l), which has been reported previously for the Nb2 bioassay. Free hGH did not correlate with clinical state. CONCLUSIONS Because the results of the Elegance ELISA and the bioassay correlate well, even though there is greater bioactivity at higher hormone concentrations, it is evident that an appropriate immunoassay is able to act as a reliable indicator for clinical assessment. In those rare cases where bio-inactive GH exists, our bioassay should provide an appropriate means to demonstrate this.

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This article focuses on how US professional sports utilize the New International Division of Cultural Labor to supplement an overly costly local labor pool and over-supplied local market. We argue that while the classic problem of over-production is slowly eroding the sealed-off nature of US culture, the forces of its hyper-protectionist capitalism continue to characterize sports, precluding equal exchange.

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[1] Comprehensive measurements are presented of the piezometric head in an unconfined aquifer during steady, simple harmonic oscillations driven by a hydrostatic clear water reservoir through a vertical interface. The results are analyzed and used to test existing hydrostatic and nonhydrostatic, small-amplitude theories along with capillary fringe effects. As expected, the amplitude of the water table wave decays exponentially. However, the decay rates and phase lags indicate the influence of both vertical flow and capillary effects. The capillary effects are reconciled with observations of water table oscillations in a sand column with the same sand. The effects of vertical flows and the corresponding nonhydrostatic pressure are reasonably well described by small-amplitude theory for water table waves in finite depth aquifers. That includes the oscillation amplitudes being greater at the bottom than at the top and the phase lead of the bottom compared with the top. The main problems with respect to interpreting the measurements through existing theory relate to the complicated boundary condition at the interface between the driving head reservoir and the aquifer. That is, the small-amplitude, finite depth expansion solution, which matches a hydrostatic boundary condition between the bottom and the mean driving head level, is unrealistic with respect to the pressure variation above this level. Hence it cannot describe the finer details of the multiple mode behavior close to the driving head boundary. The mean water table height initially increases with distance from the forcing boundary but then decreases again, and its asymptotic value is considerably smaller than that previously predicted for finite depth aquifers without capillary effects. Just as the mean water table over-height is smaller than predicted by capillarity-free shallow aquifer models, so is the amplitude of the second harmonic. In fact, there is no indication of extra second harmonics ( in addition to that contained in the driving head) being generated at the interface or in the interior.

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The influence of near-bed sorting processes on heavy mineral content in suspension is discussed. Sediment concentrations above a rippled bed of mixed quartz and heavy mineral sand were measured under regular nonbreaking waves in the laboratory. Using the traditional gradient diffusion process, settling velocity would be expected to strongly affect sediment distribution. This was not observed during present trials. In fact, the vertical gradients of time-averaged suspension concentrations were found to be similar for the light and heavy minerals, despite their different settling velocities. This behavior implies a convective rather than diffusive distribution mechanism. Between the nonmoving bed and the lowest suspension sampling point, fight and heavy mineral concentration differs by two orders of magnitude. This discrimination against the heavy minerals in the pickup process is due largely to selective entrainment at the ripple face. Bed-form dynamics and the nature of quartz suspension profiles are found to be little affected by the trialed proportion of overall heavy minerals in the bed (3.8-22.1%).

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Nesta pesquisa foi analisado o comportamento térmico e higrométrico em diferentes locais da Regional Praia do Canto no município de Vitória (ES) tanto no período chuvoso quanto no seco por meio da técnica de transecto móvel. A análise confirmou que as mudanças de uso e cobertura da terra associado com as características do relevo influenciam diretamente as variáveis meteorológicas, neste caso a temperatura do ar e umidade relativa do ar. A análise das condições médias de temperatura do ar e umidade relativa do ar permitiu observar dois núcleos aquecidos um ao norte e outro ao sul na área em estudo. Às 15h, tanto no verão como no inverno, a temperatura do ar atingiu o valor máximo e as taxas de umidade relativa, o seu valor mínimo. No verão e inverno, as áreas mais aquecidas ficaram bem definidas, áreas correspondentes aos núcleos aquecidos. As maiores influências do tecido urbano nas variáveis meteorológicas foram verificadas sob atuação da Alta Subtropical do Atlântico Sul. A maritimidade têm um peso importante no comportamento topoclimático urbano, sobre tudo na parte da manhã e da tarde. Na porção centro-leste da área em estudo observou-se até 3ºC a menos nos períodos vespertinos em relação aos pontos localizados na porção norte e sul. Os pontos à centroleste sofrem influência direta dos efeitos da maritimidade e dos arranjos dos prédios que formam sombreamento (Cânions Urbanos), fato que dificulta a formação de núcleos aquecidos durante o dia sobre esta porção. Foram observadas nos dois períodos, tanto no período chuvoso (verão) como também, no período seco (inverno), elevado gradiente térmico, estes localizadas onde há intenso fluxo de veículos, e também nas áreas de construção mais verticalizadas. A intensidade do gradiente térmico é maior sobre a atuação da Alta Subtropical do Atlântico Sul. Às 09 horas, são registrados os maiores gradientes térmicos para os dois períodos analisados. A umidade relativa do ar mantevese elevada durante os dois campos, tanto no verão quanto inverno. Os menores valores de umidade foram registrados em pontos que compõem o núcleo aquecido verificado na parte norte da área em estudo. Em virtude do comportamento das variáveis observadas foram identificadas três unidades Topoclimáticas Urbanas na Regional Praia do Canto.

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The aim of this article is to examine Brazil and the United States bilateral relations from 2003/2010 and their strategic patterns during the Presidency of Luis Inácio Lula da Silva. The goal is to understand the development of this dialogue in the 21st century and its previous background in the Post Cold War world, identifying its evolution and change due to Brazil's growing regional and global role and US relative position

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The article shows how domestic aspects influence the United States national and international climate policy. To accomplish the task, the authors analyzes the discussions when Bill Clinton was ruling the country, a time during which global discussions were forwarded. The paper recalls the debate in the Bush administration and the growing polarization since Barack Obama took office.

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This article is divided in three sections. The first one explores the so-called "strategic partnership" between Brazil and China. In the second section we shall examine how US-China relations in the global system could affect both Brazil-US, and Brazil-China bilateral relations. A final section presents some recommendations for Brazil strategic orientations regarding the current systemic transition in the allotment of global power.

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The United States has gone further than any country in the "privatization of security". Other countries may find the economic or financial logic in the use of contractors persuasive. The US experience with contracting out security, particularly in Iraq, was problematic, and can serve as a cautionary tale in order that other countries might learn how to avoid the pitfalls.