COMPARAÇÃO DO ATRITO IN VITRO EM BRAQUETES ESTÉTICOS CONVENCIONAIS E AUTOLIGADOS

O objetivo do presente estudo consistiu em comparar in vitro o atrito produzido por braquetes estéticos, convencionais e autoligados quando inseridos fios retangulares de aço inoxidável de diferentes dimensões, nas angulações de zero e três graus entre os braquetes. Foram utilizados 120 braquetes de 6 marcas comerciais (Gemini, Clarity convencional, Transcend, Inspire, Clarity autoligado, Damon autoligado), sendo 20 braquetes de cada marca comercial. Para os ensaios laboratoriais, foram colados dois pares de braquetes de cada marca comercial em uma placa metálica, com uma angulação de zero e três graus entre os braquetes. Foram empregados os fios retangulares de aço inoxidável 0,017 x 0,025 , 0,019 x 0,025 e 0,021 x0,025 em uma máquina de ensaios universal Instron . Para a comparação entre os braquetes nos diferentes fios e angulações, foi utilizada a análise de variância e o teste de Tukey (p<0,05). Os resultados demonstraram que na angulação de zero grau, os braquetes autoligados apresentaram menor atrito em relação aos convencionais em todos os fios avaliados, sendo que, o braquete Clarity autoligado apresentou menor atrito estatisticamente significante que o Damon, exceto no fio 0,021 x 0,025 , em que ambos os braquetes autoligados apresentaram atrito estatisticamente semelhante. O braquete Inspire demonstrou o maior atrito em relação aos demais braquetes nos fios 0,019 x0,025 e 0,021 x0,025 . Na angulação de três graus, observou-se resultados semelhantes aos braquetes posicionados sem angulação comparando os braquetes autoligados em relação aos convencionais. Contudo, verificou-se que o atrito entre os braquetes convencionais ocorreu em ordem crescente sendo braquetes Gemini, Clarity convencional, Transcend e Inspire. Pôde-se concluir que a angulação entre os braquetes aumenta consideravelmente o atrito. Além disso, em ambas as angulações, os braquetes autoligados demonstraram menor atrito em relação aos convencionais, sendo que o braquete Clarity autoligado promoveu menor atrito que o Damon estético, exceto no fio 0,021 x 0,025 .(AU)

COMPARAÇÃO DO ATRITO IN VITRO EM BRAQUETES ESTÉTICOS CONVENCIONAIS E AUTOLIGADOS

O objetivo do presente estudo consistiu em comparar in vitro o atrito produzido por braquetes estéticos, convencionais e autoligados quando inseridos fios retangulares de aço inoxidável de diferentes dimensões, nas angulações de zero e três graus entre os braquetes. Foram utilizados 120 braquetes de 6 marcas comerciais (Gemini, Clarity convencional, Transcend, Inspire, Clarity autoligado, Damon autoligado), sendo 20 braquetes de cada marca comercial. Para os ensaios laboratoriais, foram colados dois pares de braquetes de cada marca comercial em uma placa metálica, com uma angulação de zero e três graus entre os braquetes. Foram empregados os fios retangulares de aço inoxidável 0,017 x 0,025 , 0,019 x 0,025 e 0,021 x0,025 em uma máquina de ensaios universal Instron . Para a comparação entre os braquetes nos diferentes fios e angulações, foi utilizada a análise de variância e o teste de Tukey (p<0,05). Os resultados demonstraram que na angulação de zero grau, os braquetes autoligados apresentaram menor atrito em relação aos convencionais em todos os fios avaliados, sendo que, o braquete Clarity autoligado apresentou menor atrito estatisticamente significante que o Damon, exceto no fio 0,021 x 0,025 , em que ambos os braquetes autoligados apresentaram atrito estatisticamente semelhante. O braquete Inspire demonstrou o maior atrito em relação aos demais braquetes nos fios 0,019 x0,025 e 0,021 x0,025 . Na angulação de três graus, observou-se resultados semelhantes aos braquetes posicionados sem angulação comparando os braquetes autoligados em relação aos convencionais. Contudo, verificou-se que o atrito entre os braquetes convencionais ocorreu em ordem crescente sendo braquetes Gemini, Clarity convencional, Transcend e Inspire. Pôde-se concluir que a angulação entre os braquetes aumenta consideravelmente o atrito. Além disso, em ambas as angulações, os braquetes autoligados demonstraram menor atrito em relação aos convencionais, sendo que o braquete Clarity autoligado promoveu menor atrito que o Damon estético, exceto no fio 0,021 x 0,025 .(AU)

Broad spectrum chemokine antagonistic activity of a human poxvirus chemokine homolog

A secreted CC chemokine homolog, encoded by the MC148 gene of molluscum contagiosum virus, potently interfered with the chemotaxis of human monocytes, lymphocytes, and neutrophils in response to a large number of CC and CXC chemokines with diverse receptor specificities. Evidence that the viral protein binds to human chemokine receptors was obtained by competition binding and calcium mobilization experiments. The broad spectrum chemokine antagonistic activity of MC148 can explain the prolonged absence of an inflammatory response in skin tumors that harbor replicating molluscum contagiosum virus.

Transposable elements as sources of variation in animals and plants

A tremendous wealth of data is accumulating on the variety and distribution of transposable elements (TEs) in natural populations. There is little doubt that TEs provide new genetic variation on a scale, and with a degree of sophistication, previously unimagined. There are many examples of mutations and other types of genetic variation associated with the activity of mobile elements. Mutant phenotypes range from subtle changes in tissue specificity to dramatic alterations in the development and organization of tissues and organs. Such changes can occur because of insertions in coding regions, but the more sophisticated TE-mediated changes are more often the result of insertions into 5′ flanking regions and introns. Here, TE-induced variation is viewed from three evolutionary perspectives that are not mutually exclusive. First, variation resulting from the intrinsic parasitic nature of TE activity is examined. Second, we describe possible coadaptations between elements and their hosts that appear to have evolved because of selection to reduce the deleterious effects of new insertions on host fitness. Finally, some possible cases are explored in which the capacity of TEs to generate variation has been exploited by their hosts. The number of well documented cases in which element sequences appear to confer useful traits on the host, although small, is growing rapidly.

Commonplace book of John Bullard, 1775-1779

This bound volume contains excerpts copied by Jonathan Bullard from books he read as a student at Harvard in the mid 1770s. Excerpts include an unattributed poem titled "On Friendship," which appeared in the "poetical essays" section of Volume 36 of the London Magazine in 1767; Joseph Butler, The Analogy of Religion, 1736; The Quaker's Grace; a history of England; Newton's laws; Plutarch's Morals; Benjamin Franklin's writings on the Aurora Borealis. The volume also includes several extracts from articles about the death of John Paddock (Class of 1776), who drowned in the Charles in the summer of 1773, sheet music for two songs, "The Rapture," and "A Song" from Henry Harington's "Damon and Chlora," and a transcription of the satirical "Book of Harvard," written in response to the Butter Rebellion of 1766. Interleaved in the middle of the volume is a transcription from an ecclesiastical event moderated by Ebenezer Bridge in Medford, Mass. on November 20, 1779. The variety of texts suggests the commonplace book was not used solely for academic works.

(Table 2) Age determination of sediment cores from the Panama Basin

Application of the 230Th normalization method to estimate sediment burial fluxes in six cores from the eastern equatorial Pacific (EEP) reveals that bulk sediment and organic carbon fluxes display a coherent regional pattern during the Holocene that is consistent with modern oceanographic conditions, in contrast with estimates of bulk mass accumulation rates (MARs) derived from core chronologies. Two nearby sites (less than 10 km apart), which have different MARs, show nearly identical 230Th-normalized bulk fluxes. Focusing factors derived from the 230Th data at the foot of the Carnegie Ridge in the Panama Basin are >2 in the Holocene, implying that lateral sediment addition is significant in this part of the basin. New geochemical data and existing literature provide evidence for a hydrothermal source of sediment in the southern part of the Panama Basin and for downslope transport from the top of the Carnegie Ridge. The compilation of core records suggests that sediment focusing is spatially and temporally variable in the EEP. During oxygen isotope stage 2 (OIS 2, from 13-27 ka BP), focusing appears even higher compared to the Holocene at most sites, similar to earlier findings in the eastern and central equatorial Pacific. The magnitude of the glacial increase in focusing factors, however, is strongly dependent on the accuracy of age models. We offer two possible explanations for the increase in glacial focusing compared to the Holocene. The first one is that the apparent increase in lateral sediment redistribution is partly or even largely an artifact of insufficient age control in the EEP, while the second explanation, which assumes that the observed increase is real, involves enhanced deep sea tidal current flow during periods of low sea level stand.

Thallium concentrations and isotope composition of MORB glasses and altered oceani crust from DSDP/ODP Hole 504B and DSDP Hole 52-417D

Hydrothermal fluids expelled from the seafloor at high and low temperatures play pivotal roles in controlling seawater chemistry. However, the magnitude of the high temperature water flux of mid-ocean ridge axes remains widely disputed and the volume of low temperature vent fluids at ridge flanks is virtually unconstrained. Here, we determine both high and low temperature hydrothermal fluid fluxes using the chemical and isotopic mass balance of the element thallium (Tl) in the ocean crust. Thallium is a unique tracer of ocean floor hydrothermal exchange because of its contrasting behavior during seafloor alteration at low and high temperatures and the distinctive isotopic signatures of fresh and altered MORB and seawater. The calculated high temperature hydrothermal water flux is (0.17-2.93)*10**13 kg/yr with a best estimate of 0.72*10**13 kg/yr. This result suggests that only about 5 to 80% of the heat available at mid-ocean ridge axes from the crystallization and cooling of the freshly formed ocean crust, is released by high temperature black smoker fluids.The residual thermal energy ismost likely lost via conduction and/or through the circulation of intermediate temperature hydrothermal fluids that do not alter the chemical budgets of Tl in the ocean crust. The Tl-based calculations indicate that the low temperature hydrothermal water flux at ridge flanks is (0.2-5.4)*10**17 kg/yr. This implies that the fluids have an average temperature anomaly of only about 0.1 to 3.6 °C relative to ambient seawater. If these low temperatures are correct then both Sr and Mg are expected to be relatively unreactive in ridge-flank hydrothermal systems and this may explain why the extent of basalt alteration that is observed for altered ocean crust appears insufficient to balance the oceanic budgets of 87Sr/86Sr and Mg.

1987 University of Michigan Football Team

1991 University of Michigan Football Team

1992 University of Michigan Football Team

1993 University of Michigan Football Team