22 research outputs found
Contamination
Micro-organisms can be transported through the environment in a number of ways; they can be conveyed in liquids or in aerosols, on particles of solids, or either inside objects or on their surfaces. An object or environment can become contaminated either by direct contact with a carrier of contamination or by contact with some intermediary that has itself has come into direct contact with a source of micro-organisms (Figure 1). Almost anything can qualify as an intermediary according to the definition given above. For example, as Figure 2 shows a person may sneeze into her hand and then transfer viral particles from her hand to a door handle which, as a result, becomes a source of infection. To give another example, a healthcare worker treating a patient infected with antibiotic resistant bacteria may transmit the infection to another patient simply by hand contact. As used here, the term contamination will be taken as referring to the unwanted transfer of infectious biological agents from one location to another. Moreover, the term ‘infectious biological agent’ is meant to include both prokaryotic and eukaryotic micro-organisms, viruses and prions. [continues...
Seismic analyses of Wappapello Dam
Wappapello Dam is a rolled-fill, earth dam located on the St. Francis River, approximately 15
miles north of Poplar Bluff, in Missouri, USA. The dam is currently owned and operated by the
US Army Corps of Engineers, St. Louis District (USACE-CELMS). The dam was constructed
between 1938 to 1941 for flood control purposes. The dam is approximately 73 ft high and the
crest is 30 ft wide at El. 419.74 ft (NGVD). The dam is approximately 2,700 ft long.
The dam is founded on approximately 120 ft of alluvium underlain by bedrock material identified
as dolomite. The upper 40 ft of the alluvial deposits consist of loose, fine sands and silts, less
than 500 years old, identified as the Young Point Bar Deposits. This deposit has been identified
as potentially liquefiable, and the USACE have initiated a number of studies over the years to
determine the dynamic behaviour of Wappapello Dam.
The first phase of the seismic study was carried out in 1982 by the USACE-Memphis District and
consisted of a one-dimensional liquefaction assessment of Wappapello Dam and the underlying
foundation soils. The main conclusions resulting from this work indicated that the Young Point
Bar Deposits were indeed susceptible to liquefaction under the design earthquake loads.
The second phase of the seismic study was carried out in 1988 b> the USACE-St. Louis District
and consisted of limit equilibrium stability analyses, assigning post-liquefaction residual strength
values to the liquefied deposits. The residual strength values were determined using an
empirically-based correlation relationship with field measured penetration values. The postearthquake
limit equilibrium factor of safety was about 1.0 for the estimated residual strength, and therefore, the main conclusion from the phase 2 studies was that the likelihood of an earthquakeinduced
embankment slide causing a reservoir release was low.
Since 1988, further advances have been made in the liquefaction assessment procedures, the
assessment of residual strength and the evaluation of post-liquefaction deformation analyses.
Therefore, the USACE initiated the third phase of the seismic study of Wappapello Dam. This
phase included a critical review of the phases 1 and 2 work, to ensure that advances made in the
liquefaction assessment techniques and the residual strength evaluations since 1988 have not
changed the previous conclusions, and a more rigorous evaluation of the post-earthquake
deformation analyses, to ensure that the magnitude of the movements are within acceptable limits.
The post-earthquake deformation analyses was carried out using the finite element computer
programs, TARA-3 and TARA-3FL, developed by Dr. W.D.L. Finn of the University of British
Columbia, Canada.
The phase 3 work deformation analyses indicated that the magnitude of the post-earthquake
movements were in the order of 25 ft vertically and greater than 200 ft horizontally, if the same
design parameters as used in the phase 2 work were assumed. The discrepancy between the
results of the finite element analyses and the limit equilibrium slope stability analyses was
attributed to the different failure mechanisms assumed in each analysis. In the finite element
analysis, failure was a result of the squeezing out of the liquefied foundation deposits due to the
high gravity loads of the dam and the sliding on the softened material as a result of reservoir
loading. In the limit equilibrium slope stability model, the failure is modelled by a circular slip
surface cutting through both the embankment having a high strength of 3,000 psf and the Young Point Bar Deposit with a low, post-liquefied strength of 115 psf. The seismic stability of
structures with extensive zones of liquefiable materials in the foundation should not be assessed
using limited equilibrium slope stability analyses as the conclusions resulting from this type of
analysis may be misleading.
Additional deformation analyses were carried out in the phase 3 work using more realistic fieldmeasured
penetration test values for the Young Point Bar Deposit. Parametric analyses were
carried out by assuming different residual strength correlation relationships and varying ( N^
values for the Young Point Bar Deposits located downstream of the dam toe (which was unknown
during the phase 3 work). The deformation values ranged from less than about 3 ft of vertical
and horizontal deformations to greater than 20 ft vertically and 250 ft horizontally for the varying
strength assumptions. Therefore, the seismic stability of Wappapello Dam depends on two critical
input parameters:
the penetration test values of the Young Point Bar Deposits located downstream of the
dam toe; and
the evaluation of residual strength.
The following recommendations are made following the phase 3 studies:
further field investigations should be carried out to determine the (Nj)^ values of the
Young Point Bar Deposits located downstream of the dam toe;
further studies should be carried out to determine the residual strength of the Young Point
Bar Deposits. Additional laboratory testing and review of the empirically-derived residual
strength vs (N,)^ database should be carried out to establish appropriate Sur values for this
site;
after the ( N ^ values of the Young Point Bar Deposit have been established and the
appropriate design Sur values have been assigned, further deformation analyses should be
carried out to determine the post-earthquake deformations of Wappapello Dam. The
maximum acceptable post-earthquake deformation limits to ensure seismic stability of Wappapello Dam should be established by the USACE. If the estimated deformations are
not acceptable, potential remedial measures should be assessed and implemented.Applied Science, Faculty ofCivil Engineering, Department ofGraduat
Recommended from our members
Fraternalism gone awry : the Ku Klux Klan in Houston, 1920-1925
Houston was an exciting city during the 1920s. The oil boom was in full swing, and as a result, Houston was transformed. An influx of people put pressures on city resources as well as on community interaction. These changes occurred within the context of one of the greatest periods of social turmoil in the history of the United States. Postwar America was evolving so rapidly that society was undergoing severe stresses. Disillusionment with the war, Prohibition, and technological change all played significant roles in this tumult. One would expect to see a backlash to this change; a backlash did indeed occur. The Red Scare was one manifestation of this reaction. Another was a general popular outcry against change. Seizing upon this popular outcry, William Joseph Simmons recreated the Ku Klux Klan; an organization originally designed to maintain white supremacy in the Reconstruction South. Reorganized in 1915, the Klan grew at a significant rate after World War I ended. By 1920, with the help of professional organizers and promoters, the Klan had expanded into Texas. The first Klan chapter organized in Texas was Sam Houston Klan No. 1, located in Houston. The Houston chapter grew quickly in both membership and power. In Houston the Klan assumed many roles. It sought to be a social regulator, attempting to enforce its own particular brand of social mores. It also sought to be a social benefactor, donating great amounts of money to worthy charities. As Klan power and confidence grew, it sought to become a social legislator by becoming involved in politics. The order undertook all of these roles under the guise of fraternalism. These roles, as well as the fraternal aspects of the organization, eventually gave way as the public became increasingly aware of the activities of the Klan and disapproval of the Klan mounted. Society's evolving attitude was linked directly to a gradual acceptance of the changes that were taking place within American society. Moreover, the Klan simply overstepped the bounds of societal acceptance. In attempting to explain how the Klan gained influence in Houston, this study relies on the convincing work of Kenneth Jackson. Jackson essentially concluded that there was "... a statistically significant correlation between Klan success and population growth." This can be demonstrated in Houston. This correlation between population growth and Klan success does not, however, explain what factors were behind the Klan's acceptance in Houston. Part of the goal of this study is to illuminate some of the reasons why the organization could take roots in HoustonHistor
General Studies Track Reviewed and Reported from East Richland High School, Olney, Illinois
What To Do If You Didn't Score the Internship
You touched up your resume, donned your business casual best,and knocked their socks off in the interview, but you didn’t get the internship. Now what? Here are ten things to do to keep your summer from being a total bust.</p
Are the social relationships of young insulin-dependent diabetic patients affected by illness?
In order to compare the social relationships of young adults with Type 1 diabetes with those of healthy controls, 80 young people aged 16–25 years were interviewed in-depth with a semi-structured questionnaire. Results demonstrated that subjects with diabetes had an equally high commitment to social arenas, but were significantly more likely to be socially isolated and were less likely to have very close relationships. Subjects had more attitudinal constraints with regard to having close relationships, and were more likely to report a fear of intimacy. They were less likely to have children, and many voiced their concerns regarding the impact their diabetes might have on both marriage and future parenthood. This study suggests that young adults with diabetes have more negative social experiences which may affect their feelings with regard to having close relationships. The absence of supportive relationships may impact on diabetes management; however this has yet to be fully ascertained in a young adult population