Arts - Buffalo State College
Arts - Buffalo State College
Arts - Buffalo State College
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104<br />
Physical Geography, Sciences, and Mathematics<br />
Studies of Growth and Optical Properties<br />
of LuFe2O4 Thin Films<br />
Aaron Sprow, Physics and Anthony Delmont, Physics<br />
Faculty Mentor: Professor Ram Rai, Physics<br />
Our research was primarily concerned with the preparation<br />
method and optical characterization of epitaxial lutetium iron oxide<br />
LuFe2O4 (LFO) thin films. Growth parameters considered included<br />
pellet composition, pellet size, evaporation method, substrate<br />
composition, and substrate temperature. Successful results were<br />
achieved using stoichiometric proportions of Fe2O3 and Lu2O3 that<br />
were ground and pressed into approximately 3 gram per pellet,<br />
followed by sintering at 1100 0C. The LFO thin film deposition<br />
process started with heating the target pellet by an electron beam<br />
for roughly an hour, and then slowly evaporating LFO onto (001)<br />
LNO, (111) YSZ, (001) sapphire, and (001) quartz substrates at 750<br />
0C, to a thickness of about 300 nm. We measured transmittance<br />
and absorbance on the annealed LFO thin films as a function of<br />
wavelength, varying from ultra-violet to near infrared wavelengths<br />
(200 – 3000 nm). The optical data demonstrate that LFO is an<br />
insulator having a well-defined energy gap and several electronic<br />
excitations associated with charge transfer transitions. Estimating<br />
from the absorption spectra, the energy band gap was found to be<br />
about 2.20 eV at 300K.<br />
Presentation Type and Session: Poster VI<br />
Studies of the Gap Junction Protein<br />
Connexin31<br />
Orlando McEwan, BIO 498: Biology Honors<br />
Faculty Mentor: Professor Martha Skerrett, Biology<br />
Gap junction channels allow direct communication between<br />
adjacent cells. Gap junction channels of chordates are composed<br />
of connexins, with six connexins required to create a half-channel,<br />
also known as a connexon or hemichannel in each adjacent cell.<br />
An intercellular gap junction channel is created when a connexon<br />
from one cell docks with a connexon from an adjacent cell. In<br />
humans, twenty connexins are expressed in specific but overlapping<br />
patterns to create gap junctions with a diverse set of properties.<br />
Connexin31 (Cx31) is expressed in the auditory system and skin<br />
of humans where it is expected to interact heterotypically and<br />
heteromerically with several other connexins. Mutations in Cx31<br />
are associated with multiple human diseases including deafness<br />
and erythrokeratodermia variabilis (EKV). The mutation Cx31L34P<br />
causes EKV and this study was designed to further assess the<br />
characteristics of this mutation at a molecular level. The amino<br />
acid leucine at position 34, was modified to tryptophan (Cx31<br />
L34W) using site-directed mutagenesis. Other studies suggest that<br />
the amino acid at position 34 interacts closely with another protein<br />
domain and we aimed to confirm this for Cx31 by substituting<br />
tryptophan for the native leucine at position 34.<br />
Presentation Type and Session: Poster VI<br />
Surface Water Quality and Risk Analysis In<br />
a Peri-Urban Area, Thailand<br />
Jameieka Price, Masters Multidisciplinary Studies<br />
Faculty Mentor: Professor Kim Irvine, Geography and Planning<br />
The Rangsit Canal, Pathum Thani, Thailand, receives runoff and<br />
contaminant inputs from urban and agricultural activities. Water<br />
quality in a section of the canal was examined by comparing sample<br />
results with Thailand’s water quality standards, the approximate<br />
delta method to characterize system metabolism, and a microbial<br />
risk analysis to assess potential for waterborne infections. Dissolved<br />
oxygen and BOD levels did not meet Thailand’s Class 3 standards.<br />
Continuous, automated monitoring of dissolved oxygen revealed a<br />
pronounced diel trend driven by photosynthesis during the day and<br />
respiration at night. Compared to many water bodies, however, the<br />
primary production of the canal was low and can be classified as<br />
heterotrophic. Based on a microbial risk assesment and considering<br />
infection risk standards, E.coli levels measured in the local sewer<br />
system (10^6 CFU/100 mL) and canal (10^4 CFU/100 mL)<br />
produced unacceptably high risk for activities that included<br />
swimming, vegetable farming, fishing, and sewer pump station<br />
operations. E.coli in piped water to an informal community on the<br />
canal was 0 CFU/100 mL in half the samples. The highest E.coli level<br />
(800 CFU /100mL) associated with the piped water source was found<br />
in a tradiontal (uncoverd) water storage jar, which emphasizes the<br />
importance of appropriate water storage.<br />
Presentation Type and Session: Oral – Science, Mathematics<br />
and Technology<br />
Textural and Structural Connections<br />
Along the Metamorphic Field Gradient In<br />
Philadelphia, PA<br />
Jennifer Wehrfritz, Earth Sciences and Geology and Albert<br />
Tahan, Geology<br />
Faculty Mentor: Professor Gary Solar, Earth Sciences and Science<br />
Education<br />
The Wissahickon schist type locality along Wissahickon Creek<br />
in SE Pennsylvania (Philadelphia), is composed of pelitic schist<br />
(metamorphosed shale) interlayered with psammitic gneiss and<br />
quartzite (metamorphosed sandstone). The type locality is known<br />
for its complete record of [Barrovian] metamorphic zones. The<br />
metamorphic field gradient increases SSE in the creek valley<br />
for 5km from chlorite to second sillimanite zone, and at a high<br />
angle to the trend of the mineral-defined structures (fabrics). The<br />
chlorite zone in the N is within and adjacent to the ENE-striking,<br />
dextral-transcurrent Huntingdon Valley shear zone system (active<br />
at 300 million years ago). A transect along the creek is across<br />
both the metamorphic zones and the structural grain, permitting<br />
documentation of the relations between the metamorphic and<br />
deformation fabrics. We mapped along the east valley slope starting<br />
in the chlorite zone to the SSE for 2.8km, into the kyanite zone.