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Determination of marine migratory behavior and its relationship to selected physical traits for least cisco (Coregonus sardinella) of the western Arctic coastal plain, AlaskaSeigle, John C. 19 December 2003 (has links)
With increased resource development on the western Arctic coastal plain of Alaska
(especially within the oil extraction industry) it is important to understand the basic
life history attributes of whitefish stocks in the region in order to ensure appropriate
management. These fish are a crucial part of subsistence harvests for native Alaskans.
Multiple forms of the whitefish least cisco (Coregonus sardinella) have been
described based on both appearance and life history traits. Two major forms of least
cisco have been mentioned in the literature: a larger normal amphidromous form with
fork lengths of approximately 420 mm and a dwarf lake resident form with lengths up
to 230 mm. However, there is considerable evidence for additional forms and life
history strategies of least cisco. I investigated the relationship between migratory
behavior and selected physical traits of least cisco in six lakes and one brackish lagoon
in the western Arctic coastal plain of Alaska. I used electron microprobe technology to
determine the levels of Sr and Ca in the otoliths of 258 least cisco in order to resolve
their marine migratory life history. I also investigated the relationship between
migratory behavior and the numbers of gill rakers, lateral line scales, anal rays and
dorsal rays as well as condition factor. The vast majority of least cisco captured in
these sites were normal in form, yet only ~12% of all samples yielded any sign of sea-run
behavior. Evidence for migratory behavior was low even for sites within close
proximity to brackish waters. Fish exhibiting marine migratory behavior tended to
make their first migrations to sea before age three (mean=2.6 years), although fish in
one coastal site (Joeb's) averaged over 5 years of age at first marine visit. There was
some evidence of higher condition factors for fish with sea-run migratory experience.
There were significant differences in lateral line and dorsal ray numbers among sites
but none for anal rays or gill rakers. Variability in all of these characters was high, and
fish from coastal sites tended to have greater variability than those from inland sites.
Only dorsal rays showed significant differences in meristic traits between sea-run and
resident least cisco. These results suggest that least cisco exhibit high variability in
physical traits. Also, least cisco appear to be flexible in their use of the marine
environment, even within similar forms in the same lake. Some of the most basic life
history characteristics of least cisco remain uncertain. With increased resource
extraction occurring on the western Arctic coastal plain of Alaska, it is important to
continue to investigate these and other life history strategies so as to ensure a
sustainable fishery for native inhabitants of the region. / Graduation date: 2004
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A proposed inventory method for analyzing the visual resources of Alaska's north slopeLaurizio, Daniel Gerard January 2011 (has links)
Typescript (photocopy). / Digitized by Kansas State University Libraries
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Topics in applied microeconomics : time allocation and natural resource use on Alaska's North Slope and market power in the U.S. motor carrier industryNebesky, William E. 04 February 1994 (has links)
This paper presents two applications of empirical microeconomics
based on choice theoretic optimization principles. The first topic
explores the determinants of subsistence time allocation in a utility
theoretic model of household production. The second topic examines firm
pricing behavior in a deregulated, but concentrated industry setting.
The first part of this applied microeconomic analysis estimates
the subsistence time versus wage labor time allocations of Alaska's
North Slope inhabitants using ordered probit based on a household
production model. The explanatory variables measure labor supply,
demographic, and cultural influences.
The major findings are as follows. First parameter estimates
differ statistically and substantially between Inupiat versus non-Inupiat residents, implying that optimal natural resource management
decisions may vary with the ethnicity of the resource owners. Second,
marital status, age, gender, and participation in generalized gift
giving and receiving are important determinants of subsistence time
allocations. Third, time spent in wage labor appears to be exogenous to
the subsistence time allocation decision, indicating that the time
allocation process is recursive. Fourth, we find an inverse
relationship between wage labor time and subsistence participation.
This means that reductions in wage employment opportunities lead to
increased subsistence activity. For the North Slope, this implies that
Prudhoe oil depletion will result in an increase in the use of
subsistence natural resources.
The second part of this study turns from the individual behavior
to firm behavior. During the 1980's, researchers have noted a trend
towards increased concentration in the general freight, less-than-truckload
(LTL) portion of the U.S. motor carrier industry. The purpose
of this study is to employ new empirical industrial organization (NEIO)
techniques to determine whether the more concentrated post-1980, LTL
motor carrier industry is exerting anti-competitive monopoly pricing
behavior.
The NEIO approach is used to formulate the relationship between
market price and marginal cost in what is referred to as the
representative firm's 'supply relation.' The firm's supply relation is
estimated jointly with the cost function and the factor share equations
under the assumption that cross equation disturbance terms are
correlated (SUR). An instrumental variables procedure is used to test
and control for correlation between output (on the right hand side) and
the disturbance terms in the cost and supply equations.
The results indicate that the trend toward increased industry
concentration does not imply anti-competitive performance in the sense
of rising price-cost margins. / Graduation date: 1994
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INVESTIGATION OF GAS HYDRATE-BEARING SANDSTONE RESERVOIRS AT THE "MOUNT ELBERT" STRATIGRAPHIC TEST WELL, MILNE POINT, ALASKABoswell, Ray, Hunter, Robert, Collett, Timothy S., Digert, Scott, Hancock, Steve H., Weeks, Micaela, Mount Ebert Science Team 07 1900 (has links)
In February 2007, the U.S. Department of Energy, BP Exploration (Alaska), Inc., and the U.S.
Geological Survey conducted an extensive data collection effort at the "Mount Elbert #1" gas
hydrates stratigraphic test well on the Alaska North Slope (ANS). The 22-day field program
acquired significant gas hydrate-bearing reservoir data, including a full suite of open-hole well
logs, over 500 feet of continuous core, and open-hole formation pressure response tests. Hole
conditions, and therefore log data quality, were excellent due largely to the use of chilled oilbased
drilling fluids. The logging program confirmed the existence of approximately 30 m of gashydrate
saturated, fine-grained sand reservoir. Gas hydrate saturations were observed to range
from 60% to 75% largely as a function of reservoir quality. Continuous wire-line coring operations (the first conducted on the ANS) achieved 85% recovery through 153 meters of
section, providing more than 250 subsamples for analysis. The "Mount Elbert" data collection
program culminated with open-hole tests of reservoir flow and pressure responses, as well as gas
and water sample collection, using Schlumberger's Modular Formation Dynamics Tester (MDT)
wireline tool. Four such tests, ranging from six to twelve hours duration, were conducted. This
field program demonstrated the ability to safely and efficiently conduct a research-level openhole
data acquisition program in shallow, sub-permafrost sediments. The program also
demonstrated the soundness of the program's pre-drill gas hydrate characterization methods and
increased confidence in gas hydrate resource assessment methodologies for the ANS.
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Physical controls on hydrate saturation distribution in the subsurfaceBehseresht, Javad 22 February 2013 (has links)
Many Arctic gas hydrate reservoirs such as those of the Prudhoe Bay and Kuparuk River area on the Alaska North Slope (ANS) are believed originally to be natural gas accumulations converted to hydrate after being placed in the gas hydrate stability zone (GHSZ) in response to ancient climate cooling. A mechanistic model is proposed to predict/explain hydrate saturation distribution in “converted free gas” hydrate reservoirs in sub-permafrost formations in the Arctic. This 1-D model assumes that a gas column accumulates and subsequently is converted to hydrate. The processes considered are the volume change during hydrate formation and consequent fluid phase transport within the column, the descent of the base of gas hydrate stability zone through the column, and sedimentological variations with depth. Crucially, the latter enable disconnection of the gas column during hydrate formation, which leads to substantial variation in hydrate saturation distribution. One form of variation observed in Arctic hydrate reservoirs is that zones of very low hydrate saturations are interspersed abruptly between zones of large hydrate saturations. The model was applied on data from Mount Elbert well, a gas hydrate stratigraphic test well drilled in the Milne Point area of the ANS. The model is consistent with observations from the well log and interpretations of seismic anomalies in the area. The model also predicts that a considerable amount of fluid (of order one pore volume of gaseous and/or aqueous phases) must migrate within or into the gas column during hydrate formation. This work offers the first explanatory model of its kind that addresses "converted free gas reservoirs" from a new angle: the effect of volume change during hydrate formation combined with capillary entry pressure variation versus depth.
Mechanisms by which the fluid movement, associated with the hydrate formation, could have occurred are also analyzed. As the base of the GHSZ descends through the sediment, hydrate forms within the GHSZ. The net volume reduction associated with hydrate formation creates a “sink” which drives flow of gaseous and aqueous phases to the hydrate formation zone. Flow driven by saturation gradients plays a key role in creating reservoirs of large hydrate saturations, as observed in Mount Elbert. Viscous-dominated pressure-driven flow of gaseous and aqueous phases cannot explain large hydrate saturations originated from large-saturation gas accumulations. The mode of hydrate formation for a wide range of rate of hydrate formation, rate of descent of the BGHSZ and host sediments characteristics are analyzed and characterized based on dimensionless groups. The proposed transport model is also consistent with field data from hydrate-bearing sand units in Mount Elbert well. Results show that not only the petrophysical properties of the host sediment but also the rate of hydrate formation and the rate of temperature cooling at the surface contribute greatly to the final hydrate saturation profiles. / text
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