Relevant bibliographies by topics / Deer Creek

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Deer Creek'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Deer Creek"

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Jagoda, Kalinga, Bharat Maheshwari, and Gregory Gutowski. "Deer Creek Land Development (DCLD)." International Journal of Commerce and Management 22, no. 2 (June 22, 2012): 133–44. http://dx.doi.org/10.1108/10569211211239430.

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Yeager, Elizabeth A., and Sarah A. Stutzman. "Deer Creek Farms: Tradition into the Future." American Journal of Agricultural Economics 96, no. 2 (February 13, 2014): 598–605. http://dx.doi.org/10.1093/ajae/aat108.

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Spence, Brian C., and E. J. Dick. "Geographic variation in environmental factors regulating outmigration timing of coho salmon (Oncorhynchus kisutch) smolts." Canadian Journal of Fisheries and Aquatic Sciences 71, no. 1 (January 2014): 56–69. http://dx.doi.org/10.1139/cjfas-2012-0479.

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The environmental cues that regulate smoltification and trigger downstream movement by salmon should vary across space in response to differences in the predictability of favorable conditions for migration and ocean entry. To examine this, we modeled the short-term outmigration probability of four coho salmon (Oncorhynchus kisutch) populations in three distinct geographic regions in relation to photoperiod, temperature, streamflow, lunar phase, and interactions among these variables. For smolts in Deer and Flynn creeks, Oregon (1960–1972), migration probability was influenced by numerous factors, including photoperiod, temperature (absolute and change), flow (absolute and change), and lunar phase, with certain factors interacting. Smolts from Carnation Creek, British Columbia (1972–1986) responded to a similarly diverse suite of factors (excluding lunar phase), though in somewhat different ways. In contrast, migration timing of smolts in Sashin Creek, Alaska (1959–1969) was best explained by a model that included only photoperiod, temperature, and the interaction between these terms. These population differences suggest fundamental differences across regions in the selection processes operating in both marine and freshwater environments.
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Beschta, Robert L., and William J. Ripple. "INCREASED WILLOW HEIGHTS ALONG NORTHERN YELLOWSTONE's BLACKTAIL DEER CREEK FOLLOWING WOLF REINTRODUCTION." Western North American Naturalist 67, no. 4 (December 2007): 613–17. http://dx.doi.org/10.3398/1527-0904(2007)67[613:iwhany]2.0.co;2.

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Casbeer, Warren, Gustavious Williams, and M. Borup. "Phosphorus Distribution in Delta Sediments: A Unique Data Set from Deer Creek Reservoir." Hydrology 5, no. 4 (October 11, 2018): 58. http://dx.doi.org/10.3390/hydrology5040058.

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Recently, Deer Creek Reservoir (DCR) underwent a large drawdown to support dam reconstruction. This event exposed sediments inundated by the reservoir, since dam completion in the early 1940s. This event allowed us to take sediment data samples and evaluate them for phosphorous (P) content. It is difficult for normal reservoir sediment studies to have sediment samples at high spatial resolution because of access. During the drawdown, we collected 91 samples on a grid 100 m in one direction and 200 m in the other. This grid defined an area of approximately 750,000 m2 (185 acre). We took both surface samples, and at some sites, vertical samples. We determined water soluble P for all the samples, and P in four other reservoirs or fractions for 19 samples. Results showed water soluble P in the range of 2.28 × 10−3 to 9.81 × 10−3, KCl-P from 2.53 × 10−3 to 1.10 × 10−2, NaOH-P from 5.30 × 10−2 to 4.60 × 10−1, HCl-P from 1.28 × 10−1 to 1.34, and residual (mostly organic) P from 8.23 × 10−1 to 3.23 mg/g. We provide this data set to the community to support and encourage research in this area. We hope this data set will be used and analyzed to support other research efforts.
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Kelly, A. J., E. Karl Sauer, S. L. Barbour, E. A. Christiansen, and R. A. Widger. "Deformation of the Deer Creek bridge by an active landslide in clay shale." Canadian Geotechnical Journal 32, no. 4 (August 1, 1995): 701–24. http://dx.doi.org/10.1139/t95-069.

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Two parallel, concurrently active slip surfaces of a landslide in clay shale of the Cretaceous Lea Park Formation are causing deformation of a bridge structure across the North Saskatchewan River near Deer Creek, Saskatchewan. The upper slip occurs at the contact between the shale and glacial deposits, which is common in this region. However, the second slip occurs deep in the shale, 24 m below the upper slip zone. This multilevel landslide mechanism, not reported previously in this region, is resulting in a complex deformation pattern where components of the structure are moving at different rates. The multilevel slip mechanism is related to a unique combination of the hydrogeology and geologic structure at this site. Under an upward groundwater gradient, slip surfaces occur at discontinuities in available shearing resistance at different elevations in the shale. The discontinuities are gouge zones in the clay shale, which are the result of a combination of glacial shear and regional tectonism where parameters have been reduced to a residual state ([Formula: see text] and c′ = 0). The pore-water pressures for the slope stability analysis were generated from a site specific finite element seepage model using boundary conditions determined from a regional finite element seepage model. The groundwater models were calibrated from piezometer data and from hydrochemistry of water from farm wells, piezpmeters, and natural surface ponds. The hydrochemistry was used to delineate groundwater, discharge areas from recharge areas. The validity of the landslide mechanism is supported by a stability analysis integrated with the finite element seepage analysis, which demonstrates that two separate parallel slip surfaces at different depths can be at a state of limiting equilibrium concurrently. Key words : bridge deformation, Cretaceous shale, integrated models, residual strength, multilevel slips.
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Goodrich, R. R., J. F. T. Agapito, C. Pollastro, and L. J. Lafrentz. "Longwall mining through a graben with anomalous stresses at the deer creek mine." International Journal of Rock Mechanics and Mining Sciences 35, no. 4-5 (June 1998): 401–2. http://dx.doi.org/10.1016/s0148-9062(98)00038-2.

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Rains, R. Bruce, James A. Burns, and Robert R. Young. "Postglacial alluvial terraces and an incorporated bison skeleton, Ghostpine Creek, southern Alberta." Canadian Journal of Earth Sciences 31, no. 10 (October 1, 1994): 1501–9. http://dx.doi.org/10.1139/e94-133.

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Ghostpine Creek near Three Hills, southern Alberta, is a tributary of the Red Deer River. It has three sets of paired alluvial terraces (T-1 to T-3) in a downstream part of the valley. The rare discovery of a largely intact skeleton of plains bison (Bison bison bison) in a T-2 point bar prompted terrace mapping, 14C dating, and interpretation of the postglacial evolution of the valley. Downvalley portions of the creek began incision into the newly drained bed of glacial Lake Drumheller probably about 13 000 BP. Localized valley deepening up to 20 m, the production of erosional benches and residual spurs, and the development of partly convex-up creek paleothalwegs occurred between about 13 000 and 7600 BP, by which time basal T-1 alluvium was beginning to accumulate. Subsequent aggradation of T-1 sediment and then degradation of about 3–4 m were followed by aggradation of T-2 alluvium. These trends had taken place by 2600 BP, when the bison died and its skeletal remains were buried in uppermost sediment of a T-2 point bar. Between 2600 BP and now, the creek incised about 5 m below the former T-2 channel position and aggraded, partly synchronously, up to 3 m of T-3–floodplain alluvium. Radiocarbon-dated alluvial terrace sequences in Alberta show generally comparable trends of rapid early creek incision followed by partially overlapping episodes of net aggradation and degradation from basin to basin. However, such episodes were not closely synchronized between basins.
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Natkaniec-Nowak, Lucyna, Magdalena Dumańska-Słowik, Adam Gaweł, Anna Łatkiewicz, Joanna Kowalczyk-Szpyt, Anna Wolska, Stanislava Milovská, Jarmila Luptáková, and Karolina Ładoń. "Fire agate from the Deer Creek deposit (Arizona, USA) – new insights into structure and mineralogy." Mineralogical Magazine 84, no. 2 (February 5, 2020): 343–54. http://dx.doi.org/10.1180/mgm.2020.8.

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AbstractFire agates from Deer Creek are highly appreciated gemstones due to the presence of optical phenomena and rainbow colours that cause fiery effects to be observed on their characteristic brown base. The specific morphology of poorly ordered chalcedony (crystallinity index = 0.1–1.5) with an admixture of mogánite (av. 6.6%), micro-quartz and opal-C forming a colloform texture seems to be responsible for the presence of fire effect in these agates. The multi-layered silica spheroidal forms (‘bubble’-like structure), already noted in hand specimens, could be the centres of reflection and interference of white light. Numerous, microscopic inclusions of Fe and Ti compounds randomly scattered within some silica zones, together with microstructural features of agate, could determine the colour and size of the domains with the optical effect. Deer Creek fire agates form veins within their host volcanic rocks. The silica mineralisation filling the network of fissures in the host rocks was supplied cyclically with aqueous fluids of varying composition, enriched periodically in CO2, Fe, Ti, Mn, Zn and Ca. As a result, the red-brown colour of fire agates was created by scattered pigments of tiny iron oxides (magnetite, maghemite) and titanium oxides (rutile, anatase) within the silica matrix. The precipitation of strongly disordered silica with a characteristic colloform texture is diagnostic for boiling processes in this area.
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Trabert, Sarah. "Partners and Power: Understanding Ancestral Wichita and French Trade at the Deer Creek Site." International Journal of Historical Archaeology 23, no. 2 (August 27, 2018): 444–61. http://dx.doi.org/10.1007/s10761-018-0473-2.

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Dissertations / Theses on the topic "Deer Creek"

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Morse, Keir A. "Vascular plant inventory of Deer Creek Center property in Selma, Oregon /." View full-text version online through Southern Oregon Digital Archives, 2008. http://soda.sou.edu/awdata/080321z1.pdf.

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Thesis (M.S.)--Southern Oregon University, 2008.
Includes bibliographical references (leaves 36-38). Also available via Internet as PDF file through Southern Oregon Digital Archives: http://soda.sou.edu. Search Bioregion Collection.
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Stephens, Ryan A. "Field Algae Measurements Using Empirical Correlations at Deer Creek Reservoir." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2722.

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Deer Creek Reservoir in Utah has a history of high algae concentrations. Despite recent nutrient reduction efforts, seasonal algae continue to present problems. Cost effective, accurate, and comprehensive monitoring is important to understand the reservoir processes driving this problem and characterizing the algae spatial and temporal distributions are an important part of this effort. Current laboratory methods for accurately measuring algae are expensive and time consuming and are based on water samples taken in the field and transported to the laboratory. This approach only provides data for relatively few point samples because of the time and expense of sample collection and analysis. These relatively few samples do not describe the complex spatial and temporal trends in the algal data. Algae exhibit non-uniform distributions, especially in the vertical direction. In situ probes are able to measure chlorophyll-a and provide a less expensive measuring alternative than laboratory methods. These probes provide relatively quick, high resolution vertical profile measurements, which allows for more comprehensive horizontal and temporal sampling. To have confidence in the probe data, good correlations between in situ chlorophyll-a measurements and laboratory algae or chlorophyll measurements are important, but these correlations can be reservoir and time dependant as reservoir conditions change. Therefore, they must be developed for each study site. This study reports on efforts at Deer Creek Reservoir to develop these correlations and provide a general description of the dynamic reservoir algal processes. I found that chlorophyll-a is weakly correlated to most algae species in the reservoir. However, it correlated well with total phytoplankton biovolume and the dominant algal species, which for this study was the diatom. Variations in correlation strength among the several algae species was assumed to most likely be affected by environmental factors, sample methods, algae species diversity, and the accuracy of the optical chlorophyll-a sensor. The data analysis indicate that the field methods used to obtain laboratory samples may have been a significant source of error because of the difficulty of matching the location of a probe measurement to the location of a sample. Field samples were not taken at the same depths as probe measurements and field samples from two locations were either mixed before laboratory analysis or the sample was a composite over a 2-meter range. Based on my observations, I have made several recommendations to improve the accuracy of the correlation between algae and chlorophyll-a.
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Casbeer, Warren C. "Phosphorus Fractionation and Distribution across Delta of Deer Creek Reservoir." BYU ScholarsArchive, 2009. https://scholarsarchive.byu.edu/etd/2004.

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Eutrophication of reservoir systems, which causes deterioration of water quality through increased algal growth, is detrimental to our sustainable water supply and additionally impairs other beneficial reservoir uses. Limiting the amount of phosphorus (P) entering the system has been the key management tool for this problem, as P is the main limiting nutrient for plant and algal growth. These efforts have focused on controlling input of P from point sources, such as effluents from wastewater treatment plants, dairies, and industrial factories. Even in systems (such as reservoirs) with significantly reduced external P loading, however, there has been continued eutrophication and slower than expected recovery of reservoirs in water quality restoration projects. Other nutrient sources have been studied to explain this phenomenon. The continual eutrophication has been potentially attributed to availability of nutrients from deposited sediments. This is referred to as nutrient recycling, as nutrients previously trapped within sediments may become available within the water column. Deer Creek Reservoir (DCR), a significant water supply in Utah, has had greatly improved water quality after reduction of external P loading. However, there are still large algal blooms at times as well as other water quality issues without clearly attributable causes. Part of the explanation might lie within the deposited sediments, which are present both on the sediment delta and within the reservoir. This thesis provides data that can help researchers understand what role sediment has in the continuation of water quality problems at DCR. Sediment samples were taken across the delta to define both the spatial extent and distribution of P and chemical form, or ‘pool’, of the P. The pools can be used to estimate the ability of the sediment-bound P to move into the water column under various conditions. Results reported here indicate that significant amounts of P are found within these sediments, though not all of it can easily become available for algal growth. We characterized P distribution by taking 91 samples on 6 transects across the exposed delta. Transects were separated by 200 m and samples were taken eery 100 m along the transects. The samples were all analyzed for water soluble P content, and 19 samples were additionally characterized for KCl-, NaOH-, HCl-, and organic (by digestion) P fractions. Total P was determined for these as well by summation. The data showed that water soluble P ranged from 2.28E-03 and 9.81E-03 mg P g−1 dry sediment and showed a decreasing trend along the reservoir. KCl-P ranged from 2.53E-03 and 1.10E-02, NaOH-P from 5.30E-02 to 4.60E-01, HCl-P from 1.28E-01 and 1.34E+00, and organic (residual) P from 8.23E-01 to 3.23E+00 mg·g−1.
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Dameron-Hager, Irene Frances. "The contribution of environmental history to the development of a model to aid watershed management: a comparative study of the Big Darby Creek and Deer Creek Watersheds in Ohio." The Ohio State University, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=osu1078778562.

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Dameron-Hager, Irene F. "The contribution of environmental history to the development of a model to aid watershed management a comparative study of the Big Darby Creek and Deer Creek Watersheds in Ohio /." Columbus, Ohio : Ohio State University, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1078778562.

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Thesis (Ph. D.)--Ohio State University, 2004.
Title from first page of PDF file. Document formatted into pages; contains xiii, 253 p.; also includes graphics (some col.). Includes abstract and vita. Advisor: Earl F. Epstein, Dept. of Natural Resources. Includes bibliographical references (p. 228-238).
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Ferguson, Earl W. "The multi-site church and disciplemaking." Chicago, Ill : McCormick Theological Seminary, 1997. http://www.tren.com.

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Ricks, Colin Rodger. "Quantifying Mass Sediment Movement in Deer Creek Reservoir During Spring Runoff and Potential Water Quality Impacts." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2880.

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The accurate prediction of water quality is essential for management of reservoirs used for drinking water supply. Since algae are a major source of taste and odor problems in drinking water, understanding and controlling algal growth and production is an important task. Deer Creek Reservoir supplies drinking water for over one million people in northern Utah and has been highly eutrophic in the past. Despite major reductions in external nutrient loading, including phosphorus, seasonal algal blooms in Deer Creek have not decreased to desired levels. Resuspension of sediment has been suggested as a potential source of internal nutrient loading for water bodies (including reservoirs in the Utah/Wyoming area) and may be responsible for delays in water quality improvement. I investigated sediment deposition and resuspension rates at the upper end of the reservoir and evaluated these sediments as a possible internal source of phosphorus. Sonar and GPS systems were used to make measurements of recently deposited sediment in the submerged Provo River delta of Deer Creek Reservoir during the period of May, June, July, and August 2011. ArcGIS 10 was used to interpolate survey points and calculate sediment volume changes, including areas of deposition and erosion. These data were used to develop approximate sedimentation rates for the soft sediment – which is most susceptible to resuspension during reservoir drawdown. I used previously measured field phosphorous concentrations in the sediment to estimate if these processes could affect reservoir phosphorous concentrations. The study used two survey areas, a small area near the Provo River inlet early in the year, and an extended larger area starting on June 23rd. I found that sediment volume in the smaller study area was increasing at a rate of 27-109 m3/day during the spring season. Data show that rates are slightly correlated with flow and reservoir elevation. Typically by August, Deer Creek reservoir would have been drawn down 2 to 4 m. However, due to a heavy snow pack in 2011, Deer Creek reservoir was not drawn down. When the reservoir is drawn down, the sediments in the upper region of the delta, where the survey was conducted, will be resuspended and deposited lower in the reservoir. These processes will likely result in releasing the phosphates currently bound to the sediment into the water column. Based on previous measurements of readily soluble phosphates bound to the sediment, this resuspension could release between 80 and 230 kg of phosphorus from the study area into the water column during critical times during the warm months–conditions well suited for algal growth. This amount of phosphorus, while an upper bound of what could be expected under actual field conditions, could raise phosphorus concentrations in the survey area by as much as 0.38 mg/L. The potential P (80-230 kg) release could account for 14%-42% of the TMDL. This is a potentially significant amount, especially if released during the critical late-summer period, and warrants more detailed study.
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Di, Vittorio Damien. "Spatial Translation and Scaling Up of LID Practices in Deer Creek Watershed in East Missouri." Thesis, Southern Illinois University at Edwardsville, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1566440.

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This study investigated two important aspects of hydrologic effects of low impact development (LID) practices at the watershed scale by (1) examining the potential benefits of scaling up of LID design, and (2) evaluating downstream effects of LID design and its spatial translation within a watershed. The Personal Computer Storm Water Management Model (PCSWMM) was used to model runoff reduction with the implementation of LID practices in Deer Creek watershed (DCW), Missouri. The model was calibrated from 2003 to 2007 (R2 = 0.58 and NSE = 0.57), and validated from 2008 to 2012 (R2 = 0.64 and NSE = 0.65) for daily direct runoff. Runoff simulated for the study period, 2003 to 2012 (NSE = 0.61; R2 = 0.63), was used as the baseline for comparison to LID scenarios. Using 1958 areal imagery to assign land cover, a predevelopment scenario was constructed and simulated to assess LID scenarios' ability to restore predevelopment hydrologic conditions. The baseline and all LID scenarios were simulated using 2006 National Land Cover Dataset.

The watershed was divided in 117 subcatchments, which were clustered in six groups of approximately equal areas and two scaling concepts consisting of incremental scaling and spatial scaling were modelled. Incremental scaling was investigated using three LID practices (rain barrel, porous pavement, and rain garden). Each LID practice was simulated at four implementation levels (25%, 50%, 75%, and 100%) in all subcatchments for the study period (2003 to 2012). Results showed an increased runoff reduction, ranging from 3% to 31%, with increased implementation level. Spatial scaling was investigated by increasing the spatial extent of LID practices using the subcatchment groups and all three LID practices (combined) implemented at 50% level. Results indicated that as the spatial extent of LID practices increased the runoff reduction at the outlet also increased, ranging from 3% to 19%. Spatial variability of LID implementation was examined by normalizing LID treated area to impervious area for each subcatchment group. The normalized LID implementation levels for each group revealed a reduction in runoff at the outlet of the watershed, ranging from 0.6% to 3.7%. This study showed that over a long-term period LID practices could restore pre-development hydrologic conditions. The optimal location for LID practice implementation within the study area was found to be near the outlet; however, these results cannot be generalized for all watersheds.

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Gonzalez, Nicolas Alejandro. "Principal Components Analysis, Factor Analysis and Trend Correlations of Twenty-Eight Years of Water Quality Data of Deer Creek Reservoir, Utah." BYU ScholarsArchive, 2012. https://scholarsarchive.byu.edu/etd/3309.

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I evaluated twenty-eight years (1980-2007) of spatial-temporal water quality data from Deer Creek Reservoir in Utah. The data came from three sampling points representing the lotic, transitional and lentic zones. The data included measurements of climatological, hydrological and water quality conditions at four depths; Surface, Above Thermocline, Below Thermocline and Bottom. The time frame spanned dates before and after the completion of the Jordanelle Reservoir (1987-1992), approximately fourteen miles upstream of Deer Creek. I compared temporal groupings and found that a traditional month distribution following standard seasons was not effective in characterizing the measured conditions; I developed a more representative seasonal grouping by performing a Tukey-Kramer multiple comparisons adjustment and a Bonferronian correction of the Student's t comparison. Based on these analyses, I determined the best groupings were Cold (December - April), Semi-Cold (May and November), Semi-Warm (June and October), Warm (July and September) and Transition (August). I performed principal component analysis (PCA) and factor analysis (FA) to determine principal parameters associated with the variability of the water quality of the reservoir. These parameters confirmed our seasonal groups showing the Cold, Transition and Warm seasons as distinct groups. The PCA and FA showed that the variables that drive most of the variability in the reservoir are specific conductivity and variables related with temperature. The PCA and FA showed that the reservoir is highly variable. The first 3 principal components and rotated factors explained a cumulative 59% and 47%, respectively of the variability in Deer Creek. Both parametric and nonparametric approaches provided similar correlations but the evaluations that included censored data (nutrients) were considerably different with the nonparametric approach being preferred.
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Chilton, Reed Earl. "Developing Methods to Assess the Potential Effects of Global Climate Change on Deer Creek Reservoir Using Water Quality Modeling." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2468.

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To evaluate the potential impacts of future climate change on a temperate reservoir, I used a calibrated water quality and hydrodynamic model validated using three years of data (2007-2009) from Deer Creek Reservoir (Utah). I evaluated the changes due to altered air temperatures, inflow rates, and nutrient loads that might occur under Global Climate Change (GCC). I developed methods to study GCC on reservoirs. I produced Average Water Temperature Plots, Stratification Plots, and Total Concentration Plots. Average Water Temperature Plots show the sensitivity of the water temperature to various parameters. Stratification Plots quantify stratification length and strength as well as ice-cover periods. Total Concentration Plots analyze the reservoir as a whole concerning water quality parameters. Increasing air temperature increased the water temperature, lengthened stratification time, increased stratification strength, decreased the ice-cover period, decreased the total algae concentration, decreased the flows, and caused peak nutrient concentrations to occur earlier. Decreasing flows caused increased water temperature, shorter stratification periods, weaker stratification, and increased nutrient concentrations. Increasing phosphate concentrations caused increases in total algae, dissolved oxygen, and phosphate concentrations. Variations in Nitrate-Nitrite concentrations did not influence the tested parameters. I found that the reservoir is only sensitive to these changes during the spring and summer. The tools which I developed were used to run the model scenarios, organize the data, and plot the results. They can be used on other reservoirs and for other water quality parameters.
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Books on the topic "Deer Creek"

1

Tales from Deer Creek. Kearney, NE: Morris Publishing, 2005.

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Showdown at Deer Creek. New York: Thomas Bouregy & Co., 2006.

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Whittaker, Richard B. The deer of Potato Creek. North Liberty, IN: Whitt's 3' Enterprises, 1986.

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Idema, Kelly. Owl Creek/Meeteetse mule deer habitat evaluation project. [Cheyenne, Wyo.]: Wyoming Game and Fish Dept., 2004.

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Pate, Larry. Garden Creek deer: Public involvement in conflict resolution. [Cheyenne, Wyo.]: Wyoming Game and Fish Dept., 1992.

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Yoder, Nyce Dorothy, ed. "Talks" that teach. Goshen, IN (1603 S. 15th St., Goshen, IN 46526-4558): D.Y. Nyce, 2012.

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Tourangeau, Phillip C. Arsenic concentrations in deer and elk tissue from Upper Prospect Creek, Montana. Missoula, Mont: [Gordon Environmental Laboratory, Univ. of Montana?], 1985.

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Smith, Barry S. Water resources of Wildcat Creek and Deer Creek basins, Howard and parts of adjacent counties, Indiana, 1979-82. Indianapolis, Ind: U.S. Dept. of the Interior, Geological Survey, 1985.

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Williams, Donald R. Nutrients and organic compounds in Deer Creek and South Branch Plum Creek in southwestern Pennsylvania, April 1996 through September 1998. New Cumberland, Pa: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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Williams, Donald R. Nutrients and organic compounds in Deer Creek and South Branch Plum Creek in southwestern Pennsylvania, April 1996 through September 1998. New Cumberland, Pa: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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Book chapters on the topic "Deer Creek"

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Welch, Bruce L. "Value of “Hobble Creek” Mountain Big Sagebrush as a Winter Forage for Mule Deer." In The Biology of Deer, 467. New York, NY: Springer New York, 1992. http://dx.doi.org/10.1007/978-1-4612-2782-3_115.

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Ostendorf, Berndt. "Samuel Huntington: From Creed to Culture." In Kultur. Theorien der Gegenwart, 92–105. Wiesbaden: VS Verlag für Sozialwissenschaften, 2011. http://dx.doi.org/10.1007/978-3-531-92056-6_8.

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Eisfeld, Rainer. "Vom Buschkrieg in Kansas zum „Massaker“ am Rock Creek (Nebraska)." In Die bewaffnete Gesellschaft der USA, 71–123. Wiesbaden: Springer Fachmedien Wiesbaden, 2021. http://dx.doi.org/10.1007/978-3-658-33530-4_3.

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Everitt, Benjamin L., and Andrew E. Godfrey. "The Deep Creek Mudflow of April 16, 1979, Uintah County, Utah, USA." In Environmental Geotechnics and Problematic Soils and Rocks, 349–55. London: CRC Press, 2021. http://dx.doi.org/10.1201/9781003211051-34.

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Aldaeef, Abdulghader A., and Mohammad T. Rayhani. "Adfreeze Strength and Creep Behavior of Pile Foundations in Warming Permafrost." In Advances in Analysis and Design of Deep Foundations, 254–64. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-61642-1_20.

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Fu, Yu Can, Hong Jun Xu, and Fang Hong Sun. "Experimental Study on Creep Feed Deep Grinding Titanium Alloy with Slotted CBN Grinding Wheel." In Advances in Grinding and Abrasive Technology XIII, 166–70. Stafa: Trans Tech Publications Ltd., 2006. http://dx.doi.org/10.4028/0-87849-986-5.166.

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Ezeajugh, Lambert E., and Lex G. Vanderstaay. "Mobilized Resistances Based on Static, Dynamic, and Numerical Methods at the Jingi Jingi Creek Bridge Replacement Project, Queensland, Australia." In 10th International Conference on Stress Wave Theory and Testing Methods for Deep Foundations, 611–25. 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959: ASTM International, 2019. http://dx.doi.org/10.1520/stp161120170157.

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MacWilliams, M., R. Street, and P. Kitanidis. "Modeling floodplain flow on lower Deer Creek, CA." In River Flow 2004, 1429–39. CRC Press, 2004. http://dx.doi.org/10.1201/b16998-188.

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Movassaghi, Greta, Michelle Fisher, James Doyle, and Roger Nichols. "Watershed Restoration in Deer Creek, Washington—A Ten-Year Review." In Sustainable Fisheries Management. CRC Press, 1999. http://dx.doi.org/10.1201/9781439822678.ch38.

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House, Craig, Vincent May, and Anita Diaz. "15. Sika Deer trampling and saltmarsh creek erosion: Preliminary investigation." In The Ecology of Poole Harbour, 189–93. Elsevier, 2005. http://dx.doi.org/10.1016/s1568-2692(05)80020-8.

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Conference papers on the topic "Deer Creek"

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Foky, Trent, Alice Hinzmann, Chantal Iosso, Eliza Van Wetter, and Lyman P. Persico. "UNRAVELING THE GEOMORPHIC HISTORY OF BLACKTAIL DEER CREEK." In 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346817.

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Dumańska-Słowik, Magdalena, Lucyna Natkaniec-Nowak, Adam Gaweł, Joanna Kowalczyk-Szpyt, Stanislava Milovska, and Anna Łatkiewicz. "Fire Phenomenon in Agate from Deer Creek (Arizona, USA)." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.623.

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Stephens, Ryan, Oliver Obregon, Reed E. Chilton, Gustavious P. Williams, and E. James Nelson. "Field Algae Measurements Using Empirical Correlations at Deer Creek Reservoir." In World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)396.

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Phinney, April, Lyman P. Persico, Andrew Luhmann, Chantal Iosso, Alice Hinzmann, Trent Foky, and Eliza Van Wetter. "GEOMORPHIC CONTROLS ON HYDRAULIC PROCESSES OF BLACKTAIL DEER CREEK, YELLOWSTONE NATIONAL PARK." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-360039.

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Obregon, Oliver, Gustavious P. Williams, E. James Nelson, Jerry B. Miller, Nicolas A. Gonzalez, and Nathan R. Swain. "Simulated Climate Change Effects in Deer Creek Reservoir with a Two-Dimensional Model." In World Environmental And Water Resources Congress 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412312.347.

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Van Wetter, Eliza, Trent Foky, Trent Foky, Alice Hinzmann, Alice Hinzmann, Chantal Iosso, Chantal Iosso, et al. "EVERY PEBBLE COUNTS: A RECONSTRUCTION OF THE FLUVIAL HISTORY OF BLACKTAIL DEER CREEK." In 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346814.

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Denham, Samantha M., and Tarka Wilcox. "POTENTIAL EXTENTS AND VOLUME SCENARIOS OF LANDSLIDE INDUCED IMPOUNDMENT LAKES WITHIN DEER CREEK DRAINAGE, WASHINGTON." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301550.

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Lounsbury, Derek, Oliver Obregon, Reed Chilton, Rolando F. Velasquez, Gustavious P. Williams, and E. James Nelson. "Sediment Oxygen Demand and Pore Water Phosphate Flux: Measurement, Characterization, and Monitoring in Deer Creek Reservoir." In World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)108.

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Buehler, Blake, Pablo Moreno, Gustavious P. Williams, E. James Nelson, Oliver Obregon, Nicolas Gonzalez, and Nathan R. Swain. "Correlations between Total Solids, Total Suspended Solids, Total Volatile Suspended Solids, and Phosphate at Deer Creek Reservoir." In World Environmental And Water Resources Congress 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412312.341.

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Simmons, Marvin D., Brook Brosi, and Tommy Haskins. "Remedial Treatment Exploration, Wolf Creek Dam (REPRINT)." In Proceedings of the Fourth International Conference on Grouting and Deep Mixing. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412350.0097.

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Reports on the topic "Deer Creek"

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Shem, L. M., G. D. Van Dyke, and R. E. Zimmerman. Pipeline corridors through wetlands - impacts on plant communities: Deep Creek and Brandy Branch crossings, Nassau County, Florida. Office of Scientific and Technical Information (OSTI), December 1994. http://dx.doi.org/10.2172/10119538.

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Chevrier, T. S., and E. C. Turner. Lithostratigraphy of deep-water lower Paleozoic strata in the central Misty Creek embayment, Mackenzie Mountains, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292568.

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Ondov, J. M., J. A. Dodd, and J. A. Tuncel. Investigation of submicrometer aerosols for apportioning the impacts of airborne particulate matter at Deep Creek Lake: Final report. Office of Scientific and Technical Information (OSTI), April 1988. http://dx.doi.org/10.2172/6282970.

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Rogers, David W. Geologic Map of the Deep Creek Mountains Wilderness Study Area, Tooele and Juab Counties, Utah (GIS Reproduction of USGS MF-2099 [1989]). Utah Geological Survey, June 2020. http://dx.doi.org/10.34191/ofr-717dr.

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McParland, D., R. McKillop, and A. Blais-Stevens. Adjustments in channel planform and longitudinal profile at proposed pipeline crossings of Smoky River, Deep Valley Creek, and Little Smoky River, northwestern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2018. http://dx.doi.org/10.4095/308339.

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Lavoie, D., O. H. Ardakani, and C. Rivard. Synthesis of organic matter composition and maturation and gas data from selected deep source rock units for some wells in the Fox Creek area. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328238.

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Water resources of Wildcat Creek and Deer Creek basins, Howard and parts of adjacent counties, Indiana, 1979-82. US Geological Survey, 1985. http://dx.doi.org/10.3133/wri854076.

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Nutrients and organic compounds in Deer Creek and south branch Plum Creek in southwestern Pennsylvania, April 1996 through September 1998. US Geological Survey, 2001. http://dx.doi.org/10.3133/wri004061.

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Water-surface profile and flood boundaries for the computed 100-year flood, Lame Deer Creek, Northern Cheyenne Indian Reservation, Montana. US Geological Survey, 1994. http://dx.doi.org/10.3133/wri934216.

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Mineral resources of the Upper Deep Creek Wilderness Study Area, Owyhee County, Idaho. US Geological Survey, 1987. http://dx.doi.org/10.3133/b1719g.

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