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• 1. [Article] Emergent thermodynamics in a system of macroscopic, chaotic surface waves

  The properties of conventional materials are inextricably linked with their molecular composition; to make water flow like wine would require changing its molecular identity. To circumvent this restriction, ...

  Citation × Citation Citation Abstract Copy Title: Emergent thermodynamics in a system of macroscopic, chaotic surface waves Author: Welch, Kyle Year: 2016 The properties of conventional materials are inextricably linked with their molecular composition; to make water flow like wine would require changing its molecular identity. To circumvent this restriction, I have contstructed and characterized a two-dimensional metafluid, so-called because its constitutive dynamics are derived not from atoms and molecules but from macroscopic, chaotic surface waves excited on a vertically agitated fluid. Unlike in conventional fluids, the viscosity and temperature of this metafluid are independantly tunable. Despite this unconventional property, our system is surprisingly consistent with equilibrium thermodynamics, despite being constructed from macroscopic, non-equilibrium elements. As a programmable material, our metafluid represents a new platform on which to study complex phenomena such as self-assembly and pattern formation. We demonstrate one such application in our study of short-chain polymer analogs embedded in our system. Title: Emergent thermodynamics in a system of macroscopic, chaotic surface waves Author: Welch, Kyle Year: 2016 The properties of conventional materials are inextricably linked with their molecular composition; to make water flow like wine would require changing its molecular identity. To circumvent this restriction, I have contstructed and characterized a two-dimensional metafluid, so-called because its constitutive dynamics are derived not from atoms and molecules but from macroscopic, chaotic surface waves excited on a vertically agitated fluid. Unlike in conventional fluids, the viscosity and temperature of this metafluid are independantly tunable. Despite this unconventional property, our system is surprisingly consistent with equilibrium thermodynamics, despite being constructed from macroscopic, non-equilibrium elements. As a programmable material, our metafluid represents a new platform on which to study complex phenomena such as self-assembly and pattern formation. We demonstrate one such application in our study of short-chain polymer analogs embedded in our system. Close

• 2. [Article] Review of Estimates of ground-water recharge, base flow, and stream reach gains and losses in the Willamette River Basin, Oregon

  1 p. Review produced for HC 441: Science Colloquium: Willamette River Environmental Health, Robert D. Clark Honors College, University of Oregon, Spring term, 2004.

  Citation × Citation Citation Abstract Copy Title: Review of Estimates of ground-water recharge, base flow, and stream reach gains and losses in the Willamette River Basin, Oregon Author: Gordon, Eleanor, Lee, Karl K., Risley, John C., Geological Survey (U.S.) Year: 2006, 2004 1 p. Review produced for HC 441: Science Colloquium: Willamette River Environmental Health, Robert D. Clark Honors College, University of Oregon, Spring term, 2004. Title: Review of Estimates of ground-water recharge, base flow, and stream reach gains and losses in the Willamette River Basin, Oregon Author: Gordon, Eleanor, Lee, Karl K., Risley, John C., Geological Survey (U.S.) Year: 2006, 2004 1 p. Review produced for HC 441: Science Colloquium: Willamette River Environmental Health, Robert D. Clark Honors College, University of Oregon, Spring term, 2004. Close

• 3. [Article] MORPHOLOGICAL VARIATION OF PISASTER OCHRACEUS IN RESPONSE TO WAVE EXPOSURE

  52 pages. A thesis presented to the Department of Biology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2...

  Citation × Citation Citation Abstract Copy Title: MORPHOLOGICAL VARIATION OF PISASTER OCHRACEUS IN RESPONSE TO WAVE EXPOSURE Author: Bjorkquist, Alyssa Year: 2016 52 pages. A thesis presented to the Department of Biology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Title: MORPHOLOGICAL VARIATION OF PISASTER OCHRACEUS IN RESPONSE TO WAVE EXPOSURE Author: Bjorkquist, Alyssa Year: 2016 52 pages. A thesis presented to the Department of Biology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Close

• 4. [Article] Trout Creek swamp restoration environmental assessment

  51 pp. Map, table, references. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is ...

  Citation × Citation Citation Abstract Copy Title: Trout Creek swamp restoration environmental assessment Author: Sisters Ranger District (Or.) Year: 2008, 2002 51 pp. Map, table, references. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is just south of Whispering Pines Campground, at the junction of Forest Roads 1018 and 1520. Captured May 25, 2007. Title: Trout Creek swamp restoration environmental assessment Author: Sisters Ranger District (Or.) Year: 2008, 2002 51 pp. Map, table, references. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is just south of Whispering Pines Campground, at the junction of Forest Roads 1018 and 1520. Captured May 25, 2007. Close

• 5. [Article] Trout Creek swamp restoration decision notice and finding of no significant impact

  7 pp. Map. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is just south of Whispering ...

  Citation × Citation Citation Abstract Copy Title: Trout Creek swamp restoration decision notice and finding of no significant impact Author: Sisters Ranger District (Or.) Year: 2008, 2002 7 pp. Map. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is just south of Whispering Pines Campground, at the junction of Forest Roads 1018 and 1520. Captured May 25, 2007. Title: Trout Creek swamp restoration decision notice and finding of no significant impact Author: Sisters Ranger District (Or.) Year: 2008, 2002 7 pp. Map. The swamp is located about 10 miles west of Sisters, in Deschutes County, Oregon, on the Sisters Ranger District of the Deschutes National Forest (Figure 1). The swamp is just south of Whispering Pines Campground, at the junction of Forest Roads 1018 and 1520. Captured May 25, 2007. Close

• 6. [Article] A Model of Basal Hydrologic Networks and Effective Stress Beneath an Ice Sheet

  Subglacial processes that control the water pressure and flow determine the large-scale behavior of the overlying ice by regulating basal resistance. We implement a model in which a steady-state subglacial ...

  Citation × Citation Citation Abstract Copy Title: A Model of Basal Hydrologic Networks and Effective Stress Beneath an Ice Sheet Author: Papamarcos, Sara Year: 2012 Subglacial processes that control the water pressure and flow determine the large-scale behavior of the overlying ice by regulating basal resistance. We implement a model in which a steady-state subglacial conduit system is surrounded by fully saturated porous media. We investigate branching in this system at fixed angles of 15 degrees, 30 degrees and 45 degrees to the direction of ice flow and further assess these systems by calculating the hydraulic potential gradient to determine conduit flow path. We solve our governing equations for porous media flow and allow ice infiltration of the pore space to occur at a critical effective stress N infiltration. For low values of N infiltration, ice infiltration of sediment allows these conduits to follow their original paths. Where insufficient ice infiltration occurs, the conduit path instead lies parallel to the direction of ice flow. Our results speak to the importance of incorporating small-scale processes into models of subglacial hydrologic networks. Title: A Model of Basal Hydrologic Networks and Effective Stress Beneath an Ice Sheet Author: Papamarcos, Sara Year: 2012 Subglacial processes that control the water pressure and flow determine the large-scale behavior of the overlying ice by regulating basal resistance. We implement a model in which a steady-state subglacial conduit system is surrounded by fully saturated porous media. We investigate branching in this system at fixed angles of 15 degrees, 30 degrees and 45 degrees to the direction of ice flow and further assess these systems by calculating the hydraulic potential gradient to determine conduit flow path. We solve our governing equations for porous media flow and allow ice infiltration of the pore space to occur at a critical effective stress N infiltration. For low values of N infiltration, ice infiltration of sediment allows these conduits to follow their original paths. Where insufficient ice infiltration occurs, the conduit path instead lies parallel to the direction of ice flow. Our results speak to the importance of incorporating small-scale processes into models of subglacial hydrologic networks. Close

• 7. [Article] A Hierarchical Modeling Approach to Simulating the Geomorphic Response of River Systems to Climate Change

  Anthropogenic climate change significantly affects water resources. River flows in mountainous regions are driven by snowmelt and are therefore highly sensitive to increases in temperature resulting from ...

  Citation × Citation Citation Abstract Copy Title: A Hierarchical Modeling Approach to Simulating the Geomorphic Response of River Systems to Climate Change Author: Praskievicz, Sarah Year: 2014 Anthropogenic climate change significantly affects water resources. River flows in mountainous regions are driven by snowmelt and are therefore highly sensitive to increases in temperature resulting from climate change. Climate-driven hydrological changes are potentially significant for the fluvial geomorphology of river systems. In unchanging climatic and tectonic conditions, a river's morphology will develop in equilibrium with inputs of water and sediment, but climate change represents a potential forcing on these variables that may push the system into disequilibrium and cause significant changes in river morphology. Geomorphic factors, such as channel geometry, planform, and sediment transport, are major determinants of the value of river systems, including their suitability for threatened and endangered species and for human uses of water. This dissertation research uses a hierarchical modeling approach to investigate potential impacts of anthropogenic climate change on river morphology in the interior Pacific Northwest. The research will address the following theoretical and methodological objectives: 1) Develop downscaled climate change scenarios, based on regional climate-model output, including changes in daily minimum and maximum temperature and precipitation. 2) Estimate how climate change scenarios affect river discharge and suspended-sediment load, using a basin-scale hydrologic model. 3) Examine potential impacts of climate-driven hydrologic changes on stream power and shear stress, bedload sediment transport, and river morphology, including channel geometry and planform. The downscaling approach, based on empirically-estimated local topographic lapse rates, produces high-resolution climate grids with positive forecast skill. The hydrologic modeling results indicate that projected climate change in the study rivers will change the annual cycle of hydrology, with increased winter discharge, a decrease in the magnitude of the spring snowmelt peak, and decreased summer discharge. Geomorphic modeling results suggest that changes in reach-averaged bedload transport are highly sensitive to likely changes in the recurrence interval of the critical discharge needed to mobilize bed sediments. This dissertation research makes an original contribution to the climate-change impacts literature by linking Earth processes across a wide range of spatial scales to project changes in river systems that may be significant for management of these systems for societal and ecological benefits. This dissertation includes unpublished co-authored material. Title: A Hierarchical Modeling Approach to Simulating the Geomorphic Response of River Systems to Climate Change Author: Praskievicz, Sarah Year: 2014 Anthropogenic climate change significantly affects water resources. River flows in mountainous regions are driven by snowmelt and are therefore highly sensitive to increases in temperature resulting from climate change. Climate-driven hydrological changes are potentially significant for the fluvial geomorphology of river systems. In unchanging climatic and tectonic conditions, a river's morphology will develop in equilibrium with inputs of water and sediment, but climate change represents a potential forcing on these variables that may push the system into disequilibrium and cause significant changes in river morphology. Geomorphic factors, such as channel geometry, planform, and sediment transport, are major determinants of the value of river systems, including their suitability for threatened and endangered species and for human uses of water. This dissertation research uses a hierarchical modeling approach to investigate potential impacts of anthropogenic climate change on river morphology in the interior Pacific Northwest. The research will address the following theoretical and methodological objectives: 1) Develop downscaled climate change scenarios, based on regional climate-model output, including changes in daily minimum and maximum temperature and precipitation. 2) Estimate how climate change scenarios affect river discharge and suspended-sediment load, using a basin-scale hydrologic model. 3) Examine potential impacts of climate-driven hydrologic changes on stream power and shear stress, bedload sediment transport, and river morphology, including channel geometry and planform. The downscaling approach, based on empirically-estimated local topographic lapse rates, produces high-resolution climate grids with positive forecast skill. The hydrologic modeling results indicate that projected climate change in the study rivers will change the annual cycle of hydrology, with increased winter discharge, a decrease in the magnitude of the spring snowmelt peak, and decreased summer discharge. Geomorphic modeling results suggest that changes in reach-averaged bedload transport are highly sensitive to likely changes in the recurrence interval of the critical discharge needed to mobilize bed sediments. This dissertation research makes an original contribution to the climate-change impacts literature by linking Earth processes across a wide range of spatial scales to project changes in river systems that may be significant for management of these systems for societal and ecological benefits. This dissertation includes unpublished co-authored material. Close

• 8. [Article] Paying the water bill : community support for agriculture and river restoration in central Oregon

  2 pages

  Citation × Citation Citation Abstract Copy Title: Paying the water bill : community support for agriculture and river restoration in central Oregon Author: University of Oregon. Ecosystem Workforce Program Year: 2016, 2013 2 pages Title: Paying the water bill : community support for agriculture and river restoration in central Oregon Author: University of Oregon. Ecosystem Workforce Program Year: 2016, 2013 2 pages Close

• 9. [Article] After the Flow: Landscape Response to the Emplacement of Holocene Lava Flows, Central Oregon Cascades, USA

  Effusive volcanic eruptions repave landscapes rapidly with lava flows, resetting the underlying landscape and ecosystem. The unique physical properties of lava pose interesting challenges for recovery, ...

  Citation × Citation Citation Abstract Copy Title: After the Flow: Landscape Response to the Emplacement of Holocene Lava Flows, Central Oregon Cascades, USA Author: Deligne, Natalia Year: 2012 Effusive volcanic eruptions repave landscapes rapidly with lava flows, resetting the underlying landscape and ecosystem. The unique physical properties of lava pose interesting challenges for recovery, as lava flows can be highly permeable while lava itself is dense, sterile, and generally inhospitable towards life. This dissertation examines two aspects of landscape recovery following lava flow emplacement: (1) hydrologic adaptation of surface and groundwater to recent volcanism and (2) plant colonization of young lava flows. I examine two sites in the central Oregon Cascades: the c. 3 ka Sand Mountain volcanic field (SMVF), located in the headwaters of the McKenzie River, a critical water resource for the state of Oregon, and the c. 1.5 ka Collier Cone lava flow, originating on the north flanks of North Sister volcano. My investigation of the SMVF and upper McKenzie River watershed reveals a complex volcanic history with profound impacts on the configuration and short-term discharge of the McKenzie River: lava flows from the SMVF and other Holocene vents have buried, dammed, and altered the path of the McKenzie River. Moreover, given the large groundwater contribution from the SMVF to the McKenzie River, I estimate that SMVF activity caused McKenzie River discharge in present-day Eugene, Oregon to decrease by up to 20% for days to months at a time; future regional mafic volcanic activity could have a similar impact. The SMVF and the Collier Cone lava flow are notable for the juxtaposition of barren exposed lava and mature forests on the same or similarly aged lava flows. I use a combination of LiDAR analysis, field observations, and soil characterization to examine soil and vegetation at these two sites and find that the presence of an external soil source greatly facilitates plant establishment, growth, and survival. Here, external soil sources are syn- or post-eruptive tephra (SMVF) or flood-borne deposits (Collier Cone lava flow). External soil appears to provide a substrate for plants to grow in along with key nutrients and sufficient moisture; overall, external soil sources are key for the initial recovery following an effusive volcanic disturbance. This dissertation includes co-authored material submitted for publication. Title: After the Flow: Landscape Response to the Emplacement of Holocene Lava Flows, Central Oregon Cascades, USA Author: Deligne, Natalia Year: 2012 Effusive volcanic eruptions repave landscapes rapidly with lava flows, resetting the underlying landscape and ecosystem. The unique physical properties of lava pose interesting challenges for recovery, as lava flows can be highly permeable while lava itself is dense, sterile, and generally inhospitable towards life. This dissertation examines two aspects of landscape recovery following lava flow emplacement: (1) hydrologic adaptation of surface and groundwater to recent volcanism and (2) plant colonization of young lava flows. I examine two sites in the central Oregon Cascades: the c. 3 ka Sand Mountain volcanic field (SMVF), located in the headwaters of the McKenzie River, a critical water resource for the state of Oregon, and the c. 1.5 ka Collier Cone lava flow, originating on the north flanks of North Sister volcano. My investigation of the SMVF and upper McKenzie River watershed reveals a complex volcanic history with profound impacts on the configuration and short-term discharge of the McKenzie River: lava flows from the SMVF and other Holocene vents have buried, dammed, and altered the path of the McKenzie River. Moreover, given the large groundwater contribution from the SMVF to the McKenzie River, I estimate that SMVF activity caused McKenzie River discharge in present-day Eugene, Oregon to decrease by up to 20% for days to months at a time; future regional mafic volcanic activity could have a similar impact. The SMVF and the Collier Cone lava flow are notable for the juxtaposition of barren exposed lava and mature forests on the same or similarly aged lava flows. I use a combination of LiDAR analysis, field observations, and soil characterization to examine soil and vegetation at these two sites and find that the presence of an external soil source greatly facilitates plant establishment, growth, and survival. Here, external soil sources are syn- or post-eruptive tephra (SMVF) or flood-borne deposits (Collier Cone lava flow). External soil appears to provide a substrate for plants to grow in along with key nutrients and sufficient moisture; overall, external soil sources are key for the initial recovery following an effusive volcanic disturbance. This dissertation includes co-authored material submitted for publication. Close

• 10. [Article] EFFECTS OF ACUTE PASSIVE HEAT EXPOSURE

  42 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, ...

  Citation × Citation Citation Abstract Copy Title: EFFECTS OF ACUTE PASSIVE HEAT EXPOSURE Author: Harris, Sarianne Year: 2016 42 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Title: EFFECTS OF ACUTE PASSIVE HEAT EXPOSURE Author: Harris, Sarianne Year: 2016 42 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Close

• 11. [Article] Protecting Stream Ecosystem Health in the Face of Rapid Urbanization and Climate Change

  The ability to anticipate and evaluate the combined impacts of urbanization and climate change on streamflow regimes is critical to developing proactive strategies that protect aquatic ecosystems. I developed ...

  Citation × Citation Citation Abstract Copy Title: Protecting Stream Ecosystem Health in the Face of Rapid Urbanization and Climate Change Author: Wu, Hong Year: 2015 The ability to anticipate and evaluate the combined impacts of urbanization and climate change on streamflow regimes is critical to developing proactive strategies that protect aquatic ecosystems. I developed an interdisciplinary modeling framework to compare and contrast the effectiveness of integrated stormwater management, or its absence, with two regional growth patterns for maintaining streamflow regimes in the context of climate change. In three adjacent urbanizing watersheds in Oregon's Willamette Valley, I conducted a three-step sequence to: 1) simulate land use change under four future development scenarios with the agent-based model Envision; 2) model resultant hydrological change under the recent past and two future climate regimes using the Soil and Water Assessment Tool; and 3) assess scenario impacts on streamflow regimes using 10 ecologically significant flow metrics. I evaluated each scenario in each basin using a flow metric typology based on the magnitude of change in each metric and the degree to which such changes could be mitigated, i.e., insensitive, sensitive and manageable, and sensitive and resistant. My results demonstrated distinct signatures of urbanization and climate change on flow regimes. Urbanization and climate change in isolation led to significant flow alterations in all three basins. Urbanization consistently led to increases in flow regime flashiness and severity of extreme flow events, whereas climate change primarily caused a drying trend. Climate change tended to exacerbate the impacts of urbanization but also mitigated urban impacts on several metrics. The combined impacts of urbanization and climate change caused substantial changes to metric sensitivities, which further differed by basin and climate regime, highlighting the uncertainties of streamflow regime responses to development and the value of spatially explicit modeling that can reveal complex interactions between natural and human systems. Scenario comparisons demonstrated the importance of integrated stormwater management and, secondarily, compact regional growth. My findings reveal the need for regional flow-ecology research that substantiates the ecological significance of each flow metric, develops specific targets for manageable ones, and explores potential remedies for resistant ones. The interdisciplinary modeling framework shows promise as a transferable tool for local watershed management. This dissertation includes previously unpublished co-authored material. Title: Protecting Stream Ecosystem Health in the Face of Rapid Urbanization and Climate Change Author: Wu, Hong Year: 2015 The ability to anticipate and evaluate the combined impacts of urbanization and climate change on streamflow regimes is critical to developing proactive strategies that protect aquatic ecosystems. I developed an interdisciplinary modeling framework to compare and contrast the effectiveness of integrated stormwater management, or its absence, with two regional growth patterns for maintaining streamflow regimes in the context of climate change. In three adjacent urbanizing watersheds in Oregon's Willamette Valley, I conducted a three-step sequence to: 1) simulate land use change under four future development scenarios with the agent-based model Envision; 2) model resultant hydrological change under the recent past and two future climate regimes using the Soil and Water Assessment Tool; and 3) assess scenario impacts on streamflow regimes using 10 ecologically significant flow metrics. I evaluated each scenario in each basin using a flow metric typology based on the magnitude of change in each metric and the degree to which such changes could be mitigated, i.e., insensitive, sensitive and manageable, and sensitive and resistant. My results demonstrated distinct signatures of urbanization and climate change on flow regimes. Urbanization and climate change in isolation led to significant flow alterations in all three basins. Urbanization consistently led to increases in flow regime flashiness and severity of extreme flow events, whereas climate change primarily caused a drying trend. Climate change tended to exacerbate the impacts of urbanization but also mitigated urban impacts on several metrics. The combined impacts of urbanization and climate change caused substantial changes to metric sensitivities, which further differed by basin and climate regime, highlighting the uncertainties of streamflow regime responses to development and the value of spatially explicit modeling that can reveal complex interactions between natural and human systems. Scenario comparisons demonstrated the importance of integrated stormwater management and, secondarily, compact regional growth. My findings reveal the need for regional flow-ecology research that substantiates the ecological significance of each flow metric, develops specific targets for manageable ones, and explores potential remedies for resistant ones. The interdisciplinary modeling framework shows promise as a transferable tool for local watershed management. This dissertation includes previously unpublished co-authored material. Close

• 12. [Article] Mechanisms of heat acclimation and exercise performance

  xvii, 245 p. : ill. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.

  Citation × Citation Citation Abstract Copy Title: Mechanisms of heat acclimation and exercise performance Author: Lorenzo, Santiago, 1978- Year: 2010 xvii, 245 p. : ill. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number. Title: Mechanisms of heat acclimation and exercise performance Author: Lorenzo, Santiago, 1978- Year: 2010 xvii, 245 p. : ill. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number. Close

• 13. [Article] Columbia County : Stormwater and erosion control ordinance

  24 pp. Bookmarks supplied by UO. Published November 21, 2001. Captured February 2, 2009.

  Citation × Citation Citation Abstract Copy Title: Columbia County : Stormwater and erosion control ordinance Author: Columbia County (Or.) Year: 2009, 2001 24 pp. Bookmarks supplied by UO. Published November 21, 2001. Captured February 2, 2009. Title: Columbia County : Stormwater and erosion control ordinance Author: Columbia County (Or.) Year: 2009, 2001 24 pp. Bookmarks supplied by UO. Published November 21, 2001. Captured February 2, 2009. Close

• 14. [Article] Forgetting Nature: The Importance of Including Environmental Flows in International Water Agreements

  34 pages

  Citation × Citation Citation Abstract Copy Title: Forgetting Nature: The Importance of Including Environmental Flows in International Water Agreements Author: Hardberger, Amy Year: 2016 34 pages Title: Forgetting Nature: The Importance of Including Environmental Flows in International Water Agreements Author: Hardberger, Amy Year: 2016 34 pages Close

• 15. [Article] Silverton Notice of Adopted Amendment (2011-08-05)

  6 pp. Adopted 2011-08-05. Department of Land Conservation and Development Notice of Adopted Amendment

  Citation × Citation Citation Abstract Copy Title: Silverton Notice of Adopted Amendment (2011-08-05) Author: Silverton Year: 2014, 2011 6 pp. Adopted 2011-08-05. Department of Land Conservation and Development Notice of Adopted Amendment Title: Silverton Notice of Adopted Amendment (2011-08-05) Author: Silverton Year: 2014, 2011 6 pp. Adopted 2011-08-05. Department of Land Conservation and Development Notice of Adopted Amendment Close

• 16. [Article] Martin Creek instream restoration environmental assessment

  28 pp. References, appendix. Martin Creek, a major tributary of Middle Creek, runs through Section 35 of T. 31 S., R. 7 W., and Sections 1, 2, 12 and 13 of T. 32 S., R. 7 W. Captured July 26, 2007.

  Citation × Citation Citation Abstract Copy Title: Martin Creek instream restoration environmental assessment Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 28 pp. References, appendix. Martin Creek, a major tributary of Middle Creek, runs through Section 35 of T. 31 S., R. 7 W., and Sections 1, 2, 12 and 13 of T. 32 S., R. 7 W. Captured July 26, 2007. Title: Martin Creek instream restoration environmental assessment Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 28 pp. References, appendix. Martin Creek, a major tributary of Middle Creek, runs through Section 35 of T. 31 S., R. 7 W., and Sections 1, 2, 12 and 13 of T. 32 S., R. 7 W. Captured July 26, 2007. Close

• 17. [Article] Eruptive Processes of Mafic Arc Volcanoes – Subaerial and Submarine Perspectives

  xviii, 179 p. : ill. (some col.). Includes 3 video files.

  Citation × Citation Citation Abstract Copy Title: Eruptive Processes of Mafic Arc Volcanoes – Subaerial and Submarine Perspectives Author: Deardorff, Nicholas D., 1980- Year: 2012, 2011 xviii, 179 p. : ill. (some col.). Includes 3 video files. Title: Eruptive Processes of Mafic Arc Volcanoes – Subaerial and Submarine Perspectives Author: Deardorff, Nicholas D., 1980- Year: 2012, 2011 xviii, 179 p. : ill. (some col.). Includes 3 video files. Close

• 18. [Article] Increasing stream flows to sustain salmon in the Northwest: an economic and policy assessment

  26 p.

  Citation × Citation Citation Abstract Copy Title: Increasing stream flows to sustain salmon in the Northwest: an economic and policy assessment Author: Jaeger, William K., Mikesell, Raymond Year: 2006, 2000 26 p. Title: Increasing stream flows to sustain salmon in the Northwest: an economic and policy assessment Author: Jaeger, William K., Mikesell, Raymond Year: 2006, 2000 26 p. Close

• 19. [Article] Valuation of Ecosystem Services in Trinity County, California

  xvii, 141 p. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.

  Citation × Citation Citation Abstract Copy Title: Valuation of Ecosystem Services in Trinity County, California Author: MacFarland, Katherine Dana Year: 2010 xvii, 141 p. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number. Title: Valuation of Ecosystem Services in Trinity County, California Author: MacFarland, Katherine Dana Year: 2010 xvii, 141 p. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number. Close

• 20. [Article] Tube hood orientations of Pista pacifica (Polychaeta: Terebellidae)

  vi, 58 p. ; ill., maps. A print copy of this title is available from the Oregon Institute of Marine Biology library, under the call number OIMB QL391.A6 W5.

  Citation × Citation Citation Abstract Copy Title: Tube hood orientations of Pista pacifica (Polychaeta: Terebellidae) Author: Winnick, Kenneth Brian, 1954- Year: 2009, 1981 vi, 58 p. ; ill., maps. A print copy of this title is available from the Oregon Institute of Marine Biology library, under the call number OIMB QL391.A6 W5. Title: Tube hood orientations of Pista pacifica (Polychaeta: Terebellidae) Author: Winnick, Kenneth Brian, 1954- Year: 2009, 1981 vi, 58 p. ; ill., maps. A print copy of this title is available from the Oregon Institute of Marine Biology library, under the call number OIMB QL391.A6 W5. Close

• 21. [Article] MWMC Wastewater Facilities Plan for the Eugene-Springfield Regional Wastewater Treatment Facilities

  28 pp. Document contains content through Executive Summary. Diagram, tables, chart. Originally published April 2004, updated December 2004 to include Oregon Department of Environmental Quality comments...

  Citation × Citation Citation Abstract Copy Title: MWMC Wastewater Facilities Plan for the Eugene-Springfield Regional Wastewater Treatment Facilities Author: Metropolitan Wastewater Management Commission (Eugene, Or.) Year: 2013, 2004 28 pp. Document contains content through Executive Summary. Diagram, tables, chart. Originally published April 2004, updated December 2004 to include Oregon Department of Environmental Quality comments. Title: MWMC Wastewater Facilities Plan for the Eugene-Springfield Regional Wastewater Treatment Facilities Author: Metropolitan Wastewater Management Commission (Eugene, Or.) Year: 2013, 2004 28 pp. Document contains content through Executive Summary. Diagram, tables, chart. Originally published April 2004, updated December 2004 to include Oregon Department of Environmental Quality comments. Close

• 22. [Article] The transport and distribution of the toxic diatom Pseudo-nitzschia spp. in the Coos Bay estuary and the adjacent continental shelf

  Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 84-88). Description: x, 88 leaves : ill. ; 29 cm.

  Citation × Citation Citation Abstract Copy Title: The transport and distribution of the toxic diatom Pseudo-nitzschia spp. in the Coos Bay estuary and the adjacent continental shelf Author: Cziesla, Christopher A., 1969- Year: 2009, 1999 Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 84-88). Description: x, 88 leaves : ill. ; 29 cm. Title: The transport and distribution of the toxic diatom Pseudo-nitzschia spp. in the Coos Bay estuary and the adjacent continental shelf Author: Cziesla, Christopher A., 1969- Year: 2009, 1999 Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 84-88). Description: x, 88 leaves : ill. ; 29 cm. Close

• 23. [Article] Modeling Circulation Dynamics and Submarine Melt in Greenland Fjords

  Meltwater accumulated on the Greenland Ice Sheet drains to glacier beds, discharging into fjords hundreds of meters below sea level. The injection of meltwater at depth generates an upwelling plume that ...

  Citation × Citation Citation Abstract Copy Title: Modeling Circulation Dynamics and Submarine Melt in Greenland Fjords Author: Carroll, Dustin Year: 2017 Meltwater accumulated on the Greenland Ice Sheet drains to glacier beds, discharging into fjords hundreds of meters below sea level. The injection of meltwater at depth generates an upwelling plume that entrains warm ocean water as it rises along the terminus, increasing submarine melt and driving a fjord-scale exchange flow. However, due to sparse ocean-glacier observations, we lack a process understanding of how plumes control fjord circulation and submarine melt. Combining numerical modeling, theory, and observations, this dissertation investigates near-glacier plume dynamics, the influence of glacier depth on plume structure and submarine melt, and the role of fjord-glacier geometry on circulation in tidewater glacier fjords. In Chapter II, I use buoyant plume theory and a nonhydrostatic, three-dimensional ocean–ice model to investigate the sensitivity of plume dynamics to subglacial discharge, turbulent diffusivity, and conduit geometry. Large discharges result in plumes with positive temperature and salinity anomalies in the upper water column. Fjord circulation is sensitive to conduit geometry; distributed subglacial discharge results in a stronger return flow of warm water toward the terminus. In Chapter III, I use buoyant plume theory, initialized with realistic ranges of subglacial discharge, glacier depth, and ocean stratification, to investigate how plume structure and submarine melt vary during summer months in 12 Greenland fjords. Grounding line depth is a primary control on plume-induced submarine melt: deep glaciers produce warm, salty subsurface plumes that undercut termini, and shallow glaciers produce cold, fresh surface-confined plumes that can overcut. Finally, in Chapter IV, I use regional-scale numerical ocean simulations to systematically evaluate how fjord circulation forced by subglacial plumes, tides, and wind stress depends on fjord width, glacier depth, and sill height. Glaciers grounded below sill depth can draw shelf waters over a shallow sill and into fjord basins with seasonal subglacial discharge; this process is independent of external shelf forcing. These results underscore the first-order effect that subglacial discharge and fjord-glacier geometry have in controlling fjord circulation and, thus, ocean heat flux to the ice. This dissertation includes previously published and co-authored material. Title: Modeling Circulation Dynamics and Submarine Melt in Greenland Fjords Author: Carroll, Dustin Year: 2017 Meltwater accumulated on the Greenland Ice Sheet drains to glacier beds, discharging into fjords hundreds of meters below sea level. The injection of meltwater at depth generates an upwelling plume that entrains warm ocean water as it rises along the terminus, increasing submarine melt and driving a fjord-scale exchange flow. However, due to sparse ocean-glacier observations, we lack a process understanding of how plumes control fjord circulation and submarine melt. Combining numerical modeling, theory, and observations, this dissertation investigates near-glacier plume dynamics, the influence of glacier depth on plume structure and submarine melt, and the role of fjord-glacier geometry on circulation in tidewater glacier fjords. In Chapter II, I use buoyant plume theory and a nonhydrostatic, three-dimensional ocean–ice model to investigate the sensitivity of plume dynamics to subglacial discharge, turbulent diffusivity, and conduit geometry. Large discharges result in plumes with positive temperature and salinity anomalies in the upper water column. Fjord circulation is sensitive to conduit geometry; distributed subglacial discharge results in a stronger return flow of warm water toward the terminus. In Chapter III, I use buoyant plume theory, initialized with realistic ranges of subglacial discharge, glacier depth, and ocean stratification, to investigate how plume structure and submarine melt vary during summer months in 12 Greenland fjords. Grounding line depth is a primary control on plume-induced submarine melt: deep glaciers produce warm, salty subsurface plumes that undercut termini, and shallow glaciers produce cold, fresh surface-confined plumes that can overcut. Finally, in Chapter IV, I use regional-scale numerical ocean simulations to systematically evaluate how fjord circulation forced by subglacial plumes, tides, and wind stress depends on fjord width, glacier depth, and sill height. Glaciers grounded below sill depth can draw shelf waters over a shallow sill and into fjord basins with seasonal subglacial discharge; this process is independent of external shelf forcing. These results underscore the first-order effect that subglacial discharge and fjord-glacier geometry have in controlling fjord circulation and, thus, ocean heat flux to the ice. This dissertation includes previously published and co-authored material. Close

• 24. [Article] Enabling Sustainable Irrigation: Determining the feasibility of landscape-based strategies

  Examining committee: David Hulse, chair; Roxi Thoren

  Citation × Citation Citation Abstract Copy Title: Enabling Sustainable Irrigation: Determining the feasibility of landscape-based strategies Author: Carroll, Madeline Year: 2013 Examining committee: David Hulse, chair; Roxi Thoren Title: Enabling Sustainable Irrigation: Determining the feasibility of landscape-based strategies Author: Carroll, Madeline Year: 2013 Examining committee: David Hulse, chair; Roxi Thoren Close

• 25. [Article] Laboratory Experiments in Cold Temperature Rock Deformation

  ix, 44 p. : ill. (some col.)

  Citation × Citation Citation Abstract Copy Title: Laboratory Experiments in Cold Temperature Rock Deformation Author: Van Alst, Laura Jane Year: 2012, 2011 ix, 44 p. : ill. (some col.) Title: Laboratory Experiments in Cold Temperature Rock Deformation Author: Van Alst, Laura Jane Year: 2012, 2011 ix, 44 p. : ill. (some col.) Close

• 26. [Article] Superscribing Sustainability: Reformulating China's Contemporary Urbanism

  Within China's post-1980's urban planning discourse, shan-shui, a significance-laden compound character set translatable as `mountain-water' or `landscape', aligned with urban sustainability. The focus ...

  Citation × Citation Citation Abstract Copy Title: Superscribing Sustainability: Reformulating China's Contemporary Urbanism Author: Rodenbiker, Jesse Year: 2013, 2014 Within China's post-1980's urban planning discourse, shan-shui, a significance-laden compound character set translatable as `mountain-water' or `landscape', aligned with urban sustainability. The focus of this genealogical discourse analysis delineates the origins, evolution, interpretation, and application of the term shan-shui within China's contemporary urbanization as a developing urban design paradigm, informed through transnational flows of urban design practices. This work highlights case studies showing this discourse's morphological materializations and analyzes interviews, publications, media, letter exchanges, and urban designs to problematize the use of shan-shui within the discursive processes of urban development and sustainability discourses. The superscription of shan-shui generates a rubric through which Chinese cultural and symbolic elements are (re)formulated in contemporary urban developments and conjoined with sustainable urban design practices facilitating multifaceted ends including efforts towards sustainable urban development, bourgeoning neo-classical urban aesthetics, conceptual bridging of human-nature relations, land-centric capital accumulation, and a vernacular urbanism. Title: Superscribing Sustainability: Reformulating China's Contemporary Urbanism Author: Rodenbiker, Jesse Year: 2013, 2014 Within China's post-1980's urban planning discourse, shan-shui, a significance-laden compound character set translatable as `mountain-water' or `landscape', aligned with urban sustainability. The focus of this genealogical discourse analysis delineates the origins, evolution, interpretation, and application of the term shan-shui within China's contemporary urbanization as a developing urban design paradigm, informed through transnational flows of urban design practices. This work highlights case studies showing this discourse's morphological materializations and analyzes interviews, publications, media, letter exchanges, and urban designs to problematize the use of shan-shui within the discursive processes of urban development and sustainability discourses. The superscription of shan-shui generates a rubric through which Chinese cultural and symbolic elements are (re)formulated in contemporary urban developments and conjoined with sustainable urban design practices facilitating multifaceted ends including efforts towards sustainable urban development, bourgeoning neo-classical urban aesthetics, conceptual bridging of human-nature relations, land-centric capital accumulation, and a vernacular urbanism. Close

• 27. [Article] Portland : State of the river 2006-07

  68 pp. Maps, tables, charts, figures, illus. Published November, 2007. Captured December 12, 2008.

  Citation × Citation Citation Abstract Copy Title: Portland : State of the river 2006-07 Author: Portland (Or.). Office of Transportation, Port of Portland (Or.), Portland (Or.), Portland (Or.). Bureau of Development Services, Portland (Or.). Water Bureau, Portland Development Commission, Portland (Or.). Bureau of Planning, Portland (Or.). Office of Sustainable Development, Portland Parks and Recreation Year: 2008, 2007 68 pp. Maps, tables, charts, figures, illus. Published November, 2007. Captured December 12, 2008. Title: Portland : State of the river 2006-07 Author: Portland (Or.). Office of Transportation, Port of Portland (Or.), Portland (Or.), Portland (Or.). Bureau of Development Services, Portland (Or.). Water Bureau, Portland Development Commission, Portland (Or.). Bureau of Planning, Portland (Or.). Office of Sustainable Development, Portland Parks and Recreation Year: 2008, 2007 68 pp. Maps, tables, charts, figures, illus. Published November, 2007. Captured December 12, 2008. Close

• 28. [Article] Swiftwater 2004 instream restoration projects finding of no significant impact

  4 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14).

  Citation × Citation Citation Abstract Copy Title: Swiftwater 2004 instream restoration projects finding of no significant impact Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 4 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14). Title: Swiftwater 2004 instream restoration projects finding of no significant impact Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 4 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14). Close

• 29. [Article] Potential Impacts of Climate Change on Hood Canal Hypoxia

  31 pages

  Citation × Citation Citation Abstract Copy Title: Potential Impacts of Climate Change on Hood Canal Hypoxia Author: Schandl, Maria Year: 2017, 2015 31 pages Title: Potential Impacts of Climate Change on Hood Canal Hypoxia Author: Schandl, Maria Year: 2017, 2015 31 pages Close

• 30. [Article] North Fork John Day Wild and Scenic River management plan environmental assessment, decision notice and finding of no significant impact

  200 pp. Tables, appendices, glossary, maps. "The North Fork John Day River is located in Northeast Oregon on both the Umatilla and Wallowa-Whitman National Forests, starting in the North Fork John Day ...

  Citation × Citation Citation Abstract Copy Title: North Fork John Day Wild and Scenic River management plan environmental assessment, decision notice and finding of no significant impact Author: North Fork John Day Ranger District (Or.), Baker Ranger District (Or.) Year: 2008, 1993 200 pp. Tables, appendices, glossary, maps. "The North Fork John Day River is located in Northeast Oregon on both the Umatilla and Wallowa-Whitman National Forests, starting in the North Fork John Day Wilderness (Section 13, T 8 S, R 36 E) and flowing north and then west to its confluence with Camas Creek (Section 33, T 6 S, R 31 E)." Decision notice is dated September 13, 1993. Captured June 12, 2008. Title: North Fork John Day Wild and Scenic River management plan environmental assessment, decision notice and finding of no significant impact Author: North Fork John Day Ranger District (Or.), Baker Ranger District (Or.) Year: 2008, 1993 200 pp. Tables, appendices, glossary, maps. "The North Fork John Day River is located in Northeast Oregon on both the Umatilla and Wallowa-Whitman National Forests, starting in the North Fork John Day Wilderness (Section 13, T 8 S, R 36 E) and flowing north and then west to its confluence with Camas Creek (Section 33, T 6 S, R 31 E)." Decision notice is dated September 13, 1993. Captured June 12, 2008. Close

• 31. [Article] Comprehensive examination of the differences in thermoregulatory and ventilatory responses between humans with and without a PFO under different environmental conditions

  The existence of a patent foramen ovale (PFO) has been known about for nearly 2,000 years. The prevalence of a PFO has been shown to be 25-40% in the general population. Despite the fact that blood flowing ...

  Citation × Citation Citation Abstract Copy Title: Comprehensive examination of the differences in thermoregulatory and ventilatory responses between humans with and without a PFO under different environmental conditions Author: Davis, James Year: 2016 The existence of a patent foramen ovale (PFO) has been known about for nearly 2,000 years. The prevalence of a PFO has been shown to be 25-40% in the general population. Despite the fact that blood flowing through a PFO acts as a shunt, there has been little research looking at the effect a PFO has on physiology in otherwise healthy humans. In Chapter IV, the effect of a PFO on core temperature (Tcore) prior to, and during exercise, was investigated. The design of this experiment included appropriate controls for a thermoregulatory study (i.e. measuring at same time of day, appropriate hydration and food intake, etc.). Results from this study indicate that subjects with a PFO (PFO+) have a Tcore that is ~0.4°C higher at rest and during exercise than subjects without a PFO (PFO–). Additionally, this study showed that PFO– subjects do not increase Tcore to the same extent breathing cold air as they do breathing ambient air during a 10-minute exercise bout, whereas there was no difference in Tcore increase between these two conditions for PFO+ subjects. These findings suggest that the difference in Tcore between PFO+ and PFO– subjects is potentially due to differences in respiratory heat loss. The studies for Chapter V examined differences in thermoregulatory and ventilatory responses during hot water (40°C) and cold water (20°C) immersion. This study found that compared to PFO– subjects, PFO+ subjects 1) increase Tcore at the same rate during hot water immersion and 2) do not cool off as quickly during cold water immersion. Additionally, in subjects who reached a ventilatory threshold, PFO+ subjects had blunted ventilatory responses to increased Tcore compared to PFO– subjects. Finally, in Chapter VI it was shown that PFO+ subjects have blunted ventilatory responses during acute exposure to hyperoxic and normoxic hypercapnia. However, there were no differences in ventilatory responses between PFO+ and PFO– subjects during exposure to either isocapnic or poikilocapnic hypoxia. These findings suggest that PFO+ subjects have a blunted central chemoreflex. This dissertation contains previously, unpublished co-authored material. Title: Comprehensive examination of the differences in thermoregulatory and ventilatory responses between humans with and without a PFO under different environmental conditions Author: Davis, James Year: 2016 The existence of a patent foramen ovale (PFO) has been known about for nearly 2,000 years. The prevalence of a PFO has been shown to be 25-40% in the general population. Despite the fact that blood flowing through a PFO acts as a shunt, there has been little research looking at the effect a PFO has on physiology in otherwise healthy humans. In Chapter IV, the effect of a PFO on core temperature (Tcore) prior to, and during exercise, was investigated. The design of this experiment included appropriate controls for a thermoregulatory study (i.e. measuring at same time of day, appropriate hydration and food intake, etc.). Results from this study indicate that subjects with a PFO (PFO+) have a Tcore that is ~0.4°C higher at rest and during exercise than subjects without a PFO (PFO–). Additionally, this study showed that PFO– subjects do not increase Tcore to the same extent breathing cold air as they do breathing ambient air during a 10-minute exercise bout, whereas there was no difference in Tcore increase between these two conditions for PFO+ subjects. These findings suggest that the difference in Tcore between PFO+ and PFO– subjects is potentially due to differences in respiratory heat loss. The studies for Chapter V examined differences in thermoregulatory and ventilatory responses during hot water (40°C) and cold water (20°C) immersion. This study found that compared to PFO– subjects, PFO+ subjects 1) increase Tcore at the same rate during hot water immersion and 2) do not cool off as quickly during cold water immersion. Additionally, in subjects who reached a ventilatory threshold, PFO+ subjects had blunted ventilatory responses to increased Tcore compared to PFO– subjects. Finally, in Chapter VI it was shown that PFO+ subjects have blunted ventilatory responses during acute exposure to hyperoxic and normoxic hypercapnia. However, there were no differences in ventilatory responses between PFO+ and PFO– subjects during exposure to either isocapnic or poikilocapnic hypoxia. These findings suggest that PFO+ subjects have a blunted central chemoreflex. This dissertation contains previously, unpublished co-authored material. Close

• 32. [Article] THE EFFECT OF A PATENT FORAMEN OVALE ON THERMOREGULATORY AND VENTILATORY RESPONSES DURING PASSIVE HEATING AND COOLING

  41 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, ...

  Citation × Citation Citation Abstract Copy Title: THE EFFECT OF A PATENT FORAMEN OVALE ON THERMOREGULATORY AND VENTILATORY RESPONSES DURING PASSIVE HEATING AND COOLING Author: Hay, Madeline Year: 2016 41 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Title: THE EFFECT OF A PATENT FORAMEN OVALE ON THERMOREGULATORY AND VENTILATORY RESPONSES DURING PASSIVE HEATING AND COOLING Author: Hay, Madeline Year: 2016 41 pages. A thesis presented to the Department of Human Physiology and the Clark Honors College of the University of Oregon in partial fulfillment of the requirements for degree of Bachelor of Science, Spring 2016. Close

• 33. [Article] Galena Watershed analysis--Supplement 2002

  818 pp. Tables, figures, maps, references, glossary, appendices, illus. "Analysis was performed on 49,4733 acres of the Davis, Placer, Vinegar, Tincup, Little Butte, Butte, Vincent, Little Boulder, Deerhorn ...

  Citation × Citation Citation Abstract Copy Title: Galena Watershed analysis--Supplement 2002 Author: Blue Mountain Ranger District (Or.) Year: 2008, 2003 818 pp. Tables, figures, maps, references, glossary, appendices, illus. "Analysis was performed on 49,4733 acres of the Davis, Placer, Vinegar, Tincup, Little Butte, Butte, Vincent, Little Boulder, Deerhorn and Granite Boulder subwatersheds and the tributaries to the Middle- Fork of the John Day River (Chapters 1-4 this document, see also Map A page 1 and Appendix E, Maps 1-31). The Middle Fork of the John Day River originates south of the North Fork of the John Day River in the Blue Mountains, and flows westerly for approximately 75 miles, then merges with the North Fork about 18 miles above Monument, Oregon. The analysis area is located about 25 air miles northeast of John Day, Oregon." Captured June 11, 2008. Title: Galena Watershed analysis--Supplement 2002 Author: Blue Mountain Ranger District (Or.) Year: 2008, 2003 818 pp. Tables, figures, maps, references, glossary, appendices, illus. "Analysis was performed on 49,4733 acres of the Davis, Placer, Vinegar, Tincup, Little Butte, Butte, Vincent, Little Boulder, Deerhorn and Granite Boulder subwatersheds and the tributaries to the Middle- Fork of the John Day River (Chapters 1-4 this document, see also Map A page 1 and Appendix E, Maps 1-31). The Middle Fork of the John Day River originates south of the North Fork of the John Day River in the Blue Mountains, and flows westerly for approximately 75 miles, then merges with the North Fork about 18 miles above Monument, Oregon. The analysis area is located about 25 air miles northeast of John Day, Oregon." Captured June 11, 2008. Close

• 34. [Article] Swiftwater 2004 instream restoration projects decision record

  3 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14; W.M.) Captured July 24, 2008.

  Citation × Citation Citation Abstract Copy Title: Swiftwater 2004 instream restoration projects decision record Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 3 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14; W.M.) Captured July 24, 2008. Title: Swiftwater 2004 instream restoration projects decision record Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 2004 3 pp. North Fork Big Tom Folley Creek (T21S, R7W, Sections 35 and 26), Big Tom Folley Creek (T22 and 21S, R7W, Sections 2 and 36), and Susan Creek (T26S, R2W, Section 14; W.M.) Captured July 24, 2008. Close

• 35. [Article] Deep Creek watershed restoration environmental assessment

  128 pp. Tables, map, index, glossary, references, appendices. T. 13 S., R. 22 E., Sections 11, 13, 14, 23-26, 35, 36 T. 13 S., R. 23 E., Sections 7-36 T. 13 S., R. 24 E., Sections 18, 19, 29-32 T. 14 S., ...

  Citation × Citation Citation Abstract Copy Title: Deep Creek watershed restoration environmental assessment Author: Paulina Ranger District (Or.) Year: 2008, 2004 128 pp. Tables, map, index, glossary, references, appendices. T. 13 S., R. 22 E., Sections 11, 13, 14, 23-26, 35, 36 T. 13 S., R. 23 E., Sections 7-36 T. 13 S., R. 24 E., Sections 18, 19, 29-32 T. 14 S., R. 22 E., Sections 1, 2, 11-14, 23-27, 35, 36 T. 14 S., R. 23 E., Sections 1-36 T. 14 S., R. 24 E., Sections 5-8, 16-18, 19-21, 28-32 T. 15 S., R. 22 E., Sections 1, 2 T. 15 S., R. 23 E., Sections 5, 6. Captured May 30, 2007. Title: Deep Creek watershed restoration environmental assessment Author: Paulina Ranger District (Or.) Year: 2008, 2004 128 pp. Tables, map, index, glossary, references, appendices. T. 13 S., R. 22 E., Sections 11, 13, 14, 23-26, 35, 36 T. 13 S., R. 23 E., Sections 7-36 T. 13 S., R. 24 E., Sections 18, 19, 29-32 T. 14 S., R. 22 E., Sections 1, 2, 11-14, 23-27, 35, 36 T. 14 S., R. 23 E., Sections 1-36 T. 14 S., R. 24 E., Sections 5-8, 16-18, 19-21, 28-32 T. 15 S., R. 22 E., Sections 1, 2 T. 15 S., R. 23 E., Sections 5, 6. Captured May 30, 2007. Close

• 36. [Article] Swiftwater 2004 instream restoration projects environmental assessment

  17 pp. Tables, maps, appendices, references. North Fork Big Tom Folley: Township 21 South, Range 7 West, Sections 35 and 26; Big Tom Folley Creek: Township 22 and 21 South, Range 7 West, Sections 2 and ...

  Citation × Citation Citation Abstract Copy Title: Swiftwater 2004 instream restoration projects environmental assessment Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 1995 17 pp. Tables, maps, appendices, references. North Fork Big Tom Folley: Township 21 South, Range 7 West, Sections 35 and 26; Big Tom Folley Creek: Township 22 and 21 South, Range 7 West, Sections 2 and 36; Susan Creek: Township 26 South, Range 2 West, Section 14. Captured July 27, 2007. Title: Swiftwater 2004 instream restoration projects environmental assessment Author: United States. Bureau of Land Management. Roseburg District Office Year: 2008, 1995 17 pp. Tables, maps, appendices, references. North Fork Big Tom Folley: Township 21 South, Range 7 West, Sections 35 and 26; Big Tom Folley Creek: Township 22 and 21 South, Range 7 West, Sections 2 and 36; Susan Creek: Township 26 South, Range 2 West, Section 14. Captured July 27, 2007. Close

• 37. [Article] Recent Mafic Eruptions at Newberry Volcano and in the Central Oregon Cascades: Physical Volcanology and Implications for Hazards

  Mafic eruptions have been the dominant form of volcanic activity in central Oregon throughout the Holocene. These eruptions have produced cinder cones, extensive lava flows, and tephra blankets. In most ...

  Citation × Citation Citation Abstract Copy Title: Recent Mafic Eruptions at Newberry Volcano and in the Central Oregon Cascades: Physical Volcanology and Implications for Hazards Author: McKay, Daniele Year: 2012 Mafic eruptions have been the dominant form of volcanic activity in central Oregon throughout the Holocene. These eruptions have produced cinder cones, extensive lava flows, and tephra blankets. In most cases, the extent and volume of the tephra blankets has not been determined, despite the fact that future tephra production would pose considerable hazards to transportation, infrastructure, and public health. The economy of the region, which is largely based in tourism, would also be negatively impacted. For this reason, developing a better understanding of the extent and dynamics of tephra production at recent mafic vents is critical, both in terms of mitigating the hazards associated with future eruptions and in improving our scientific understanding of explosive mafic activity. Here I present detailed field and laboratory studies of tephra from recent mafic vents at Newberry Volcano and in the central Oregon High Cascades. Studies of Newberry vents show that eruption style is strongly correlated with eruptive volume, that extensive magma storage and assimilation occurred prior to the eruption of these vents, and that minimum pre-magmatic water content as recorded by plagioclase was 2.5 wt.%. Detailed mapping and physical studies of tephra deposits from High Cascades vents show that several recent eruptions produced extensive tephra deposits. These deposits are physically similar to well-documented historic eruptions that have been characterized as violent strombolian. At least one Cascade cinder cone (Sand Mountain) produced a tephra deposit that is unusually large in volume and characterized by uniformly fine-grained clasts, which is interpreted as evidence for syn-eruptive interaction with external water. Microtextural characteristics of tephra, along with an evaluation of possible water sources, support this interpretation. These investigations demonstrate that magma storage and eruption style at mafic vents is both variable and complex. Additionally, these studies show that cinder cones in central Oregon have the potential to erupt much more explosively than previously assumed. The results of this study will be an important tool for developing comprehensive regional hazard assessments. This dissertation includes previously published and unpublished co-authored material. Title: Recent Mafic Eruptions at Newberry Volcano and in the Central Oregon Cascades: Physical Volcanology and Implications for Hazards Author: McKay, Daniele Year: 2012 Mafic eruptions have been the dominant form of volcanic activity in central Oregon throughout the Holocene. These eruptions have produced cinder cones, extensive lava flows, and tephra blankets. In most cases, the extent and volume of the tephra blankets has not been determined, despite the fact that future tephra production would pose considerable hazards to transportation, infrastructure, and public health. The economy of the region, which is largely based in tourism, would also be negatively impacted. For this reason, developing a better understanding of the extent and dynamics of tephra production at recent mafic vents is critical, both in terms of mitigating the hazards associated with future eruptions and in improving our scientific understanding of explosive mafic activity. Here I present detailed field and laboratory studies of tephra from recent mafic vents at Newberry Volcano and in the central Oregon High Cascades. Studies of Newberry vents show that eruption style is strongly correlated with eruptive volume, that extensive magma storage and assimilation occurred prior to the eruption of these vents, and that minimum pre-magmatic water content as recorded by plagioclase was 2.5 wt.%. Detailed mapping and physical studies of tephra deposits from High Cascades vents show that several recent eruptions produced extensive tephra deposits. These deposits are physically similar to well-documented historic eruptions that have been characterized as violent strombolian. At least one Cascade cinder cone (Sand Mountain) produced a tephra deposit that is unusually large in volume and characterized by uniformly fine-grained clasts, which is interpreted as evidence for syn-eruptive interaction with external water. Microtextural characteristics of tephra, along with an evaluation of possible water sources, support this interpretation. These investigations demonstrate that magma storage and eruption style at mafic vents is both variable and complex. Additionally, these studies show that cinder cones in central Oregon have the potential to erupt much more explosively than previously assumed. The results of this study will be an important tool for developing comprehensive regional hazard assessments. This dissertation includes previously published and unpublished co-authored material. Close

• 38. [Article] Chronic passive heat therapy as a novel means of improving vascular function in sedentary humans

  Cardiovascular disease is the leading cause of death in the developed world. The majority of cardiovascular diseases are characterized by disorders of the arteries, predominantly caused by endothelial ...

  Citation × Citation Citation Abstract Copy Title: Chronic passive heat therapy as a novel means of improving vascular function in sedentary humans Author: Brunt, Vienna Year: 2016 Cardiovascular disease is the leading cause of death in the developed world. The majority of cardiovascular diseases are characterized by disorders of the arteries, predominantly caused by endothelial dysfunction and arterial stiffening. Passive heat stress results in elevations in core temperature (inducing heat shock protein expression) and changes in cardiovascular hemodynamics, such as increased cardiac output and shear stress, that are similar to exercise. Thus, repeated passive heat stress (“heat therapy”) may provide an alternative means of improving cardiovascular health, particularly for patients with limited exercise tolerance and/or capabilities. Therefore, the goal of this dissertation was to perform integrative studies to determine the effects of heat therapy on vascular function and the associated cellular pathways in young, sedentary humans. Twenty subjects were assigned to participate in 8 weeks (4-5x/week) of heat therapy (N=10; immersion in a 40.5°C bath sufficient to maintain rectal temperature ≥38.5°C for 60 min/session) or thermoneutral water immersion (N=10; sham). As discussed in Chapter V, we found that heat therapy improved numerous well-established biomarkers of conduit vessel/macrovascular function, including flow-mediated dilation (a measure of endothelial function), arterial stiffness, intima media thickness, and blood pressure. Heat therapy also improved microvascular function, as discussed in Chapter VI, measured as improved cutaneous thermal hyperemia and nitric oxide-dependent dilation (the difference between microdialysis sites receiving Lactated Ringer’s [control] and nitric oxide synthase inhibition). No changes were observed in any variables in sham subjects. In Chapter VII, we showed that both direct cellular heating and serum collected from human subjects following heat therapy improved nitric oxide bioavailability and angiogenesis in cultured endothelial cells, providing potential mechanisms by which heat therapy improves vascular function in vivo. Therefore, the studies described herein provide comprehensive evidence that passive heat therapy improves vascular health and insight into the mechanisms involved. Our data presented in Chapters IV-VII, combined with pilot data we conducted in spinal cord injured individuals (Chapter VIII), strongly indicate that passive heat therapy could be used as a simple and effective tool to improve cardiovascular health in a variety of patient populations. This dissertation includes published and unpublished co-authored material. Title: Chronic passive heat therapy as a novel means of improving vascular function in sedentary humans Author: Brunt, Vienna Year: 2016 Cardiovascular disease is the leading cause of death in the developed world. The majority of cardiovascular diseases are characterized by disorders of the arteries, predominantly caused by endothelial dysfunction and arterial stiffening. Passive heat stress results in elevations in core temperature (inducing heat shock protein expression) and changes in cardiovascular hemodynamics, such as increased cardiac output and shear stress, that are similar to exercise. Thus, repeated passive heat stress (“heat therapy”) may provide an alternative means of improving cardiovascular health, particularly for patients with limited exercise tolerance and/or capabilities. Therefore, the goal of this dissertation was to perform integrative studies to determine the effects of heat therapy on vascular function and the associated cellular pathways in young, sedentary humans. Twenty subjects were assigned to participate in 8 weeks (4-5x/week) of heat therapy (N=10; immersion in a 40.5°C bath sufficient to maintain rectal temperature ≥38.5°C for 60 min/session) or thermoneutral water immersion (N=10; sham). As discussed in Chapter V, we found that heat therapy improved numerous well-established biomarkers of conduit vessel/macrovascular function, including flow-mediated dilation (a measure of endothelial function), arterial stiffness, intima media thickness, and blood pressure. Heat therapy also improved microvascular function, as discussed in Chapter VI, measured as improved cutaneous thermal hyperemia and nitric oxide-dependent dilation (the difference between microdialysis sites receiving Lactated Ringer’s [control] and nitric oxide synthase inhibition). No changes were observed in any variables in sham subjects. In Chapter VII, we showed that both direct cellular heating and serum collected from human subjects following heat therapy improved nitric oxide bioavailability and angiogenesis in cultured endothelial cells, providing potential mechanisms by which heat therapy improves vascular function in vivo. Therefore, the studies described herein provide comprehensive evidence that passive heat therapy improves vascular health and insight into the mechanisms involved. Our data presented in Chapters IV-VII, combined with pilot data we conducted in spinal cord injured individuals (Chapter VIII), strongly indicate that passive heat therapy could be used as a simple and effective tool to improve cardiovascular health in a variety of patient populations. This dissertation includes published and unpublished co-authored material. Close

• 39. [Article] NITRIC OXIDE SIGNALLING PATHWAYS FOLLOWING CHRONIC PASSIVE HEAT THERAPY

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• 40. [Article] Remote measurement of gravel-bed river depths and analysis of the geomorphic response of rivers to canals and small dams

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