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Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range
Portland State University PDXScholar Environmental Science and Management Faculty Publications and Presentations Environmental Science and Management 3-2016 Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range Megan K. Creutzburg Portland State University, [email protected] Robert M. Scheller Portland State University, [email protected] Melissa S. Lucash Portland State University, [email protected] Louisa B. Evers Bureau of Land Management Stephen D. LeDuc United States Environmental Protection Agency See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/esm_fac Part of the Forest Biology Commons Let us know how access to this document benefits ou.y Citation Details Creutzburg, M. K., Scheller, R. M., Lucash, M. S., Evers, L. B., LeDuc, S. D., & Johnson, M. G. (2015). Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range. GCB Bioenergy. This Article is brought to you for free and open access. It has been accepted for inclusion in Environmental Science and Management Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Megan K. Creutzburg, Robert M. Scheller, Melissa S. Lucash, Louisa B. Evers, Stephen D. LeDuc, and Mark G. Johnson This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/esm_fac/118 GCB Bioenergy (2016) 8, 357–370, doi: 10.1111/gcbb.12255 Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range MEGAN K. CREUTZBURG1 , ROBERT M. SCHELLER1 , MELISSA S. LUCASH1 , LOUISA B. EVERS2 , STEPHEN D. LEDUC3 and MARK G. -
Geological and Seismic Evidence for the Tectonic Evolution of the NE Oman Continental Margin and Gulf of Oman GEOSPHERE, V
Research Paper GEOSPHERE Geological and seismic evidence for the tectonic evolution of the NE Oman continental margin and Gulf of Oman GEOSPHERE, v. 17, no. X Bruce Levell1, Michael Searle1, Adrian White1,*, Lauren Kedar1,†, Henk Droste1, and Mia Van Steenwinkel2 1Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK https://doi.org/10.1130/GES02376.1 2Locquetstraat 11, Hombeek, 2811, Belgium 15 figures ABSTRACT Arabian shelf or platform (Glennie et al., 1973, 1974; Searle, 2007). Restoration CORRESPONDENCE: [email protected] of the thrust sheets records several hundred kilometers of shortening in the Late Cretaceous obduction of the Semail ophiolite and underlying thrust Neo-Tethyan continental margin to slope (Sumeini complex), basin (Hawasina CITATION: Levell, B., Searle, M., White, A., Kedar, L., Droste, H., and Van Steenwinkel, M., 2021, Geological sheets of Neo-Tethyan oceanic sediments onto the submerged continental complex), and trench (Haybi complex) facies rocks during ophiolite emplace- and seismic evidence for the tectonic evolution of the margin of Oman involved thin-skinned SW-vergent thrusting above a thick ment (Searle, 1985, 2007; Cooper, 1988; Searle et al., 2004). The present-day NE Oman continental margin and Gulf of Oman: Geo- Guadalupian–Cenomanian shelf-carbonate sequence. A flexural foreland basin southwestward extent of the ophiolite and Hawasina complex thrust sheets is sphere, v. 17, no. X, p. 1– 22, https:// doi .org /10.1130 /GES02376.1. (Muti and Aruma Basin) developed due to the thrust loading. Newly available at least 150 km across the Arabian continental margin. The obduction, which seismic reflection data, tied to wells in the Gulf of Oman, suggest indirectly spanned the Cenomanian to Early Maastrichtian (ca 95–72 Ma; Searle et al., Science Editor: David E. -
The Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-Huei Chen Jane Kertis Pete Teensma
Forests of the Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-huei Chen Jane Kertis Pete Teensma The Oregon Coast Range supports some of the most dense Ocean, so they are warm and often highly productive, com- and productive forests in North America. In the pre-harvest- pared to the Cascade Range and central Oregon forests. ing period these forests arose as a result of large fires-the Isaac's (1949) site index map shows much more site class I largest covering 330,000 ha (Teensma and others 1991). and I1 land in the Coast Range than in the Cascades. In the These fires occurred mostly at intervals of 150 to 300 years. summers, humid maritime air creates a moisture gradient The natural disturbance regime supported a diverse fauna from the coastal western hemlock-Sitka spruce (Tsuga and large populations of anadromous salmonids (salmon heterophylla-Piceasitchensis) zone with periodic fog extend- and related fish). In contrast, the present disturbance re- ing 4 to 10 km inland, through Douglas-fir (Pseudotsuga gime is dominated by patch clearcuts of about 10-30 ha menziesii var. rnenziesii)-western hemlock forests in the superimposed on most of the forest land with agriculture on central zone to the drier interior-valley foothill zone of the flats near rivers. Ages of most managed forests are less Douglas-fir, bigleaf maple (Acer rnacrophyllum)and Oregon than 60 years. This logging has coincided with significant oak (Quercus garryana). declines in suitable habitat and populations of some fish and wildlife species. Some of these species have been nearly extirpated. -
Glacial Tectonics: a Deeper Perspective Robert M
Quaternary Science Reviews 19 (2000) 1391}1398 Glacial tectonics: a deeper perspective Robert M. Thorson* Department of Geology and Geophysics, University of Connecticut, 345 Mansxeld Road (U-45), Storrs, CT 06269, USA Abstract The upper 5}10 km of the lithosphere is sensitive to slight changes ((0.1 MPa) in local stress caused by di!erential loading, #uid #ow, the mechanical transfer of strain between faults, and viscoelastic relaxation in the aesthenosphere. Lithospheric stresses induced by mass and #uid transfers associated with Quaternary ice sheets a!ected the tectonic regimes of stable cratons and active plate margins. In the latter case, it is di$cult to di!erentiate glacially induced fault displacements from nonglacial ones, particularly if residual glacial stresses are considered. Glaciotectonics, a sub-subdiscipline within Quaternary geology is historically focussed on reconstructing past glacier regimes and, by de"nition, does not include these e!ects. The term `glacial tectonicsa is hereby suggested for investigations focussed on the past and continuing in#uences of ice sheets on contemporary tectonics. ( 2000 Elsevier Science Ltd. All rights reserved. 1. Introduction e!ects of glacial mass transfers is blurring the distinction between the study of tectonics, per se, and the study of Presently, there is a conceptual shift in the geosciences `glaciotectonicsa, which, historically, has been primarily away from increasing specialization, towards more inte- concerned with deformed glacial deposits. grative problems at global scales, a shift embodied by the In this paper I show how the physical coupling be- phrase `Earth System Sciencea (Kump et al., 1999). Si- tween glaciation and crustal deformation extends far multaneously, technologically driven advances in instru- beyond the decollement between ice and its substrate (i.e. -
Mill Creek Watershed Assessment
Yamhill Basin Council Mill Watershed Assessment December 30, 1999 Funding for the Mill Assessment was provided by the Oregon Watershed Enhancement Board and Resource Assistance for Rural Environments. Mill Assessment Project Manager: Robert J. Bower, Principal Author Co-authors: Chris Lupoli, Linfield College intern, for Riparian section and assisted with Wetlands Conditions section. Tamara Quandt, Linfield College intern, for Sensitive Species section. Editors: Melissa Leoni, Yamhill Basin Council, McMinnville, OR Alison Bower, Forest Ecologist, Corvallis, OR Contributors: Bill Ferber, Salem, Water Resources Department (WRD) Chester Novak, Salem, Bureau Land Management (BLM) Dan Upton, Dallas, Willamette Industries David Anderson, Monmouth, Boise Cascade Dean Anderson, Dallas, Polk County Geographical Information Systems (GIS) Dennis Ades, Salem, Department of Environmental Quality (DEQ) Gary Galovich, Corvallis, Oregon Department Fish and Wildlife (ODFW) Mark Koski, Salem, Bureau of Land Management (BLM) Patrick Hawe, Salem, Bureau of Land Management (BLM) Rob Tracey, McMinnville, Natural Resource and Conservation Service (NRCS) Stan Christensen, McMinnville, Yamhill Soil Water Conservation District Susan Maleki, Corvallis, Oregon Watershed Enhancement Board (OWEB) Warren Tausch, Tillamook Bureau of Land Management (BLM) Special Thanks: ! John Cruickshank, Gooseneck Creek resident for his assistance with the Historical, and Channel Modification sections and in the gathering of historical photographs. ! Gooseneck Creek Watershed Group for their support and guidance. ! John Caputo, Yamhill County GIS. ! BLM and Polk County GIS for providing some of the GIS base layers used to create the maps in this assessment. ! USDA Service Center, Natural Resource Conservation Service, McMinnville, for copying and office support. ! Polk and Yamhill Soil and Water Conservation Districts. ! Nick Varnum, PNG Environmental Inc., Tigard, for assisting with the Hydrology and Channel Habitat Typing sections. -
Outline of Angiosperm Phylogeny
Outline of angiosperm phylogeny: orders, families, and representative genera with emphasis on Oregon native plants Priscilla Spears December 2013 The following listing gives an introduction to the phylogenetic classification of the flowering plants that has emerged in recent decades, and which is based on nucleic acid sequences as well as morphological and developmental data. This listing emphasizes temperate families of the Northern Hemisphere and is meant as an overview with examples of Oregon native plants. It includes many exotic genera that are grown in Oregon as ornamentals plus other plants of interest worldwide. The genera that are Oregon natives are printed in a blue font. Genera that are exotics are shown in black, however genera in blue may also contain non-native species. Names separated by a slash are alternatives or else the nomenclature is in flux. When several genera have the same common name, the names are separated by commas. The order of the family names is from the linear listing of families in the APG III report. For further information, see the references on the last page. Basal Angiosperms (ANITA grade) Amborellales Amborellaceae, sole family, the earliest branch of flowering plants, a shrub native to New Caledonia – Amborella Nymphaeales Hydatellaceae – aquatics from Australasia, previously classified as a grass Cabombaceae (water shield – Brasenia, fanwort – Cabomba) Nymphaeaceae (water lilies – Nymphaea; pond lilies – Nuphar) Austrobaileyales Schisandraceae (wild sarsaparilla, star vine – Schisandra; Japanese -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
A Prototype System for Multilingual Data Discovery of International Long-Term Ecological Research (ILTER) Network Data
Ecological Informatics 40 (2017) 93–101 Contents lists available at ScienceDirect Ecological Informatics journal homepage: www.elsevier.com/locate/ecolinf A prototype system for multilingual data discovery of International Long-Term Ecological Research (ILTER) Network data Kristin Vanderbilt a,⁎,JohnH.Porterb, Sheng-Shan Lu c,NicBertrandd,DavidBlankmane, Xuebing Guo f, Honglin He f, Don Henshaw g, Karpjoo Jeong h, Eun-Shik Kim i,Chau-ChinLinc,MargaretO'Brienj, Takeshi Osawa k, Éamonn Ó Tuama l, Wen Su f, Haibo Yang m a Department of Biology, MSC03 2020, University of New Mexico, Albuquerque, NM 87131, USA b Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA c Taiwan Forestry Research Institute, 53 Nan Hai Rd., Taipei, Taiwan d Centre for Ecology & Hydrology, Lancaster Environmental Centre, Lancaster LA1 4AP, UK e Jerusalem 93554, Israel f Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China g U.S. Forest Service Pacific Northwest Research Station, Forestry Sciences Laboratory, 3200 SW Jefferson Way, Corvallis, OR 97331, USA h Department of Internet and Multimedia Engineering, Konkuk University, Seoul 05029, Republic of Korea i Kookmin University, Department of Forestry, Environment, and Systems, Seoul 02707, Republic of Korea j Marine Science Institute, University of California, Santa Barbara, CA 93106, USA k National Institute for Agro-Environmental Sciences, Tsukuba, Ibaraki 305-8604, Japan l GBIF Secretariat, Universitetsparken 15, DK-2100 Copenhagen Ø, Denmark m School of Ecological and Environmental Sciences, East China Normal University, 500 Dongchuan Rd., Shanghai 200241, China article info abstract Article history: Shared ecological data have the potential to revolutionize ecological research just as shared genetic sequence Received 6 September 2016 data have done for biological research. -
Selecting Target Datasets for Semantic Enrichment
Task Force on Enrichment and Evaluation 29/10/2015 Selecting target datasets for semantic enrichment Editors Antoine Isaac, Hugo Manguinhas, Valentine Charles (Europeana Foundation R&D) and Juliane Stiller (Max Planck Institute for the History of Science) 1. INTRODUCTION 2 2. METHODS FOR ANALYZING AND SELECTING DATASETS FOR SEMANTIC ENRICHMENT 2 2.1. Analyse your source data 3 2.2. Identify your requirements 4 2.3. Find your targets 5 2.4. Select your targets 6 2.4.1. Availability 6 2.4.2. Access 6 2.4.3. Granularity and Coverage 6 2.4.4. Quality 9 2.4.5. Connectivity 10 2.4.6. Size 10 2.5. Test the selected target 14 3. BUILDING A NEW TARGET FOR ENRICHMENT 14 3.1. Refining existing targets to build a new target 14 3.1.1. Building a classification for Europeana Food and Drink 15 3.1.2. Building a vocabulary for First World War in Europeana 1914-1918 15 3.2. Building a new target from scratch 15 REFERENCES 16 1/17 Task Force on Evaluation and Enrichment – Selecting target datasets for semantic enrichment 1. Introduction As explained in the main report one of the components of the enrichment process is the target vocabulary. The selection of the target against which the enrichment will be performed, being a dataset of cultural objects or a specific knowledge organization system, needs to be carefully done. In many cases the selection of the appropriate target for the source data will determine the quality of the enrichments. The Task Force recommends users to re-use existing targets when performing enrichments as it increases interoperability between datasets and reduces redundancies between the different targets1. -
Mountain Ranges in India for Banking & SSC Exam
Mountain Ranges in India for Banking & SSC Exam - GK Notes in PDF Every year 11th December is observed as the 'International Mountain Day.' A theme is set for this day to mark a purpose and to create awareness. This year's theme is “#MountainsMatter.” It will highlight the importance of mountains and their need for youth, water, disaster risk reduction, food, indigenous peoples and biodiversity. Mountains play a pivotal role in our life by altering the weather pattern and climatic conditions. They are also rich in endemic species and has great impact on Natural Ecosystem of the country. Thus, the knowledge of Mountain Ranges is very important from the point of view of various Banking, SSC and other Government Exams. To help you prepare this topic, here's the account of the major Mountain Ranges in India. A Mountain Range is a sequential chain or series of mountains or hills with similarity in form, structure and alignment that have arisen from the same cause, usually an orogeny. List of the prominent Mountain Ranges in India ⇒ The Himalaya Range • Himalaya is the highest mountain ranges in India • The word Himalaya literally translates to "abode of snow" from Sanskrit. • The Himalayan Mountain range is the youngest mountain range of India and new fold mountain is formed by the collision of two tectonic plates. • Himalayan Mountain Range has almost every highest peak of the world. • On an average they have more than 100 peaks with height more than 7200 m. 1 | P a g e • Nanga Parbat and Namcha Barwa are considered as the western and eastern points of the Himalaya. -
Species at Risk Assessment—Pacific Rim National Park Reserve Of
Species at Risk Assessment—Pacific Rim National Park Reserve of Canada Prepared for Parks Canada Agency by Conan Webb 3rd May 2005 2 Contents 0.1 Acknowledgments . 10 1 Introduction 11 1.1 Background Information . 11 1.2 Objective . 16 1.3 Methods . 17 2 Species Reports 20 2.1 Sample Species Report . 21 2.2 Amhibia (Amphibians) . 23 2.2.1 Bufo boreas (Western toad) . 23 2.2.2 Rana aurora (Red-legged frog) . 29 2.3 Aves (Birds) . 37 2.3.1 Accipiter gentilis laingi (Queen Charlotte goshawk) . 37 2.3.2 Ardea herodias fannini (Pacific Great Blue heron) . 43 2.3.3 Asio flammeus (Short-eared owl) . 49 2.3.4 Brachyramphus marmoratus (Marbled murrelet) . 51 2.3.5 Columba fasciata (Band-tailed pigeon) . 59 2.3.6 Falco peregrinus (Peregrine falcon) . 61 2.3.7 Fratercula cirrhata (Tufted puffin) . 65 2.3.8 Glaucidium gnoma swarthi (Northern pygmy-owl, swarthi subspecies ) . 67 2.3.9 Megascops kennicottii kennicottii (Western screech-owl, kennicottii subspecies) . 69 2.3.10 Phalacrocorax penicillatus (Brandt’s cormorant) . 73 2.3.11 Ptychoramphus aleuticus (Cassin’s auklet) . 77 2.3.12 Synthliboramphus antiquus (Ancient murrelet) . 79 2.3.13 Uria aalge (Common murre) . 83 2.4 Bivalvia (Oysters; clams; scallops; mussels) . 87 2.4.1 Ostrea conchaphila (Olympia oyster) . 87 2.5 Gastropoda (Snails; slugs) . 91 2.5.1 Haliotis kamtschatkana (Northern abalone) . 91 2.5.2 Hemphillia dromedarius (Dromedary jumping-slug) . 95 2.6 Mammalia (Mammals) . 99 2.6.1 Cervus elaphus roosevelti (Roosevelt elk) . 99 2.6.2 Enhydra lutris (Sea otter) . -
Advanced Mechanics of Materials
ADVANCED MECHANICS OF MATERIALS By Dr. Sittichai Seangatith SCHOOL OF CIVIL ENGINEERING INSTITUTE OF ENGINEERING SURANAREE UNIVERSITY OF TECHNOLOGY May 2001 SURANAREE UNIVERSITY OF TECHNOLOGY INSTITUTE OF ENGINEERING SCHOOL OF CIVIL ENGINEERING 410 611 ADVANCED MECHANICS OF MATERIALS 1st Trimester /2002 Instructor: Dr. Sittichai Seangatith ([email protected]) Prerequisite: 410 212 Mechanics of Materials II or consent of instructor Objectives: Students successfully completing this course will 1. understand the concept of fundamental theories of the advanced mechanics of material; 2. be able to simplify a complex mechanic problem down to one that can be analyzed; 3. understand the significance of the solution to the problem of any assumptions made. Textbooks: 1. Advanced Mechanics of Materials; 4th Edition, A.P. Boresi and O.M. Sidebottom, John Wiley & Sons, 1985 2. Advanced Mechanics of Materials; 2nd Edition, R.D. Cook and W.C. Young, Prentice Hall, 1999 3. Theory of Elastic Stability; 2nd Edition, S.P. Timoshenko and J.M. Gere, McGraw-Hill, 1963 4. Theory of Elasticity; 3rd Edition, S.P. Timoshenko and J.N. Goodier, McGraw- Hill, 1970 5. Theory of Plates and Shells; 2nd Edition, S.P. Timoshenko and S. Woinowsky- Krieger, McGraw-Hill, 1970 6. Mechanical Behavior of Materials; 2nd Edition, N.E. Dowling, Prentice Hall, 1999 7. Mechanics of Materials; 3th Edition, R.C. Hibbeler, Prentice Hall, 1997 Course Contents: Chapters Topics 1 Theories of Stress and Strain 2 Stress-Strain Relations 3 Elements of Theory of Elasticity 4 Applications of Energy Methods 5 Static Failure and Failure Criteria 6 Fatigue 7 Introduction to Fracture Mechanics 8 Beams on Elastic Foundation 9 Plate Bending 10 Buckling and Instability Conduct of Course: Homework, Quizzes, and Projects 30% Midterm Examination 35% Final Examination 35% Grading Guides: 90 and above A 85-89 B+ 80-84 B 75-79 C+ 70-74 C 65-69 D+ 60-64 D below 60 F The above criteria may be changed at the instructor’s discretion.