Fpn63 Northern Cedar Swamp Factsheet
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Peat and Peatland Resources of Southeastern Ontario
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Northern Fen Communitynorthern Abstract Fen, Page 1
Northern Fen CommunityNorthern Abstract Fen, Page 1 Community Range Prevalent or likely prevalent Infrequent or likely infrequent Absent or likely absent Photo by Joshua G. Cohen Overview: Northern fen is a sedge- and rush-dominated 8,000 years. Expansion of peatlands likely occurred wetland occurring on neutral to moderately alkaline following climatic cooling, approximately 5,000 years saturated peat and/or marl influenced by groundwater ago (Heinselman 1970, Boelter and Verry 1977, Riley rich in calcium and magnesium carbonates. The 1989). community occurs north of the climatic tension zone and is found primarily where calcareous bedrock Several other natural peatland communities also underlies a thin mantle of glacial drift on flat areas or occur in Michigan and can be distinguished from shallow depressions of glacial outwash and glacial minerotrophic (nutrient-rich) northern fens, based on lakeplains and also in kettle depressions on pitted comparisons of nutrient levels, flora, canopy closure, outwash and moraines. distribution, landscape context, and groundwater influence (Kost et al. 2007). Northern fen is dominated Global and State Rank: G3G5/S3 by sedges, rushes, and grasses (Mitsch and Gosselink 2000). Additional open wetlands occurring on organic Range: Northern fen is a peatland type of glaciated soils include coastal fen, poor fen, prairie fen, bog, landscapes of the northern Great Lakes region, ranging intermittent wetland, and northern wet meadow. Bogs, from Michigan west to Minnesota and northward peat-covered wetlands raised above the surrounding into central Canada (Ontario, Manitoba, and Quebec) groundwater by an accumulation of peat, receive inputs (Gignac et al. 2000, Faber-Langendoen 2001, Amon of nutrients and water primarily from precipitation et al. -
Field Indicators of Hydric Soils
United States Department of Field Indicators of Agriculture Natural Resources Hydric Soils in the Conservation Service United States In cooperation with A Guide for Identifying and Delineating the National Technical Committee for Hydric Soils Hydric Soils, Version 8.2, 2018 Field Indicators of Hydric Soils in the United States A Guide for Identifying and Delineating Hydric Soils Version 8.2, 2018 (Including revisions to versions 8.0 and 8.1) United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with the National Technical Committee for Hydric Soils Edited by L.M. Vasilas, Soil Scientist, NRCS, Washington, DC; G.W. Hurt, Soil Scientist, University of Florida, Gainesville, FL; and J.F. Berkowitz, Soil Scientist, USACE, Vicksburg, MS ii In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. -
Post-Fire Variability in Siberian Alder in Interior Alaska: Distribution Patterns, Nitrogen Fixation Rates, and Ecosystem Consequences
Post-fire variability in Siberian alder in Interior Alaska: distribution patterns, nitrogen fixation rates, and ecosystem consequences Item Type Thesis Authors Houseman, Brian Richard Download date 24/09/2021 00:34:34 Link to Item http://hdl.handle.net/11122/8128 POST-FIRE VARIABILITY IN SIBERIAN ALDER IN INTERIOR ALASKA: DISTRIBUTION PATTERNS, NITROGEN FIXATION RATES, AND ECOSYSTEM CONSEQUENCES By Brian Richard Houseman, B.A. A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Biological Sciences University of Alaska Fairbanks December 2017 APPROVED: Dr. Roger Ruess, Committee Chair Dr. Teresa Hollingsworth, Committee Co-Chair Dr. Dave Verbyla, Committee Member Dr. Kris Hundertmark, Chair Department of Biology and Wildlife Dr. Paul Layer, Dean College of Natural Science and Mathematics Dr. Michael Castellini, Dean of the Graduate School i ProQuest Number:10642427 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. ProQuest 10642427 Published by ProQuest LLC ( 2017). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, MI 48106 - 1346 ABSTRACT The circumpolar boreal forest is responsible for a considerable proportion of global carbon sequestration and is an ecosystem with limited nitrogen (N) pools. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Compressibility Behavior of Tropical Peat Reinforced with Cement Columns
American Journal of Applied Sciences 4 (10): 786-791, 2007 ISSN 1546-9239 © 2007 Science Publications Compressibility Behavior of Tropical Peat Reinforced with Cement Columns 1Youventharan Duraisamy, 2Bujang B.K. Huat and 2Azlan A. Aziz 1University Malaysia Pahang, Malaysia 2University Putra Malaysia, Serdang, Selangor, Malaysia Abstract : This paper presents the compressibility of tropical peat reinforced with cylin- drical cement columns. When a cement column is installed vertically in peat, its compres- sibility is reduced because of the hardened skeleton matrix formed by cement particles bonding with adjacent soil particles in the presence of pore water. The effects of the ce- ment column diameter on the compressibility have been investigated in this study. The results indicated that compressibility index Cc and Cα decreased with increasing diameter of the cement column. Specimens with 45 mm (area ratio = 0.09) diameter and 60 mm (area ratio = 0.16) diameter of single cement column were cured for 7, 14 and 28 days, after which they were subjected to Rowe Cell Consolidation test. Results are also pre- sented from test conducted on groups of cement columns using four (area ratio = 0.04) and nine (area ratio = 0.09) columns of 15 mm diameter each to investigate the influence of number of cement columns on compressibility of peat soil. Based on the results ob- tained, it shows that cement columns can successfully reduce the compressibility of tropi- cal peat. Keywords: Cement columns, deep soil mixing, organic soil, peat soil, Rowe Cell consol- idation. INTRODUCTION Experimental Design and Laboratory Work: The main objective of this research is to find out the effect of Peat represents the extreme form of soft soil. -
2009) Summary Report: Tanacross Shaded Fuelbreak AA39, 9/29/09
2009 SUMMARY REPORT R.R. Jandt 9/29/09 Tanacross Shaded Fuel Break AA39 Fuel Reduction Project Local residents, working with the village council and Alaska Fire Service, received federal funding to reduce the fire risk and hazard to private residential structures by modifying fuel structure and continuity of 66 acres around the community of Tanacross. Treatment was intended to produce a more open stand to slow the rate of spread and intensity of an accidental fire. At the same time, residents wanted to minimize the visual and ecological impact of the shaded fuel break by using hand Figure 1. Hand crew thinning spruce stand and removing crews to treat the area instead of ladder fuels around Tanacross. heavy equipment (Fig. 1). Vegetation Cover Three permanent transects, measuring 30m x 3m, were established in 2001 to monitor changes in understory vegetation cover. Though vegetation composition differed slightly between transects, pre-treatment (2001) understory cover was dominated by heath shrub, such as low-bush cranberry (Vaccinium vitis-idaea) and live feather moss with some tall willows (Salix bebbiana, primarily). Other common species pre-treatment included crowberry (Empetrum nigrum), twinflower (Linnaea borealis), and bastard toadflax (Geocaulon lividum). White spruce (Picea glauca) was the dominant overstory tree. Transects were monitored from 2002-2004 and in 2009 to assess changes in cover type. The most notable change was loss of viability of the feather moss cover on the forest floor in the first two summers following the treatment (Fig. 2, 3). Live moss was almost 50% of the substrate (ground cover) in 2001, whereas by 2003 less than 5% was recorded as live and 22% of the substrate cover was dead feather moss. -
Ecological Site XA232X02Y210 Boreal Forest Loamy Frozen Plains Warm
Natural Resources Conservation Service Ecological site XA232X02Y210 Boreal Forest Loamy Frozen Plains Warm Last updated: 5/18/2020 Accessed: 09/26/2021 General information Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site. MLRA notes Major Land Resource Area (MLRA): 232X–Yukon Flats Lowlands The Yukon Flats Lowlands MLRA is an expansive basin characterized by numerous levels of flood plains and terraces that are separated by minimal breaks in elevation. This MLRA is in Interior Alaska and is adjacent to the middle reaches of the Yukon River. Numerous tributaries of the Yukon River are within the Yukon Flats Lowlands MLRA. The largest are Beaver Creek, Birch Creek, Black River, Chandalar River, Christian River, Dall River, Hadweenzic River, Hodzana River, Porcupine River, and Sheenjek River. The MLRA has two distinct regions— lowlands and marginal uplands. The lowlands have minimal local relief and are approximately 9,000 square miles in size (Williams 1962). Landforms associated with the lowlands are flood plains and stream terraces. The marginal uplands consist of rolling and dissected plains that are a transitional area between the lowlands and adjacent mountain systems. The marginal uplands are approximately 4,700 square miles in size (Williams 1962). This MLRA is bounded by the Yukon-Tanana Plateau to the south, Hodzana Highlands to the west, Porcupine Plateau to the east, and southern foothills of the Brooks Range to the north (Williams 1962). These surrounding hills and mountains partially isolate the Yukon Flats Lowlands MLRA from weather systems affecting other MLRAs of Interior Alaska. -
Calcareous Fens in Southeast Alaska
United States Department of Agriculture Calcareous Fens in Southeast Forest Service Pacifi c Northwest Alaska Research Station 1 Research Note Michael H. McClellan, Terry Brock, and James F. Baichtal PNW-RN-536 February 2003 Abstract Calcareous fens have not been identifi ed previously in southeast Alaska. A limited survey in southeast Alaska identifi ed several wetlands that appear to be calcare- ous fens. These sites were located in low-elevation discharge zones that are below recharge zones in carbonate highlands and talus foot-slopes. Two of six surveyed sites partly met the Minnesota Department of Natural Resources water chemistry criteria for calcareous fens, with pH values of 6.7 to 7.4 and calcium concentrations of 41.8 to 51.4 mg/L but fall short with regard to specifi c conductivity (315 to 380 μS/cm). Alkalinity was not determined. The vegetation was predominately herbaceous, with abundant Sitka sedge (Carex aquatilis) and scattered shrubs such as Barclay’s willow (Salix barclayi) and redosier dogwood (Cornus sericea ssp. sericea). The taxa found in these fens have been reported at other sites in southeast Alaska, although many were at the southern limits of their known ranges. The soils were Histosols composed of 0.6 to greater than 1 m of sedge peat. We found no evidence of calcium carbonate precipitates (marl or tufa) in the soil. Keywords: Alaska (southeast), fens, calcareous fens, wetlands, peatlands, karst. Introduction Calcareous fens, a subtype of extremely rich fen, are important because of their rarity, their distinctive water chemistry, and because they frequently harbor rare or endangered plants (Calcareous Fen Technical Committee 1994). -
The Use of Subsidence to Estimate Carbon Loss from Deforested and Drained Tropical Peatlands in Indonesia
Review The Use of Subsidence to Estimate Carbon Loss from Deforested and Drained Tropical Peatlands in Indonesia Gusti Z. Anshari 1,2 , Evi Gusmayanti 1,3 and Nisa Novita 4,* 1 Magister of Environmental Science, Universitas Tanjungpura, Pontianak 78124, Indonesia; [email protected] (G.Z.A.); [email protected] (E.G.) 2 Soil Science Department, Universitas Tanjungpura, Pontianak 78124, Indonesia 3 Agrotechnology Department, Universitas Tanjungpura, Pontianak 78124, Indonesia 4 Yayasan Konservasi Alam Nusantara, DKI Jakarta 12160, Indonesia * Correspondence: [email protected] Abstract: Drainage is a major means of the conversion of tropical peat forests into agriculture. Accordingly, drained peat becomes a large source of carbon. However, the amount of carbon (C) loss from drained peats is not simply measured. The current C loss estimate is usually based on a single proxy of the groundwater table, spatially and temporarily dynamic. The relation between groundwater table and C emission is commonly not linear because of the complex natures of heterotrophic carbon emission. Peatland drainage or lowering groundwater table provides plenty of oxygen into the upper layer of peat above the water table, where microbial activity becomes active. Consequently, lowering the water table escalates subsidence that causes physical changes of organic matter (OM) and carbon emission due to microbial oxidation. This paper reviews peat bulk density (BD), total organic carbon (TOC) content, and subsidence rate of tropical peat forest and drained peat. Data of BD, TOC, and subsidence were derived from published and unpublished sources. We Citation: Anshari, G.Z.; Gusmayanti, found that BD is generally higher in the top surface layer in drained peat than in the undrained peat. -
Freshwater Subaqueous Soil Survey
Outline Introduction to subaqueous soils Chapter 1 - Characterization and mapping of freshwater subaqueous soil resources Chapter 2 - Freshwater subaqueous soils: accumulation of metals (arsenic and lead) and the determination of sedimentation rates Chapter 3 – Freshwater subaqueous soils and carbon accounting Chapter 4 – Aquatic invasive plants, total extractable phosphorus, and freshwater subaqueous soil relationships Subaqueous Soil Investigated as soil for the past 10-15 years Occur in water that is generally <2.5 m deep Support submerged aquatic vegetation Undergoes pedogenesis (soil forming processes) Incorporated in Soil Taxonomy (2010) Little work has been completed in freshwater systems Previous Subaqueous Soil Mapping in Rhode Island NRCS, Mapcoast, URI Coastal ponds and embayments Bathymetry data were used to create landform base maps Delineation of landscape units Vibracoring and field descriptions Mapping and interpretations (i.e. shellfish management, dredged materials, eelgrass restoration, and carbon accounting) Study Sites 3 natural ponds: Worden Pond Watchaug Pond Tucker Pond 3 created ponds: Belleville Pond Bowdish Reservoir Smith & Sayles Reservoir Summary Table of Study Sites Smith Bowdish and Belleville Tucker Worden Watchaug Name Reservoir Sayles Pond Pond Pond Pond Reservoir Area (ha) 103 75 48 39 444 231 Watershed 1478 640 1366 317 317 317 Size (mi²) Maximum 3.0 3.4 2.7 9.8 2.1 13.1 Depth (m) Average 1.8 1.5 1.5 3.4 1.2 2.4 Depth (m) Year 1850 1865 1800 N/A N/A N/A Impounded Summary Table of Study -
Understanding Mountain Soils
2015 In every mountain region, soils constitute the foundation for agriculture, supporting essential ecosystem functions and food security. Mountain soils benefit not only the 900 million people living in the world’s mountainous areas but also billions more living downstream. Soil is a fragile resource that needs time to regenerate. Mountain soils are particularly susceptible to climate change, deforestation, unsustainable farming practices and resource extraction methods that affect their fertility and trigger land degradation, desertification and disasters such as floods and landslides. Mountain peoples often have a deep-rooted connection to the soils they live on; it is a part of their heritage. Over the centuries, they have developed solutions and techniques, indigenous practices, knowledge and sustain- able soil management approaches which have proved to be a key to resilience. This publication, produced by the Mountain Partnership as a contribution to the International Year of Soils 2015, presents the main features of mountain soil systems, their environmental, economic and social values, the threats they are facing and the cultural traditions concerning them. Case studies provided by Mountain Partnership members and partners around the world showcase challenges and opportunities as well as lessons learned in soil management. This publication presents a series of lessons learned and recommendations to inform moun- Understanding Mountain soils tain communities, policy-makers, development experts and academics who support sustainable