Life in a Wetland
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Biogas for Agriculture
2007 IGER INNOVATIONS Biogas for agriculture Phil Hobbs, Alastair Ward and Guillermo Pardo Biogas feedstock 44 Current research 44 2007 IGER INNOVATIONS Biogas for agriculture Phil Hobbs, Alastair Ward and Guillermo Pardo he production of biogas as a fuel obtained from Biogas feedstock B I the fermentation of organic wastes has undoubted O Livestock manure slurry is the main source of G A Tbenefits for the environment . These benefits include feedstock for biogas production, having a dry matter S F both reduced methane emissions from livestock content of about 5 -15% w/w, but potentially a wide O R enterprises and the production of green energy which range of organic wastes can be used as starter A G can be fed into the national electricity grid. The heat materials, ranging from fats and greases to vegetable R I C generated from biogas production can also be used wastes . Some potential sources, such as food and U L T locally for heating livestock buildings or hot water. abattoir wastes , would need to be heat -treated before U R E Biogas is about 70% methane and 30% CO 2. The use as a biogas feedstock as a biosecurity measure, actual methane producers are microbes known as however, in order to prevent any contained ‘methanogens ’. These belong to some of the oldest pathogens escaping to reinfect farm livestock via groups of organisms on the planet , known as the grazing or other crop sources. Organic wastes Archaea . They are common in wetlands, where they imported onto the farm are also a good source of are responsible for producing marsh gas , and are also nutrients for spreading on the land and can commonly found in the gut of ruminants such as significantly reduce artificial fertiliser use , both cattle, and in their faeces . -
Maritime Swamp Forest (Typic Subtype)
MARITIME SWAMP FOREST (TYPIC SUBTYPE) Concept: Maritime Swamp Forests are wetland forests of barrier islands and comparable coastal spits and back-barrier islands, dominated by tall trees of various species. The Typic Subtype includes most examples, which are not dominated by Acer, Nyssa, or Fraxinus, not by Taxodium distichum. Canopy dominants are quite variable among the few examples. Distinguishing Features: Maritime Shrub Swamps are distinguished from other barrier island wetlands by dominance by tree species of (at least potentially) large stature. The Typic Subtype is dominated by combinations of Nyssa, Fraxinus, Liquidambar, Acer, or Quercus nigra, rather than by Taxodium or Salix. Maritime Shrub Swamps are dominated by tall shrubs or small trees, particularly Salix, Persea, or wetland Cornus. Some portions of Maritime Evergreen Forest are marginally wet, but such areas are distinguished by the characteristic canopy dominants of that type, such as Quercus virginiana, Quercus hemisphaerica, or Pinus taeda. The lower strata also are distinctive, with wetland species occurring in Maritime Swamp Forest; however, some species, such as Morella cerifera, may occur in both. Synonyms: Acer rubrum - Nyssa biflora - (Liquidambar styraciflua, Fraxinus sp.) Maritime Swamp Forest (CEGL004082). Ecological Systems: Central Atlantic Coastal Plain Maritime Forest (CES203.261). Sites: Maritime Swamp Forests occur on barrier islands and comparable spits, in well-protected dune swales, edges of dune ridges, and on flats adjacent to freshwater sounds. Soils: Soils are wet sands or mucky sands, most often mapped as Duckston (Typic Psammaquent) or Conaby (Histic Humaquept). Hydrology: Most Maritime Swamp Forests have shallow seasonal standing water and nearly permanently saturated soils. Some may rarely be flooded by salt water during severe storms, but areas that are severely or repeatedly flooded do not recover to swamp forest. -
PESHTIGO RIVER DELTA Property Owner
NORTHEAST - 10 PESHTIGO RIVER DELTA WETLAND TYPES Drew Feldkirchner Floodplain forest, lowland hardwood, swamp, sedge meadow, marsh, shrub carr ECOLOGY & SIGNIFICANCE supports cordgrass, marsh fern, sensitive fern, northern tickseed sunflower, spotted joe-pye weed, orange This Wetland Gem site comprises a very large coastal • jewelweed, turtlehead, marsh cinquefoil, blue skullcap wetland complex along the northwest shore of Green Bay and marsh bellflower. Shrub carr habitat is dominated three miles southeast of the city of Peshtigo. The wetland by slender willow; other shrub species include alder, complex extends upstream along the Peshtigo River for MARINETTE COUNTY red osier dogwood and white meadowsweet. Floodplain two miles from its mouth. This site is significant because forest habitats are dominated by silver maple and green of its size, the diversity of wetland community types ash. Wetlands of the Peshtigo River Delta support several present, and the overall good condition of the vegetation. - rare plant species including few-flowered spikerush, The complexity of the site – including abandoned oxbow variegated horsetail and northern wild raisin. lakes and a series of sloughs and lagoons within the river delta – offers excellent habitat for waterfowl. A number This Wetland Gem provides extensive, diverse and high of rare animals and plants have been documented using quality wetland habitat for many species of waterfowl, these wetlands. The area supports a variety of recreational herons, gulls, terns and shorebirds and is an important uses, such as hunting, fishing, trapping and boating. The staging, nesting and stopover site for many migratory Peshtigo River Delta has been described as the most birds. Rare and interesting bird species documented at diverse and least disturbed wetland complex on the west the site include red-shouldered hawk, black tern, yellow shore of Green Bay. -
Tidal Wetland Gross Primary Production Across the Continental
RESEARCH ARTICLE Tidal Wetland Gross Primary Production Across 10.1029/2019GB006349 the Continental United States, 2000–2019 Special Section: R. A. Feagin1 , I. Forbrich2 , T. P. Huff1, J. G. Barr3, J. Ruiz‐Plancarte4 , J. D. Fuentes4 , Carbon cycling in tidal wet- 4 5 5 6 7 R. G. Najjar , R. Vargas , A. Vázquez‐Lule , L. Windham‐Myers , K. D. Kroeger , lands and estuaries of the con- 8 1 9 8 8 2 tiguous United States E. J. Ward , G. W. Moore , M. Leclerc , K. W. Krauss , C. L. Stagg , M. Alber , S. H. Knox10 , K. V. R. Schäfer11, T. S. Bianchi12 , J. A. Hutchings13 , H. Nahrawi9,14 , 1 1 1 1,15 6 16 Key Points: A. Noormets , B. Mitra , A. Jaimes , A. L. Hinson , B. Bergamaschi , J. S. King , and 17 • We created the Blue Carbon (BC) G. Miao model, which mapped the Gross Primary Production (GPP) of all 1Department of Ecology and Conservation Biology, Texas A&M University, College Station, TX, USA, 2Marine Biological tidal wetlands within the Laboratory, Woods Hole, MA, USA, 3Elder Research, Charlottesville, VA, USA, 4Department of Meteorology and continental United States 5 • Atmospheric Science, Pennsylvania State University, University Park, PA, USA, Department of Plant and Soil Sciences, The BC model provides maps of tidal 6 7 wetland GPP at sub‐250 m scales University of Delaware, Newark, DE, USA, United States Geological Survey, Menlo Park, CA, USA, United States 8 and at 16‐day intervals for the years Geological Survey, Woods Hole, MA, USA, United States Geological Survey, Wetland and Aquatic Research Center, 2000‐2019 Lafayette, LA, USA, 9Atmospheric Biogeosciences, University of Georgia, Athens, GA, USA, 10Department of Geography, • 2 The average daily GPP per m was University of British Columbia, Vancouver, BC, USA, 11Department of Biological Sciences, Rutgers University, Newark, 4.32 ± 2.45 g C/m2/day, and the total NJ, USA, 12Departmet of Geological Sciences, University of Florida, Gainesville, FL, USA, 13Department of Earth and annual GPP for the continental 14 United States was 39.65 ± 0.89 Tg Planetary Sciences, Washington University, St. -
Exploring Our Wonderful Wetlands Publication
Exploring Our Wonderful Wetlands Student Publication Grades 4–7 Dear Wetland Students: Are you ready to explore our wonderful wetlands? We hope so! To help you learn about several types of wetlands in our area, we are taking you on a series of explorations. As you move through the publication, be sure to test your wetland wit and write about wetlands before moving on to the next exploration. By exploring our wonderful wetlands, we hope that you will appreciate where you live and encourage others to help protect our precious natural resources. Let’s begin our exploration now! Southwest Florida Water Management District Exploring Our Wonderful Wetlands Exploration 1 Wading Into Our Wetlands ................................................Page 3 Exploration 2 Searching Our Saltwater Wetlands .................................Page 5 Exploration 3 Finding Out About Our Freshwater Wetlands .............Page 7 Exploration 4 Discovering What Wetlands Do .................................... Page 10 Exploration 5 Becoming Protectors of Our Wetlands ........................Page 14 Wetlands Activities .............................................................Page 17 Websites ................................................................................Page 20 Visit the Southwest Florida Water Management District’s website at WaterMatters.org. Exploration 1 Wading Into Our Wetlands What exactly is a wetland? The scientific and legal definitions of wetlands differ. In 1984, when the Florida Legislature passed a Wetlands Protection Act, they decided to use a plant list containing plants usually found in wetlands. We are very fortunate to have a lot of wetlands in Florida. In fact, Florida has the third largest wetland acreage in the United States. The term wetlands includes a wide variety of aquatic habitats. Wetland ecosystems include swamps, marshes, wet meadows, bogs and fens. Essentially, wetlands are transitional areas between dry uplands and aquatic systems such as lakes, rivers or oceans. -
Coastal Wetland Trends in the Narragansett Bay Estuary During the 20Th Century
u.s. Fish and Wildlife Service Co l\Ietland Trends In the Narragansett Bay Estuary During the 20th Century Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century November 2004 A National Wetlands Inventory Cooperative Interagency Report Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century Ralph W. Tiner1, Irene J. Huber2, Todd Nuerminger2, and Aimée L. Mandeville3 1U.S. Fish & Wildlife Service National Wetlands Inventory Program Northeast Region 300 Westgate Center Drive Hadley, MA 01035 2Natural Resources Assessment Group Department of Plant and Soil Sciences University of Massachusetts Stockbridge Hall Amherst, MA 01003 3Department of Natural Resources Science Environmental Data Center University of Rhode Island 1 Greenhouse Road, Room 105 Kingston, RI 02881 November 2004 National Wetlands Inventory Cooperative Interagency Report between U.S. Fish & Wildlife Service, University of Massachusetts-Amherst, University of Rhode Island, and Rhode Island Department of Environmental Management This report should be cited as: Tiner, R.W., I.J. Huber, T. Nuerminger, and A.L. Mandeville. 2004. Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century. U.S. Fish and Wildlife Service, Northeast Region, Hadley, MA. In cooperation with the University of Massachusetts-Amherst and the University of Rhode Island. National Wetlands Inventory Cooperative Interagency Report. 37 pp. plus appendices. Table of Contents Page Introduction 1 Study Area 1 Methods 5 Data Compilation 5 Geospatial Database Construction and GIS Analysis 8 Results 9 Baywide 1996 Status 9 Coastal Wetlands and Waters 9 500-foot Buffer Zone 9 Baywide Trends 1951/2 to 1996 15 Coastal Wetland Trends 15 500-foot Buffer Zone Around Coastal Wetlands 15 Trends for Pilot Study Areas 25 Conclusions 35 Acknowledgments 36 References 37 Appendices A. -
Muck: Causes and Corrective Actions1 Mark V
FA200 A Beginner’s Guide to Water Management—Muck: Causes and Corrective Actions1 Mark V. Hoyer, Daniel E. Canfield, Jr. and Mark Brenner2 This publication was produced by: Florida LAKEWATCH 2017 UF/IFAS School of Forest Resources and Conservation / Fisheries and Aquatic Sciences 7922 NW 71st Street Gainesville, Florida 32653-3071 Phone: 352/392-4817 FAX: 352/392-3672 E-mail: [email protected] Website: http://lakewatch.ifas.ufl.edu Copies are available for download from the LAKEWATCH website: http://lakewatch.ifas.ufl.edu/data.shtml Muck from pond at Fisheries and Aquatic Sciences, Gainesville, FL. Credits: Mark Hoyer, UF/IFAS Introduction Informational Circular 112 Muck is both the popular and the scientific term for the material found on the bottom of many depressions that Florida LAKEWATCH have held water for any length of time. It is of great impor- tance to many recreational lake users because its presence UF/IFAS Fisheries and Aquatic Sciences can ruin their enjoyment of the water body. Its dark color School of Forest Resources and Conservation and “oozy” feel lead many people to believe muck could be Gainesville, Florida an indicator of a polluted system. January 2017 Another cause for people’s distaste for muck is the stink. Bacterial decomposition of the organic matter in muck 1. This document is FA200, one of a series of the School of Forest Resources and Conservation Program in Fisheries and Aquatic Sciences, UF/IFAS Extension. Original publication date February 2017. Visit the EDIS website at http://edis.ifas.ufl.edu. 2. Mark V. Hoyer, director, Florida LAKEWATCH, UF/IFAS Program in Fisheries and Aquatic Sciences of the School of Forest Resources and Conservation; Daniel E. -
Odors, Explained
OdorCap Information Sheet Unique Odors w/ Encapsulation Technology Several Distinctive Odors Explained Hydrogen sulfides Gas This is the by-product of anaerobic activity. This anaerobic activity survives very well in low oxygen levels or no oxygen levels of the sewer water or the sewer transmission lines. This is the main reason to try and remove this type of bacteria from the sewer lines being in the water or the line. These levels can even become dangerous to personnel working and living around the area. Low levels Hydrogen sulfide has a very strong odor and can be smelled at levels as low as 0.005 - 0.02 parts per million (ppm). Higher levels may cause an offensive, rotten-egg odor, and can irritate eyes, nose, and throat. The lungs and nasal passages may also become inflamed. Eyes may become sore and watery. Your throat may itch, and you may start to cough. Long-term health effects of low-level hydrogen sulfide exposure are unknown. High levels At levels above 100 ppm, hydrogen sulfide is very dangerous. The gas loses its odor by overpowering the sense of smell and begins to affect the whole body. At 250 ppm, a person my quickly lose consciousness. They may experience powerful stinging of the eyes, throat, and suffer from severe lung inflammation. At 500 ppm and higher, people can have convulsions, respiratory arrest, and heart failure. High exposure levels may also cause permanent brain damage. According to the National Institute for Occupational Safety and Health (NIOSH), hydrogen sulfide is a leading cause of sudden death from workplace chemical exposure. -
Appendix a Basics of Landfill
APPENDIX A BASICS OF LANDFILL GAS Basics of Landfill Gas (Methane, Carbon Dioxide, Hydrogen Sulfide and Sulfides) Landfill gas is produced through bacterial decomposition, volatilization and chemical reactions. Most landfill gas is produced by bacterial decomposition that occurs when organic waste solids, food (i.e. meats, vegetables), garden waste (i.e. leaf and yardwaste), wood and paper products, are broken down by bacteria naturally present in the waste and in soils. Volatilization generates landfill gas when certain wastes change from a liquid or solid into a vapor. Chemical reactions occur when different waste materials are mixed together during disposal operations. Additionally, moisture plays a large roll in the speed of decomposition. Generally, the more moisture, the more landfill gas is generated, both during the aerobic and anaerobic conditions. Landfill Gas Production and Composition: In general, during anaerobic conditions, the composition of landfill gas is approximately 50 percent methane and 50 percent carbon dioxide with trace amounts (<1 percent) of nitrogen, oxygen, hydrogen sulfide, hydrogen, and nonmethane organic compounds (NMOCs). The more organic waste and moisture present in a landfill, the more landfill gas is produced by the bacteria during decomposition. The more chemicals disposed in a landfill, the more likely volatile organic compounds and other gasses will be produced. The Four Phases of Bacterial Decomposition: “Bacteria decompose landfill waste in four phases. The composition of the gas produced changes with each of the four phases of decomposition. Landfills often accept waste over a 20-to 30-year period, so waste in a landfill may be undergoing several phases of decomposition at once. -
A Climate Change Adaptation Framework for Hudson River
PROTECTING THE PATHWAYS: A Climate Change Adaptation Framework for Hudson River Estuary Tidal Wetlands PROTECTING THE PATHWAYS: A Climate Change Adaptation Framework for Hudson River Estuary Tidal Wetlands Scenic Hudson, May 2016 Nava Tabak & Dr. Sacha Spector Research and planning partners: New York State Department of Environmental Conservation Hudson River Estuary Program Hudson River National Estuarine Research Reserve Cary Institute of Ecosystem Studies The Nature Conservancy Hudsonia Ltd. Warren Pinnacle Consulting, Inc. Cover Photo: Robert Rodriguez, Jr. Robert Rodriguez, Jr. Robert Rodriguez, TIDAL WETLAND: KEYSTONE HABITATS OF THE HUDSON The Hudson River Estuary (HRE), stretching approximately 150 miles from the Battery in Manhattan to the Federal Dam in Troy, is a region of rich biological resources. At the heart of this estuarine ecosystem are approximately 7,000 acres of intertidal wetlands—keystone elements in the Hudson’s aquatic and ter- restrial ecology. Encompassing both brackish and freshwater tidal habitats such as mud and sand flats, emergent broad-leaf and graminoid-dominated marshes, and shrub and tree swamps, the Hudson’s tidal wetlands are fundamentally important to support- ing the species and functions of the estuary. They serve as feed- ing, nursery and refuge areas for the nearly 200 species of fish known from the HRE, including 11 migratory species of sturgeon, herring, bass, and eels that journey between the Hudson and the Erik Kiviat/Hudsonia Atlantic. A myriad of migrating and overwintering shorebirds and Golden-club (orontium aquaticum) waterfowl also depend on these rich tidal habitats. Many species of rare plants and animals, such as golden-club and the secretive least bittern, are specialist occupants of these wetlands. -
The Verlot Peat Area Was Investigated by Rigg, Ac Thick
188 PEAT RESOURCES OF WASHINGTON Verlot peat area and the layer of fibrous peat and muck under it was 4 feet The Verlot peat area was investigated by Rigg, ac thick. companied by C. E. Torrence and D. Tunstall, August Lake Ketchum peat area 13 to 15, 1926. The following description is based on field The Lake Ketchum peat area (19 acres) 1s m secs. 6 notes made at that time, supplemented by some explana and 7, T. 32 N., R. 4 E., about 3 miles north of East Stan tions. wood by State Highway IE and a crooked dead-end road The peat area was estimated at 15 to 20 acres. Its loca up a steep slope. The deposit borders the north shore tion was estimated to be about 2 miles south of the old of the lake (map, fig. 193). The lake and the topography Mackie statio~ (an abandoned sawmill) on the old of the region surrounding it are shown on the Mount Monte Cristo Branch (now abandoned) of the Northern Vernon quadrangle. The elevation of the peat is about 175 Pacific Railway. The location of Mackie is shown on feet above sea level, and it is less than 2 miles from the Forest Service maps of the Snoqualmie National Forest. shore of Skagit Bay. It lies in a depression in glacial The peat is probably in sec. 25 or 36, T. 30 N., R. 8 E. It drift of the region. The lake has no surface outlet. On was reached from the station by a rather steep, rocky wet the soil map of Snohomish County (Anderson et al., 1947) trail which extended over the mountainous region and the area is mapped as Gre~nwood peat and Carbondale down to the Pilchuck River. -
Salt Marsh Monitoring by The
SaltSalt MarshMarsh MonitoringMonitoring byby thethe U.S.U.S. FishFish && WildlifeWildlife ServiceService’’ss NortheastNortheast RegionRegion Ralph Tiner Regional Wetland Coordinator U.S. Fish and Wildlife Service-Northeast Region February 2010 TypesTypes ofof MonitoringMonitoring RemotelyRemotely sensedsensed MonitoringMonitoring Area and type changes (e.g., trends analysis) Can cover large or small areas OnOn--thethe--groundground MonitoringMonitoring Addressing processes (accretion, erosion, subsidence, salt balance, etc.) Analyzing vegetation and soil changes Plot analysis Reference wetlands Evaluating wildlife habitat RemotelyRemotely SensedSensed MonitoringMonitoring NWINWI usesuses aerialaerial imageryimagery toto tracktrack wetlandwetland changeschanges inin wetlandwetland typetype WetlandWetland StatusStatus && TrendsTrends StudiesStudies == aa typetype ofof monitoringmonitoring For large geographic areas Statistical Sampling – analyze changes in 4-square mile plots; generate estimates For small areas Area-based Analysis –analyze complete area for changes over time RegionRegion vsvs LocalLocal ReportsReports CanfieldCanfield Cove,Cove, CTCT 19741974 20042004 Canfield Island Cove 60 50 40 s e 30 Acr 20 10 0 1974 1981 1986 1990 1995 2000 2004 Low Marsh High Marsh Flat ConsiderationsConsiderations forfor SiteSite--specificspecific MonitoringMonitoring SpecialSpecial aerialaerial imageryimagery LowLow tidetide PeakPeak ofof growinggrowing seasonseason NormalNormal issuesissues re:re: qualityquality (e.g.,(e.g.,