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BMP #: Constructed Wetlands
Structural BMP Criteria BMP #: Constructed Wetlands Constructed Wetlands are shallow marsh sys- tems planted with emergent vegetation that are designed to treat stormwater runoff. U.S. Fish and Wildlife Service, 2001 Key Design Elements Potential Applications z Adequate drainage area (usually 5 to 10 acres Residential Subdivision: YES minimum) Commercial: YES Ultra Urban: LIMITED Industrial: YES z Maintenance of permanent water surface Retrofit: YES Highway/Road: YES z Multiple vegetative growth zones through vary- ing depths Stormwater Functions z Robust and diverse vegetation Volume Reduction: Low z Relatively impermeable soils or engineered liner Recharge: Low Peak Rate Control: High z Sediment collection and removal Water Quality: High z Adjustable permanent pool and dewatering Pollutant Removal mechanism Total Suspended Solids: x Nutrients: x Metals: x Pathogens: x Pennsylvania Stormwater Management Manual 1 Section 5 - Structural BMPs Figure 1. Demonstration Constructed Wetlands in Arizona (http://ag.arizona.edu/AZWATER/arroyo/094wet.html) Description Constructed Wetlands are shallow marsh systems planted with emergent vegetation that are designed to treat stormwater runoff. While they are one of the best BMPs for pollutant removal, Constructed Wetlands (CWs) can also mitigate peak rates and even reduce runoff volume to a certain degree. They also can provide considerable aesthetic and wildlife benefits. CWs use a relatively large amount of space and require an adequate source of inflow to maintain the perma- nent water surface. Variations Constructed Wetlands can be designed as either an online or offline facilities. They can also be used effectively in series with other flow/sediment reducing BMPs that reduce the sediment load and equalize incoming flows to the CW. -
NATIONAL WETLANDS INVENTORY and the NATIONAL WETLANDS RESEARCH CENTER PROJECT REPORT FOR: GALVESTON BAY INTRODUCTION the U.S. Fi
NATIONAL WETLANDS INVENTORY AND THE NATIONAL WETLANDS RESEARCH CENTER PROJECT REPORT FOR: GALVESTON BAY INTRODUCTION The U.S. Fish & Wildlife Service's National Wetlands Inventory is producing maps showing the location and classification of wetlands and deepwater habitats of the United States. The Classification of Wetlands and Deepwater Habitats of the United States by Cowardin et al. is the classification system used to define and classify wetlands. Upland classification will utilize the system put forth in., A Land Use and Land Cover Classification System For Use With Remote Sensor Data. by James R. Anderson, Ernest E. Hardy, John T. Roach, and Richard E. Witmer. Photo interpretation conventions, hydric soils-lists and wetland plants lists are also available to enhance the use and application of the classification system. The purpose of the report to users is threefold: (1) to provide localized information regarding the production of NWI maps, including field reconnaissance with a discussion of imagery and interpretation; (2) to provide a descriptive crosswalk from wetland codes on the map to common names and representative plant species; and (3) to explain local geography, climate, and wetland communities. II. FIELD RECONNAISSANCE Field reconnaissance of the work area is an integral part for the accurate interpretation of aerial photography. Photographic signatures are compared to the wetland's appearance in the field by observing vegetation, soil and topography. Thus information is weighted for seasonality and conditions existing at the time of photography and at ground truthing. Project Area The project area is located in the southeastern portion of Texas along the coast. Ground truthing covered specific quadrangles of each 1:100,000 including Houston NE, Houston SE, Houston NW, and Houston SW (See Appendix A, Locator Map). -
The Evolution and Genomic Basis of Beetle Diversity
The evolution and genomic basis of beetle diversity Duane D. McKennaa,b,1,2, Seunggwan Shina,b,2, Dirk Ahrensc, Michael Balked, Cristian Beza-Bezaa,b, Dave J. Clarkea,b, Alexander Donathe, Hermes E. Escalonae,f,g, Frank Friedrichh, Harald Letschi, Shanlin Liuj, David Maddisonk, Christoph Mayere, Bernhard Misofe, Peyton J. Murina, Oliver Niehuisg, Ralph S. Petersc, Lars Podsiadlowskie, l m l,n o f l Hans Pohl , Erin D. Scully , Evgeny V. Yan , Xin Zhou , Adam Slipinski , and Rolf G. Beutel aDepartment of Biological Sciences, University of Memphis, Memphis, TN 38152; bCenter for Biodiversity Research, University of Memphis, Memphis, TN 38152; cCenter for Taxonomy and Evolutionary Research, Arthropoda Department, Zoologisches Forschungsmuseum Alexander Koenig, 53113 Bonn, Germany; dBavarian State Collection of Zoology, Bavarian Natural History Collections, 81247 Munich, Germany; eCenter for Molecular Biodiversity Research, Zoological Research Museum Alexander Koenig, 53113 Bonn, Germany; fAustralian National Insect Collection, Commonwealth Scientific and Industrial Research Organisation, Canberra, ACT 2601, Australia; gDepartment of Evolutionary Biology and Ecology, Institute for Biology I (Zoology), University of Freiburg, 79104 Freiburg, Germany; hInstitute of Zoology, University of Hamburg, D-20146 Hamburg, Germany; iDepartment of Botany and Biodiversity Research, University of Wien, Wien 1030, Austria; jChina National GeneBank, BGI-Shenzhen, 518083 Guangdong, People’s Republic of China; kDepartment of Integrative Biology, Oregon State -
Biodiversity and Trophic Ecology of Hydrothermal Vent Fauna Associated with Tubeworm Assemblages on the Juan De Fuca Ridge
Biogeosciences, 15, 2629–2647, 2018 https://doi.org/10.5194/bg-15-2629-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Biodiversity and trophic ecology of hydrothermal vent fauna associated with tubeworm assemblages on the Juan de Fuca Ridge Yann Lelièvre1,2, Jozée Sarrazin1, Julien Marticorena1, Gauthier Schaal3, Thomas Day1, Pierre Legendre2, Stéphane Hourdez4,5, and Marjolaine Matabos1 1Ifremer, Centre de Bretagne, REM/EEP, Laboratoire Environnement Profond, 29280 Plouzané, France 2Département de sciences biologiques, Université de Montréal, C.P. 6128, succursale Centre-ville, Montréal, Québec, H3C 3J7, Canada 3Laboratoire des Sciences de l’Environnement Marin (LEMAR), UMR 6539 9 CNRS/UBO/IRD/Ifremer, BP 70, 29280, Plouzané, France 4Sorbonne Université, UMR7144, Station Biologique de Roscoff, 29680 Roscoff, France 5CNRS, UMR7144, Station Biologique de Roscoff, 29680 Roscoff, France Correspondence: Yann Lelièvre ([email protected]) Received: 3 October 2017 – Discussion started: 12 October 2017 Revised: 29 March 2018 – Accepted: 7 April 2018 – Published: 4 May 2018 Abstract. Hydrothermal vent sites along the Juan de Fuca community structuring. Vent food webs did not appear to be Ridge in the north-east Pacific host dense populations of organised through predator–prey relationships. For example, Ridgeia piscesae tubeworms that promote habitat hetero- although trophic structure complexity increased with ecolog- geneity and local diversity. A detailed description of the ical successional stages, showing a higher number of preda- biodiversity and community structure is needed to help un- tors in the last stages, the food web structure itself did not derstand the ecological processes that underlie the distribu- change across assemblages. -
Constructed Wetlands
VA DEQ STORMWATER DESIGN SPECIFICATION NO. 13 CONSTRUCTED WETLAND VIRGINIA DEQ STORMWATER DESIGN SPECIFICATION No. 13 CONSTRUCTED WETLANDS VERSION 1.9 March 1, 2011 SECTION 1: DESCRIPTION Constructed wetlands, sometimes called stormwater wetlands, are shallow depressions that receive stormwater inputs for water quality treatment. Wetlands are typically less than 1 foot deep (although they have greater depths at the forebay and in micropools) and possess variable microtopography to promote dense and diverse wetland cover (Figure 13.1). Runoff from each new storm displaces runoff from previous storms, and the long residence time allows multiple pollutant removal processes to operate. The wetland environment provides an ideal environment for gravitational settling, biological uptake, and microbial activity. Constructed wetlands are the final element in the roof-to-stream runoff reduction sequence. They should only be considered for use after all other upland runoff reduction opportunities have been exhausted and there is still a remaining water quality or Channel Protection Volume to manage. Version 1.9, March 1, 2011 Page 1 of 30 VA DEQ STORMWATER DESIGN SPECIFICATION NO. 13 CONSTRUCTED WETLAND SECTION 2: PERFORMANCE The overall stormwater functions of constructed wetlands are summarized in Table 13.1. Table 13.1. Summary of Stormwater Functions Provided by Constructed Wetlands Stormwater Function Level 1 Design Level 2 Design Annual Runoff Volume Reduction (RR) 0% 0% Total Phosphorus (TP) EMC 50% 75% Reduction1 by BMP Treatment Process Total Phosphorus (TP) Mass Load 50% 75% Removal 1 Total Nitrogen (TN) EMC Reduction by 25% 55% BMP Treatment Process Total Nitrogen (TN) Mass Load 25% 55% Removal Yes. -
Vertical and Horizontal Trophic Networks in the Aroid-Infesting Insect Community of Los Tuxtlas Biosphere Reserve, Mexico
insects Article Vertical and Horizontal Trophic Networks in the Aroid-Infesting Insect Community of Los Tuxtlas Biosphere Reserve, Mexico Guadalupe Amancio 1 , Armando Aguirre-Jaimes 1, Vicente Hernández-Ortiz 1,* , Roger Guevara 2 and Mauricio Quesada 3,4 1 Red de Interacciones Multitróficas, Instituto de Ecología A.C., Xalapa, Veracruz 91073, Mexico 2 Red de Biologia Evolutiva, Instituto de Ecología A.C., Xalapa, Veracruz 91073, Mexico 3 Laboratorio Nacional de Análisis y Síntesis Ecológica, Escuela Nacional de Estudios Superiores Unidad Morelia, Universidad Nacional Autónoma de México, Morelia 58190 Michoacán, Mexico 4 Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, Morelia 58190 Michoacán, Mexico * Correspondence: [email protected] Received: 20 June 2019; Accepted: 9 August 2019; Published: 15 August 2019 Abstract: Insect-aroid interaction studies have focused largely on pollination systems; however, few report trophic interactions with other herbivores. This study features the endophagous insect community in reproductive aroid structures of a tropical rainforest of Mexico, and the shifting that occurs along an altitudinal gradient and among different hosts. In three sites of the Los Tuxtlas Biosphere Reserve in Mexico, we surveyed eight aroid species over a yearly cycle. The insects found were reared in the laboratory, quantified and identified. Data were analyzed through species interaction networks. We recorded 34 endophagous species from 21 families belonging to four insect orders. The community was highly specialized at both network and species levels. Along the altitudinal gradient, there was a reduction in richness and a high turnover of species, while the assemblage among hosts was also highly specific, with different dominant species. -
Variability of Large Marine Ecosystems in Response to Global Climate Change
Sherman et al. ICESCM 2007/D:20 ICES CM 2007/D:20 Variability of Large Marine Ecosystems in response to global climate change K. Sherman, I. Belkin, J. O’Reilly and K. Hyde Kenneth Sherman, John O’Reilly, Kimberly Hyde USDOC/NOAA, NMFS Narragansett Laboratory 28 Tarzwell Drive Narragansett, Rhode Island 02882 USA +1 401-782-3210 phone +1 401 782-3201 FAX [email protected] [email protected] [email protected] Igor Belkin Graduate School of Oceanography University of Rhode Island 215 South Ferry Road Narragansett, Rhode Island 02882 USA +1 401 874-6728 phone +1 401 874-6728 FAX [email protected] Abstract: A fifty year time series of sea surface temperature (SST) and time series on fishery yields are examined for emergent patterns relative to climate change. More recent SeaWiFS derived chlorophyll and primary productivity data were also included in the examination. Of the 64 LMEs examined, 61 showed an emergent pattern of SST increases from 1957 to 2006, ranging from mean annual values of 0.08°C to 1.35°C. The rate of surface warming in LMEs from 1957 to 2006 is 4 to 8 times greater than the recent estimate of the Japan Meteorological Society’s COBE estimate for the world oceans. Effects of SST warming on fisheries, climate change, and trophic cascading are examined. Concern is expressed on the possible effects of surface layer warming in relation to thermocline formation and possible inhibition of vertical nutrient mixing within the water column in relation to bottom up effects of chlorophyll and primary productivity on global fisheries resources. -
Facilitation Plays a Key Role in Marsh-Mangrove Interactions Along a Salinity Gradient in South Texas
FACILITATION PLAYS A KEY ROLE IN MARSH-MANGROVE INTERACTIONS ALONG A SALINITY GRADIENT IN SOUTH TEXAS A Thesis by MIKAELA J ZIEGLER BS, University of South Florida, 2014 Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in MARINE BIOLOGY Texas A&M University-Corpus Christi Corpus Christi, Texas August 2018 © Mikaela J. Ziegler All Rights Reserved August 2018 FACILITATION PLAYS A KEY ROLE IN MARSH-MANGROVE INTERACTIONS ALONG A SALINITY GRADIENT IN SOUTH TEXAS A Thesis by MIKAELA J ZIEGLER This thesis meets the standards for scope and quality of Texas A&M University-Corpus Christi and is hereby approved. Ed Proffitt, PhD Chair Lee Smee, PhD Donna Devlin, PhD Committee Member Committee Member August 2018 ABSTRACT Climate change is resulting in fewer and less intense freezes which allows tropical mangroves, Avicennia germinans, to expand into saltmarshes in the Gulf of Mexico, causing a regime shift from herbaceous to woody plant dominance in many areas. Species interactions may affect the extent and rate of this regime shift. The Stress Gradient Hypothesis (SGH) predicts that at low stress plant-plant interactions will be competitive and shift to facilitative at high stress. Climate models show rising temperatures and changing precipitation patterns may lead to prolonged hypersaline conditions in some areas. Hypersalinity stress converts salt marsh dominance from S. alterniflora to succulent forb species or unvegetated tidal flats. Understanding how interactions between marsh species along stress gradients affect different life stages of A. germinans can provide more insight into which salt marsh habitats are vulnerable to encroachment. -
Constructed Stormwater Wetlands
Constructed Wetlands Stormwater Wetlands Purpose Water Quantity Flow attenuation Runoff volume reduction Water Quality Pollution prevention Soil erosion N/A Sediment control N/A Description Nutrient loading N/A Stormwater wetlands are constructed wetland systems designed to Pollutant removal maximize the removal of pollutants from stormwater runoff via several mechanisms: microbial breakdown of pollutants, plant uptake, Total suspended sediment (TSS) retention, settling and adsorption. Stormwater wetlands temporarily Total phosphorus (P) store runoff in shallow pools that support conditions suitable for the growth of wetland plants. Stormwater wetlands also promote the Nitrogen (N) growth of microbial populations which can extract soluble carbon and Heavy metals nutrients and potentially reduce BOD and fecal coliform levels concentrations. Floatables Oil and grease Like detention basins and wet ponds, stormwater wetlands may be used in connection with other BMP components, such as sediment Other forebays and micropools. These engineered wetlands differ from Fecal coliform wetlands constructed for compensatory storage purposes and wet- lands created for restoration. Typically, stormwater wetlands will not Biochemical oxygen demand have the full range of ecological functions of natural wetlands; (BOD) stormwater wetlands are designed specifically for flood control and water quality purposes. Similar to wet ponds, stormwater wetlands require relatively large contributing drainage areas and/or dry Primary design benefit weather base flow. Minimum contributing drainage areas should be at least ten acres, although pocket type wetlands may be appropriate for Secondary design benefit smaller sites if sufficient ground water flow is available. Little or no design benefit The use of stormwater wetlands is limited by a number of site constraints, including soils types, depth to groundwater, contributing drainage area, and available land area. -
Measuring Plant Dominance
Measuring Plant Dominance I. Definition = measure of the relative importance of a plant species with repsect to the degree of influence that the species exerts on the other components (e.g., other plants, animal, soils) of the community. A. Influence based on competition for resources (e.g., light, water, nutrients) B. Difficult to measure influence below ground so dominance is usually estimated with above ground characteristics. II. Types of Dominance A. Aspect dominance: 1. Tallest layer is the dominant layer (reduces climatic extremes by intercepting light and precipitation, reducing wind velocity, and retaining heat). 2. Limitation: Ignores an understory that may be changing while the dominant plant remains the same B. Sociologic dominance 1. Used when interested in understory dominance. (Often used when overstory is constant and unchanging). 2. Limitation: doesn’t work well in systems with diverse overstory species C. Relative dominance 1. Examines the dominant species in each layer of the plant community 2. Useful for multiple use management (overcomes limitations of first two types) III. Why monitory dominance? A. Dominant species are often used to identify or classify and ecological type (e.g., Art.tri/Agr.spi. habitat type). B. If the dominant spp are identified, one can predict changes that may occur in response to long-term precipitation changes or disease. C. If the dominant spp are identified, management options can be more clearly understood. D. Can be used in long-term monitoring programs to determine if management or preservation regimes are positively affecting the ecosystem. IV. Evaluating dominance: A. Can be a single species, a group of species, or and entire growth form B. -
Ecology of Freshwater and Estuarine Wetlands: an Introduction
ONE Ecology of Freshwater and Estuarine Wetlands: An Introduction RebeCCA R. SHARITZ, DAROLD P. BATZER, and STeveN C. PENNINGS WHAT IS A WETLAND? WHY ARE WETLANDS IMPORTANT? CHARACTERISTicS OF SeLecTED WETLANDS Wetlands with Predominantly Precipitation Inputs Wetlands with Predominately Groundwater Inputs Wetlands with Predominately Surface Water Inputs WETLAND LOSS AND DeGRADATION WHAT THIS BOOK COVERS What Is a Wetland? The study of wetland ecology can entail an issue that rarely Wetlands are lands transitional between terrestrial and needs consideration by terrestrial or aquatic ecologists: the aquatic systems where the water table is usually at or need to define the habitat. What exactly constitutes a wet- near the surface or the land is covered by shallow water. land may not always be clear. Thus, it seems appropriate Wetlands must have one or more of the following three to begin by defining the wordwetland . The Oxford English attributes: (1) at least periodically, the land supports predominately hydrophytes; (2) the substrate is pre- Dictionary says, “Wetland (F. wet a. + land sb.)— an area of dominantly undrained hydric soil; and (3) the substrate is land that is usually saturated with water, often a marsh or nonsoil and is saturated with water or covered by shallow swamp.” While covering the basic pairing of the words wet water at some time during the growing season of each year. and land, this definition is rather ambiguous. Does “usu- ally saturated” mean at least half of the time? That would This USFWS definition emphasizes the importance of omit many seasonally flooded habitats that most ecolo- hydrology, soils, and vegetation, which you will see is a gists would consider wetlands. -
Lakes: Ann, Gilchrist, Grove, Leven, Reno, Villard, Smith)
Status and Trend Monitoring Summary for Selected Pope and Douglas County, Minnesota Lakes 2000 (Lakes: Ann, Gilchrist, Grove, Leven, Reno, Villard, Smith) Minnesota Pollution Control Agency Environmental Outcomes Division Environmental Monitoring and Analysis Section Andrea Plevan and Steve Heiskary September 2001 Printed on recycled paper containing at least 10 percent fibers from paper recycled by consumers. This material may be made available in other formats, including Braille, large format and audiotape. MPCA Status and Trend Monitoring Summary for 2000 Pope County Lakes Part 1: Purpose of study and background information on MN lakes The Minnesota Pollution Control Agency’s (MPCA) core lake-monitoring programs include the Citizen Lake Monitoring Program (CLMP), the Lake Assessment Program (LAP), and the Clean Water Partnership (CWP) Program. In addition to these programs, the MPCA annually monitors numerous lakes to provide baseline water quality data, provide data for potential LAP and CWP lakes, characterize lake conditions in different regions of the state, examine year-to-year variability in ecoregion reference lakes, and provide additional trophic status data for lakes exhibiting trends in Secchi transparency. In the latter case, we attempt to determine if the trends in Secchi transparency are “real,” i.e., if supporting trophic status data substantiate whether a change in trophic status has occurred. The lake sampling efforts also provide a means to respond to citizen concerns about protecting or improving the lake in cases where no data exists to evaluate the quality of the lake. For efficient sampling, we tend to select geographic clusters of lakes (e.g., focus on a specific county) whenever possible.