Background information of groundwater dependent ecosystems (GDE) on Estonian Gauja-Koiva river basin
|
|
- Ambrose Banks
- 5 years ago
- Views:
Transcription
1 Background information of groundwater dependent ecosystems (GDE) on Estonian Gauja-Koiva river basin Elve Lode & Martin Küttim
2 Content Some facts about the Koiva river Something about GDEs Ecological data base of GDEs in Koiva river catchment Known spring-fens in Koiva river catchment
3 Location of Koiva river and it catchment Length of the Koiva river (in Estonia) = 26 km, i.e. between km from the mouth of the Gauja river Catchment area (in Estonia) = 1302 km 2 (ca 25% from all Gauja river catchment) (EELIS data base; Eesti NSV jõgede, ojade ja kraavide ametlik nimestik, 1986)
4 Koiva river stream network The longest river in the catchment is the Mustjõgi river (L= 84 km, F= 1820 km 2, in Estonia 994 km 2 ) Totally there are about 50 flowing water bodies in the Koiva river basin data base, but 80% of them are brooks (EELIS data base; Eesti NSV jõgede, ojade ja kraavide ametlik nimestik, 1986)
5 Groundwater-Dependent Ecosystems (GDEs) are ecosystems that rely upon groundwater for their continued existence Groundwater-Dependent Terrestrial Ecosystems (GWDTEs) are wetlands which critically depend on groundwater flows and /or chemistries Prerequisites for occurrence of GDEs or GWDTEs P 1. General atmosphere-ground conditions a) Availability of sufficient water (mainly from the atmosphere) b) Availability to form recharge and discharge areas on the landscape
6 2. Interaction between general hydro-geological conditions and surface topology, i.e. type of GDEs or GWDTEs a) Availability to form regional groundwater dependent ecosystems on the landscape or a) Availability to form local groundwater dependent ecosystems on the landscape
7 3. Ecosystem dynamics within non-disturbed atmosphere-hydro-geologic-surface topology conditions, - as a reference a) Dynamics of discharge area hydrology, i.e. water quantity and quality in wet phase and dry phase b) Dynamics of ecosystems plant cover, i.e. horizontal zonation and it dynamics in wet phase and dry phase Example of ecological zonation of regional groundwater dependent ecosystem on the ground 1. Zone of permanent inundation and/or flowing discharge 2. Zone of aeration and reduced saturation 3. Saturated shoulder of the mound 4. Non-wetland area 5. Discharge tail during the wet phase 6. Wetland to non-wetland transition zone 7. Discharge tail during dry phase 8. Discharge tail during the dry phase Type 1a Wetlands located in off-stream environments, within floodplains
8 Example of ecological zonation of regional groundwater dependent ecosystem Example of ecological zonation of mixed groundwater dependent ecosystem and influenced by surface water flows Type 2 Semi-permanent brackish, palustrine wetlands with minor wetland soils and minor vegetation cover, mainly connected to regional groundwater systems Type 3 Permanent to semi-permanent riverine wetlands with minor wetland soils and moderate vegetation cover, sourced from local and regional groundwater systems and significantly influenced by surface water flows type-2 & type-3
9 Examples of ecological zonation of local groundwater dependent ecosystem Type 4 & 5 Semi-permanent fresh riverine-to-palustrine wetlands with minor wetland soils and moderate vegetation cover, mainly connected to local groundwater systems. 4 & type-5
10 Questions needed to answer * What is the list of the terminology what we will agree to use? Groundwater-Dependent Ecosystems (GDEs) (are ecosystems that rely upon groundwater for their continued existence) or Groundwater dependent terrestrial ecosystems (GWDTEs) (are wetlands which critically depend on groundwater flows and /or chemistries) * What is the spring mire? Not all fens are the spring mires and not all springs are forming spring mires! * What are the threshold values (TVs) for the GDEs or GWDTE? (Groundwater dependent terrestrial ecosystem (GWDTE) threshold values (TVs) are groundwater chemical concentrations which have been derived from empirical evidence) * How to mesaure and report the ecosystem conditions? 1) General atmosphere-ground conditions 2) Interaction between general hydro-geological conditions and surface topology 3) Ecosystem dynamics within non-disturbed atmosphere-hydro-geologic-surface topology conditions, as a reference 4) Disturbances
11 Ecological data base of Koiva river catchment Red polygons 1. Matsi spring mire 3 areas 2. Varstu spring mire 1 area Green polygons A, , 3113
12 Spring fens in Estonia (Paal & Leibak 2011) Spring fens in South-Estonia (Ilomets et al 2012) Symbols: green dots - calcareous spring fens in good state; blue squares - drained sites; red triangles - abandoned tufa deposits or damaged sites
13 Spring fen vegetation
14 Spring fen vegetation: community composition Cotton-grasses: Eriophorum angustifolium E. latifolium Schoenus ferrugineus Sesleria caerulea Sedges: Carex davalliana C. hostiana C. dioica C. diandra C. rostrata Pinguicula vulgaris etc
15 Environmental factors controlling the vegetation composition High water table Low fluctuation of water table Stabile temperature Low availability of nutrients High ph Precipitation of tufa (?)
16 Water table ~ vegetation (Küttim 2013)
17 Spring fens in Koiva catchment Matsi Varstu More?
18 Matsi spring fens (Ilomets et al 2014) Location: Võru county, Varstu parish, Matsi village Geologically: in Võru-Hargla valley, by the Mustjõgi river Area: 4.6 ha (in three parts) Northern part 3.4 ha In a relatively good state, but surrounded by the ditches and a road Mostly open habitats, but wooded in drier part Vegetation: Dominated everywhere by Menyanthes trifoliata Sedges (Carex lasiocarpa, C. rostrata) Abundant Epipactis palustris (protected II cat.!)
19 Matsi spring fens (Ilomets et al 2014)
20 Matsi spring fens (Ilomets et al 2014) Oppressional springs (igritsevad) in the northern and central part, overflowing water in the south Tufa precipitation in the northern and central part, iron precipitation in the south Water table near surface ( cm below surface) Minor slope (1 m per 50 m) ph Sedge-brown moss peat with tufa layers
21
22
23 Thank You!
Landscapes & Hydric Soils Bruce Vasilas University of Delaware
Landscapes & Hydric Soils Bruce Vasilas University of Delaware Hydric soils are defined as soils that formed under conditions of saturation, flooding, or ponding long enough during the growing season to
More informationIntroduction to the Hydrogeomorphic (HGM) Classification System
Introduction to the Hydrogeomorphic (HGM) Classification System Objectives The Student Will be Able to: Define the 7 HGM Classes List the 3 Parameters That Define HGM Classes List the Major Water Budget
More informationMs. A. Mormando's Class *
8 th Grade Science Essential Standard: 8.E.1.1 Explain the structure of the hydrosphere including: Water distribution on Earth; Local river basin and water availability Stream - A stream is a body of water
More informationBiodiversity Blueprint Overview
Biodiversity Blueprint Overview Climate Variability Climate projections for the Glenelg Hopkins Regions suggest that the weather will be hotter and drier in the coming years which will impact on land use,
More informationPermafrost-influenced Geomorphic Processes
Section 4 Permafrost-influenced Geomorphic Processes Geomorphic processes vary greatly among ecoregions in northern Alaska, extending from the Beaufort Sea coast to the Brooks Range (Figure 4.1). Regional
More informationModule 3. Basic Ecological Principles
Module 3. Basic Ecological Principles Ecosystem Components Abiotic Biotic Species & Habitat The Biomes of North America Communities Energy & Matter Cycles in Ecosystems Primary Productivity Simple Ecosystem
More informationCreating ponds for Marsh Clubmoss Lycopodielle inundata
Creating ponds for Marsh Clubmoss Lycopodielle inundata Freshwater Habitats Trust 1. What is Marsh Clubmoss? Marsh Clubmoss Lycopodiella inundata is not a true moss but a primitive non-flowering plant
More informationOrigin of the Atmosphere. Note: No free oxygen at this point!!! (A) (B)
Origin of the Atmosphere (A) During the early stages of segregation within Earth (A), gaseous materials escaped from Earth s interior. A process called volcanic outgassing An atmosphere gradually evolved,
More informationEarth s Major Terrerstrial Biomes. *Wetlands (found all over Earth)
Biomes Biome: the major types of terrestrial ecosystems determined primarily by climate 2 main factors: Depends on ; proximity to ocean; and air and ocean circulation patterns Similar traits of plants
More informationHow Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin?
How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin? Bruce Rhoads Department of Geography University of Illinois at Urbana-Champaign
More informationKakagon Sloughs, Bad River Reservation 1980s Jim Meeker, Northland College
Natural history of coastal wetlands in the greater Chequamegon Bay region Kakagon Sloughs, Bad River Reservation 1980s Jim Meeker, Northland College small large northern Great Lake wetlands are dominated
More informationWhy Geomorphology for Fish Passage
Channel Morphology - Stream Crossing Interactions An Overview Michael Love Michael Love & Associates mlove@h2odesigns.com (707) 476-8938 Why Geomorphology for Fish Passage 1. Understand the Scale of the
More informationGIS and Coastal Nutrients Luke Cole
GIS and Coastal Nutrients Luke Cole Human population density has been widely utilized as a valid predictor of terrestrial nitrogen loads into marine systems. As 50% of the world s population lives within
More informationSurface Water Short Study Guide
Name: Class: Date: Surface Water Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The three ways in which a stream carries
More informationWATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle
WATER ON AND UNDER GROUND Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin. Describe how floods occur and what factors may make
More informationConsulting Services (Pty.) Ltd.
Wetland Consulting Services (Pty.) Ltd. 98/726/07 P.O. Box 72295 Lynnwood Ridge Pretoria 0040 Consulting Services (Pty.) Ltd. Specialist wetland and riparian consultants Room S 57 Building 33 CSIR Meiring
More informationSubtidal permanently flooded with tidal water. Irregularly exposed surface exposed by tides less often than daily
Types of Wetlands Tidal Systems COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands Tidal Estuarine Wetland 1 Definition and Formation of Estuaries u Estuary : partially
More informationTypes of Wetlands. Tidal Systems
Types of Wetlands Tidal Systems 1 COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands 2 Tidal Estuarine Wetland 3 Definition and Formation of Estuaries Estuary: : partially
More informationWetland and Riparian Mapping: An Overview of the Montana Program
Wetland and Riparian Mapping: An Overview of the Montana Program Meghan Burns, Catherine McIntyre, Karen Newlon Ecology Program Montana Natural Heritage Program Helena, MT Montana Natural Heritage Program
More informationWetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont. Mike Kline and Laura Lapierre Vermont DEC
Wetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont Mike Kline and Laura Lapierre Vermont DEC NWI+ Hydro-Geomorphic Characterization of Wetlands and
More informationADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN
ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN Conor Shea - Hydrologist U.S. Fish and Wildlife Service Conservation Partnerships Program Arcata, CA Learning Objectives Examine
More informationAquifer an underground zone or layer of sand, gravel, or porous rock that is saturated with water.
Aggradation raising of the streambed by deposition that occurs when the energy of the water flowing through a stream reach is insufficient to transport sediment conveyed from upstream. Alluvium a general
More informationCR AAO Bridge. Dead River Flood & Natural Channel Design. Mitch Koetje Water Resources Division UP District
CR AAO Bridge Dead River Flood & Natural Channel Design Mitch Koetje Water Resources Division UP District Old County Road AAO Bridge Map courtesy of Marquette County Silver Lake Basin McClure Basin
More informationOpportunities to Improve Ecological Functions of Floodplains and Reduce Flood Risk along Major Rivers in the Puget Sound Basin
Opportunities to Improve Ecological Functions of Floodplains and Reduce Flood Risk along Major Rivers in the Puget Sound Basin Christopher Konrad, US Geological Survey Tim Beechie, NOAA Fisheries Managing
More informationScience EOG Review: Landforms
Mathematician Science EOG Review: Landforms Vocabulary Definition Term canyon deep, large, V- shaped valley formed by a river over millions of years of erosion; sometimes called gorges (example: Linville
More informationThe River Restoration Centre therrc.co.uk. Understanding Fluvial Processes: supporting River Restoration. Dr Jenny Mant
The River Restoration Centre therrc.co.uk Understanding Fluvial Processes: supporting River Restoration Dr Jenny Mant Jenny@therrc.co.uk Understanding your catchment Hydrology Energy associated with the
More informationUK Flooding Feb 2003
UK Flooding 2000 06 Feb 2003 Britain has taken a battering from floods in the last 5 years, with major events in 1998 and 2000, significant floods in 2001 and minor events in each of the other years. So
More informationNatural Shoreline Landscapes on Michigan Inland Lakes
Natural Shoreline Landscapes on Michigan Inland Lakes Excerpts from Chapters 2 and 3 Photo Photo by Jane by Jane Herbert Herbert Did you know? Twenty-four species of amphibians, 25 species of reptiles,
More informationAQUATIC RESOURCES DELINEATION REFRESHER
AQUATIC RESOURCES DELINEATION REFRESHER James Jamie Robb Wetland Specialist, Office of the Chief 12 October 2016 US Army Corps of Engineers Ordinary High Water Mark (OHWM) How is the OHWM characterized
More informationSurface Processes Focus on Mass Wasting (Chapter 10)
Surface Processes Focus on Mass Wasting (Chapter 10) 1. What is the distinction between weathering, mass wasting, and erosion? 2. What is the controlling force in mass wasting? What force provides resistance?
More informationFavourable Condition of Blanket Bog on Peak District SSSIs. Richard Pollitt Lead Adviser, Conservation & Land Management, Dark and South West Peak
Favourable Condition of Blanket Bog on Peak District SSSIs Richard Pollitt Lead Adviser, Conservation & Land Management, Dark and South West Peak Definitions SSSI Site of Special Scientific Interest statutory
More informationWetlands and Riparian Mapping Framework Technical Meeting
Wetlands and Riparian Mapping Framework Technical Meeting Meghan Burns Landscape Ecologist Linda Vance Senior Ecologist Why wetland and riparian mapping? Preliminary site assessment for the presence of
More informationReview of Riparian Function Riparian Management Riparian Monitoring
Review of Riparian Function Riparian Management Riparian Monitoring Water Shed Water Catchment Water catching creek Water shedding creek Properly functioning riparian area Properly Functioning Riparian
More informationWisconsin s Hydrogeology: an overview
2012 Soil and Water Conservation Society Conference Stevens Point, WI Feb 9, 2012 Wisconsin s Hydrogeology: an overview Ken Bradbury Wisconsin Geological and Natural History Survey University of Wisconsin-Extension
More informationCHAPTER 6 & 7 VOCABULARY
CHAPTER 6 & 7 VOCABULARY 1. Biome 2. Climate 3. Latitude 4. Altitude 5. Emergent layer 6. Epiphyte 7. Understory 8. Permafrost 9. Wetland 10.Plankton 11.Nekton 12.Benthos 13.Littoral zone 14.Benthic zone
More informationPermafrost & climate change in northern Finland Dr Steve Gurney
Permafrost & climate change in northern Finland Dr Steve Gurney Senior Lecturer in Geomorphology University of Reading, UK Docent in cold climate geomorphology University of Turku, Finland Topics Introduction
More informationRepresentative Reference Area Akehurst, Venner meadow, Burnette lake, Fork meadow, paradise meadow, Rimrock swamp, Goose Carex,
Description This mixed sedge wetland community is the most common wetland type in BC s interior rangelands. These sedge species are able to tolerate anaerobic soil conditions for the entire growing season.
More informationA Help Guide for Using gssurgo to Find Potential Wetland Soil Landscapes
A Help Guide for Using gssurgo to Find Potential Wetland Soil Landscapes Wetland Mapping Consortium Webinar September 17, 2014 Dr. John M. Galbraith Crop & Soil Environmental Sciences Virginia Tech Wetland
More informationHaiti and Dominican Republic Flash Flood Initial Planning Meeting
Dr Rochelle Graham Climate Scientist Haiti and Dominican Republic Flash Flood Initial Planning Meeting September 7 th to 9 th, 2016 Hydrologic Research Center http://www.hrcwater.org Haiti and Dominican
More informationDirected Reading. Section: Types of Maps
Skills Worksheet Directed Reading Section: Types of Maps 1. What are some of the characteristics of an area shown on maps used by Earth scientists? a. types of animals, types of plants, types of minerals
More informationChiang Rai Province CC Threat overview AAS1109 Mekong ARCC
Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.
More information27. Running Water I (p ; )
27. Running Water I (p. 424-436; 440-444) Hydrosphere How much of the Earth s surface is covered by water? Earth's water is collectively called the and is stored in a number of so-called as follows: 1.
More informationChapter 52 An Introduction to Ecology and the Biosphere
Chapter 52 An Introduction to Ecology and the Biosphere Ecology The study of the interactions between organisms and their environment. Ecology Integrates all areas of biological research and informs environmental
More informationFresh Water: Streams, Lakes Groundwater & Wetlands
Fresh Water:, Lakes Groundwater & Wetlands Oct 27 Glaciers and Ice Ages Chp 13 Nov 3 Deserts and Wind and EXAM #3 Slope hydrologic cycle P = precip I = precip intercepted by veg ET = evapotranspiration
More informationOverview of fluvial and geotechnical processes for TMDL assessment
Overview of fluvial and geotechnical processes for TMDL assessment Christian F Lenhart, Assistant Prof, MSU Research Assoc., U of M Biosystems Engineering Fluvial processes in a glaciated landscape Martin
More informationLower South Fork McKenzie River Floodplain Enhancement Project
Lower South Fork McKenzie River Floodplain Enhancement Project McKenzie River Ranger District Willamette National Forest Project Location The project is located in the South Fork McKenzie River Watershed,
More informationSun, Moon, Hydrosphere Worksheet - Answers
Sun, Moon, Hydrosphere Worksheet - Answers Question 1 WHAT TERM CORRESPONDS TO EACH OF THE FOLLOWING DEFINITIONS? a) a landform, slope or terrain that can affect water circulation b) the Earth s blue envelope
More informationEcosystems Chapter 4. What is an Ecosystem? Section 4-1
Ecosystems Chapter 4 What is an Ecosystem? Section 4-1 Ecosystems Key Idea: An ecosystem includes a community of organisms and their physical environment. A community is a group of various species that
More informationAppendix E: Cowardin Classification Coding System
Appendix E: Cowardin Classification Coding System The following summarizes the Cowardin classification coding system and the letters and numbers used to define the USFWS NWI wetland types and subtypes:
More informationSTUDY GUIDE FOR CONTENT MASTERY. Surface Water Movement
Surface Water SECTION 9.1 Surface Water Movement In your textbook, read about surface water and the way in which it moves sediment. Complete each statement. 1. An excessive amount of water flowing downslope
More informationGeog Lecture 19
Geog 1000 - Lecture 19 Fluvial Geomorphology and River Systems http://scholar.ulethbridge.ca/chasmer/classes/ Today s Lecture (Pgs 346 355) 1. What is Fluvial Geomorphology? 2. Hydrology and the Water
More informationFluvial Systems Lab Environmental Geology Lab Dr. Johnson
Fluvial Systems Lab Environmental Geology Lab Dr. Johnson *Introductory sections of this lab were adapted from Pidwirny, M. (2006). "Streamflow and Fluvial Processes". Fundamentals of Physical Geography,
More informationDeveloping a Landscape-Level Reference Standard Wetland Profile for the Prairie Pothole Region, Montana
Developing a Landscape-Level Reference Standard Wetland Profile for the Prairie Pothole Region, Montana Prepared for: The U.S. Environmental Protection Agency Prepared by: Melissa Hart and Linda Vance
More information6.1 Water. The Water Cycle
6.1 Water The Water Cycle Water constantly moves among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth s water supply is the water cycle. The Water Cycle
More informationRivers T. Perron
1 Rivers T. Perron 12.001 After our discussions of large-scale topography, how we represent topography in maps, and how topography interacts with geologic structures, you should be frothing at the mouth
More informationIn the space provided, write the letter of the description that best matches the term or phrase. a. any form of water that falls to Earth s
Skills Worksheet Concept Review In the space provided, write the letter of the description that best matches the term or phrase. 1. condensation 2. floodplain 3. watershed 4. tributary 5. evapotranspiration
More informationThank you to all of our 2015 sponsors: Media Partner
Thank you to all of our 2015 sponsors: Media Partner Fluvial System Concepts and Their Application in Greenfield Stream Corridor Realignment Dr. Paul Villard, P.Geo. GEO Morphix Ltd. Overview Major realignment
More informationSimulating the groundwater discharge to wetlands. Mukwonago Basin Example and Potential Application in Dane County
Simulating the groundwater discharge to wetlands Mukwonago Basin Example and Potential Application in Dane County Conceptual Model Topography is major control on flow to wetlands Land Surface Water Table
More informationKarr J.R. and D.R. Dudley Ecological perspective on water quality goals. Environmental Manager 5:55-68.
Ecological Integrity Assessment: An Approach for Assessing Ecosystem Condition to Guide Conservation and Management Ecological Integrity " the ability of an ecosystem to support and maintain i a balanced
More informationWetlands in a Watershed/Landscape Context Vegetation & Wildlife August 15, Kendra Moseley, Regional ESS, Soil Science Division
Wetlands in a Watershed/Landscape Context Vegetation & Wildlife August 15, 2018 - Kendra Moseley, Regional ESS, Soil Science Division Vegetation in Wetlands Vegetation as an Indicator of Hydrology Vegetation
More informationImaging Critical Zone Processes
Imaging Critical Zone Processes Kamini Singha Hydrologic Science and Engineering Colorado School of Mines With contributions from: Xavier Comas, Jorden Hayes, and Andy Parsekian Key critical zone processes
More information12 10 8 6 4 2 0 40-50 50-60 60-70 70-80 80-90 90-100 Fresh Water What we will cover The Hydrologic Cycle River systems Floods Groundwater Caves and Karst Topography Hot springs Distribution of water in
More informationVEGETATION EVA BOEHRINGER
VEGETATION EVA BOEHRINGER April 2, 2014 WUP CONSULTATIVE COMMITTEE WUP Consultative Committee (WUP CC) recognized that riparian and wetland vegetation in the reservoir drawdown zone is valuable for fish,
More informationDistinct landscape features with important biologic, hydrologic, geomorphic, and biogeochemical functions.
1 Distinct landscape features with important biologic, hydrologic, geomorphic, and biogeochemical functions. Have distinguishing characteristics that include low slopes, well drained soils, intermittent
More information2. Irrigation. Key words: right amount at right time What if it s too little too late? Too much too often?
2. Irrigation Key words: right amount at right time What if it s too little too late? 2-1 Too much too often? To determine the timing and amount of irrigation, we need to calculate soil water balance.
More informationSTREAM SYSTEMS and FLOODS
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Runoff Transpiration Earth s Water and the Hydrologic Cycle The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationPrecipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle Runoff Transpiration The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationLecture 29: Soil Formation
Lecture 29: Soil Formation Factors Controlling Soil Formation 1. Parent material: Soil precursor 2. Climate: Temperature and precipitation 3. Biota: Native vegetation, microbes, soil animals, humans 4.
More informationCrows Landing Naval Base Easement
1 of 15 West Stanislaus Resource Conservation District Crows Landing Naval Base Easement Annual Reserve Monitoring Report Jamie McFarlin 11/112012 2 of 15 West Stanislaus Resource Conservation District
More informationMarl Prairie vegetation response to 20th century land use and its implications for management in the Everglades
Marl Prairie vegetation response to 20th century land use and its implications for management in the Everglades C. Bernhardt, D. Willard, B. Landacre US Geological Survey Reston, VA USA U.S. Department
More informationCatastrophic Events Impact on Ecosystems
Catastrophic Events Impact on Ecosystems Hurricanes Hurricanes An intense, rotating oceanic weather system with sustained winds of at least 74 mph and a welldefined eye Conditions for formation: Warm water
More informationA hydrological study of Waen y Griafolen blanket bog, North Wales
A hydrological study of Waen y Griafolen blanket bog, North Wales GRAHAM HALL, ROGER CRATCHLEY & SARAH JOHNSON Centre for Arid Zone Studies, School of Agricultural and Forest Sciences, University of Wales,
More informationEcology 312 SI STEVEN F. Last Session: Aquatic Biomes, Review This Session: Plate Tectonics, Lecture Quiz 2
Ecology 312 SI STEVEN F. Last Session: Aquatic Biomes, Review This Session: Plate Tectonics, Lecture Quiz 2 Questions? Warm up: KWL KNOW: On a piece of paper, write down things that you know well enough
More informationInfluence of the Major Drainages to the Mississippi River and Implications for System Level Management
Influence of the Major Drainages to the Mississippi River and Implications for System Level Management Brian M. Vosburg Geologist Louisiana Coastal Protection and Restoration Authority brian.vosburg@la.gov
More informationBright blue marble floating in space. Biomes & Ecology
Bright blue marble floating in space Biomes & Ecology Chapter 50 Spheres of life Molecules Cells (Tissues Organ Organ systems) Organisms Populations Community all the organisms of all the species that
More informationThe Effect of Weather, Erosion, and Deposition in Texas Ecoregions
The Effect of Weather, Erosion, and Deposition in Texas Ecoregions 7.8B: I can analyze the effects of weathering, erosion, and deposition on the environment in ecoregions of Texas Weathering The breakdown
More informationSAN FRANCISCO DISTRICT INFORMATION REQUESTED FOR VERIFICATION OF CORPS JURISDICTION
DEPARTMENT OF THE ARMY SAN FRANCISCO DISTRICT, U.S. ARMY CORPS OF ENGINEERS 1455 MARKET STREET SAN FRANCISCO, CALIFORNIA 94103-1398 SAN FRANCISCO DISTRICT INFORMATION REQUESTED FOR VERIFICATION OF CORPS
More informationYear 6. Geography. Revision
Year 6 Geography Revision November 2017 Rivers and World knowledge How the water cycle works and the meaning of the terms evaporation, condensation, precipitation, transpiration, surface run-off, groundwater
More informationNational Atlas of Groundwater Dependent Ecosystems (GDE)
National Atlas of Groundwater Dependent Ecosystems (GDE) Dr. Zaffar Sadiq Mohamed-Ghouse Executive Consultant & Practice Head-Spatial SKM, Australia zsadiq@globalskm.com Geospatial World Forum 2013, Rotterdam,
More informationUNIT 5: ECOLOGY Chapter 15: The Biosphere
CORNELL NOTES Directions: You must create a minimum of 5 questions in this column per page (average). Use these to study your notes and prepare for tests and quizzes. Notes will be stamped after each assigned
More informationFactors influencing nutrient and sediment retention by riverine wetlands in the Chesapeake watershed Greg Noe, Cliff Hupp, Ed Schenk, Nancy Rybicki
Factors influencing nutrient and sediment retention by riverine wetlands in the Chesapeake watershed Greg Noe, Cliff Hupp, Ed Schenk, Nancy Rybicki National Research Program, Reston VA U.S. Department
More informationRANGE AND ANIMAL SCIENCES AND RESOURCES MANAGEMENT - Vol. II - Catchment Management A Framework for Managing Rangelands - Hugh Milner
CATCHMENT MANAGEMENT A FRAMEWORK FOR MANAGING RANGELANDS Hugh Milner International Water Management Consultant, Australia Keywords: Rangeland management; catchments and watersheds; catchment management
More informationEcoregions Glossary. 7.8B: Changes To Texas Land Earth and Space
Ecoregions Glossary Ecoregions The term ecoregions was developed by combining the terms ecology and region. Ecology is the study of the interrelationship of organisms and their environments. The term,
More informationWhat is a water table? What is an aquifer? What is the difference between a spring and a well?
CHAPTER 11 3 Water Underground SECTION The Flow of Fresh Water BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a water table? What is an aquifer? What
More information2012 Rainfall, Runoff, Water Level & Temperature Beebe Lake Wright County, MN (# )
www.fixmylake.com 18029 83 rd Avenue North Maple Grove, MN 55311 mail@freshwatersci.com (651) 336-8696 2012 Rainfall, Runoff, Water Level & Temperature Beebe Lake Wright County, MN (#86-0023) Prepared
More information3.11 Floodplains Existing Conditions
Other stormwater control practices may be needed to mitigate water quality impacts. In addition to detention facilities, other practices such as vegetated basins/buffers, infiltration basins, and bioswales
More information3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e
Introduction to Environmental Geology, 5e Running Water: summary in haiku form Edward A. Keller Chapter 9 Rivers and Flooding Lecture Presentation prepared by X. Mara Chen, Salisbury University The hydro
More informationHow to integrate wetland processes in river basin modeling? A West African case study
How to integrate wetland processes in river basin modeling? A West African case study stefan.liersch@pik-potsdam.de fred.hattermann@pik-potsdam.de June 2011 Outline Why is an inundation module required?
More informationSUPPLEMENTARY MATERIAL
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 SUPPLEMENTARY MATERIAL Hoset KS, Ruffino L, Tuomi M, Oksanen T, Oksanen L, Mäkynen A, Johansen B and Moe T. Changes in the spatial configuration and strength
More informationWhich map shows the stream drainage pattern that most likely formed on the surface of this volcano? A) B)
1. When snow cover on the land melts, the water will most likely become surface runoff if the land surface is A) frozen B) porous C) grass covered D) unconsolidated gravel Base your answers to questions
More informationSESSION 6: FLUVIAL LANDFORMS
SESSION 6: FLUVIAL LANDFORMS KEY CONCEPTS: Fluvial Landforms Management of River Catchment Areas Slope Elements X-PLANATION: FLUVIAL LANDFORMS Rivers form landforms as they erode the landscape. These landforms
More informationEcology. Ecology terminology Biomes Succession Energy flow in ecosystems Loss of energy in a food chain
Ecology Ecology terminology Biomes Succession Energy flow in ecosystems Loss of energy in a food chain Terminology Ecology- the study of the interactions of living organisms with one another and with their
More information12 SWAT USER S MANUAL, VERSION 98.1
12 SWAT USER S MANUAL, VERSION 98.1 CANOPY STORAGE. Canopy storage is the water intercepted by vegetative surfaces (the canopy) where it is held and made available for evaporation. When using the curve
More informationObservations on Surface Water in the Seminary Fen in Spring, Prepared 6/4/13 by Sam Wetterlin; updated 7/28/13
Observations on Surface Water in the Seminary Fen in Spring, 2013 Prepared 6/4/13 by Sam Wetterlin; updated 7/28/13 Ordinarily, a calcareous fen is primarily dependent on upwelling mineral-rich, oxygen-poor
More informationChapter 7 Part III: Biomes
Chapter 7 Part III: Biomes Biomes Biome: the major types of terrestrial ecosystems determined primarily by climate 2 main factors: Temperature and precipitation Depends on latitude or altitude; proximity
More informationEnvironmental Science
Environmental Science A Study of Interrelationships Cui Jiansheng Hebei University of Science and Technology CH06 Kinds of Ecosystems and Communities Chapter Objectives After reading this chapter, you
More informationChapter 13. Groundwater
Chapter 13 Groundwater Introduction Groundwater is all subsurface water that completely fills the pores and other open spaces in rocks, sediments, and soil. Groundwater is responsible for forming beautiful
More information2.6.3 Forms of standing open water
Fig. 33 Distinctive forms created by oioi restiad rushland, New River Estuary, Southland. These pikelets are elevating themselves above the level of mudflats and tidal channels as the rushes trap sediment.
More informationFlash flood disaster in Bayangol district, Ulaanbaatar
Flash flood disaster in Bayangol district, Ulaanbaatar Advanced Training Workshop on Reservoir Sedimentation Management 10-16 October 2007. IRTCES, Beijing China Janchivdorj.L, Institute of Geoecology,MAS
More informationUpper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California
Upper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California Mike Rudd (Project Manager), Charley Miller & Chad Krofta Declines in Tahoe s Water Clarity The
More information