Grade 2 at Home Learning the Learning This Week Will Focus on a Cross-Curriculum Approach in Reading/Writing, Mathematics and Science
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Freshwater Ecosystems and Biodiversity
Network of Conservation Educators & Practitioners Freshwater Ecosystems and Biodiversity Author(s): Nathaniel P. Hitt, Lisa K. Bonneau, Kunjuraman V. Jayachandran, and Michael P. Marchetti Source: Lessons in Conservation, Vol. 5, pp. 5-16 Published by: Network of Conservation Educators and Practitioners, Center for Biodiversity and Conservation, American Museum of Natural History Stable URL: ncep.amnh.org/linc/ This article is featured in Lessons in Conservation, the official journal of the Network of Conservation Educators and Practitioners (NCEP). NCEP is a collaborative project of the American Museum of Natural History’s Center for Biodiversity and Conservation (CBC) and a number of institutions and individuals around the world. Lessons in Conservation is designed to introduce NCEP teaching and learning resources (or “modules”) to a broad audience. NCEP modules are designed for undergraduate and professional level education. These modules—and many more on a variety of conservation topics—are available for free download at our website, ncep.amnh.org. To learn more about NCEP, visit our website: ncep.amnh.org. All reproduction or distribution must provide full citation of the original work and provide a copyright notice as follows: “Copyright 2015, by the authors of the material and the Center for Biodiversity and Conservation of the American Museum of Natural History. All rights reserved.” Illustrations obtained from the American Museum of Natural History’s library: images.library.amnh.org/digital/ SYNTHESIS 5 Freshwater Ecosystems and Biodiversity Nathaniel P. Hitt1, Lisa K. Bonneau2, Kunjuraman V. Jayachandran3, and Michael P. Marchetti4 1U.S. Geological Survey, Leetown Science Center, USA, 2Metropolitan Community College-Blue River, USA, 3Kerala Agricultural University, India, 4School of Science, St. -
Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: a Critical Review of Current Knowledge
Utah State University DigitalCommons@USU All Graduate Plan B and other Reports Graduate Studies 12-2013 Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge Danielle Barandiaran Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/gradreports Part of the Soil Science Commons Recommended Citation Barandiaran, Danielle, "Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge" (2013). All Graduate Plan B and other Reports. 332. https://digitalcommons.usu.edu/gradreports/332 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Plan B and other Reports by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. METHYLMERCURY FATE IN THE HYPERSALINE ENVIRONMENT OF THE GREAT SALT LAKE: A CRITICAL REVIEW OF CURRENT KNOWLEDGE By Danielle Barandiaran A paper submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Soil Science Approved: Astrid Jacobson Jeanette Norton Major Professor Committee Member - Paul Grossl Teryl Roper Committee Member Department Head UTAH STATE UNIVERSITY Logan, Utah 2013 Copyright © Danielle Barandiaran 2013 All Rights Reserved iii ABSTRACT Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge by Danielle Barandiaran, Master of Science Utah State University, 2013 Major Professor: Dr. Astrid R. Jacobson Department: Plants, Soils & Climate Methylmercury (MeHg) is a highly potent neurotoxic form of the environmental pollutant Mercury (Hg). -
The Great Salt Lake Osmotic Power Potential
The Great Salt Lake Osmotic Power Potential Maher Kelada MIK Technology 2100 West Loop South, Suite 900 Houston, Texas, USA 77027 [email protected] Abstract: This is a proposal to develop a new source of renewable energy relying on hypersaline osmotic power generation technology that has been developed by MIK Technology, potentially for generating up to 400 megawatts of sustainable power from the Great Salt Lake, Utah, operating isothermally without generating any emissions. The proposed technology would reduce Utah State’s demand for coal by 10% or natural gas by 50%, using a clean and safe renewable source of energy. I. Osmotic Power Generation Concept Osmosis is nature’s gift to life. It is the vehicle that transports fluids in all living cells and without it, all biological functions and all forms of life cease to exist! Osmosis is the spontaneous movement of water, through a semi-permeable membrane that is permeable to water but impermeable to solute. Water moves from a solution in which solute is less concentrated to a solution in which solute is more concentrated. The driving force of the flow movement is the difference in the chemical potential on the two sides of the semi-permeable membrane, with the solvent moving from a region of higher potential (generally of a lower solute concentration) to the region of lower potential (generally of a higher solute concentration). The term “Chemical Potential” at times can be ambiguous and elusive. In fact, it is one of the most important partial molal quantities. It is the energy source associated with the activity of the ions of an ionizable substance. -
Water on Earth (Pages 392–395) Key Concept
Name Date Class Fresh Water ■ Adapted Reading and Study Water on Earth (pages 392–395) The Water Cycle (pages 392–393) Key Concept: In the water cycle, water moves from bodies of water, land, and living things on Earth’s surface to the atmosphere and back to Earth’s surface. • The water cycle is how water moves from Earth’s surface to the atmosphere and back again. The water cycle never stops. It has no beginning or end. • The sun is the source of energy for the water cycle. • Water evaporates from Earth’s surface. Water is always evaporating from oceans and lakes. Water is given off by plants as water vapor. • When water vapor in the air cools, it condenses. The result of this condensation is clouds. • From clouds, water falls back to Earth as precipitation. Precipitation is water that falls to Earth as rain, snow, hail, or sleet. • If the precipitation falls on land, it may soak into the soil. Or, it may run off into rivers and lakes. Answer the following questions. Use your textbook and the ideas above. 1. The process by which water moves from Earth’s surface to the atmosphere and back again is the . 2. Water that falls to Earth as rain, snow, hail, or Fresh Water Fresh sleet is called . © Pearson Education, Inc., publishing as Pearson Prentice Hall. All rights reserved. 185 Name Date Class Fresh Water ■ Adapted Reading and Study 3. Circle the letter of each sentence that is true about the water cycle. a. The water cycle begins with the formation of clouds. -
Lesson 4: Sediment Deposition and River Structures
LESSON 4: SEDIMENT DEPOSITION AND RIVER STRUCTURES ESSENTIAL QUESTION: What combination of factors both natural and manmade is necessary for healthy river restoration and how does this enhance the sustainability of natural and human communities? GUIDING QUESTION: As rivers age and slow they deposit sediment and form sediment structures, how are sediments and sediment structures important to the river ecosystem? OVERVIEW: The focus of this lesson is the deposition and erosional effects of slow-moving water in low gradient areas. These “mature rivers” with decreasing gradient result in the settling and deposition of sediments and the formation sediment structures. The river’s fast-flowing zone, the thalweg, causes erosion of the river banks forming cliffs called cut-banks. On slower inside turns, sediment is deposited as point-bars. Where the gradient is particularly level, the river will branch into many separate channels that weave in and out, leaving gravel bar islands. Where two meanders meet, the river will straighten, leaving oxbow lakes in the former meander bends. TIME: One class period MATERIALS: . Lesson 4- Sediment Deposition and River Structures.pptx . Lesson 4a- Sediment Deposition and River Structures.pdf . StreamTable.pptx . StreamTable.pdf . Mass Wasting and Flash Floods.pptx . Mass Wasting and Flash Floods.pdf . Stream Table . Sand . Reflection Journal Pages (printable handout) . Vocabulary Notes (printable handout) PROCEDURE: 1. Review Essential Question and introduce Guiding Question. 2. Hand out first Reflection Journal page and have students take a minute to consider and respond to the questions then discuss responses and questions generated. 3. Handout and go over the Vocabulary Notes. Students will define the vocabulary words as they watch the PowerPoint Lesson. -
The Importance of the Salton Sea and Other Terminal Lakes in Supporting
The Importance of the Salton Sea and Other Terminal Lakes in Supporting Birds of the Pacific Flyway Terminal lakes, so called because they have no outlet, are characteristic water features of the Great Basin of the Intermountain West. Through the process of continued evaporation, minerals and salts that flow into these water bodies are retained and concentrated over time. The salinity of the water varies considerably among terminal lakes, depending on the quality of the source water and the length of time the lake has been in existence. Several of these, including the Great Salt Lake, Mono Lake, and the Salton Sea, have become more saline than the ocean. While all of these lakes support unique physical characteristics and aquatic ecosystems, one characteristic common to all is the importance they play in sustaining birds using the Pacific Flyway and portions of the Central Flyway. Physical and Biological Characteristics of Terminal Lakes in the West Terminal lakes along the Pacific Flyway (Exhibit 1) vary widely in their physical and biological characteristics. Elevations range from 6,381 feet at Mono Lake to -227 feet at the Salton Sea. They also vary greatly in depth and salinity, as shown in Exhibits 2 and 3. Most of these lakes are shallow with seasonal water input and high evaporation in the summer. Water quality is typically characterized by hard water and saline conditions, an artifact of dissolved constituents accumulating and increasing in concentration over time. While water quality in terminal lakes limits the diversity of the aquatic community to salt-tolerant organisms, these lakes often are very productive, and provide an ample food supply for waterbirds. -
Geologic Site of the Month: Why Is Sebago Lake So Deep?
Why is Sebago Lake so deep? Maine Geological Survey Maine Geologic Facts and Localities February, 1999 Why is Sebago Lake so deep? 43° 51‘ 13.36“ N, 70° 33‘ 43.98“ W Text by Robert A. Johnston Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Why is Sebago Lake so deep? Maine Geological Survey Introduction Modern geophysical equipment allows geologists to investigate previously unmapped environments, including ocean and lake floors. Recent geophysical research studied the types, composition, areal extent, and thickness of sediments on the bottom of Sebago Lake in southwestern Maine. Geologists used side- scan sonar and seismic reflection profiling to map the bottom of the lake. Approximately 58 percent of the lake bottom was imaged with side-scan sonar and over 60 miles of seismic reflection profiles were collected. This web site will discuss the findings of the seismic reflection profiling. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Why is Sebago Lake so deep? Maine Geological Survey Physiographic setting Sebago Lake, although second in surface area to Moosehead Lake, is Maine's deepest lake. With a water depth of 316 feet, its deepest part is 49 feet below sea level! Sebago Lake is located in southwestern Maine 20 miles northwest of Portland and 50 miles southeast of the White Mountains. It lies along the transition between the Central Highlands and the Coastal Lowlands physiographic regions of New England (Figure 1). The abrupt change in landscape can be seen in panoramic views from several vantage points near Sebago Lake. Denny, 1982 Denny, Maine Geological Survey From From Figure 1. -
The Arkansas River Flood of June 3-5, 1921
DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE 0ns SMITH, Director Water-Supply Paper 4$7 THE ARKANSAS RIVER FLOOD OF JUNE 3-5, 1921 BY ROBERT FOLLANS^EE AND EDWARD E. JON^S WASHINGTON GOVERNMENT PRINTING OFFICE 1922 i> CONTENTS. .Page. Introduction________________ ___ 5 Acknowledgments ___ __________ 6 Summary of flood losses-__________ _ 6 Progress of flood crest through Arkansas Valley _____________ 8 Topography of Arkansas basin_______________ _________ 9 Cause of flood______________1___________ ______ 11 Principal areas of intense rainfall____ ___ _ 15 Effect of reservoirs on the flood__________________________ 16 Flood flows_______________________________________ 19 Method of determination________________ ______ _ 19 The flood between Canon City and Pueblo_________________ 23 The flood at Pueblo________________________________ 23 General features_____________________________ 23 Arrival of tributary flood crests _______________ 25 Maximum discharge__________________________ 26 Total discharge_____________________________ 27 The flood below Pueblo_____________________________ 30 General features _________ _______________ 30 Tributary streams_____________________________ 31 Fountain Creek____________________________ 31 St. Charles River___________________________ 33 Chico Creek_______________________________ 34 Previous floods i____________________________________ 35 Flood of Indian legend_____________________________ 35 Floods of authentic record__________________________ 36 Maximum discharges -
Stream Restoration, a Natural Channel Design
Stream Restoration Prep8AICI by the North Carolina Stream Restonltlon Institute and North Carolina Sea Grant INC STATE UNIVERSITY I North Carolina State University and North Carolina A&T State University commit themselves to positive action to secure equal opportunity regardless of race, color, creed, national origin, religion, sex, age or disability. In addition, the two Universities welcome all persons without regard to sexual orientation. Contents Introduction to Fluvial Processes 1 Stream Assessment and Survey Procedures 2 Rosgen Stream-Classification Systems/ Channel Assessment and Validation Procedures 3 Bankfull Verification and Gage Station Analyses 4 Priority Options for Restoring Incised Streams 5 Reference Reach Survey 6 Design Procedures 7 Structures 8 Vegetation Stabilization and Riparian-Buffer Re-establishment 9 Erosion and Sediment-Control Plan 10 Flood Studies 11 Restoration Evaluation and Monitoring 12 References and Resources 13 Appendices Preface Streams and rivers serve many purposes, including water supply, The authors would like to thank the following people for reviewing wildlife habitat, energy generation, transportation and recreation. the document: A stream is a dynamic, complex system that includes not only Micky Clemmons the active channel but also the floodplain and the vegetation Rockie English, Ph.D. along its edges. A natural stream system remains stable while Chris Estes transporting a wide range of flows and sediment produced in its Angela Jessup, P.E. watershed, maintaining a state of "dynamic equilibrium." When Joseph Mickey changes to the channel, floodplain, vegetation, flow or sediment David Penrose supply significantly affect this equilibrium, the stream may Todd St. John become unstable and start adjusting toward a new equilibrium state. -
Implications for Management AFRICAN GREAT LAKES
AFRICAN GREAT LAKES CONFERENCE 2nd – 5th MAY 2017, ENTEBBE, UGANDA Dynamics of Fish Stocks of Commercial Importance in Lake Victoria, East Africa: Implications for Management Robert Kayanda, Anton Taabu-Munyaho, Dismas Mbabazi, Hillary Mrosso, and Chrisphine Nyamweya INTRODUCTION • Lake Victoria with a surface area of 68,800 sqkm is the world’s second largest freshwater body • It supports one of the world’s most productive inland fisheries with the estimated total fish landings from the lake for the period of 2011 to 2014 have been about 1 million tons with a beach value increasing from about US$ 550 Million in 2011 to about US$ 840 million in 2014. • It supports about 220,000 fishers (Frame Survey 2016) • The fish stocks of Lake Victoria have changed dramatically since the introduction of Nile perch Lates niloticus during the late 1950s and early 1960s Fishery Haplochromines The Original Fish Fauna Brycinus sp Protopterus Rastrineobola Mormyrus spp Barbus spp Bagrus docmac Labeo Schilbe intermedius Oreochromis variabilis Clarias gariepinus Mormyrus spp Synodontis victoriae Oreochromis leucostictus INTRODUCTION Currently, the fisheries is dominated by four major commercial important species, these are; •Nile perch •Dagaa •Nile tilapia •Haplochromis Apart from Nile tilapia only estimated through trawl and catch surveys, the other 3 are estimated through trawl, acoustics, and catch INTRODUCTION This paper summarizes current knowledge of the status of the fish stocks and reviews the need for species specific management plans for the major commercial important fish species of Lake Victoria (Nile perch, Nile tilapia, dagaa and haplochromines). Methods • Fisheries dependent – Frame surveys – Catch assessment surveys • Fisheries independent – Acoustic – Bottom trawl Biomass and relative abundance • Total biomass from the surveys 3500 remained fairly stable over time. -
The End of the Holocene Humid Period in the Central Sahara and Thar Deserts: Societal Collapses Or New Opportunities? Andrea Zerboni1, S
60 SCIENCE HIGHLIGHTS: CLIMATE CHANGE AND CULTURAL EVOLUTION doi: 10.22498/pages.24.2.60 The end of the Holocene Humid Period in the central Sahara and Thar deserts: societal collapses or new opportunities? Andrea Zerboni1, S. biagetti2,3,4, c. Lancelotti2,3 and M. Madella2,3,5 The end of the Holocene Humid Period heavily impacted on human societies, prompting the development of new forms of social complexity and strategies for food security. Yearly climatic oscillations played a role in enhancing the resilience of past societies. The Holocene Humid Period or Holocene settlements (Haryana, India), show a general changes in settlement pattern, rather than full- climatic Optimum (ca. 12–5 ka bP), in its local, trend towards desertification and higher fledged abandonment. monsoon-tuned variants of the African Humid evapotranspiration between 5.8 and 4.2 ka bP, Period (DeMenocal et al. 2000; Gasse 2000) followed by an abrupt increase in δ18O values In the SW Fazzan, the transition from the Late and the period of strong Asian southwest (or and relative abundance of carbonates, indic- Pastoral (5-3.5 ka bP) to the Final Pastoral summer) monsoon (Dixit et al. 2014), is one ative of a sudden decrease in Indian summer (3.5-2.7 ka bP) marks the ultimate adaptation of the best-studied climatic phases of the monsoon precipitations (Dixit et al. 2014). to hyperarid conditions and, later, the rise Holocene. Yet the ensuing trend towards arid- of the Garamantian kingdom (2.7-1.5 ka bP; ity, the surface processes shaping the pres- Aridification and cultural processes Mori et al. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic