Sand Dune Stabilization
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Review Article Biological Method in Stabilization of Sand Dunes Using the Ornamental Plants and Woody Trees: Review Article
Journal of Innovations in Pharmaceuticals and Biological Sciences JIPBS www.jipbs.com ISSN: 2349-2759 Review article Biological method in stabilization of sand dunes using the ornamental plants and woody trees: Review article Metwally S.A.*1, Abouziena H.F.2, Bedour M.H. Abou- Leila3, M.M. Farahat1, E. El. Habba1 1Department of Ornamental Plants and Woody Trees, National Research Centre, Dokki, Cairo, Egypt, 12622. 2Department of Botany, National Research Centre, Dokki, Cairo, Egypt, 12622. 3 Department of Water Relation and Field irrigation, National Research Centre, Dokki, Cairo, Egypt, 12622. Abstract Sand dunes are considered one of the most obstacles that face the horizontal or vertical expansion of agriculture in the desert. Sand dunes are a collection of a loose grouping of sand on the land surface in the form of a pile with top. In the recent years, increasing attention has been taken to cultivate the timber trees and ornamental plants in a narrow range to combat the desertification, sand encroachment and sand dunes. The climate factors are characterized by high temperature, strong winds laden with sand and sandy dunes, lead to soil erosion and remove the fertility soil in the surface layer, and destroying cultivated lands. Therefore, it's important to planting windbreaks and stabilization sand dunes to reduce the damage and loss of all areas of development aspects. The methods used for combating the sand dunes can be classified into two types; biological methods or plant measure and the second are the mechanical methods or engineering measure. We will focus in this article on the biological methods where the trees, shrubs and grasses are planted. -
Sand Dune Systems in Iran - Distribution and Activity
Sand Dune Systems in Iran - Distribution and Activity. Wind Regimes, Spatial and Temporal Variations of the Aeolian Sediment Transport in Sistan Plain (East Iran) Dissertation Thesis Submitted for obtaining the degree of Doctor of Natural Science (Dr. rer. nat.) i to the Fachbereich Geographie Philipps-Universität Marburg by M.Sc. Hamidreza Abbasi Marburg, December 2019 Supervisor: Prof. Dr. Christian Opp Physical Geography Faculty of Geography Phillipps-Universität Marburg ii To my wife and my son (Hamoun) iii A picture of the rock painting in the Golpayegan Mountains, my city in Isfahan province of Iran, it is written in the Sassanid Pahlavi line about 2000 years ago: “Preserve three things; water, fire, and soil” Translated by: Prof. Dr. Rasoul Bashash, Photo: Mohammad Naserifard, winter 2004. Declaration by the Author I declared that this thesis is composed of my original work, and contains no material previously published or written by another person except where due reference has been made in the text. I have clearly stated the contribution by others to jointly-authored works that I have included in my thesis. Hamidreza Abbasi iv List of Contents Abstract ................................................................................................................................................. 1 1. General Introduction ........................................................................................................................ 7 1.1 Introduction and justification ........................................................................................................ -
Komandorsky Zapovednik: Strengthening Community Reserve Relations on the Commander Islands
No. 36 Summer 2004 Special issue: Russia’s Marine Protected Areas PROMOTING BIODIVERSITY CONSERVATION IN RUSSIA AND THROUGHOUT NORTHERN EURASIA CONTENTS CONTENTS Voice from the Wild (A letter from the editors)......................................1 Komandorsky Zapovednik: Strengthening Community Reserve Relations on the Commander Islands......................................24 AN INTRODUCTION TO MARINE Lazovsky Zapovednik: PROTECTED AREAS Working to Create a Marine Buffer Zone...................................................28 MPAs: An Important Tool in Marine Conservation......…………………...2 Kurshskaya Kosa National Park: Tides of Change: Tracing the Development Preserving World Heritage on the Baltic Sea ..........................................30 of Marine Protected Areas in Russia .................................................................4 Dalnevostochny Morskoi Zapovednik: How Effective Are Our MPAs? Looking for Answers An Important Role to Play.........................................................................................6 with Russia’s First Marine Protected Area..................................................32 The Challenges that Lie Ahead.....................………………………………………………8 Russia’s Marine Biosphere Reserves......………………………………………………10 MPA Workshop Offers Opportunities for Dialogue..........................13 THE FUTURE Plans for the Future: Developing a Network of Marine Protected Areas .....................................................……....………………...35 CASE STUDIES An Introduction .............................................................................……....………………...14 -
Status and Protection of Globally Threatened Species in the Caucasus
STATUS AND PROTECTION OF GLOBALLY THREATENED SPECIES IN THE CAUCASUS CEPF Biodiversity Investments in the Caucasus Hotspot 2004-2009 Edited by Nugzar Zazanashvili and David Mallon Tbilisi 2009 The contents of this book do not necessarily reflect the views or policies of CEPF, WWF, or their sponsoring organizations. Neither the CEPF, WWF nor any other entities thereof, assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, product or process disclosed in this book. Citation: Zazanashvili, N. and Mallon, D. (Editors) 2009. Status and Protection of Globally Threatened Species in the Caucasus. Tbilisi: CEPF, WWF. Contour Ltd., 232 pp. ISBN 978-9941-0-2203-6 Design and printing Contour Ltd. 8, Kargareteli st., 0164 Tbilisi, Georgia December 2009 The Critical Ecosystem Partnership Fund (CEPF) is a joint initiative of l’Agence Française de Développement, Conservation International, the Global Environment Facility, the Government of Japan, the MacArthur Foundation and the World Bank. This book shows the effort of the Caucasus NGOs, experts, scientific institutions and governmental agencies for conserving globally threatened species in the Caucasus: CEPF investments in the region made it possible for the first time to carry out simultaneous assessments of species’ populations at national and regional scales, setting up strategies and developing action plans for their survival, as well as implementation of some urgent conservation measures. Contents Foreword 7 Acknowledgments 8 Introduction CEPF Investment in the Caucasus Hotspot A. W. Tordoff, N. Zazanashvili, M. Bitsadze, K. Manvelyan, E. Askerov, V. Krever, S. Kalem, B. Avcioglu, S. Galstyan and R. Mnatsekanov 9 The Caucasus Hotspot N. -
Sand Dunes Computer Animations and Paper Models by Tau Rho Alpha*, John P
Go Home U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Sand Dunes Computer animations and paper models By Tau Rho Alpha*, John P. Galloway*, and Scott W. Starratt* Open-file Report 98-131-A - This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this program has been used by the U.S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith. * U.S. Geological Survey Menlo Park, CA 94025 Comments encouraged tralpha @ omega? .wr.usgs .gov [email protected] [email protected] (gobackward) <j (goforward) Description of Report This report illustrates, through computer animations and paper models, why sand dunes can develop different forms. By studying the animations and the paper models, students will better understand the evolution of sand dunes, Included in the paper and diskette versions of this report are templates for making a paper models, instructions for there assembly, and a discussion of development of different forms of sand dunes. In addition, the diskette version includes animations of how different sand dunes develop. Many people provided help and encouragement in the development of this HyperCard stack, particularly David M. Rubin, Maura Hogan and Sue Priest. -
Sand Dune Stabilization and Reclamation in Southeastern Colorado
Sand Dune Stabilization And Reclamation In Southeastern Colorado Mike Scharp Parker Ag Services, LLC 4570 Kashmire Drive Colorado Springs, CO 80920 ABSTRACT This paper will discuss how and why Enviro-Gro Technologies (EGT) developed a large- scale sand dune reclamation program using New York City biosolids. The biosolids were applied during the winter of 1992 and 1993. The application site is located about 25 miles east of Lamar, CO and is comprised of 258 acres. Reclamation of the site resulted in its stabilization because vegitation was established on the site thus eliminating the encroachment into other areas. Based upon experience and negotiation with the Colorado Department of Public Health and Environment (CDPH&E) and the United State Environmental Protection Agency (USEPA) an application rate of 30 dry tons per acre was permitted. In addition, 10 dry tons per acre of woodchips were co-applied. The intent was that the excess carbon would bind some of nitrogen on the site and thus limit the amount of nitrogen that would leach from the site. Although data indicates that alternative application rates of 10 and 20 dry tons per acre of biosolids were applied for demonstration purposes, little data exist regarding these parcels. Therefore, this paper will deal with the main part of the site where 30 dry tons per acre of biosolids was applied. BACKGROUND Enviro-Gro Technologies began April 22, 1992 applying New York City biosolids near Lamar, CO. Typically about 150 wet tons of biosolids were land applied on privately owned dry land winter wheat. The average application rate was of 2.0 dry tons per acre. -
Types of Landslides.Indd
Landslide Types and Processes andslides in the United States occur in all 50 States. The primary regions of landslide occurrence and potential are the coastal and mountainous areas of California, Oregon, Land Washington, the States comprising the intermountain west, and the mountainous and hilly regions of the Eastern United States. Alaska and Hawaii also experience all types of landslides. Landslides in the United States cause approximately $3.5 billion (year 2001 dollars) in dam- age, and kill between 25 and 50 people annually. Casualties in the United States are primar- ily caused by rockfalls, rock slides, and debris flows. Worldwide, landslides occur and cause thousands of casualties and billions in monetary losses annually. The information in this publication provides an introductory primer on understanding basic scientific facts about landslides—the different types of landslides, how they are initiated, and some basic information about how they can begin to be managed as a hazard. TYPES OF LANDSLIDES porate additional variables, such as the rate of movement and the water, air, or ice content of The term “landslide” describes a wide variety the landslide material. of processes that result in the downward and outward movement of slope-forming materials Although landslides are primarily associ- including rock, soil, artificial fill, or a com- ated with mountainous regions, they can bination of these. The materials may move also occur in areas of generally low relief. In by falling, toppling, sliding, spreading, or low-relief areas, landslides occur as cut-and- La Conchita, coastal area of southern Califor- flowing. Figure 1 shows a graphic illustration fill failures (roadway and building excava- nia. -
King's Research Portal
King’s Research Portal DOI: 10.1016/j.gloplacha.2014.11.010 Document Version Early version, also known as pre-print Link to publication record in King's Research Portal Citation for published version (APA): Yan, N., & Baas, A. C. W. (2015). Parabolic dunes and their transformations under environmental and climatic changes: Towards a conceptual framework for understanding and prediction. GLOBAL AND PLANETARY CHANGE, 124, 123-148. https://doi.org/10.1016/j.gloplacha.2014.11.010 Citing this paper Please note that where the full-text provided on King's Research Portal is the Author Accepted Manuscript or Post-Print version this may differ from the final Published version. If citing, it is advised that you check and use the publisher's definitive version for pagination, volume/issue, and date of publication details. And where the final published version is provided on the Research Portal, if citing you are again advised to check the publisher's website for any subsequent corrections. General rights Copyright and moral rights for the publications made accessible in the Research Portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognize and abide by the legal requirements associated with these rights. •Users may download and print one copy of any publication from the Research Portal for the purpose of private study or research. •You may not further distribute the material or use it for any profit-making activity or commercial gain •You may freely distribute the URL identifying the publication in the Research Portal Take down policy If you believe that this document breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. -
Gabion Retaining Walls with Alternate Fill Materials
Gabion Retaining Walls with Alternate Fill Materials IGC 2009, Guntur, INDIA GABION RETAINING WALLS WITH ALTERNATE FILL MATERIALS K.S. Beena Reader, School of Engineering, Cochin University of Science and Technology, Cochin–682022, India. E-mail: [email protected] P.K. Jayasree Lecturer in Civil Engineering, College of Engineering, Trivandrum–695 016, India. E-mail: [email protected] ABSTRACT: Although gabions have been used from ancient times, it is only in the last few decades that their wide spread use has lead them to become an accepted construction material in Civil Engineering. Gabion retaining walls are mass gravity structure made up of strong mesh containers known as gabion boxes, filled with quarry stone. Considering the cost and scarcity of quarry stones, the replacement of it with some other cheaper material will make the construction more economical. This aspect is studied here. Considering the specific gravity, friction, cost and availability, quarry dust and red soil was selected as the fill material. Model gabion retaining walls were constructed for the purpose in which, different combinations of quarry dust, red soil and coarse aggregate were taken as the filling material. Analyzing the lateral deformations of various cases, it can be concluded that a 50%–50% combination of alternative material and aggregate will perform better than the coarse aggregate alone, considering the cost of construction. 1. INTRODUCTION dry stone gravity mass wall made of gabion boxes. They are cost effective, environmental friendly and durable structures. Retaining walls, one of the major geotechnical applications, Because of these reasons gabions are widely used now days are mainly used in the case of highways and railways to all over the world. -
Landslide Triggering Mechanisms
kChapter 4 GERALD F. WIECZOREK LANDSLIDE TRIGGERING MECHANISMS 1. INTRODUCTION 2.INTENSE RAINFALL andslides can have several causes, including Storms that produce intense rainfall for periods as L geological, morphological, physical, and hu- short as several hours or have a more moderate in- man (Alexander 1992; Cruden and Vames, Chap. tensity lasting several days have triggered abun- 3 in this report, p. 70), but only one trigger (Varnes dant landslides in many regions, for example, 1978, 26). By definition a trigger is an external California (Figures 4-1, 4-2, and 4-3). Well- stimulus such as intense rainfall, earthquake shak- documented studies that have revealed a close ing, volcanic eruption, storm waves, or rapid stream relationship between rainfall intensity and acti- erosion that causes a near-immediate response in vation of landslides include those from California the form of a landslide by rapidly increasing the (Campbell 1975; Ellen et al. 1988), North stresses or by reducing the strength of slope mate- Carolina (Gryta and Bartholomew 1983; Neary rials. In some cases landslides may occur without an and Swift 1987), Virginia (Kochel 1987; Gryta apparent attributable trigger because of a variety or and Bartholomew 1989; Jacobson et al. 1989), combination of causes, such as chemical or physi- Puerto Rico (Jibson 1989; Simon et al. 1990; cal weathering of materials, that gradually bring the Larsen and Torres Sanchez 1992)., and Hawaii slope to failure. The requisite short time frame of (Wilson et al. 1992; Ellen et al. 1993). cause and effect is the critical element in the iden- These studies show that shallow landslides in tification of a landslide trigger. -
Slope Stability 101 Basic Concepts and NOT for Final Design Purposes! Slope Stability Analysis Basics
Slope Stability 101 Basic Concepts and NOT for Final Design Purposes! Slope Stability Analysis Basics Shear Strength of Soils Ability of soil to resist sliding on itself on the slope Angle of Repose definition n1. the maximum angle to the horizontal at which rocks, soil, etc, will remain without sliding Shear Strength Parameters and Soils Info Φ angle of internal friction C cohesion (clays are cohesive and sands are non-cohesive) Θ slope angle γ unit weight of soil Internal Angles of Friction Estimates for our use in example Silty sand Φ = 25 degrees Loose sand Φ = 30 degrees Medium to Dense sand Φ = 35 degrees Rock Riprap Φ = 40 degrees Slope Stability Analysis Basics Explore Site Geology Characterize soil shear strength Construct slope stability model Establish seepage and groundwater conditions Select loading condition Locate critical failure surface Iterate until minimum Factor of Safety (FS) is achieved Rules of Thumb and “Easy” Method of Estimating Slope Stability Geology and Soils Information Needed (from site or soils database) Check appropriate loading conditions (seeps, rapid drawdown, fluctuating water levels, flows) Select values to input for Φ and C Locate water table in slope (critical for evaluation!) 2:1 slopes are typically stable for less than 15 foot heights Note whether or not existing slopes are vegetated and stable Plan for a factor of safety (hazards evaluation) FS between 1.4 and 1.5 is typically adequate for our purposes No Flow Slope Stability Analysis FS = tan Φ / tan Θ Where Φ is the effective -
B1: Extend Existing Pipe
A: Downtown Diversion Pipe b c Source: Woolpert, Inc. 2006 with modifications Map highlighting conservation easement. Advantages • Will divert 40-44% of total flow.; and The diversion pipe would run along the railroad. • Reduce the impact on Sand River because it would reduce the outflow from the 10’ pipe. Disadvantages • Conservation easement will be needed along the railroad; • Will require additional storage capacity; and • Will be costly. CSX Railroad and Red Cross Location the diversion pipe would West watershed junction box. leave the railroad at Dibble road. B1: Extend Existing Pipe Source: Woolpert, Inc. 2006 Source: Woolpert, Inc. 2006 Map showing the suggested extension of the pipe. Section of the alterations made to the canyon in order to extend the existing pipe. Advantages • Minimizes amount of new sediment from entering Barton’s Pond; • Easiest method to stabilize the canyon; and • Could be constructed without any additional permits. Drawbacks • Does not dissipate the force of the flow of water or energy; and • The problem is shifted downstream. Considerations Existing canyon walls that The existing pipe that would be • Flow still needs to be returned to the surface. would be filled in and stabilized extended through the canyon of to extend the pipe. Sand River B2: Gabion Baskets as an Erosion Solution Flow a Source: Woolpert, Inc. 2006 Pipe Permeable Geotextile Fabric d b Source: Woolpert, Inc. 2006 Source: Woolpert, Inc. 2006 with modifications Source: Woolpert, Inc. 2006 Sections of the gabions along Sand River a - Section the length of the section of proposed gabions b - Section of a gabion dam Advantages c - Section of the gabion walls with permeable geotextile fabric • Ease of handling and transportation; d - Section of gabion walls without permeable layer against the earth • Speed of construction; • Aesthetically more pleasing than some options; • Provides more natural stream pattern and profile; • Dissipates the energy of the stream; and • If properly constructed, vegetated gabions strengthen with time.