Alaskan Update
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Porosity and Permeability Lab
Mrs. Keadle JH Science Porosity and Permeability Lab The terms porosity and permeability are related. porosity – the amount of empty space in a rock or other earth substance; this empty space is known as pore space. Porosity is how much water a substance can hold. Porosity is usually stated as a percentage of the material’s total volume. permeability – is how well water flows through rock or other earth substance. Factors that affect permeability are how large the pores in the substance are and how well the particles fit together. Water flows between the spaces in the material. If the spaces are close together such as in clay based soils, the water will tend to cling to the material and not pass through it easily or quickly. If the spaces are large, such as in the gravel, the water passes through quickly. There are two other terms that are used with water: percolation and infiltration. percolation – the downward movement of water from the land surface into soil or porous rock. infiltration – when the water enters the soil surface after falling from the atmosphere. In this lab, we will test the permeability and porosity of sand, gravel, and soil. Hypothesis Which material do you think will have the highest permeability (fastest time)? ______________ Which material do you think will have the lowest permeability (slowest time)? _____________ Which material do you think will have the highest porosity (largest spaces)? _______________ Which material do you think will have the lowest porosity (smallest spaces)? _______________ 1 Porosity and Permeability Lab Mrs. Keadle JH Science Materials 2 large cups (one with hole in bottom) water marker pea gravel timer yard soil (not potting soil) calculator sand spoon or scraper Procedure for measuring porosity 1. -
Method 9100: Saturated Hydraulic Conductivity, Saturated Leachate
METHOD 9100 SATURATED HYDRAULIC CONDUCTIVITY, SATURATED LEACHATE CONDUCTIVITY, AND INTRINSIC PERMEABILITY 1.0 INTRODUCTION 1.1 Scope and Application: This section presents methods available to hydrogeologists and and geotechnical engineers for determining the saturated hydraulic conductivity of earth materials and conductivity of soil liners to leachate, as outlined by the Part 264 permitting rules for hazardous-waste disposal facilities. In addition, a general technique to determine intrinsic permeability is provided. A cross reference between the applicable part of the RCRA Guidance Documents and associated Part 264 Standards and these test methods is provided by Table A. 1.1.1 Part 264 Subpart F establishes standards for ground water quality monitoring and environmental performance. To demonstrate compliance with these standards, a permit applicant must have knowledge of certain aspects of the hydrogeology at the disposal facility, such as hydraulic conductivity, in order to determine the compliance point and monitoring well locations and in order to develop remedial action plans when necessary. 1.1.2 In this report, the laboratory and field methods that are considered the most appropriate to meeting the requirements of Part 264 are given in sufficient detail to provide an experienced hydrogeologist or geotechnical engineer with the methodology required to conduct the tests. Additional laboratory and field methods that may be applicable under certain conditions are included by providing references to standard texts and scientific journals. 1.1.3 Included in this report are descriptions of field methods considered appropriate for estimating saturated hydraulic conductivity by single well or borehole tests. The determination of hydraulic conductivity by pumping or injection tests is not included because the latter are considered appropriate for well field design purposes but may not be appropriate for economically evaluating hydraulic conductivity for the purposes set forth in Part 264 Subpart F. -
Comparison of Hydraulic Conductivities for a Sand and Gravel Aquifer in Southeastern Massachusetts, Estimated by Three Methods by LINDA P
Comparison of Hydraulic Conductivities for a Sand and Gravel Aquifer in Southeastern Massachusetts, Estimated by Three Methods By LINDA P. WARREN, PETER E. CHURCH, and MICHAEL TURTORA U.S. Geological Survey Water-Resources Investigations Report 95-4160 Prepared in cooperation with the MASSACHUSETTS HIGHWAY DEPARTMENT, RESEARCH AND MATERIALS DIVISION Marlborough, Massachusetts 1996 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information write to: Copies of this report can be purchased from: Chief, Massachusetts-Rhode Island District U.S. Geological Survey U.S. Geological Survey Earth Science Information Center Water Resources Division Open-File Reports Section 28 Lord Road, Suite 280 Box 25286, MS 517 Marlborough, MA 01752 Denver Federal Center Denver, CO 80225 CONTENTS Abstract.......................................................................................................................^ 1 Introduction ..............................................................................................................................................................^ 1 Hydraulic Conductivities Estimated by Three Methods.................................................................................................... 3 PenneameterTest.............................................................^ 3 Grain-Size Analysis with the Hazen Approximation............................................................................................. 8 SlugTest...................................................^ -
Gravel Roads Maintenance & Frontrunner Training Workshop
A Ditch In Time Gravel Roads Maintenance Workshop 1 So you think you’ve got a wicked driveway 2 1600’ driveway with four switchbacks and 175’ of elevation change (11% grade) 3 Rockhouse Development, Conway 4 5 6 Swift River (left) through National Forest into Saco River that drains the MWV Valley’s developments 7 The best material starts as solid rock that is drilled & blasted… 8 Then crushed into smaller pieces and screened to produce specific size aggregate 9 How strong should it be? One big truck = 10,000 cars! 10 11 The road surface… • Lots of small aggregate (stones) to provide strength with a shape that will lock stones together to support wheels • Sufficient “fines,” the binder that will lock the stones together, to keep the stones from moving around 12 • The stone: hard and uniform in size and more angular than that made just from screening bank run gravel 13 • A proper combination of correctly sized broken rock, sand and silt/clay soil materials will produce a road surface that hardens into a strong and stable crust that forms a reasonably impervious “roof” to our road • An improper balance- a surface that is loose, soft & greasy when wet, or excessively dusty when dry (see samples) 14 One way to judge whether gravel will pack or not… 15 Here’s another way… 16 Or: The VeryFine test The sticky palm test As shown in the Camp Roads manual 17 • “Dirty” gravel packs but does not drain • “Clean” gravel drains but does not pack 18 Other road surfacing materials: • Rotten Rock- traditional surfacing material in the Mt Washington Valley -
Dicionarioct.Pdf
McGraw-Hill Dictionary of Earth Science Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto Copyright © 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Manufactured in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be repro- duced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 0-07-141798-2 The material in this eBook also appears in the print version of this title: 0-07-141045-7 All trademarks are trademarks of their respective owners. Rather than put a trademark symbol after every occurrence of a trademarked name, we use names in an editorial fashion only, and to the benefit of the trademark owner, with no intention of infringement of the trademark. Where such designations appear in this book, they have been printed with initial caps. McGraw-Hill eBooks are available at special quantity discounts to use as premiums and sales promotions, or for use in corporate training programs. For more information, please contact George Hoare, Special Sales, at [email protected] or (212) 904-4069. TERMS OF USE This is a copyrighted work and The McGraw-Hill Companies, Inc. (“McGraw- Hill”) and its licensors reserve all rights in and to the work. Use of this work is subject to these terms. Except as permitted under the Copyright Act of 1976 and the right to store and retrieve one copy of the work, you may not decom- pile, disassemble, reverse engineer, reproduce, modify, create derivative works based upon, transmit, distribute, disseminate, sell, publish or sublicense the work or any part of it without McGraw-Hill’s prior consent. -
(Sds) : Sand & Gravel
SAFETY DATA SHEET (SDS) : SAND & GRAVEL SECTION I – IDENTIFICATION PRODUCT IDENTIFIER TRADE NAME OTHER SYNONYMS Natural Sand & Gravel, Gravel Gravel Sand Construction Aggregate, River Rock, Pea Gravel, Course Aggregate RECOMMENDED USE AND RESTRICTION ON USE Used for construction purposes This product is not intended or designed for and should not be used as an abrasive blasting medium or for foundry applications. MANUFACTURER/SUPPLIER INFORMATION Martin Marietta Materials 4123 Parklake Ave Raleigh, North Carolina 27612 Phone: 919-781-4550 For additional health, safety or regulatory information and other emergency situations, call 919-781-4550 SECTION II – HAZARD(S) IDENTIFICATION HAZARD CLASSIFICATION: Category 1A Carcinogen Category 1 Specific Target Organ Toxicity (STOT) following repeated exposures Category 1 Eye Damage Category 1 Skin Corrosive SIGNAL WORD: DANGER HAZARD STATEMENTS: May cause cancer by inhalation. Causes damage to lungs, kidneys and autoimmune system through prolonged or repeated exposure by inhalation. Causes severe skin burns and serious eye damage. PRECAUTIONARY STATEMENTS Do not handle until the safety information presented in this SDS has been read and understood. Do not breathe dusts or mists. Do not eat, drink or smoke while manually handling this product. Wash skin thoroughly after manually handling. If swallowed: Rinse mouth and do not induce vomiting. If on skin (or hair): Rinse skin after manually handling and wash contaminated clothing if there is potential for direct skin contact before reuse. If inhaled excessively: Remove person to fresh air and keep comfortable for breathing. If in eyes: Rinse cautiously with water for several minutes. Remove contact lenses, if present and easy to do, and continue rinsing. -
Step 2-Soil Mechanics
Step 2 – Soil Mechanics Introduction Webster defines the term mechanics as a branch of physical science that deals with energy and forces and their effect on bodies. Soil mechanics is the branch of mechanics that deals with the action of forces on soil masses. The soil that occurs at or near the surface of the earth is one of the most widely encountered materials in civil, structural and architectural engineering. Soil ranks high in degree of importance when compared to the numerous other materials (i.e. steel, concrete, masonry, etc.) used in engineering. Soil is a construction material used in many structures, such as retaining walls, dams, and levees. Soil is also a foundation material upon which structures rest. All structures, regardless of the material from which they are constructed, ultimately rest upon soil or rock. Hence, the load capacity and settlement behavior of foundations depend on the character of the underlying soils, and on their action under the stress imposed by the foundation. Based on this, it is appropriate to consider soil as a structural material, but it differs from other structural materials in several important aspects. Steel is a manufactured material whose physical and chemical properties can be very accurately controlled during the manufacturing process. Soil is a natural material, which occurs in infinite variety and whose engineering properties can vary widely from place to place – even within the confines of a single construction project. Geotechnical engineering practice is devoted to the location of various soils encountered on a project, the determination of their engineering properties, correlating those properties to the project requirements, and the selection of the best available soils for use with the various structural elements of the project. -
Estimating Permeability from the Grain-Size Distributions of Natural Sediment
Wright State University CORE Scholar Browse all Theses and Dissertations Theses and Dissertations 2010 Estimating Permeability from the Grain-Size Distributions of Natural Sediment Lawrence Mastera Wright State University Follow this and additional works at: https://corescholar.libraries.wright.edu/etd_all Part of the Earth Sciences Commons, and the Environmental Sciences Commons Repository Citation Mastera, Lawrence, "Estimating Permeability from the Grain-Size Distributions of Natural Sediment" (2010). Browse all Theses and Dissertations. 994. https://corescholar.libraries.wright.edu/etd_all/994 This Thesis is brought to you for free and open access by the Theses and Dissertations at CORE Scholar. It has been accepted for inclusion in Browse all Theses and Dissertations by an authorized administrator of CORE Scholar. For more information, please contact [email protected]. ESTIMATING PERMEABILITY FROM THE GRAIN-SIZE DISTRIBUTIONS OF NATURAL SEDIMENT A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science By LAWRENCE JOHN MASTERA B.S., Norwich University, 2008 2010 Wright State University WRIGHT STATE UNIVERSITY SCHOOL OF GRADUATE STUDIES June 10, 2010 I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION BY Lawrence John Mastera ENTITLED Estimating Permeability from the Grain-Size Distributions of Natural Sediment BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Master of Science. Robert W. Ritzi, Jr., Ph.D. Thesis Director David F. Dominic, Ph.D. Department Chair Committee on Final Examination Robert W. Ritzi, Jr., Ph.D. David F. Dominic, Ph.D. Mark N. Goltz, Ph.D. Ramya Ramanathan, Ph.D. John A. Bantle, Ph.D. -
Performance-Based Hydraulic Conductivity Models for Unbound Granular Materials
Performance-Based Hydraulic Conductivity Models for Unbound Granular Materials Haithem Soliman, Ph.D. Assistant Professor Department of Civil & Geological Engineering University of Saskatchewan Email: [email protected] Ahmed Shalaby, P.Eng. Professor and Head Department of Civil Engineering University of Manitoba E-mail: [email protected] Paper prepared for presentation at the “Advanced Testing and Modeling of Road and Embankment Materials” Session of the 2016 Annual Conference of the Transportation Association of Canada Toronto, Ontario. 1 Abstract Specifications for unbound granular materials (UGM) must be based on the function of the unbound layer (drainable layer, high stiffness, or both). Using performance-based specifications that are based on laboratory performance of UGM (resilient modulus, permanent deformation, and permeability) provides durable and longer lasting unbound layers. This paper investigates the effect of fines content variation on the permeability (hydraulic conductivity) of two types of UGM, gravel and 100% crushed limestone. Hydraulic conductivity tests were conducted on compacted gravel UGM with 4.0% fines, 9.0% fines, and 14.5% fines. For 100% crushed limestone, hydraulic conductivity tests were conducted on compacted samples with 4.5% fines, 10.5% fines, and 16.0% fines. For gravel, the hydraulic conductivity decreased by 84% due to increasing fines content from 4.0% to 14.5%. For Limestone, the hydraulic conductivity decreased by 81% due to increasing fines content from 4.5% to 16.0%. For gradations with comparable fines content, limestone material showed higher hydraulic conductivity than that for gravel. The laboratory measured hydraulic conductivity was compared to Level 2 design inputs in the Mechanistic-Empirical Pavement Design Guide (Pavement ME). -
Beltcov Andrei.Pdf (5.892Mb)
Faculty of Science and Technology MASTER’S THESIS Study program/ Specialization: Spring semester, 2016 Offshore Technology/ Marine and Subsea Technology Open Writer: Andrei Y. Beltcov ………………………………………… (Writer’s signature) Faculty supervisor: Professor Ove Tobias Gudmestad (University of Stavanger) External supervisor(s): Professor Anatoly Borisovich Zolotukhin (Gubkin University) Title of thesis: «Development concepts for Sakhalin's offshore field development» Credits (ECTS):30 Key words: Pages: 15 + enclosure: 4 Concept development, Concept selection, Sakhalin’s Island offshore development, Concept selection criteria. Stavanger, June, 15, 2016 Abstract When a company undertakes to develop an oilfield, certain activities represent the foundation of the development, ranging from information about the metocean conditions at the site to marketing. The concept phase itself includes screening of concepts, selection of concept and concept development. Use of engineering data and calculations that represents a feasibility study of offshore oil and gas field is essentially the screening of concepts. The selection of concept consists of finding a solution that would meet world technical, environmental and safety demands. Despite the fact that Sakhalin Island shelf contains enormous hydrocarbon reserves, it is also a very environmentally sensitive region. High environmental risks and extreme weather conditions entail high capital expenditures, which put significant burden of responsibility on the project team during the development concept stage. This is of great importance during the early stages of concept selection. Selecting the optimum Sakhalin Shelf development concept is the aim of my thesis. Significance in the concept selection chain affects selection of various parameters affecting the optimum development concept and subsequent prioritization. Special attention is paid to challenges and peculiarities that can be faced at the Sakhalin Region and could affect the concept of field development. -
Appendix A. Basic Information About Landslides 60 the Landslide Handbook—A Guide to Understanding Landslides
Appendix A. Basic Information about Landslides 60 The Landslide Handbook —A Guide to Understanding Landslides Part 1. Glossary of Landslide Terms Full references citations for glossary are at the end of the list. alluvial fan An outspread, gently sloping Digital Terrain Model (DTM) The term used Geographic Information System (GIS) A mass of alluvium deposited by a stream, by United States Department of Defense and computer program and associated data bases especially in an arid or semiarid region other organizations to describe digital eleva- that permit cartographic information (includ- where a stream issues from a narrow canyon tion data. (Reference 3) ing geologic information) to be queried onto a plain or valley floor. Viewed from drawdown Lowering of water levels in riv- by the geographic coordinates of features. above, it has the shape of an open fan, the ers, lakes, wells, or underground aquifers due Usually the data are organized in “layers” apex being at the valley mouth. (Reference 3) to withdrawal of water. Drawdown may leave representing different geographic entities such as hydrology, culture, topography, and bedding surface/plane In sedimentary or unsupported banks or poorly packed earth so forth. A geographic information system, stratified rocks, the division planes that sepa- that can cause landslides. (Reference 3) or GIS, permits information from different rate each successive layer or bed from the electronic distance meter (EDM) A device layers to be easily integrated and analyzed. one above or below. It is commonly marked that emits ultrasonic waves that bounce off (Reference 3) by a visible change in lithology or color. -
Challenges of Dredging in the Arctic and Other Deep Ocean Locations
Proceedings of Western Dredging Association and Texas A&M University Center for Dredging Studies' "Dredging Summit and Expo 2015" CHALLENGES OF DREDGING IN THE ARCTIC AND OTHER DEEP OCEAN LOCATIONS R. E. Randall1 and C. K. Jin2 ABSTRACT Dredging in the Arctic Ocean is challenging due to ice cover, permafrost, iceberg scour, whaling season, ice gouging, and remote location. In the deep ocean 1000 m (3280 ft), dredging is a technique for recovering minerals from the deep ocean waters where water depth is a major challenge for the pumping system. Another application for dredging in the deep ocean and beneath ice covered waters is for recovering petroleum reserves. This paper reviews the recent literature of current systems used for deep ocean mining and the need for developing oil and gas development beneath ice covered water. Conceptual ideas are discussed for overcoming the dredging challenges that include the use of remotely operated vehicles, trenchers, hopper dredges and self-propelled cutter suction dredges. Keywords: Dredging, trenching, arctic, ocean mining, deep water. INTRODUCTION The demand for essential industrial resources, such as oil and gas, has been increasing, which accelerates the decrease in such resources on land and in coastal regions. Accordingly, expanding the exploration to harsh environmental regions, especially the Arctic and deep oceans, turns out to be a promising solution since they are far less developed. For example, it is reported that the area north of the Arctic Circle comprises 13% and 30% of the undiscovered oil and gas in the world, respectively (Gautier et al. 2009). As one of the most important applications in a severe ocean environment, dredging has been utilized to excavate material and minerals, or even improve the environment (Bray et al.