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Seismic Lines in Treed Boreal Peatlands As Analogs for Wildfire
fire Article Seismic Lines in Treed Boreal Peatlands as Analogs for Wildfire Fuel Modification Treatments Patrick Jeffrey Deane, Sophie Louise Wilkinson * , Paul Adrian Moore and James Michael Waddington School of Geography and Earth Sciences, McMaster University, 1280 Main Street West, Hamilton, ON L8S 4K1, Canada; [email protected] (P.J.D.); [email protected] (P.A.M.); [email protected] (J.M.W.) * Correspondence: [email protected] Received: 8 April 2020; Accepted: 4 June 2020; Published: 6 June 2020 Abstract: Across the Boreal, there is an expansive wildland–society interface (WSI), where communities, infrastructure, and industry border natural ecosystems, exposing them to the impacts of natural disturbances, such as wildfire. Treed peatlands have previously received little attention with regard to wildfire management; however, their role in fire spread, and the contribution of peat smouldering to dangerous air pollution, have recently been highlighted. To help develop effective wildfire management techniques in treed peatlands, we use seismic line disturbance as an analog for peatland fuel modification treatments. To delineate below-ground hydrocarbon resources using seismic waves, seismic lines are created by removing above-ground (canopy) fuels using heavy machinery, forming linear disturbances through some treed peatlands. We found significant differences in moisture content and peat bulk density with depth between seismic line and undisturbed plots, where smouldering combustion potential was lower in seismic lines. Sphagnum mosses dominated seismic lines and canopy fuel load was reduced for up to 55 years compared to undisturbed peatlands. Sphagnum mosses had significantly lower smouldering potential than feather mosses (that dominate mature, undisturbed peatlands) in a laboratory drying experiment, suggesting that fuel modification treatments following a strategy based on seismic line analogs would be effective at reducing smouldering potential at the WSI, especially under increasing fire weather. -
Origins of Mechanical Compaction the Fresno Grader
Part 1 ORIGINS OF MECHANICAL COMPACTION THE FRESNO GRADER Abajiah McCall invented the horse- drawn dirt bucket scrapper in Fresno County, California in 1885. It became known as the “Fresno Scrapper” and was widely employed as the prime earth moving device until the widespread advent of self- powered scrappers in the 1930s. Above left: 10-horse team pulling an elevating grader to load hopper dumping wagons during construction of the Central Reservoir for the People’s Water Co. in Oakland, California in 1909. Note old Buffalo- Springfield steam roller compacting the dam’s embankment, in left background Below Left: Marion shovel loading a hopper dumping wagon at the San Pablo Dam site of the East Bay Water Company in 1920, in Richmond, California. At 220 ft high with a volume of 2.2 million yds3 it was the highest and largest earth dam in the world when completed in 1922. “Load Compaction” of Trestle Fills In the early days large embankments were constructed by side-dumping rail cars or wagons from temporary wooden trestles, as shown at left. Engineers assumed that, after placement and infiltration by rain, the soil would ‘compact’ under its own dead load. The first sheepsfoot rollers The first sheepsfoot roller was built in Los Angeles in 1902, using a 3-ft diameter log studded with railroad spikes protruding 7 inches, distributed so the spikes were staggered in alternate rows. This layout was soon modified to increase weight and efficiency, initially by increasing its length to 8 ft. Note the leading wheels on the early models shown here, absent later. -
Construction Quality Assurance Final Report On
CONSTRUCTION QUALITY ASSURANCE FINAL REPORT ON-SITE DISPOSAL FACILITY, PHASE I1 CELL 3 November 1999 Revision 0 United States Department of Energy Fernald Environmental Management Project Fernald, Ohio Prepared by GeoSyntec Consultants Fernald Field Office 7400 Willey Road, Mail Stop 3 8 Hamilton, Ohio 4.50 13 Under , Fluor Daniel Fernald Subcontract 95PS005028 GeoSyntec Consultants TABLE OF CONTENTS 1. INTRODUCTION ............................................................................................................................ 1 1.1 TERMSOF REFERENCE.................................................................................................................... 1 1.2 BACKGROUND................................................................................................................................ 1 1.3 REPORTORGANIZATION ................................................................................................................... 3 2 . PROJECT DESCRIPTION ............................................................................................................. 4 3. CONSTRUCTION QUALITY ASSURANCE PROGRAM ............ :............................................ 8 3.1 SCOPEOF SERVICES........................................................................................................................ .8 3.1.1 Overview...................................... ..................................................................... 8 3.1.2 Review of Documents .......................................................... -
Density Prediction from Ground-Roll Inversion Soumya Roy*And Robert R
Density prediction from ground-roll inversion Soumya Roy*and Robert R. Stewart, University of Houston, Houston, Texas 77204 Summary Montana, and d) the Barringer (Meteor) Crater, Arizona. Modeling data are useful to test the ground-roll inversion Bulk densities are often predicted from seismic velocities method and the existing density prediction formula. Field using the Gardner’s relation if density information is data are used to test the dependability of the predictions for unavailable. P-wave velocity is used in the Gardner’s varied geological settings and rock properties (especially relation. We used a modified Gardner’s relation to predict for the near-surface). bulk densities from S-wave velocities where we estimated S-wave velocities using the noninvasive ground-roll inversion method. Different types of seismic data sets have Seismic data sets from various settings been used: i) numerical and physical modeling; ii) data from: Red Lodge, Montana, and the Barringer (Meteor) a) Numerical modeling: Synthetic seismic data sets for a Crater, Arizona. The main objectives of the paper are: i) to three-layered (two layers over a half-space) model are test the modified Gardner’s relation for different types of generated using a elastic finite-difference numerical materials, ii) to estimate errors between known and modeling code for layered isotropic medium (Manning, predicted bulk densities, and iii) to compare different 2007 and Al Dulaijan, 2008). We used the code written by empirical exponent values to minimize the error. We Manning (2007). We used receiver interval of 2 m with a estimate predicted densities with maximum error of 0.5 receiver spread of 300 stations, source-receiver offset of 10 gm/cc for known values (the blank glass model and m, and shot interval of 10 m. -
Chapter 21 Soil Improvement
CHAPTER 21 SOIL IMPROVEMENT 21.1 INTRODUCTION General practice is to use shallow foundations for the foundations of buildings and other such structures, if the soil close to the ground surface possesses sufficient bearing capacity. However, where the top soil is either loose or soft, the load from the superstructure has to be transferred to deeper firm strata. In such cases, pile or pier foundations are the obvious choice. There is also a third method which may in some cases prove more economical than deep foundations or where the alternate method may become inevitable due to certain site and other environmental conditions. This third method comes under the heading foundation soil improvement. In the case of earth dams, there is no other alternative than compacting the remolded soil in layers to the required density and moisture content. The soil for the dam will be excavated at the adjoining areas and transported to the site. There are many methods by which the soil at the site can be improved. Soil improvement is frequently termed soil stabilization, which in its broadest sense is alteration of any property of a soil to improve its engineering performance. Soil improvement 1. Increases shear strength 2. Reduces permeability, and 3. Reduces compressibility The methods of soil improvement considered in this chapter are 1. Mechanical compaction 2. Dynamic compaction 3. Vibroflotation 4. Preloading 5. Sand and stone columns 951 952 Chapter 21 6. Use of admixtures 7. Injection of suitable grouts 8. Use of geotextiles 21.2 MECHANICAL COMPACTION Mechanical compaction is the least expensive of the methods and is applicable in both cohesionless and cohesive soils. -
Downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE)
INTERNATIONAL SOCIETY FOR SOIL MECHANICS AND GEOTECHNICAL ENGINEERING This paper was downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE). The library is available here: https://www.issmge.org/publications/online-library This is an open-access database that archives thousands of papers published under the Auspices of the ISSMGE and maintained by the Innovation and Development Committee of ISSMGE. lb/13 Large Scale Shear Tests Essais de Cisaillement à Grande Échelle by E. S chultze, Professor Dr.-Ing., Technische Hochschule, Aachen, G erm any Summary Sommaire Direct shearing tests with a plane of shear of 1 m2 were carried Des essais directs de cisaillement, avec une surface à cisailler de out in an open-pit of a lignite mine during 1953 in order to explore 1 m2, furent exécutés au cours de l’année 1953 dans une exploitation in situ the shearing strength between the lignite and the underlying de lignite à ciel ouvert. Il s’agissait d’étudier la résistance au cisaille beds. ment entre la lignite et la base d’un gisement. An apparatus for large scale triaxial compression tests has been set Au cours de l’année 1954 fut mis en marche un appareil pour des up which permits the insertion and the shearing off of samples 1 -25 m essais de pression triaxiale à grande échelle, qui permet de monter des long and 0-5 m diameter. The latéral pressure is produced by ex- essais de 1 -25 m de hauteur et 0-5 m de diamètre. La pression hausting the air out of the specimen and may be increased up to latérale est obtenue par aspiration de l’air de l’échantillon; cette 0-9 kg/cm2. -
LABORATORY 2 SOIL DENSITY I Objectives Measure Particle Density
LABORATORY 2 SOIL DENSITY I Objectives Measure particle density, bulk density, and moisture content of a soil and to relate to total pore space. II Introduction A Particle Density Soil particle density (g / cm3) is mass of soil solids (oven-dry) per unit volume of soil solids. Particle density depends on the densities of the various constituent solids and their relative abundance. The particle density of most mineral soils lies between 2.5 and 2.7 g / cm3. The range is fairly naarrow because common soil minerals differ little in density. An average value of 2.65 g / cm3 is often assumed. In contrast, organic soils have lower particle densities since the density of organic matter is much less than that of mineral particles. In this laboratory, you will determine the particle density of a particular soil. It is easy to measure the mass of a small sample of soil but not so easy to accurately measure the volume of soil solids that make up this mass. Briefly, the volume of a known mass of soil solids is determined by indirectly measuring the volume of water displaced by the soil solids. The mass of water displaced is actually measured, then the corresponding volume found from the known density of water. B Bulk Density Soil bulk density (g / cm3) is mass of soil solids (oven-dry) per unit of volume of soil. The volume includes all pore space as well as space occupied by soil solids. Soil structure and texture largely determine bulk density. Soil structure refers to the arrangement of soil particles into secondary bodies called aggregates. -
Influence of Relative Compaction on the Shear Strength of Compacted Surface Sands
International Journal of Environmental Science and Development, Vol. 5, No. 1, February 2014 Influence of Relative Compaction on the Shear Strength of Compacted Surface Sands Nabil F. Ismael and Mariam Behbehani strength characteristics of the compacted fill. Abstract—Construction of structures always involves This paper aims to answer these questions and to learn excavation, and recompaction following foundation installation. more about the properties of compacted sand fills by means In some cases foundations are placed on compacted sandy soils. of a laboratory-testing program. Testing included basic The influence of relative compaction on the strength of sandy characteristics, compaction tests, and direct shear tests. In soils in Kuwait is examined herein by a comprehensive laboratory testing program on surface samples. The program view of recent work indicating significant soil improvement includes basic properties, compaction and, direct shear tests. with artificial cementation [6], the effect of using 1 % by Various soil parameters were determined including the weight ordinary Portland cement additive (Type I) on the compaction characteristics, the cohesion c, angle of friction φ. shear strength parameters of compacted surface sands is also The results indicate that as the relative compaction increases examined. towards 100%, the strength increases and the soil compressibility decreases. A comparison was made between the soil parameters for the samples compacted on the dry side, and on the wet side of optimum moisture content at several relative II. TESTING PROGRAM compaction ratios. The difference in the values obtained for the The testing program consisted of: two cases are explained. The effect of using 1% by weight 1) Collecting large bulk sample of surface sand from one cement additive is also examined. -
Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H
St. Louis Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H. Cramer, Robert A. Bauer, Jae-won Chung, J. David Rogers, Larry Pierce, Vicki Voigt, Brad Mitchell, David Gaunt, Robert A. Wil- liams, David Hoffman, Gregory L. Hempen, Phyllis J. Steckel, Oliver S. Boyd, Connor M. Watkins, Kathleen Tucker, and Natasha S. McCallister ABSTRACT We present probabilistic and deterministic seismic and liquefac- (NMSZ) earthquake sequence. This sequence produced modi- tion hazard maps for the densely populated St. Louis metropolitan fied Mercalli intensity (MMI) for locations in the St. Louis area area that account for the expected effects of surficial geology on that ranged from VI to VIII (Nuttli, 1973; Bakun et al.,2002; earthquake ground shaking. Hazard calculations were based on a Hough and Page, 2011). The region has experienced strong map grid of 0.005°, or about every 500 m, and are thus higher in ground shaking (∼0:1g peak ground acceleration [PGA]) as a resolution than any earlier studies. To estimate ground motions at result of prehistoric and contemporary seismicity associated with the surface of the model (e.g., site amplification), we used a new the major neighboring seismic source areas, including the Wa- detailed near-surface shear-wave velocity model in a 1D equiva- bashValley seismic zone (WVSZ) and NMSZ (Fig. 1), as well as lent-linear response analysis. When compared with the 2014 U.S. a possible paleoseismic earthquake near Shoal Creek, Illinois, Geological Survey (USGS) National Seismic Hazard Model, about 30 km east of St. Louis (McNulty and Obermeier, 1997). which uses a uniform firm-rock-site condition, the new probabi- Another contributing factor to seismic hazard in the St. -
Effect of Oil Contamination on the Liquefaction Behavior of Sandy Soils S
World Academy of Science, Engineering and Technology International Journal of Geological and Environmental Engineering Vol:8, No:5, 2014 Effect of Oil Contamination on the Liquefaction Behavior of Sandy Soils S. A. Naeini, M. M. Shojaedin viscosity of the contaminant oil. Khamehchiyan et al. (2007) Abstract—Oil leakage from the pipelines and the tanks carrying [4] carried out the laboratory testing, including Atterberg them, or during oil extraction, could lead to the changes in the limits, compaction, direct shear, uniaxial compression and characteristics and properties of the soil. In this paper, conducting a permeability tests, on clayey and sandy soils such as CL, SM series of experimental cyclic triaxial tests, the effects of oil and SP sampled from the coastal soils. The contaminated contamination on the liquefaction potential of sandy soils is investigated. The studied specimens are prepared by mixing the samples were prepared by mixing the soils with crude oil in Firoozkuh sand with crude oil in 4, 8 and 12 percent by soil dry the amount of 2%, 4%, 8%, 12%, and 16% by dry weight. weight. The results show that the oil contamination up to 8% causes This research noted to some limitations for addition of more an increase in the soil liquefaction resistance and then with increase crude oil to the soil samples. The results indicated a decrease in the contamination, the liquefaction resistance decreases. in strength, permeability, maximum dry density, optimum water content and Atterberg limits. The uncontaminated and Keywords—Cyclic triaxial test, Liquefaction resistance, Oil crude oil-contaminated clay were compared by Habib-ur- contamination, Sandy soil. -
Geotechnical Properties and Sediment Characterization for Dredged Material Models
ERDC TN-DOER-N13 December 2001 Geotechnical Properties and Sediment Characterization for Dredged Material Models PURPOSE: This technical note provides an overview of geotechnical engineering properties of dredged materials and input requirements for selected fate of dredged material models. There are numerous models that have been developed or are being developed that require information regarding geotechnical properties and material characteristics for dredged material. BACKGROUND: The U.S. Army Corps of Engineers (USACE) is responsible for maintaining navigationon25,000miles(40,234 km)ofwaterwaysthatserveabout400portsintheUnited States. Billions of tax dollars have funded the USACE civil works mission to maintain and operate these waterways, including dredging activities. The U.S. Army Engineer Research and Develop- ment Center (ERDC) has been tasked to provide enhanced planning and operational tools for helping the USACE Districts more effectively accomplish the various dredging tasks. A priori numerical modeling of a particular dredging operation provides a cost-effective tool to establish operational parameters and forecast optimum dredging scenarios prior to actual dredging operations. Once dredging has started, analytical models are available or are being developed to track operational dredging status to allow feedback into the dredging management process as a compliance monitoring tool. On a broader scale, numerical models allow for effective and economical regional dredging and sediment management planning, including project design. In general, numerical dredging models require input data on the dredged material sediment characteristics, the water body characteristics, the biological and chemical parameters, the environ- mental forcing functions, and the dredging operations. This technical note addresses the model input requirements for dredged material sediment characteristics and engineering properties. -
The Effect of Laboratory Compaction on the Shear Behavior of a Highly Plastic Clay After Saturation and Consolidation
SCHOOL OF CIVIL ENGINEERING JOINT HIGHWAY RESEARCH PROJECT FHWA/IN/JHRP-79-7 THE EFFECT OF LABORATORY COMPACTION ON THE SHEAR BEHAVIOR OF A HIGHLY PLASTIC CLAY AFTER SATURATION AND CONSOLIDATION J. M. Johnson C. W. Lovell PURDUE UNIVERSITY INDIANA STATE HIGHWAY COMMISSION Digitized by the Internet Archive in 2011 with funding from LYRASIS members and Sloan Foundation; Indiana Department of Transportation http://www.archive.org/details/effectoflaboratoOOjohn Interim Report THE EFFECT OF LABORATORY COMPACTION ON THE SHEAR BEHAVIOR OF A HIGHLY PLASTIC CLAY AFTER SATURATION AND CONSOLIDATION TO: H. L. Michael, Director July 11, 1979 Joint Highway Research Project Project: C-36-5M FROM: C. W. Lovell, Research Engineer Joint Highway Research Project File: 6-6-13 Attached is an Interim Report on the HPR Part II Study titled "Improving Embankment Design and Performance". This is Interim Report No. 6 and is titled "The Effect of Laboratory Compaction on the Shear Behavior of a Highly Plastic Clay After Saturation and Consolidation". It is authored by J. M. Johnson and C. W. Lovell of our staff. The report describes the experimental program on the effective stress strength behavior of laboratory compacted St. Croix clay. The effects of compaction water content and effort level were evaluated for the clay after it had been saturated and consolidated under confining pressures simulating various embankment positions. Prediction equations were developed for the effective stress parameters, for the pore pressure parameter at failure, and for the volumetric strain during saturation and consolidation. These equations are largely in terms of the compaction variables. Research on these relation- ships for field compacted soil continues.