Subsurface Conditions Mission Bay San Francisco, California Presented by Hadi J. Yap, PhD, PE, GE DTX Project Meeting San Francisco County Transportation.

Slides:



Advertisements
Similar presentations
Engineering the Geological Chaos of Franciscan and Other Bimrocks
Advertisements

Soil The product of weathering of rocks
Features of EROSION & Features of DEPOSITION
1 Prepared for: International Society for Micropiles (ISM) 2009 International Workshop on Micropiles London, England May 13 th, 2009 A DECADE OF LOAD HOLD.
Soil Portfolio By Tim Butterfield. What is soil? Soil is the medium in which crops are grown to feed human and other living things. It is also is a loose.
MASS MOVEMENTS. IMPORTANT CONCEPT: ROLE OF GRAVITY Gravity causes the downward and outward movement of landslides and the collapse of subsiding ground.
Richmond/San Rafael Bridge HIGH CAPACITY MICROPILE CONSTRUCTION AGRA Foundations, Inc.
For flow of 1 m/s in round-bottom channel of radius 1 m, what is the Reynold’s number? Is the flow laminar or turbulent? Re < 500 laminar Re > 2000 turbulent.
FIXED MARINE STRUCTURES
USING THE RAPID LOAD TESTER TO PROVIDE PROJECT QUALITY CONTROL.
Earthquake induced LIQUEFACTION by Jimmy McLauchlan Peat Nicholas Case study: Mexico City, 1985.
Geotechnical Investigation Step 1 - Gather Existing Information Structure Data Bridge, building, road, wall, etc. Type - stories, loads, materials, etc.
Soils of Wisconsin Topic C. Soil Uncemented aggregate of mineral grains and decayed organic matter with liquid and gas in the empty spaces between the.
Soils in Construction (Engineering)
The four components of soil:
Bricks Introduction Structural member Load transfer medium
Issues to be considered :foundations Professor Chris Gorse and Ian Dickinson These slides should be read in conjunction with Emmitt, S. and Gorse, C. (2010)
Local Site Effects Seismic Site Response Analysis CEE 531/ESS 465.
Pile Testing and Evaluation for the Sand Creek Byway, Sandpoint, Idaho Presented by Dean E. Harris, P.E., CH2M HILL.
Classification, Engineering Properties & Consolidation Methods.
Abstract Earthquakes are one of the most powerful natural disasters that occur in the world. Ground motion and shaking during an earthquake can be detected.
Soils Investigation Soil Investigation
COMPACTION Topic COMPACTION Presented to Dr. Ayub Elahi Presented by Group leader. M.Zeeshan haider yousaf Zia. # 14 Haider ayub # 13 Bilal ansari #35.
 Soil grains come from weathering of bedrock ◦ Physical weathering – granular soils ◦ Chemical weather – creates clay  Soil is either residual or transport.
Commercial Foundations
Earthquakes. Describing Earthquakes Intensity vs. Magnitude.
But they are clustered along the Pacific Coast. Why?
Collection, Preparation
Un-hardening Phenomenon of SCW (Soil Cement Wall) Built in Organic Soils Chung R. Song, Ph. D, PE Department of Civil Engineering The University of Mississippi.
February Chagrin Loam Proposed Method of Management French Drain Vertical “Pit” Drains ~2 Feet Wide 10 Feet Deep 120 Feet Long 1 Foot 8 Inches.
Soil! By: Oksanna Loya.
Soil covers much of the land on Earth. Provides a substrate for plants to anchor their roots. Provides homes for many animals.
Copyright © 2006 Pearson Education, Inc., publishing as Benjamin Cummings World soil conditions Soils are becoming degraded in many regions.
Water Movement Below Surface
The Ground Beneath Our Feet
Soil By, Mrs. Schuette’s Second Grade Class 2013.
Soils. Soil Weathering and erosion transports materials across Earth’s surface Weathering and erosion transports materials across Earth’s surface The.
THE NATURE OF SOIL By Sarik Salim. The nature of Soil Soil is defined as a collection of mineral particles that was formed due to the weathering process.
SOIL NCES: 6.E.2.3 & 2.4 Kim Lachler Updated 11/11/14.
12.2 Soil Key Ideas: Soil is made of weathered rock and organic material. Climate and other factors affect the composition of the soil.
SMALL-SCALE SPATIAL VARIATION OF WATER QUALITY WITHIN THE MISSISSIPPI RIVER VALLEY ALLUVIAL AQUIFER ARKANSAS, USA Ken Steele 1, Tim Kresse 2 and Ralph.
HEWLETT PACKARD BUILDING 5 SEISMIC UPGRADE CORVALLIS, OREGON, USA TOM A. ARMOUR, P.E. SESSION III STRUCTURAL SUPPORT & SEISMIC APPLICATIONS IWM 2002 MAY.
Geotechnical Engineering
Nathan D. Webb.  Background  Pennsylvanian oil production  Stratigraphy & geologic setting  Study area  Methods  Geophysical log correlation & facies.
Ch 5 - Soils Important effect of weathering for people!
1 BROOKHAVEN SCIENCE ASSOCIATES NSLS – II CFAC Review Conventional Facilities Geotechnical Conditions Tom Joos Civil/Structural Engineer BNL Plant Engineering.
Classical and Finite Difference Method to Estimate pile Capacity Compared With Pile Load Test Results Yogesh Prashar, P.E., GE Force Pulse Conference,
Soils: One of Our Natural Resources!. Some call it dirt…..But it is Soil !!! Soil is made of loose, weathered rock and organic material.
Soil No soil, No planet Earth. Soil Terminology Vocabulary: Soil Horizon – layers or zones of soil. Soil profile: different zones or layers starting at.
Soils: One of Our Natural Resources!. Some call it dirt…..But it is Soil !!! Soil is made of loose, weathered rock and organic material.
Student Concept Map Sedimentary Rocks Dr. David Steer.
Engineering Presentation. Basic Soil Mechanics Soil type classification Gravel, sand, silt, clay Soil strength classification Granular soils (sand and.
Deserts. Arid Climates In an arid climate rainfall is 400mm (15.6 in) per year. Evaporation rate _______ precipitation. Thus, both deserts and the extreme.
Geotechnical Investigation Report
Day 19 Objective You will learn about soil texture and composition in order to determine soil’s value as a resource and conservation measures. Warm-Up.
Soils and Growing Media
Soil Formation and Composition.  I. Soil Formation –A. When bedrock is exposed, it weathers. –B. Particles of rock mix with other material. –C. Soil.
Soil concepts and characteristics of soils. INTRODUCTION Soil - covers most of the earth’s land surface Soil - natural medium for the growth of plants.
What Environment are Sedimentary Rocks Formed?
Geotechnical Investigation
Richmond/San Rafael Bridge HIGH CAPACITY MICROPILE CONSTRUCTION
October 11, 2011.
Sedimentary Rocks.
Structural Analysis - What is it?
The Ground Beneath Our Feet
The Ground Beneath Our Feet
Soil is A loose mixture of small minerals and rock fragments, organic material, water, and air.
The Ground Beneath Our Feet
Roger A. Failmezger, P.E., F. ASCE, D. GE
The Ground Beneath Our Feet
Presentation transcript:

Subsurface Conditions Mission Bay San Francisco, California Presented by Hadi J. Yap, PhD, PE, GE DTX Project Meeting San Francisco County Transportation Authority 11 October 2011

Mission Bay Site Location

United States Coast Survey Map - February 1852

1982 Aerial Photograph with 1857 Coast Survey Overlay

T&R Projects in the area

N3A 42 28

Typical Stratigraphic Layers Fill Bay Mud Colma Sand Old Bay Clay Colluvium/Alluvium Franciscan Complex Bedrock

Typical Stratigraphic Layers Fill –Non-engineered, generally loose to medium dense –Heterogeneous material consisting of sand, clay, silt, gravel, bedrock fragments, abandoned structures, construction debris, and organics

Typical Stratigraphic Layers Bay Mud –Soft clay and silt with occasional sand lenses and organic material –Low strength and high compressibility

Typical Stratigraphic Layers Colma Formation –Dense to very dense sand with occasional clay lenses –Generally contains up to 20% fines (silt and clay) –High strength and low compressibility

Typical Stratigraphic Layers Old Bay Clay –Stiff to hard clay and silt –Occasionally contains sand and gravel lenses –Moderate strength and moderate compressibility

Typical Stratigraphic Layers Colluvium –Dense sands and gravels and stiff to hard clays –High strength and low compressibility

Typical Stratigraphic Layers Franciscan Complex bedrock –Deformed bedding planes and shear zones due to seismic activity –Highly variable in hardness & strength –Deeply to moderately weathered –High strength and low compressibility

N3A 42 28

Idealized subsurface Conditions – Block 42