My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
3210 36TH PL NE 2018-01-02 MF Import
>
Address Records
>
36TH PL NE
>
3210
>
3210 36TH PL NE 2018-01-02 MF Import
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
3/4/2022 3:27:47 PM
Creation date
3/31/2017 8:32:27 AM
Metadata
Fields
Template:
Address Document
Street Name
36TH PL NE
Street Number
3210
Imported From Microfiche
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
171
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
The results of our analyses indicate that several zones in ihe loose to medium dense sandy soils <br /> encountered in the explorations below th� organic silt have a moderate potential for liqucfaction during a <br /> design carthquake event, and a low to moderate potential during an event with a lower level of ground <br /> shaking. The organic silt and silt deposits located above the sand have a low potential for liquefaction <br /> � during a design eaRhquake(a magnitude G.5 earthquake with a PGA of 0.27g). <br /> I Our analyses indicate that settlements caused by liquefaction of the saturated loose to medium dense sand <br /> � layers at this site during a design carthyuake could be on the order of 1 to 3 inches. Foundations for the <br /> I planned structums will be cunstructed ovcr tl�e liquefiable suils and will therefore be prone to liqueiaction <br /> induced settlement. Because of thc random nature of liquefaction, differential settlements may be on thc <br /> same order as the total setdements. However, surface expression of the differential szttlement may Uc <br /> reduced duc to the anticipated fill placement above existing site grades. <br /> In addition to setdements, there is the possibility that lateral spreading of the soils could occur as a resuk <br /> of liquclaction. I.ateral spreading involves la[eral displacemcnt of largc, surficial blocks of non-liquefied <br /> soil, as well as the liquefied soil, as the underlying soil layer liquefes. Lateral spreading generally <br /> Idevclops in areas whcre sloping ground is present or near a free face, such as a river or slough. It <br /> liquefaction were to occur within Ihe sands at the site, we anticipa[c that [here �eould be a modcratc <br /> � potential for lateral spreading to occur, characterizcd by movement of thc soils to���ards the Snohomish <br /> i Ri��er or Steamboat Slough. In general, the magnitude of latcral spmad will decrease with increasing <br /> distance behveen the point of interest and Ihe Snohomish Itiver or Steamboat Slaugh. During a design <br /> earthquake, lateral spread displaccments across the site are estimated to be on die order of 0.� to 1.5 feet. <br /> I . . , <br /> The design recommendations for the structural foundations presented abo�e do not take into the account <br /> the e[fects of liquefaction and laieral sprcading. Measures to mitigate the eCfects of' lateral spreading <br /> includc constructing a foundation systcm that will effectively limit lateral spreading, or <br /> densifying/minforcing the Gquefiable soils. Remediation would most likely consist of densifying the sand <br /> deposits with methods such vibrocompaction or installing stone c�lumns. These mitigation measures are <br /> typic.Ily very cosdy and not common;y accomplished for projccts of this rype. <br /> We recommend that Concrete Nor'nest be made aware of d�c risks associated with liquefaction and <br /> I lateral spreading a[ this site. We can provic(c recommendations for mitigating the seismic harard at die <br /> � site upon reyuest. <br /> 2003 IBC Seismic Design Information <br /> We rccommend the 2003 Intemational Building code (IBC) parameters be used for project d�sign. Based <br /> on our interpretation oi the conditions encounrered during our field subsurface borings, test pits, and C['T <br /> explorations, we conclude the project si.e is classified as Site Class �, as defined in the 2003 [BC. The <br /> design parameters for the 2003 IBC are summarized in Table 3. The Site Class, short penod spectral <br /> response accelrration (SS), I-second period spectral response acceleration (SI), and Seismic Coefficients <br /> F,� and r�prescnted in Tablc 3. <br /> Fi(c No.8937-001-00 Page 18 �iEOENGINEEfl� <br /> Oc�oGcr!/,?006 <br />
The URL can be used to link to this page
Your browser does not support the video tag.