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2400 33RD ST GEOTECHNICAL INVESTIGATION 2018-01-02 MF Import
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2400 33RD ST GEOTECHNICAL INVESTIGATION 2018-01-02 MF Import
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Last modified
12/15/2021 3:49:33 PM
Creation date
4/1/2017 3:36:00 PM
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Address Document
Street Name
33RD ST
Street Number
2400
Tenant Name
GEOTECHNICAL INVESTIGATION
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sc 130 Milbor-Pita <br />Woanrra arc <br />impermeable due to the variety nf grain sizes. Typically, it does have <br />discontinuous seams of sandier material that may contain water. <br />4.2.2.5 Silty Sand — Advance Outwash <br />Below the till in the deeper borings is a silty to clean medium sand unit. It is <br />interlayered with silt and clay seams, probably formed as the glacier made minor <br />advances and retreats. <br />4.2.3 Groundwater <br />There are several :..)nes of groundwater below the site, however they appear to be <br />discontinuous. There is a zone within the upper five feet of material, along the top of the <br />stiff silt unit. This appears to be seasoi:al, indicating that is it fed by precipitation rather <br />than a regional groundwater zone. The silt/clay itself does have some sandier lenses that <br />appear to be slightly more permeable and contain small amounts of water. There is <br />another zone on the top of the till at a depth of approximately 18 to 20 feet, which is <br />sometimes present as a softer zone within the overlying silt. These water -bearing layers <br />are referred to as "perched" water zones. The true regional groundwater level is at <br />approximately 35 to 39 feet below the site. This zone was encountered in MP-5 at a <br />depth of 38 feet, and the water level rose to 17.5 feet within minutes, indicating that it is <br />confined below the till and silt. A true water level was not obtainable due to water <br />flowing into the well from an upper perched water zone. The drilling became difficult <br />below 38 feet due to the sand "heaving" into the boring due to the upward pressure of the <br />confined water. <br />5.0 CONCLUSIONS AND RECOMMENDATIONS <br />The results of our exploration program indicate that compressible silt/clay deposits <br />overlying dense, glacially consolidated till deposits are bedded relatively uniformly <br />beneath the site. The fill and silt/clay will not provide adequate support for the proposed <br />structure due to settlement. If the silt/clay is over -excavated and replaced with structural <br />fill placed from the underlying dense soil to the footing elevation, the resulting bearing <br />capacity on the structural fill would be 5,000 pounds per square foot. <br />Deep foundation alternatives include drilled shafts (piers), auger -cast piles, and driven <br />piles. These are discussed in Section 5.3.2 below. <br />The following sections contain recommendations on seismic design criteria, building <br />foundation design, pavement design, deep foundation design (including axial <br />compression, pull-out and lateral analysis), lateral earth pressures, general earthwork <br />considerations, temporary excavations, and site drainage and erosion considerations. <br />5.1 Site Earthwork <br />5.1.1 Pre-Subgrade Preparation <br />Prior to earthwork operations, the site's demolition debris should be removed and the <br />ground cleared of all deleterious materials, including buried pipelines, building <br />foundations and floor slabs, vegetation and buried organic rich soil and/or wood debris, <br />(n-otcchnical, tuuicl mid Environmental Ingmeas <br />3080 125" Ave NE Phone (425) 869-5778 <br />ncllme, WA 98005 Pages Fax (425)861-0677 <br />
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