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12-13446
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2012
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12-13446
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Last modified
7/18/2013 10:45:07 AM
Creation date
7/18/2013 10:45:03 AM
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Building Department
Building Department - Doc Type
Permit
Permit #
12-13446
Building Department - Name
QUIROS MARTINEZ,ELIAS
Address
5411 TANGERINE DR
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Subsidence lnvt;stigation SDII Project Number•3023547 <br /> Quiros-Martir�ez Residence-Zephyrhills,Florida <br /> Evidence of sinkhole activity was identified at the site, including: (1) the systematic pattern of <br /> declining N �ralues through clay-rich soils overlying limestone in SPT borings B-] and B-2; (2) <br /> multiple feet �f weight-of-rod/hammer strength materials overlying limestone in SPT borings B- <br /> 1 and B-2; and (3) the rapid losses of drilling fluid circulation above the limestone in SPT <br /> borings B-1 a�nd B-2. <br /> 2.4 Labo�ratory Soil Analysis <br /> Laboratory arialyses of soils are used to determine the suitability of the soil for construction and <br /> load bearing ,:�s well as for quality-control purposes. The analytical methods for laboratory tests <br /> included in th is investigation are summarized in Appendix A. Results from the tests are provided <br /> in Appendix 1=). <br /> Particle size �inalyses were perfonned on soil samples collected from hand auger borings HA-1 <br /> and HA-4 an�� SPT boring B-2 (Figure 4) for quality control purposes. The laboratory data <br /> indicated that the samples were poorly graded sand (SP) with approximately 3 percent fines <br /> content, poorl;y graded sand with silt (SP-SM) with approximately 7 percent fines content, and <br /> clayey sand (�SC) with approximately 14 to 23 percent fines content. The clay- or silt-sized <br /> fractions were not present in quantities sufficient to indicate a concern for soil suitability. <br /> 2.5 Geolo�;ic and Geotechnical Evaluation Summary <br /> The SPT data indicate that sinkhole activity, as defined by §627.706 Florida Statutes, exists at <br /> the site. Evicience of sinkhole aciivity was identified at the site, including: (1) the systematic <br /> pattern of decl ining N values through clay-rich soils overlying limestone in SPT borings B-1 and <br /> B-2; (2) multi.ple feet of weight-of-rod/hammer strength materials overlying limestone in SPT <br /> borings B-] a��.d B-2; and (3)the rapid losses of drilling fluid circulation above the limestone in <br /> SPT borings B-1 and B-2. <br /> 2-3 <br />
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