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<br />Subsidence Investigation <br />Mathew/Aley Rental Property <br />Claim No. 223968 <br /> <br />BCI Project No. 03-15564 <br />November 2007 <br />Page 9 <br /> <br />4.0 CONCLUSIONS <br /> <br />It is BCl's professional opinion that the distress to the Mathew/Aley rental property can be attributed to a <br />combination of factors, including possible sinkhole activity. Based on the results of our investigation, the minor <br />cracking distress to the house is due to minor differential settlement of the foundation, which can be attributed, in <br />part, to the to the long-term densification of the very loose to loose sandy soils that locally underlie the structure. <br />However, the occurrence and morphology of the ground collapse feature below the front porch exhibited the <br />typical characteristics of a cover-collapse sinkhole. When this condition is considered with the localized zone of <br />very soft and unstable limestone encountered in boring SPT-3, it appears that sinkhole activity may be affecting <br />the house to some extent. The analysis described in this report is of sufficient scope to identify sinkhole activity, <br />as defmed by S627. 706-707 Florida Statutes, as a possible contributing cause of the damage with a reasonable, <br />professional probability. <br /> <br />Primary factors in our conclusions include the following: <br /> <br />. Based on our test pit excavations, the house foundation is embedded at a depth of 16 inches below grade. <br />The addition foundation is embedded at a depth of approximately 4 inches below grade. The hand cone <br />penetrometer probings indicate the surficial sandy soils around the perimeter of the house are very loose <br />to loose to depths ranging from 64 to greater than 96 inches below grade. In the SPT borings, very loose <br />to loose sands were encountered to depths up to 10 feet below grade. These data indicate the house and <br />addition foundations are locally bearing on very loose to loose sandy soils, which are susceptible to the <br />effects of long-term densification. Given these soil conditions, some minor differential settlement of the <br />foundation and slab structures and associated minor cracking would be expected to occur. In addition, a <br />lack of rain gutters along the roof drip edges can result in excessive amounts of moisture being introduced <br />into the near surface sandy soils. This would act to increase the densification effects. <br /> <br />. The occurrence and morphology of the collapse feature under the front porch was typical of a recently <br />formed cover-collapse sinkhole. The feature widened with depth, was steeped sided and lacked any <br />association with buried debris that would suggest a shallow origin for the collapse. <br /> <br />8 Evidence of unstable limestone was encountered in boring SPT-3, located on the south side of the house. <br />In the boring, a significant interval of very soft limestone (weight-of-hammer) was encountered from 38Y2 <br />to 47 feet below grade. In addition, a loss of drilling fluid circulation was associated with the very soft <br />rock zone. When these subsurface conditions are considered in conjunction with the cracking distress to <br />the house and the nearby ground collapse, it appears that minor ground settlement associated with soil <br />raveling and a developing sinkhole condition may be impacting the structure to some extent. <br /> <br />Overall, the current level of cracking distress to the house is minor. However, remedial measures to <br />stabilize the house against further sinkhole-related settlement should be implemented. The ground collapse <br />feature should be filled with flowable fill (sand-cement mixture) to stabilize and prevent further enlargement of <br />the collapse. In addition, a program of compaction grouting is recommended to address the deeper subsurface <br />zones of very soft and apparently raveled soils. Since the grouting will likely not be fully effective in stabilizing <br />the shallow very loose sands directly below the foundation, a program of shallow chemical grouting is also <br />recommended. While marginally anomalous elevation differentials were found in the floor elevation survey, the <br />minor cracking distress to the structure indicates the elevation anomalies largely are not related to significant <br />movement of the foundation or floor slab. Given these conditions, foundation underpinning to re-level the <br />structure is not necessary. We also recommend that rain gutters with downspout extensions that discharge <br />stormwater a minimum of 4 feet from the foundation be installed on all roof drip edges. A remediation plan is <br />included with this report. <br />