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Agenda - 03-23-1993 - VII-A
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Agenda - 03-23-1993 - VII-A
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1/4/2017 3:04:16 PM
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BOCC
Date
3/23/1993
Meeting Type
Regular Meeting
Document Type
Agenda
Agenda Item
VII-A
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Minutes - 19930323
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\Board of County Commissioners\Minutes - Approved\1990's\1993
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Mr. Reginald Gillespie <br /> L2757-92 <br /> August 3, 1992 <br /> Page 2 <br /> Near surface geologic and manmade structures significantly influence the total <br /> magnetic field. The closer the magnetic sensor is to a near surface structure, the <br /> greater effect that structure has on changing the total magnetic field where the object <br /> is located. Magnetic susceptibility is the degree to which a substance may be <br /> magnetized. For example, formations that contain a high percentage of ferrous <br /> material (i.e., diabase dikes) would have a relatively high susceptibility whereas a <br /> formation that contains little or no ferrous materials would have a low susceptibility. <br /> Based on these two factors, magnetics could be used to determine whether these <br /> formations are present at prospective sites. <br /> Typically, these investigations involve the use of a gradiometer to determine the <br /> amount of ferrous material in the underlying formations. The earth's vertical <br /> magnetic gradient is particularly sensitive to near surface variations as they are <br /> typically very localized especially in the cases of diabase dikes. The effects of the <br /> near surface structures on the magnetic field rapidly decrease as the distance <br /> between the object and sensor increases. <br /> This method offers four key advantages: <br /> • it is non-invasive with no disturbance of the tract (i.e., trees, road <br /> cutting, drilling) <br /> • the relative quickness for conducting a survey (the site can be covered <br /> in 1 to 3 days, depending on the size of the area and level of detail of <br /> the survey) <br /> • anomalous structures can be located in the field <br /> • the minimal cost for the procedure <br /> Aquaterra has used the magnetic survey techniques for mapping diabase dikes for <br /> both water supply and ground water remediation. Although the diabase dikes are <br /> relatively impermeable, when they are injected through the older rocks, they form <br /> very permeable zones on either side of the dike which can readily transmit ground <br /> water and contaminants. Their presence is considered a major limitation for a <br /> prospective landfill site. 'Aquaterra has mapped for two clients in the Research <br /> Triangle Park over 1,500 acres of land, locating nearly 4 miles of dikes. The magnetic <br /> survey results were used to place 5 extraction wells and numerous monitoring wells <br /> for ground water remediation and one well for water supply. <br /> Electrical Resistivity Soundings <br /> Further definition of the depth to bedrock can be assessed using electrical survey <br /> methods such as DC Resistivity. Vertical electric soundings (YES) can be used to <br /> determine whether a traceable geologic bedrock unit can be found. Generally, <br /> bedrock is more resistant than soils or sediments because of the soils or sediments <br /> fluid content. If this is achieved, several lines consisting of VES will be conducted <br /> through the prospective site to determine whether this unit has continuity. The <br /> depth of the traceable unit will be determined by using a geophysical model; the <br /> AQUATERRA <br />
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