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Çѱ¹Áö¹Ý°øÇÐȸ / v.21, no.5, 2005³â, pp.231-241
ÇÔ¼öºñ¿Í Áß±Ý¼Ó ¿À¿°µµ¿¡ µû¸¥ À¯Àü»ó¼öÀÇ º¯È­
( Variations of Complex Permittivity due to Water Content and Heavy Metal Contamination )
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Laboratory experiments were performed to examine the effects of water content and to see if permittivity had sufficient sensitivity to identify subsurface contamination. Both real and imaginary permittivities of unsaturated sand were strongly governed by the volumetric water content. Especially, a linear relationship between real permittivity and volumetric water content was derived at high frequencies (MHz ranges). Heavy metals in pore fluid result in significant increases in the effective imaginary permittivity, due to ionic conduction, but decreases in the real permittivity arises due to the decreased orientational polarization of water molecules caused by hydration of ions. Clear increase in the effective imaginary permittivity with heavy metal concentration was found to be valuable in the application of electrical methods for detecting heavy metals in the subsurface. However, because the permittivity is primarily dependent on the volumetric water content of soil, pre-evaluation on the volumetric water content is required.
 
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Heavy metal;Permittivity;Subsurface contamination;Volumetric water content;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.21, no.5, 2005³â, pp.231-241
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200504704326163)
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