کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6318637 | 1619198 | 2013 | 10 صفحه PDF | دانلود رایگان |
An estimated 229Â 000Â m3 of coal fly ash remains in the river system after dredging to clean-up the 2008 Tennessee Valley Authority (TVA) spill in Kingston, Tennessee. The ash is heterogeneous with clear, orange and black spheres and non-spherical amorphous particles. Combustion produces iron oxides that allow low field magnetic susceptibility (ÏLF) and percent frequency dependent susceptibility (ÏFD%) to be used to discriminate between coal fly ash and sediments native to the watershed. Riverbed samples with ÏLF greater than 3.0Â ÃÂ 10â6Â m3/kg, have greater than 15% ash measured by optical point counting. ÏLF is positively correlated with total ash, allowing ash detection in riverbed sediments and at depth in cores. The ratio of ash sphere composition is altered by river transport introducing variability in ÏLF. Measurement of ÏLF is inexpensive, non-destructive, and a reliable analytical tool for monitoring the fate of coal ash in this fluvial environment.
⺠Coal fly ash is composed of spheres (clear, orange, black) and amorphous particles. ⺠Black spheres dominate the magnetic susceptibility signal (ÏLF). ⺠The river sorts ash but maintains a ratio of clear: orange: black ash. ⺠ÏLF measurements can predict % ash spheres from simple linear regression. ⺠ÏLF can be used to track coal ash in the riverbed and in sediment cores.
Journal: Environmental Pollution - Volume 174, March 2013, Pages 179-188