Ae. Foscolos et al., ASSESSMENT OF ENVIRONMENTAL-IMPACT OF COAL EXPLORATION AND EXPLOITATION IN THE DRAMA BASIN, NORTHEASTERN GREEK-MACEDONIA, Energy sources, 20(9), 1998, pp. 795-820
Forty-three samples of lignites and their partings from sir boreholes
from the Drama Basin, Macedonia, in northwestern Greece were analyzed
for their mineralogy and geochemistry. Mineralogical analysis of low t
emperature (120 degrees C) ashes indicates that quartz and gypsum are
present in all samples, while feldspars, clay minerals, and pyrite are
present in most samples. Amphiboles, magnetite, diopside, anatase, si
derite, stromayerite, and kizerite are encountered in order of abundan
ce in fewer samples. In addition, calcite is present in all partings.
Mineralogical analysis of high temperature (855 degrees C) ashes revea
ls the presence of quartz, feldspars, anhydrite, and hematite in most
of the samples while maghemite, lime, and rutile are encountered in or
der of abundance in fewer samples. Sulfur content of these lignites is
low to medium (0.4-1.17 percent daf) and is mostly inorganic (sulfur
associated with mineral matter). Sulfur associated with macerals (orga
nic sulfur) as determined in low temperature ash ranges between 0.3-11
.9 percent of total sulfur. Most elements in these lignites are associ
ated with mineral matter or do not show any preference, except Br, Hf;
Mn, Mo, Sb, U, and V, which are bound to coal macerals (organic). The
source of As, Mo, Sb, U, V, and W, which is encountered in high conce
ntrations, is due to the surrounding crystalline rocks. These elements
are mobilized and transported by surficial water, deposited syngeneti
cally in the peat swamp and finally incorporated in the lignite.