198
]
c
..
o
.
Q
~ 0 - - -
C)
~"O~~
:
.-~ :;L """ :a.
o
~QOO
- 0 0
-0 ..... I I ,..
'" DOOE!
T. Schiindorf et al.
Fig. 9. Plumes of dissolved mercury of
groundwater
day) than can be transferred by the groundwater recharge. This is confirmed by
investigation results of the aquifer matrix in the immediate downgradient area
where a significant Hg abundance was found to exist with still mobilizable
fractions in the aquifer and the groundwater fluctuation zone.
]
c
..
o
.
Q
~ 0 - - -
C)
~"O~~
:
.-~ :;L """ :a.
o
~QOO
- 0 0
-0 ..... I I ,..
'" DOOE!
T. Schiindorf et al.
Fig. 9. Plumes of dissolved mercury of
groundwater
day) than can be transferred by the groundwater recharge. This is confirmed by
investigation results of the aquifer matrix in the immediate downgradient area
where a significant Hg abundance was found to exist with still mobilizable
fractions in the aquifer and the groundwater fluctuation zone.