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(a)
30
1000 t /d
ALL VOLCANOES
(Burton et al. , 2013)
25
20
15
10
5
1
1.5
2
2.5 3
Log CO 2
3.5
4
4.5
5
(b)
Aiuppa et al. , 2011
ETNA
7
500 t/d
STROMBOLI
5000 t /d
6
Aiuppa et al. , 2006
10 000 t /d
5
Burton
et al. , 2007
4
Aiuppa et al. , 2008
Allard et al. , 1991
3
2
1
Allard et al. , 1994
0
1
1.5
2 .53
Log CO 2
3.5
4
4.5
5
Figure 6.6
(a) Histogram of volcanic CO 2
fluxes (log scale) for the 33 volca-
noes listed in Burton et al .( 2013 ); CO 2
fluxes span three orders of magnitude,
with a mode at ~ 1000 t/day. (b) Histogram of CO 2
fluxes (log scale) for
Stromboli (white; data are for 5 years of daily CO 2 measurements during
2006
2011; from Aiuppa et al ., 2011 ) and Etna (black; 3 years of daily CO 2
measurements during 2009
-
-
2011; from Patanè et al ., 2013 ). Previous CO 2
two orders of
magnitude) temporal variations of CO 2 emissions from both volcanoes cast
doubts on the validity of campaigns involving spot measurements, and empha-
sise the need for continuous long-term observations of CO 2
flux estimates for both volcanoes are indicated. The large (
>
flux using perman-
ent networks.
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