Monthly analysis of atmospheric precipitation
Year |
2013 |
Region |
Karlovarsky |
District |
Cheb |
Measuring programme |
KLY1B, Lysina |
Type of measuring programme |
Bulk samples |
Organization |
CGS |
Matter |
Unit |
Method |
2012 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
70.4 |
232.6 |
115.3 |
48.9 |
28.8 |
30.2 |
170.0 |
216.1 |
33.6 |
93.4 |
91.9 |
52.3 |
vodivost |
µS/cm |
EC meter |
8.3 |
8.4 |
14.7 |
20.2 |
16.7 |
18.8 |
8.9 |
8.9 |
14.5 |
9.4 |
8.7 |
9.1 |
pH |
- |
pH meter |
5.02 |
4.76 |
4.53 |
4.37 |
4.52 |
5.20 |
5.63 |
6.21 |
6.11 |
5.10 |
4.91 |
4.85 |
Na+
|
ug/l |
FAAS |
60 |
90 |
250 |
130 |
130 |
280 |
40 |
140 |
710 |
140 |
200 |
400 |
K+
|
ug/l |
FAAS |
20 |
50 |
40 |
20 |
50 |
140 |
70 |
210 |
400 |
60 |
170 |
390 |
NH4
+
|
ug/l |
PMT |
310 |
130 |
240 |
370 |
640 |
1 950 |
410 |
450 |
710 |
270 |
110 |
250 |
Mg2+
|
ug/l |
FAAS |
10 |
70 |
40 |
20 |
30 |
60 |
20 |
50 |
130 |
60 |
20 |
80 |
Ca2+
|
ug/l |
FAAS |
50 |
90 |
70 |
60 |
140 |
260 |
200 |
250 |
670 |
210 |
130 |
160 |
Mn |
ug/l |
FAAS |
2.5 |
7.0 |
2.1 |
2.5 |
2.5 |
2.5 |
2.5 |
9.0 |
7.0 |
2.5 |
7.0 |
8.0 |
Zn |
ug/l |
FAAS |
15.0 |
20.0 |
5.0 |
5.0 |
15.0 |
29.0 |
5.0 |
187.0 |
117.0 |
18.0 |
74.0 |
79.0 |
Al |
ug/l |
GF-AAS |
5 |
154 |
18 |
21 |
31 |
17 |
6 |
35 |
31 |
20 |
34 |
45 |
Fe |
ug/l |
FAAS |
25 |
180 |
50 |
25 |
25 |
25 |
25 |
50 |
25 |
25 |
25 |
25 |
Pb |
ug/l |
GF-AAS |
0.7 |
0.2 |
0.4 |
0.7 |
0.9 |
7.6 |
0.2 |
4.0 |
4.3 |
0.3 |
3.9 |
8.6 |
Cd |
ug/l |
GF-AAS |
0.02 |
0.06 |
0.02 |
0.02 |
0.51 |
0.28 |
0.02 |
0.74 |
0.39 |
0.04 |
0.17 |
1.37 |
Ni |
ug/l |
GF-AAS |
|
|
|
|
|
|
|
|
|
|
|
|
F-
|
ug/l |
ISE |
26 |
40 |
40 |
40 |
40 |
44 |
40 |
40 |
40 |
40 |
40 |
25 |
Cl-
|
ug/l |
HPLC |
320 |
300 |
450 |
560 |
240 |
660 |
460 |
380 |
150 |
400 |
180 |
260 |
NO3
-
|
ug/l |
HPLC |
1 190 |
1 140 |
1 650 |
2 490 |
3 000 |
4 560 |
1 170 |
1 060 |
1 430 |
1 560 |
1 450 |
1 130 |
SO4
2-
|
ug/l |
HPLC |
920 |
390 |
880 |
1 940 |
850 |
1 000 |
630 |
1 460 |
810 |
1 410 |
1 020 |
510 |