Monthly analysis of atmospheric precipitation
Year |
2013 |
Region |
Karlovarsky |
District |
Sokolov |
Measuring programme |
KPB1B, Pluhuv bor |
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 |
51.8 |
131.2 |
81.3 |
40.1 |
20.8 |
15.4 |
85.6 |
188.2 |
40.8 |
69.3 |
61.9 |
52.2 |
vodivost |
µS/cm |
EC meter |
9.9 |
9.3 |
15.4 |
20.0 |
17.6 |
25.1 |
12.7 |
8.9 |
14.6 |
8.9 |
8.6 |
11.9 |
pH |
- |
pH meter |
4.96 |
4.70 |
4.54 |
4.33 |
4.51 |
5.61 |
5.81 |
5.22 |
5.88 |
5.33 |
4.93 |
4.83 |
Na+
|
ug/l |
FAAS |
60 |
80 |
280 |
140 |
140 |
350 |
70 |
120 |
160 |
100 |
200 |
150 |
K+
|
ug/l |
FAAS |
50 |
30 |
50 |
30 |
50 |
170 |
190 |
130 |
540 |
110 |
50 |
80 |
NH4
+
|
ug/l |
PMT |
360 |
110 |
190 |
200 |
560 |
2 740 |
690 |
330 |
790 |
310 |
80 |
320 |
Mg2+
|
ug/l |
FAAS |
30 |
20 |
50 |
30 |
50 |
110 |
70 |
40 |
90 |
90 |
30 |
50 |
Ca2+
|
ug/l |
FAAS |
70 |
50 |
90 |
60 |
220 |
460 |
520 |
210 |
340 |
230 |
140 |
160 |
Mn |
ug/l |
FAAS |
2.5 |
8.0 |
10.0 |
6.0 |
13.0 |
18.0 |
5.0 |
2.5 |
11.0 |
2.5 |
7.0 |
6.0 |
Zn |
ug/l |
FAAS |
19.0 |
5.0 |
5.0 |
13.0 |
15.0 |
32.0 |
5.0 |
22.0 |
23.0 |
17.0 |
12.0 |
44.0 |
Al |
ug/l |
GF-AAS |
5 |
21 |
10 |
24 |
18 |
16 |
10 |
18 |
18 |
6 |
11 |
12 |
Fe |
ug/l |
FAAS |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
25 |
Pb |
ug/l |
GF-AAS |
0.2 |
0.2 |
0.2 |
0.5 |
0.4 |
0.6 |
0.2 |
1.3 |
0.8 |
0.2 |
1.2 |
1.1 |
Cd |
ug/l |
GF-AAS |
0.02 |
0.02 |
0.02 |
0.02 |
0.18 |
0.09 |
0.02 |
0.09 |
0.02 |
0.02 |
0.05 |
0.19 |
Ni |
ug/l |
GF-AAS |
5.1 |
1.1 |
0.2 |
0.4 |
1.1 |
0.6 |
0.5 |
4.9 |
2.5 |
3.6 |
2.8 |
1.8 |
F-
|
ug/l |
ISE |
10 |
10 |
10 |
10 |
10 |
23 |
10 |
10 |
10 |
10 |
10 |
10 |
Cl-
|
ug/l |
HPLC |
930 |
1 240 |
540 |
310 |
230 |
690 |
550 |
170 |
180 |
320 |
130 |
230 |
NO3
-
|
ug/l |
HPLC |
1 180 |
5 050 |
1 580 |
2 210 |
2 930 |
5 570 |
2 010 |
990 |
1 060 |
1 010 |
970 |
1 370 |
SO4
2-
|
ug/l |
HPLC |
640 |
1 830 |
250 |
910 |
810 |
2 390 |
2 690 |
830 |
680 |
910 |
660 |
520 |