Monthly analysis of atmospheric precipitation
Year |
2016 |
Region |
Karlovarsky |
District |
Sokolov |
Measuring programme |
KPB2S, Pluhuv bor |
Type of measuring programme |
Throughfall spruce |
Organization |
CGS |
Matter |
Unit |
Method |
2015 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
73.1 |
59.2 |
37.7 |
57.9 |
26.9 |
12.2 |
27.5 |
78.7 |
78.6 |
41.9 |
70.4 |
47.0 |
vodivost |
µS/cm |
EC meter |
33.5 |
26.8 |
30.8 |
24.0 |
39.8 |
55.6 |
68.1 |
19.6 |
21.9 |
24.5 |
37.1 |
27.1 |
pH |
- |
pH meter |
5.24 |
4.83 |
4.77 |
4.81 |
5.09 |
5.22 |
5.83 |
4.96 |
5.22 |
5.18 |
4.62 |
4.76 |
Na+
|
ug/l |
FAAS |
465 |
430 |
580 |
410 |
420 |
620 |
750 |
180 |
150 |
190 |
190 |
190 |
K+
|
ug/l |
FAAS |
1 165 |
1 140 |
935 |
1 385 |
3 940 |
1 135 |
3 020 |
1 785 |
1 515 |
1 200 |
1 825 |
1 340 |
NH4
+
|
ug/l |
PMT |
515 |
485 |
560 |
200 |
400 |
2 680 |
3 730 |
195 |
750 |
555 |
1 320 |
590 |
Mg2+
|
ug/l |
FAAS |
1 365 |
775 |
905 |
540 |
1 195 |
1 020 |
1 320 |
455 |
330 |
305 |
465 |
590 |
Ca2+
|
ug/l |
FAAS |
465 |
575 |
730 |
535 |
710 |
1 700 |
1 425 |
515 |
455 |
565 |
840 |
815 |
Mn |
ug/l |
FAAS |
175.0 |
129.5 |
168.0 |
99.0 |
204.0 |
186.5 |
214.5 |
64.0 |
68.5 |
58.5 |
105.0 |
133.5 |
Zn |
ug/l |
FAAS |
13.5 |
14.0 |
14.5 |
5.0 |
15.5 |
52.5 |
34.5 |
25.5 |
7.5 |
13.5 |
16.5 |
47.5 |
Pb |
ug/l |
GF-AAS |
1.4 |
1.5 |
1.7 |
1.0 |
1.5 |
0.8 |
1.5 |
1.0 |
0.8 |
0.6 |
1.4 |
0.9 |
Cd |
ug/l |
GF-AAS |
0.03 |
0.05 |
0.08 |
0.02 |
0.06 |
0.06 |
0.10 |
0.05 |
0.02 |
0.04 |
0.05 |
0.06 |
Ni |
ug/l |
GF-AAS |
3.3 |
3.0 |
4.1 |
2.7 |
3.7 |
2.7 |
5.0 |
3.4 |
1.6 |
2.0 |
2.8 |
2.5 |
F-
|
ug/l |
ISE |
45 |
10 |
10 |
10 |
10 |
24 |
16 |
30 |
10 |
10 |
26 |
10 |
Cl-
|
ug/l |
HPLC |
1 960 |
1 470 |
1 410 |
875 |
960 |
1 335 |
2 225 |
465 |
335 |
945 |
670 |
675 |
NO3
-
|
ug/l |
HPLC |
2 980 |
5 560 |
6 440 |
4 970 |
7 160 |
13 650 |
15 560 |
50 |
3 460 |
5 660 |
10 910 |
6 950 |
SO4
2-
|
ug/l |
HPLC |
1 070 |
1 600 |
2 730 |
1 230 |
4 770 |
5 930 |
7 420 |
1 770 |
1 410 |
2 340 |
2 930 |
2 920 |