Monthly analysis of atmospheric precipitation
Year |
2017 |
Region |
Karlovarsky |
District |
Cheb |
Measuring programme |
KNZ2S, Na Zelenem |
Type of measuring programme |
Throughfall spruce |
Organization |
CGS |
Matter |
Unit |
Method |
2016 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
35.8 |
32.0 |
26.2 |
24.9 |
56.8 |
25.7 |
63.3 |
35.1 |
57.8 |
56.5 |
45.6 |
87.3 |
vodivost |
µS/cm |
EC meter |
41.5 |
64.3 |
33.9 |
82.1 |
26.8 |
56.5 |
39.8 |
26.0 |
32.9 |
33.7 |
27.3 |
39.9 |
pH |
- |
pH meter |
4.90 |
4.66 |
4.66 |
4.36 |
5.08 |
4.93 |
4.75 |
5.17 |
6.62 |
6.68 |
6.22 |
5.44 |
Na+
|
ug/l |
FAAS |
560 |
1 380 |
950 |
1 730 |
750 |
840 |
480 |
370 |
280 |
240 |
240 |
880 |
K+
|
ug/l |
FAAS |
3 820 |
7 160 |
1 810 |
4 840 |
1 780 |
2 570 |
3 250 |
4 760 |
2 650 |
3 080 |
2 090 |
4 010 |
NH4
+
|
ug/l |
PMT |
1 110 |
1 010 |
560 |
660 |
1 020 |
3 090 |
1 240 |
80 |
2 010 |
2 180 |
1 640 |
580 |
Mg2+
|
ug/l |
FAAS |
360 |
870 |
450 |
1 540 |
300 |
490 |
340 |
290 |
200 |
160 |
110 |
320 |
Ca2+
|
ug/l |
FAAS |
1 260 |
1 990 |
1 050 |
3 480 |
720 |
1 470 |
1 010 |
800 |
720 |
660 |
420 |
720 |
Mn |
ug/l |
FAAS |
207.0 |
522.0 |
266.0 |
1010.0 |
236.0 |
247.0 |
165.0 |
134.0 |
13.0 |
14.0 |
11.0 |
168.0 |
Zn |
ug/l |
FAAS |
77.0 |
37.0 |
25.0 |
48.0 |
28.0 |
39.0 |
20.0 |
14.0 |
5.0 |
10.0 |
5.0 |
5.0 |
Pb |
ug/l |
GF-AAS |
1.6 |
1.6 |
0.7 |
1.9 |
1.2 |
2.0 |
1.1 |
0.7 |
0.2 |
0.3 |
0.2 |
0.5 |
Cd |
ug/l |
GF-AAS |
0.08 |
0.10 |
0.08 |
0.21 |
0.06 |
0.12 |
0.11 |
0.06 |
0.02 |
0.02 |
0.02 |
0.06 |
Ni |
ug/l |
GF-AAS |
1.1 |
1.3 |
0.7 |
1.4 |
1.9 |
1.9 |
1.3 |
1.6 |
0.8 |
0.8 |
0.5 |
0.8 |
F-
|
ug/l |
ISE |
44 |
10 |
10 |
28 |
10 |
10 |
10 |
24 |
10 |
33 |
37 |
23 |
Cl-
|
ug/l |
HPLC |
2 150 |
4 110 |
1 880 |
3 160 |
1 470 |
1 830 |
940 |
1 310 |
780 |
1 080 |
1 020 |
5 390 |
NO3
-
|
ug/l |
HPLC |
4 220 |
7 660 |
4 860 |
11 930 |
4 250 |
12 540 |
7 680 |
50 |
3 780 |
5 210 |
3 630 |
3 070 |
SO4
2-
|
ug/l |
HPLC |
4 030 |
7 030 |
3 580 |
12 350 |
1 800 |
5 080 |
2 900 |
1 070 |
870 |
1 270 |
1 360 |
1 260 |