Monthly analysis of atmospheric precipitation
Year |
2018 |
Region |
Kralovehradecky |
District |
Trutnov |
Measuring programme |
HMOPS, Modry potok |
Type of measuring programme |
Throughfall spruce |
Organization |
CGS |
Matter |
Unit |
Method |
2017 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
95.9 |
132.8 |
232.3 |
9.0 |
61.5 |
35.7 |
36.2 |
76.3 |
79.2 |
22.2 |
61.3 |
106.5 |
vodivost |
µS/cm |
EC meter |
19.5 |
19.3 |
16.3 |
26.3 |
30.0 |
36.6 |
54.5 |
28.2 |
23.6 |
45.8 |
27.3 |
25.4 |
pH |
- |
pH meter |
4.82 |
4.88 |
4.78 |
4.80 |
4.67 |
4.97 |
6.68 |
5.69 |
5.63 |
5.44 |
5.42 |
4.87 |
Na+
|
ug/l |
FAAS |
540 |
440 |
320 |
680 |
430 |
350 |
250 |
280 |
230 |
210 |
260 |
590 |
K+
|
ug/l |
FAAS |
630 |
1 140 |
530 |
570 |
1 180 |
2 160 |
4 060 |
2 380 |
2 020 |
3 730 |
3 300 |
1 940 |
NH4
+
|
ug/l |
PMT |
190 |
110 |
170 |
780 |
700 |
1 650 |
4 010 |
1 610 |
1 320 |
2 430 |
650 |
630 |
Mg2+
|
ug/l |
FAAS |
150 |
150 |
110 |
160 |
260 |
360 |
330 |
180 |
130 |
370 |
140 |
160 |
Ca2+
|
ug/l |
FAAS |
450 |
420 |
350 |
690 |
1 030 |
1 170 |
940 |
650 |
530 |
1 120 |
450 |
360 |
Mn |
ug/l |
FAAS |
30.0 |
22.0 |
27.0 |
21.0 |
60.0 |
71.0 |
16.0 |
36.0 |
34.0 |
43.0 |
25.0 |
27.0 |
Zn |
ug/l |
FAAS |
23.0 |
17.0 |
2.5 |
30.0 |
25.0 |
17.0 |
13.0 |
11.0 |
2.5 |
13.0 |
2.5 |
14.0 |
Pb |
ug/l |
GF-AAS |
0.2 |
0.5 |
0.5 |
1.2 |
1.5 |
0.9 |
0.6 |
1.0 |
1.1 |
1.2 |
0.2 |
0.5 |
Cd |
ug/l |
GF-AAS |
0.02 |
0.02 |
0.02 |
0.06 |
0.06 |
0.04 |
0.02 |
0.02 |
0.02 |
0.02 |
0.02 |
0.07 |
Ni |
ug/l |
GF-AAS |
0.3 |
0.3 |
0.3 |
0.3 |
0.3 |
1.5 |
0.3 |
0.3 |
0.3 |
2.5 |
0.3 |
0.7 |
F-
|
ug/l |
ISE |
10 |
10 |
10 |
10 |
10 |
10 |
20 |
20 |
20 |
25 |
32 |
10 |
Cl-
|
ug/l |
HPLC |
1 100 |
940 |
630 |
1 180 |
1 220 |
840 |
980 |
920 |
650 |
1 030 |
1 320 |
2 020 |
NO3
-
|
ug/l |
HPLC |
1 750 |
1 780 |
1 410 |
3 730 |
3 500 |
4 990 |
6 810 |
3 860 |
3 260 |
9 650 |
3 910 |
2 820 |
SO4
2-
|
ug/l |
HPLC |
1 560 |
1 680 |
1 390 |
2 110 |
3 720 |
3 970 |
3 120 |
3 380 |
1 330 |
1 710 |
860 |
1 140 |