Monthly analysis of atmospheric precipitation
Year |
2019 |
Region |
Stredocesky |
District |
Kolin |
Measuring programme |
SLESS, Lesni potok |
Type of measuring programme |
Throughfall spruce |
Organization |
GLI AS CR |
Matter |
Unit |
Method |
2018 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
32.1 |
20.7 |
39.5 |
26.4 |
18.5 |
29.2 |
55.5 |
66.0 |
46.6 |
50.3 |
31.3 |
16.2 |
vodivost |
µS/cm |
EC meter |
77.4 |
53.6 |
47.3 |
28.6 |
87.1 |
109.2 |
50.7 |
33.6 |
42.5 |
37.1 |
38.0 |
41.0 |
pH |
- |
pH meter |
5.36 |
5.22 |
5.08 |
5.32 |
5.55 |
5.84 |
6.14 |
6.55 |
5.86 |
6.33 |
6.13 |
6.08 |
Na+
|
ug/l |
FAAS |
650 |
930 |
1 170 |
530 |
1 530 |
1 090 |
580 |
510 |
490 |
410 |
450 |
680 |
K+
|
ug/l |
FAAS |
6 740 |
5 300 |
3 420 |
1 780 |
5 390 |
6 150 |
4 450 |
3 620 |
4 880 |
3 520 |
3 750 |
4 680 |
NH4
+
|
ug/l |
PMT |
3 000 |
1 600 |
1 060 |
520 |
3 820 |
7 050 |
2 640 |
1 550 |
1 710 |
1 210 |
1 330 |
1 050 |
Mg2+
|
ug/l |
FAAS |
660 |
550 |
600 |
330 |
690 |
600 |
340 |
270 |
310 |
200 |
280 |
380 |
Ca2+
|
ug/l |
FAAS |
1 690 |
1 250 |
1 230 |
900 |
1 860 |
1 860 |
1 110 |
970 |
1 100 |
790 |
990 |
1 350 |
Mn |
ug/l |
FAAS |
488.0 |
437.0 |
503.0 |
347.0 |
510.0 |
282.0 |
194.0 |
105.0 |
149.0 |
75.0 |
81.0 |
233.0 |
Zn |
ug/l |
FAAS |
21.0 |
15.0 |
18.0 |
2.5 |
22.0 |
19.0 |
13.0 |
11.0 |
14.0 |
25.0 |
11.0 |
18.0 |
Pb |
ug/l |
GF-AAS |
0.2 |
0.8 |
1.0 |
0.6 |
0.9 |
0.8 |
0.2 |
0.4 |
0.4 |
0.7 |
0.8 |
0.8 |
Cd |
ug/l |
GF-AAS |
0.08 |
0.05 |
0.07 |
0.02 |
0.07 |
0.08 |
0.05 |
0.02 |
0.20 |
0.04 |
0.05 |
0.05 |
Ni |
ug/l |
GF-AAS |
1.1 |
0.8 |
1.6 |
0.3 |
1.0 |
1.9 |
0.3 |
0.3 |
0.3 |
0.3 |
1.8 |
3.3 |
F-
|
ug/l |
ISE |
55 |
35 |
28 |
30 |
69 |
109 |
55 |
24 |
40 |
30 |
24 |
10 |
Cl-
|
ug/l |
HPLC |
2 650 |
2 270 |
2 550 |
1 110 |
4 010 |
2 920 |
970 |
800 |
1 220 |
670 |
1 110 |
1 730 |
NO3
-
|
ug/l |
HPLC |
8 860 |
5 830 |
5 170 |
3 920 |
13 640 |
17 720 |
7 450 |
2 460 |
6 950 |
4 240 |
5 600 |
7 310 |
SO4
2-
|
ug/l |
HPLC |
9 530 |
6 070 |
5 380 |
3 840 |
8 640 |
8 230 |
3 360 |
1 830 |
1 650 |
1 260 |
1 560 |
1 850 |