Monthly analysis of atmospheric precipitation
Year |
2016 |
Region |
Kralovehradecky |
District |
Rychnov nad Kneznou |
Measuring programme |
HUDLE, U dvou loucek |
Type of measuring programme |
Throughfall beech |
Organization |
FGMRI |
Matter |
Unit |
Method |
2015 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
323.4 |
64.5 |
86.2 |
140.6 |
113.6 |
53.8 |
33.4 |
76.3 |
94.8 |
61.8 |
29.4 |
151.4 |
vodivost |
µS/cm |
EC meter |
21.7 |
23.6 |
17.4 |
15.6 |
31.1 |
63.3 |
49.2 |
32.2 |
66.7 |
27.5 |
51.4 |
25.0 |
pH |
- |
pH meter |
5.45 |
5.88 |
5.34 |
5.88 |
4.92 |
4.03 |
6.90 |
4.70 |
4.15 |
4.77 |
4.88 |
5.50 |
Na+
|
ug/l |
FAAS |
260 |
410 |
310 |
280 |
230 |
240 |
310 |
190 |
250 |
80 |
230 |
140 |
K+
|
ug/l |
FAAS |
1 140 |
970 |
430 |
430 |
480 |
810 |
8 310 |
3 600 |
2 790 |
1 170 |
3 900 |
3 310 |
NH4
+
|
ug/l |
PMT |
50 |
830 |
640 |
610 |
2 460 |
2 120 |
920 |
110 |
850 |
130 |
160 |
60 |
Mg2+
|
ug/l |
FAAS |
180 |
240 |
160 |
170 |
170 |
160 |
650 |
310 |
400 |
170 |
560 |
270 |
Ca2+
|
ug/l |
FAAS |
710 |
580 |
1 100 |
1 080 |
700 |
1 000 |
2 210 |
850 |
1 880 |
1 030 |
2 960 |
1 020 |
Mn |
ug/l |
FAAS |
19.0 |
30.0 |
50.0 |
18.0 |
18.0 |
21.0 |
37.0 |
6.0 |
88.0 |
19.0 |
71.0 |
32.0 |
Zn |
ug/l |
FAAS |
46.0 |
81.0 |
24.0 |
34.0 |
79.0 |
30.0 |
84.0 |
39.0 |
141.0 |
49.0 |
33.0 |
30.0 |
Pb |
ug/l |
GF-AAS |
1.1 |
2.7 |
1.1 |
2.2 |
1.8 |
2.0 |
1.7 |
0.8 |
2.4 |
1.2 |
1.8 |
1.5 |
Cd |
ug/l |
GF-AAS |
0.05 |
0.15 |
0.09 |
0.10 |
0.14 |
0.13 |
0.07 |
0.05 |
0.16 |
0.04 |
0.08 |
0.12 |
Ni |
ug/l |
GF-AAS |
0.2 |
10.4 |
0.9 |
0.5 |
1.8 |
13.5 |
0.7 |
0.2 |
0.2 |
0.2 |
6.8 |
1.5 |
F-
|
ug/l |
ISE |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
29 |
31 |
31 |
10 |
10 |
Cl-
|
ug/l |
HPLC |
2 170 |
1 000 |
450 |
430 |
460 |
330 |
640 |
460 |
580 |
150 |
750 |
440 |
NO3
-
|
ug/l |
HPLC |
3 850 |
4 690 |
2 330 |
2 490 |
4 660 |
10 260 |
1 300 |
7 390 |
14 670 |
5 660 |
12 930 |
5 190 |
SO4
2-
|
ug/l |
HPLC |
2 710 |
2 210 |
1 870 |
1 510 |
4 080 |
2 320 |
3 190 |
1 820 |
2 820 |
1 040 |
3 400 |
1 830 |