Monthly analysis of atmospheric precipitation
Year |
2010 |
Region |
Vysocina |
District |
Pelhrimov |
Measuring programme |
JSALB, Salacova Lhota |
Type of measuring programme |
Bulk samples |
Organization |
CGS |
Matter |
Unit |
Method |
2009 |
Monthly concentrations |
11 |
12 |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
RAIN |
mm |
VOL |
31.6 |
61.8 |
74.2 |
19.4 |
33.9 |
54.8 |
103.2 |
69.5 |
87.1 |
276.1 |
83.7 |
7.7 |
vodivost |
µS/cm |
EC meter |
22.5 |
22.5 |
15.3 |
46.8 |
23.4 |
13.6 |
15.5 |
11.6 |
15.2 |
11.6 |
13.8 |
|
pH |
- |
pH meter |
5.50 |
5.30 |
4.74 |
6.04 |
5.14 |
5.07 |
4.84 |
5.60 |
4.54 |
4.70 |
6.42 |
|
Na+
|
ug/l |
FAAS |
190 |
290 |
150 |
580 |
460 |
70 |
130 |
850 |
80 |
50 |
150 |
|
K+
|
ug/l |
FAAS |
390 |
390 |
50 |
550 |
240 |
80 |
310 |
270 |
100 |
40 |
460 |
|
NH4
+
|
ug/l |
PMT |
1 810 |
220 |
370 |
1 850 |
1 450 |
650 |
310 |
250 |
30 |
40 |
1 410 |
|
Mg2+
|
ug/l |
FAAS |
130 |
240 |
50 |
530 |
150 |
50 |
100 |
320 |
50 |
40 |
60 |
|
Ca2+
|
ug/l |
FAAS |
530 |
1 840 |
250 |
3 510 |
570 |
280 |
390 |
510 |
310 |
200 |
410 |
|
Mn |
ug/l |
FAAS |
8.0 |
8.0 |
7.0 |
63.0 |
11.0 |
12.0 |
3.0 |
9.0 |
14.0 |
8.0 |
3.0 |
|
Zn |
ug/l |
FAAS |
66.0 |
65.0 |
32.0 |
143.0 |
46.0 |
17.0 |
23.0 |
60.0 |
39.0 |
19.0 |
24.0 |
|
Al |
ug/l |
GF-AAS |
5 |
21 |
20 |
109 |
82 |
104 |
154 |
5 |
5 |
5 |
5 |
133 |
Fe |
ug/l |
FAAS |
80 |
25 |
25 |
25 |
70 |
25 |
25 |
25 |
25 |
25 |
25 |
|
Pb |
ug/l |
GF-AAS |
0.2 |
0.9 |
0.5 |
2.0 |
0.2 |
0.5 |
3.8 |
0.2 |
0.2 |
0.2 |
0.2 |
2.7 |
Cd |
ug/l |
GF-AAS |
0.02 |
0.02 |
0.02 |
0.16 |
0.02 |
0.02 |
0.02 |
0.08 |
0.02 |
0.02 |
0.02 |
0.83 |
Ni |
ug/l |
GF-AAS |
0.3 |
0.3 |
0.3 |
2.8 |
3.8 |
0.6 |
2.7 |
0.3 |
0.8 |
0.3 |
0.6 |
0.3 |
F-
|
ug/l |
ISE |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
10 |
|
Cl-
|
ug/l |
HPLC |
300 |
360 |
160 |
570 |
420 |
110 |
130 |
270 |
90 |
25 |
240 |
|
NO3
-
|
ug/l |
HPLC |
2 270 |
3 380 |
1 960 |
7 870 |
2 800 |
1 400 |
1 520 |
150 |
1 080 |
630 |
1 050 |
|
SO4
2-
|
ug/l |
HPLC |
2 760 |
2 660 |
1 450 |
5 740 |
2 180 |
1 130 |
1 560 |
1 660 |
830 |
1 440 |
860 |
|