Krasnodar GRES Project Volume I11 Environmental Assessment
Krasnodar GRES Project Volume I11 Environmental Assessment Krasnodar GRES Project Volume I11 Environmental Assessment
Table 4.13 Average Long-Term Intensity of Inversions (Isotherms), Centigrade (Minvody metlstn) Months I I I Ill Iv V VI VII Vlll I x X XI XI I Altitude of the Lower Boundary of Inversions (Isotherms), km Earth 0,Ol-0,19 0,19-0,99 6,2 517 3,6 2,9 2, 5 212 212 21 1 a6 413 5 , 6 G12 Elevated inversions that may occur above the stack at the proposed Krasnodar GRES power plant at 200-500 m and inhibit air ascent have the average @ recurrence of 10-15%. The average thickness of such inversions is 300-400 m with intensity of 1-4 degrees. 63 5 17 519 414 Il8 114 1 I3 117 3,o 319 6,4 63 3,1 413 2,4 1 14 2,2 113 1 ,o 110 l12 2,6 3,O 41 1 Temperature sounding tests at the Perepravnaya meteorological station Veselyi hail control station agree with the data of the Minvody serological station accepted as long-term values for the Krasnodar GRES site. Average inversion recurrence rate, starting at the ground level, for the Krasnodar GRES site will be 30-50%. The thickness will be 300-500 m with intensity of 2-6 degrees. In winter, inversion thickness and intensity is greater than in the warm period of the year. During temperature sounding at the Perepravnaya met station in the summer of 1987 at 0-200 m altitude, a 30% occurrence of inversions and isotherms were observed. Of those cases, approximately 60% were observed in the morning hours. Their intensity was insignificant - 0.0 to 5 degrees, thickness - 50-100 m. PAGE 4-1 3
4.1.3 Air Quality Impact by Nitrogen Oxides The background concentrations of emissions into the atmosphere in Mostovskoy are based on the data of the Krasnodar hydrometeorologic regional center. These concentrations take into account the emissions of motor transport vehicles and heating boiler houses. 4.1.4 General Air Quality Impact Including Radiation General air quality in terms of pollutants is based on their background concentration and is independent of solar radiation. Table 4.14 Background Concentration of the Main Air Pollutants for Mostovskoy Village the Krasnodar Territory Pollutants Suspended matter NO2 m SO2 Mostovskoy Background Value, mg/m3 0.3 0.03 0.8 0.05 4.1.5 Main Sources of Nitrogen Oxides Concentration Average Daily Maximum Permissible Concentration, mg/m3 Russian Standards', World Bank Standards 0.05 0.1 0.085 in 30 min. 1 .O 0.05 --- 0.1 As seen from the background concentration values (Table 4.141, nitrogen oxides in the atmospheric air of the power plant construction site are not in excess of the maximum permissible concentration values. Table 4.15 summarizes air pollution by the enterprises in the Mostovskoy and Labinsk Districts PAGE 4-1 4
- Page 19 and 20: e Plant Sewage Discharge - Potentia
- Page 21 and 22: The off-site air monitoring station
- Page 23 and 24: In addition, the plant electric tra
- Page 25 and 26: @ In addition, several public meeti
- Page 27 and 28: @ Training facilities should be ins
- Page 29 and 30: 2.0 POLICY, LEGAL AND ADMINISTRATIV
- Page 31 and 32: 2.1.1 EIA Preparation, Review, and
- Page 33 and 34: e Regulations by the Russian Federa
- Page 35 and 36: * and 2.2.3 Occupational Health and
- Page 37 and 38: electromagnetic field intensities b
- Page 39 and 40: PH Contaminant or Parameter BOD Hea
- Page 41 and 42: TABLE 2.6 Electromagnetic Field Int
- Page 43 and 44: negligence or non-negligence; degre
- Page 45 and 46: e Odessa Declaration on the Black S
- Page 47 and 48: Environmental and workplace quality
- Page 49 and 50: consists of large gravel mixed with
- Page 51 and 52: 3.2.7 Water Source The source of op
- Page 53 and 54: standards in addition to any design
- Page 55 and 56: 3.3.4 Estimated Plant Emissions Air
- Page 57 and 58: Adding a new double-circuit 220 kV
- Page 59 and 60: The summer is hot and long (it begi
- Page 61 and 62: Notes: 1. Previous meteorological s
- Page 63 and 64: 4.1 .I .4 Annual and Seasonal Preci
- Page 65 and 66: Months I I I I I I IV V V I VII Vll
- Page 67 and 68: During rainfall and fog the western
- Page 69: Years 1979 1979 1980 1980 1980 1980
- Page 73 and 74: Appendices 8 and 9 are indicative o
- Page 75 and 76: River Laba Malaya Laba Point Doguzh
- Page 77 and 78: a steady low water level which can
- Page 79 and 80: i, Section F, ' 1 m BS m m2 1 41 4.
- Page 81 and 82: Section 1 2 3 4 Sum i, m BS Q I m3/
- Page 83 and 84: Table 4.21 Average Annual Water Dis
- Page 85 and 86: River Site La ba Kaladzhinskaya La
- Page 87 and 88: Dimensionality 8 % mln. m3 8 O h ml
- Page 89: Table 4.29 Chemical Composition of
- Page 92 and 93: Sampling Date 14.V 15.VI 2.8 20.V 2
- Page 94 and 95: Table 4.34 Recorded Disposals into
- Page 96 and 97: 4.2.2.2 Thickness and Occurrence of
- Page 98 and 99: 4.2.2.4 The Regions of Groundwater
- Page 100 and 101: 4.3. I. 1 Stratigraphy In the Cauca
- Page 102 and 103: * These An earthquake closest to th
- Page 104 and 105: a 4.3.1.4 Relief In a geomorphologi
- Page 106 and 107: 4.3.1.5 Mineralogy The deposits of
- Page 108 and 109: 4.3.1.8 Frozen-State Regime Climate
- Page 110 and 111: Humic-gley soil constitutes 17% and
- Page 112 and 113: a reaches In terms of humus horizon
- Page 114 and 115: @ In terms of the leaching extent,
- Page 116 and 117: Form of Use Arable land Perennial p
- Page 118 and 119: @ River Laba Malaya Laba 4.4.1 Land
Table 4.13<br />
Average Long-Term Intensity of Inversions (Isotherms), Centigrade (Minvody<br />
metlstn)<br />
Months<br />
I<br />
I I<br />
Ill<br />
Iv<br />
V<br />
VI<br />
VII<br />
Vlll<br />
I x<br />
X<br />
XI<br />
XI I<br />
Altitude of the Lower Boundary of Inversions (Isotherms), km<br />
Earth<br />
0,Ol-0,19<br />
0,19-0,99<br />
6,2<br />
517<br />
3,6<br />
2,9<br />
2, 5<br />
212<br />
212<br />
21 1<br />
a6<br />
413<br />
5 , 6<br />
G12<br />
Elevated inversions that may occur above the stack at the proposed <strong>Krasnodar</strong><br />
<strong>GRES</strong> power plant at 200-500 m and inhibit air ascent have the average<br />
@ recurrence of 10-15%. The average thickness of such inversions is 300-400 m<br />
with intensity of 1-4 degrees.<br />
63<br />
5 17<br />
519<br />
414<br />
Il8<br />
114<br />
1 I3<br />
117<br />
3,o<br />
319<br />
6,4<br />
63<br />
3,1<br />
413<br />
2,4<br />
1 14<br />
2,2<br />
113<br />
1 ,o<br />
110<br />
l12<br />
2,6<br />
3,O<br />
41 1<br />
Temperature sounding tests at the Perepravnaya meteorological station Veselyi<br />
hail control station agree with the data of the Minvody serological station<br />
accepted as long-term values for the <strong>Krasnodar</strong> <strong>GRES</strong> site.<br />
Average inversion recurrence rate, starting at the ground level, for the <strong>Krasnodar</strong><br />
<strong>GRES</strong> site will be 30-50%. The thickness will be 300-500 m with intensity of 2-6<br />
degrees.<br />
In winter, inversion thickness and intensity is greater than in the warm period of<br />
the year.<br />
During temperature sounding at the Perepravnaya met station in the summer of<br />
1987 at 0-200 m altitude, a 30% occurrence of inversions and isotherms were<br />
observed. Of those cases, approximately 60% were observed in the morning<br />
hours. Their intensity was insignificant - 0.0 to 5 degrees, thickness - 50-100 m.<br />
PAGE 4-1 3
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