94
Z. Michalczy, M. Łoś
Its value was 1.80 1/s km2 for the basin above the city, 0.91 1/s kn2 in the centre of Lublin, and 1.93 1/s km2 in Sobianowice, i.e. a little mon than in the upper part of the basin. From the measurements mentioned f shortage of river supplies can be found, and even a decrement at an amount o 0.42 m3/s of flowing waters.
TABLE 1. Mean unitary flows and outflows calculated from five flow masurement series carried out by the Department of Hydrography, Maria Curie-Sdodowska University, and the Municipal Company for Water Supply and Treatmen in Lublin in rainless periods of 1990—1992 (measurements were madę on the days:9.05.1990, 12.07.1990, 19.05.1991, 23.07.1992 and 18.08.1992)
No |
River |
Measurement locality |
Basin area [km2] |
Flow [m3/s] |
Unitry outflow ['s km2] |
1 |
Bystrzyca |
Nowiny |
480 |
0.865 |
1.80 |
2 |
Krężniczanka |
Krężnica |
225 |
0.330 |
1.48 |
3 |
Bystrzyca |
Wrotków |
718 |
0.768 | |
4 |
Czerniejówka |
Głuszczyzna |
56 |
0.089 | |
5 |
Czerniejówka |
Lublin |
172 |
0.023 | |
6 |
Czechówka |
Dąbrowica |
29 |
0.018 |
0.61 |
7 |
Czechówka |
Sławinek |
67 |
0.001 |
0.01 |
8 |
Bystrzyca |
Tatary |
1046 |
0.875 |
0.84 |
9 |
Ciemięga |
Pliszczyn |
152 |
0.263 |
1.73 |
10 |
Bystrzyca |
Sobianowice |
1265 |
2.440 |
1.93 |
On the basis of hydrometrie materials for 1982-1991 the nagnitude of the outflow from the particular parts of the Bystrzyca river >asin and Lublin differential collecting area was estimated (Table 2). Hylrometric data from the Pliszczyn water-gauge on the Cimięga river, cosing its basin with relatively smali transformation of water conditions, W3re taken as the basis for calculations. The mean outflow from this basin was 3.22 1/s km2. In the years 1982-1991 the average area of the Lublin cepression funnel was 178 km2. Assuming the mean outflow at 3.22 1/skm2, the supply in this funnel was only 0.57 m3/s. This is a decided smal amount to compensate for the exploitation of underground water in tie Lublin region, estimated on average at 1.6 m3/s. The remaining part of;he water exploited from communal and industrial intakes (1.03 m3/s), reaching water-bearing layers, comes from top waters in the city area. Unierground supply from the upper part of the Bystrzyca river basin and its tibutaries may also have a positive influence. Of 1.60 m3 water exploited ai amount of 1.51 m3/s returns as wastewater to the Bystrzyca river, which is discharged within the Lublin differential collecting area, and 3.09 m3/s constitutes non-returnable loss.
In recent years, very advantageous changes in water managenent have taken place in Lublin. Economizing on water and reduced industrial