PhD Ospanova Zh.Kh1, Sc.D., professor M.R. Khanturin1 ,
Sc.D., professor Isaeva A.U.2
1Eurasian National University named after
L.N.Gumilev,
Astana,
Republic of Kazakhstan,
2Southern Kazakhstan state university named after
M.Auezov,
Shymkent city, Republic of Kazakhstan
Natural waters ecological status
of Southern Kazakhstan region
Natural factors determining the kind
composition of hydrobionts are hydrological, hydrothermal and hydrochemical parameters
of the watercourse, which change substantially with decreasing geographic level, towards of which all oblast (regional) rivers flow. In addition, in the same direction is increasing the level of anthropogenic
impact on water sources associated with the surface waste water inflow from
human settlements, agricultural landscapes and enterprise industrial areas. The combination of these factors significantly affects
the formation of communities of aquatic vegetation. In this connection,
hydrochemical researches have been carried out for studying influence of water
pollution degree on zooplankton species diversity. For this purpose
the chemical analysis of waters of all investigated rivers, in sites before and
after technogenic sources has been performed. The basic types of pollutants and seasonal dynamics of
variation of their content in water were defined.
It has been established, that the basic
sources of pollution are unorganized dump of garbage and sewage from
settlements, superficial drains from territory of agricultural objects and
sewage of the industrial enterprises, and polluting substances - nitrates,
nitrites, mineral oil, sulfates, chlorides, ions of magnesium, copper and some
heavy metals which mid-annual concentration exceeds norm in 1.4 – 5.8 maximum permissible
concentration MPC. Thus, the nature of polluting
substances and impurity degree of the water environment of the investigated
reservoirs are in strict dependence on influence specified above sources of
pollution. For example, a major source of water pollution in the river Badam by
ions of heavy metals are wastewaters and underground waters of industrial
territory of JSC "Yuzhpolimetall" (UPM). Waters of the rivers
Koshkar-Ata and Mashat become soiled by organic substances through municipal and superficial
sewage of inhabited quarters and industrial objects. As receipt process of pollutants in the rivers carries a seasonal nature
connected with meteorological conditions of seasons, the concentration
of polluting substances in water varies essentially. Surface seasonal streams, formed as a
result of heavy rainfall and snow thawing in autumn and spring months, contribute to the flow in the rivers salvo doses of pollutants. For this reason, the maximum indicators
of impurity have on spring and autumn, and minimum for summer and winter
months. The level of impurity of the river Arys water increases in process of
water acceptance of its main
tributaries. In process of tributaries number increase, running into the river, quantitative and
qualitative indicators of water
pollution alter, which also
vary from season to
season. The
concentration of principal types of
pollutants defined the water pollution index (WPI), based on that a ranked list of the investigated reservoirs to
quality classes is made. The analysis of the received data has shown that to a
category of very pure (WPI – 0.24
- 0.25 ± 0.01, 1 class of quality) 3 rivers of the
area concern only. And among other investigated 26 rivers and water basins to a
category of pure (WPI – 0.5-1.0 ± 0.02, the second class of quality) concern
11 ones, to moderately polluted-8 rivers (WPI – 1.78
- 2.41±0.03. 3 class of quality), to polluted-1 river (WPI – 3.8 ± 0.02. 4 class of quality), to dirty-2
rivers (WPI – 5.01 - 5.01 ± 0.14. 5 class of quality), to very dirty-1
river (WPI – 8.9 ± 0.2. 6 class of quality) and 1 river - to
extremely dirty (WPI–12.6 ± 0.61, 7 class of quality). By the analysis of
researches results revealed that concerning to 1 and 2 quality classes of
waters reservoirs are located in foothill areas, out of industrial zones of the
area which are characterized by the small extent (8-10 km) and low anthropogenic impact.
These rivers are characterized by a narrow
channel with a rocky bottom and a rapid current. The water
temperature in winter and summer months fluctuates in limits from 0-20 Ñ till
12-140 Ñ accordingly. The main pollutants of the aquatic environment are ions of
magnesium and sulphates the concentration of
which does not exceed value of maximum permissible concentration (MPC). The insignificant content of organic pollutants and the lowered water
temperature limit the rates of
biochemical processes, as evidenced by indicators BOD5 - from 0.6 ± 0.03 mg
O2/dm3 to 1.05 ± 0.04 mg O2/dm3. These
conditions of aquatic environment are the natural selective
factor for zooplankton community formation, adapted to the conditions of not
polluted aquatic environment with a relatively low temperature.
Reservoirs of subsequent classes of
quality, proceeding through many settlements and industrial zones, are exposed
to pollution by mineral and organic substances. For instance, such rivers of a
spring source as Togus and Lengersaj, have a length of not more than 12 km which lies through large
settlements like Togus and Lenger. Their water resources are limited and, for
this reason, seasonal fluctuation is reflected very strongly. The water
temperature in winter and summer months ranges from 6-8 till 20-250 Ñ accordingly. Household sewage from the
population which contains organic substances in a considerable quantity is the main source of pollution. During warmer months water environment
of these reservoirs is characterised by intensive rates of a course of
biochemical processes. Sharply
increases the water content of total nitrogen and other nutrients and a
deficiency of oxygen dissolved in water (BOD5 - from 34.6±1.03 mg O2/dm3
to 61.05 ± 0.04 mg O2/dm3) increases water
saprobity. Parameters of water environment characteristics established earlier contribute
formation of zooplankton, consisting only from kinds resistant
against specified conditions of inhabitancy. Contrary, rivers Mashat and Bogen
are characterised to
have a
greater way by extent before merge to the river Arys. Throughout
this way there is a change
of hydrothermal, hydrochemical and saprobiological characteristics of the aquatic
environment. These rivers at the sources, in foothills of Tjulkubassky and
Bajdibeksky areas, under these characteristics correspond to the first class of
quality as the rivers of glacier.
However, in process of lowering
of geographical level, the temperature and level of their waters impurity
raises.
In the case of the river Mashat, this is due to the flow of rivers through such
towns as Mashat, Kershetas and to location on its banks for more than 30
sanatoriums and holiday camps. On this interval there is a
pollution of the river by mineral and organic substances which leads to its
sharp decrease of hydrochemical and saprobiological characteristics. The level of
water mineralization increases
of 4.3 times or more. In the river estuary before merging with
the river Arys WPI
makes 2.40 that corresponds to the third class of waters quality, moderately
polluted. The basic characteristics change of the aquatic environment of the river Bogen occurs
similarly to indicators of the river Mashat. Due to a rapid current and average
temperature (4-50 Ñ in the winter and 18-200 Ñ in the summer) aquatic environments of these
rivers do not have a high rate of biochemical processes, as evidenced by
indicators BOD5 – 1.6 ± 0.08 mg
O2/dm3 in winter and 2.15 ± 0.41 mg
O2/dm3 in summer months. Above established parameters of
the water environment create new conditions for zooplankton community that structure will depend on the
degree of adaptability and competitiveness of its constituent kinds.
The main extent of the river Badam is on the
plain territories of the oblast (region). In winter and summer months the
water temperature in the river varies from 3-4 to 160 C-180 C,
accordingly. Sharp
increase of water mineralization level occurs on a site in the extent about 20
km which falls within
the industrial zone of Shymkent city. The main source of
waters pollution of the river Badam are surface wastewaters and underground
waters from industrial territory of JSC "UPM" which has hydraulic
interrelation with the river. Except ions of magnesium, calcium and iron ions
of such heavy metals as lead and the cadmium also get to river water, the concentration of which, seasonally
exceed in the MAC
indicators 2.1 - 3.5
times. Results of
chemical analyses of the waters held in 2005-2008 showed that the content of heavy
metals ions around a gauging
station ¹1 does not exceed the limit values. In this area,
the main pollutants of river waters are nitrates and nitrites (11.5±1.1 and 0.034±0.001 mg/l
N) which come
with waters of the rivers Togus and Lengersaj. Pollution of river water by ions
of lead, cadmium and zinc occurs in the interval of the river which is located on
territory of an industrial zone of JSC "UPM". As shown in Figures 143 and
144 in the gauging station ¹2 pollutant concentrations exceed the MAC - on sulfates
3.5-fold; by nitrite - 2.2; of magnesium - 2.1, -3.5, on lead, the cadmium - 2.8 and 3.4 for zinc. In the area of gauging station
¹3 somewhat
rises the level of water impurity of the river organic compounds which come along with
river Koshkar-Ata. However indicators of BOD5 in this segment of the river do not
exceed 2.55 – 3.22 ± 0.12 mg
O2/dm3. Thus, in the estuary water quality meets Class 4,
the polluted waters (WPI
equal to 3.80 ± 0.01).
The river Koshkar-Ata concerns
to the fifth class of waters quality and is characterised as a dirty one.
Sources of pollution of the river waters are public drains of a private sector.
The water environment of the river is polluted by various organic compounds, which are dominated by
nitrites, nitrates, oil and other organic contaminants. In addition chlorides,
sulfates and mineral salts of copper, zinc, magnesium and iron concentrations
are found which are slightly higher than the limit values. The high content
of organic chemistry in the conditions of the water environment temperature
rise promotes strengthening of the biochemical processes connected with their
recycling. In these
conditions, the intensification of the absorption of oxygen dissolved in water
and development of aquatic organisms that severely degrade the performance
saprobiological waters.
According to its
geographical location and level of technogenic impact is a unique model river
watercourse. It originates from large underground water sources in the city
centre of Shymkent city
and 12 km runs into the river
Badam. Hydrological characteristics of a watercourse are uniform on all extent of the
river. A channel in width of 5-12 meters with a sandy-silty bottom, flat
coasts, a moderated current. Water temperature at sources within a year
fluctuates in the range
8 - 14±1.30 Ñ.
However, on the middle
and latter parts of the
river it makes 5 – 20 ± 2.20 Ñ and 3 – 25 ± 1.10 Ñ accordingly. As the distance from the source of the river level rises technogenic impact sharply increses, accordingly hydrochemical indicators of
its waters that entails also
changes of specific structure of zooplankton community and algoflora.
The dependence of a
specific variety of zooplankton on hydrochemical indicators of reservoirs is
established.