by webadmin | Jan 25, 2015 | Bez kategorii
Natural Environment Monitoring 2011, No 12, 103-116
ANALYSIS OF THE STATE OF MUNICIPAL WASTE LANDFILLS IN THE ŚWIĘTOKRZYSKIE VOIVODSHIP IN TERMS OF ECOLOGICAL REVIEW
Tomasz Kwiatkowski, Maria Żygadło
Summary
In Świętokrzyskie voivodship a total of 50 municipal landfills are located. In 2010 only 15 active municipal landfill were in operation. The total area operated landfills is approximately 40 hectares. The voivodship has continued the process of closing landfills, which do not meet the technical requirements, or their capacity has been exhausted. Administrative actions focused on objects (Tab. 2) contributed to their proper functioning. All landfill sites destined to be modernized in term 2005–2009 have been upgraded with the exception of landfill “Staszów”. These activities have also contributed indirectly to extend the service life of landfills. With the adjustment to the requirements of landfill regulations the negative impact on the environment will be minimized. The analysis of the active capacity of municipal waste landfills in operation shows that in Świętokrzyskie remained only about 3 230 920.64 m3 of free landfill capacity (as of 31.12.2009), which will ensure that the needs of the region only about 11-year period of operation. For the landfill “Staszów” fall the half of the capacity. The spoken landfill until 31.12.2010 was not adapted to the requirements of law, while it is in the process of adjustment (has a valid building permit). In the case of the closure of that landfill the remaining free capacity of total number of landfills ability to receive municipal waste in the region will decrease by approximately 50%. In addition, the landfills destinated for modernization, namely: Klępie Dolne, Wola Jastrzębska, Słupcza, Bugaj, Grabowiec, Wyszyna Machorowska, Radoszyce, Fałków, Marcinków were closed.
With regard to the closed municipal landfill in Świętokrzyskie, the process of rehabilitation, is very slowly which may serve over the years a serious threat to the environment. This particularly concerns the objects, which are located in areas threatened by flood.
by webadmin | Jan 25, 2015 | Bez kategorii
Natural Environment Monitoring 2011, No 12, 93-101
SPATIAL VARIABILITY OF SELECTED PHYSICO-CHEMICAL SOIL PROPERTIES IN THE CENTRAL PART OF THE ŚWIĘTOKRZYSKIE (HOLY CROSS) MOUNTAINS
Rafał Kozłowski, Edyta Adwent
Summary
In the present study, the results of research into the problem of soil acidification, conducted in the central Świętokrzyskie (Holy Cross) Mountains geoecosystem, have been discussed. Field research conducted in the area of the Natural Environment Integrated Monitoring Base Station at Święty Krzyż covered the top mineral horizon (0–10 cm) of rusty podsolic precipitation-andgley soil. Basing on laboratory research which covered measurements of pH in H2O and KCl, as well as Hh and Hw, it may be concluded that in the geoecosystem at issue a distinct differentiation of the horizon occurs. The spatial distribution of exchange and hydrolytic acidity, as well as soil reaction, forms a specific micromosaic around tree trunks.
The statistical testing analyses, conducted by means of the Mann-Whitney U test, have shown considerable statistical differences in pH and Hw values depending on tree trunk and species. It has been found that the acidified stemflow which runs down tree trunks most strongly affects the measured quantities within the distance of up to 50 cm.
by webadmin | Jan 25, 2015 | Bez kategorii
Natural Environment Monitoring 2011, No 12, 85-91
A QUANTITATIVE COMPARISON OF WET AND TOTAL DEPOSITION IN THE CENTRAL PART OF THE ŚWIĘTOKRZYSKIE MOUNTAINS
Rafał Kozłowski
Summary
The physico-chemical properties as well as the chemism of atmospheric precipitation affected by the pollution of atmospheric air are among the major elements which influence present-day degradation of the natural environment. It is a fact that water, apart from acting as a partner for physical reactions, is also a carrier of anthropogenic transformation of the natural environment. The present study offers a quantitative analysis of results of wet and total deposition in the years 20082009. To this end, the Eigenbrodt UNS 130 E automatic collector of wet precipitation and the Hellmann rain gauge have been used. The conducted analysis has shown significant discrepancies both in the physicochemical properties and the chemical composition of wet and total precipitation waters.
by webadmin | Jan 25, 2015 | Bez kategorii
Natural Environment Monitoring 2011, No 12, 69-83
GEOECOSYSTEMS POLISH STATE – AN ASSESSMENT BASED ON SELECTED GEOINDICATORS IN THE INTEGRATED MONITORING OF THE NATURAL ENVIRONMENT PROGRAMME
Andrzej Kostrzewski, Józef Szpikowski, Grażyna Szpikowska
Summary
Assessment of current status, trends, threats and protection of the geographical environment is the primary purpose of research carried out since 1994 under the Integrated Monitoring of the Natural Environment. Quantitative and qualitative geoindicators, compiled on the basis of stockpiled IMNE database, allow for a fuller and more comprehensive assessment of the Polish geoecosystems. In the hydrological year 2010 the IMNE research program was conducted in eight Base Stations representing different landscape zones Polish, subjected to varying degrees of changes of natural and anthropogenic pressures. The year 2010, like the previous one, was a favorable period for delivery of water to the environment, which consequently led to the reconstruction of disturbed water retention deficient rainfall in 2002–2006. Applied geoindicators confirm a number of significant changes geoecosystems improvement: reducing pollution and increasing the pH in precipitation and a decrease in sulphate concentrations in rain waters, groundwater and surface water. Present in the atmosphere nitrogen oxides increase their participation in the acidification of precipitation by decreasing the role of sulfur dioxide. Still remain the problem of nitrogen compounds in groundwater in agricultural areas, which remained after the period of intensive fertilization, and whose removal from geoecosystem may be extended for many years. Weak trends indicating decrease of nitrogen concentrations in groundwater and surface water may mean that they are potentially a risk of eutrophication of waters in the studied geoecosystems. The presented results of a proposal to develop a quantitative methodological observed landscape changes based on long observational series obtained in IMNE. The obtained results have theoretical and practical significance for the study of planning and decision-making at different levels of environmental management.
by webadmin | Jan 25, 2015 | Bez kategorii
Natural Environment Monitoring 2011, No 12, 59-68
GENESIS AND FLOODS COURSE IN THE FLYSCH BYSTRZANKA CATCHMENT IN THE PERIOD 1995–2009
Małgorzata Kijowska
Summary
Floods in small streams are the subject of numerous publications, especially in recent years, when marked the increase extreme meteorological and hydrological risk. The size of the floods is related mainly with weather conditions, especially with the precipitation and the other elements e.g. the period prior the floods, the state of the catchment retention, the manner and condition of the vegetation cover, the catchment parameters and in the winter: the water content in snow or depth of the soil freeze. Studies on the genesis and floods course were conducted in the flysch Bystrzanka catchment in the period 1995–2009. The catchment location makes two relief types to interweave. These are the relief of the Carpathian Foothills and of the Beskidy Mts., controlled by geologic structures and tectonics.
The predominate type of the floods in the catchment are normal floods inducted by rainfall. The discharge with the high water level represent mean 7% of the hydrological year, are short (3,2 day) with one discharge wave, usually single. Floods which occur in the winter half year have a longer duration. It is related with the way of water supply to the main stream by the slowly snowmelt from the different and asymmetric part of the catchment. The discharge which are notice in the Bystrzanka stream are typical of the Eastern Macroregion – with the runoff predominance in the winter half year (November–April) (54%). The discharge coefficient show the complex regime, snow-rain. Analyzed period (1995–2009) in terms of the genesis, the number of floods, course, is typical in comparison to the other small stream but well reflects the environment transient from west to east and from Carpathian Foothills to Beskidy Mts.
