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The assessment of anthropogenic immission load of area is important indicator in the process of immission participation determination to agricultural crop detraction. Despite the rapid concentration detraction of all immissions in the air environment dominates the opinion, that it continues in latent scale of damaging in the economically significant scale. Demonstration of this effect scale is economically and technically difficult. That is why the indirect methods of load assessment are developed, whereas the level of their validity is the cardinal inefficiency. Determination of concentrations of pollutants recognized methods are costly and labour-consuming and are also linked to energy networks. In the present work we follow the content of SO2 in the atmosphere because of their greatest contribution to atmospheric pollution. Their objectives is based on selected methods simply set the load area of sulphur and nitrogen transformation of the volume concentration of SO2 the deposition rate and replace the costly and labour intensive methods. In this paper we compare two direct methods sorption-cumulative and chemiluminescence. The amounts of SO2 observed sorption-cumulative method in the individual periods was several times higher than the amount measured by AMS Leles. Results showed relatively large differences between different methods. The above methods can replace costly and labour intensive methods.
The water basin bottom relief during its lifetime is shaped by the acumulation of the sediments, cleaning processes or the abrasive effects of the water flow. These modifications of the relief leads to the changes of the water basin acumulation capacity. The usage of the GIS for this task means the usage of digital terrain model (DTM), which represents the bottom of surveyed basin. The proposed method for the assessment of the basin capacity uses the poin-type objects. For the collecting of the point coordinates (x, y, z), we used the arrangement of the measuring equippment consisting of the GPS receiver and sonar, which was mounted to the raft boat. The data collection was done during the sailing on the water basin Golianovo. Final DTM was used for the calculation of the water basin capacity with the usage of zonal statistics in ArcGIS 10.
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