This project defined changes in soil properties after construction of subsurface tile drainage. We compared the physical and chemical properties of soil samples taken before construction of drainage and new soil samples taken from identical sites at present. The research was made for Stagnic Cambisols (Dystric) and Haplic Stagnosols. The pH value and saturation of the topsoil sorption complex of both soil types statistically increased and simultaneously the cation exchange capacity (CEC) decreased. In the topsoil of Stagnosols, the effective cation exchange capacity and porosity also decreased, and at the same time the particle density and bulk density increased. Soil organic matter and minimum air capacity increased in the topsoil of Cambisols. Porosity and minimum air capacity increased in both soils in the subsoil. In the Cambisol subsoil, the CEC and bulk density decreased. We can assume that after drainage Stagnosols are susceptible to soil compaction, especially in topsoil.

Coal mining has an impact on the countryside and landscape where the exploitation of the mineral occurs, particularly with regard to the way it is mined, the technology used, the surface area, and the shape of the coalfield and extent of mining. The impact of mining, which is predominantly negative, is gradually being eliminated today in accordance with applicable laws by applying knowledge and experience and with the help of a variety of reclamation and revitalization activities. The newly created landscape gives the area new value and opportunity for use. The process of restoring a landscape after coal mining should be primarily guided by the principle of sustainable development to ensure that a balance of the social, economic and environmental aspects is achieved. This article discusses the theoretical basis of the individual possibilities for restoring the landscape in such a way that the anthropogenic formations caused by coal mining are best incorporated into the surrounding landscape and likewise meet the social and economic needs of society. A model area can be found in the northern part of the Czech Republic that has been scarred by coal strip mining for nearly 200 years, but the adverse effects on the landscape have been successfully smoothed over by reclamation methods.

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The article is focused on the changes in soil characteristics caused by the drainage of agricultural soils in the Czech Republic. The basis of the research was to compare current state with the state before drainage using available historical data. To resolve the subject of the research, two smaller study areas with different soil uses were chosen. The Haklovy Dvory area is an arable land that is intensively used. The other area is used mainly for grazing (extensively) and it is called Železná study area. In many cases, historical data regarding the quality of surface water and groundwater (well water) in the two areas is readily available; therefore, the same approach was taken for monitoring the current quality of drainage water. Several chemical indicators were measured in the water: pH, alkalinity-acidity, overall hardness, concentration of selected cations (magnesium, calcium, potassium, ammonia), concentration of bicarbonates, nitrates, nitrites, sulphates, phosphates, chlorides and the electrical conductivity of the water. During the entire course of the monitoring, no serious water pollution was found in Železná study area (with the exception of one sample point). In case of the intensively managed Haklovy Dvory study area, a significant pollution in all drainage water samples was confirmed. We can safely formulate a hypothesis that the drainage water quality is related to the type of agriculture procedure practiced on the land. Mainly the intensive type of agriculture, because of the use of fertilizers, has a negative impact on drainage water quality, and subsequently on the quality of surface watercourses.

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