Open AccessSpecification of the Climate Character in the Study Area of Projected Hydric Reclamation
Author(s) -
Dagmar Dlouhá,
Viktor Dubovský
Publication year - 2021
Publication title -
inżynieria mineralna
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.215
H-Index - 9
ISSN - 1640-4920
DOI - 10.29227/im-2021-01-10
Subject(s) - hydric soil , land reclamation , hydrology (agriculture) , environmental science , surface runoff , precipitation , subsoil , water balance , soil science , geology , soil water , geotechnical engineering , meteorology , geography , ecology , archaeology , biology
Hydrical reclamation of the residual pit of Most-Ležáky is part of the comprehensive revitalisation of the land affected in the past bymining activity with an area of 1264 ha. Thus, in terms of remediation and reclamation, the most appropriate way to reclaim theresidual pit, as one of the final stages of the long-term reclamation activities that have been going on in the area for more than half acentury, occurs under the given conditions. The Lake Most, our study area, was planned and created as a hydric recultivation of theformer surface Most-Ležáky mine located near the town of Most, in the foothills of the Ore Mountains, approximately 80 kilometersnorthwest of the capital of the Czech Republic - Prague. The Lake Most represents extensive hydric reclamation, which is unique in thesense that it does not have a natural inflow and runoff, therefore an artificial feeder from the Ohře River had to be built. The main goalof the ongoing research is to construct a mathematical model predicting the water balance of Lake Most. Therefore, it is important toseparate amount of water that is lost by the evaporation and amount of water that is lost into the subsoil. If we do not wish to use onlytemperature equations but more complex methods and equations to calculate evaporation instead, we need to have relative humidity,atmospheric pressure, wind speed, and daylight length values. In addition to the climatic data needed to calculate the evaporation,the amount of precipitation is needed to construct the balance equation of the area. An important objective in planning all hydricreclamations is to ensure their long-term sustainability, which is based on a detailed description of the study area's climate and localhydrological conditions. In our article we focus on assessing the evolution of climate in the area of this hydric reclamation. We haveprocessed a long-term series of measurements in monthly averages from the Kopisty meteostation data provided by the Institute ofAtmospheric Physics of the CAS.