Kvantifikácia zásob vody v zóne aerácie pôd ako zdroja vody pre biosféru

Abstract eng:
Hydrological cycle comprises of water transport between reservoirs of water in gaseous, liquit or solid state, and plays central role in Earth´s climate. Part of precipitation which falls on soil surface or vegetation, can create surface runoff. One part of precipitation could be catched by vegetation in a form of interception and can evaporate. Other part infiltrates into soil and enriches subsurface water storage. Evaluation of water content in soil aeration zone at demarked area is possible only in relation to catchments, from which the studied area comprises. The water content is evaluated in relation to water runoff from studied catchment. The contribution of the project will be assessment of water resources courses in an soil aeration zone over forest ecosystem of Žitný ostrov during the some years. Water storages will be calculated from monitored data of soil moisture.

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