Detail publikace

Changes of water content on upstream face of dam Kobeřice

Originální název

Changes of water content on upstream face of dam Kobeřice

Anglický název

Changes of water content on upstream face of dam Kobeřice

Jazyk

en

Originální abstrakt

For the soil moisture mapping indirect methods are used very often. Electrical methods are based on injecting the electrical current (direct or alternating) into the soil and electrical potential field distribution is measured. In our case, the moisture mapping is based on measuring of electrical impedance by special apparatus with Z-meter devices which were developed with the support of the previous EUREKA projects. The results presented in this paper are conducted on the earth dam of the small water reservoir Bezedník III, which is located in the Litava river basin. Some results obtained between the years 2016 and 2018 by using different Z-meter devices are shown.

Anglický abstrakt

For the soil moisture mapping indirect methods are used very often. Electrical methods are based on injecting the electrical current (direct or alternating) into the soil and electrical potential field distribution is measured. In our case, the moisture mapping is based on measuring of electrical impedance by special apparatus with Z-meter devices which were developed with the support of the previous EUREKA projects. The results presented in this paper are conducted on the earth dam of the small water reservoir Bezedník III, which is located in the Litava river basin. Some results obtained between the years 2016 and 2018 by using different Z-meter devices are shown.

Dokumenty

BibTex


@inproceedings{BUT151180,
  author="Jana {Pařílková} and Luboš {Pařílek} and Zuzana {Műnsterová} and Jan {Mikulka} and Jan {Dušek} and Robert {Ševčík}",
  title="Changes of water content on upstream face of dam Kobeřice",
  annote="For the soil moisture mapping indirect methods are used very often. Electrical methods are based on injecting the electrical current (direct or alternating) into the soil and electrical potential field distribution is measured. In our case, the moisture mapping is based on measuring of electrical impedance by special apparatus with Z-meter devices which were developed with the support of the previous EUREKA projects. The results presented in this paper are conducted on the earth dam of the small water reservoir Bezedník III, which is located in the Litava river basin. Some results obtained between the years 2016 and 2018 by using different Z-meter devices are shown.",
  address="Brno University of Technology, VUTIUM",
  booktitle="EUREKA 2018
6th colloquium and working session",
  chapter="151180",
  edition="neuv.",
  howpublished="print",
  institution="Brno University of Technology, VUTIUM",
  number="1",
  year="2018",
  month="october",
  pages="22--25",
  publisher="Brno University of Technology, VUTIUM",
  type="conference paper"
}