Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Maile Polikarpus"'
Publikováno v:
Hydrology Research, Vol 54, Iss 7, Pp 840-854 (2023)
The DRASTIC method is one of the most widely used groundwater vulnerability assessment techniques. In areas where the main useful aquifers are covered with an extra layer of diverse sediments, a further modification of the DRASTIC method is required
Externí odkaz:
https://doaj.org/article/c2994930a350430eaa589ca4e55ab776
Autor:
Oliver Koit, Inga Retike, Jaanus Terasmaa, Jānis Bikše, Elve Lode, Marko Vainu, Konrāds Popovs, Alise Babre, Pamela Abreldaal, Karin Sisask, Siim Tarros, Andres Marandi, Marlen Hunt, Magdaleena Männik, Maile Polikarpus
As groundwater does not follow human-drawn boundaries such as country borders, groundwater pollution in one country can adversely affect groundwater quality and availability in a neighboring country. It is vital to develop a conceptual understanding
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a236b14c81eb4c2e8d302439a1dd230
https://doi.org/10.5194/egusphere-egu22-5008
https://doi.org/10.5194/egusphere-egu22-5008
Developing accurate groundwater vulnerability maps is necessary for environmental planning and protection of groundwater resources. The DRASTIC method is one of the most widely used groundwater vulnerability assessment techniques. To achieve a more p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e423b0ad7a1eb496fee11096a4f2ce9
https://doi.org/10.21203/rs.3.rs-1260704/v2
https://doi.org/10.21203/rs.3.rs-1260704/v2
Developing accurate groundwater vulnerability maps is necessary for environmental planning and protection of groundwater resources. The DRASTIC method is one of the most widely used groundwater vulnerability assessment techniques. In formerly glaciat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fccb4d38d338b41981580c7d948d9e4
https://doi.org/10.21203/rs.3.rs-1260704/v1
https://doi.org/10.21203/rs.3.rs-1260704/v1
Autor:
Siim Tarros, Aiga Krauze, Elve Lode, Jaanus Terasmaa, Kersti Türk, Janis Bikše, Agnese Priede, Kristiina Ojamäe, Andres Marandi, Maile Polikarpus
European water policy requires to carry out nine tests for characterisation of groundwater bodies status, including the development of joint transboundary groundwater management principles. Gauja/Koiva and Salaca/Salatsi Rivers have a joint, Estonian
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4bcb2541a8d3430096dc4dd72ef577f2
https://doi.org/10.5194/egusphere-egu21-1979
https://doi.org/10.5194/egusphere-egu21-1979
Autor:
Inga Retike, Joonas Pärn, Maile Polikarpus, Marko Vainu, Martin Küttim, Jaanus Terasmaa, Oliver Koit, Karin Sisask, Pamela Abreldaal, Siim Tarros
Publikováno v:
Journal of Hydrology. 600:126656
A pilot study was carried out in the Matsi spring fen, southern Estonia to test a proposed methodology ( Terasmaa et al., 2020 ) for identifying potential effects of groundwater bodies on groundwater dependent terrestrial ecosystems (GDTE). A compreh
Publikováno v:
Applied Geochemistry. 38:103-109
The concentrations of dissolved cations and anions are fundamental to the water quality of groundwaters, particularily pertaining to their use as a drinking water source. Currently, assessment of total dissolved solids requires laboratory-based analy
Autor:
Andres Marandi, Marko Kohv, Helen Hiiemaa, Maile Polikarpus, Argo Jõeleht, Enn Karro, Tiit Hang
Publikováno v:
Hydrogeology Journal. 21:1581-1591
The water balance of wetlands plays an integral role in their function. Developments adjacent to wetlands can affect their water balance through impacts on groundwater flow and increased discharge in the area, and they can cause lowering of the wetla
Autor:
Kalle Kirsimäe, A. Kärki, Väino Puura, Sten Suuroja, Kalle Suuroja, Juho Kirs, Maile Polikarpus
Publikováno v:
Meteoritics & Planetary Science. 37:449-457
The well-preserved Krdla impact crater, on Hiiumaa Island, Estonia, is a 4-km diameter structure formed in a shallow Ordovician sea about 455 Ma ago into a target composed of thin (~150 m) unconsolidated sedimentary layer above a crystalline basement