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Last Issues

2025

  • Volume 98, iss. 1

2024

  • Volume 97, iss. 4
  • Volume 97, iss. 3 - Integrating Quaternary Sciences in Poland – POLQUA
  • Volume 97, iss. 2
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Results 1 - 3 of 3 for groundwater (0.0015 seconds)

Hydrochemical effects of submarine groundwater discharge to the Puck Bay (Southern Baltic Sea, Poland) [100.00% relevance]

Hydrochemical effects of submarine groundwater discharge to the Puck Bay (Southern Baltic Sea, … and in near-bottom salinity caused by groundwater discharge to the Puck … Geographia Polonica ( … 1996) vol. 67 Hydrochemical effects of submarine groundwater discharge to the Puck Bay (Southern Baltic Sea, … Polonica (1996) vol. 67, pp. 103-120 | submarine groundwater discharge, chlorinity of porewaters, salinity of … , Baltic Sea Hydrochemical effects of submarine groundwater discharge to the Puck Bay (Southern Baltic Sea,

article/item/7870.html - 14.12 kB

Maximum recessions of shallow groundwater level in central Poland [100.00% relevance]

Maximum recessions of shallow groundwater level in central Poland This article presents a … method of describing maximum recessions of groundwater level,drawing on an analysis based on data … ) vol. 83, iss. 1 Maximum recessions of shallow groundwater level in central Poland Przemysław Tomalski … Polonica (2010) vol. 83, iss. 1, pp. 5-12 | groundwater, maximum recessions of water table Maximum … recessions of shallow groundwater level in central Poland, Przemysław Tomalski,

article/item/7628.html - 13.75 kB

Dynamics of shallow groundwater temperature in the Vistula abandoned valley, the Płock Basin [80.00% relevance]

Dynamics of shallow groundwater temperature in the Vistula abandoned valley, the … Płock Basin The temperature of shallow groundwater is markedly affected by air temperature,the … Polonica (1988) vol. 53 Dynamics of shallow groundwater temperature in the Vistula abandoned valley, the … 1988) vol. 53, pp. 115-128 | Dynamics of shallow groundwater temperature in the Vistula abandoned valley, the

article/item/8107.html - 14.48 kB

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