The Institution of Transmission Easement in Poland

The text presents an analysis of the institution of transmission easement, which is featured from the perspective of civil-law and public-law relations. The text does not address all the issues related to the institution of transmission easement, that is, no comprehensive analysis of the issues of the grounds for easement establishment, expiry, or remuneration and compensation for easement was conducted. The text presents a general description of the establishment of transmission easement against the backdrop of the Polish Civil Code and the Bill on Transmission Corridors of 18 July 2013, which is currently being drafted. The analysis of the easement institution, apart from the synthetic approach to legal provisions, features a functional and teleological interpretation. It is worth pointing out the aim that the legislator wished to achieve with respect to the work on new considerations both in the domain of the private and public law: 1. the legislator aimed to regulate the disorderly legal status of civil-law relations, but also to avoid dispute in the future, 2. with the aid of new regulations, the legislator wished to respond to the public interest.

Isotope characterisation of deep aquifers in the Gwda catchment, northern Poland

We present the results of isotope measurements (δ 18 O, δ D, δ 13 C DIC and 14 C) and chemical analyses (TDS, TOC, HCO 3– , SO 42– , Cl – , NO 3– , NH 4+ , Ca 2+ , Mg 2+ Na + and K + ) conducted on groundwater samples collected from deep Cenozoic aqui- fers. These aquifers are the basic source of drinking water at numerous localities within the study area in northern Po- land. Most of the δ 18 O determinations are characterised by low variability (i.e., > 70 per cent of δ 18 O are between –9.5‰ and –9.2‰). In most cases tritium activity was not detected or its content slightly exceeded the uncertainty of measure- ment (from ±0.3 T.U. to ± 0.5 T.U.). On average, 14 C activity is twice higher than that under similar conditions and in hydrogeological systems. The δ 13 C DIC values fall within the –13.6‰ to –12.8‰ range. A slight variability is observed when considering all isotope and chemical data within the study area and under these hydrogeological conditions. In general, the results of isotope and chemical analyses seem to be homogeneous, indicating the presence of closely similar groundwaters in the system, irrespective of geological formation. It is likely that there is a significant hydraulic connec- tion between shallow and deep aquifers in the Gwda catchment, which indicates the potential for seepage of pollutants from shallow Pleistocene to deep Miocene aquifers. This can endanger the latter by e.g., high concentrations of NO 3– , SO 42– and Cl – ions from shallow aquifers within the Gwda catchment.