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Wyświetlanie 1-4 z 4
Tytuł:
Agresywność chemiczna płytkich wód podziemnych Wrocławia
Chemical aggressiveness of shallow groundwater in Wrocław
Autorzy:
Trałka, Marta
Modelska, Magdalena
Błachowicz, Marek
Powiązania:
https://bibliotekanauki.pl/articles/2076166.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
agresywność chemiczna
płytkie wody gruntowe
Wrocław
chemical aggressiveness
shallow groundwater
Opis:
Evaluation of the chemical aggressiveness of shallow ground - water for the area of Wrocław was performed in accordance with the Polish Standard (PN-EN 206+A1:2016-12). This standard requires determination of pH and concentration of ammonium, magnesium, sulphate and aggressive carbon dioxide in water. The research was carried out on 96 groundwater samples collected in the period March-May 2021 from Holocene, Pleistocene and Neogene deposits. The results show that 58% of shallow groundwater in Wrocław was aggressive towards concrete and steel. The slight (XA1), moderate (XA2) and high (XA3) aggressiveness was characteristic for 32%, 23% and 3% of the analysed waters, respectively. The significant classification factors were the concentrations of aggressive carbon dioxide, sulphate ions and, less significant, pH. The presence of magnesium and ammonium ions in groundwater did not have any classification significance because of low concentrations. The occurrence of aggressive groundwater is associated with the environment of river sediments, mainly of Holocene and Pleistocene age. Groundwater beneath till and clay formations, mainly of Pleistocene age, and of anthropogenic banks and dumps shows significantly lower aggressiveness. Aggressiveness of groundwater sampled from the aquifer covered by Neogene clay deposit is not demonstrated. The aggressiveness of Wrocław groundwater shows a mosaic space character resulting from the geological structure of the city's subsurface formations and is probably also related to the form of land development. The most aggressive ones were associated with green, agricultural and liquidated municipal waste dump areas.
Źródło:
Przegląd Geologiczny; 2021, 69, 12; 901--908
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość trytu i skład izotopowy tlenu w płytkich wodach podziemnych w punktach badawczych krajowej sieci monitoringu
Tritium content and oxygen isotopic composition in shallow groundwater in observation points of the national monitoring network
Autorzy:
Nowicki, Z.
Leśniak, P.M.
Wilamowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075445.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
tryt
stabilne izotopy
czas przebywania
płytkie wody podziemne
tritium
stable isotopes
residence time
shallow groundwater
Opis:
The points of the national network of groundwater monitoring comprise a stable benchmarks in quality and quantity monitoring. The obtained data (tritium and δ18O) are important for understanding the groundwater cycling and are indirect indicators of aquifer vulnerability to anthropogenic pollution. The goal of this paper is to present the relation of the tritium content and delta value of stable isotopes of oxygen against the groundwater sampling depth in 2004–2012. It is demonstrated that the remains of “nuclear” tritium concentration is still present in groundwater as a tritium peak at depths around 30 m. Determination of dynamics of recharge in groundwater bodies, based on national network observation points is associated to the estimation of the groundwater residence time in aquifers and remains one the vital problem of hydrogeology.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 976--980
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Warunki rozwoju i rozmieszczenie torfowisk w Kotlinie Orawsko-Nowotarskiej
Development conditions and distribution of peat bogs in the Orava-Nowy Targ Basin
Autorzy:
Łajczak, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074702.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Kotlina Orawsko-Nowotarska
Karpaty Zachodnie
torfowiska niskie
torfowiska wysokie
wypływy wód gruntowych
Orava-Nowy Targ Basin
Western Carpathians
low peat bogs
raised peat bogs
shallow groundwater circulation
Opis:
The Orava-Nowy Targ Basin is the only intramontane basin in the Carpathian Mountains, where numerous low and raised peat bogs developed in the Holocene. The peat bogs were originally comprising about 40% of the basin area. to became confined to 12%, in result of several centuries of exploitation of peat. On the basis of investigations on geomorphological location of the preserved relics of peat bogs, and reconstructions of their original extent, an attempt was made to identify natural environment factors which had the biggest influence on development of peat-forming process within the Orava-Nowy Targ Basin. The most important of these factors were found to be landforms of fluvioglacial and fluvial accumulation and their composition, as well climatic conditions. However, it should be stated that distribution of raised peat bogs appears to be mainly controlled by the mode of circulation of shallow groundwaters and location of their stable outflows. This is an aspect of development of peat bogs that has not been studied up to now.
Źródło:
Przegląd Geologiczny; 2009, 57, 8; 694-694
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Reduction of the extent of peat deposits and their water retention capacity in the Orava-Nowy Targ Basin and Bieszczady Mts. due to human activity
Autorzy:
Łajczak, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075088.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
anthropopression
raised bog
peat dome
post-peat area
peat extraction
reclamation works
shallow groundwater
Orava-Nowy Targ Basin
Bieszczady Mts.
antropopresja
wysokie torfowisko
kopuła torfowa
młodsze potorfie
wydobycie torfu
prace rekultywacyjne
płytkie wody podziemne
Kotlina Orawsko-Nowotarska
Bieszczady
Opis:
The paper deals with the problem of anthropogenic changes in the extent of peat deposits, their volume and water retention capacity of raised and valley peat bogs in the Polish part of the Orava-Nowy Targ Basin and the Bieszczady Mts. This problem has not received a great deal of attention in the research literature. Special attention was paid to the remnants of peat domes and post-peat areas. The decrease in the area of peat bogs, the volume of peat deposit and the quantity of water retained within them were estimated for the last ca. 400 years. This paper is based on an analysis of maps produced over the last 230 years as well as aerial photographs. Field data and laboratory data were also analyzed as part of this research.
Źródło:
Przegląd Geologiczny; 2013, 61, 9; 532--540
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-4 z 4

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