Hit papers significantly outperform the citation benchmark for their cohort. A paper qualifies
if it has ≥500 total citations, achieves ≥1.5× the top-1% citation threshold for papers in the
same subfield and year (this is the minimum needed to enter the top 1%, not the average
within it), or reaches the top citation threshold in at least one of its specific research
topics.
Determining the turnover time of groundwater systems with the aid of environmental tracers
1982642 citationsPiotr Małoszewski, A. Zuberprofile →
On the physical meaning of the dispersion equation and its solutions for different initial and boundary conditions
Citations per year, relative to A. Zuber A. Zuber (= 1×)
peers
Mary P. Anderson
Countries citing papers authored by A. Zuber
Since
Specialization
Citations
This map shows the geographic impact of A. Zuber's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by A. Zuber with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites A. Zuber more than expected).
This network shows the impact of papers produced by A. Zuber. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by A. Zuber. The network helps show where A. Zuber may publish in the future.
Co-authorship network of co-authors of A. Zuber
This figure shows the co-authorship network connecting the top 25 collaborators of A. Zuber.
A scholar is included among the top collaborators of A. Zuber based on the total number of
citations received by their joint publications. Widths of edges
represent the number of papers authors have co-authored together.
Node borders
signify the number of papers an author published with A. Zuber. A. Zuber is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Zuber, A., et al.. (2011). Wody podziemne Piwnicznej-Zdroju, ich wiek i obszary zasilania, według danych izotopowych. Biuletyn Państwowego Instytutu Geologicznego.1 indexed citations
3.
Zuber, A., et al.. (2010). Groundwater ages and altitudes of recharge areas in the Polish Tatra Mts. as determined from 3 H, d18 O and d2 H data. Geological Quarterly. 52(1). 71–80.4 indexed citations
4.
Zuber, A., et al.. (2010). ON THE ORIGIN OF CHLORIDE WATERS IN THE POLISH FLYSCH CARPATHIANS. Biuletyn Państwowego Instytutu Geologicznego. 441(441). 201–208.4 indexed citations
5.
Duliński, Marek, et al.. (2010). WATER AGES IN THERMAL SYSTEM OF THE PODHALE BASIN (INNER CARPATHIANS, SOUTHERN POLAND). Biuletyn Państwowego Instytutu Geologicznego. 441(441). 7–18.1 indexed citations
6.
Witczak, S., et al.. (2010). Hydrodynamic modelling, environmental tracers and hydrochemistry of a confined sandy aquifer (Kędzierzyn-Głubczyce Subtrough, SW Poland). Geological Quarterly. 51(1). 1–16.11 indexed citations
7.
Ciężkowski, Wojciech, et al.. (2010). Mineral and thermal waters of Poland. Przegląd Geologiczny. 58. 762–773.25 indexed citations
8.
Duliński, Marek, et al.. (2009). Znaczniki oerodowiskowe w wodach termalnych niecki podhalańskiej. Przegląd Geologiczny. 57.1 indexed citations
9.
Ciężkowski, Wojciech, et al.. (2009). Typy chemiczne szczaw w Karpatach fliszowych a wiek wody. Biuletyn Państwowego Instytutu Geologicznego. 436. 47–54.1 indexed citations
10.
Olszewska, Barbara, et al.. (2009). Pochodzenie i wiek wody mineralnej w Dobrowodzie k. Buska Zdroju. Przegląd Geologiczny. 57(4). 286–293.6 indexed citations
11.
Zuber, A., et al.. (2009). Ultrafiltracja i diageneza jako ważne procesy formujące skład izotopowy i chemiczny wody w niektórych basenach sedymentacyjnych. Biuletyn Państwowego Instytutu Geologicznego. 575–582.1 indexed citations
12.
Zuber, A., et al.. (2008). Touristic geoattractions of Polish Spas. Przegląd Geologiczny. 56. 706–710.8 indexed citations
13.
Śliwka, I., et al.. (2004). Headspace Extraction Method for Simultaneous Determination of SF 6 , CCl 3 F, CCl 2 F 2 and CCl 2 FCClF 2 in Water. Chemia Analityczna. 49(4). 535–549.7 indexed citations
14.
Zuber, A., et al.. (2004). Występowanie i geneza wód chlorkowych Soli. Przegląd Geologiczny. 52(12). 1179–1179.5 indexed citations
Oszczypko, Nestor & A. Zuber. (2002). Geological and isotopic evidence of diagenetic waters in the Polish Flysch Carpathians. Jagiellonian University Repository (Jagiellonian University).27 indexed citations
17.
Różański, Kazimierz & A. Zuber. (2000). Wody infiltracji glacjalnej w Europie - mit czy rzeczywistość. Przegląd Geologiczny. 48(9). 796–803.5 indexed citations
18.
Zuber, A., Wojciech Ciężkowski, J. Grabczak, & Marek Duliński. (1999). Wieki i położenie obszarów zasilania wód mineralnych Krynicy oszacowane ze zmian czasowych stężeń trytu oraz wartości δ18O i δD. Przegląd Geologiczny. 47(6). 574–583.3 indexed citations
Zuber, A. & J. Grabczak. (1987). O genezie wód chlorkowych w Karpatach fliszowych (ciąg dalszy polemiki). Przegląd Geologiczny. 35(7). 366–372.
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
bibliographic database. While OpenAlex provides broad and valuable coverage of the global
research landscape, it—like all bibliographic datasets—has inherent limitations. These include
incomplete records, variations in author disambiguation, differences in journal indexing, and
delays in data updates. As a result, some metrics and network relationships displayed in
Rankless may not fully capture the entirety of a scholar's output or impact.