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      <abstractText>Characterizing the lithological and hydraulic behavior of heterogeneous groundwater systems presents a significant challenge in hydrogeology. Traditional methods often rely on sparse data points that lead to inaccurate representations of the complex systems. This study presents an innovative approach to the characterization of the heterogeneous groundwater systems using wireline logs analyzed by machine learning (ML) techniques to infer the lithological variations and estimate aquifer parameters within the Quaternary aquifer system in the Debrecen area, Eastern Hungary. Initially, Manhattan distance-based k-means analysis as an outliers-resistance clustering method is employed to identify distinct lithological clusters based on the well logs responses. The results of the k-means clustering were then used to train ML classifiers including linear discriminant analysis, gradient boosting, random forest, and support vector machine for automated mapping of the lithofacies distribution. Additionally, the study introduced the first application of isometric map (IsoMap) to estimate the shale content and hydraulic conductivity within the aquifer system. The IsoMapping extracts latent components that capture essential features of the wireline logs and correlate them to the aquifer parameters. The regression between the latent component and the deterministically estimated shale volume and hydraulic conductivity showed significant exponential relationships resulting in universal equations that can be used independently to estimate these parameters. For more robust estimation, genetic algorithm global optimization was applied to refine the regression parameters governing these relationships to overcome the limitations associated with linearized estimations. The proposed approach provided a fast, automated, and effective alternative for characterizing heterogeneous groundwater, offering reliable inputs for groundwater flow and contaminant transport models.</abstractText>
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      <label>Püspöki Z. et al. A quasi-continuous long-term (5 Ma) Mid-European mountain permafrost record based on fluvial magnetic susceptibility and its contribution to the explanation of Plio–Pleistocene glaciations. 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&lt;div class=&quot;title&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;35572752&quot; target=&quot;_blank&quot;&gt;A quasi-continuous long-term (5 Ma) Mid-European mountain permafrost record based on fluvial magnetic susceptibility and its contribution to the explanation of Plio–Pleistocene glaciations&lt;/a&gt;&lt;/div&gt;    &lt;div&gt;		&lt;span class=&quot;journal-title&quot;&gt;BOREAS&lt;/span&gt;

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				&lt;div class=&quot;journal-subject&quot;&gt;Folyóirat szakterülete: Scopus - Ecology, Evolution, Behavior and Systematics&amp;nbsp;&amp;nbsp;&amp;nbsp;SJR indikátor:&amp;nbsp;Q1&lt;/div&gt;
				&lt;div class=&quot;journal-subject&quot;&gt;Folyóirat szakterülete: Scopus - Geology&amp;nbsp;&amp;nbsp;&amp;nbsp;SJR indikátor:&amp;nbsp;Q1&lt;/div&gt;
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Forrás	 Idéző
	
	
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&lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2026.05.05. 15:23 Bereczki László (Geológia, geofizika)
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        &lt;div class=&quot;lockedBy&quot;&gt;Központi kezelésű 2026.05.13. 20:15  Vasvari Lilian (MTMT Központ, admin)
        &lt;/div&gt;


	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Export Date: 20 March 2025&lt;/pre&gt;
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      <comment>József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Geology, Institute of Geography and Earth Sciences, Eötvös Loránd University (ELTE), Budapest, Hungary            
            József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Geophysics and Space Science, Institute of Geography and Earth Sciences, Eötvös Loránd University (ELTE), Budapest, Hungary            
            Department of Geology and Geological Engineering, Université Laval, Québec City, Canada            
            Export Date: 29 November 2024            
            Correspondence Address: Czauner, B.; József and Erzsébet Tóth Endowed Hydrogeology Chair, Hungary; email: czauner.brigitta@ttk.elte.hu</comment>
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(2024) SCIENTIFIC REPORTS 2045-2322 14 1</label><template>&lt;div class=&quot;JournalArticle Publication short-list&quot;&gt; &lt;div class=&quot;authors&quot;&gt; &lt;span class=&quot;author-name&quot; mtid=&quot;10029746&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10029746&quot; target=&quot;_blank&quot;&gt;Czauner, Brigitta ✉&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10059904&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10059904&quot; target=&quot;_blank&quot;&gt;Szijártó, Márk&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10008382&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10008382&quot; target=&quot;_blank&quot;&gt;Sztanó, Orsolya&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; 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							&lt;span class=&quot;author-name&quot; &gt;Molson John
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Geology, Institute of Geography and Earth Sciences, Eötvös Loránd University (ELTE), Budapest, Hungary            
            József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Geophysics and Space Science, Institute of Geography and Earth Sciences, Eötvös Loránd University (ELTE), Budapest, Hungary            
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      <comment>Supervisory Authority for Regulatory Affairs, Alkotás út 50, Budapest, H-1123, Hungary            
            Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, CB2 1ER, United Kingdom            
            Wigner Research Centre for Physics, Konkoly-Thege Miklós u. 29-33, Budapest, H-1121, Hungary            
            Department of Mineralogy and Geology, University of Debrecen, Egyetem tér 1, Debrecen, H-4032, Hungary            
            Németh László u. 2/C, Dunakeszi, H-2120, Hungary            
            Petőfi Lutheran Grammar School of Aszód, Régész u. 34, Aszód, H-2170, Hungary            
            Western Balkans Green Center, Naphegy tér 8, Budapest, H-1016, Hungary            
            Faculty of Earth Science and Engineering, University of Miskolc, Egyetemváros, Miskolc, H-3515, Hungary            
            István út 21. IV/36, Debrecen, H-4031, Hungary            
            Department of Geophysics and Space Science, Eötvös Lóránd University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary            
            Middle-Danube-Valley Water Directorate, Rákóczi u. 41, Budapest, H-1088, Hungary            
            Export Date: 7 July 2023            
            Correspondence Address: Gibbard, P.L.; Scott Polar Research Institute, Lensfield Road, United Kingdom; email: plg1@cam.ac.uk</comment>
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      <title>Obliquity-driven mountain permafrost-related fluvial magnetic susceptibility cycles in the Quaternary mid-latitude long-term (2.5 Ma) fluvial Maros Fan in the Pannonian Basin</title>
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      <abstractText>Magnetic susceptibility (MS) of the Quaternary long-term mid-latitude Maros fluvial fan (Pannonian Basin) was
recorded to understand the stratigraphical features of source-proximal fluvial depositional settings. Three fully cored
500-m-deep boreholes were sampled at 0.5-m intervals; low-field and frequency dependent MS were measured, and
complementary hysteresis and SEM-EDAX investigationswere performed on selected samples. Logged susceptibility
data were also used to log correlations established by a simultaneous comparison of wireline log and laboratory
measurements. Time-series analyses of the susceptibility records reveal a ∼41-ka and ∼100-ka cyclicity. Towards the
source-distal sections the intensity of the ∼41-ka cycles decreases, while that of the ∼100-ka cycles remains strong.
Stratigraphical and spectral similarities were observed between the Maros fluvial fan and Chinese loess records;
however, based on complementary magnetic data, the magnetic phase of the Maros Fan sections is related to the
detrital magnetite that originates from the catchment during early postglacial permafrost degradations. The
amplification of the ∼41-ka cycles can be attributed to the very high susceptibility values in source-proximal settings
and to the special stratigraphical feature of the distributive fluvial systems. This comprises the increased avulsion
frequency on the fluvial fans in ‘glacial recession periods’, in concert with the ‘early postglacial’ occurrence of the
permafrost-related magnetite originating from the catchment. As a local phenomenon, this is significant since it
records the obliquity-driven variations in permafrost development in a catchment. However, fluvial and alluvial fans
are widespread depositional landforms within the Eurasian mountain range and were possibly the same during the
Quaternary deglaciations. Thus, obliquity-driven magnetic susceptibility variations in source-proximal fan deposits
attached or adjacent to regions of loess deposition should also be considered when scanning for potential source
material of aeolian deposits.</abstractText>
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(2023) BOREAS 0300-9483 1502-3885 52 3 402-426</label><template>&lt;div class=&quot;JournalArticle Publication short-list&quot;&gt; &lt;div class=&quot;authors&quot;&gt; &lt;span class=&quot;author-name&quot; mtid=&quot;10043232&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10043232&quot; target=&quot;_blank&quot;&gt;Püspöki, Z.&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; &gt; Gibbard, P.L. ✉ &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10009008&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10009008&quot; target=&quot;_blank&quot;&gt;Kiss, L.F.&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10036965&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10036965&quot; target=&quot;_blank&quot;&gt;McIntosh, R.W.&lt;/a&gt; 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&lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2026.05.05. 15:19 Bereczki László (Geológia, geofizika)
&lt;/div&gt;


        &lt;div class=&quot;lockedBy&quot;&gt;Központi kezelésű 2024.04.13. 18:37  Vasvari Lilian (MTMT Központ, admin)
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Supervisory Authority for Regulatory Affairs, Alkotás út 50, Budapest, H-1123, Hungary            
            Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, CB2 1ER, United Kingdom            
            Wigner Research Centre for Physics, Konkoly-Thege Miklós u. 29-33, Budapest, H-1121, Hungary            
            Department of Mineralogy and Geology,...&lt;/pre&gt;
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      <label>Zoltán Püspöki et al. LONG TERM PANNONIAN FLUVIAL MAGNETIC SUSCEPTIBILITY RECORDS DOCUMENTING ALPINE PERMAFROST DEVELOPMENT IN COLD EVENTS OF THE EUROPEAN QUATERNARY. (2021) Megjelent: Quaternary stratigraphy – palaeoenvironment and humans in Eurasia: INQUA SEQS 2021 Conference proceedings pp. 93-94</label><template>&lt;div class=&quot;BookChapter Publication short-list&quot;&gt; &lt;div class=&quot;authors&quot;&gt; &lt;span class=&quot;author-name&quot; mtid=&quot;10043232&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10043232&quot; target=&quot;_blank&quot;&gt;Zoltán, Püspöki&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; &gt; Philip, Leonard Gibbard &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; &lt;/div &gt;&lt;div class=&quot;title&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;32708912&quot; mtid=&quot;32708912&quot; target=&quot;_blank&quot;&gt;LONG TERM PANNONIAN FLUVIAL MAGNETIC SUSCEPTIBILITY RECORDS DOCUMENTING ALPINE PERMAFROST DEVELOPMENT IN COLD EVENTS OF THE EUROPEAN QUATERNARY&lt;/a&gt;&lt;/div&gt; &lt;div class=&quot;InBook&quot;&gt;In: Ratajczak-Skrzatek, Urszula; Kovalchuk, Oleksandr; Stefaniak, Krzysztof (szerk.) &lt;span class=&quot;booktitle&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;32711263&quot; target=&quot;_blank&quot;&gt;Quaternary stratigraphy – palaeoenvironment and humans in Eurasia: INQUA SEQS 2021 Conference proceedings &lt;/a&gt;&lt;/span &gt; &lt;/div&gt;&lt;div class=&quot;pub-info&quot;&gt; &lt;span class=&quot;publishedAt&quot;&gt;Wroclaw, Lengyelország : &lt;span class=&quot;publisher&quot;&gt;University of Wroclaw&lt;/span&gt;, &lt;span class=&quot;publisher&quot;&gt;Polish Geological Society&lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2021)&lt;/span&gt; &lt;span class=&quot;page&quot;&gt; pp. 93-94. , 2 p. &lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;pub-end&quot;&gt;&lt;div class=&quot;identifier-list&quot;&gt; &lt;span class=&quot;identifiers&quot;&gt; &lt;span class=&quot;id identifier oa_GREEN&quot; title=&quot; Green &quot;&gt; 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target=&quot;_blank&quot;&gt;LONG TERM PANNONIAN FLUVIAL MAGNETIC SUSCEPTIBILITY RECORDS DOCUMENTING ALPINE PERMAFROST DEVELOPMENT IN COLD EVENTS OF THE EUROPEAN QUATERNARY&lt;/a&gt;&lt;/div&gt; &lt;div class=&quot;InBook&quot;&gt;&lt;div class=&quot;chapter-in&quot;&gt;In:&lt;/div&gt; &lt;div class=&quot;authors&quot;&gt; &lt;div class=&quot;autype autype-1&quot;&gt; &lt;span class=&quot;author-name&quot; &gt;Ratajczak-Skrzatek Urszula &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; &gt;Kovalchuk Oleksandr &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; &gt;Stefaniak Krzysztof &lt;/span&gt; (szerk.) &lt;/div&gt; &lt;/div&gt; &lt;div class=&quot;booktitle&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;32711263&quot; target=&quot;_blank&quot;&gt;Quaternary stratigraphy – palaeoenvironment and humans in Eurasia: INQUA SEQS 2021 Conference proceedings &lt;/a&gt;&lt;/div&gt; &lt;div class=&quot;conference&quot;&gt; Konferencia helye, ideje: &lt;span class=&quot;location&quot;&gt;Wroclaw, Lengyelország &lt;span class=&quot;conference-date&quot;&gt;2021.12.13. - 2021.12.13.&lt;/span&gt; &lt;/div&gt; &lt;span class=&quot;publishedAt&quot;&gt;Wroclaw: &lt;span class=&quot;publishers&quot;&gt;University of Wroclaw&lt;/span&gt;, &lt;span class=&quot;publishers&quot;&gt;Polish Geological Society&lt;/span&gt;, &lt;span class=&quot;page&quot;&gt; pp 93-94 &lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2021)&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;pub-footer&quot;&gt; &lt;span class=&quot;language&quot; xmlns=&quot;http://www.w3.org/1999/html&quot;&gt;Nyelv: Angol | &lt;/span&gt; &lt;span class=&quot;identifiers&quot;&gt; &lt;span class=&quot;id identifier oa_GREEN&quot; title=&quot; Green &quot;&gt; &lt;a style=&quot;color:black&quot; title=&quot;138304&quot; target=&quot;_blank&quot; href=&quot;https://real.mtak.hu/138304&quot;&gt; REAL &lt;/a&gt; &lt;/span&gt; &lt;/span&gt; &lt;span class=&quot;bookchapter-ids&quot;&gt;Befoglaló link(ek):&lt;/span&gt; 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