Geochemical and hydraulic modeling of cavernous structures in potash seams : = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen

Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes f...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Steding, Svenja [verfasserIn] Kühn, Michael - 1967- [akademischer betreuerIn] Schneider, Wilfried [akademischer betreuerIn] Bozau, Elke - 1966- [akademischer betreuerIn] Kempka, Thomas - 1976- [akademischer betreuerIn] Wilke, Max - 1966- [akademischer betreuerIn]
Körperschaften:	Universität Potsdam [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Universität Potsdam ; 2022

Format:	E-Book
Sprache:	Englisch

Erschienen:	Potsdam: 2022

Schlagwörter:	Kalibergbau / Salzkaverne / Flöz / Geochemie / Höhle / Modell Kalisalzlagerstätte / Kalibergwerk / Hydrogeochemie / Hydrogeologie / Kaverne / Modellierung
Formangabe:	Hochschulschrift

Anmerkung:	Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation
Umfang:	1 Online-Ressource (IX, 104 Seiten, 13409 KB) ; Illustrationen, Diagramme

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Steding, Svenja: Geochemical and hydraulic modeling of cavernous structures in potash seams - Potsdam, 2022

Links:	Link aufrufen Volltext Volltext Link aufrufen Link aufrufen

DOI / URN:	urn:nbn:de:kobv:517-opus4-548182 10.25932/publishup-54818

Katalog-ID:	1801764484

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520			\|a Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits.
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topic_title	551.49 DE-101 550 DE-101 MONTAN DE-105 fid 2027 01 DE-105 00 s ebook Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd
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title_full	Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke
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title_sub	= Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen
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title_sort	geochemical and hydraulic modeling of cavernous structures in potash seams = geochemische und hydraulische modellierung kavernöser strukturen in kaliflözen
title_auth	Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen
abstract	Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation
abstractGer	Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation
abstract_unstemmed	Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation
url	https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 https://doi.org/10.25932/publishup-54818 https://d-nb.info/1257218565/34 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818
author2	Kühn, Michael 1967- Schneider, Wilfried Bozau, Elke 1966- Kempka, Thomas 1976- Wilke, Max 1966- Universität Potsdam
author2Str	Kühn, Michael 1967- Schneider, Wilfried Bozau, Elke 1966- Kempka, Thomas 1976- Wilke, Max 1966- Universität Potsdam
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allfields	urn:nbn:de:kobv:517-opus4-548182 urn 10.25932/publishup-54818 doi (DE-627)1801764484 (DE-599)KXP1801764484 (OCoLC)1316788284 DE-627 ger DE-627 rda eng XA-DE-BB 551.49 DE-101 550 DE-101 MONTAN DE-105 fid Steding, Svenja verfasserin (DE-588)1257464124 (DE-627)1801734151 aut Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen Potsdam 2022 1 Online-Ressource (IX, 104 Seiten, 13409 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation Dissertation Universität Potsdam 2022 kumulative Dissertation Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd (DE-627) Kühn, Michael 1967- akademischer betreuerin (DE-588)1032411473 (DE-627)738443212 (DE-576)380034441 dgs Schneider, Wilfried akademischer betreuerin (DE-588)1161608850 (DE-627)1024890465 (DE-576)506753301 dgs Bozau, Elke 1966- akademischer betreuerin (DE-588)113790058 (DE-627)480697337 (DE-576)173894410 dgs Kempka, Thomas 1976- akademischer betreuerin (DE-588)137209606 (DE-627)591017431 (DE-576)30281552X dgs Wilke, Max 1966- akademischer betreuerin (DE-588)121248941 (DE-627)705333965 (DE-576)292608330 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Steding, Svenja Geochemical and hydraulic modeling of cavernous structures in potash seams Potsdam, 2022 IX, 104 Seiten (DE-627)1801765944 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2022-06-27 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-54818 2022-06-27 Resolving-System kostenfrei Volltext https://d-nb.info/1257218565/34 2022-06-27 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818 application/pdf 2022-06-27 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP FID-MONTAN GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 045F 551.49 20 01 0084 4159175600 x 30-06-22 21 01 0046 4159192254 z 30-06-22 22 01 0018 4159208673 SUBolrd xu 30-06-22 23 01 0830 4159224822 olr-d x 30-06-22 30 01 0104 4159237339 z 30-06-22 40 01 0007 4159246400 xsn 30-06-22 60 01 0705 4159263372 OLRD z 30-06-22 63 01 3401 415928048X ORD x 30-06-22 65 01 0003 4169925009 GBV-ODiss Open Access z 18-07-22 70 01 0089 4159290337 zdo 30-06-22 105 01 0841 4159490875 z 30-06-22 110 01 3110 4159305474 x 30-06-22 132 01 0959 415931905X OLR-DISS x 30-06-22 151 01 0546 415942113X OLR-ODISS z 30-06-22 161 01 0960 4159434134 ORD z 30-06-22 285 01 0517 413395386X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. 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spelling	urn:nbn:de:kobv:517-opus4-548182 urn 10.25932/publishup-54818 doi (DE-627)1801764484 (DE-599)KXP1801764484 (OCoLC)1316788284 DE-627 ger DE-627 rda eng XA-DE-BB 551.49 DE-101 550 DE-101 MONTAN DE-105 fid Steding, Svenja verfasserin (DE-588)1257464124 (DE-627)1801734151 aut Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen Potsdam 2022 1 Online-Ressource (IX, 104 Seiten, 13409 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation Dissertation Universität Potsdam 2022 kumulative Dissertation Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd (DE-627) Kühn, Michael 1967- akademischer betreuerin (DE-588)1032411473 (DE-627)738443212 (DE-576)380034441 dgs Schneider, Wilfried akademischer betreuerin (DE-588)1161608850 (DE-627)1024890465 (DE-576)506753301 dgs Bozau, Elke 1966- akademischer betreuerin (DE-588)113790058 (DE-627)480697337 (DE-576)173894410 dgs Kempka, Thomas 1976- akademischer betreuerin (DE-588)137209606 (DE-627)591017431 (DE-576)30281552X dgs Wilke, Max 1966- akademischer betreuerin (DE-588)121248941 (DE-627)705333965 (DE-576)292608330 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Steding, Svenja Geochemical and hydraulic modeling of cavernous structures in potash seams Potsdam, 2022 IX, 104 Seiten (DE-627)1801765944 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2022-06-27 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-54818 2022-06-27 Resolving-System kostenfrei Volltext https://d-nb.info/1257218565/34 2022-06-27 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818 application/pdf 2022-06-27 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP FID-MONTAN GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 045F 551.49 20 01 0084 4159175600 x 30-06-22 21 01 0046 4159192254 z 30-06-22 22 01 0018 4159208673 SUBolrd xu 30-06-22 23 01 0830 4159224822 olr-d x 30-06-22 30 01 0104 4159237339 z 30-06-22 40 01 0007 4159246400 xsn 30-06-22 60 01 0705 4159263372 OLRD z 30-06-22 63 01 3401 415928048X ORD x 30-06-22 65 01 0003 4169925009 GBV-ODiss Open Access z 18-07-22 70 01 0089 4159290337 zdo 30-06-22 105 01 0841 4159490875 z 30-06-22 110 01 3110 4159305474 x 30-06-22 132 01 0959 415931905X OLR-DISS x 30-06-22 151 01 0546 415942113X OLR-ODISS z 30-06-22 161 01 0960 4159434134 ORD z 30-06-22 285 01 0517 413395386X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. 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allfields_unstemmed	urn:nbn:de:kobv:517-opus4-548182 urn 10.25932/publishup-54818 doi (DE-627)1801764484 (DE-599)KXP1801764484 (OCoLC)1316788284 DE-627 ger DE-627 rda eng XA-DE-BB 551.49 DE-101 550 DE-101 MONTAN DE-105 fid Steding, Svenja verfasserin (DE-588)1257464124 (DE-627)1801734151 aut Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen Potsdam 2022 1 Online-Ressource (IX, 104 Seiten, 13409 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation Dissertation Universität Potsdam 2022 kumulative Dissertation Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd (DE-627) Kühn, Michael 1967- akademischer betreuerin (DE-588)1032411473 (DE-627)738443212 (DE-576)380034441 dgs Schneider, Wilfried akademischer betreuerin (DE-588)1161608850 (DE-627)1024890465 (DE-576)506753301 dgs Bozau, Elke 1966- akademischer betreuerin (DE-588)113790058 (DE-627)480697337 (DE-576)173894410 dgs Kempka, Thomas 1976- akademischer betreuerin (DE-588)137209606 (DE-627)591017431 (DE-576)30281552X dgs Wilke, Max 1966- akademischer betreuerin (DE-588)121248941 (DE-627)705333965 (DE-576)292608330 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Steding, Svenja Geochemical and hydraulic modeling of cavernous structures in potash seams Potsdam, 2022 IX, 104 Seiten (DE-627)1801765944 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2022-06-27 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-54818 2022-06-27 Resolving-System kostenfrei Volltext https://d-nb.info/1257218565/34 2022-06-27 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818 application/pdf 2022-06-27 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP FID-MONTAN GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 045F 551.49 20 01 0084 4159175600 x 30-06-22 21 01 0046 4159192254 z 30-06-22 22 01 0018 4159208673 SUBolrd xu 30-06-22 23 01 0830 4159224822 olr-d x 30-06-22 30 01 0104 4159237339 z 30-06-22 40 01 0007 4159246400 xsn 30-06-22 60 01 0705 4159263372 OLRD z 30-06-22 63 01 3401 415928048X ORD x 30-06-22 65 01 0003 4169925009 GBV-ODiss Open Access z 18-07-22 70 01 0089 4159290337 zdo 30-06-22 105 01 0841 4159490875 z 30-06-22 110 01 3110 4159305474 x 30-06-22 132 01 0959 415931905X OLR-DISS x 30-06-22 151 01 0546 415942113X OLR-ODISS z 30-06-22 161 01 0960 4159434134 ORD z 30-06-22 285 01 0517 413395386X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. Weitere Informationen finden Sie unter https://creativecommons.org/licenses/ z 13-05-22 293 01 3293 4159474756 ORD z 30-06-22 370 01 4370 4159486061 x 30-06-22 2027 01 DE-105 414370000X 00 --%%-- Dn --%%-- --%%-- l01 07-06-22 2403 01 DE-LFER 4145015142 00 --%%-- --%%-- n --%%-- l01 08-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 21 01 0046 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 22 01 0018 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 23 01 0830 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 30 01 0104 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 40 01 0007 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 60 01 0705 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 LF 65 01 0003 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 70 01 0089 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 105 01 0841 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 110 01 3110 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 132 01 0959 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 161 01 0960 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 285 01 0517 https://doi.org/10.25932/publishup-54818 LF 293 01 3293 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 370 01 4370 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 2403 01 DE-LFER https://doi.org/10.25932/publishup-54818 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 TI 8235 285 00 DE-517 00 TG 4520 285 00 DE-517 00 TH 4560 285 00 DE-517 00 TZ 4000 2027 01 DE-105 00 (DE-627)1294229311 DK 553.632 2027 01 DE-105 00 (DE-627)1294185594 DK 622.363.2 2027 01 DE-105 00 (DE-627)1293831727 DK 551.442 2027 01 DE-105 00 (DE-627)1292102578 DK 550.4 2027 01 DE-105 00 (DE-627)1293657883 DK 622.268.8 2027 01 DE-105 00 (DE-627)1296402207 DK 622.031 2027 01 DE-105 00 (DE-627)1293812447 DK 55.001.57 2027 01 DE-105 00 (DE-627)129248635X DK 556.3 2027 01 DE-105 00 (DE-627)1292244216 DK 550.8.05 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 285 01 0517 ACQ 293 01 3293 ORD 23 01 0830 2022-06-30:08:41:59
allfieldsGer	urn:nbn:de:kobv:517-opus4-548182 urn 10.25932/publishup-54818 doi (DE-627)1801764484 (DE-599)KXP1801764484 (OCoLC)1316788284 DE-627 ger DE-627 rda eng XA-DE-BB 551.49 DE-101 550 DE-101 MONTAN DE-105 fid Steding, Svenja verfasserin (DE-588)1257464124 (DE-627)1801734151 aut Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen Potsdam 2022 1 Online-Ressource (IX, 104 Seiten, 13409 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation Dissertation Universität Potsdam 2022 kumulative Dissertation Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd (DE-627) Kühn, Michael 1967- akademischer betreuerin (DE-588)1032411473 (DE-627)738443212 (DE-576)380034441 dgs Schneider, Wilfried akademischer betreuerin (DE-588)1161608850 (DE-627)1024890465 (DE-576)506753301 dgs Bozau, Elke 1966- akademischer betreuerin (DE-588)113790058 (DE-627)480697337 (DE-576)173894410 dgs Kempka, Thomas 1976- akademischer betreuerin (DE-588)137209606 (DE-627)591017431 (DE-576)30281552X dgs Wilke, Max 1966- akademischer betreuerin (DE-588)121248941 (DE-627)705333965 (DE-576)292608330 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Steding, Svenja Geochemical and hydraulic modeling of cavernous structures in potash seams Potsdam, 2022 IX, 104 Seiten (DE-627)1801765944 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2022-06-27 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-54818 2022-06-27 Resolving-System kostenfrei Volltext https://d-nb.info/1257218565/34 2022-06-27 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818 application/pdf 2022-06-27 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP FID-MONTAN GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 045F 551.49 20 01 0084 4159175600 x 30-06-22 21 01 0046 4159192254 z 30-06-22 22 01 0018 4159208673 SUBolrd xu 30-06-22 23 01 0830 4159224822 olr-d x 30-06-22 30 01 0104 4159237339 z 30-06-22 40 01 0007 4159246400 xsn 30-06-22 60 01 0705 4159263372 OLRD z 30-06-22 63 01 3401 415928048X ORD x 30-06-22 65 01 0003 4169925009 GBV-ODiss Open Access z 18-07-22 70 01 0089 4159290337 zdo 30-06-22 105 01 0841 4159490875 z 30-06-22 110 01 3110 4159305474 x 30-06-22 132 01 0959 415931905X OLR-DISS x 30-06-22 151 01 0546 415942113X OLR-ODISS z 30-06-22 161 01 0960 4159434134 ORD z 30-06-22 285 01 0517 413395386X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. Weitere Informationen finden Sie unter https://creativecommons.org/licenses/ z 13-05-22 293 01 3293 4159474756 ORD z 30-06-22 370 01 4370 4159486061 x 30-06-22 2027 01 DE-105 414370000X 00 --%%-- Dn --%%-- --%%-- l01 07-06-22 2403 01 DE-LFER 4145015142 00 --%%-- --%%-- n --%%-- l01 08-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 21 01 0046 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 22 01 0018 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 23 01 0830 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 30 01 0104 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 40 01 0007 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 60 01 0705 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 LF 65 01 0003 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 70 01 0089 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 105 01 0841 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 110 01 3110 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 132 01 0959 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 161 01 0960 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 285 01 0517 https://doi.org/10.25932/publishup-54818 LF 293 01 3293 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 370 01 4370 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-548182 2403 01 DE-LFER https://doi.org/10.25932/publishup-54818 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 TI 8235 285 00 DE-517 00 TG 4520 285 00 DE-517 00 TH 4560 285 00 DE-517 00 TZ 4000 2027 01 DE-105 00 (DE-627)1294229311 DK 553.632 2027 01 DE-105 00 (DE-627)1294185594 DK 622.363.2 2027 01 DE-105 00 (DE-627)1293831727 DK 551.442 2027 01 DE-105 00 (DE-627)1292102578 DK 550.4 2027 01 DE-105 00 (DE-627)1293657883 DK 622.268.8 2027 01 DE-105 00 (DE-627)1296402207 DK 622.031 2027 01 DE-105 00 (DE-627)1293812447 DK 55.001.57 2027 01 DE-105 00 (DE-627)129248635X DK 556.3 2027 01 DE-105 00 (DE-627)1292244216 DK 550.8.05 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 285 01 0517 ACQ 293 01 3293 ORD 23 01 0830 2022-06-30:08:41:59
allfieldsSound	urn:nbn:de:kobv:517-opus4-548182 urn 10.25932/publishup-54818 doi (DE-627)1801764484 (DE-599)KXP1801764484 (OCoLC)1316788284 DE-627 ger DE-627 rda eng XA-DE-BB 551.49 DE-101 550 DE-101 MONTAN DE-105 fid Steding, Svenja verfasserin (DE-588)1257464124 (DE-627)1801734151 aut Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen Potsdam 2022 1 Online-Ressource (IX, 104 Seiten, 13409 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Literaturverzeichnis: Seite 96-101 Volltext: PDF kumulative Dissertation Dissertation Universität Potsdam 2022 kumulative Dissertation Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. Therefore, the objective of the present thesis is to describe the evolution of cavernous structures along potash seams in space and time in order to improve hazard mitigation during the utilization of salt deposits. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4163048-8 (DE-627)105457663 (DE-576)20987824X Kalibergbau gnd s (DE-588)4461775-6 (DE-627)230759068 (DE-576)212678965 Salzkaverne gnd s (DE-588)4154649-0 (DE-627)105521779 (DE-576)209812931 Flöz gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4025362-4 (DE-627)106293907 (DE-576)208960333 Höhle gnd s (DE-588)4039798-1 (DE-627)106226576 (DE-576)209036699 Modell gnd (DE-627) s (DE-588)4163055-5 (DE-627)105457639 (DE-576)209878282 Kalisalzlagerstätte gnd s (DE-588)4722593-2 (DE-627)34975540X (DE-576)215753607 Kalibergwerk gnd s (DE-588)4225478-4 (DE-627)104978848 (DE-576)21030667X Hydrogeochemie gnd s (DE-588)4026307-1 (DE-627)104689129 (DE-576)208965998 Hydrogeologie gnd s (DE-588)4120557-1 (DE-627)105775681 (DE-576)209536098 Kaverne gnd s (DE-588)4170297-9 (DE-627)105403466 (DE-576)209929170 Modellierung gnd (DE-627) Kühn, Michael 1967- akademischer betreuerin (DE-588)1032411473 (DE-627)738443212 (DE-576)380034441 dgs Schneider, Wilfried akademischer betreuerin (DE-588)1161608850 (DE-627)1024890465 (DE-576)506753301 dgs Bozau, Elke 1966- akademischer betreuerin (DE-588)113790058 (DE-627)480697337 (DE-576)173894410 dgs Kempka, Thomas 1976- akademischer betreuerin (DE-588)137209606 (DE-627)591017431 (DE-576)30281552X dgs Wilke, Max 1966- akademischer betreuerin (DE-588)121248941 (DE-627)705333965 (DE-576)292608330 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Steding, Svenja Geochemical and hydraulic modeling of cavernous structures in potash seams Potsdam, 2022 IX, 104 Seiten (DE-627)1801765944 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-548182 2022-06-27 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-54818 2022-06-27 Resolving-System kostenfrei Volltext https://d-nb.info/1257218565/34 2022-06-27 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/54818 application/pdf 2022-06-27 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP FID-MONTAN GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 045F 551.49 20 01 0084 4159175600 x 30-06-22 21 01 0046 4159192254 z 30-06-22 22 01 0018 4159208673 SUBolrd xu 30-06-22 23 01 0830 4159224822 olr-d x 30-06-22 30 01 0104 4159237339 z 30-06-22 40 01 0007 4159246400 xsn 30-06-22 60 01 0705 4159263372 OLRD z 30-06-22 63 01 3401 415928048X ORD x 30-06-22 65 01 0003 4169925009 GBV-ODiss Open Access z 18-07-22 70 01 0089 4159290337 zdo 30-06-22 105 01 0841 4159490875 z 30-06-22 110 01 3110 4159305474 x 30-06-22 132 01 0959 415931905X OLR-DISS x 30-06-22 151 01 0546 415942113X OLR-ODISS z 30-06-22 161 01 0960 4159434134 ORD z 30-06-22 285 01 0517 413395386X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. 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authorswithroles_txt_mv	Steding, Svenja @@aut@@ Kühn, Michael @@dgs@@ Schneider, Wilfried @@dgs@@ Bozau, Elke @@dgs@@ Kempka, Thomas @@dgs@@ Wilke, Max @@dgs@@
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title	Geochemical and hydraulic modeling of cavernous structures in potash seams = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen
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title_alt	Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen
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up_date	2024-07-04T23:45:58.228Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a2200265 4500</leader><controlfield tag="001">1801764484</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220725090312.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220513s2022 gw \|\|\|\|\|om 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">urn:nbn:de:kobv:517-opus4-548182</subfield><subfield code="2">urn</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.25932/publishup-54818</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)1801764484</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)KXP1801764484</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1316788284</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE-BB</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">551.49</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">MONTAN</subfield><subfield code="q">DE-105</subfield><subfield code="2">fid</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Steding, Svenja</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(DE-588)1257464124</subfield><subfield code="0">(DE-627)1801734151</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Geochemical and hydraulic modeling of cavernous structures in potash seams</subfield><subfield code="b"> = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen</subfield><subfield code="c">vorgelegt von Svenja Steding ; Gutachter*in(nen): Michael Kühn, Wilfried Schneider, Elke Bozau ; Betreuer: Michael Kühn, Thomas Kempka, Max Wilke</subfield></datafield><datafield tag="246" ind1="3" ind2="1"><subfield code="a">Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Potsdam</subfield><subfield code="c">2022</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (IX, 104 Seiten, 13409 KB)</subfield><subfield code="b">Illustrationen, Diagramme</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Literaturverzeichnis: Seite 96-101</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Volltext: PDF</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">kumulative Dissertation</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Universität Potsdam</subfield><subfield code="d">2022</subfield><subfield code="g">kumulative Dissertation</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Salt deposits offer a variety of usage types. These include the mining of rock salt and potash salt as important raw materials, the storage of energy in man-made underground caverns, and the disposal of hazardous substances in former mines. The most serious risk with any of these usage types comes from the contact with groundwater or surface water. It causes an uncontrolled dissolution of salt rock, which in the worst case can result in the flooding or collapse of underground facilities. Especially along potash seams, cavernous structures can spread quickly, because potash salts show a much higher solubility than rock salt. However, as their chemical behavior is quite complex, previous models do not account for these highly soluble interlayers. 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Geochemical and hydraulic modeling of cavernous structures in potash seams : = Geochemische und hydraulische Modellierung kavernöser Strukturen in Kaliflözen

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