Simulating groundwater flow in karst aquifers with distributed parameter models—Comparison of porous-equivalent media and hybrid flow approaches (Q58542): Difference between revisions

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Kuniansky, E.L., 2016, Simulating groundwater flow in karst aquifers with distributed parameter models—Comparison of porous-equivalent media and hybrid flow approaches: U.S. Geological Survey Scientific Investigations Report 2016–5116, 14 p., http...
USGS Numbered Series published by U.S. Geological Survey in 2016
Property / instance of
 
Property / instance of: USGS Scientific Investigations Report / rank
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Property / instance of: USGS Scientific Investigations Report / reference
 
Property / publication date
2016
Timestamp+2016-01-01T00:00:00Z
Timezone+00:00
CalendarGregorian
Precision1 year
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Property / publication date: 2016 / rank
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Property / publication date: 2016 / reference
 
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Property / instance of: USGS Open-File Report / rank
 
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Property / publication date
 
15 July 2016
Timestamp+2016-07-15T00:00:00Z
Timezone+00:00
CalendarGregorian
Precision1 day
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Property / publication date: 15 July 2016 / rank
 
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Property / addresses subject
 
Property / addresses subject: Karst Hydrogeology and Geohazards / rank
 
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Property / addresses subject: Karst Hydrogeology and Geohazards / reference
 
Property / addresses subject
 
Property / addresses subject: Groundwater Flow and Transport Modeling / rank
 
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Property / addresses subject: Groundwater Flow and Transport Modeling / reference
 
Property / addresses subject
 
Property / addresses subject: Tunnel Grouting Techniques / rank
 
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Property / addresses subject: Tunnel Grouting Techniques / reference
 
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Property / OpenAlex ID: W2531026311 / rank
 
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Latest revision as of 22:42, 11 September 2024

USGS Numbered Series published by U.S. Geological Survey in 2016
  • sir20165116
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English
Simulating groundwater flow in karst aquifers with distributed parameter models—Comparison of porous-equivalent media and hybrid flow approaches
USGS Numbered Series published by U.S. Geological Survey in 2016
  • sir20165116

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