2017
DOI: 10.1007/s00767-016-0348-6
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Grundwasserfließgeschehen Mecklenburg-Vorpommerns – Geohydraulische Modellierung mit Detrended Kriging

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Cited by 3 publications
(5 citation statements)
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“…Monitoring comprised the uppermost three regional aquifer systems, but not all of them are contiguous (Hennig et al, 2002). In addition to the regional aquifer systems, in some areas shallow local aquifers with an extent of usually a few square kilometres, occasionally more than 100 km 2 , have been identified and are monitored as well (Hilgert and Hennig, 2017). These local aquifers are not strictly hydraulically decoupled from the regional aquifer systems, but their hydraulic connection is inhibited (Hilgert and Hennig, 2017).…”
Section: Study Regionmentioning
confidence: 99%
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“…Monitoring comprised the uppermost three regional aquifer systems, but not all of them are contiguous (Hennig et al, 2002). In addition to the regional aquifer systems, in some areas shallow local aquifers with an extent of usually a few square kilometres, occasionally more than 100 km 2 , have been identified and are monitored as well (Hilgert and Hennig, 2017). These local aquifers are not strictly hydraulically decoupled from the regional aquifer systems, but their hydraulic connection is inhibited (Hilgert and Hennig, 2017).…”
Section: Study Regionmentioning
confidence: 99%
“…In addition to the regional aquifer systems, in some areas shallow local aquifers with an extent of usually a few square kilometres, occasionally more than 100 km 2 , have been identified and are monitored as well (Hilgert and Hennig, 2017). These local aquifers are not strictly hydraulically decoupled from the regional aquifer systems, but their hydraulic connection is inhibited (Hilgert and Hennig, 2017). A mean annual groundwater recharge of +122.3 mm for the whole of Mecklenburg-Vorpommern was estimated for the years 1971 to 2000 by Hilgert (2009) based on the work of Hennig and Hilgert (2007).…”
Section: Study Regionmentioning
confidence: 99%
See 1 more Smart Citation
“…Monitoring comprised the uppermost three regional aquifer systems, but not all of them are contiguous (Hennig et al, 2002). In addition to the regional aquifer systems, in some areas shallow local aquifers with an 135 extent of usually a few km 2 , occasionally more than 100 km 2 , have been identified and are monitored as well (Hilgert and Hennig, 2017). These local aquifers are not strictly hydraulically decoupled from the regional aquifer systems, but their hydraulic connection is inhibited (Hilgert and Hennig, 2017).…”
Section: Study Regionmentioning
confidence: 99%
“…In addition to the regional aquifer systems, in some areas shallow local aquifers with an 135 extent of usually a few km 2 , occasionally more than 100 km 2 , have been identified and are monitored as well (Hilgert and Hennig, 2017). These local aquifers are not strictly hydraulically decoupled from the regional aquifer systems, but their hydraulic connection is inhibited (Hilgert and Hennig, 2017). A mean annual groundwater recharge of +122.3 mm for the whole Mecklenburg-Vorpommern was estimated for the years 1971 to 2000 by Hilgert (2009) based on the work of Hennig and Hilgert (2007).…”
Section: Study Regionmentioning
confidence: 99%