E. Stouthamer - Academia.edu (original) (raw)
Papers by E. Stouthamer
Environmental Research Communications, 2019
The low-lying and populous Vietnamese Mekong delta is rapidly losing elevation due to acceleratin... more The low-lying and populous Vietnamese Mekong delta is rapidly losing elevation due to accelerating subsidence rates, primarily caused by increasing groundwater extraction. This strongly increases the delta’s vulnerability to flooding, salinization, coastal erosion and, ultimately, threatens its nearly 18 million inhabitants with permanent inundation. We present projections of extraction-induced subsidence and consequent delta elevation loss for this century following six mitigation and non-mitigation extraction scenarios using a 3D hydrogeological model with a coupled geotechnical module. Our results reveal the long-term physically response of the aquifer system following different groundwater extraction pathways and show the potential of the hydrogeological system to recover. When groundwater extraction is allowed to increase continuously, as it did over the past decades, extraction-induced subsidence has the potential to drown the Mekong delta single-handedly before the end of the...
Geomorphology, 2016
The geomorphological development of Holocene coastal plains around the world has been studied sin... more The geomorphological development of Holocene coastal plains around the world has been studied since the beginning of the twentieth century from various disciplines, resulting in large amounts of data. However, the overwhelming quantities and heterogeneous nature of this data have caused the divided knowledge to remain inconsistent and fragmented. To keep improving the understanding of coastal plain geomorphology and geology, cataloguing of data and integration of knowledge are essential. In this paper we present a GIS that incorporates the accumulated data of the Netherlands’ coastal plain and functions as a storage and integration tool for coastal plain mapped data. The GIS stores redigitised architectural elements (beach barriers, tidal channels, intertidal flats, supratidal flats, and coastal fresh water peat) from earlier mappings in separate map layers. A coupled catalogue-style database stores the dating information of these elements, besides references to source studies and annotations regarding changed insights. Using scripts, the system automatically establishes palaeogeographical maps for any chosen moment, combining the above mapping and dating information. In our approach, we strip the information to architectural element level, and we separate mapping from dating information, serving the automatic generation of time slice maps. It enables a workflow in which the maker can iteratively regenerate maps, which speeds up fine-tuning and thus the quality of palaeogeographical reconstruction. The GIS currently covers the late Holocene coastal plain development of the Netherlands. This period witnessed widespread renewed flooding along the southern North Sea coast, coinciding with large-scale reclamation and human occupation. Our GIS method is generic and can be expanded and adapted to allow faster integrated processing of growing amounts of data for many coastal areas and other large urbanising lowlands around the world. It allows maintaining actual data overview and facilitates new ways of analysis at national, regional, and local scales. © 2016 Elsevier B.V.
Environmental Research Letters, 2017
Proceedings of the International Association of Hydrological Sciences, 2015
4th International Geologica Belgica Meeting 2012. Moving Plates and Melting Icecaps – Processes a... more 4th International Geologica Belgica Meeting 2012. Moving Plates and Melting Icecaps – Processes and Forcing Factors in Geology. Brussels 11-14/09/12
In many deltas worldwide subsidence still is an underestimated problem, while the threat posed by... more In many deltas worldwide subsidence still is an underestimated problem, while the threat posed by land subsidence low-lying urbanizing and urbanized deltas exceeds the threat of sea-level rise induced by climate change. Human-induced subsidence is driven by the extraction of hydrocarbons and groundwater, drainage of phreatic groundwater, and loading by buildings and infrastructure. The consequences of subsidence are increased flood risk and flood water depth, rising groundwater levels relative to the land surface, land loss, damage to buildings and infrastructure, and salinization of ground and surface water.. The Netherlands has a long history of subsidence. Large-scale drainage of the extensive peatlands in the western and northern parts of the Netherlands started approximately 1000 years ago as a result of rapid population growth. Subsidence is still ongoing due to (1) continuous drainage of the former peatland, which is now mainly in use as agricultural land and built-up area, (...
In order to improve our insights in the sequence stratigraphic and architectural development of l... more In order to improve our insights in the sequence stratigraphic and architectural development of lower deltaic hydrocarbon reservoirs we study the Last Interglacial Rhine delta (MIS-5), and compare it to its well investigated counterpart, the Holocene (MIS-1) Rhine- Meuse delta (Berendsen & Stouthamer, 2000). The Last Interglacial record has experienced a full glacialinterglacial cycle of sea-level and climate change in a subsiding tectonic setting, and arguably is in a more relevant state of preservation when the delta is to be used as a reservoir analogue.
Quaternary Science Reviews, 2016
This paper describes the sedimentary architecture, chronostratigraphy and palaeogeography of the ... more This paper describes the sedimentary architecture, chronostratigraphy and palaeogeography of the late Middle and Late Pleistocene (Marine Isotope Stage/MIS 6-2) incised Rhine-valley fill in the central Netherlands based on six geological transects, luminescence dating, biostratigraphical data and a 3D geological model. The incised-valley fill consists of a ca. 50 m thick and 10-20 km wide sand-dominated succession and includes a well-developed sequence dating from the Last Interglacial: known as the Eemian in northwest Europe. The lower part of the valley fill contains coarse-grained fluvio-glacial and fluvial Rhine sediments that were deposited under Late Saalian (MIS 6) cold-climatic periglacial conditions and during the transition into the warm Eemian interglacial (MIS 5e-d). This unit is overlain by fine-grained fresh-water flood-basin deposits, which are transgressed by a fine-grained estuarine unit that formed during marine high-stand. This ca. 10 m thick sequence reflects gradual drowning of the Eemian interglacial fluvial Rhine system and transformation into an estuary due to relative sea-level rise. The chronological data suggests a delay in timing of regional Eemian interglacial transgression and sea-level high-stand of several thousand years, when compared to eustatic sea-level. As a result of this glacio-isostatic controlled delay, formation of the interglacial lower deltaic system took only place for a relative short period of time: progradation was therefore limited. During the cooler Weichselian Early Glacial period (MIS 5d-a) deposition of deltaic sediments continued and extensive westward progradation of the Rhine system occurred. Major parts of the Eemian and Weichselian Early Glacial deposits were eroded and buried as a result of sea-level lowering and climate cooling during the early Middle Weichselian (MIS 4-3). Near complete sedimentary preservation occurred along the margins of the incised valley allowing the detailed reconstruction presented here. © 2015 Elsevier Ltd.
Proceedings of the International Association of Hydrological Sciences, 2020
Geologie En Mijnbouw, 2002
Approximately 200,000 lithological borehole descriptions, 1200 14C dates, 36,000 dated archaeolog... more Approximately 200,000 lithological borehole descriptions, 1200 14C dates, 36,000 dated archaeological artifacts, and gradients of palaeochannels were used to reconstruct the Holocene evolution of the fluvial part of the Rhine-Meuse delta. Ages of all Holocene channel belts were stored in a Geographical Information System database that enables generation of palaeogeographic maps for any time during the Holocene. The time resolution
Proceedings of the International Association of Hydrological Sciences, 2015
ABSTRACT Wij bevelen aan in wetsvoorstel dan wel toelichting expliciet te maken dat een gestrooml... more ABSTRACT Wij bevelen aan in wetsvoorstel dan wel toelichting expliciet te maken dat een gestroomlijnde geïntegreerde internetinterface onderdeel zal zijn van de invoering van de BRO. Wij bevelen aan de ‘representatieve vertegenwoordiging afnemers’ uit Artikel 4 specifiek ook op dit uitvoeringsaspect inspraak te verlenen.
International Journal of Sediment Research, 2013
... 1. Five SN cross-sections including time lines (Gouw & Erkens, 2007 NJG) 2. History of se... more ... 1. Five SN cross-sections including time lines (Gouw & Erkens, 2007 NJG) 2. History of sediment delivery to the Holocene delta (PhD thesis Erkens) 3. Mapping and dating Rhine deposition in the Gelderse IJssel valley (Cohen) 4. Late Glacial/Holocene landscape change in the ...
Cohen, K.M., E. Stouthamer, W.Z. Hoek, M.J.P. Gouw, G. Erkens (2007) Palaeogeography of the Holoc... more Cohen, K.M., E. Stouthamer, W.Z. Hoek, M.J.P. Gouw, G. Erkens (2007) Palaeogeography of the Holocene Rhine-Meuse delta: complete stratigraphical coverage of a sizable coastal prism. 11-ième congrès Français de sédimentologie, Caen 23-25 octobre 2007, France. ASF publication 57, p. 70. Oral presentation.
Environmental Research Communications, 2019
The low-lying and populous Vietnamese Mekong delta is rapidly losing elevation due to acceleratin... more The low-lying and populous Vietnamese Mekong delta is rapidly losing elevation due to accelerating subsidence rates, primarily caused by increasing groundwater extraction. This strongly increases the delta’s vulnerability to flooding, salinization, coastal erosion and, ultimately, threatens its nearly 18 million inhabitants with permanent inundation. We present projections of extraction-induced subsidence and consequent delta elevation loss for this century following six mitigation and non-mitigation extraction scenarios using a 3D hydrogeological model with a coupled geotechnical module. Our results reveal the long-term physically response of the aquifer system following different groundwater extraction pathways and show the potential of the hydrogeological system to recover. When groundwater extraction is allowed to increase continuously, as it did over the past decades, extraction-induced subsidence has the potential to drown the Mekong delta single-handedly before the end of the...
Geomorphology, 2016
The geomorphological development of Holocene coastal plains around the world has been studied sin... more The geomorphological development of Holocene coastal plains around the world has been studied since the beginning of the twentieth century from various disciplines, resulting in large amounts of data. However, the overwhelming quantities and heterogeneous nature of this data have caused the divided knowledge to remain inconsistent and fragmented. To keep improving the understanding of coastal plain geomorphology and geology, cataloguing of data and integration of knowledge are essential. In this paper we present a GIS that incorporates the accumulated data of the Netherlands’ coastal plain and functions as a storage and integration tool for coastal plain mapped data. The GIS stores redigitised architectural elements (beach barriers, tidal channels, intertidal flats, supratidal flats, and coastal fresh water peat) from earlier mappings in separate map layers. A coupled catalogue-style database stores the dating information of these elements, besides references to source studies and annotations regarding changed insights. Using scripts, the system automatically establishes palaeogeographical maps for any chosen moment, combining the above mapping and dating information. In our approach, we strip the information to architectural element level, and we separate mapping from dating information, serving the automatic generation of time slice maps. It enables a workflow in which the maker can iteratively regenerate maps, which speeds up fine-tuning and thus the quality of palaeogeographical reconstruction. The GIS currently covers the late Holocene coastal plain development of the Netherlands. This period witnessed widespread renewed flooding along the southern North Sea coast, coinciding with large-scale reclamation and human occupation. Our GIS method is generic and can be expanded and adapted to allow faster integrated processing of growing amounts of data for many coastal areas and other large urbanising lowlands around the world. It allows maintaining actual data overview and facilitates new ways of analysis at national, regional, and local scales. © 2016 Elsevier B.V.
Environmental Research Letters, 2017
Proceedings of the International Association of Hydrological Sciences, 2015
4th International Geologica Belgica Meeting 2012. Moving Plates and Melting Icecaps – Processes a... more 4th International Geologica Belgica Meeting 2012. Moving Plates and Melting Icecaps – Processes and Forcing Factors in Geology. Brussels 11-14/09/12
In many deltas worldwide subsidence still is an underestimated problem, while the threat posed by... more In many deltas worldwide subsidence still is an underestimated problem, while the threat posed by land subsidence low-lying urbanizing and urbanized deltas exceeds the threat of sea-level rise induced by climate change. Human-induced subsidence is driven by the extraction of hydrocarbons and groundwater, drainage of phreatic groundwater, and loading by buildings and infrastructure. The consequences of subsidence are increased flood risk and flood water depth, rising groundwater levels relative to the land surface, land loss, damage to buildings and infrastructure, and salinization of ground and surface water.. The Netherlands has a long history of subsidence. Large-scale drainage of the extensive peatlands in the western and northern parts of the Netherlands started approximately 1000 years ago as a result of rapid population growth. Subsidence is still ongoing due to (1) continuous drainage of the former peatland, which is now mainly in use as agricultural land and built-up area, (...
In order to improve our insights in the sequence stratigraphic and architectural development of l... more In order to improve our insights in the sequence stratigraphic and architectural development of lower deltaic hydrocarbon reservoirs we study the Last Interglacial Rhine delta (MIS-5), and compare it to its well investigated counterpart, the Holocene (MIS-1) Rhine- Meuse delta (Berendsen & Stouthamer, 2000). The Last Interglacial record has experienced a full glacialinterglacial cycle of sea-level and climate change in a subsiding tectonic setting, and arguably is in a more relevant state of preservation when the delta is to be used as a reservoir analogue.
Quaternary Science Reviews, 2016
This paper describes the sedimentary architecture, chronostratigraphy and palaeogeography of the ... more This paper describes the sedimentary architecture, chronostratigraphy and palaeogeography of the late Middle and Late Pleistocene (Marine Isotope Stage/MIS 6-2) incised Rhine-valley fill in the central Netherlands based on six geological transects, luminescence dating, biostratigraphical data and a 3D geological model. The incised-valley fill consists of a ca. 50 m thick and 10-20 km wide sand-dominated succession and includes a well-developed sequence dating from the Last Interglacial: known as the Eemian in northwest Europe. The lower part of the valley fill contains coarse-grained fluvio-glacial and fluvial Rhine sediments that were deposited under Late Saalian (MIS 6) cold-climatic periglacial conditions and during the transition into the warm Eemian interglacial (MIS 5e-d). This unit is overlain by fine-grained fresh-water flood-basin deposits, which are transgressed by a fine-grained estuarine unit that formed during marine high-stand. This ca. 10 m thick sequence reflects gradual drowning of the Eemian interglacial fluvial Rhine system and transformation into an estuary due to relative sea-level rise. The chronological data suggests a delay in timing of regional Eemian interglacial transgression and sea-level high-stand of several thousand years, when compared to eustatic sea-level. As a result of this glacio-isostatic controlled delay, formation of the interglacial lower deltaic system took only place for a relative short period of time: progradation was therefore limited. During the cooler Weichselian Early Glacial period (MIS 5d-a) deposition of deltaic sediments continued and extensive westward progradation of the Rhine system occurred. Major parts of the Eemian and Weichselian Early Glacial deposits were eroded and buried as a result of sea-level lowering and climate cooling during the early Middle Weichselian (MIS 4-3). Near complete sedimentary preservation occurred along the margins of the incised valley allowing the detailed reconstruction presented here. © 2015 Elsevier Ltd.
Proceedings of the International Association of Hydrological Sciences, 2020
Geologie En Mijnbouw, 2002
Approximately 200,000 lithological borehole descriptions, 1200 14C dates, 36,000 dated archaeolog... more Approximately 200,000 lithological borehole descriptions, 1200 14C dates, 36,000 dated archaeological artifacts, and gradients of palaeochannels were used to reconstruct the Holocene evolution of the fluvial part of the Rhine-Meuse delta. Ages of all Holocene channel belts were stored in a Geographical Information System database that enables generation of palaeogeographic maps for any time during the Holocene. The time resolution
Proceedings of the International Association of Hydrological Sciences, 2015
ABSTRACT Wij bevelen aan in wetsvoorstel dan wel toelichting expliciet te maken dat een gestrooml... more ABSTRACT Wij bevelen aan in wetsvoorstel dan wel toelichting expliciet te maken dat een gestroomlijnde geïntegreerde internetinterface onderdeel zal zijn van de invoering van de BRO. Wij bevelen aan de ‘representatieve vertegenwoordiging afnemers’ uit Artikel 4 specifiek ook op dit uitvoeringsaspect inspraak te verlenen.
International Journal of Sediment Research, 2013
... 1. Five SN cross-sections including time lines (Gouw & Erkens, 2007 NJG) 2. History of se... more ... 1. Five SN cross-sections including time lines (Gouw & Erkens, 2007 NJG) 2. History of sediment delivery to the Holocene delta (PhD thesis Erkens) 3. Mapping and dating Rhine deposition in the Gelderse IJssel valley (Cohen) 4. Late Glacial/Holocene landscape change in the ...
Cohen, K.M., E. Stouthamer, W.Z. Hoek, M.J.P. Gouw, G. Erkens (2007) Palaeogeography of the Holoc... more Cohen, K.M., E. Stouthamer, W.Z. Hoek, M.J.P. Gouw, G. Erkens (2007) Palaeogeography of the Holocene Rhine-Meuse delta: complete stratigraphical coverage of a sizable coastal prism. 11-ième congrès Français de sédimentologie, Caen 23-25 octobre 2007, France. ASF publication 57, p. 70. Oral presentation.