Estimating the thickness of unconsolidated coastal aquifers along the global coastline

Knowledge of aquifer thickness is crucial for setting up numerical groundwater flow models to support groundwater resource management and control. Fresh groundwater reserves in coastal aquifers are particularly under threat of salinization and depletion as a result of climate change, sea-level rise, and excessive groundwater withdrawal under urbanization. To correctly assess the possible impacts of these pressures we need better information about subsurface conditions in coastal zones. Here, we propose a method that combines available global datasets to estimate, along the global coastline, the aquifer thickness in areas formed by unconsolidated sediments. To validate our final estimation results, we collected both borehole and literature data. Additionally, we performed a numerical modelling study to evaluate the effects of varying aquifer thickness and geological complexity on simulated saltwater intrusion. The results show that our aquifer thickness estimates can indeed be used for regional-scale groundwater flow modelling but that for local assessments additional geological information should be included. The final dataset has been made publicly available (https://doi.pangaea.de/10.1594/PANGAEA.880771).</p

Sustainability of fresh groundwater resources in fifteen major deltas around the world

Population growth, urbanization and intensification of irrigated agriculture in the world’s deltas boost the demand for fresh water, with extensive groundwater extraction as a result. This, in turn, leads to salt water intrusion and upconing, which poses a threat to freshwater and food security. Managing fresh groundwater resources in deltas requires accurate knowledge about the current status and behaviour of their fresh groundwater resources. However, this knowledge is scarcely present, especially for groundwater at larger depths. Here, we use three-dimensional variable-density groundwater model simulations over the last 125 ka to estimate the volume of fresh groundwater resources for 15 major deltas around the world. We estimate current volumes of onshore fresh groundwater resources for individual deltas to vary between 1010 m3 and 1012 m3. Offshore, the estimated volumes of fresh groundwater are generally smaller, though with a considerably higher variability. In 9 out of 15 simulated deltas, fresh groundwater volumes developed over thousands of years. Based on current groundwater extraction and recharge rates, we estimate the time until in-situ fresh groundwater resources are completely exhausted, partly leading to groundwater level decline and mostly replacement with river water or saline groundwater. This straightforward analysis shows that 4 out of 15 deltas risk complete exhaustion of fresh groundwater resources within 300 m depth in 200 years. These deltas also suffer from saline surface water which means their groundwater resources will progressively salinize. With a fourfold increase in extraction rates, seven deltas risk a complete exhaustion within 200 years. Of these seven deltas, six suffer from saline surface water. We stress that the groundwater of these six vulnerable deltas should be carefully managed, to avoid non-renewable groundwater use. The progressive exhaustion of fresh groundwater resources in these deltas will hamper their ability to withstand periods of water scarcity

Shallow rainwater lenses in deltaic areas with saline seepage

In deltaic areas with saline seepage, freshwater availability is often limited to shallow rainwater lenses lying on top of saline groundwater. Here we describe the characteristics and spatial variability of such lenses in areas with saline seepage and the mechanisms that control their occurrence and size. Our findings are based on different types of field measurements and detailed numerical groundwater models applied in the south-western delta of the Netherlands. By combining the applied techniques we could extrapolate measurements at point scale (groundwater sampling, temperature and electrical soil conductivity (TEC)-probe measurements, electrical cone penetration tests (ECPT)) to field scale (continuous vertical electrical soundings (CVES), electromagnetic survey with EM31), and even to regional scale using helicopter-borne electromagnetic measurements (HEM). The measurements show a gradual mixing zone between infiltrating fresh rainwater and upward flowing saline groundwater. The mixing zone is best characterized by the depth of the centre of the mixing zone &lt;i&gt;D&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt;, where the salinity is half that of seepage water, and the bottom of the mixing zone &lt;i&gt;B&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt;, with a salinity equal to that of the seepage water (Cl-conc. 10 to 16 g l&lt;sup&gt;−1&lt;/sup&gt;). &lt;i&gt;D&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt; is found at very shallow depth in the confining top layer, on average at 1.7 m below ground level (b.g.l.), while &lt;i&gt;B&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt; lies about 2.5 m b.g.l. The model results show that the constantly alternating upward and downward flow at low velocities in the confining layer is the main mechanism of mixing between rainwater and saline seepage and determines the position and extent of the mixing zone (&lt;i&gt;D&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt; and &lt;i&gt;B&lt;/i&gt;&lt;sub&gt;mix&lt;/sub&gt;). Recharge, seepage flux, and drainage depth are the controlling factors

Opties voor een klimaatbestendige zoetwatervoorziening in Laag Nederland, tussentijds integratierapport

Dit rapport geeft een tussentijds overzicht van ‘state of the art’ kennis uit lopend onderzoek van het consortium ‘Climate Proof Fresh Water Supply’ (CPFWS) dat in het kader van het onderzoeksprogramma Kennis voor Klimaat wordt uitgevoerd. De focus van dit onderzoek naar een klimaatbestendige zoetwatervoorziening ligt op lokale en regionale oplossingen in Laag Nederland voor land- en tuinbouw en natuur. De zoetwatervoorziening van dit gebied wordt naast droogte vooral bedreigd door verzilting van grond- en oppervlaktewater. In zes samenhangende werkpakketten wordt geanalyseerd hoe dit gebied meer zelfvoorzienend kan worden én hoe aanpassingen in het (hoofd)watersysteem kunnen bijdragen aan de watervoorziening van het gebied. Centraal in de aanpak zijn een 3-tal casestudies in de Hotspots Haaglanden, Rotterdam Regio en Zuidwestelijke delta

Integraal waterbeheer : kritische zone en onzekerheden : integraal hoofdrapport

In het kader van het Nationaal Modellen- en Datacentrum (NMDC) is in 2011 het NMDC innovatieproject 'Integraal waterbeheer - van kritische zone tot kritische onzekerheden' gestart (www.nmdc.eu). Dit project heeft tot doel om de modellen voor bodem, water, vegetatie en klimaat(verandering) door samenwerking beter op elkaar aan te laten sluiten, daarbij beter geschikt te maken om effecten van klimaatverandering te berekenen en om de verschillende typen onzekerheden bij dit soort studies in beeld te brengen. Het project is uitgevoerd door Alterra, Deltares, KNMI, PBL en TNO. In twee cases (Baakse Beek en Walcheren) hebben zij hun state-of-the-art modellen voor meteo, gewasgroei, vegetatie-ontwikkeling, hydrologie en geologie ingezet en aan elkaar gekoppeld. Dit rapport behandelt integraal de resultaten van het innovatieproject. De resultaten van de case voor de Baakse Beek zijn specifiek opgenomen in een NMDC deelrapport (Van Ek et al., 2012). Voor de case Walcheren wordt verwezen naar een artikel in voorbereiding (Kroes, J. et al., 2013). De resultaten bieden nieuwe inzichten in de vocht- en zouthuishouding van de bodem, potenties voor grondwaterafhankelijke natuur en groei van landbouwgewassen in het huidige klimaat en projecties voor klimaatverandering rond 2050. In het project zijn verschillende methoden toegepast om inzicht te krijgen in verschillende onzekerheden, hetgeen voor dergelijke integrale (model)studies praktische aanknopingspunten biedt voor de analyse van onzekerheden en effectieve samenwerking tussen de instituten

Balancing supply and demand of fresh water under increasing drought and salinisation in the Netherlands

The latest climate impact assessments show that climate change will cause an increasing mismatch between demand and supply of fresh water in many densely populated deltas around the world. Recent studies for the Netherlands show that the current water supply strategy is not climate proof in the long-run. Therefore, a future ‘climate proof’ fresh water supply is national priority on the Dutch water policy agend

HIV infection and HERV expression: a review

The human genome contains multiple copies of retrovirus genomes known as endogenous retroviruses (ERVs) that have entered the germ-line at some point in evolution. Several of these proviruses have retained (partial) coding capacity, so that a number of viral proteins or even virus particles are expressed under various conditions. Human ERVs (HERVs) belong to the beta-, gamma-, or spuma- retrovirus groups. Endogenous delta- and lenti- viruses are notably absent in humans, although endogenous lentivirus genomes have been found in lower primates. Exogenous retroviruses that currently form a health threat to humans intriguingly belong to those absent groups. The best studied of the two infectious human retroviruses is the lentivirus human immunodeficiency virus (HIV) which has an overwhelming influence on its host by infecting cells of the immune system. One HIV-induced change is the induction of HERV transcription, often leading to induced HERV protein expression. This review will discuss the potential HIV-HERV interactions