Research paperThe influence of groundwater currents on diffusion processes in a lake bottom: an old report reviewed
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Cited by (22)
Salinity management in the coastal region of the Netherlands: A historical perspective
2015, Agricultural Water ManagementCitation Excerpt :In the Middle Ages, the inland lake gradually evolved into the Zuiderzee, which stood in open connection with the North Sea. Up to about 1600 the Zuiderzee was only slightly brackish and it is reasonable, following Volker and Van der Molen (1991), to take the year 1638 as the starting point of the salinization of the sediments of the Zuiderzee. The 1916 Zuiderzee Storm Flood led to an intensive monitoring of the salinity status of the Waterland and Anna Paulowna polders in North Holland by agricultural engineers C. Nobel and Sikke Smeding (1889–1967) (Smeding, 1919–1920, 1921; Nobel, 1921).
Chlorine stable isotope evidence for salinization processes of confined groundwater in southwestern Nobi Plain aquifer system, central Japan
2014, Journal of HydrologyCitation Excerpt :Diffusion coefficients for Cl−, DCL, in sediments varies widely from 10−12 to 10−9 m2/s in previous studies. Silty clay or sandy clay deposits have relatively high DCL (1.6–2.1 × 10−10 m2/s, till to clay, Hendry et al., 2000; 4.6 × 10−10 m2/s, fine sand to humic clayey deposits, Beekman et al., 2011; 5.7 × 10−10 m2/s, sea bottom sediments, Volker and van der Molen, 1991; 6.0 × 10−10 m2/s, silty clay till to sandy clayey silt till, Desaulniers et al., 1986; 7 × 10−10 m2/s, clay with sand, Groen et al., 2000; 1.3 × 10−9 m2/s, fresh or brackish water sediments, Eggenkamp et al., 1994). On the other hand, massive clay sediments have low DCL around 10−12 m2/s (1–5 × 10−12 m2/s, clay, Lavastre et al., 2005; 4.0–5.5 × 10−12 m2/s, clay by experimental measurement, Van Loon et al., 2003).
An integrated modelling approach to reconstruct complex solute transport mechanisms - Cl and δ37Cl in pore water of sediments from a former brackish lagoon in The Netherlands
2011, Applied GeochemistryCitation Excerpt :The EMSD (Erosion-Mixing-Sedimentation-Diffusion) model developed to include these processes synthesizes present knowledge of geology, particularly at site D, and historical information on storm surges in the area. The results imply that Volker’s hypothesis (republished by Volker and Van der Molen, 1991) for historical transport is incomplete and incorrect with respect to geological and historical data. Simulations using depth dependent diffusion coefficients which are related to porosity changes did not improve the results.
Chloride transport in a recently reclaimed Dutch polder
2002, Journal of HydrologyMeasurement of advective water velocity in lake sediment using natural helium gradients
1994, Journal of Hydrology