This paper deals with the hydrological properties of deltaic sediments. A detailed study was made of the geological history of part of the delta plain of the Rhine and Meuse. Such hydrological properties as thickness of aquifers and semi-permeable layers, transmissibility of the aquifers were determined.
|Place of Publication||Wageningen|
|Number of pages||12|
|Publication status||Published - 1961|
|Name||Nota / Instituut voor Cultuurtechniek en Waterhuishouding|
- south-west netherlands