Extent and significance of water repellency in dunes along the Dutch coast

Citation
Lw. Dekker et al., Extent and significance of water repellency in dunes along the Dutch coast, J HYDROL, 231, 2000, pp. 112-125
Citations number
35
Categorie Soggetti
Environment/Ecology,"Civil Engineering
Journal title
JOURNAL OF HYDROLOGY
ISSN journal
00221694 → ACNP
Volume
231
Year of publication
2000
Pages
112 - 125
Database
ISI
SICI code
0022-1694(20000529)231:<112:EASOWR>2.0.ZU;2-R
Abstract
Depth, degree and spatial variability of water repellency were examined in the surface layers of dune sands along the coast of the Netherlands. Soil s amples were collected at six depths of up to 50 cm at 865 dune sand sites i n nature reserves. The potential water repellency was measured on dried sam ples using the water drop penetration time (WDPT) test. The vegetation at t he sires consisted of marram grass, buckthorn, grey hair grass, pine, oak, other grasses and heather. The 5190 samples were dried at the laboratory, a fter which the potential water repellency was measured using the WDPT test. About 60-70% of the samples taken at several depths in the young dunes wit h a sparse vegetation of marram grass were wettable, whereas the other samp les were slightly to strongly water repellent. The samples taken at a depth of 0-5 cm in the surface layer at the sites with different vegetations wer e all strongly to extremely water repellent. At all of these sites, the sev erity of water repellency decreased with depth. The decrease was most evide nt at the grey hair grass sites. No significant differences in severity of water repellency were found between the samples taken under a cover of buck thorn, pine and oak, any of the grasses and heather. The large variability over short distances in the water repellency and water content of the soil in the dune sands is shown by the intensive sampling of soil blocks at the Ouddorp, Westduinen, Schoorl and Zwanenwater sites. Drier as well as wetter soil areas were visualized in contour pints of the soil water content dist ributions in transects from the blocks. Large differences in wetting capaci ty between samples taken at several depths at the Ouddorp site were assesse d by measurements of the wetting rate. in all cases, wetter samples wetted faster than their drier counterparts. (C) 2000 Elsevier Science B.V, All ri ghts reserved.