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document
Verhagen, H.J. (author)
Simple design rule for artificial beach nourishment, as applied in the Netherlands.
conference paper 1992
document
Roelse, P. (author), Verhagen, H.J. (author)
In the Netherlands much land was captured from the sea. At the same time however along the coast severe losses of land occurred. The main reasons were sea level rise and effects of decreasing tidal volumes of estuaries. Besides there were the local effects of shifting tidal channels and periodical movements of the coastline. Building of groynes,...
conference paper 1991
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Stigter, C. (author), Verhagen, H.J. (author), De Vriend, H.J. (author), Van der Weijde, R.W. (author), Van Raalten, C. (author), Loxham, M. (author)
In the Netherlands today much attention is paid to the effect of coastal structures on the environment. In the past it was usual to quantify the effect of such a structure on its environment solely with the purpose of deciding whether that effect could imply any hazard to the structure itself (or to structures in the neighbourhood). Nowadays...
conference paper 1990
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Pilarczyk, K.W. (author), Verhagen, H.J. (author), Roelse, P. (author), Adriaanse, L. (author), Consemulder, J. (author)
Beoogt de instanties, bedrijven of personen, die betrokken zijn bij het beheer en onderhoud van de Nederlandse kust, die noodzakelijke kennis over zandsuppleties te verschaffen. De diverse aspecten van kustverdediging door middel van zandsuppletie komen aan de orde: achtergrondinformatie over kustprocessen en kustlijnontwikkeling,...
report 1988
document
Verhagen, H.J. (author), Maranus, J.W. (author)
Langs de Zeeuwse kust bewegen grote massa's zand van zuid naar noord. Deze zandgolven zorgen voor een cyclisch kustgedrag. Bij de besluitvorming over kustverdedigingswerken en strandsuppleties is inzicht in de kinematica van deze golven essentieel.
journal article 1987
document
Bijker, E.W. (author), Van der Leijé, J.P. (author), Pilon, J.J. (author), Svasek, J.N. (author), In 't Veld, J.K. (author), Verhagen, H.J. (author)
When longshore sediment transport is interrupted by a construction along a coast, e.g harbour moles or a dredged approach channel, the equilibrium of the coastline may be disturbed. When the disruption is caused by breakwaters, the longshore transport that is held back will cause accretion updrift of the breakwaters and erosion downdrift of them...
conference paper 1981
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