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pro vyhledávání: '"J.S. Schoonees"'
Akademický článek
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Publikováno v:
Coastal Engineering. 53:1045-1058
The south-western shoreline along the entrance channel inside the Port of Richards Bay has experienced continued erosion. Four groynes were constructed to stabilise the shoreline. Monitoring of shoreline evolution provided valuable data on the accret
Autor:
J.S. Schoonees
Publikováno v:
Coastal Engineering. 40:141-160
The annual variation in the net longshore sediment transport rates at three South African and at one North African site is investigated. The net rates at these sites, given in the first table, show large variations. It was found that measurements of
Autor:
J.S. Schoonees, A.K. Theron
Publikováno v:
Coastal Engineering. 25:1-41
Cross-shore sediment transport models are used to model beach profile changes in order to determine, for example, coastal set-back lines, behaviour of beach fill and beach profile variations adjacent to coastal structures. A study was undertaken to e
Autor:
J.S. Schoonees, A.K. Theron
Publikováno v:
Coastal Engineering. 19:1-25
A literature search was undertaken to collect field data on longshore sediment transport. This yielded a large number of data sets (273 points for bulk transport rates) from a variety of sites around the world. Data are especially lacking for transpo
Publikováno v:
Coastal Engineering 2004.
Publikováno v:
Coastal Structures 2003.
This study involved the design of beach diamond mining between Alexander Bay Harbor and the mouth of the Orange River on the west coast of South Africa. To mine this area entailed creating artificial sand beaches overlying rocky areas. Numerical mode
Publikováno v:
Coastal Engineering 2002.
Autor:
J.S. Schoonees, J.P. Moller
Publikováno v:
Coastal Engineering 1982.
False Bay is situated near Cape Town in the Republic of South Africa. The National Research Institute for Oceanology (NRIO) of the Council for Scientific and Industrial Research (CSIR) was commissioned to undertake studies on a recreational scheme in
Akademický článek
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