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  • 11
    Book
    Book
    Saltmarshes : morphodynamics, conservation and engineering significance (1992)
    Cambridge [u.a.] : Cambridge Univ. Press
    Details Availability
    Keywords: Salt marshes ; Konferenzschrift 1991 ; Seemarsch ; Dynamische Geomorphologie ; Seemarsch ; Naturschutz ; Seemarsch ; Technik ; Seemarsch ; Seemarsch
    Type of Medium: Book
    Pages: VIII, 184 S. , Ill., graph. Darst., Kt.
    Edition: 1. publ.
    ISBN: 0521418410
    URL: https://external.dandelon.com/download/attachments/dandelon/ids/DE00445C45174A465CE2CC125779800291C78.pdf
    DDC: 574.52636
    RVK:
    RB 10295
    Language: English
    Note: Literaturangaben
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  • 12
    Book
    Book
    Sediment transport and depositional processes (1994)
    Oxford [u.a.] : Blackwell Scientific Publications
    Details Availability
    Keywords: sediment transport ; Aufsatzsammlung ; Sedimenttransport ; Sedimenttransport ; Sedimentation
    Type of Medium: Book
    Pages: IX, 397 S , zahlr. Ill., graph. Darst , 25 cm
    Edition: 1. publ.
    ISBN: 0632031123
    URL: http://www.gbv.de/dms/bowker/toc/9780632031122.pdf
    DDC: 551.3
    RVK:
    RB 10121
    RVK:
    RB 10351
    Language: English
    Note: Includes bibliographical references and index
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  • 13
    Book
    Book
    Aeolian sediments : ancient and modern (1993)
    Oxford [u.a.] : Blackwell Scientific Publications
    Details Availability
    Keywords: Wind erosion ; wind erosion ; Konferenzschrift 1990 ; Konferenzschrift ; Aufsatzsammlung ; Äolische Sedimentation ; Äolisches Sediment ; Düne ; Sedimentologie ; Äolische Sedimentation ; Äolisches Sediment ; Düne ; Sedimentologie ; Äolisches Sediment
    Type of Medium: Book
    Pages: VIII, 167 S. , Ill., graph. Darst., Kt.
    ISBN: 0632035447
    Series Statement: Special publication of the International Association of Sedimentologists 16
    URL: http://digitale-objekte.hbz-nrw.de/webclient/DeliveryManager?pid=2698232&custom_att_2=simple_viewer
    DDC: 551.37
    RVK:
    TH 2500
    Language: English
    Note: Includes bibliographical references and index
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  • 14
    Electronic Resource
    Electronic Resource
    GRANNY: A PACKAGE FOR PROCESSING GRAIN SIZE AND SHAPE DATA (1989)
    Oxford, UK : Blackwell Publishing Ltd
    Terra nova 1 (1989), S. 0 
    Details
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3121.1989.tb00436.x
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  • 15
    Electronic Resource
    Electronic Resource
    Sedimentology, stratigraphy and landscape evolution of a Holocene coastal dune system, Lodbjerg, NW Jutland, Denmark (2001)
    Oxford UK : Blackwell Science Ltd
    Sedimentology 48 (2001), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The stratigraphy and landscape evolution of the Lodbjerg coastal dune system record the interplay of environmental and cultural changes since the Late Neolithic. The modern dunefield forms part of a 40 km long belt of dunes and aeolian sand-plains that stretches along the west coast of Thy, NW Jutland. The dunefield, which is now stabilized, forms the upper part of a 15–30 m thick aeolian succession. The aeolian deposits drape a glacial landscape or Middle Holocene lake sediments. The aeolian deposits were studied in coastal cliff exposures and their large-scale stratigraphy was examined by ground-penetrating radar mapping. The contact between the aeolian and underlying sediments is a well-developed peaty palaeosol, the top of which yields dates between 2300 BC and 600 BC. Four main aeolian units are distinguished, but there is some lateral stratigraphic variation in relation to underlying topography. The three lower aeolian units are separated by peaty palaeosols and primarily developed as 1–4 m thick sand-plain deposits; these are interpreted as trailing edge deposits of parabolic dunes that moved inland episodically. Local occurrence of large-scale cross-stratification may record the head section of a migrating parabolic dune. The upper unit is dominated by large-scale cross-stratification of various types and records cliff-top dune deposition. The nature of the aeolian succession indicates that the aeolian landscape was characterized by alternating phases of activity and stabilization. Most sand transported inland was apparently preserved. Combined evidence from luminescence dating of aeolian sand and radiocarbon dating of palaeosols indicates that phases of aeolian sand movement were initiated at about 2200 BC, 700 BC and AD 1100. Episodes of inland sand movement were apparently initiated during marked climate shifts towards cooler, wetter and more stormy conditions; these episodes are thought to record increased coastal erosion and strong-wind reworking of beach and foredune sediments. The intensity, duration and areal importance of these sand-drift events increased with time, probably reflecting the increasing anthropogenic pressure on the landscape. The formation of the cliff-top dunes after AD 1800 records the modern retreat of the coastal cliffs.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.2001.00345.x
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  • 16
    Electronic Resource
    Electronic Resource
    Drainage and Elevation as Factors in the Restoration of Salt Marsh in Britain (2002)
    Boston, MA, USA : Blackwell Science Inc
    Restoration ecology 10 (2002), S. 0 
    Details
    ISSN: 1526-100X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Intertidal restoration through realignment of flood defenses has become an important component of the U.K. coastal and estuarine management strategy. Although experimentation with recent deliberate breaches is in progress, the long-term prognosis for salt marsh restoration can be investigated at a number of sites around Essex, southeast England where salt marshes have been reactivated (unmanaged restoration) by storm events over past centuries. These historically reactivated marshes possess higher creek densities than their natural marsh counterparts. Both geomorphology and sedimentology determine the hydrology of natural and restored salt marshes. Elevation relative to the tidal frame is known to be the primary determinant of vegetation colonization and succession. Yet vegetation surveys and geotechnical analysis at a natural marsh, where areas with good drainage exist in close proximity to areas of locally hindered drainage at the same elevation, revealed a significant inverse relationship between water saturation in the root zone and the abundance of Atriplex portulacoides, normally the physiognomic dominant on upper salt marsh in the region. Elsewhere in Essex natural and restored marshes are typified by very high sediment water contents, and this is reflected in low abundance of A. portulacoides. After a century of reestablishment no significant difference could be discerned between the vegetation composition of the storm-reactivated marshes and their natural marsh counterparts. We conclude that vegetation composition may be restored within a century of dike breaching, but this vegetation does not provide a reliable indicator of ecological functions related to creek structure.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1526-100X.2002.t01-1-02036.x
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  • 17
    Electronic Resource
    Electronic Resource
    Reduction of Fe(III) in sediments by sulphate-reducing bacteria (1993)
    [s.l.] : Nature Publishing Group
    Nature 361 (1993), S. 436-438 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Nodular concretions of intimately mixed siderite and FeS are growing within sulphide-rich, Recent, salt-marsh sediments on the coast of Norfolk, UK5. The host mud around the concretions contain FeS but little siderite. Although modelled growth rates6 for carbonate concretions imply that formation ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/361436a0
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