Effects of morphological changes on metal accumulation in a salt marsh sediment of the Skallingen peninsula, Denmark

被引:16
作者
Christiansen C. [1 ]
Bartholdy J. [1 ]
Kunzendorf H. [1 ,2 ]
机构
[1] Institute of Geography, University of Copenhagen, Copenhagen K DK-1350
[2] Gamma Dating Center, Institute of Geography, University of Copenhagen, Copenhagen K DK-1350
关键词
Dating; Metal accumulation; Morphology; Salt marsh; Sedimentation; Skallingen;
D O I
10.1023/A:1014393201487
中图分类号
学科分类号
摘要
In 1931 a red-colored, sandy marker horizon was placed on the emerging Skallingen salt marsh. Sedimentation on top of the marker horizon since then shows two opposing tendencies. Coincident with salt marsh development the sediments display up to 1964 a fining upward sequence with an increasing content of organic matter. Since 1964 a nearby creek has meandered towards the sampling plot. Consequently, the sediments become coarser with a decreasing organic matter content. The morphological induced changes in sedimentary conditions strongly influence metal content in the sediments and thereby hide anthropogenic induced concentration variations. Thus, an apparently diminishing Zn content (per kg dry weight) since 1964 could indicate lesser load to the area. However, corrected for grain size effects there is an increasing content of Zn. Other metal concentrations (e.g. Cu) show a diminishing trend when corrected for grain size effects and therefore indicate a reduced anthropogenic induced load of these metals to the salt marsh.
引用
收藏
页码:11 / 23
页数:12
相关论文
共 36 条
[1]  
Aagaard T., Nielsen N., Nielsen J., Skallingen - Origin and Evolution of a Barrier Spit, (1995)
[2]  
Ackermann F., A procedure for correcting the grain size effect in heavy metal analyses of estuarine and coastal sediments, Env. Tech. Lett., 1, pp. 518-527, (1980)
[3]  
Allen J.R.L., Salt-marsh growth and stratification: A numerical model with special reference to the Severn Estuary, southwest Britain, Marine Geol., 95, pp. 77-96, (1990)
[4]  
Ball D.F., Loss-on-ignition as an estimate of organic matter and organic carbon in non-calcareous soils, J. Soil Sci., 15, pp. 84-89, (1964)
[5]  
Bartholdy J., Anthony D., Tidal dynamics and seasonal dependent import and export of fine-grained sediment through a backbarrier tidal channel of the Danish Wadden Sea, Tidal Sedimentology, Modern and Ancient. SEPM Sp. Publ, 61, pp. 43-52, (1998)
[6]  
Bartholdy J., Madsen P.F., Accumulation of fine grained material in a Danish tidal area, Marine Geol., 67, pp. 121-137, (1985)
[7]  
Boorman L.A., Salt marshes - Present functioning and future changes, Mang. Salt Marsh., 3, pp. 227-241, (1999)
[8]  
Bricker S.B., The history of Cu, Pb, and Zn inputs to Narragansett Bay, Rhode Island as recorded by salt-marsh sediments, Estuaries, 16, pp. 589-607, (1993)
[9]  
Cacador I., Vale C., Catarino F., Accumulation of Zn, Cu, Cr and Ni in sediments between roots of the Tagus estuary salt marshes, Portugal, Est. Coast. Shelf Sci., 42, pp. 393-403, (1996)
[10]  
Christiansen C., Bartholdy J., Hansen T., Lillie S., Nielsen J., Nielsen N., Pejrup M., Salt marsh accretion during sea-level rise and an outlook on the future, Danish Studies related to Climate Change, (2001)