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A field experiment on the influence of the postulated global climatic change on coastal marshland soils
Author(s) -
Blume HansPeter,
MüllerThomsen Udo
Publication year - 2007
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.200521892
Subject(s) - environmental science , bioturbation , salt marsh , hydrology (agriculture) , soil water , topsoil , soil science , geology , sediment , geomorphology , oceanography , geotechnical engineering
A climatic scenario postulates an increase of atmospheric CO 2 , 55 cm water‐level rise combined with a 30 cm higher tidal amplitude for the North Sea. Further, more frequent and stronger west storms, a 2.5°C mean‐annual‐temperature increase together with 15% more rainfall during winter time are to be expected until 2050 due to recent human impact. The possible consequences of the postulated changes in temperature and flooding dynamics were studied for soil formation as well as for soil‐ecological attributes and processes of two sites at Hedwigenkoog foreshore in N Germany: a Hypersali‐tidalic Fluvisol ( protothionic, calcaric ) (1.5 m asl with >500 annual floods) and a Gleyi‐sali‐tidalic Fluvisol ( calcaric ) under a salt meadow (2.2 m asl with 70 annual floods). Temperature, water, redox, nutrient and gas dynamics were measured at different soil depths for a period of 2 y. The topsoil of the Gleyi‐sali‐tidalic Fluvisol was permanently heated over an area of 14 m 2 to simulate a temperature rise of 1.5–2.5°C. The results are discussed in relation to two realistic scenarios. If the ground level of the Gleyi‐sali‐tidalic Fluvisol is heaved up (due to sedimentation) as intensively as the sea level rises, it may be assumed that the soil unit including vegetation cover in principle will not noticeably change. Then, the temperature increase will intensify the activity of soil organisms, bioturbation, and formation of a crumb structure, however, there will be no further accumulation of soil humus. If there was no sedimentation during the next 50 y, the salt meadow itself together with the upper part of the Gleyi‐sali‐tidalic Fluvisol would be destroyed by erosion, and a Hypersali‐tidalic Fluvisol would be formed similar to the studied one.