10.11.2014 Views

RD&D-Programme 2004 - SKB

RD&D-Programme 2004 - SKB

RD&D-Programme 2004 - SKB

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

The above work will be pursued in cooperation with the programmes for geochemistry and<br />

hydrology and is dependent on the results of the surface hydrology measurements on the sites.<br />

20.6 Terrestrial ecosystems<br />

The terrestrial ecosystems – for example forest, agricultural land and mire – are characterized<br />

by the fact that they normally have a groundwater table that always or usually lies just below the<br />

ground surface. The dominant transport processes from the groundwater up to these systems are<br />

root uptake, capillary force and the groundwater’s level fluctuations. Root uptake and accumulation<br />

in biomass are, however, the most important processes for radionuclide transport to people<br />

and other consumers. Mires and other wetlands are the special cases where the groundwater<br />

table fluctuates around the level of the ground surface during most of the year, but otherwise<br />

have properties similar to those of land types where the groundwater table is always below<br />

ground level. General soil processes will therefore be dealt with in this section, and then forest<br />

and wetlands as special cases.<br />

Forest is the dominant ecosystem for the hypothetical sitings /20-47/ and can be a possible<br />

recipient, see Figure 20-2. However, the results of studies of discharge of deep groundwater<br />

from repository depth show that few streamlines end up in the forest, see section 20.5. Most<br />

exit under streams and on the shorelines of lakes and seas, as well as in wetlands. The forest<br />

has been the focus of several projects that have studied the fallout from Chernobyl, among<br />

other things, see further /20-48/. Most studies have mainly been concerned with the short-term<br />

consequences of radionuclide transport. Few calculations have been done of the migration<br />

and accumulation of radionuclides from a deep repository in forest. An attempt was made in<br />

the Forest Working Group of Biomass /20-49/. The most important long-term processes are<br />

accumulation of nuclides in the soil profile and biological leaching processes that move nuclides<br />

to biota. The upward transport of radionuclides from the groundwater table into the roots and<br />

vegetation is also essential. The forest question is closely linked to near-surface hydrology and<br />

Tree layer<br />

Ash<br />

Asp<br />

Birch<br />

Mixed forest<br />

No tree layer (other)<br />

No tree layer (forest)<br />

Old pine<br />

Old spruce<br />

Unspec. young conifers<br />

Young birch<br />

Yoyng pine<br />

Young spruce<br />

Water<br />

0 1,000 Metre<br />

Figure 20-2. The forest in the Forsmark area after satellite image interpretation /20-47/.<br />

280 RD&D-<strong>Programme</strong> <strong>2004</strong>

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!