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Titlebook: Umwelt Wirtschafts Forum; Institut für Umweltwirtschaftsanalysen Book 1992 Springer-Verlag Berlin Heidelberg 1992 Forum.Umwelt.Wirtschaft

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21#
發(fā)表于 2025-3-25 07:11:26 | 只看該作者
22#
發(fā)表于 2025-3-25 11:16:57 | 只看該作者
Institut für Umweltwirtschaftsanalysenese landscapes extend from the Andes adjacent areas to the political border with Peru and Colombia to the east and northeast, respectively. This is a unique region which has been shaped by the arrangement of the geological structures and the climatic change that the region has suffered over geologic
23#
發(fā)表于 2025-3-25 13:41:16 | 只看該作者
24#
發(fā)表于 2025-3-25 17:30:03 | 只看該作者
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發(fā)表于 2025-3-25 20:45:25 | 只看該作者
26#
發(fā)表于 2025-3-26 02:20:02 | 只看該作者
Michael Rohrgiving a wide-ranging insight into Icelandic nature in general. It gives a short overview of Icelandic climate and land use with special consideration to the volcanic geology, which is the single most important factor in determining soil formation on this island: the formation of Andosols. The book
27#
發(fā)表于 2025-3-26 08:07:09 | 只看該作者
28#
發(fā)表于 2025-3-26 08:50:56 | 只看該作者
Horst Wolfl and tectonics in the geoform of structural origin. Geomorphology plays an important role in soil formation through relief, surface morphodynamics, morphoclimatic context, weathering and time (age). The geological zones and their related geomorphic features are dealt with as related to soil distrib
29#
發(fā)表于 2025-3-26 16:03:10 | 只看該作者
Stefan Maiertic Strategy on Soils (2006) identified seven ‘environmental, economic, social and cultural functions’. In research studies from Ireland, these ecosystem services have been rearranged into the following five main soil functions for agricultural land (1) primary production, (2) water purification and
30#
發(fā)表于 2025-3-26 18:57:53 | 只看該作者
Rudolf J. Lauffnd evolution. In the western and central part of the Alpine region, crystalline rocks prevail over sedimentary ones (mainly limestone and dolostone), which are widespread in the eastern part. Leptosols, Cambisols, Podzols, Chernozems and Phaeozems form the main soilscapes in these mountain areas. Se
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