Landscape Modelling and Decision Support by Wilfried Mirschel & Vitaly V. Terleev & Karl-Otto Wenkel

Author:Wilfried Mirschel & Vitaly V. Terleev & Karl-Otto Wenkel
Language: eng
Format: epub
ISBN: 9783030374211
Publisher: Springer International Publishing

aSC—soil cover, HC—humus cover, and SS—subsoil

On the basis of forest lands, SC total SOC amounts the SOC stock densities (Mg ha−1) for the different SSG were calculated (Fig. 13.8). It is important also to mention that these mean SOC sequestration capacities were calculated as mean weighted by the area in relation to whole SC and separately to mineral and peat soils. By the scenario I (Table 13.5) in the Estonian forest land SC totally 367 Tg of SOC is sequestrated, whereas 66.2% of it is located in the HC and 33.8% in SS. From the total SOC amounts, 55.0% is located in SC of mineral soils and 45.0% in peat soils.

Fig. 13.8Different soil species’ SOC superficial densities (Mg ha−1) per soil cover or solum. The mean density level for all soils, and separately for organic and mineral soils is given on the figure by horizontal lines. For soil names by their codes see Table 13.2

Download

Copyright Disclaimer:
This site does not store any files on its server. We only index and link to content provided by other sites. Please contact the content providers to delete copyright contents if any and email us, we'll remove relevant links or contents immediately.