Ecological Modelling 221 (2010) 953–959
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Ecological Modelling
journal homepage: www.elsevier.com/locate/ecolmodel
Modelling dynamics of soil organic matter under different historical land-use
management techniques in European Russia
Maxim Bobrovsky
a
, Alexander Komarov
a
, Alexey Mikhailov
a,∗
, Larisa Khanina
b
a
Institute of Physico-Chemical and Biological Problems in Soil Science RAS, 2, Institutskaya ul., Pushchino 142290, Russia
b
Institute of Mathematical Problems in Biology RAS, Russia
article info
Article history:
Received 21 April 2008
Received in revised form
16 December 2009
Accepted 17 December 2009
Available online 18 January 2010
Keywords:
Soil organic matter (SOM)
Slash-and-burn system
Field-forest shifting system
Three-field crop rotation
EFIMOD
ROMUL
abstract
We have analyzed an influence of the traditional agricultural system techniques on the soil organic matter
dynamics using the model of carbon and nitrogen cycling in forest ecosystems EFIMOD linked with the
model of SOM dynamics ROMUL. Forest stands on the loamy soddy-podzolic soils (Alfisoils) located in
the Central European Russia have been taken for the case study. The following land-use management
scenarios were simulated: (a) slash-and-burn system with 3 years for crops and 120, 60 and 25 years
for forest; (b) three-field crop rotation system with organic fertilization (dung) every 3 and 9 years and
the same rotation without fertilization; and (c) short-term field-forest shifting system with 10 years for
crops and 10 and 25 years for forest. Analysis of the results showed that the frequency of agricultural
use in mixed field-forest land-use systems was crucial for soil organic matter dynamics. Under the short
interval between agriculture, the stocks of all soil organic matter pools decreased. Under all scenarios
except the three-field crop rotation with fertilization and the slash-and-burn system with 120 years for
forest, a strong reduction of soil organic matter occurred after 30–130 years of the agricultural impacts.
The highest reduction rates were modelled under the short-term field-forest shifting system and three-
field rotation without fertilization. Fertilization led to stabilization of soil organic matter pools and gave
a possibility for a long time stable agricultural use.
© 2010 Elsevier B.V. All rights reserved.
1. Introduction
Modelling of different techniques of historical land-use man-
agement can be applied in decision of a range of tasks. It allows for
the assessing levels of soil organic matter (SOM) under traditional
land-use systems, for the assessing admissible ‘lifetime’ of differ-
ent agricultural systems in different environmental conditions, for
obtaining the new data to understand ecosystems’ history, and for
the test of historical reconstructions concepts. Moreover usually
the models of global carbon cycle assume that significant anthro-
pogenic impact started in the middle of XIX century (Houghton,
2003; Denman et al., 2007). However, historical reviews show
that various intensive anthropogenic impacts were widespread
throughout Europe long before this time. Consecutive replace-
ments of agricultural systems and lands rotation (forests, arable
lands, grasslands, etc.) took place during all the early medieval time.
Periods of land’s intensive use and land abandoning (when forest
vegetation had been regenerated naturally) took turns. This led to
forest habitats changing and to essential modifications of biogeo-
∗
Corresponding author. Tel.: +7 496 7730755; fax: +7 496 7330595.
E-mail addresses: maxim.bobrovsky@gmail.com (M. Bobrovsky),
alexey.mikh@gmail.com (A. Mikhailov).
chemical cycles, first of all to modifications of carbon cycle (AGH,
1999; Song and Woodcock, 2003; Lal, 2005). In European Rus-
sia, the essential part of impacts was concerned about traditional
agriculture systems as follows: slash-and-burn system, short-term
field-forest shifting system, and three-field system. These land-
use systems defined frequency and structure of human impacts to
lands, lands rotation, etc.
The slash-and-burn system is considered to be the first agricul-
tural system in forested regions of Europe. It had been widespread
since 7000 years B.P. in South-Eastern Europe (Willis et al., 1995),
since 6000 years B.P. in Northern Europe (Eriksson et al., 2002), and
since 5000 years B.P. in Central European Russia (Krasnov, 1987). It
is a quite productive agricultural system which is effective enough
in forested regions. The ratio of planted to harvested grain in the
first few years of the slash-and-burn was within the range from
1:10–1:100 (Milov, 1998). That is why the slash-and-burn was used
in some regions of the Northern and the Eastern Europe till the
middle of 20th century (Bobrovsky, 2004). For example, in Finland
about 25% of rye crops were grown by the slash-and-burn in 1830
(Linkola, 1988).
As population density increased and forest area decreased
throughout Europe, the slash-and-burn agricultural system had
been gradually substituted by the tillage agriculture with spe-
cial draught animal implements. Tillage agriculture appeared
0304-3800/$ – see front matter © 2010 Elsevier B.V. All rights reserved.
doi:10.1016/j.ecolmodel.2009.12.013