Self-restoration of post-agrogenic sandy soils in the southern Taiga of Russia: Soil development, nutrient status, and carbon dynamics

Kalinina, Olga; Goryachkin, S. V.; Karavaeva, N. A.; Lyuri, D.I.; Najdenko, L.; Giani, Luise

doi:10.1016/j.geoderma.2009.05.014

Cited by 71 publications

(50 citation statements)

References 27 publications

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“…Obtained results show that the vegetation type can overrule other forming factors given by altitude (such as temperature or precipitation gradient) that are responsible for soil development. The same conclusion was drawn by Berger et al When we consider the timescale of spruce plantation in the area, it has been long enough for Podzol development (Mokma et al 2003;Zanelli et al 2007;Kalinina et al 2009). The timescale, which is represented by two centuries of spruce monoculture planting (Vacek et al 2008), provided enough time for the full development of Haplic Podzols.…”

Section: Distribution Of Soil Unitssupporting

confidence: 77%

“…Significant morphologic changes of the soil profile can be observed within a relatively short period. Significant changes in the soil chemistry and morphology that indicate the podzolization process can be observed already after a few tens or hundreds of years (Olsson & Melkerud 1989;Mokma et al 2003;Zanelli et al 2007;Dlouhá et al 2009;Kalinina et al 2009). …”

Section: Anthropically Induced Changes Of Soil Formation Processmentioning

confidence: 99%

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Soil toposequence under man-planted vegetation in the Krkonoše Mts., Czech Republic

Penížek

Zádorová

2012

Soil & Water Res.

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Abstract:Mountainous areas represent regions with specific soil cover pattern that is naturally given by an altitudinal gradient. The objective of our study was to describe the soil cover development on the altitudinal gradient under changed environment given by man-planted vegetation and acidification. The studied area is characterized by spruce monoculture planting that replaced the original broadleaf natural vegetation and high load of anthropic acidification. The common hypothesis considering the sequence of Dystric Cambisol-Entic Podzol-Haplic Podzol with increasing altitude was not proved. The results of our study indicate that the influence of spruce vegetation causes the occurrence of Haplic Podzols at low altitudes where the natural soil formation does not induce their development. Results showed that the vegetation type can overrule other altitude-related soil-forming factors. The conversion of natural broadleaf and mixed forests to spruce monocultures leads to the expansion of podzolization process to lower altitudes.

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Section: Distribution Of Soil Unitssupporting

confidence: 77%

Section: Anthropically Induced Changes Of Soil Formation Processmentioning

confidence: 99%

Soil toposequence under man-planted vegetation in the Krkonoše Mts., Czech Republic

Penížek

Zádorová

2012

Soil & Water Res.

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“…Several processes have contributed to the decline of Arctic sea ice cover, but the role of these processes needs better quantification (Smedsrud et al, 2013;Vihma et al, 2014). Further studies are needed on the impacts of changes in cloud cover and radiative forcing (Kay et al, 2008), atmospheric heat transport (Kapsch et al, 2013) and oceanic heat transport (Döscher et al, 2014). In addition, as the ice thickness has decreased, the sea ice cover becomes increasingly sensitive to the icealbedo feedback .…”

Section: The Arctic Ocean In the Climate Systemmentioning

confidence: 99%

“…According to recent estimates, the total area of abandoned agricultural land in Russia in the 1990s to 2010s is at about 57 million ha, of which 18 million ha have been restored by forests and 6 million ha of this are located in Asian Russia . As a result, these areas have become active accumulators of atmospheric CO 2 (Kalinina et al, 2009). These new forests (substituting resources) could form the basis for sustainable development in these regions, in case relevant management programs for the forests re-established on abandoned lands are going to be implemented.…”

Section: Social System -State-of-the-art and Future Research Needs 2mentioning

confidence: 99%

Pan-Eurasian Experiment (PEEX): towards a holistic understanding of the feedbacks and interactions in the land–atmosphere–ocean–society continuum in the northern Eurasian region

et al. 2016

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Abstract. The northern Eurasian regions and Arctic Ocean will very likely undergo substantial changes during the next decades. The Arctic-boreal natural environments play a crucial role in the global climate via albedo change, carbon sources and sinks as well as atmospheric aerosol production from biogenic volatile organic compounds. Furthermore, it is expected that global trade activities, demographic movement, and use of natural resources will be increasing in the Arctic regions. There is a need for a novel research approach, which not only identifies and tackles the relevant multi-disciplinary research questions, but also is able to make a holistic system analysis of the expected feedbacks. In this paper, we introduce the research agenda of the Pan-Eurasian Experiment (PEEX), a multi-scale, multi-disciplinary and international program started in 2012 (https://www.atm.helsinki.fi/peex/). PEEX sets a research approach by which large-scale research topics are investigated from a system perspective and which aims to fill the key gaps in our understanding of the feedbacks and interactions between the land-atmosphereaquatic-society continuum in the northern Eurasian region. We introduce here the state of the art for the key topics in the PEEX research agenda and present the future prospects of the research, which we see relevant in this context.

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“…Chronosequence approaches have been used frequently to investigate changes in vegetation and soil properties during secondary succession after land-use abandonment (Zak et al 1990;Hooker and Compton 2003;van der Waal et al 2006;Allison et al 2007;Kalinina et al 2009;Baer et al 2002;Kalinina et al 2011). The basic idea of this approach is to substitute space for time and to study a range of sites that constitute a timeline of successional states (Bardgett et al 2005;Walker et al 2010).…”

Section: Introductionmentioning

confidence: 99%

Dynamics of soil carbon, nitrogen, and phosphorus in calcareous soils after land-use abandonment – A chronosequence study

et al. 2015

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Aims The objective of this study was to investigate changes in soil total organic C (TOC), total nitrogen (TN), phosphorus (P) fractions, and microbial community structure during secondary succession after abandonment of vineyards on calcareous soils. Methods Two chronosequences covering 200 years and differing in aspect and slope were established in Hungary, and the upper 10 cm of the mineral soils were studied. Results We found strong increases in TOC concentrations after land-use abandonment, especially at the south-exposed sites. The TOC/TN ratio increased by a factor of 1.3 in the south-west exposed chronosequence and by a factor of 1.6 in south exposed chronosequence. The concentration of labile P (NaHCO 3 -extractable P) diminished during the first 50 years after land-use abandonment, leading to low P availability at the later stages of the succession. The total organic P (TOP) concentration increased during the first 40 years after abandonment. At the later stages of succession, TOP concentrations decreased again, while the ratio of TOC/TOP increased continuously over 200 years. The ratio of arbuscular-mycorrhizal-fungi-to-bacteria (AMF/bacteria) increased strongly during the first decade after abandonment of the vineyards. Conclusions Our study indicates that impacts of former cultivation on secondary ecosystems persisted for more than a century, and that especially P concentrations showed long lasting legacy effects.

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Self-restoration of post-agrogenic sandy soils in the southern Taiga of Russia: Soil development, nutrient status, and carbon dynamics

Cited by 71 publications

References 27 publications

Soil toposequence under man-planted vegetation in the Krkonoše Mts., Czech Republic

Soil toposequence under man-planted vegetation in the Krkonoše Mts., Czech Republic

Pan-Eurasian Experiment (PEEX): towards a holistic understanding of the feedbacks and interactions in the land–atmosphere–ocean–society continuum in the northern Eurasian region

Dynamics of soil carbon, nitrogen, and phosphorus in calcareous soils after land-use abandonment – A chronosequence study

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