Dynamics of carbon balance components in fallow arable lands on the Valdai Upland (original) (raw)
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Soil organic carbon is an essential part of soil and a valuable natural resource. Due to land use change SOC stocks are usually altered, which can seriously affect the environment and the ecosystem. The objective of this study was to investigate effects of different land use regimes (cropland, meadow and forest) and different soil types (Fluvisols, Chernozems, Vertisols and Solonetz) on SOC stocks. The results imply that soil type was the principal factor affecting SOC stocks. Topsoil SOC stocks (0-30 cm) decreased in the following order: Vertisols (93 t ha-1) > Chernozems (68 t ha-1) > Solonetz (65 t ha-1) > Fluvisols (48 t ha-1). The conversion of native ecosystems (forests and meadows) to croplands induced a significant SOC stock decrease and a considerable degradation of soil. Forests contain 72 t ha-1 of SOC, meadows 71 t ha-1 and cropland 62 t ha-1. The highest historical loss of SOC stock due to the conversion of native ecosystems was obtained in Chernozems (16-18%),...
Soil Science and Plant Nutrition, 2012
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Agriculture (Pol'nohospodárstvo), 2013
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Annual cycling of soil organic carbon (SOC) is the main driving force in the formation and functioning of soil cover. Therefore knowledge about it forms the scientific base for sustainable management and ecologically sound soil protection. Systematized parameters of the mean annual cycling of SOC by soils are analysed on the basis of the SOC stock densities (Mg ha -1 ) of 16 mineral soil groups. The SOC stocks according to soil groups for the soil cover (solum) as a whole and for their epipedon were calculated on the basis of mean SOC densities and their distribution area of soil types. In the Estonian mineral soil cover (32 351 km 2 ) a total of 323 ± 46 Tg (10 12 g) SOC is retained; 42% of this is sequestered into stabilized humus, 40% into unstable raw humus, and 18% into forest (grassland) floor and shallow peat layers. Of the total SOC stock, 75% is situated in biologically active epipedons and 25% in subsoil. The annual SOC inputs and outputs in natural soils, which were calculated on the basis of annual productivity, ranged from 0.2 to 3.6 Mg ha -1 yr -1 . The influence of land management peculiarities on the annual cycling and balance of SOC has been demonstrated by our own experimental research, as well as by data published in the literature. In this work the pedo-ecological causal regularities of SOC sequestration in mineral soil cover (SOC concentration, soil thickness, moisture regime, texture, carbonate content), and agro-technological possibilities for its regulation (crops and their rotation, level of subsidization and soil amelioration) are discussed.
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