• Authors:
    • Kurganova,I.
    • Lopes de Gerenyu,V.
    • Kuzyakov,Y.
  • Source: Catena; ScienceDirect
  • Volume: 122
  • Year: 2015
  • Summary: Most land use changes (LUC) significantly affect the amount of carbon (C) sequestered in vegetation and soil, thereby, shifting the C balance in ecosystems. Disintegration of the USSR and the followed collapse of collective farming system have led to abandonment of more than 58millionha (Mha) of former croplands in Russia and Kazakhstan that comprise together about 90% of land area in the former USSR. This was the most widespread and abrupt LUC in the 20th century in the northern hemisphere. The spontaneous withdrawal of croplands in 1990s caused several benefits for environment including substantial C sequestration in post-agrogenic ecosystems. The new estimations of net ecosystem production (NEP) and changes in soil organic carbon stocks ({increment}SOC) in post-agrogenic ecosystems presented here are based on the uniform bio-climatic approach, and hereby, allow to update C balance of the former USSR. The total extra C sink in abandoned croplands in Russia (45.5Mha) and Kazakhstan (12.9Mha) is estimated to be 155±27MtCyr-1 and 31±2MtCyr-1, respectively. This additional C sink could cover about 18% of the global CO2 release due to deforestation and other land use changes or compensate annually about 36% and 49% of the current fossil fuel emissions in Russia and Kazakhstan, respectively. The extra C sink to the post-agrogenic ecosystems in Russia and Kazakhstan contributes possibly about 1/3 part to the total current C balance of the former USSR. Hence, the disintegration of the former USSR significantly affected national and global C budget over few decades after LUC. © 2015 Elsevier B.V.
  • Authors:
    • Kurganova,I.
    • Gerenyu,V. L. de
    • Kuzyakov,Y.
  • Source: Research Articles
  • Volume: 133
  • Year: 2015
  • Summary: Most land use changes (LUC) significantly affect the amount of carbon (C) sequestered in vegetation and soil, thereby, shifting the C balance in ecosystems. Disintegration of the USSR and the followed collapse of collective farming system have led to abandonment of more than 58 million ha (Mha) of former croplands in Russia and Kazakhstan that comprise together about 90% of land area in the former USSR. This was the most widespread and abrupt LUC in the 20th century in the northern hemisphere. The spontaneous withdrawal of croplands in 1990s caused several benefits for environment including substantial C sequestration in post-agrogenic ecosystems. The new estimations of net ecosystem production (NEP) and changes in soil organic carbon stocks (Delta SOC) in post-agrogenic ecosystems presented here are based on the uniform bio-climatic approach, and hereby, allow to update C balance of the former USSR. The total extra C sink in abandoned croplands in Russia (45.5 Mha) and Kazakhstan (12.9 Mha) is estimated to be 15527 Mt C yr -1 and 312 Mt C yr -1, respectively. This additional C sink could cover about 18% of the global CO 2 release due to deforestation and other land use changes or compensate annually about 36% and 49% of the current fossil fuel emissions in Russia and Kazakhstan, respectively. The extra C sink to the post-agrogenic ecosystems in Russia and Kazakhstan contributes possibly about 1/3 part to the total current C balance of the former USSR. Hence, the disintegration of the former USSR significantly affected national and global C budget over few decades after LUC.
  • Authors:
    • Meshalkina,J.
    • Yaroslavtsev,A.
    • Mazirov,I.
    • Samardzic,M.
    • Valentini,R.
    • Vasenev,I.
  • Source: Eurasian Journal of Soil Science
  • Volume: 4
  • Issue: 3
  • Year: 2015
  • Summary: The eddy covariance (EC) technique as a powerful statistics-based method of measurement and calculation the vertical turbulent fluxes of greenhouses gases within atmospheric boundary layers provides the continuous, long-term flux information integrated at the ecosystem scale. An attractive way to compare the agricultural practices influences on GHG fluxes is to divide a crop area into subplots managed in different ways. The research has been carried out in the Precision Farming Experimental Field of the Russian Timiryazev State Agricultural University (RTSAU, Moscow) in 2013 under the support of RF Government grant # 11.G34.31.0079, EU grant # 603542 LUC4C (7FP) and RF Ministry of education and science grant # 14-120-14-4266-ScSh. Arable Umbric Albeluvisols have around 1% of SOC, 5.4 pH (KCl) and NPK medium-enhanced contents in sandy loam topsoil. The CO 2 flux seasonal monitoring has been done by two eddy covariance stations located at the distance of 108 m. The LI-COR instrumental equipment was the same for the both stations. The stations differ only by current crop version: barley or vetch and oats. At both sites, diurnal patterns of NEE among different months were very similar in shape but varied slightly in amplitude. NEE values were about zero during spring time. CO 2 fluxes have been intensified after crop emerging from values of 3 to 7 mol/s.m 2 for emission, and from 5 to 20 mol/s.m 2 for sink. Stabilization of the fluxes has come at achieving plants height of 10-12 cm. Average NEE was negative only in June and July. Maximum uptake was observed in June with average values about 8 mol CO 2 m -2 s -1. Although different kind of crops were planted on the fields A and B, GPP dynamics was quite similar for both sites: after reaching the peak values at the mid of June, GPP decreased from 4 to 0.5 g C CO 2 m -2 d -1 at the end of July. The difference in crops harvesting time that was equal two weeks did not significantly influence the daily GPP patterns. Cumulative assimilation of CO 2 at the end of the growing season was about 150 g C m -2 for both sites. So the difference in NEE was the consequence of essentially higher respiration rates in case of vetch and oats (about 350 g C m -2) comparing to barley (250 g C m -2) that needs additional research. The results have shown high daily and seasonal dynamic of CO 2 emission too as a result of different and contrasted conditions: crop type, crop development stage, soil moisture and air temperature. Obtained unique for Russian agriculture data are useful for land-use practices environmental assessment, for soil organic carbon dynamics analysis and agroecological evaluation.
  • Authors:
    • Regina, K.
    • Palosuo, T.
    • de Gerenyu, V. L.
    • Kurganova, I.
    • Heikkinen, J.
  • Source: Nutrient Cycling in Agroecosystems
  • Volume: 98
  • Issue: 1
  • Year: 2014
  • Summary: The collapse of Soviet Union in early 1990s led to abandonment of large area of arable land which is assumed to act as a carbon (C) sink. We studied the ability of two dynamic soil C models (Yasso07 and RothC) to predict changes in soil C content after cropland abandonment. The performance of the models was compared using the results of a long-term experiment in Pushchino, Moscow region (54A degrees 50'N, 37A degrees 35'E) in Russia. The experiment was divided in four combinations of fertilizer or mowing treatments on former cropland soil. The soil C content was determined in the year of establishment (1980) and thereafter in 1999 and 2004. The soil C stocks increased by about 1.5- to 1.8-fold during the study period. Both models predicted the overall change in soil C relatively well (modelling efficiency of Yasso07 and RothC were 0.60 and 0.73, respectively). According to the models, the soil gained on average 140-150 g C m(-2) year(-1) during the first 5 years after conversion of cropland to grassland. The C sequestration rate decreased to 40-50 g C m(-2) year(-1) after 20 years of land use change. The sequestration rates estimated in this study are comparable to the rates observed in other studies.
  • Authors:
    • Lopes de Gerenyu, V.
    • Kurganova, I.
    • Six, J.
    • Kuzyakov, Y.
  • Source: Global Change Biology
  • Volume: 20
  • Issue: 3
  • Year: 2014
  • Summary: The collapse of collective farming in Russia after 1990 and the subsequent economic crisis led to the abandonment of more than 45 million ha of arable lands (23% of the agricultural area). This was the most widespread and abrupt land use change in the 20th century in the northern hemisphere. The withdrawal of land area from cultivation led to several benefits including carbon (C) sequestration. Here, we provide a geographically complete and spatially detailed analysis of C sequestered in these abandoned lands. The average C accumulation rate in the upper 20 cm of mineral soil was 0.960.08 Mg C ha -1 yr -1 for the first 20 years after abandonment and 0.190.10 Mg C ha -1 yr -1 during the next 30 years of postagrogenic evolution and natural vegetation establishment. The amount of C sequestered over the period 1990-2009 accounts to 42.63.8 Tg C per year. This C sequestration rate is equivalent to ca. 10% of the annual C sink in all Russian forests. Furthermore, it compensates all fire and postfire CO 2 emissions in Russia and covers about 4% of the global CO 2 release due to deforestation and other land use changes. Our assessment shows a significant mitigation of increasing atmospheric CO 2 by prolonged C accumulation in Russian soils caused by collective farming collapse.
  • Authors:
    • Mahanta, S. K.
    • Ghosh, P. K.
  • Source: Invited Article
  • Volume: 35
  • Issue: 2
  • Year: 2014
  • Summary: Globally soils contain around twice the amount of carbon in the atmosphere and thrice in vegetation. Therefore, soil is both 'a source and a sink' for greenhouse gases and balance between the functions is very delicate. The gases move continuously from one pool to another maintaining balance in different pools of the ecosystem. Appropriate management of soil offers to the potential to provide solutions for each of the challenges related to food security and climate change. The estimated carbon sequestration potential of world soils lies between 0.4 to 1.2 Gt per year which includes 0.01-0.30 Gt per year from grasslands. Carbon sequestration can be enhanced in grasslands through grazing management, sowing favorable forage species, fertilizer application and irrigation, restoration of degraded grasslands etc. However, there are certain limitations that hinder in adopting the practices for enhancing carbon sequestration in grasslands. The limitations include continuous degradation of grasslands, changing climate, paucity of information on carbon stock of grasslands from developing countries, disagreement on systems for documenting carbon stock changes over a period of time, hindrance in policy implementations etc.
  • Authors:
    • Siegfried, W.
    • Rohr, C.
    • Riemann, D.
    • Retso, D.
    • Pribyl, K.
    • Nordl, O.
    • Litzenburger, L.
    • Limanowka, D.
    • Labbe, T.
    • Kotyza, O.
    • Kiss, A.
    • Himmelsbach, I.
    • Glaser, R.
    • Dobrovolny, P.
    • Contino, A.
    • Camenisch, C.
    • Burmeister, K.
    • Brazdil, R.
    • Bieber, U.
    • Barriendos, M.
    • Alcoforado, M.
    • Luterbacher, J.
    • Gruenewald, U.
    • Herget, J.
    • Seneviratne, S.
    • Wagner, S.
    • Zorita, E.
    • Werner, J.
    • Pfister, C.
    • Wetter, O.
    • Soderberg, J.
    • Spring, J.
  • Source: Climatic Change
  • Volume: 125
  • Issue: 3-4
  • Year: 2014
  • Summary: The heat waves of 2003 in Western Europe and 2010 in Russia, commonly labelled as rare climatic anomalies outside of previous experience, are often taken as harbingers of more frequent extremes in the global warming-influenced future. However, a recent reconstruction of spring-summer temperatures for WE resulted in the likelihood of significantly higher temperatures in 1540. In order to check the plausibility of this result we investigated the severity of the 1540 drought by putting forward the argument of the known soil desiccation-temperature feedback. Based on more than 300 first-hand documentary weather report sources originating from an area of 2 to 3 million km(2), we show that Europe was affected by an unprecedented 11-month-long Megadrought. The estimated number of precipitation days and precipitation amount for Central and Western Europe in 1540 is significantly lower than the 100-year minima of the instrumental measurement period for spring, summer and autumn. This result is supported by independent documentary evidence about extremely low river flows and Europe-wide wild-, forest- and settlement fires. We found that an event of this severity cannot be simulated by state-of-the-art climate models.
  • Authors:
    • Polyanskaya, N.
    • Suslov, S.
    • Kuchin, N.
  • Source: Ekonomika Sel'skokhozyaistvennykh i Pererabatyvayushchikh Predpriyatii
  • Issue: 3
  • Year: 2012
  • Summary: In 2009, production of leguminous and cereal grain crops in Russia's Nizhny Novgorod Oblast' totalled 1 432 400 tonnes, and the average crop yield was 2.44 tonnes/ha - the highest yield in 50 years. However extremely hot and dry weather conditions in 2010 caused a sharp reduction in harvest volumes, so that Nizhny Novgorod Oblast' had a total harvest of just 541 500 tonnes and an average crop yield of 1.36 tonnes/ha. 2010 harvest figures for the region were significantly lower than in 2006, when the total harvest volume was 1 169 900 tonnes and the average crop yield 2.05 tonnes/ha. Crop yields in Nizhny Novgorod Oblast' vary significantly between years, with yields being highly dependent on climate conditions. The greatest variation in yields occurs with maize, millet, and buckwheat crops. Strong variation in yields is also evident for wheat and leguminous crops, and moderate variation occurs in yields of rye, barley, and oats. For agricultural enterprises, the most significant factor influencing their production volumes and incomes is the structure of crops produced. The structure of crops produced in Nizhny Novgorod Oblast' has changed significantly since the pre-reform period, with a marked shift towards cultivation of food grade cereal grains, and away from production of feed crops. In 2010, wheat accounted for 56.8% of the region's total harvest, barley 21.9%, oats 10.7%, rye 7.6%, legumes 2.5%, triticale 0.4%, and groats crops 0.1%. Agricultural organizations continue to be the main cereal grain producers, despite increases in land areas used for cereal grain cultivation by private (peasant) farmers. In 2010, agricultural enterprises accounted for 92.2% of cereal grain production. Individual secondary farms account for only an insignificant proportion of grain crop production. Problems faced by enterprises operating in the region's cereal grain segment include a poor technical base, low rates of fertiliser application, and difficulties in securing suitably qualified workers. Approximately 80% of machines used by these enterprises have been in use for longer than their intended operating life. These problems have adverse effects on the efficiency of harvesting operations and on crop yields. It is important to address these issues if higher and more stable production volumes are to be achieved, and the profitability of crop production activities improved.
  • Authors:
    • Inubushi, K.
    • Kawahigashi, M.
    • Funakawa, S.
    • Ivanov, I.
    • Manakhov, D.
    • Zdanovich, G.
    • Manakhova, E.
    • Prikhodko, V.
    • Okitsu, S.
    • Matsushima, M.
    • Sugihara, S.
    • Nagano, H.
  • Source: Soil Science & Plant Nutrition
  • Volume: 58
  • Issue: 2
  • Year: 2012
  • Summary: The effects of different land-use histories on contents of soil carbon (C) and nitrogen (N) and fluxes of greenhouse gases [carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)] measured using the closed chamber method were investigated in the Arkaim museum reserve located in the South Ural of Russia. A natural forest site (NF) and two grassland sites that had different land-use histories (CL: cropland until 1991; PST: pasture until 1991; both sites have been fallow for 18 years) were selected for soil sampling and gas flux measurements. The vegetation in NF was mainly Betula pendula Roth. with steppe cherry and grassy cover. Perennial grasses (Stipa spp., Festuca spp. and others) have been planted in CL and PST since 1991 to establish reserve mode, and the projective cover of these plants were > 90% in both sites in 2009. Soil samples were taken from the A horizon in the three sites, and additionally samples of the O horizon were taken from NF. The contents of soil C and N [total C, total N, soluble organic C, soluble N and microbial biomass C (MBC)] in the O horizon of NF were the largest among all investigated soils (p 0.05). Our current research indicated that, in soils of the Eurasian steppe zone of Russia, total C, total N and MBC were affected not only by current land-use (i.e., fallow grassland vs. natural forest) but also by past (until 18 years ago) land-use.
  • Authors:
    • Shabalina, E. V.
    • Korobitsyn, S. L.
    • Platunov, A. A.
  • Source: Kormoproizvodstvo
  • Issue: 1
  • Year: 2011
  • Summary: Productivity and fodder value of perennial legume and legume-grass mixtures under cover of vetch-oat mixture were studied in 2009-2010 in Kirov Region, Russia. Cover mixture consisted of spring vetch cv. Orlovskaya 4 and oat cv. Ulov with sowing rate of 0.12 and 0.06 t/ha, respectively. Red clover cv. Kirovskii 159, birds-foot trefoil cv. Solnyshko and cooksfoot cv. Khlynovskaya were used as undercrop mixture in following combinations: (1) red clover, (2) red clover + birds-foot trefoil, (3) birds-foot trefoil, (4) red clover + cooksfoot, (5) red clover + birds-foot trefoil + cooksfoot. Data on dry mass yield and number of fodder units per kg of dry mass for cover mixture and unvercover crops, as well as crude protein and cellulose content for unvercover crops are summarized in 2 tables. Productivity of cover mixture and unvercover crops varied from 3.81 to 4.18 t/ha, and from 3.86 and to 4.80 t/ha respectively with no significant difference between variants. The highest crude protein content of 17.2% was achieved in variant (3), but again with no significant difference between variants. Authors concluded that further work will be needed to achieve the high and balanced yield of cover and unvercover crops.