Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

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Найдено документов в текущей БД: 3

    Weak northern and strong tropical land carbon uptake from vertical profiles of atmospheric CO(2)
[Text] / B. B. Stephens [et al.] // Science. - 2007. - Vol. 316, Is. 5832. - P1732-1735, DOI 10.1126/science.1137004. - Cited References: 32 . - 4. - ISSN 0036-8075
РУБ Multidisciplinary Sciences

Аннотация: Measurements of midday vertical atmospheric CO(2) distributions reveal annual-mean vertical CO(2) gradients that are inconsistent with atmospheric models that estimate a large transfer of terrestrial carbon from tropical to northern latitudes. The three models that most closely reproduce the observed annual-mean vertical CO(2) gradients estimate weaker northern uptake of -1.5 petagrams of carbon per year (Pg C year(-1)) and weaker tropical emission of +0.1 Pg C year(-1) compared with previous consensus estimates of -2.4 and +1.8 Pg C year(-1), respectively. This suggests that northern terrestrial uptake of industrial CO(2) emissions plays a smaller role than previously thought and that, after subtracting land-use emissions, tropical ecosystems may currently be strong sinks for CO(2).

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Держатели документа:
Natl Ctr Atmospher Res, Boulder, CO 80305 USA
Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
Natl Ocean & Atmospher Adm, Boulder, CO 80305 USA
Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
Tohoku Univ, Ctr Atmospher & Ocean Studies, Sendai, Miyagi 9808578, Japan
Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan
Nagoya Univ, Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan
Cent Aerol Observ, Dolgoprudnyi 141700, Russia
Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
Max Planck Inst Biogeochem, D-07701 Jena, Germany
Sukachev Inst Forest, Krasnoyarsk 660036, Russia
CSIRO Marine & Atmospher Res, Aspendale, Vic 3195, Australia
Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA

Доп.точки доступа:
Stephens, B.B.; Gurney, K.R.; Tans, P.P.; Sweeney, C...; Peters, W...; Bruhwiler, L...; Ciais, P...; Ramonet, M...; Bousquet, P...; Nakazawa, T...; Aoki, S...; Machida, T...; Inoue, G...; Vinnichenko, N...; Lloyd, J...; Jordan, A...; Heimann, M...; Shibistova, O...; Langenfelds, R.L.; Steele, L.P.; Francey, R.J.; Denning, A.S.

    Interactive Effects of Land Use and Climate on Soil Organic Carbon Storage in Western Siberian Steppe Soils
/ G. Guggenberger, N. Bischoff, O. Shibistova [et al.] ; ed.: M. . Fruhauf [et al.] // KULUNDA: CLIMATE SMART AGRICULTURE: SOUTH SIBERIAN AGRO-STEPPE AS : SPRINGER INTERNATIONAL PUBLISHING AG, 2020. - P183-199. - (Innovations in Landscape Research), DOI 10.1007/978-3-030-15927-6_13. - Cited References:45. - The paper is based on the results of the research work carried out in the scope of the German-Russian cooperation project KULUNDA. The project is financed by the German Federal Ministry of Education and Research (BMBF; FKZ 01LL0905I). We would like to thank all colleagues from the Russian and German partner institutions for their cooperation and support during the investigations. . -
РУБ Agricultural Economics & Policy + Green & Sustainable Science &

Аннотация: Soils store much more carbon (C) than all terrestrial plants and the Earth's atmosphere together, and the C exchange between soils and atmosphere largely influences the CO2 contents in the atmosphere. While converting native ecosystems into agricultural land in the past caused a huge historical release of C into the atmosphere, an optimization of the management of agricultural soils offers the possibility of restoring parts of the previously lost C in the soil. However, in this respect, interrelationships of land use and soil management with climate change must be considered. In this chapter, land use and climatic effects on soil organic carbon (SOC) stocks in the large western Siberian grasslands will be evaluated and scenarios of future development of SOC storage will be given. A combination of soil analysis along a climatic gradient from the forest steppe to the dry steppe and a modelling approach with the Lund-Potsdam-Jena managed Land (LPJmL) model revealed, that since their cultivation soils of the Kulunda steppe lost about 20-35% of their organic C. Surprisingly, not only particulate organic C was affected but likewise also organic C located within mineral-organic associations was lost, and the proportion of the lost C is independent from the climatic conditions. Parts of this lost organic C can be restored by abandoning arable land. However, due to political and economic constraints, this does not seem to be likely. Minimum or zero tillage may provide an option to increase the organic C storage in western Siberian steppe soils, but the potential effect may be limited. The LPJmL model simulates a continuing climate-change driven C loss from soil, which corroborates results of soil analysis along the climatic gradient. The management of SOC stock has to be evaluated also for its effect on soil erosion, water deficiency and nutrient shortage.

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Держатели документа:
Leibniz Univ Hannover, Inst Soil Sci, Herrenhauser Str 2, D-30419 Hannover, Germany.
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia.
Landesamt Bergbau Energie & Geol LBEG, Referat L3-2 Landwirtschaft, D-30655 Hannover, Germany.
Inst Klimafolgenforsch PIK, Telegraphenberg A56, D-14412 Potsdam, Germany.
Russian Acad Sci, Inst Water & Environm Problems, Siberian Branch, Molodezhnaya St 1, Barnaul 656038, Russia.
Univ Kopenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.
Martin Luther Univ Halle Wittenberg, Soil Sci & Soil Protect, Von Seckendorff Pl 3, D-06120 Halle, Germany.

Доп.точки доступа:
Guggenberger, G.; Bischoff, N.; Shibistova, O.; Muller, C.; Rolinski, S.; Puzanov, A.; Prishchepov, A. V.; Schierhorn, F.; Mikutta, R.; Fruhauf, M... \ed.\; Guggenberger, G... \ed.\; Meinel, T... \ed.\; Theesfeld, I... \ed.\; Lentz, S... \ed.\; German Federal Ministry of Education and Research (BMBF)Federal Ministry of Education & Research (BMBF) [FKZ 01LL0905I]

    Changes in Soil Organic Carbon Concentration and Stock after Forest Regeneration of Agricultural Fields in Taiwan
/ Y. H. Lin, P. C. Lee, O. V. Menyailo, C. H. Cheng // Forests. - 2021. - Vol. 12, Is. 9. - Ст. 1222, DOI 10.3390/f12091222. - Cited References:33. - This study was supported by the Ministry of Science and Technology of Taiwan, a cooperative grant from the Ministry of Science and Technology of Taiwan and the Russian Foundation for Basic Research (RFBR), and the NTU Core Consortiums. . - ISSN 1999-4907
РУБ Forestry

Аннотация: Afforestation or abandonment of agricultural fields to forest regeneration is a method of sequestering carbon to offset the increasing atmospheric concentration of CO2. We selected 11 sites with altitudes ranging from 14 to 2056 m and with paired forest regenerated and adjacent agricultural fields. Our objectives were to (1) examine the changes in soil organic carbon (SOC) concentration and stock after forest regeneration of agricultural fields and (2) identify the factors related to elevation and adjacent agricultural practices that affect the SOC accumulation rate. Our results demonstrated overall increases in both SOC concentrations and stocks after forest regeneration of the abandoned agricultural fields. The average increase rates of SOC concentrations in the forest regenerated soil samples were 1.65 and 0.95 g C kg(-1) at 0-10 and 10-20 cm depths, respectively, representing 101% and 65% increases relative to those in the soil samples from agricultural fields. The average accumulation rates of SOC stocks in the regenerated forests were 13.0 and 6.7 ton C ha(-1) at the 0-10 and 10-20 cm depths, respectively, representing 96% and 62% increases relative to those in the agricultural soil samples. The average annual sequestration rate was 1.03 Mg C ha(-1) year(-1) for the top 0-20 cm soils, which is greater than that observed by previous reviews and meta-analyses. The tropical/subtropical climate, sampling soil depth, forest regeneration period, and tree species in this study are likely to have contributed to the high average SOC accumulation levels. In addition, the SOC stock accumulation rates were higher at low-elevation sites than at middle-elevation sites, which could also be attributed to the favorable climatic conditions at the low-elevation sites. Along with the build-up of carbon sequestration in the forest floor and tree biomass, the afforestation/abandonment of agricultural fields to forest regeneration appears to be a promising carbon offset mechanism.

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Держатели документа:
Natl Taiwan Univ, Sch Forestry & Resource Conservat, Taipei 106, Taiwan.
Inst Forest Res SB RAS, Krasnoyarsk 660036, Russia.
Soil & Water Management & Crop Nutr Lab, Joint FAO IAEA Ctr Nucl Tech Food & Agr, A-2444 Seibersdorf, Austria.

Доп.точки доступа:
Lin, Yi-Han; Lee, Pei-Chen; Menyailo, Oleg, V; Cheng, Chih-Hsin; Ministry of Science and Technology of TaiwanMinistry of Science and Technology, Taiwan; Russian Foundation for Basic Research (RFBR)Russian Foundation for Basic Research (RFBR); NTU Core Consortiums