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

w10=
Найдено документов в текущей БД: 16

    Influence of drying of the samples on the transformation of nitrogen and carbon compounds in mountain-meadow alpine soils
/ M. I. Makarov [et al.] // Eurasian Soil Sci. - 2013. - Vol. 46, Is. 7. - P778-787, DOI 10.1134/S1064229313070053. - Cited References: 32. - This study was supported by the Russian Foundation for Basic Research (project no. 10-04-00780). . - 10. - ISSN 1064-2293
РУБ Soil Science

Аннотация: The drying of samples of mountain-meadow soils characterized by their permanently high moisture under natural conditions fundamentally changes the concentrations of the labile nitrogen and carbon compounds, as well as the patterns of their microbial transformation. When the soil samples are dried, a four- to fivefold increase in the content of the extractable organic nitrogen compounds, carbon compounds, and inorganic nitrogen compounds is observed, while the content of nitrogen and carbon of the microbial biomass decreases by two-three times. The rewetting of the dried soil launches the process of the replenishment of the nitrogen and carbon reserves in the microbial biomass. However, even after two weeks of incubation, their values were 1.5-2 times lower than the initial values typical of the natural soil. The restoration of the microbial community in the samples of the previously dried soils occurs in the absence of a deficiency of labile organic compounds and is accompanied by their active mineralization and the low uptake of ammonium nitrogen by the microorganisms.

Полный текст,
WOS,
Scopus

Держатели документа:
Makarov, M. I.
Mulyukova, O. S.
Malysheva, T. I.] Moscow MV Lomonosov State Univ, Fac Soil Sci, Moscow 119992, Russia
[Menyailo, O. V.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forestry, Krasnoyarsk, Russia

Доп.точки доступа:
Makarov, M.I.; Mulyukova, O.S.; Malysheva, T.I.; Menyailo, O.V.

    Solubility of the Labile Forms of Soil Carbon and Nitrogen in K2SO4 of Different Concentrations
/ M. I. Makarov [et al.] // Eurasian Soil Sci. - 2013. - Vol. 46, Is. 4. - P369-374, DOI 10.1134/S1064229313040091. - Cited References: 33. - This study was supported by the Russian Foundation for Basic Research (project no. 10-04-00780). . - 6. - ISSN 1064-2293
РУБ Soil Science

Аннотация: The general pattern of the changes in the solubility of the labile carbon and nitrogen compounds with the changes in the concentration of the salt extractant (0.05 and 0.5 M K2SO4) has been determined for soils differing in their acidity and in their contents of organic matter and nitrogen. Different forms of extracted compounds react differently to changes in the salt concentration. The solubility of inorganic nitrogen compounds (and) does not depend on the concentration of K2SO4. In most cases, the carbon and nitrogen of the microbial biomass manifest a tendency for increasing extractability with an increase in the concentration of the K2SO4 solution. A fundamental difference is characteristic of the organic carbon and nitrogen compounds, the solubility of which in 0.5 M K2SO4 increases in different soils by 1.5-3.9 times in comparison with their solubility in 0.05 M K2SO4.

Полный текст,
WOS,
Scopus

Держатели документа:
[Makarov, M. I.
Shuleva, M. S.
Malysheva, T. I.] Moscow MV Lomonosov State Univ, Fac Soil Sci, Moscow 119991, Russia
[Menyailo, O. V.] Russian Acad Sci, Sukachev Forest Inst, Siberian Branch, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Makarov, M.I.; Shuleva, M.S.; Malysheva, T.I.; Menyailo, O.V.

    Uses of tree saps in northern and eastern parts of Europe
/ I. . Svanberg [et al.] // Acta Soc. Bot. Pol. - 2012. - Vol. 81, Is. 4. - P343-357, DOI 10.5586/asbp.2012.036. - Cited References: 176 . - 15. - ISSN 0001-6977
РУБ Plant Sciences

Аннотация: In this article we review the use of tree saps in northern and eastern Europe. Published accounts by travellers, ethnologists and ethnobotanists were searched for historical and contemporary details. Field observations made by the authors have also been used. The presented data shows that the use of tree sap has occurred in most north and eastern European countries. It can be assumed that tree saps were most used where there were extensive stands of birch or maple trees, as these two genera generally produce the largest amount of sap. The taxa most commonly used have been Betula pendula, B. pubescens, and Acer platanoides, but scattered data on the use of several other taxa are presented. Tree sap was used as a fresh drink, but also as an ingredient in food and beverages. It was also fermented to make light alcoholic products like ale and wine. Other folk uses of tree saps vary from supplementary nutrition in the form of sugar, minerals and vitamins, to cosmetic applications for skin and hair and folk medicinal use. Russia, Ukraine, Belarus, Estonia, Latvia and Lithuania are the only countries where the gathering and use of sap (mainly birch sap) has remained an important activity until recently, due to the existence of large birch forests, low population density and the incorporation of sap into the former Soviet economic system. It is evident that gathering sap from birch and other trees was more widespread in earlier times. There are records indicating extensive use of tree saps from Scandinavia, Poland, Slovakia and Romania, but it is primarily of a historical character. The extraction of tree sap in these countries is nowadays viewed as a curiosity carried out only by a few individuals. However, tree saps have been regaining popularity in urban settings through niche trading.

WOS,
Scopus

Держатели документа:
[Soukand, Renata] Estonian Literary Museum, EE-51003 Tartu, Estonia
[Svanberg, Ingvar] Uppsala Univ, Uppsala Ctr Russian & Eurasian Studies, S-75120 Uppsala, Sweden
[Luczaj, Lukasz] Univ Rzeszow, Dept Bot & Biotechnol Econ Plants, PL-36100 Kolbuszowa, Poland
[Kalle, Raivo] Estonian Univ Life Sci, Inst Vet Med & Anim Sci, EE-51014 Tartu, Estonia
[Zyryanova, Olga] Russian Acad Sci, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Denes, Andrea] Janus Pannonius Museum, Nat Hist Dept, H-7601 Pecs, Hungary
[Papp, Nora] Univ Pecs, Dept Pharmacognosy, H-7624 Pecs, Hungary
[Nedelcheva, Aneli] Sofia Univ St Kliment Ohridski, Dept Bot, Sofia 1164, Bulgaria
[Seskauskaite, Daiva] Kaunas Forestry & Environm Engn Univ Appl Sci, LT-53101 Kaunas, Lithuania
[Kolodziejska-Degorska, Iwona] Warsaw Univ Bot Garden, PL-00478 Warsaw, Poland
[Kolodziejska-Degorska, Iwona] Univ Warsaw, Inst Interdisciplinary Res Artes Liberales, PL-00046 Warsaw, Poland
[Kolosova, Valeria] Russian Acad Sci, Inst Linguist Studies, St Petersburg 199053, Russia

Доп.точки доступа:
Svanberg, I...; Soukand, R...; Luczaj, L...; Kalle, R...; Zyryanova, O...; Denes, A...; Papp, N...; Nedelcheva, A...; Seskauskaite, D...; Kolodziejska-Degorska, I...; Kolosova, V...

    Extraction of the climatic signal for moisture from tree-ring chronologies of Altai-Sayan mountain forest-steppes
[Text] / V. N. Magda [et al.] // Contemp. Probl. Ecol. - 2011. - Vol. 4, Is. 7. - P716-724, DOI 10.1134/S1995425511070034. - Cited References: 20 . - 9. - ISSN 1995-4255
РУБ Ecology

Кл.слова (ненормированные):
tree-ring chronologies -- climate reconstruction -- Altai-Sayan region

Аннотация: Studies in Central Asia (Altai-Sayan region, northwest and central Mongolia) have shown that trees growing in arid conditions of mountain forest-steppes have a mixed and unstable climatic response. It is obvious that this nature of the climatic response of trees prevents the use of tree-ring chronologies for climate reconstruction. In this connection, it is necessary to separate the climatic signal of tree-ring chronologies, i.e., extract the signal for moisture. This paper proposes a method for separating the climatic signal of tree-ring chronologies of mountain forest-steppes, and reports estimates of its reliability by two independent methods. Analysis of the chronologies obtained after separation of the signal, based on meteorological and hydrological data, has shown that these chronologies can be used for climate reconstructions.

Полный текст,
Scopus,
WOS

Держатели документа:
[Magda, V. N.
Oidupaa, O. Ch.
Vaganov, E. A.] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Block, J.] Friedrich Alexander Univ Erlangen Nuernberg, Inst Geog, Erlangen, Germany

Доп.точки доступа:
Magda, V.N.; Block, J...; Oidupaa, O.C.; Vaganov, E.A.

    Influence of climatypes of Scots pine on certain chemical and microbiological characteristics of soils
[Text] / N. B. Naumova [et al.] // Contemp. Probl. Ecol. - 2009. - Vol. 2, Is. 2. - P147-151, DOI 10.1134/S1995425509020106. - Cited References: 20. - The work was carried out with the financial support of the Integration projects of SB RAS no. 5.23 and no. 24, as well as the project "Biogeochemical Cycles in the Natural and Man-Made Landscape, Their Biospheric and Regional Meaning and Regulation," reg. no. 0120.0 406322. . - 5. - ISSN 1995-4255
РУБ Ecology

Аннотация: By using multivariate statistical analysis, the influence of Scots pine climatypes on a set of chemical and microbiological properties of soil, i.e., soil C/N, C(mic)/C(org), and C(mic)/N(mic), was revealed in a series of long-term (ca. 30 years) field experiments, which were carried out according to the same scheme under contrasting environmental and soil conditions of Siberian forestries.

Полный текст,
WOS,
Scopus

Держатели документа:
[Naumova, N. B.
Makarikova, R. P.] Russian Acad Sci, Siberian Branch, Inst Soil Sci & Agrochem, Novosibirsk 630099, Russia
[Tarakanov, V. V.] Russian Acad Sci, Siberian Branch, W Siberian Affiliat Sukachev Inst Forest, Novosibirsk 630082, Russia
[Kuz'mina, N. A.
Novikova, T. N.
Milyutin, L. I.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Naumova, N.B.; Makarikova, R.P.; Tarakanov, V.V.; Kuz'mina, N.A.; Novikova, T.N.; Milyutin, L.I.; SB RAS [5.23, 24]

    C-13 and N-15 natural abundance of the soil microbial biomass
[Text] / P. . Dijkstra [et al.] // Soil Biol. Biochem. - 2006. - Vol. 38: Annual Meeting of the American-Geophysical-Union (DEC 13-17, 2004, San Francisco, CA), Is. 11. - P3257-3266, DOI 10.1016/j.soilbio.2006.04.005. - Cited References: 61 . - 10. - ISSN 0038-0717
РУБ Soil Science

Аннотация: Stable isotope analysis is a powerful tool in the study of soil organic matter formation. It is often observed that more decomposed soil organic matter is C-13, and especially N-15-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was N-15-enriched relative to the total (3.2 parts per thousand) and extractable N pools (3.7 parts per thousand), and C-13-enriched relative to the extractable C pool (2.5 parts per thousand). The microbial biomass was also C-13-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 parts per thousand), but C-13-depleted for soils with a C4 signature (-1.1 parts per thousand). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation. (c) 2006 Elsevier Ltd. All rights reserved.

Полный текст,
WOS

Держатели документа:
No Arizona Univ, Dept Biol Sci, Flagstaff, AZ 86011 USA
No Arizona Univ, Colorado Plateau Stable Isotope Lab, Flagstaff, AZ 86011 USA
No Arizona Univ, Sch Forestry, Flagstaff, AZ 86011 USA
No Arizona Univ, Merriam Powell Ctr Environm Res, Flagstaff, AZ 86011 USA
RAS, SB, Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Dijkstra, P...; Ishizu, A...; Doucett, R...; Hart, S.C.; Schwartz, E...; Menyailo, O.V.; Hungate, B.A.

    VORTEX FORMATION DURING TETHERED FLIGHT OF FUNCTIONALLY AND MORPHOLOGICALLY 2-WINGED INSECTS, INCLUDING EVOLUTIONARY CONSIDERATIONS ON INSECT FLIGHT
[Text] / D. L. GRODNITSKY, P. P. MOROZOV // J. Exp. Biol. - 1993. - Vol. 182. - P11-40. - Cited References: 59 . - 30. - ISSN 0022-0949
РУБ Biology

Аннотация: Tethered flight of six insect species (two pentatomid bugs, a moth, a butterfly, a muscid fly and a crane fly) was studied using several modifications of a dust flow visualization procedure. The spatial structure of the near vortex wake of flying specimens was reconstructed on the basis of two-dimensional flow pictures. The dynamics of the wake was followed during a stroke cycle, revealing interspecific differences in vortex formation. It is suggested that insects create a single vortex ring during each stroke. Therefore, the hypothesis of double vortex chains advanced by Brodsky is not verified. The same is true of the jet hypothesis of Bocharova-Messner. While pronating at the top of their trajectory, the flapping wings throw air masses off their lower surfaces, but there is not a jet from between their upper sides. Flow separation from leading edges was found to be a rare phenomenon, taking place irregularly during the stroke cycle. That is why, contrary to widespread theoretical expectations, the Weis-Foch fling mechanism is not likely to contain a leading edge separation bubble, which must follow stalling at the front part of the wings. It is suggested that flying animals possess special mechanisms for extracting energy back from the near vortex wake. Some hypothetical adaptations for such an extraction in insects are put forward. Possible pathways for the evolution of insect flight are described.


Доп.точки доступа:
GRODNITSKY, D.L.; MOROZOV, P.P.

    Effect of K2SO4 concentration on extractability and isotope signature (C-13 and N-15) of soil C and N fractions
[Text] / M. I. Makarov [et al.] // Eur. J. Soil Sci. - 2015. - Vol. 66, Is. 3. - P417-426, DOI 10.1111/ejss.12243. - Cited References:35. - This work was sponsored by the Russian Foundation for Basic Research (13-04-01090) and the Netherlands Organization for Scientific Research (NWO grants 047.011.2004.005, 047.017.010 and 047.018.003). . - ISSN 1351-0754. - ISSN 1365-2389
РУБ Soil Science

Аннотация: Determination of the labile soil carbon (C) and nitrogen (N) fractions and measurement of their isotopic signatures (C-13 and N-15) has been used widely for characterizing soil C and N transformations. However, methodological questions and comparison of results of different authors have not been fully solved. We studied concentrations and C-13 and N-15 of salt-extractable organic carbon (SEOC), inorganic (N-NH4+ and N-NO3-) and organic nitrogen (SEON) and salt-extractable microbial C (SEMC) and N (SEMN) in 0.05 and 0.5mK(2)SO(4) extracts from a range of soils in Russia. Despite differences in acidity, organic matter and N content and C and N availability in the studied soils, we found consistent patterns of effects of K2SO4 concentration on C and N extractability. Organic C and N were extracted 1.6-5.5 times more effectively with 0.5mK(2)SO(4) than with 0.05mK(2)SO(4). Extra SEOC extractability with greater K2SO4 concentrations did not depend on soil properties within a wide range of pH and organic matter concentrations, but the effect was more pronounced in the most acidic and organic-rich mountain Umbrisols. Extractable microbial C was not affected by K2SO4 concentrations, while SEMN was greater when extracted with 0.5mK(2)SO(4). We demonstrate that the C-13 and N-15 values of extractable non-microbial and microbial C and N are not affected by K2SO4 concentrations, but use of a small concentration of extract (0.05mK(2)SO(4)) gives more consistent isotopic results than a larger concentration (0.5m).

WOS

Держатели документа:
Moscow MV Lomonosov State Univ, Soil Sci Dept, Moscow 119991, Russia
Inst Forest SB RAS, Dept Biogeochem, Krasnoyarsk 660036, Russia
Vrije Univ Amsterdam, Dept Ecol Sci, Fac Earth & Life Sci, Syst Ecol, NL-1081 HV Amsterdam, Netherlands

Доп.точки доступа:
Makarov, M.I.; Malysheva, T.I.; Menyailo, O.V.; Soudzilovskaia, N.A.; Van Logtestijn, R. S. P.; Cornelissen, J. H. C.; Russian Foundation for Basic Research [13-04-01090]; Netherlands Organization for Scientific Research (NWO) [047.011.2004.005, 047.017.010, 047.018.003]

    The effect of mechanical impact of high energy on the structural properties of brown coal and the reactivity for liquefaction
/ P. N. Kuznetsov [et al.] // ARPN J. Eng. Appl. Sci. - 2015. - Vol. 10, Is. 16. - P6980-6987 . - ISSN 1819-6608

Кл.слова (ненормированные):
brown coal -- Extraction -- Mechanical activation -- Supramolecular structure -- Swelling -- The hydrogenation liquefaction

Аннотация: The effect of preliminary mechanical activation in the energy-intensive mill-activator on the structural and chemical transformations of brown coals and their reactivity in contact with solvents has been established. Mechanical treatment of the brown coals from Kansk-Achinsk Basin was performed in a high-energy AGO-2 centrifugal planetary ball mill. Mechanical activation led to a partial destruction of the supramolecular structure of coal, reduction of the crosslinking degree of nano-sized polyaromatic clusters in the organic matter coal. This results in the increased reactivity of coal in the liquefaction processes (extraction and hydrogenation) to form liquid products. © 2006-2015 Asian Research Publishing Network (ARPN).

Scopus,
Полный текст

Держатели документа:
Institute of Chemistry and Chemical Technology SB RAS Akademgorodok, Krasnoyarsk, Russian Federation
Siberian Federal University Svobodny Ave., Krasnoyarsk, Russian Federation

Доп.точки доступа:
Kuznetsov, P. N.; Kuznetsova, L. I.; Kazbanova, A. V.; Buryukin, F. A.

    Determination of carbon and nitrogen in microbial biomass of southern-Taiga soils by different methods
/ M. I. Makarov [et al.] // Eurasian Soil Sci. - 2016. - Vol. 49, Is. 6. - P685-695, DOI 10.1134/S1064229316060053 . - ISSN 1064-2293

Кл.слова (ненормированные):
fumigation-extraction -- rehydration -- substrate-induced respiration

Аннотация: The results of methods for determining microbial biomass carbon vary in reproducibility among soils. The fumigation-extraction and substrate-induced respiration methods give similar results for Albic Luvisol and Gleyic Fluvisol, while the results of the rehydration method are reliably higher. In Histic Fluvisol, relatively similar results are obtained using the fumigation-extraction and rehydration methods, and the substrate-induced respiration method gives almost halved results. The seasonal dynamics of microbial biomass carbon also varies depending on the method used. The highest difference is typical for the warm period, when the concentrations found by the extraction and substrate-induced methods poorly agree between two out of three soils studied. The concentration of microbial biomass nitrogen is less sensitive to the analytical method: the differences between the results of the fumigation-extraction and rehydration methods are statistically insignificant in the all soils. To reveal stable relationships between the results of determining microbial carbon and the soil properties and analytical method, a large diversity of soils should be studied. This will allow for proposing of conversion factors for the recalculation of the obtained values to the concentrations of carbon and nitrogen in microbial biomass for different soils (or soil groups) and, hence, the more correct comparison of the results obtained by different methods. © 2016, Pleiades Publishing, Ltd.

Scopus,
Смотреть статью,
WOS

Держатели документа:
Faculty of Soil Science, Moscow State University, Moscow, Russian Federation
Sukachev Institute of Forest, Siberian Branch, Russian Academy of Sciences, Akademgorodok, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Makarov, M. I.; Malysheva, T. I.; Maslov, M. N.; Kuznetsova, E. Y.; Menyailo, O. V.

    Effect of the storage conditions of soil samples on carbon and nitrogen extractability
/ M. I. Makarov [et al.] // Eurasian Soil Sci. - 2017. - Vol. 50, Is. 5. - P549-558, DOI 10.1134/S1064229317030085 . - ISSN 1064-2293

Кл.слова (ненормированные):
carbon -- drying -- extraction -- freezing -- incubation -- nitrogen -- concentration (composition) -- extraction method -- freezing -- soil carbon -- soil nitrogen -- soil organic matter -- water content

Аннотация: Concentrations of carbon and nitrogen extractable by 0.05 M K2SO4 (Cext and Next, respectively) in 14 soils of different ecosystems vary from 16 to 205 and from 4 to 53 mg/kg, respectively. The portion of Cext in soil organic matter is 0.06 to 0.38% of total carbon, and the portion of Next is 0.12–1.05% of total nitrogen. The storage of samples and their preparation to analysis differently affect the extractability of elements. The concentration of Cext is less variable than the concentration of Next. An increase in C extractability (by 1.4–6.7 times) is a common feature of all soils under drying; at the following incubation of dried soils, the extractability of C decreases by 28–56%. The extractability of N increases not only under drying (by 1.5–7.1 times) and the following incubation of samples (by 25–60% to 2–3 times), but also under freezing of most soils and at the incubation of fresh and defrozen samples. A close direct correlation is observed between the initial water content of soil and the relative increase in C extractability under drying and N extractability under freezing and drying. © 2017, Pleiades Publishing, Ltd.

Scopus,
Смотреть статью,
WOS

Держатели документа:
Lomonosov Moscow State University, Moscow, Russian Federation
Sukachev Institute of Forest Research, Russian Academy of Sciences, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Makarov, M. I.; Kuznetsova, E. Y.; Malysheva, T. I.; Maslov, M. N.; Menyailo, O. V.

    Notes towards an optimal sampling strategy in dendrockimatology
/ A. V. Kirdyanov [et al.] // Dendrochronologia. - 2018. - Vol. 52. - P162-166, DOI 10.1016/j.dendro.2018.10.002 . - ISSN 1125-7865

Кл.слова (ненормированные):
Climate signal -- Disc samples -- Increment cores -- Locally absent rings -- Northeastern Siberia -- Sampling design -- Larix -- Larix cajanderi

Аннотация: Though the extraction of increment cores is common practice in tree-ring research, there is no standard for the number of samples per tree, or trees per site needed to accurately describe the common growth pattern of a discrete population of trees over space and time. Tree-ring chronologies composed of living, subfossil and archaeological material often combine an uneven distribution of increment cores and disc samples. The effects of taking one or two cores per tree, or even the inclusion of multiple radii measurements from entire discs, on chronology development and quality remain unreported. Here, we present four new larch (Larix cajanderi Mayr) ring width chronologies from the same 20 trees in northeastern Siberia that have been independently developed using different combinations of core and disc samples. Our experiment reveals: i) sawing is much faster than coring, with the latter not always hitting the pith; ii) the disc-based chronology contains fewer locally absent rings, extends further back in time and exhibits more growth coherency; iii) although the sampling design has little impact on the overall chronology behaviour, lower frequency information is more robustly obtained from the disc measurements that also tend to reflect a slightly stronger temperature signal. In quantifying the influence of sampling strategy on the quality of tree-ring width chronologies, and their suitability for climate reconstructions, this study provides useful insights for optimizing fieldwork campaigns, as well as for developing composite chronologies from different wood sources. © 2018 Elsevier GmbH

Scopus,
Смотреть статью,
WOS

Держатели документа:
Department of Geography, University of CambridgeCB2 3EN, United Kingdom
Sukachev Institute of Forest SB RAS, Krasnoyarsk, 660036, Russian Federation
Institute of Ecology and Geography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation
Global Change Research Institute CAS, Brno, 603 00, Czech Republic
Department of Wood Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Brno, 613 00, Czech Republic
Department of Physical Geography, Stockholm University, Stockholm, SE-106 91, Sweden
Navarino Environmental Observatory, Messinia, GR-24001, Greece
North-Eastern Federal University, 58 Belinsky Street, Yakutsk, 677000, Russian Federation
Melnikov Permafrost Institute, 36 Merzlotnaya Street, Yakutsk, 677010, Russian Federation
Swiss Federal Research Institute WSL, Birmensdorf, CH-8903, Switzerland
Department of Geography, Masaryk University61137, Czech Republic

Доп.точки доступа:
Kirdyanov, A. V.; Piermattei, A.; Kolar, T.; Rybnicek, M.; Krusic, P. J.; Nikolaev, A. N.; Reinig, F.; Buntgen, U.

    Dryland belt of Northern Eurasia: contemporary environmental changes and their consequences
/ P. Groisman [et al.] // Environ. Res. Lett. - 2018. - Vol. 13, Is. 11. - Ст. 115008, DOI 10.1088/1748-9326/aae43c. - Cited References:92. - PG and GH were supported in part by NASA grant NNX15AP81G. NT acknowledges the Russian Foundation for Basic Research grant 16-05-00496. OZ, AD, and PG were partially supported through 'ARCTIC-ERA: ARCTIC climate change and its impact on environment, infrastructures, and resource availability' sponsored by ANR (France), RFBR (Russia), and US NSF (grants 1717770 and 1558389). YC was supported by National Youth Science Fund of China grant 41701227 and by the Priority Academic Program Development of Jiangsu Higher Education Institutions in China. The work of AS was partially supported by US NSF grant 1602879 and Russian RFFI grant 18-05-60240. Grant 14.B25.31.0026 of the Ministry of Education and Science of the Russian Federation provided support to PG, NT, AS, OB, and OZ for their work conducted at the P P Shirshov Institute of Oceanology. Support for the work of IY and IK was provided by grant AP05135848 of the Ministry of Education and Sciences of the Republic of Kazakhstan. JC and RJ were supported by the Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF (grant 1313761) and the LCLUC program of NASA (grant NNX14AD85G). Grant 1717770 by the US National Science Foundation to George Washington University provided support to PG for his work at the Hydrology Science and Services Corporation via Sub-Recipient Agreement Number 17-S03R. The synthesis workshop (Ulaanbaatar, 2-5 June 2017) was partially sponsored by the 'Dynamics of Coupled Natural and Human Systems' program of the NSF (grant 1313761) and the LCLUC program of NASA (grant NNX15AD10G). . - ISSN 1748-9326
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: The dryland belt (DLB) in Northern Eurasia is the largest contiguous dryland on Earth. During the last century, changes here have included land use change (e.g. expansion of croplands and cities), resource extraction (e.g. coal, ores, oil, and gas), rapid institutional shifts (e.g. collapse of the Soviet Union), climatic changes, and natural disturbances (e.g. wildfires, floods, and dust storms). These factors intertwine, overlap, and sometimes mitigate, but can sometimes feedback upon each other to exacerbate their synergistic and cumulative effects. Thus, it is important to properly document each of these external and internal factors and to characterize the structural relationships among them in order to develop better approaches to alleviating negative consequences of these regional environmental changes. This paper addresses the climatic changes observed over the DLB in recent decades and outlines possible links of these changes (both impacts and feedback) with other external and internal factors of contemporary regional environmental changes and human activities within the DLB.

WOS,
Смотреть статью

Держатели документа:
North Carolina State Univ, NOAA, Ctr Environm Informat, Asheville, NC 28804 USA.
RAS, PP Shirshov Inst Oceanol, Moscow, Russia.
Hydrol Sci & Serv Corp, Asheville, NC 28801 USA.
Russian Inst Hydrometeorol Informat, Obninsk, Kaluga Area, Russia.
Michigan State Univ, E Lansing, MI 48824 USA.
State Hydrol Inst, St Petersburg, Russia.
Univ New Hampshire, Earth Syst Res Ctr, Durham, NH 03824 USA.
Nanjing Forestry Univ, Coll Biol & Environm, Joint Innovat Ctr Modern Forestry Studies, Nanjing, Jiangsu, Peoples R China.
SB RAS, Krasnoyarsk Fed Res Ctr, Sukachev Inst Forest, Krasnoyarsk, Russia.
Joseph Fourier Univ, Lab Glaciol & Geophys Environm, Grenoble, France.
Oklahoma State Univ, Stillwater, OK 74078 USA.
Univ Sopron, Sopron, Hungary.
Minist Energy Republ Kazakhstan, Joint Stock Co Zhasyl Damu, Alma Ata, Kazakhstan.
Natl Ctr Space Res & Technol, Alma Ata, Kazakhstan.

Доп.точки доступа:
Groisman, Pavel; Bulygina, Olga; Henebry, Geoffrey; Speranskaya, Nina; Shiklomanov, Alexander; Chen, Yizhao; Tchebakova, Nadezhda; Parfenova, Elena; Tilinina, Natalia; Zolina, Olga; Dufour, Ambroise; Chen, Jiquan; John, Ranjeet; Fan, Peilei; Mayas, Csaba; Yesserkepova, Irina; Kaipov, Ildan; NASA [NNX15AP81G]; Russian Foundation for Basic Research grant [16-05-00496]; 'ARCTIC-ERA: ARCTIC climate change and its impact on environment, infrastructures, and resource availability' - ANR (France); RFBR (Russia); US NSF [1602879, 1717770, 1558389]; National Youth Science Fund of China [41701227]; Priority Academic Program Development of Jiangsu Higher Education Institutions in China; Russian RFFI [18-05-60240]; Ministry of Education and Science of the Russian Federation [14.B25.31.0026]; Ministry of Education and Sciences of the Republic of Kazakhstan [AP05135848]; Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF [1313761]; LCLUC program of NASA [NNX15AD10G, NNX14AD85G]; US National Science Foundation [1717770, 17-S03R]; 'Dynamics of Coupled Natural and Human Systems' program of the NSF [1313761]

    Biotechnological aspects of bioconversion of post-extraction biomass and cell culture Orthilia secunda (L.) house with basidiomycetes
/ Zh. A. Koh, Yu. A. Litovka, R. Kh. Enazarov [и др.] // Khimiya Rastitel'nogo Syr'ya. - 2021. - Is. 4. - С. 359-369, DOI 10.14258/JCPRM.2020048392 . - ISSN 1029-5151
   Перевод заглавия: Биотехнологические аспекты утилизации послеэкстракционной биомассы и клеточной культуры orthilia secunda (L.) house базидиальными грибами
Аннотация: The possibility of bioconversion after the extraction residue of the medicinal plant Orthilia secunda (initial plant biomass and callus after extraction of biologically active substances) by fast growing strains of basidiomycetes Tv2-16K Trametes versicolor and Pe-17T Pleurotus eryngii was studied. The main target products are: a mycelial-plant product with a reduced content of the indigestible fraction and enriched in protein and full-fledged fruit bodies. Fungi colonize plant waste with a radial growth rate of 2.0-2.3 mm / day and a growth rate of 65-77 units. Phenol oxidase activity is 0.7-1.2 units/g·s, depending on the type after the extraction residue. In substrates after biodegradation, the proportion of difficult hydrolysable polysaccharides, easily hydrolysable polysaccharides, and lignin is on average 1.6 times lower than in the original substrate. The content of protein and extractive substances is significantly higher, especially after the extraction residue of O. secunda callus under the influence of the T. versicolor strain Tv2-16K: 12.8 and 24.3%, respectively, of the mass of dry substrate. Fruit bodies of P. eryngii strain Pe-17T were obtained on various compositions of plant substrates. The maximum fruit formation was noted on four-component substrates containing two types after extraction residues of O. secunda, wheat bran, birch or aspen sawdust: the average weight of fruit bodies from one block was 230-236 g; biological efficiency - 46-47.2%. © 2020 Altai State University. All rights reserved.

Scopus

Держатели документа:
Institute of Forest Named After V.N. Sukachev, SB, RAS, FRC, KSC, SB, RAS, Akademgorodok, 50/28, Krasnoyarsk, 660036, Russian Federation
Krasnoyarsk State Agrarian University, pr. Mira, 90, Krasnoyarsk, 660049, Russian Federation
Siberian State University of Science and Technology Named After Academician M.F. Reshetneva, pr. Mira, 82, Krasnoyarsk, 660049, Russian Federation

Доп.точки доступа:
Koh, Zh. A.; Litovka, Yu. A.; Enazarov, R. Kh.; Makolova, P. V.; Shimova, Yu. S.; Pochekutov, I. S.; Pavlov, I. N.

    Peroxide delignification of the vegetative part of Jerusalem artichoke in the medium acetic acid-water
/ T. V. Ryazanova, V. S. Fedorov, E. V. Kharyanova [и др.] // Khimiya Rastitel'nogo Syr'ya. - 2021. - Is. 4. - С. 351-358, DOI 10.14258/JCPRM.2020048520 . - ISSN 1029-5151
   Перевод заглавия: ПЕРОКСИДНАЯ ДЕЛИГНИФИКАЦИЯ ВЕГЕТАТИВНОЙ ЧАСТИ ТОПИНАМБУРА В СРЕДЕ УКСУСНАЯ КИСЛОТА - ВОДА

Кл.слова (ненормированные):
Cellulose -- Jerusalem artichoke -- Lignin -- Non-wood vegetable raw materials -- Redox-organosolvent delignification -- Vegetative part

Аннотация: The purpose of this work was to evaluate the vegetative part of Jerusalem artichoke as a raw material for the production of cellulose using redox-organosolvent delignification in the medium "CH3СOOН - H2O2 - H2O". The chemical composition of the vegetative part of Jerusalem artichoke and the influence of technological parameters of the delignification process on the yield and properties of the cellulose product were studied. It was found that the vegetative part of Jerusalem artichoke collected in October (stems without leaves) with a chemical composition of more than 50 wt.% of polysaccharides in which presented the Kurshner-Hoffer cellulose more than 90 wt.% was more promising for processing. Experimental methods have been used to determine the parameters of the process of delignification of the vegetative part of Jerusalem artichoke, which provide a high yield of cellulose (42.1 wt.%) with a low content of residual lignin (1.1 wt.%): content of H2O2 - 6.5 wt.%, CH3COOH - 23.4 wt.%, GM 15, duration - 2.5 h, catalyst H2SO4 - 0.2 wt.%. It is shown that pre-extraction of the vegetative part of Jerusalem artichoke with a 0.3% solution of dicarboxylic acids at a temperature of 80 °C with a liquid modulus of 10 for 3 hours reduces the content of residual lignin in the cellulose product to 0.5 wt.% and obtain an extract whose yield is - 7.8 wt.%, including a PB of 4.2 wt.%, which makes it promising for biochemical processing. The obtained results expand the areas of use of the vegetative part of Jerusalem artichoke and show the prospects for further more depth research to optimize the process of delignification and study the properties of the cellulose product. © 2020 Altai State University. All rights reserved.

Scopus

Держатели документа:
Siberian State University of Science and Technology named after Academician M.F. Reshetnev, pr. Krasnoyarskiy rabochiy, 31, Krasnoyarsk, 660037, Russian Federation
Institute of Forest named after V.N. Sukachev SB RAS, Federal Research Center "KSC SB RAS", Akademgorodok, 50/28, Krasnoyarsk, 660036, Russian Federation

Доп.точки доступа:
Ryazanova, T. V.; Fedorov, V. S.; Kharyanova, E. V.; Loskutov, S. R.; Kournikova, A. V.

    Reviews and syntheses: Arctic fire regimes and emissions in the 21st century
/ J. L. McCarty, J. Aalto, V. V. Paunu [et al.] // Biogeosciences. - 2021. - Vol. 18, Is. 18. - P5053-5083, DOI 10.5194/bg-18-5053-2021. - Cited References:268. - This research has been supported by Miami University, Ministry for Foreign Affairs of Finland (IBA Forest Fires, decision PC0TQ4BT-53); Business Finland (BC Footprint; grant no. 1462/31/2019); the ACRoBEAR project, funded by the Belmont Forum Climate, Environment and Health (CEH) Collaborative Research Action and the UK Natural Environment Research Council (grant no. NE/T013672/1); the Arctic Monitoring and As-sessment Programme (AMAP); the Russian Foundation for Basic Research (RFBR grant no. 19-45-240004); a joint project of the Government of Krasnoyarsk Territory and Russian Foundation for Basic Research (GKT KRFS and RFBR grant no. 20-05-00540); NASA's Weather and Data Analysis programme; and the Climate Adaptation Research Fund from Environment and Climate Change Canada. Portions of this publication were produced with the financial support of the European Union via the EU-funded Action on Black Carbon in the Arctic. Its contents are the sole responsibility of Jessica L. McCarty, Ville-Veikko Paunu, Zbigniew Klimont, and Justin J. Fain and do not necessarily reflect the views of the European Union. . - ISSN 1726-4170. - ISSN 1726-4189
РУБ Ecology + Geosciences, Multidisciplinary

Аннотация: In recent years, the pan-Arctic region has experienced increasingly extreme fire seasons. Fires in the northern high latitudes are driven by current and future climate change, lightning, fuel conditions, and human activity. In this context, conceptualizing and parameterizing current and future Arctic fire regimes will be important for fire and land management as well as understanding current and predicting future fire emissions. The objectives of this review were driven by policy questions identified by the Arctic Monitoring and Assessment Programme (AMAP) Working Group and posed to its Expert Group on Short-Lived Climate Forcers. This review synthesizes current understanding of the changing Arctic and boreal fire regimes, particularly as fire activity and its response to future climate change in the pan-Arctic have consequences for Arctic Council states aiming to mitigate and adapt to climate change in the north. The conclusions from our synthesis are the following. (1) Current and future Arctic fires, and the adjacent boreal region, are driven by natural (i.e. lightning) and human-caused ignition sources, including fires caused by timber and energy extraction, prescribed burning for landscape management, and tourism activities. Little is published in the scientific literature about cultural burning by Indigenous populations across the pan-Arctic, and questions remain on the source of ignitions above 70 degrees N in Arctic Russia. (2) Climate change is expected to make Arctic fires more likely by increasing the likelihood of extreme fire weather, increased lightning activity, and drier vegetative and ground fuel conditions. (3) To some extent, shifting agricultural land use and forest transitions from forest-steppe to steppe, tundra to taiga, and coniferous to deciduous in a warmer climate may increase and decrease open biomass burning, depending on land use in addition to climate-driven biome shifts. However, at the country and landscape scales, these relationships are not well established. (4) Current black carbon and PM2.5 emissions from wildfires above 50 and 65 degrees N are larger than emissions from the anthropogenic sectors of residential combustion, transportation, and flaring. Wildfire emissions have increased from 2010 to 2020, particularly above 60 degrees N, with 56% of black carbon emissions above 65 degrees N in 2020 attributed to open biomass burning - indicating how extreme the 2020 wildfire season was and how severe future Arctic wildfire seasons can potentially be. (5) What works in the boreal zones to prevent and fight wildfires may not work in the Arctic. Fire management will need to adapt to a changing climate, economic development, the Indigenous and local communities, and fragile northern ecosystems, including permafrost and peatlands. (6) Factors contributing to the uncertainty of predicting and quantifying future Arctic fire regimes include underestimation of Arctic fires by satellite systems, lack of agreement between Earth observations and official statistics, and still needed refinements of location, conditions, and previous fire return intervals on peat and permafrost landscapes. This review highlights that much research is needed in order to understand the local and regional impacts of the changing Arctic fire regime on emissions and the global climate, ecosystems, and pan-Arctic communities.

WOS

Держатели документа:
Miami Univ, Dept Geog, Oxford, OH 45056 USA.
Miami Univ, Geospatial Anal Ctr, Oxford, OH 45056 USA.
Finnish Meteorol Inst, Weather & Climate Change Impact Res, Helsinki, Finland.
Univ Helsinki, Dept Geosci & Geog, Helsinki, Finland.
Finnish Environm Inst SYKE, Ctr Sustainable Consumpt & Prod, Helsinki, Finland.
Univ Leeds, Sch Earth & Environm, Inst Climate & Atmospher Sci, Leeds, W Yorkshire, England.
Norwegian Inst Air Res, Dept Atmospher & Climate Res ATMOS, Kjeller, Norway.
Int Inst Appl Syst Anal IIASA, Laxenburg, Austria.
Russian Acad Sci, VN Sukachev Inst Forests, Siberian Branch, Krasnoyarsk, Russia.
Minist Environm Finland, Aleksanterinkatu 7,POB 35, Helsinki 00023, Finland.
Natl Inst Aerosp, Hampton, VA USA.
NASA, Langley Res Ctr, Hampton, VA 23665 USA.
Environm & Climate Change Canada, ASTD STB, Climate Res Div, Toronto, ON, Canada.
Arctic Monitoring & Assessment Programme AMAP Sec, Tromso, Norway.

Доп.точки доступа:
McCarty, Jessica L.; Aalto, Juha; Paunu, Ville-Veikko; Arnold, Steve R.; Eckhardt, Sabine; Klimont, Zbigniew; Fain, Justin J.; Evangeliou, Nikolaos; Venalainen, Ari; Tchebakova, Nadezhda M.; Parfenova, Elena, I; Kupiainen, Kaarle; Soja, Amber J.; Huang, Lin; Wilson, Simon; McCarty, Jessica; Miami University, Ministry for Foreign Affairs of Finland (IBA Forest Fires) [1462/31/2019]; Business Finland (BC Footprint) [1462/31/2019]; ACRoBEAR project - Belmont Forum Climate, Environment and Health (CEH) Collaborative Research Action; UK Natural Environment Research CouncilUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [NE/T013672/1]; Arctic Monitoring and As-sessment Programme (AMAP); Russian Foundation for Basic Research (RFBR)Russian Foundation for Basic Research (RFBR) [19-45-240004]; Russian Foundation for Basic ResearchRussian Foundation for Basic Research (RFBR) [20-05-00540]; NASA's Weather and Data Analysis programme; Climate Adaptation Research Fund from Environment and Climate Change Canada; European UnionEuropean Commission; Government of Krasnoyarsk Territory [20-05-00540]