Почтовый адрес: САФУ, Редакция «Лесной журнал», наб. Северной Двины, 17, г. Архангельск, Россия, 163002, ауд. 1425

Тел.: 8(8182) 21-61-18
Сайт: http://lesnoizhurnal.ru/ 
e-mail: forest@narfu.ru

RussianEnglish



архив

Запасы органического углерода в лесных почвах Северной Монголии

Версия для печати

М. Тунгалаг, С. Гэрэлбаатар, А.И. Лобанов

Рубрика: Краткие сообщения и обмен опытом

Скачать статью (pdf, 0.5MB )

УДК

574.36

DOI:

10.37482/0536-1036-2020-2-169-176

Аннотация

Запасы органического углерода в почве и их изменение в региональном и большем пространственном масштабе имеют решающее значение для оценки их глобальной инвертации в почвах и прогнозирования дальнейших изменений. Цель работы – оценить запасы органического углерода в почвах бореальных лесов северной Монголии. Исследование проводилось в лесах Булган, Сэленгэ и Тув аймаков с использованием полностью рандомизированного метода отбора пробных площадей. Для лабораторных анализов было отобрано 900 почвенных образцов на 60 пробных площадях. на каждой пробной площади заложен почвенный профиль глубиной 30 см с взятием образцов из трех слоев почвы: 0...5, 5...15 и 15...30 см. Результаты исследования показали значительное отличие в запасах органического углерода в почвах не только между аймаками, но и внутри каждого аймака. Более высокие показатели отмечены в лесных почвах Сэленгийского аймака (123,5±14,85 т/га), самые низкие – в почвах Тув аймака (51,13±7,8 т/га). Обнаружено заметно меньше органического углерода в почвах бореальных лесов Монголии по сравнению с азиатской частью России, включая Сибирь и Дальний восток, что может быть вызвано частым дефицитом воды и географическим расположением монгольских бореальных лесов, граничащих с засушливыми степями Центральной Азии. Установлено, что накопление органического углерода в почвах бореальных лесов Монголии в значительной степени связано с их расположением на горных склонах и распределением осадков по территории. Более высокое количество органического углерода в почвах обнаружено на северных склонах, в более пониженных местах с малыми склонами и возвышенностью. следовательно, влагообеспеченность в основном определяет характер распределения запасов органического углерода в почвах бореальных лесов северной Монголии.

Сведения об авторах

М. Тунгалаг1, канд. биол. наук; ORCID: https://orcid.org/0000-0001-9727-9084
С. Гэрэлбаатар1, канд. биол. наук, доц.; ORCID: https://orcid.org/0000-0002-9561-5256
А.И. Лобанов2, канд. биол. наук; ORCID: https://orcid.org/0000-0003-0505-8212
1Монгольский государственный университет, ул. Университетская, д. 3, г. Улан-Батор, Монголия, 14201; e-mail: gerelbaatar@seas.num.edu.mn
2Научно-исследовательский институт аграрных проблем хакасии, а/я 709, г. Абакан, Республика хакасия, Россия, 655019; e-mail: anatolylobanov@ksc.krasn.ru

Ключевые слова

почва лесной зоны, органический углерод, запас углерода, экспозиция склона, северная Монголия

Для цитирования

Tungalag М., Gerelbaatar S., Lobanov A.I. Organic Carbon Stocks in the Forest Soils of Northern Mongolia // Изв. вузов. лесн. журн. 2020. № 2. с. 169–176. DOI: 10.37482/0536-1036-2020-2-169-176

Литература

1. Бобкова К.С., Галенко Э.П., Тужилкина В.В., Осипов А.Ф., Кузнецов М.А. Роль бореальных лесов европейского севера России в регулировании углеродного баланса северного полушария // Управленческие аспекты развития северных территорий России: материалы всерос. науч. конф. (с междунар. участием). Сыктывкар: КРАГСИУ, 2015. Ч. 3. C. 36–41. [Bobkova K.S., Galenko E.P., Tuzhilkina V.V., Osipov A.F., Kuznetsov M.A. The Role of Boreal Forests of the European North of Russia in Carbon Balance Regulation of the Northern Hemisphere. Management Aspects of Development of the Northern Territories of Russia. Proceedings of the All-Russian Scientific Conference with International Participation. Syktyvkar, KRASSA Publ., 2015, part 3, pp. 36–41].
2. Ваганов Е.А., Ведрова Э.Ф., Верховец С.В., Ефремов С.П., Ефремова Т.Т., Круглов В.Б., Онучин А.А., Сухинин А.И., Шибистова О.Б. Леса и болота сибири в глобальном цикле углерода // Cиб. экол. журн. 2005. т. 12, № 4. C. 631–650. [Vaganov E.A., Vedrova E.F., Verkhovets S.V., Efremov S.P., Efremova T.T., Kruglov V.B., Onuchin A.A., Sukhinin A.I., Shibistova O.B. Forests and Swamps of Siberia in the Global Carbon Cycle. Sibirskiy ekologicheskiy zhurnal [Contemporary Problems of Ecology], 2005, vol. 12, no. 4, pp. 631–650].
3. Замолодчиков Д.Г., Грабовский В.И., Честных О.В. Динамика баланса углерода в лесах федеральных округов Российской Федерации // Вопр. лесн. науки. 2018. Т. 1(1). С. 1–24. [Zamolodchikov D.G., Grabowsky V.I., Chestnykh O.V. Dynamics of Carbon Budget in Forests of Federal Districts of Russian Federation. Voprosy lesnoy nauki [Forest Science Issues], 2018, vol. 1(1), pp. 1–24.]. DOI: 10.31509/2658-607X-2018-1-1-1-24
4. Ball D.F. Loss-on-Ignition as an Estimate of Organic Matter and Organic Carbon in Non-Calcareous Soils. Journal of Soil Science, 1964, vol. 15, iss. 1, pp. 84–92. DOI: 10.1111/j.1365-2389.1964.tb00247.x
5. Bayat A.T. Carbon Stock in an Apennine Beach Forest. MSC Thesis, Geo-Information Science and Earth Observation. Enschede, Netherlands, University of Twente, 2011. 54 p.
6. Berg E.E., Henry J.D., Fastie C.L., De Volder A.D., Matsuoka S.M. Spruce Beetle Outbreaks on the Kenai Peninsula, Alaska, and Kluane National Park and Reserve, Yukon Territory: Relationship to Summer Temperatures and Regional Differences in Disturbance Regimes. Forest Ecology and Management, 2006, vol. 227, iss. 3, pp. 219–232. DOI: 10.1016/j.foreco.2006.02.038
7. Carvalhais N., Forkel M., Khomik M., Bellarby J., Jung M., Migliavacca M. et al. Global Covariation of Carbon Turnover Times with Climate in Terrestrial Ecosystems. Nature, 2014, vol. 514, pp. 213–217. DOI: 10.1038/nature13731
8. Chapin F.S., Sturm M., Serreze M.C., McFadden J.P., Key J.R., Lloyd A.H. et al. Role of Land-Surface Changes in Arctic Summer Warming. Science, 2005, vol. 310, iss. 5748, pp. 657–660. DOI: 10.1126/science.1117368
9. Ciais P., Sabine C. et al. Carbon and Other Biogeochemical Cycles. Climate Change 2013: The Physical Science Basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Ed. by T.F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung et al. Cambridge, Cambridge University Press, 2013, pp. 465–570.
10. Dolman A.J., Shvidenko A., Schepaschenko D., Ciais P., Tchebakova N., Chen T. et al. An Estimate of the Terrestrial Carbon Budget of Russia Using Inventory-Based, Eddy Covariance and Inversion Method. Biogeosciences, 2012, vol. 9, iss. 12, pp. 5323–5340. DOI: 10.5194/bg-9-5323-2012
11. Dulamsuren C., Hauk M., Leuschner C. Seedling Emergence and Establishment of Pinus sylvestris in the Mongolian Forest-Steppe Ecotone. Plant Ecology, 2013, vol. 214, iss. 1, pp. 139–152. DOI: 10.1007/s11258-012-0152-z
12. Feyissa A., Soromessa T., Argaw M. Forest Carbon Stocks and Variations along Altitudinal Gradients in Egdu Forest: Implications of Managing Forests for Climate Change Mitigation. Science, Technology and Arts Research Journal, 2013, vol. 2, no. 4, pp. 40–46. DOI: 10.4314/star.v2i4.8
13. Hancock G.R., Murphy D., Evans K.G. Hillslope and Catchment Scale Soil Organic Carbon Concentration: An Assessment of the Role of Geomorphology and Soil Erosion in an Undisturbed Environment. Geoderma, 2010, vol. 155, iss. 1-2, pp. 36–45. DOI: 10.1016/j.geoderma.2009.11.021
14. Heiri O., Lotter A.F., Lemcke G. Loss on Ignition as a Method for Estimating Organic and Carbonate Content in Sediments: Reproducibility and Comparability of Results. Journal of Paleolimnology, 2001, vol. 25, pp. 101–110. DOI: 10.1023/A:1008119611481
15. Karjalainen T., Richards G. Definitions and Methodological Options to Inventory Emissions from Direct Human-Induced Degradation of Forest and Devegetation of Other Vegetation Types. IPCC Report. Ed. by J. Penman, M. Gytarsky, T. Hiraishi, T. Krug, D. Kruger, R. Pipatti et al. Japan, IGES, 2003. 32 p.
16. Kirschbaum M.U.F. Will Changes in Soil Organic Carbon Act as a Positive or Negative Feedback on Global Warming? Biogeochemistry, 2000, vol. 48, iss. 1, pp. 21–51. DOI: 10.1023/A:1006238902976
17. Köchy M., Hiederer R., Freibauer A. Global Distribution of Soil Organic Carbon – Part 1: Masses and Frequency Distributions of SOC Stocks for the Tropics, Permafrost Regions, Wetlands, and the World. Soil, 2015, vol. 1, iss. 1, pp. 351–365. DOI: 10.5194/soil-1-351-2015
18. Kurz W.A., Dymond C.C., Stinson G., Rampley G.J., Neilson E.T., Carroll A.L. et al. Mountain Pine Beetle and Forest Carbon Feedback to Climate Change. Nature, 2008, vol. 452, pp. 987–990. DOI: 10.1038/nature06777
19. Lee X., Huang Y., Huang D., Hu L., Feng Z., Cheng J. et al. Variation of Soil Organic Carbon and Its Major Constraints in East Central Asia. PLoS ONE, 2016, vol. 11(3), art. e0150709. DOI: 10.1371/journal.pone.0150709
20. Mühlenberg M., Appelfelder H., Hoffmann H., Ayush E., Wilson K.J. Structure of the Montane Taiga Forests of West Khentii, Northern Mongolia. Journal of Forest Science, 2012, vol. 58, pp. 45–56. DOI: 10.17221/97/2010-JFS
21. Mukhortova L., Schepaschenko D., Shvidenko A., McCallum I., Kraxnerb F. Soil Contribution to Carbon Budget of Russian Forests. Agricultural and Forest Meteorology, 2015, vol. 200, pp. 97–108. DOI: 10.1016/j.agrformet.2014.09.017
22. MPNFI Mongolian Multipurpose National Forest Inventory Report (2014–2016). Ulaanbaatar, Ministry of Nature and Environment, 2016. 126 p.
23. Myhre G., Shindell D. et al. Anthropogenic and Natural Radiative Forcing. Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Ed. by T.F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung et al. Cambridge, Cambridge University Press, 2013, pp. 659–740.
24. Pan Y., Birdsey R.A., Fang J., Houghton R., Kauppi P.E., Kurz W.A. et al. A Large and Persistent Carbon Sink in the Worldʼs Forests. Science, 2011, vol. 333, iss. 6045, pp. 988–993. DOI: 10.1126/science.1201609
25. Rogers B.M., Soja A.J., Goulden M.L., Randerson J.T. Influence Of Tree Species on Continental Differences in Boreal Fires and Climate Feedbacks. Nature Geoscience, 2015, vol. 8, pp. 228–234. DOI: 10.1038/ngeo2352
26. Soja A.J., Shugart H.H., Sukhinin A., Conard S., Stackhouse Jr. P.W. SatelliteDerived Mean Fire Return Intervals as Indicators of Change in Siberia (1995–2002). Miti gation and Adaptation Strategies for Global Change, 2006, vol. 11, iss. 1, pp. 75–96. DOI: 10.1007/s11027-006-1009-3
27. Trahan M.W., Schubert B.A. Temperature-Induced Water Stress in High-Latitude Forests in Response to Natural and Anthropogenic Warming. Global Change Biology, 2016, vol. 22, iss. 2, pp. 782–791. DOI: 10.1111/gcb.13121
28. Trumbore S.E., Harden J.W. Accumulation and Turnover of Carbon in Soils of the BOREAS Northern Study Area. Journal of Geophysical Research: Atmospheres, 1997, vol. 102, iss. D24, pp. 28817–28830. DOI: 10.1029/97JD02231
29. Ugawa S., Takahashi M., Morisada K., Takeuchi M., Matsuura Y., Yoshinaga S. et al. Carbon Stocks of Dead Wood, Litter, and Soil in the Forest Sector of Japan: General Description of the National Forest Soil Carbon Inventory. Bull FFPRI, 2012, vol. 11, pp. 207–221.
30. Walker X.J., Mack M.C., Johnstone J.F. Stable Carbon Isotope Analysis Reveals Widespread Drought Stress in Boreal Black Spruce Forests. Global Change Biology, 2015, vol. 21, iss. 8, pp. 3102–3113. DOI: 10.1111/gcb.12893
31. Yohannes H., Soromessa T., Argaw M. Carbon Stock Analysis along Slope and Slope Aspect Gradient in Gedo Forest: Implications for Climate Change Mitigation. Journal of Earth Science and Climate Change, 2015, vol. 6(9), art. 305. DOI: 10.4172/2157-7617.1000305
32. Zhu M., Feng Q., Zhang M., Liu W., Qin Y., Deo R.C. et al. Effects of Topography on Soil Organic Carbon Stocks in Grasslands of a Semiarid Alpine Region, Northwestern China. Journal of Soils and Sediments, 2019, vol. 19, pp. 1640–1650. DOI: 10.1007/s11368-018-2203-0

Ссылка на английскую версию:

Organic Carbon Stocks in the Forest Soils of Northern Mongolia

УДК 574.36
DOI: 10.37482/0536-1036-2020-2-169-176

ORGANIC CARBON STOCKS IN THE FOREST SOILS OF NORTHERN MONGOLIA

М. Tungalag1, PhD in Biology; ORCID: https://orcid.org/0000-0001-9727-9084
S. Gerelbaatar1, PhD in Biology, Assoc. Prof.; ORCID: https://orcid.org/0000-0002-9561-5256
A.I. Lobanov2, Candidate of Biology; ORCID: https://orcid.org/0000-0003-0505-8212
1National University of Mongolia, Ikh Surguuliin gudamj -3, P.O. Box -46A/523, Ulaanbaatar, 210646, Mongolia; e-mail: matungalag@yahoo.com, gerelbaatar@seas.num.edu.mn
2Scietific Research Institute of Agrarian Problems of Khakassia, P.O. Box 709, Abakan, Republic of Khakassia, 655019, Russian Federation; e-mail: anatolylobanov@ksc.krasn.ru

Soil organic carbon (SOC) stock and its variation on the regional and large spatial scales are critical for estimating the global SOC inventory and predicting further changes. This study was aimed at estimation of the SOC stock in the boreal forests of Northern Mongolia. The study was carried out in the forested areas of the Bulgan, Selenge and Tuv provinces using a completely randomized design. A total of 900 soil samples from 60 sampling points were collected for the laboratory analyses. At each point, a soil profile with a depth of more than 30 cm was laid out, and then soil samples were taken from three soil layers: 0–5, 5–15, and 15–30 cm of each profile. Therefore, the results of the assessment show a high difference of the SOC stock not only between the provinces, but also within each province. The higher SOC stocks were observed in the Selenge (123.5±14.85 t/ha), and lowest in the Tuv (51.23±7.8 t/ha) provinces. The estimated SOC stock in the studied regions was 93.77 t/ha on average. We found relatively less SOC stock in the boreal forests of Mongolia compared with the Asian part of Russia including Siberia and the Russian Far East. Such a less SOC stock may be caused by geographical distribution, where the Mongolian forests border the Central Asian dry steppe and frequent water deficit. However, we found that the accumulation of SOC stocks in the boreal forests of Mongolia is largely dependent on the mountain slopes and aspects combined with the distribution of precipitation across the country. Higher amount of SOC stocks were found in north-facing aspects and lower positions with low slopes of the mountains in lower altitude. Consequently, moisture supply basically determines the pattern of the SOC stock distribution in the northern boreal forests of Mongolia.
For citation: Tungalag М., Gerelbaatar S., Lobanov A.I. Organic Carbon Stocks in the Forest Soils of Northern Mongolia. Lesnoy Zhurnal [Russian Forestry Journal], 2020, no. 2, pp. 169–176. DOI: 10.37482/0536-1036-2020-2-169-176

Keywords: forest soil, organic carbon, SOC stock, aspect, Northern Mongolia.

Поступила 24.09.19 / Received on September 24, 2019