References

sergeogr

Известия Российской академии наук. Серия географическая

Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya

2587-55662658-6975

10.1134/S2587556618060146

sergeogr-784

Research Article

Природные процессы и динамика геосистем

Natural Processes and Dynamics of Geosystems

ПРОСТРАНСТВЕННОЕ РАСПРЕДЕЛЕНИЕ ОРГАНИЧЕСКОГО УГЛЕРОДА В ПОЧВАХ ВОСТОЧНО-ЕВРОПЕЙСКОЙ ТУНДРЫ И ЛЕСОТУНДРЫ В ЗАВИСИМОСТИ ОТ КЛИМАТА И РЕЛЬЕФА

Spatial Distribution of Organic Carbon in Soils of Eastern European Tundra and Forest-Tundra Depending on Climate and Topography

Шарый

П. А.

Shary

P. A.

p_shary@mail.ru

Шарая

Л. С.

Sharaya

L. S.

Пастухов

А. В.

Pastukhov

A. V.

Каверин

Д. А.

Kaverin

D. A.

Институт физико-химических и биологических проблем почвоведения РАНРоссияInstitute of Physicochemical and Biological Problems of Soil Science, Russian Academy of SciencesRussian Federation

Институт экологии Волжского бассейна РАНРоссияInstitute of Volga Basin Ecology, Russian Academy of SciencesRussian Federation

Институт биологии Коми НЦ УрО РАНРоссияInstitute of Biology, Komi Science Center, Ural Branch, Russian Academy of SciencesRussian Federation

2018

19122018

063948

2018

Шарый П.А., Шарая Л.С., Пастухов А.В., Каверин Д.А.

Shary P.A., Sharaya L.S., Pastukhov A.V., Kaverin D.A.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://izvestia.igras.ru/jour/article/view/784

Оценка запасов почвенного органического углерода (ПОУ) на участке 11 800 км2 тундры и лесотундры в бассейне р. Усы проведена с помощью множественной регрессии, учитывающей как роль таксонов почв, так и влияние климата и рельефа. Модель объясняла 84% пространственной изменчивости запасов ПОУ. Найдены отрицательные связи запасов ПОУ с климатическими нормами осадков июня, а также с высотой, обсуждаются причины этих зависимостей. На изученный участок по модели рассчитаны карта запасов ПОУ разрешения 300 м. Рассчитана также карта запасов ПОУ при использовании не меняющихся в пространстве “эталонных” значений – средних по точкам наблюдения для таксонов почв. Среднее значение запасов ПОУ по модели составило 21.6 кгС/м2 , а по матрице с “эталонами” – 32.0 кгС/м2 . Предложены скорректированные рассчитанные из модели “эталонные” значения для таксонов почв данного региона, которые в полтора раза ниже полученных по точкам наблюдения. Показано, что средние отклонения запасов ПОУ от скорректированных “эталонных” значений, отражающие влияние климата и рельефа, составляют 5.85 кгС/м2 . Осуществленный здесь учет климата и рельефа в дополнение к таксонам почв дает более корректную оценку запасов ПОУ, чем часто используемые “эталонные” значения для таксонов почв. Показано, что эти различия не малы.

Evaluation of soil organic carbon (SOC) storage in 11800 km2 area of tundra and forest-tundra in Usa River basin was carried out using multiple regression with account of soil taxa and influence of climate and topography. The model explained 84% of spatial variability in SOC storage. Negative relations were found between SOC and climatic norms of June precipitation, as well as elevation; causes of these relations are discussed. Based on the model, a gridded map of SOC storages was calculated at resolution 300 m. In addition, a grid of SOC storages was calculated using spatially uniform “reference” values that are averages by observation points for soil taxa. An average of SOC storages by the model is 21.6 kgC/m2 , while it is 32.0 kgC/m2 when the “reference” values were used. Corrected “reference” values calculated from the model were suggested that are 1.5 times lower than those obtained from observation points. It was shown that average deviations of SOC storages from corrected “reference” values, which reflect influence of climate and topography, are 5.85 kgC/m2 . When climate and topography are taken into account in addition to soil taxa, this provides more correct evaluation of SOC than frequently used “reference” values for soil taxa. It is shown that the distinctions are not small.

пространственная изменчивостьрегрессионная модельюжная тундраторфяники

spatial variabilityregression modelsouth tundrapeatlands

References1

Малкова Г.В. Мониторинг среднегодовой температуры пород на стационаре Болванский // Криосфера Земли. 2010. Т. 14. № 3. С. 3–14.

Malkova G.V. Mean-annual ground temperature monitoring on the steady-state-station “Bolvansky”. Earth’s Cryosphere, 2010, vol. 14, no. 3, pp. 3–14.

Орлов Д.С., Бирюкова О.Н., Суханова Н.И. Органическое вещество почв Российской Федерации. М.: Наука, 1996. 256 с.

Orlov D.S., Biryukova O.N., and Sukhanova N.I. Organicheskoe veshchestvo pochv Rossiiskoi Federatsii [Organic Matter of Soils of Russian Federation]. Moscow: Nauka Publ., 1996. 256 p.

Рожков В.А., Вагнер В.В., Когут Б.М., Конюшков Д.Е., Шеремет Б.В. Запасы органических и минеральных форм углерода в почвах России // Углерод в биогеоценозах. Докл. на XV ежегодных чтениях памяти акад. В.Н. Сукачева. М., 1997. С. 5–58.

Rozhkov V.A., Wagner V.V., Kogut B.M., Konyushkov D.E., and Sheremet B.V. Storage of Organic and Mineral Forms of Carbon in Soils of Russia. In Uglerod v biogeotsenozakh [Carbon in Biogeocoenoses]. Moscow, 1997, pp. 5–58. (In Russ.).

Рыжова И.М., Подвезенная М.А. Пространственная вариабельность запасов органического углерода в почвах лесных и степных биогеоценозов // Почвоведение. 2008. № 12. С. 1429–1437.

Ryzhova I.M. and Podvezennaya M.A. Spatial variability of the organic carbon pool in soils of forest and steppe biogeocenoses. Euras. Soil Sci., 2008, vol. 41, no. 12, pp. 1429–1437.

Честных О.В., Замолодчиков Д.Г., Карелин Д.В. Запасы органического углерода в почвах тундровых и лесотундровых экосистем России // Экология. 1999. № 6. С. 426–432.

Chestnykh O.V., Zamolodchikov D.G., and Karelin D.V. Storages of organic carbon in soils of tundra and frorest-tundra ecosystems of Russia. Ekologiya, 1999, no. 6, pp. 426–432. (In Russ.).

Честных О.В., Замолодчиков Д.Г., Уткин А.И., Коровин Г.Н. Распределение запасов органического углерода в почвах лесов России // Лесоведение. 1999. № 2. С. 13–21.

Chestnyh O.V., Zamolodchikov D.G., Utkin A.I., and Korovin G.N. The distribution of soil organic carbon in soils of forests of Russia. Lesovedenie, 1999, no. 2, pp. 13–21. (In Russ.).

Честных О.В., Замолодчиков Д.Г. Зависимость плотности почвенных горизонтов от глубины их залегания и содержания гумуса // Почвоведение. 2004. № 8. С. 816–863.

Chestnyh O.V. and Zamolodchikov D.G. Bulk density of soil horizons as dependent on their humus content. Euras. Soil Sci., 2004, no. 8, pp. 816–863.

Честных О.В., Замолодчиков Д.Г., Уткин А.И. Общие запасы органического углерода и азота в почвах лесного фонда России // Почвоведение. 2004. № 4. С. 30–42.

Chestnyh O.V., Zamolodchikov D.G., and Utkin A.I. Total storages of organic carbon and nitrogen in soils of forest reserves of Russia. Lesovedenie, 2004, no. 4, pp. 30–42. (In Russ.).

Шарый П.А., Пинский Д.Л. Статистическая оценка связи пространственной изменчивости содержания органического углерода в серой лесной почве с плотностью, концентрацией металлов и рельефом // Почвоведение. 2013. № 11. С. 1344–1356.

Shary P.A. and Pinskii D.L. Statistical evaluation of the relationships between spatial variability in the organic carbon content in gray forest soils, soil density, concentrations of heavy metals, and topography. Euras. Soil Sci., 2013, vol. 46, no. 11, pp. 1344–1356.

Щепащенко Д.Г., Мухортова Л.В., Швиденко А.З., Ведрова Э.Ф. Запасы органического углерода в почвах России // Почвоведение. 2013. № 2. С. 123– 132.

Shchepashchenko D.G., Mukhortova L.V., Shvidenko A.Z., and Vedrova E.F. The pool of organic carbon in the soils of Russia. Euras. Soil Sci., 2013, vol. 46, no. 2, pp. 123–132.

Circumpolar Arctic Vegetation Map. Scale 1:7.500.000. Conservation of Arctic Flora and Fauna (CAFF) Map No. 1. U.S. Fish and Wildlife Service, Anchorage, Alaska, 2003.

Circumpolar Arctic Vegetation Map. Scale 1:7,500,000. Conservation of Arctic Flora and Fauna (CAFF) Map No. 1. U.S. Fish and Wildlife Service, Anchorage, Alaska, 2003.

Danielson J.J., Gesch D.B. Global multi-resolution terrain elevation data 2010 (GMTED2010) // U.S. Geological Survey Open-File Report 2011–1073, 2011. 26 p. 13. Davidson E.A., Janssens I.A. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change // Nature. 2006. V. 440. P. 165–173.

Danielson J.J. and Gesch D.B. Global multi-resolution terrain elevation data 2010 (GMTED2010). U.S. Geological Survey Open-File Report 2011–1073, 2011. 26 p.

Epstein H.E., Yu Q., Raynolds M.K., Walker D.A., Bhatt U.S., Tucker C.J., Pinzon J.E. Climate and grazing influences on dynamics of arctic tundra vegetation and implications for permafrost: Proceedings of the Tenth International Conference on Permafrost, TICOP, Resources and Risks of Permafrost Areas in a Changing World (Salekhard, Yamal-Nenets Autonomous District, Russia, June 25–29, 2012) / Salekhard. 2012. V. 4. Extended Abstracts. P. 139–140.

Davidson E.A. and Janssens I.A. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change. Nature, 2006, vol. 440, pp. 165–173.

Gruber S. Derivation and analysis of a high-resolution estimate of global permafrost zonation // The Cryosphere. 2012. V. 6. P. 221–233.

Epstein H.E., Yu Q., Raynolds M.K., Walker D.A., Bhatt U.S., Tucker C.J., and Pinzon J.E. Climate and grazing influences on dynamics of arctic tundra vegetation and implications for permafrost. In Proceedings of the Tenth International Conference on Permafrost, TICOP, Resources and Risks of Permafrost Areas in a Changing World. Salekhard, Yamal-Nenets Autonomous District, June 25–29, 2012. Extended Abstracts, vol. 4, pp. 139–140.

Hijmans R.J., Cameron S.E., Parra J.L., Jones P.J., Jarvis A. Very high resolution interpolated climate surfaces for global land areas // Int. J. of Climatology. 2005. V. 25. P. 1965–1978.

Gruber S. Derivation and analysis of a high-resolution estimate of global permafrost zonation. The Cryosphere, 2012, vol. 6, pp. 221–233.

Hugelius G., Kuhry P. Landscape partitioning and environmental gradient analyses of soil organic carbon in a permafrost environment // Global Biogeochemical Cycles. 2009. V. 23. P. GB3006.

Hijmans R.J., Cameron S.E., Parra J.L., Jones P.J., and Jarvis A. Very high resolution interpolated climate surfaces for global land areas. Int. J. Climatol., 2005, vol. 25, pp. 1965–1978.

Hugelius G., Virtanen T., Kaverin D., Pastukhov A., Rivkin F., Marchenko S., Romanovsky V., Kuhry P. High-resolution mapping of ecosystem carbon storage and potential effects of permafrost thaw in periglacial terrain, European Russian Arctic // J. of Geophysical Res. 2011. V. 116. P. G03024.

Hugelius G. and Kuhry P. Landscape partitioning and environmental gradient analyses of soil organic carbon in a permafrost environment. Global Biogeochemical Cycles, 2009, vol. 23, pp. GB3006.

Jobbágy E.G., Jackson R.B. The vertical distribution of soil organic carbon and its relation to climate and vegetation // Ecol. Applications. 2000. V. 10. P. 423–436.

Hugelius G., Virtanen T., Kaverin D., Pastukhov A., Rivkin F., Marchenko S., Romanovsky V., and Kuhry P. High-resolution mapping of ecosystem carbon storage and potential effects of permafrost thaw in periglacial terrain, European Russian Arctic. J. Geophys. Res., 2011, vol. 116, pp. G03024.

Kolchugina T.P., Vinson T.S. Carbon balance of the continuous permafrost zone of Russia // Clim. Res. 1993. V. 3. P. 13–21.

Jobbágy E.G. and Jackson R.B. The vertical distribution of soil organic carbon and its relation to climate and vegetation. Ecological Applications, 2000, vol. 10, pp. 423–436.

Kuhry P., Mazhitova G.G., Forest P.-A., Deneva S.V., Virtanen T., Kultti S. Upscaling soil organic carbon estimates for the Usa Basin (Northeast European Russia) using GIS-based landcover and soil classification schemes // Danish J. of Geography. 2002. V. 102. P. 11–25.

Kolchugina T.P., Vinson T.S. Carbon balance of the continuous permafrost zone of Russia. Climatic Res., 1993, vol. 3, pp. 13–21.

McGuire A.D., Anderson L.G., Christensen T.R., Dallimore S., Guo L., Hayes D.J., Heimann M., Lorenson T.D., Macdonald R.W., Roulet N. Sensitivity of the carbon cycle in the Arctic to climate change // Ecol. Monographs. 2009. V. 79. P. 523–555.

Kuhry P., Mazhitova G.G., Forest P.-A., Deneva S.V., Virtanen T., and Kultti S. Upscaling soil organic carbon estimates for the Usa Basin (Northeast European Russia) using GIS-based landcover and soil classification schemes. Danish J. Geogr., 2002, vol. 102, pp. 11–25.

Montgomery D.C., Peck E.A. Introduction to Linear Regression Analysis. NY: John Wiley & Sons, 1982. 504 p.

McGuire A.D., Anderson L.G., Christensen T.R., Dallimore S., Guo L., Hayes D.J., Heimann M., Lorenson T.D., Macdonald R.W., and Roulet N. Sensitivity of the carbon cycle in the Arctic to climate change. Ecological Monographs, 2009, vol. 79, pp. 523–555.

Oberman N. Contemporary permafrost degradation of Northern European Russia: Proceedings of the Ninth International Conference on Permafrost (Fairbanks, Alaska, June 29–July 3, 2008) / Fairbanks, Alaska. 2008. V. 2. P. 1305–1310.

Montgomery D.C., Peck E.A. Introduction to Linear Regression Analysis. New York: John Wiley & Sons, 1982. 504 p.

Pastukhov A.V., Kaverin D.A., Sharaya L.S., Shary P.A. The spatial distribution of SOC in the forest tundra of the European North-East: Proceedings of the Tenth International Conference on Permafrost (TICOP). Resources and Risks of Permafrost Areas in a Changing World (Salekhard, Yamal-Nenets Autonomous District, Russia, June 25–29, 2012) / Salekhard. 2012. V. 4. Extended Abstracts. P. 443.

Oberman N. Contemporary permafrost degradation of Northern European Russia. In Proceedings of the Ninth International Conference on Permafrost, June 29–July 3, Fairbanks, Alaska, 2008, vol. 2, pp. 1305–1310.

Raynolds M.K., Walker D.A., Maier H.A. NDVI patterns and phytomass distribution in the circumpolar Arctic // Remote Sensing of Environment. 2006. V. 102. P. 271–281.

Pastukhov A.V., Kaverin D.A., Sharaya L.S., and Shary P.A. The spatial distribution of SOC in the forest tundra of the European North-East. In Proceedings of the Tenth International Conference on Permafrost (TICOP). Resources and Risks of Permafrost Areas in a Changing World. Conference held in Salekhard, Yamal-Nenets Autonomous District, Russia, June 25–29, 2012, vol. 4, Extended Abstracts, 443 p.

Romanovsky V.E., Smith S.L., Christiansen H.H. Permafrost thermal state in the polar northern hemisphere during the International Polar Year 2007–2009: a synthesis // Permafrost and Periglacial Processes. 2010. V. 21. P. 106–116.

Raynolds M.K., Walker D.A., and Maier H.A. NDVI patterns and phytomass distribution in the circumpolar Arctic. Remote Sensing of Environment, 2006, vol. 102, pp. 271–281.

Shary P.A., Sharaya L.S., Mitusov A.V. Fundamental quantitative methods of land surface analysis // Geoderma. 2002. V. 107. P. 1–32.

Romanovsky V.E., Smith S.L., and Christiansen H.H. Permafrost thermal state in the polar northern hemisphere during the International Polar Year 2007–2009: a synthesis. Permafrost and Periglacial Processes, 2010, vol. 21, pp. 106–116.

Tarnocai C., Canadell J.G., Schuur E.A.G., Kuhry P., Mazhitova G., Zimov S. Soil organic carbon stocks in the northern circumpolar permafrost region // Global Biogeochemical Cycles. 2009. V. 23. P. GB2023.

Shary P.A., Sharaya L.S., and Mitusov A.V. Fundamental quantitative methods of land surface analysis. Geoderma, 2002, vol. 107, pp. 1–32.

Walker D.A., Raynolds M.K., Daniëls F.J.A., Einarsson E., Elvebakk A., Gould W.A., Katenin A.E., Kholod S.S., Markon C.J., Melnikov E.S., Moskalenko N.G., Talbot S.S., Yurtsev B.A., et al. The circumpolar Arctic vegetation map // J. of Vegetation Sci. 2005. V. 16. P. 267–282.

Tarnocai C., Canadell J.G., Schuur E.A.G., Kuhry P., Mazhitova G., and Zimov S. Soil organic carbon stocks in the northern circumpolar permafrost region. Global Biogeochemical Cycles, 2009, vol. 23, pp. GB2023.

Walker D.A., Raynolds M.K., Daniëls F.J.A., Einarsson E., Elvebakk A., Gould W.A., Katenin A.E., Kholod S.S., Markon C.J., Melnikov E.S., Moskalenko N.G., Talbot S.S., Yurtsev B.A., et al. The circumpolar Arctic vegetation map. J. Vegetation Sci., 2005, vol. 16, pp. 267–282.

The authors declare that there are no conflicts of interest present.