esoilБюллетень Почвенного института имени В.В. ДокучаеваDokuchaev Soil Bulletin0136-16942312-4202V.V. Dokuchaev Soil Science Institute10.19047/0136-1694-2020-102-103-124esoil-570Research ArticleСтатьиОценка насыщенности почвы органическим углеродомEstimation of soil saturation with organic carbonКогутБ. М.KogutB. M.

119017, Москва, Пыжевский пер, 7, стр. 2

7 Bld. 2 Pyzhevskiy per., Moscow 119017

kogutb@mail.ruСеменовВ. М.SemenovV. M.

142290, Пущино, Институтская ул., 2

2 Institutskaya Str., Pushchino, 142290

v.m.semenov@mail.ruФИЦ “Почвенный институт им. В.В. Докучаева”РоссияFederal Research Centre “V.V. Dokuchaev Soil Science Institute”Russian FederationИнститут физико-химических и биологических проблем почвоведения РАН – обособленное подразделение ФИЦ «Пущинский научный центр биологических исследований Российской академии наук»РоссияInstitute of Physicochemical and Biological Problems of Soil Science, Russian Academy of SciencesRussian Federation2020110720200102103124Copyright © Когут Б.М., Семенов В.М., 20202020Когут Б.М., Семенов В.М.Kogut B.M., Semenov V.M.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://bulletin.esoil.ru/jour/article/view/570

Сформулированы новые дефиниции понятий “секвестрация” и “депонирование” органического углерода почвами на количественной основе, учитывающие период полного оборота аккумулированного органического вещества и его распределение по почвенному профилю. Определены уровни углеродпротекторной емкости ряда почв европейской части России согласно Hassink (1997) и Six et al. (2002), базирующиеся на информации по содержанию тонкодисперсных фракций и минералогическому составу почв. Рассчитаны степени насыщенности этих почв углеродом и их углеродсеквестрирующий потенциал по Meyer et al. (2017) и Wiesmeier et al. (2014). Установлено, что серые лесные и каштановые почвы относятся к мало насыщенным органическим углеродом, луговая слитизированная и пойменная луговая – к умеренно насыщенным, а черноземы – к насыщенным. Показано, что углеродсеквестрирующий потенциал серой лесной почвы составляет около 30 т С га-1, каштановой – не превышает 25 т С га-1, луговых почв равен 15–20 т С га-1, а черноземов – менее 5 т С га-1. Приводятся критические замечания к инициативе “4 промилле”.

New definitions of “soil carbon sequestration” and “soil carbon deposition” on a quantitative basis taking into account the period of the complete turnover of accumulated organic matter and its distribution over the soil profile are formulated. The carbon protection capacity of soils in the European part of Russia was determined according to Hassink (1997) and Six et al. (2002) based on data of the fine fractions content and the mineralogical composition of soils. The carbon saturation degree of soils and their carbon sequestration potential were calculated according to Meyer et al. (2017) and Wiesmeier et al. (2014). Gray forest and chestnut soils were classified as poorly saturated with organic carbon, meadow slitized and floodplain meadow soils were moderately saturated, and chernozems was saturated. It has been shown that the carbon sequestration potential of gray forest soil is about 30 t C ha-1, chestnut soil does not exceed 25 t C ha-1, meadow soil is 15–20 t C ha-1, and chernozem is less than 5 t C ha-1. Critical remarks to the 4 ppm initiativewere given.

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