SUMMARYForest harvesting is a major human-caused disturbance affecting carbon budgets in forest ecosystems. This study was concerned with post-logging carbon pool changes in Scots pine (Pinus sylvestris) and Siberian fir (Abies sibirica) stands. To understand carbon budget recovery trends following logging, carbon stock and fluxes were measured in stands differing in time since logging. In both Scots pine and fir stands disturbed by logging, the tree phytomass contribution to the carbon budget decreased drastically, whereas the coarse woody debris (CWD) carbon pool exhibited a marked increase. Sixty years following logging, the Scots pine stand carbon storage was almost 70 % of that prior to logging and the ratio between the phytomass and soil organic matter was the same as before the disturbance. While the phytomass carbon showed a similar trend in the fir stand of the same age, it was less than on the control stand. In a 50-55-year-old fir stand, 26 years since harvesting, the phytomass carbon recovered only by 15 %. Siberian fir and Scots pine logging sites differed in CWD loading and decomposition rate. The phytomass dynamics and CWD loading values obtained suggest that Scots pine stands which have experienced logging are most likely carbon sinks, as was clear from the phytomass production exceeding organic matter decomposition-caused fluxes. Conversely, logged fir ecosystems are likely to be sources of carbon to the atmosphere due to a large CWD loading, faster rate of its decomposition, and slow phytomass increment.Key words: carbon budget, logging, phytomass, coarse woody debris, decomposition.
RESUMENLa explotaci贸n forestal es un importante disturbio de origen humano que afecta el balance de carbono en ecosistemas forestales. Este estudio se concentr贸 en los cambios de las reservas de carbono post-cosecha de rodales de pino silvestre (Pinus sylvestris) y abeto siberiano (Abies sibirica). Para entender la recuperaci贸n del balance de carbono despu茅s de la cosecha, se midi贸 el stock y flujo de carbono en diferentes momentos posterior a la cosecha. En ambos rodales explotados, la contribuci贸n de la fitomasa forestal al balance de carbono disminuy贸 dr谩sticamente, mientras que la reserva de carbono en los residuos le帽osos de gran tama帽o (CWD) exhibi贸 un marcado incremento. Sesenta a帽os despu茅s de la cosecha, el almacenamiento de carbono en rodales de pino silvestre fue casi del 70 % respecto a lo de antes de cosecha. El radio entre la fitomasa y la materia org谩nica del suelo fue el mismo al de antes de la perturbaci贸n. Si bien la fitomasa de carbono mostr贸 una tendencia similar en el rodal de abeto, 茅ste fue menor que el rodal control. En un rodal de abeto de 50-55 a帽os de edad, 26 a帽os desde la explotaci贸n, el carbono de la fitomasa se recuper贸 en s贸lo un 15 %. Rodales explotados de abetos de Siberia y de pino silvestre difirieron en la carga de CWD y en la tasa de descomposici贸n. La din谩mica de la fitomasa y los valores de carga de CWD sugieren que los rodales explotados de pino silvestre son probablemente s...