资源环境科技发展态势分析平台

The objective of this study was to investigate the effect of afforestation of post-arable sandy soils (Dystric Arenosols) with Scots pine (Pima sylvestris L.) on the amount and distribution of C-org, N-tot and P-tot stocks between genetic soil horizons. The study was performed at three locations with five classes of afforestation each: 10-, 20-, 30-, 40-, 50-year-old stands, which additionally included the arable and the continuous forest soils as reference. The soil was sampled by genetic horizon, including the organic one, down to 100 cm, from its whole thickness, and from A horizon of the afforested soils from: 0-5, 5-10 and 10-20 cm. In the organic horizon of the afforested soils, the stock of C-org, N-tot and P-tot, increased significantly with stand age, and an average rate of accumulation was 33.6, 1.30 and 0.04 g m(-2) year(-1) respectively. C-org stocks in the former plough layer were found to decrease within the first decade of afforestation, and subsequently, the values gradually increased. With organic horizon included the respective stocks reached the level comparable with the related horizon of the arable soil after approx. 20-30 years. Subsoil B, BC and C horizons together accounted for approx. 35% of the C-org stocks in the entire profile. N-tot stocks in mineral soil horizons initially dropped in the first decade after afforestation, which was subsequently followed by an increase; however, after 50 years, still the observed values were lower in comparison with both the respective arable and continuous forest soils. P-tot stocks in the mineral soil horizon declined over the chronosequence, and in the profile at 50-year-old stands, they were lower in comparison with both the arable and the continuous forest soils. Stand age and sampling by genetic horizons, including the organic horizon, from the entire soil profile should be considered for estimation of changes in C-org, N-tot and P-tot stocks following afforestation of agricultural soils.