Spatial Distribution of Organic Matter and Nitrogen in the Entic Podzols of the Prioksko-Terrasnyi Reserve and Its Relationship with the Structure of Forest Phytocenoses

• Published in: Eurasian soil science 2020-08, Vol.53 (8), p.1021-1032
• Main Authors: Priputina, I. V., Frolova, G. G., Shanin, V. N., Myakshina, T. N., Grabarnik, P. Ya
• Format: Article
• Language: English
• Subjects: Carbon sinks; Carbon-nitrogen ratio; Coniferous forests; Deciduous forests; Decomposing organic matter; Distribution; Earth and Environmental Science; Earth Sciences; Ecosystems; Environment models; Fertility; Forest ecosystems; Forest soils; Forests; Genesis and Geography of Soils; Geotechnical Engineering & Applied Earth Sciences; Ground cover; Heterogeneity; Horizon; Humus; Litter; Litter fall; Mixed forests; Nitrogen; Organic carbon; Organic matter; Patchiness; Plant communities; Plant species; Podzolic soils; Podzols; Soil; Soil fertility; Soils; Spatial distribution; Spatial heterogeneity; Spatial variations; Species; Terrestrial ecosystems; Thickness
• ISSN: 1064-2293; 1556-195X
• DOI: 10.1134/S1064229320080128

Estimates of the spatial heterogeneity of the organic matter distribution in forest soils determined by the influence of the species and spatial structure of phytocenoses are relevant for many environmental problems, including the calculation of carbon sinks and modeling of the dynamics of forest ecosystems. We analyzed the data on the organic carbon (C org ) and total nitrogen (N tot ) contents in the O (forest litter) and AY (humus) horizons of Entic Podzols in the Prioksko-Terrasnyi Reserve (54.89° N, 37.56° E). The studied site is located in a coniferous–deciduous forest formed after overgrowing of the cutting area of pine stands. We sampled the O and AY horizons along transects between trees of different species, i.e., near the trunks, under the crown, and in the intercrown space. The contents of C org and N tot in the O horizon varied within 17.6–44.9 and 0.84–1.79%, respectively. The ranges for the AY horizon were greater: 0.71–8.5% (C org ) and 0.035–0.33% (N tot ). The relationship between the contents of C org and N tot in the O and AY horizons was close to linear ( r s = 0.72 and r s = 0.96, respectively). We also obtained similar C : N ratios for the both horizons. The litter thickness and the content of N tot in the O horizon, as well as the content of C org in the AY horizon, significantly differed in different parts of the transects ( P < 0.05). The differences in the litter thickness and the C org content in the O horizon under the crowns of different tree species were also significant. In samples from the AY horizon taken in intercrown spaces, the N tot content correlated with the demand of plant species of the ground cover for soil fertility. The data obtained reflect the influence of specific features of spatial patterns of surface and root litterfall in multispecies communities of mixed forest stands on the spatial variability of C org and N tot contents in soil.