scholarly journals Supplementary material to "Leaching of inorganic and organic phosphorus and nitrogen in contrasting beech forest soils – seasonal patterns and effects of fertilization"

Author(s):  
Jasmin Fetzer ◽  
Emmanuel Frossard ◽  
Klaus Kaiser ◽  
Frank Hagedorn
2020 ◽  
Author(s):  
Markus Krüger ◽  
Karin Potthast ◽  
Beate Michalzik ◽  
Alexander Tischer ◽  
Kirsten Küsel ◽  
...  

AbstractNitrification in forest soils is often associated with increased leaching of nitrate to deeper soil layers with potential impacts on groundwater resources, further enhanced under scenarios of anthropogenic atmospheric nitrogen deposition and predicted weather extremes. We aimed to disentangle the relationships between soil nitrification potential, seepage-mediated nitrate leaching and the vertical translocation of nitrifiers in soils of a temperate mixed beech forest in central Germany before, during and after the severe summer drought 2018. Leaching of nitrate assessed below the litter layer and in 4, 16 and 30 cm soil depth showed high temporal and vertical variation with maxima at 16 and 30 cm during and after the drought period. Maximum of soil potential nitrification activity of 4.4 mg N kg-1 d-1 only partially coincided with maximum nitrate leaching of 10.5 kg N ha-2. Both ammonia oxidizing bacteria (AOB) and ammonia oxidizing archaea (AOA) were subject to translocation by seepage, and AOB decreased at least by half and AOA increased by one to three orders of magnitude in their abundance in seepage with increasing soil depth. On the level of the total bacterial population, an increasing trend with depth was also observed for Cand. Patescibacteria while Bacteroidetes were strongly mobilized from the litter layer but poorly transported further down. Despite stable population densities in soil over time, abundances of AOA, AOB and total bacteria in seepage increased by one order of magnitude after the onset of autumn rewetting. Predicted future higher frequency of drought periods in temperate regions may result in more frequent seepage-mediated seasonal flushes of nitrate and bacteria from forest soils. Moreover, the observed translocation patterns point to taxon-specific differences in the susceptibility to mobilization, suggesting that only selected topsoil derived microbial groups are likely to affect subsoil or groundwater microbial communities and their functional potential.


2017 ◽  
Vol 68 (4) ◽  
pp. 205-211 ◽  
Author(s):  
Tomasz Wanic ◽  
Jan Bodziarczyk ◽  
Michał Gąsiorek ◽  
Paweł Hawryło ◽  
Agnieszka Józefowska ◽  
...  

Abstract The primary objective of this study was to characterise the edaphic conditions of forest areas in the Pieniny National Park (PNP), and to describe the dependencies between properties of forest soils and types of forest plant communities. The “Soil Trophic Index” (SIGg) for mountainous areas was applied. The evaluation of the trophism for 74 forest monitoring employed the soil trophic index for mountainous areas SIGg or SIGgo. Plant communities in the forest monitoring areas were classified according to the Braun-Blanquet’s phytosociological method. Soils of PNP present in the forest monitoring areas were mostly classified as eutrophic brown soils (72.9%), rendzinas (10.8%), brown rendzinas (5.41%), and rubble initial soils (5.41%). Pararendzinas, dystrophic brown soils, and gley soils were less common (total below 5.5%). In the forest monitoring areas of PNP, eutrophic soils predominate over mesotrophic soils. High SIGg index of the soils is caused by high values of acidity and nitrogen content. The Carpathian beech forest Dentario glandulosae-Fagetum and thermophilic beech forest Carici albae-Fagetum associations are characterised by high naturalness and compatibility of theoretical habitats. The soils of the Carpathian fir forest Dentario glandulosae-Fagetum abietetosum subcommunity is characterised by a higher share of silt and clay particles and lower acidity as compared to the Carpathian beech forest Dentario glandulosae-Fagetum typicum subcommunity. The soils of the forest monitoring areas in PNP stand out in terms of their fertility against forest soils in other mountainous areas in Poland.


2013 ◽  
Vol 1 (No. 1) ◽  
pp. 3-9
Author(s):  
Mládková Lenka ◽  
Borůvka Marcela Rohošková and Luboš

This paper is focused on soil organic matter quality assessment in acid forest soils. Soil samples were collected in the Jizera Mountains region. Vegetation cover of sampling sites was formed by spruce or beech monocultures. Humus quality was assessed by the ratio of absorbances of pyrophosphate soil extract at the wavelengths of 400 and 600 nm (A400/A600). Humus fractionation was performed on selected soil samples. DRIFT spectra of individual fractions were measured. Higher pH and lower C and N contents were found in beech forest than in spruce forest. A400/A600 well correlates with C and N contents (r = 0.510*** and 0.615***, respectively). C and N content increases as to humus quality decreases. DRIFT spectra of fulvic acids turned out to be unsuitable for describing differences in humus quality. DRIFT spectra of humic acids and humin were hence more suitable. The difference between spruce and beech forest was found in 1514.cm–1 (C=C bounds of benzene rings) and 1550 cm–1 (N-H bounds in monosubstituted amides) bands intensities. Humic acids and humin coming from the O horizons of beech forest are relatively enriched by nitrogen functional groups. Values of humic acids aromaticity index did not differ between beech and spruce forests. DRIFT spectroscopy was shown as a possible method for detailed humus quality studying.


2013 ◽  
Vol 58 ◽  
pp. 286-295 ◽  
Author(s):  
Zhengfang Wang ◽  
Mo Shi ◽  
Jihua Li ◽  
Liang Zhou ◽  
Zhongwei Wang ◽  
...  

1969 ◽  
Vol 20 (4) ◽  
pp. 653 ◽  
Author(s):  
OL Jones ◽  
SM Bromfield

Ground samples of hayed-off pasture plants were decomposed in the laboratory under continuously moist, and intermittently moist and dry, conditions. During the course of decomposition they were leached at different frequencies and the resulting changes in inorganic and organic phosphorus measured. The dissolution of superphosphate and its conversion to organic phosphorus were also studied under some of these conditions.Inorganic phosphate was readily leached from the samples when microbes were inhibited. Microbial activity, on the other hand, largely prevented the loss of inorganic phosphate by leaching from a phalaris sample over a period of 3 months. Intermittent drying increased the amount of phosphate leached from decomposing plants but the leaching frequencies examined had little effect. The percentage of the phosphorus leached from plants varied with the type of material. In all cases less than half was recovered as inorganic phosphate, even after decomposition and leaching for 6 months. When superphosphate granules were leached in the presence of decomposing plants the conversion of fertilizer phosphate to organic phosphorus was small, but the dissolution of phosphate was sometimes retarded. The recycling of phosphate in hayed-off pastures is discussed in the light of these results.


2003 ◽  
Vol 51 (2) ◽  
pp. 151 ◽  
Author(s):  
Nicole A. Sawyer ◽  
Susan M. Chambers ◽  
John W. G. Cairney

Utilisation of orthophosphate, inositol hexaphosphate and DNA by isolates of Amanita alboverrucosa, A. conicoverrucosa, A. fuscosquamosa, A. muscaria, A. nauseosa, A. ochrophylla, A. pyramidifera, A.�roseolamellata, A. xanthocephala and six unidentified Amanita species from eastern Australian temperate sclerophyll forests was examined during growth in axenic liquid cultures. With the exception of A. nauseosa and A.�xanthocephala on DNA, isolates of all taxa were shown to utilise orthophosphate and both organic substrates as sole phosphorus sources. Considerable intraspecific variation in utilisation of the organic phosphorus sources relative to orthophosphate was observed for A. muscaria and the native Australian taxa. Overall the data suggest that Amanita spp. may contribute significantly to organic phosphorus mobilisation in Australian forest soils.


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