Soil solution fluxes and composition trends reveal risks of nitrate leaching from forest soils of Italy

CATENA ◽  
2021 ◽  
Vol 200 ◽  
pp. 105175
Author(s):  
Guia Cecchini ◽  
Anna Andreetta ◽  
Aldo Marchetto ◽  
Stefano Carnicelli
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.


Soil Research ◽  
2010 ◽  
Vol 48 (3) ◽  
pp. 286 ◽  
Author(s):  
R. G. McLaren ◽  
A. Black ◽  
L. M. Clucas

In this study we examined the bioavailability and chemistry of Cu, Ni, and Zn in metal-spiked, biosolids-amended forest (Pinus radiata) soils that had undergone a simulated conversion back to agricultural use. Mixing of the biosolids-treated forest litter into the underlying mineral soil resulted in high concentrations of each metal in easily extractable and soil solution forms. There was also very little change in these concentrations during a subsequent 2-year incubation period of the samples. Chemical speciation of the soil solutions using WHAM 6 showed that Cu was dominated by organic complexes, whereas most Ni and Zn was present as Ni2+ and Zn2+, with generally <5% of these elements present as organic complexes. Addition of lime to the soils substantially decreased both readily extractable and soil solution metal concentrations. However, even in their unlimed state, although plant metal concentrations were increased by the original biosolids treatments, there were no adverse effects due to the metals on plant growth as determined in a wheat germination and seedling growth test. In this study, the DGT technique showed considerable promise for assessing metal availability to plants. However, the study suggests that conversion of biosolids-treated forest soils back for agricultural use is unlikely to result in any substantial problems related to the metal loadings built up in the forest litter layer.


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