Soil-solution chemistry in a low-elevation spruce-fir ecosystem, Howland, Maine

1995 ◽  
Vol 84 (1-2) ◽  
pp. 129-145 ◽  
Author(s):  
Ivan J. Fernandez ◽  
Gregory B. Lawrence ◽  
Yowhan Son
2012 ◽  
Vol 46 ◽  
pp. 165-173 ◽  
Author(s):  
Yang Cao ◽  
Tarja Lehto ◽  
Sirpa Piirainen ◽  
Jussi V.K. Kukkonen ◽  
Paavo Pelkonen

2018 ◽  
Vol 24 (8) ◽  
pp. 3603-3619 ◽  
Author(s):  
James Johnson ◽  
Elisabeth Graf Pannatier ◽  
Stefano Carnicelli ◽  
Guia Cecchini ◽  
Nicholas Clarke ◽  
...  

2001 ◽  
Vol 1 ◽  
pp. 457-466 ◽  
Author(s):  
E. Ring ◽  
L. Hogbom ◽  
H.A. Nohrstedt

Biofuels, such as brash from forest fellings, have been proposed as an alternative energy source. Brash removal may affect the sustainability of forest production, e.g., through a change in the availability of cations and N in the soil. We report initial effects of brash removal on inorganic N content in humus and mineral soil, soil-solution chemistry, and field-layer biomass after clear felling an N-fertilisation experiment in central Sweden. The experiment comprised six different fertiliser levels, ranging from 0 to 600 kg N ha�1. Urea was given every 5th year during 1967 to 1982 to replicated plots, giving total doses of 0 to 2400 kg N ha�1. Clear felling took place in 1995, 13 years after the last fertilisation. The removal of brash decreased the NO3� content in the humus layer after clear felling. A decrease in the NO3� concentration of the soil solution was indicated during most of the study period as well. No effect of the previous N fertilisation was found in the humus layer, but in the mineral soil there was an increase in NO3� content for the highest N dose after clear felling (p = 0.06). The soil-solution chemistry and the field-layer biomass showed an irregular pattern with no consistent effects of brash removal or previous fertilisation.


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