Nitrogen mineralisation in deciduous forest soils in south Sweden in gradients of soil acidity and deposition

1998 ◽  
pp. 415-420
Author(s):  
Ursula Falkengren-Grerup ◽  
Jörg Brunet ◽  
Martin Diekmann
2001 ◽  
Vol 1 ◽  
pp. 548-555 ◽  
Author(s):  
H. Honoki ◽  
T. Kawakami ◽  
H. Yasuda ◽  
I. Maehara

Nitrate leakage from deciduous forest soils into streams was investigated for two adjacent hills. Many of the streams on Kureha Hill, located in Toyama City, Japan, have extremely high nitrate concentrations. The nitrate concentration of Hyakumakidani, one of the streams on Kureha Hill, averaged 158 μeq l-1and reached 470 μeq l-1during an episodic event. In contrast, the streams on Imizu Hill, adjacent to Kureha Hill, had low concentrations, below 15 μeq l-1. Even during an episode, the nitrate concentrations increased to no more than 75 μeq l-1.Both areas have similar blown forest soils, C/N ratios in O horizons, and vegetation consisting primarily of deciduous trees. However, soil incubation experiments, which lasted for 4 weeks, revealed that the nitrification rates in the surface soils of Kureha Hill were much higher than in the soils of Imizu Hill.


2012 ◽  
Vol 77 (6) ◽  
pp. 833-843 ◽  
Author(s):  
Ivica Djalovic ◽  
Djordje Jockovic ◽  
Goran Dugalic ◽  
Goran Bekavac ◽  
Bozana Purar ◽  
...  

Soil acidity and aluminum toxicity are considered most damaging soil conditions affecting the growth of most crops. This paper reviews the results of tests of pH, exchangeable acidity and mobile aluminum (Al) concentration in profiles of pseudogley soils from Cacak-Kraljevo basin. For that purpose, 102 soil pits were dug in 2009 in several sites around Cacak- Kraljevo basin. The tests encompassed 54 field, 28 meadow, and 20 forest soil samples. Samples of soil in the disturbed state were taken from the Ah and Eg horizons (102 samples), from the B1tg horizon in 39 field, 24 meadow and 15 forest pits (a total of 78 samples) and from the B2tg horizon in 14 field, 11 meadow, and 4 forest pits (a total of 29 samples). Mean pH values (1M KCl) of the tested soil profiles were 4.28, 3.90 and 3.80 for the Ah, Eg and B1tg horizons, respectively. Soil pH of forest samples was lower than those in meadow and arable land samples (mean values of 4.06, 3.97 and 3.85 for arable land, meadow and forest samples, respectively). Soil acidification was especially intensive in deep horizons, as 27% (Ah), 77% (Eg) and 87% (B1tg) soil samples had the pH value below 4.0. Mean values of total exchangeable acidity (TEA) were 1.55, 2.33 and 3.40 meq 100 g-1 for the Ah, Eg and B1tg horizons, respectively. The TEA values in forest soils were considerably higher (3.39 meq 100 g-1) than those in arable soils and meadow soils (1.96 and 1.93, respectively). Mean mobile Al contents of tested soil samples were 11.02, 19.58 and 28.33 mg Al 100 g-1 for the Ah, Eg and B1tg horizons, respectively. According to the pH and TEA values, mobile Al was considerably higher in the forest soils (the mean value of 26.08 mg Al 100 g-1) than in the arable soils and meadow soils (the mean values of 16.85 and 16.00 mg Al 100 g-1, respectively). The Eg and B1tg horizons of the forest soil had especially high mobile Al contents (the mean values of 28.50 and 32.95 mg Al 100 g-1, respectively). High levels of mobile Al were especially frequent in the forest soils, with 35% (Ah), 85.0% (Eg) and 93.3% (B1tg) of the tested samples ranging above 10 mg Al 100 g-1.


2003 ◽  
Vol 35 (6) ◽  
pp. 855-866 ◽  
Author(s):  
J.M. Xue ◽  
R. Sands ◽  
P.W. Clinton ◽  
T.W. Payn ◽  
M.F. Skinner

2020 ◽  
Author(s):  
Anna Walkiewicz ◽  
Piotr Bulak ◽  
Bruce Osborne ◽  
Mohammad Ibrahim Khalil ◽  
Syed Faiz-ul Islam ◽  
...  

<p>Forest soils are often a sink for atmospheric methane (CH<sub>4</sub>) and are thus worth special attention in the context of mitigation of greenhouse gases (GHGs) and offset of agricultural GHG emissions at farm to national levels. The litter layer influences the exchange of GHGs between soil and atmosphere; however, most studies focus on the contribution of only soil to the CH<sub>4</sub> cycle. In order to improve the inventory of this gas, it is worth investigating how litter influences the exchange of GHGs. Its effect on CH<sub>4</sub> uptake may vary in deciduous and coniferous sites due to the different properties of litter. Field experiments were carried out to assess the CH<sub>4</sub> uptake capability in 5 different soil types (with and without litter) under different forest types (deciduous, coniferous, and mixed) in Poland. During summer 2019, the highest CH<sub>4</sub> uptake (about 2 mg C m<sup>-2</sup> day<sup>-1</sup>) in a variant without litter on the ground was detected in Dystric Cambisol (with the highest C/N ratio) under a 100-year-old coniferous forest and in Albic Luvisol under a 58-year-old mixed forest. The presence of the litter level reduced the CH<sub>4</sub> flux in the range of 6-27% in these locations. Methane consumption was the lowest in silty soils (~ 0.4 – 1 mg C m<sup>-2</sup> day<sup>-1</sup>) in the mixed forest and decreased by 13-29% when covered with the litter layer. The negative effect of the litter layer on CH<sub>4</sub> absorption was the lowest (~ 3-4%) in sandy Eutric Gleysol under a 75-year-old deciduous forest with 90% of oak and 10% of European hornbeam. The dry conditions in the summer 2019 (with total rainfall 163 mm during the tested months in the studied region) resulted in low moisture in both the litter and soil. However, even low-humidity litter (below 10%) reduced CH<sub>4</sub> consumption rates in the measured sites.</p><p>Research was partially conducted under the project financed by Polish National Centre for Research and Development within of ERA-NET CO-FUND ERA-GAS Programme (ERA-GAS/I/GHG-MANAGE/01/2018).</p>


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