Corrigendum “Temperature sensitivity of C and N mineralization in temperate forest soils at low temperatures”

Schütt, Marianne; Borken, Werner; Spott, Oliver; Stange, Claus Florian; Matzner, Egbert

doi:10.1016/j.soilbio.2014.06.001

Cited by 5 publications

(2 citation statements)

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“…Roberts et al 2005;Harrington et al 2013). Changes in the soil microclimate may influence mineralization and nitrification rates (Kriebitzsch 1978;Schütt et al 2014aSchütt et al , 2014b. When studying leachates from lysimeters containing soil organic horizons, Emmett et al (1991) found that a covering of polystyrene beads resulted in NO 3 -losses similar to those recorded with a covering of fresh logging residues.…”

Section: Introductionmentioning

confidence: 99%

Soil and soil-water chemistry below different amounts of logging residues at two harvested forest sites in Sweden

Ring¹,

Högbom²,

Nohrstedt³

et al. 2015

Silva Fenn.

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Logging residues (LR),i.e. tops, branches, and needles, are increasingly being harvested for energy production in Fennoscandia. These residues are temporarily piled on site awaiting transport. This study was undertaken to investigate effects on the soil and soil-water chemistry below different amounts of LR at two recently harvested coniferous sites in Sweden. Seven treatments were included and the studied amounts of LR ranged from no LR left on the ground to four times the estimated LR amount of the harvested stands. Two treatments included eight times the estimated LR amount of the harvested stands but here the LR were removed after 7 or 20 weeks. Soil-water samples were collected during the first six or seven growing seasons. Effects of treatment were detected in the soil water for 11 chemical variables at the northern site, and for the NO and Cl concentrations at the southern site. The strongest response was generally found in the treatment with four times the estimated LR amount, for which the highest concentrations were recorded in most cases. In the first three seasons, the water flux through the LR decreased with an increasing amount of residue. Effects on the exchangeable store of Ca in the mor layer and the upper 20 cm of the mineral soil was detected at both sites. At the northern site, the weight of the remaining LR, ground vegetation and all other material above the mor layer in the treatments with two and four times the estimated LR amount was roughly twice the corresponding weights at the southern site seven years after treatment. Although strong effects on the soil-solution chemistry were detected at one of the study sites, in the treatments corresponding to two and four times the estimated logging residue amount, the effect on the leaching from an entire regeneration area is likely to be relatively small given the percentage of the area hosting these logging residue amounts (ca. 20% after stem-only harvesting and 9% after fuel-adapted felling). 3--2+

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Section: Introductionmentioning

confidence: 99%

Soil and soil-water chemistry below different amounts of logging residues at two harvested forest sites in Sweden

Ring¹,

Högbom²,

Nohrstedt³

et al. 2015

Silva Fenn.

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“…High microbial biomass N tends to increase ammonification (Schütt et al, 2014), which explains, at least in part, the higher net NH 4 + content in the intact than in degraded soil. The higher NO 3 − content than NH 4 + in the degraded soil indicated fast nitrification and poor NO 3 − uptake by microorganisms.…”

Section: N Forms and Poolsmentioning

confidence: 99%

Long‐term active restoration of extremely degraded alpine grassland accelerated turnover and increased stability of soil carbon

Bai

Degen

et al. 2020

Global Change Biology

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Soil nutrient contents and organic carbon (C) stability are key indicators for restoration of degraded grassland. However, the effects of long-term active restoration of extremely degraded grassland on soil parameters have been equivocal. The aims of this study were to evaluate the impact of active restoration of degraded alpine grassland on: (a) soil organic matter (SOM) mineralization; and (b) the importance of biotic factors for temperature sensitivity (Q 10) of SOM mineralization. Soils were sampled from intact, degraded and restored alpine grasslands at altitudes ranging between S U PP O RTI N G I N FO R M ATI O N Additional supporting information may be found online in the Supporting Information section. How to cite this article: Bai Y, Ma L, Degen AA, et al. Longterm active restoration of extremely degraded alpine grassland accelerated turnover and increased stability of soil carbon.

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Short-Term Eucalyptus and Phragmites Biochar’s Efficiency in Mineralization of Soil Carbon

Koçak

Ortaş

2021

J Soil Sci Plant Nutr

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Corrigendum “Temperature sensitivity of C and N mineralization in temperate forest soils at low temperatures”

Cited by 5 publications

References 0 publications

Soil and soil-water chemistry below different amounts of logging residues at two harvested forest sites in Sweden

Soil and soil-water chemistry below different amounts of logging residues at two harvested forest sites in Sweden

Long‐term active restoration of extremely degraded alpine grassland accelerated turnover and increased stability of soil carbon

Short-Term Eucalyptus and Phragmites Biochar’s Efficiency in Mineralization of Soil Carbon

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