Agrosphere Institute, Institute of Bio- and Geosciences (IBG-3), Forschungszentrum Jülich, Jülich, Germany.
Institute of Crop Science and Resource Conservation (INRES), Soil Science and Soil Ecology, University of Bonn, Nussallee, Bonn, Germany.
PLoS One. 2019 Aug 1;14(8):e0220476. doi: 10.1371/journal.pone.0220476. eCollection 2019.
Clear-cuts of forests severely affect soil structure and thus soil organic matter (SOM) and nutrient cycling dynamics therein, though with yet unknown consequences for SOM composition as well as phosphorus (P) and sulfur (S) chemical form within the soil microaggregate size fraction. To determine the effects of conventional clear-cutting on soil chemistry in a Cambisol of the Wüstebach Forest (northwestern Germany), we sampled the mineral A- and B-horizons prior to clear-cut as well as 10 and 24 month thereafter. We measured the SOM composition of soil microaggregates using pyrolysis field ionization mass spectrometry (Py-FIMS), as well as P and S chemical form and speciation using wet-chemical extractions and X-ray absorption near edge structure (XANES) spectroscopy. We found that clear-cut led to an increase of the microaggregate size fraction up to 6% due to break-down of macroaggregates and initially significantly increased total elemental concentrations (C, N, P, S) due to the introduction of slash-residues. The SOM of slash-residues consisted to a substantial amount of sterols and was generally found to be of low thermal stability and probably did not contribute to aggregate stability. Deterioration of the aggregate structure probably led to an exposure of originally inaccessible sites within aggregates to the attack by soil microorganisms and thus to an increased P and S turnover as reflected in a significantly reduction of available P proportions (4 to 7%) and a reduction of the most reduced S forms (5%). A probable increased microbial activity and contribution to SOM after clear-cut is also reflected in the significantly increasing hexose:pentose ratio by 0.25 between 10 and 24 month after clear-cut, significantly increasing the general thermal stability of SOM in the microaggregate size fraction and believed to contribute to aggregate stability. This indicated that a first deterioration of the aggregate structure after clear-cut might in the long-term be remediated with time.
森林皆伐严重影响土壤结构,进而影响土壤有机质(SOM)和养分循环动态,尽管其对土壤微团聚体中 SOM 组成以及磷(P)和硫(S)化学形态的影响尚不清楚。为了确定传统皆伐对德国西北部 Wüstebach 森林中黑钙土土壤化学的影响,我们在皆伐前采集了矿物 A 层和 B 层的土壤样本,以及皆伐后 10 个月和 24 个月后的样本。我们使用热裂解场电离质谱(Py-FIMS)测定了土壤微团聚体中的 SOM 组成,还使用湿化学提取和 X 射线吸收近边结构(XANES)光谱法测定了 P 和 S 的化学形态和形态。我们发现,皆伐导致微团聚体大小增加了 6%,这是由于大团聚体的分解,同时由于采伐残留物的引入,总元素浓度(C、N、P、S)最初显著增加。采伐残留物的 SOM 中含有大量甾醇,通常具有较低的热稳定性,可能不会有助于团聚体的稳定性。团聚体结构的恶化可能导致原本无法接近的团聚体内的部位受到土壤微生物的攻击,从而导致 P 和 S 周转率增加,表现在有效 P 比例(4%至 7%)显著降低和最还原 S 形态(5%)降低。皆伐后微生物活性和 SOM 贡献的增加也反映在 10 个月至 24 个月后 hexose:pentose 比值显著增加了 0.25,这显著增加了微团聚体中 SOM 的总体热稳定性,并有助于团聚体的稳定性。这表明,皆伐后团聚体结构的初步恶化可能会随着时间的推移而得到长期修复。