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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Black carbon and soil properties at historical charcoal production sites in Germany
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Black carbon and soil properties at historical charcoal production sites in Germany

机译:德国历史悠久的木炭生产基地的黑碳和土壤特性

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The use of charcoal as a soil amendment is currently of great interest to sequester carbon and improve soil fertility, however, studies of sites where charcoal amendments to the soil have been made many years ago are lacking at the moment. In this study we investigated historical charcoal production sites in Germany that have not been in use for >60 years, and evaluated the effects of the former charcoal inputs on soil and vegetation parameters relative to those of adjacent, unamended areas. Surface soil samples (0-5, 5-20 cm) were taken from five sites located on extremely acidic (Siegerland, pH 3.8-4.1) and base rich soils (Eifel, pH 4.8-5.3) in species poor (Luzulo-Fagetum) and species rich (Hordelymo-Fagetum) beech forests, respectively. We determined stocks of black carbon (BC) and natural soil organic carbon (SOC = total C minus BC) as well as of soil nutrient stocks (NO3-N, P, K, Mg), cation exchange capacity and water holding capacity, and we mapped plant composition to calculate richness and evenness. The results showed that historical charcoal production sites were enriched with BC and also exhibited increased stocks of natural SOC and total N possibly due to enhanced stabilization of natural SOC by the charcoal. The availability of nitrate-nitrogen, phosphate and potassium was increased when the charcoal was added to the base rich soils and less so when charcoal was added to the extremely acidic soils. Plant biodiversity was not different between the sites of historical charcoal addition and the reference sites. We conclude that charcoal additions may increase soil carbon storage capacity over prolonged periods of time without negatively affecting plant ecological interactions over the long term
机译:目前,使用木炭作为土壤改良剂对固碳和改善土壤肥力具有极大的兴趣,但是,目前缺乏对许多年前对土壤进行木炭改良剂的场所的研究。在这项研究中,我们调查了德国历史上超过60年未使用的木炭生产地点,并评估了前木炭投入对土壤和植被参数的影响(相对于邻近的未修改区域)。地表土壤样品(0-5、5-20 cm)是从极弱物种(Luzulo-Fagetum)的极酸性(Siegerland,pH 3.8-4.1)和基础丰富的土壤(Eifel,pH 4.8-5.3)的五个地点采集的和物种丰富的(Hordelymo-Fagetum)山毛榉林。我们确定了黑碳(BC)和天然土壤有机碳(SOC =总C减去BC)以及土壤养分储量(NO3-N,P,K,Mg)的存量,阳离子交换能力和持水能力,以及我们绘制了植物成分图以计算丰富度和均匀度。结果表明,历史上的木炭生产场所富含BC,也可能显示出天然SOC和总氮的增加,这可能是由于木炭对天然SOC的增强了稳定性。当将木炭添加到富含碱的土壤中时,硝酸盐,氮,磷酸盐和钾的有效性增加,而当将木炭添加到极酸性的土壤中时,硝酸盐,氮,磷酸盐和钾的有效性增加。在历史木炭添加地点和参考地点之间,植物生物多样性没有差异。我们得出的结论是,添加木炭可以长期增加土壤的碳储存能力,而不会长期影响植物的生态相互作用

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