科研之友
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摘要
Due to long-lasting historic fly-ash deposition from lignite-fired power plants, soils of forest ecosystems in Central Germany have been affected by a variety of contaminants. In addition to heavy metals and oxides, another fly-ash compound is Black carbon (BC) which supposedly has been accumulated as well. BC as a generic term describing different forms of pyrogenetic carbon is considered as a very stable fraction of the C cycle. In this study, BC content of organic layers of 38 sites from two adjacent forested areas was determined using a simplified benzenepolycarboxylic acid (BPCA) method. Considerable amounts of BC were detected in both areas. It accounted for up to 11.2 and 15.6% of total organic carbon (TOC) in the Oe and Oa horizons, respectively. On average, slightly higher BC contents were found in the Oe (23.0 g BC kg(-1)), whereas BC/TOC ratios were higher in the Oa. The BC/TOC ratio of the Oe horizon tended to decrease with increasing distance from the former main emitters. In contrast to expectations, BC contents of the Oa horizon tended to increase with increasing distance. The deposition gradient, in previous research found for other fly-ash compounds, could not be observed for BC. Higher values in more remote forests might be taken as an indicator for the influence of additional emission sources. Further research is needed to confirm the results and to elucidate the potential impact of (soot-) BC on humus dynamics in the study area.
- 出版日期2011-1
