National Museum of Health and Medicine, 2460 Linden Lane, Bldg 2500, Silver Spring, MD 20910, USA.
Forensic Sci Int. 2012 Oct 10;222(1-3):4-10. doi: 10.1016/j.forsciint.2012.04.028. Epub 2012 May 20.
The University of Tennessee Anthropology Research Facility (ARF) is known for its unique contribution to forensic science as a site of human decomposition research. Studies conducted at ARF are integral in our understanding of the processes of human decomposition. As such, the authors are interested in the long-term effects of continuous human decomposition on the soil environment. Soil samples collected from within and outside the ARF were evaluated for moisture content, pH, organic content, total carbon and nitrogen content, and biomass by lipid-bound phosphorus, and total extracted DNA. Analyses revealed no significant differences (p<0.05) among the sampled areas within the facility, and yet demonstrated a possible trend toward increased levels of total N, Lipid-P, and water, suggesting an influx of high-quality nutrients into the ARF soil. Furthermore, elevated pH readings, presumably resulting from ammonification of the soil, were observed in areas of high decomposition. The negative control samples proved significantly different from nearly all samples collected within the facility, the exceptions being total carbon content and extractable DNA. These findings indicate that while landscape samples inside may be similar to themselves, they are dissimilar to those taken in a similar temperate forest biome with no recorded history of human decomposition.
田纳西大学人类学研究设施(ARF)以其在法医科学领域作为人类分解研究场所的独特贡献而闻名。在 ARF 进行的研究对于我们理解人类分解过程至关重要。因此,作者对连续的人类分解对土壤环境的长期影响感兴趣。从 ARF 内部和外部采集的土壤样本,通过脂质结合磷和总提取 DNA 来评估其水分含量、pH 值、有机含量、总碳氮含量和生物量。分析结果表明,设施内各采样区域之间没有显著差异(p<0.05),但显示出总氮、脂磷和水分水平可能呈上升趋势,表明高营养物质可能涌入 ARF 土壤。此外,在高分解区域观察到 pH 值升高,推测是由于土壤氨化所致。阴性对照样本与设施内采集的几乎所有样本都有显著差异,除了总碳含量和可提取 DNA。这些发现表明,虽然内部的景观样本可能与自身相似,但与那些在没有记录的人类分解史的类似温带森林生物群落中采集的样本不同。