University of Arkansas, 330 Old Main, Department of Anthropology, Fayetteville, AR 72701, United States.
Forensic Sci Int. 2010 Oct 10;202(1-3):e49-52. doi: 10.1016/j.forsciint.2010.02.024. Epub 2010 Mar 19.
An increasing number of anthropological decomposition studies are utilizing accumulated degree days (ADD) to quantify and estimate the post-mortem interval (PMI) at given decompositional stages, or the number of ADD required for certain events, such as tooth exfoliation, to occur. This study addresses the utility of retroactively applying temperature data from the closest National Weather Service (NWS) station to these calculations as prescribed in the past. Hourly temperature readings were collected for 154 days at a research site in Farmington, AR between June 30 and December 25, 2008. These were converted to average daily temperatures by calculating the mean of the 24 hourly values, following the NWS reporting procedure. These data were compared to comparable data from the Owl Creek and Drake Field NWS stations, the two closest to the research site, located 5.7 and 9.9km away, respectively. Paired samples t-tests between the research site and each of the NWS stations show significant differences between the average daily temperature data collected at the research station, and both Owl Creek (2.0°C, p<0.001) and Drake Field (0.6°C, p<0.001). When applied to a simulated recovery effort, the further NWS station also proved to represent the better model for the recovery site. Using a published equation for estimating post-mortem interval using ADD and total body decomposition scores (Megyesi et al., 2005 [1]), the Drake Field data produced estimates of PMI more closely mirroring those of the research site than did Owl Creek. This demonstrates that instead of automatically choosing the nearest NWS station, care must be taken when choosing an NWS station for retroactively gathering temperature data for application of PMI estimation techniques using accumulated degree days to ensure the station adequately reflects temperature conditions at the recovery site.
越来越多的人类学尸体分解研究利用积日温度(ADD)来量化和估计特定分解阶段的死后间隔(PMI),或发生某些事件(如牙齿脱落)所需的 ADD 数量。本研究探讨了过去规定的将最近的国家气象局(NWS)站的温度数据 retroactive 应用于这些计算的效用。2008 年 6 月 30 日至 12 月 25 日,在阿肯色州法明顿的一个研究地点收集了 154 天的每小时温度读数。这些读数通过计算 24 小时值的平均值转换为平均日温度,遵循 NWS 报告程序。将这些数据与 Owl Creek 和 Drake Field NWS 站的可比数据进行比较,这两个站是离研究地点最近的两个站,分别相距 5.7 和 9.9 公里。研究地点与每个 NWS 站之间的配对样本 t 检验显示,研究地点采集的平均日温度数据与 Owl Creek(2.0°C,p<0.001)和 Drake Field(0.6°C,p<0.001)之间存在显著差异。当应用于模拟恢复工作时,进一步的 NWS 站也被证明是恢复地点的更好模型。利用 Megyesi 等人(2005 [1])发表的使用 ADD 和全身分解评分估计死后间隔的方程,Drake Field 数据产生的 PMI 估计值更接近研究地点的估计值,而不是 Owl Creek。这表明,在使用积日温度法估算 PMI 时,不能自动选择最近的 NWS 站,而应在选择用于收集温度数据以应用 PMI 估算技术的 NWS 站时格外小心,以确保该站充分反映恢复地点的温度条件。