Fancher J P, Aitkenhead-Peterson J A, Farris T, Mix K, Schwab A P, Wescott D J, Hamilton M D
Department of Anthropology, Texas State University, San Marcos, TX 78666, United States.
Department of Soil and Crop Sciences, Texas A&M University, College Station, TX 77843, United States.
Forensic Sci Int. 2017 Oct;279:130-139. doi: 10.1016/j.forsciint.2017.08.002. Epub 2017 Aug 18.
Soil samples from the Forensic Anthropology Research Facility (FARF) at Texas State University, San Marcos, TX, were analyzed for multiple soil characteristics from cadaver decomposition islands to a depth of 5centimeters (cm) from 63 human decomposition sites, as well as depths up to 15cm in a subset of 11 of the cadaver decomposition islands plus control soils. Postmortem interval (PMI) of the cadaver decomposition islands ranged from 6 to 1752 days. Some soil chemistry, including nitrate-N (NO-N), ammonium-N (NH-N), and dissolved inorganic carbon (DIC), peaked at early PMI values and their concentrations at 0-5cm returned to near control values over time likely due to translocation down the soil profile. Other soil chemistry, including dissolved organic carbon (DOC), dissolved organic nitrogen (DON), orthophosphate-P (PO-P), sodium (Na), and potassium (K), remained higher than the control soil up to a PMI of 1752days postmortem. The body mass index (BMI) of the cadaver appeared to have some effect on the cadaver decomposition island chemistry. To estimate PMI using soil chemistry, backward, stepwise multiple regression analysis was used with PMI as the dependent variable and soil chemistry, body mass index (BMI) and physical soil characteristics such as saturated hydraulic conductivity as independent variables. Measures of soil parameters derived from predator and microbial mediated decomposition of human remains shows promise in estimating PMI to within 365days for a period up to nearly five years. This persistent change in soil chemistry extends the ability to estimate PMI beyond the traditionally utilized methods of entomology and taphonomy in support of medical-legal investigations, humanitarian recovery efforts, and criminal and civil cases.
对得克萨斯州立大学圣马科斯分校法医人类学研究设施(FARF)的土壤样本进行了分析,这些样本取自63个人体分解地点的尸体分解岛,深度达5厘米(cm),在11个尸体分解岛的子集中以及对照土壤中深度达15cm。尸体分解岛的死后间隔(PMI)为6至1752天。一些土壤化学指标,包括硝态氮(NO-N)、铵态氮(NH-N)和溶解无机碳(DIC),在PMI早期值时达到峰值,随着时间推移,它们在0-5cm处的浓度恢复到接近对照值,这可能是由于向下层土壤迁移所致。其他土壤化学指标,包括溶解有机碳(DOC)、溶解有机氮(DON)、正磷酸盐-P(PO-P)、钠(Na)和钾(K),在死后PMI长达1752天时仍高于对照土壤。尸体的体重指数(BMI)似乎对尸体分解岛的化学性质有一定影响。为了利用土壤化学指标估计PMI,采用向后逐步多元回归分析,将PMI作为因变量,土壤化学指标、体重指数(BMI)以及饱和导水率等物理土壤特性作为自变量。从人类遗骸的捕食者和微生物介导分解中得出的土壤参数测量值显示,在长达近五年的时间内,有望将PMI估计在365天以内。土壤化学性质的这种持续变化扩展了估计PMI的能力,超越了传统使用的昆虫学和埋藏学方法,以支持法医调查、人道主义恢复工作以及刑事和民事案件。