ITS4.2/BG1.12 | Scientific investigation applied to geological evidence and environment: the contribution of Earth and Natural Sciences in Forensic and Human-Environmental Interaction issues
EDI
Scientific investigation applied to geological evidence and environment: the contribution of Earth and Natural Sciences in Forensic and Human-Environmental Interaction issues
Co-organized by NH10
Convener: Roberta Somma | Co-conveners: Udo Zimmermann, Jason H. Byrd, Sebastiano Ettore Spoto, Luca Trombino
Orals
| Mon, 24 Apr, 14:00–15:45 (CEST)
 
Room 0.94/95
Posters on site
| Attendance Mon, 24 Apr, 16:15–18:00 (CEST)
 
Hall A
Posters virtual
| Attendance Mon, 24 Apr, 16:15–18:00 (CEST)
 
vHall BG
Orals |
Mon, 14:00
Mon, 16:15
Mon, 16:15
The use of geological evidence may help the judicial system to solve cases of homicides, corpse concealments, hit-and-run accidents, kidnappings, sexual assaults, geohazard problematics, environmental damages, animal maltreatment, wildlife crimes, gemstone and fossil frauds. Forensic geologists may be supported by a team of experts during the scientific investigation.
Earth and Natural Sciences may be simultaneously involved in a holistic approach for analyzing inorganic, anthropogenic, and organic materials found on the outdoor crime scenes. These sciences may also be devoted to environmental issues due to the human-environmental interactions responsible for crucial human-driven changes in the Anthropocene and hazards in which biodiversity, climate, and public health and safety are at stake.
Different analytical methods aim to obtain information on the compatibility degree among unknown and known samples and the possible provenance.
Based on the above, different experts may collaborate with geologists and investigate geological evidence and environmental issues, together in research teams. Geologists approaching forensic geology need to master sedimentology, micropaleontology, physical geology, petrography, gemology, geochemistry, hydrogeology, soil sciences, geomorphology, stratigraphy, regional geology, remote sensing, and applied geology and geophysics. Botanists address their investigation in forensic botany by studying plant ecology, vegetal anatomy, systematics, palynology, algology, and plant DNA in soil/sediment. On the other hand, entomologists approach forensic entomology by studying chemistry, biology, human/animal health, molecular science, and animal DNA in soil/sediment.
We encourage submission of studies presenting new insights derived from different inter-disciplinary- and transdisciplinary perspectives, including earth, natural, and environmental sciences (geology, geophysics, geochemistry, ecology, geological medicine, botany, entomology, ecology, and climatology applied to the Anthropocene Epoch), legal medicine, geological medicine. Particular attention will be given to the following topics: comparative analyses; reconstruction of walking in crime scenes; search for clandestine graves; geographical profiling; gemstone frauds; pollutants in groundwaters and soil matrices and environmental forensics; ecological and human health risks.

Orals: Mon, 24 Apr | Room 0.94/95

Chairpersons: Roberta Somma, Marina Morabito, Sebastiano Ettore Spoto
14:00–14:10
14:10–14:20
|
EGU23-5269
|
ECS
|
solicited
|
Highlight
|
Virtual presentation
Ádám Nádudvari, Mariola Jabłońska, and Monika Fabiańska

During coal mining, an enormous amount of economically not used humic or sapropelic coals, coal shales are deposited as wastes nearby the coal mines in urbanised areas, e.g. Upper Silesia, Katowice – Rybnik Industrial Region, in Upper Silesian Coal Basin, Poland. These wastes start to oxidise or lose out weathering immediately; in the worst cases, they will undergo self-heating. During exothermic reactions, the heavy metals contained in these rocks, especially sulfur compounds of  Pb, Cd, Cr, Cu, Zn, Ni, Hg, As are mobilised to the environment due to their high volatility at elevated temperatures and due to low pH levels (2 – 4) occurring on the dumps (Nádudvari et al., 2021, 2022). Amongst them, the Hg mobilisation and enrichment make such coal waste dumps more dangerous. Nádudvari et al. (2021, 2022) reported >1000 mg/kg enrichment of Hg in crusts of expelled bitumen and in gases from thermally affected wastes Hg concentration reached ~100 times higher than in polluted urban air from Upper Silesia. Additionally, the MeHg formation - Methylmercury (10 – 30 μg/kg) was also significant and probably formed via chemical reactions. Furthermore, other toxic gases emitted from the vents like benzene, formaldehyde, NH3, HCl, H2S, CO, Cl2, NH3, SO2, and NO were detected, and many of their average annual concentrations exceeded numerous times the permissible Polish norms limits (Nádudvari et al., 2022). The formation of PAHs – Polycyclic Aromatic Hydrocarbons is also very common due to the burning processes, therefore, the lifetime cancer risks due to PAHs and heavy metals accumulations in the dumps are significant. Thus access to these dumps should be prohibited (Nádudvari et al., 2021). Abundant phenols are typical products of self-heating dumps, and their occurrence shows the coking conditions inside the dumps (Nádudvari et al., 2020). The potential ecological and human health risks of these dumps are moderate to very high due to the significant influence of the high Hg concentrations (Nádudvari et al., 2022).

How to cite: Nádudvari, Á., Jabłońska, M., and Fabiańska, M.: Environmental issues of self-heating coal waste dumps in Poland, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5269, https://doi.org/10.5194/egusphere-egu23-5269, 2023.

14:20–14:30
|
EGU23-5737
|
Virtual presentation
|
Monika Fabiańska, Ewa Szram, Dariusz Więcław, Magdalena Misz-Kennan, and Justyna Ciesielczuk

            Spontaneous heating of coal waste rocks stored within the dumps is the worldwide phenomenon. It occurs in oxygen-deficient conditions that can be well simulated by hydrous pyrolysis. The process leads to production of new, relatively well water soluble compounds. They should be considered a hazard to the aquatic systems, both to the surface and groundwater since many older coal waste dumps are not isolated from below. However, the amounts of water soluble compounds produced and their fingerprint are not well recognized. In this project we aimed to identify types of compounds produced using hydrous pyrolysis as laboratory simulation of self-heating carried out in controlled conditions. This will allow for identification of distribution patterns of self-heating-produced compounds also in natural waters.

            Four mudstones from two coal mines, the Janina (subbituminous) and Marcel (bituminous) (Upper Silesia Coal Basin, Poland) were selected for hydrous pyrolysis. The experiments were conducted in 1-liter reactors (Parr Co.) in temperatures 250, 360, and 400oC during 72 h. the procedure details are presented by Lewan et al. (2008). Amount of water added ranged from 200-380 mL. Dissolved organic compounds were isolated using solid phase extraction on C18 PolarPlus columns (BAKERBOND, 3g). Compounds were eluted with dichloromethane (HPLC grade). The compositions of SPE extracts was investigated with an Agilent 6890 gas chromatograph coupled with an Agilent Technology 5973 mass spectrometer.

            Hydrous pyrolysis released compounds such as phenols, carboxylic acids, aldehydes, and ketones, including numerous aromatic ketones and quinones, and S-heterocyclic compounds such as dibenzothiophenes. Phenolic derivatives, dominating in pyrolytic water phase (up to 60% of the total extract composition), comprised compounds from phenol (C0) to C4 phenols. The minimal temperature of phenol release, caused by the macromolecule cracking, was 360oC. Water phase from 250oC pyrolysis contained phenols in minor amounts only, and vitrinite, the main source of them, was not changed. The general composition of organic phase at this temperature corresponds to water leachates of Upper Silesia coal.

            Thus the major hazard to the aquatic environment is sites in coal waste dumps with self-heating temperature exceeding 250oC and compounds indicating this pollution origin are phenols with cresols and xylenols domination in the distribution.

 

Acknowledgements

The financial support of the National Science Centre, grant No 2017/27/B/ST10/00680 is gratefully acknowledged.

Lewan, M.D., Kotarba, M.J., Więcław, D., Piestrzyński, A., 2008. Evaluating transition-metal catalysis in gas generation from the Permian Kupferschiefer by hydrous pyrolysis. Geochim. Cosmochim. Acta 72, 4069-4093.

How to cite: Fabiańska, M., Szram, E., Więcław, D., Misz-Kennan, M., and Ciesielczuk, J.: Self-heating-generated compounds release to water phase simulated by hydrous pyrolysis, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5737, https://doi.org/10.5194/egusphere-egu23-5737, 2023.

14:30–14:40
|
EGU23-1336
|
On-site presentation
Marina Morabito and Roberta Somma

Contrarily to land plants, which display complex anatomical features useful in diagnostics, algae are problematic to identify at the species level. Taxonomic identifications classically are focused on morphological observations at the light microscopy, but current research showed extensive phenotypic plasticity and cryptic diversity resulting in different phylogenetic assemblages. Modern taxonomic approaches also include ultrastructural (SEM and/or TEM), phylogenetic and phylogenomics information, all methodologies that may be expensive and need the involvement of skilled experts. In criminal investigations, such methodologies may not be always applicable by the judicial system because of the costs, and morphological identification of algae at the light microscope is usually the standard method. Consequently, scientific data coming from algae are often neglected in forensic investigations, with the notable exceptions of the diatoms in drowning victims.

This research deals with a traditional morphological investigation on the detection and identification of soil microalgae in a case of disappearance. The method was useful in forensic investigations to associate control samples from the scene of the events to detected traces of unknown origin found on the victims.

Morphological characteristics (shape, size, color, taking into consideration the different state of conservation of the algae) and cellular characteristics (wall, unicellular, colonial, multicellular organization) were observed at the light microscopy.  Where species identification was not achievable with certainty, the smallest identifiable taxonomic level was recorded. A comparison of identified morphotypes as well as of the peculiar associations of taxonomic entities was made between sample of unknown origin to those of known origin and was used to evaluate similarity degree.

Observations of microalgae, in association with other geological (shape, size, color, composition of mineral grains) and botanical (shape, size, color of leaves and seeds) analyses, allowed investigators to: i) associate the walking of a person under investigation in specific sites of the scene of the events; ii) exclude that the bodies of two victims were submerged under water; iii) exclude the contact of any surface of the persons’ belongings, other than the soles of their shoes, with water basins of any kind.

The present investigation proved how a traditional light microscopic approach could be decisive to associate field samples to detected traces, basing on the identification of associations of morpho-types of microalgae.

How to cite: Morabito, M. and Somma, R.: May light microscopy observations of algae play a significative role in forensic investigations of soils?, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-1336, https://doi.org/10.5194/egusphere-egu23-1336, 2023.

14:40–14:50
|
EGU23-6763
|
On-site presentation
francesco paolo buonocunto, alfonsa milia, matilda mali, santina giandomenico, antonella di leo, lucia spada, luciana ferraro, and laura giordano

In areas characterized by geologic variability and high demographic pressure, seafloor sediment characteristics and the study of contaminants are important to reconstruct the origin and pathway of both contaminants and the sediments from source to sink.

The area off-shore the alluvial Sarno plain (Naples Bay, Eastern Tyrrhenian Sea) is bounded by the Vesuvius volcano in the northern part and by the carbonates relief of the Sorrento Peninsula in the southern part, and it is affected by metals contamination due the outflow of industrial vast.

A Geochemical and physical parameters of the sediments were analysed along a transect moving from the coast until the 100 m of water depth with the aim to explore how the onshore documented contamination affect the offshore counterpart. Surface sediment samples collected from the offshore Sarno plain, were analysed for grain size, nutrients (TOC, TN, TP) and heavy metals (Hg, Cd, As, Cr, Ni, Cu, Zn, and Pb) to evaluate the contamination status, and processed using multivariate statistical analysis. A sediment survey along the transect has been used to evaluate: 1) the relative influences of parent lithology and anthropogenic effects offshore the Sarno river; and 2) the extension of the influence of the river in the submarine area.

Four clusters are identified through PCA analysis: 1) the first resulted associated to the presence of As and Fe, low TOC content and prevalence of sandy fraction reflecting a geogenic contribution from Vesuvius Plan; 2) the second mainly include Cr, Cu, Zn, Pb and partially Cd and Hg, high TOC content and finest granulometry, reflecting the influence of the Sarno River discharges in the marine area; 3) the third include a variability in the Mn, Fe and TOC content. This area might reflect the Sorrento-Peninsula influence; 4) the forth include samples of the distal area in which a low contamination rate is displayed and irregular Hg and Cd pattern are verified, probably due to diffuse contamination origin and other coupling factors

Results indicate that 1) the area offshore Vesuvius displays physical and geochemical association mainly related to the natural origin of volcanoclastic sediments; 2) in the central area, the association of contaminants suggests their anthropogenic origin from the Sarno Plain, whereas the distal area, characterized by low rate of contamination, are mainly influenced by sediment from Sorrento Peninsula. Finally based on the contaminant and nutrient distribution it is possible to individuate the distribution of terrigenous sediments and organic matter of the Sarno delta deposits. The results show that the river should account as one of the main contribution sources of anthropogenic contaminants.  Some metals contamination anthropogenic in origin and TOC in general decreased gradually with distance from the coast and in particular is limited to the area of deposition of the river discharge.

Individuation of several marine sector with different geochemical associations permitted the reconstruction of source to sink contaminants pathway on the continental shelf.

How to cite: buonocunto, F. P., milia, A., mali, M., giandomenico, S., di leo, A., spada, L., ferraro, L., and giordano, L.: Contaminants in continental shelf sediments, a way to reconstruct a source to sink pathway (Naples Bay, Italy), EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6763, https://doi.org/10.5194/egusphere-egu23-6763, 2023.

14:50–15:00
|
EGU23-2692
|
Highlight
|
On-site presentation
Stefan Dekker, Poornima Nagesh, Oreane Edelenbosch, Hugo de Boer, Hermine Mitter, and Detlef P. van Vuuren

Pesticide use is a crucial human-driven change in the Anthropocene that negatively impacts the environment and ecosystems. While pesticides are essential to agriculture to sustain crop production and ensure global food security, they also lead to significant environmental impacts. The export of pesticides after application from the agricultural fields threatens the soil, groundwater and surface water quality in many world regions. Pesticide use is constantly increasing globally, driven mainly by agricultural intensification, despite stricter regulations and higher pesticide effectiveness. To enhance the understanding of future pesticide use and emissions and make informed farm-to-policy decisions, we developed Pesticide Agricultural Shared Socio-Economic Pathways (Pest-Agri-SSPs) in six steps. The Pest-Agri-SSPs are based on an extensive literature review and expert knowledge, considering significant climate and socio-economic drivers from farm to continental scale in combination with multiple actors impacting them. In the literature, pesticide use is associated with farmer behaviour and agricultural practices, pest damage, technique and efficiency of pesticide application, agricultural policy and demand for agricultural products. Here, we developed Pest-Agri-SSPs upon this understanding of pesticide use drivers and relating them to plausible sectoral developments, as described by the Shared Socio-economic Pathways for European agriculture and food systems (Eur-Agri-SSPs).

The Pest-Agri-SSPs present European pesticide use in five scenarios with low to high challenges to climate change adaptation and mitigation up to 2050. The most sustainable scenario (Pest-Agri-SSP1) shows a decrease in pesticide use owing to sustainable agricultural practices, technological advances and a pro-environmental orientation of agricultural policies. On the contrary, the Pest-Agri-SSP3 and Pest-Agri-SSP4 show an increase in pesticide use resulting from high challenges from pest pressure, resource depletion and relaxed agricultural policies. Pest-Agri-SSP2 presents a stabilised pesticide use resulting from strict policies and slow transitions by farmers to sustainable agricultural practices. Pest-Agri-SSP5 shows a decrease in pesticide use for most drivers, influenced mainly by rapid technological development and the application of sustainable agricultural practices. However, Pest-Agri-SSP5 also shows a relatively low rise in pesticide use driven by agricultural demand, production, and climate change. Our results highlight the need for a holistic approach to tackle pesticide use and emissions, considering the identified drivers and future developments. The storylines and qualitative assessment provide a platform to make quantitative assumptions for numerical modelling and evaluating policy targets.

Keywords: Farm characteristics, pest damage, technology, policy, socioeconomic, agriculture and food systems

Adapted version of this work has been submitted to Journal of Environmental Management: Nagesh P, Edelenbosch OY , Dekker SC, de Boer HJ, Mitter H, van Vuuren DP. Pesticide use under the influence of socio-economic and climate change: Pest-Agri-SSPs

 

 

How to cite: Dekker, S., Nagesh, P., Edelenbosch, O., de Boer, H., Mitter, H., and van Vuuren, D. P.: Pesticide use under the influence of socio-economic and climate change: Pest-Agri-SSPs, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-2692, https://doi.org/10.5194/egusphere-egu23-2692, 2023.

15:00–15:20
|
EGU23-4120
|
solicited
|
Highlight
|
On-site presentation
Alessandro Gargini and Maria Filippini

One pillar of the protection of groundwater established by the EU legislation is the “polluter pays principle”. Following this principle, the costs for the remediation of contaminated sites must be in charge of the responsible of the environmental crime. Compound Specific Isotope Analysis (CSIA), also known as “isotopic fingerprinting”, is a robust tool to apportion the source of groundwater contamination and eventually the polluter. The isotopic composition of the contaminant molecule may reflect the production process of a compound or the origin of the raw materials used in the production. Here we present the effective and decisive application of isotopic fingerprinting of carbon stable isotopes in the molecule of chlorinated hydrocarbons (chlorinated ethenes PCE-Perchloroethylene and TCE-Trichloroethylene) for the source apportionment in two contaminated sites in Italy, namely Ferrara (Emilia-Romagna region, Northern Italy) and Bussi sul Tirino (Abruzzo region, Central Italy). In both cases, industrial wastes from a production of chloromethanes, using methane and chlorine, were disposed illegally in unlined dumps resulting in a severe contamination of groundwater. The companies responsible for the contamination are different in the two sites but the production process is the same, resulting in a similar isotopic signature of the wastes. In both cases, the isotopic fingerprinting was critical to identify the chlorometane production as the source of contamination among other possible sources, despite two different hydrogeological settings (a large alluvial plain in the Ferrara site and a narrow valley with macroclastic alluvial deposits and travertines in the Bussi site). In both cases, PCE and TCE showed strongly depleted values of δ13C (isotopic ratio of the fraction of 13C respect to 12C isotopes of carbon) ranging between  -87 and -65‰ for PCE and between -79 and -64‰ for TCE. The very depleted isotopic values are related to the use of methane in the production process instead of coal, this last one being commonly adopted in the synthesis of PCE and TCE for commercial use (e.g. for laundry of textiles or metal degreasing). The groundwater contamination in the two sites had serious implications in terms of sanitary risk due to vapour intrusion into residential buildings (Ferrara site) or water ingestion by local citizens (Bussi site) from a public water supply well field site serving about 300.000 inhabitants and affected for more than 20 years by the contamination (from the opening in 1984 to the decomissioning in 2007). In both cases, complex legal issues arose either below penal or civil jurisdiction and the isotopic fingerprinting was used as the most relevant proof in order to identify the polluters.

How to cite: Gargini, A. and Filippini, M.: Isotopic fingerprinting as an effective tool for polluter apportionment in environmental crimes involving groundwater, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-4120, https://doi.org/10.5194/egusphere-egu23-4120, 2023.

15:20–15:30
|
EGU23-8174
|
ECS
|
Highlight
|
On-site presentation
Diana Hatzenbühler, Michael Weißl, Christian Baumgartner, and Michael Wagreich

The Anthropocene, the strongly debated potential new unit of the Geological Time Scale, describes the intensified anthropogenic influence on the environment and geological processes, and its traces in geological archives. Regional studies characterizing the growth of human impact, the Anthropocene transformation, are scarce, especially for urban or per-urban environments.

In this project, we investigate the anthropogenic impact of the metropolis Vienna on its peri-urban environment and the proposed beginning of the Anthropocene epoch in the 1950s CE by applying sedimentological and geochemical methods. In previous studies (Wagreich et al. 2022), the authors were able to successfully detect the human influence in urban sedimentary archives of Vienna (anthropogenic coarse sediments) using artificial isotopes and anthropogenic trace metals. For our project, we extend the study area from Vienna to the city of Hainburg to investigate Vienna’s anthropogenic impact in both anthropogenic and natural sediments downstream the Danube river. In this area, direct human intervention in the environment, such as ground excavations, backfill and damming, is highly variable, from locally strong (e.g., hydro-power dams, airport constructions), to not existing (National Park Donau-Auen), thus offering a suitable location to trace and quantify the extent of anthropogenic impact.

Within petrographic facies, sedimentological and geochemical markers are applied to characterize the anthropogenic strata in this area: The archive of fine-grained natural Danube deposits, i.e. erosional profiles and sediment cores, is analysed for trace metals, artificial radiogenic isotopes, and microplastics with the aim (i) to disentangle the anthropogenic fingerprint of Vienna from the sediment, (ii) to identify and evaluate the proposed Anthropocene geological boundary around 1950 CE, and (iii) to evaluate a potential correlative stratigraphic reference section section/ point for the Anthropocene downstream of Vienna. Finally, the Carnuntum-Vienna Anthropocene field lab offers the opportunity to integrate environmental systems modelling with an Anthropocene equation approach for the temporal and spatial growth of the anthropogenic layers (iv).           

How to cite: Hatzenbühler, D., Weißl, M., Baumgartner, C., and Wagreich, M.: Searching for the bomb spike in Danube river sediments: Extracting the anthropogenic impact of Vienna, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-8174, https://doi.org/10.5194/egusphere-egu23-8174, 2023.

15:30–15:45

Posters on site: Mon, 24 Apr, 16:15–18:00 | Hall A

Chairperson: Rosanna Maniscalco
Introduction
A.208
|
EGU23-13026
|
ECS
|
Highlight
Sebastiano Ettore Spoto

Forensic Gemmology is a branch of Forensic Science where the analysis of gemstones has legal implications, which cannot be set aside, improvised, or, even worse, done with approximation. Local and world markets and archaeological sites can currently encounter a wide range of gemmological objects that are incorrectly declared, treated, or classified. Materials in question are made by also using the latest technologies. Occasionally, cases are brought to court regarding the value of a precious gem in addition to its "authenticity," which often, to be resolved, require complex preparation. Therefore, keeping in mind the significance of gemstone identification, here are specific methodologies discussed to test the authenticity of the gemstones and to find out whether the gemstones are authentic or not. Modern challenges also concern determining whether gemstones were extracted under ethical conditions and determining whether gemstones are of synthetic or natural origins. Thus, forensic examination of gemstones becomes very difficult if proper procedures are not outlaid. The problems that need to be addressed at the international level remain relevant, for instance, creating a standard scheme for determining the ethical origin of colored gemstones, similar to the one existing in the diamond market.

How to cite: Spoto, S. E.: Old and modern challenges of Forensic Gemmology, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13026, https://doi.org/10.5194/egusphere-egu23-13026, 2023.

A.209
|
EGU23-20
Roberta Somma

In criminal cases of clandestine homicide graves, the criminal behavior and mental map of an offender may be influenced by several geographical, botanical, and geological features. Among these factors, diggability assumes for a concealer a predominating role in the concealment act because an easy and efficient digging of a hole requires that the ground is diggable. The diggability (the ease and efficiency with which soils and sediments may be dug and reinstated in a grave) may vary from very easy to difficult, and forensic geologists may qualitatively and relatively evaluate it by using a T-metal bar for offensive and defensive search purposes. Results of a diggability survey were processed in the GIS platform, reconstructing contour maps, Inverse Distance Weighting, Kriging, and Thin Plate Spline with Tension maps of a crime scene. The interpolation of the data by Thin Plate Spline with Tension rendered the best results. The diggability survey demonstrated that the pit fell in a suitable area for concealment, being one of the easiest diggable and thick sectors of the search area.

How to cite: Somma, R.: Diggability field survey for the assessment of the most suitable site for a clandestine homicide grave, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-20, https://doi.org/10.5194/egusphere-egu23-20, 2023.

A.210
|
EGU23-5477
|
ECS
Ewa Szram, Marta Kondracka, Monika Fabiańska, and Leszek Marynowski

Land reclamation is a significant environmental and economic issue. Nowadays, there is a need to restore industrial areas to a state as close to nature as possible. Therefore, it is essential to monitor the condition of soils in a quick and non-invasive way. In southern Poland, the mining industry led to the creation of diverse waste dumps like post-mining waste, tailings from flotation, or Zn-Pb wash waste dumps. The research area covers the industrial waste dumps in Olkusz, Bytom and Piekary Śląskie. For the study, soil samples were taken from 1 m soil pits to determine the migration of pollutants into the soil profile. Additionally, waste dumps contacting the soils were sampled (from 0.5 m deep pits). The total organic carbon and sulphur were determined using Eltra Elemental Analyser CS530, while the composition of the total extracts was analyzed using Agilent gas chromatograph 7890A, with a DB-5 column coupled with a mass spectrometer 5975 C XL MDS. The total concentration of trace elements was determined using atomic absorption spectrometry in an acetylene-air flame (Analyst 400, Perkin Elmer). The ERT measurements were performed using LUND electrical imaging system with SAS 4000 Terrameter produced by ABEM Malå (Guideline Geo).

The samples contain av. 3.7 wt. % TOC and 0.4 wt. % TS. In GC-MS chromatograms, the Bytom and Piekary Śląskie samples show a higher PAHs abundance than the Olkusz samples. In soil profiles near waste dumps, a higher abundance of PAHs was found not only in the surface layer but also in samples to 0.75 m depth. In soil profiles away from the landfill, a higher abundance of PAHs was found only to 0.5 m depth. The PAHs abundance was decreased below 0.5 m depth, and even some of the PAHs weren't found. The high PAHs abundance even at a depth of up to 1m was observed in soil profiles under a waste layer. In samples, the concentrations of trace elements are higher than the limit values (Cd 1.1 to 135.7, Pb 17 to 12407 and Zn 19 to 28903 mg/kg). Soil contamination and its spatial diversity with trace elements in the mining area can be successfully located and studied using ERT measurements. The impact of soil pollution was observed on the geoelectric cross-sections in the form of reduced electrical resistivity associated with an elevated trace element content compared to the unpolluted area. The differentiation of the electrical resistivity was related in particular to the sites of surface runoff from the waste dump. The sediment washed out from the waste dump changed the physical characteristics of the soil and lowered the electrical resistivity of the native geology. The results suggest that the trace elements and toxic organic compounds in wastes are mobilised by surface runoff and the infiltration of rainwater into the ground.

Acknowledgements

The financial support of the National Science Centre, grant No 2017/27/B/ST10/00680 is gratefully acknowledged.

Presentation preference: poster on-site in Vienna

 

 

How to cite: Szram, E., Kondracka, M., Fabiańska, M., and Marynowski, L.: Soil degradation caused by post-mining and post-metallurgical waste - detection using gas chromatography–mass spectrometry (GC-MS) and electrical resistivity tomography (ERT), EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5477, https://doi.org/10.5194/egusphere-egu23-5477, 2023.

A.211
|
EGU23-6304
Fabio Mondello, Marina Morabito, and Roberta Somma

In the 1978, Gianni Lombardi and Valerio Giacomini, two Italian experts in forensic geology and botany, respectively, were involved by the judicial authority for analysing the sands and plant remains found in the clothing and moccasins of the honorable Aldo Moro, kidnapped and killed by terrorists. Experts had to determine the site where this material transfer occurred.

As demonstrated by the analyses carried out by these experts, plant taxonomists can give useful information in forensic analyses especially for events occurring outdoor. Small plant traces spread in quantity, like pollens, spores, thorns, seeds and small fruits, may easily transfer to the clothing and footwear of people or to the same human body, moving outdoor in the countryside.

In 2020, 42 years later, the authors of this research were involved by the judicial systems to reconstruct the events related to the disappearance of two persons, in the Sicilian countryside, found cadavers a few days after in a site near the last sighting of them.

The research focused on the morphological description of thorns, other pointed structures, and seeds produced by plants thriving in the scene of events. For simplicity, it was chosen to use the generic term "thorns" to indicate pointed plant structures, although aware that the term "prickle" should have been used for epidermal structures, “thorns” strictly for stem-derived structures, and "spines" for other structures derived from leaves, petioles or stipules.

A photographic atlas of thorns and seeds was produced with the species found in the scene of the events. A comprehensive description of plants as they appeared in situ as well as of their thorny appendices was made, and explanatory pictures were captured, both in situ and under the stereoscopic microscope in the laboratory. The extensive biometric analysis made on thorns and seeds of all collected species in the scene of events was recorded.

Soil traces and microtraces of forensic samples of unknown origin (from the victims’ bodies and their belongings) were investigated for the presence of thorns or thorn fragments and seeds, which were then compared with those recorded in the atlas.

The organic component (vegetal elements) of the forensic geological traces from victims and their belongings was predominant in quantity over the inorganic one.

Comparative observations allowed to identify hundreds of thorns and thorn fragments and several hundreds of seeds found on the clothes and footwear of both victims, as plants thriving in the area under investigations. Basing on the punctual distribution of individual plants, the analysis of thorn traces and seeds was useful, together with geological analyses on sands and clay minerals, in reconstructing the path of the victims in the hours immediately preceding their death and, therefore, provided valuable information to the investigating authorities.

How to cite: Mondello, F., Morabito, M., and Somma, R.: Holistic approach in the forensic analysis of geological trace evidence: as Forensic Botanists and Geologists may help judicial investigations , EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6304, https://doi.org/10.5194/egusphere-egu23-6304, 2023.

A.212
|
EGU23-8782
Sebastiano D’Amico, Jason H Byrd, Emanuele Colica, Saviour Formosa, Roberta Somma, Giulia Tagliabue, and Luca Trombino

The search for homicide graves is a very strenuous activity that may lead to the identification of the burial site if it is planned based on articulated scientific approaches considering several aspects of forensic sciences. Moreover, another difficult task in such criminal cases may be the estimation of the Post-Mortem Interval (PMI) of the victim. Discrepancies between PMI estimation through entomological studies and other evaluations may be. This inconsistency is at the base of the necessity to examine and well understand the human decay process of human beings and the decay consequences in the surrounding environmental context. It is noteworthy that several processes may occur on the surrounding site the burial. Phenomena as a depression, a different growth of plants, or the occurrence of peculiar insect associations may be observed on the grave, due to the body’s decay, and the body fluids release in the underground. These aspects may be analysed in experimental fields where pig carcasses, usually used as analogues for the human cadavers, are inhumated in holes dug by means of hand instruments (pick and shovel) or mechanical excavators. These sites may be monitored by applying geological, geophysical, geochemical, and geomatic methods, as well as entomological and botanical characterization of the insects and flora, respectively. The present research is devoted to plan, analyse and monitoring of a simulated experimental field in Malta, where a simulated grave containing a pig carcass will be prepared. The research project is dedicated to geophysical and geomatic surveys to be realized before the excavations and during the project for monitoring the depression development and the shape and dimensions of the leachate plume. Geophysical methods consist of ERT tomographies, seismic and georadar profiles, parallel and orthogonal to the graves. Geological investigations are focused on characterizing the pedogenic profile and the composition, texture, and structure of the soil/sediment. Entomological research is devoted to identifying insect species typically related to body decay. Ideally and in addition to the above, botanical surveys are aimed at defining the main species and differences in the plant growth. The reconstructed evolution of the burial environment may be investigated to better assist criminal investigations into the definition of the PMI in recognition of a burial site and other significative criminological and criminalistic data.

How to cite: D’Amico, S., Byrd, J. H., Colica, E., Formosa, S., Somma, R., Tagliabue, G., and Trombino, L.: Forensic geosciences investigations on experimental fields, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-8782, https://doi.org/10.5194/egusphere-egu23-8782, 2023.

Discussion

Posters virtual: Mon, 24 Apr, 16:15–18:00 | vHall BG

Chairpersons: Roberta Somma, Marina Morabito, Sebastiano Ettore Spoto
Introduction
vBG.4
|
EGU23-5500
Francesco Crea, Chiara Alessandrello, Francesco Parello, Roberta Somma, and Sebastiano Ettore Spoto

In Forensic Geology, Environmental Forensics is devoted to ascertaining contaminants in the soil/subsoil, surface waters, and groundwaters. In such cases, forensic geologists usually accomplish activities concerning geological, hydrogeological, geochemical, and geophysical research to individuate the source of the contaminant substance and discover if this latter depends on anthropogenic or natural origins.

Preliminary chemical data on groundwaters from some areas of the Peloritani Mountains showed anomalous high contents of fluoride F-, a halogen element in the atmosphere, sea, fresh waters, and minerals. Natural sources of fluoride in the groundwaters are volcanic gas, the sea, and minerals. Fluoride is an essential component in around 300 minerals, among which the most diffused are fluorite and fluorapatite. A significant chemical feature of the ions of fluoride is that they have the same charge as the hydroxyl group OH- and present an ionic radius very similar to OH-. These chemical characteristics make it possible that F- may readily substitute the hydroxyl group in minerals such as micas, X2Y4-6Z8O20(OH,F)4.

Most of the collected groundwaters in the present research were hosted in aquifers formed by Variscan high-grade metamorphic rocks provided with fracture permeability and in aquifers made up of Tertiary to Quaternary siliciclastic deposits with porosity permeability. These aquifers have a silicate composition and are rich in biotite. Among micas, biotite is the most diffused mafic mineral in the high-medium grade metamorphic rocks (augen gneiss, gneiss, mica schists) of the Peloritani Mountains. This mineral is also widespread in weathered monomineralic lithoclasts of siliciclastic deposits (Miocene, middle to upper Pleistocene, Holocene to Actual clastic deposits) deriving from dismantling the chain's metamorphic rocks.

Previous studies on biotite from acid plutonic rocks of India demonstrated that fluoride contents might reach a concentration up to 7 wt%. Biotite mica may be likely responsible for the natural fluoride contamination of some of the studied groundwaters, in some cases also commercially exploited in the past.

WHO suggests that the F- concentration in the drinking waters must range between 700 and 1500 µg/l depending on the different climatic zones. Concentrations over 1500 µg/l in Italian drinking waters are prohibited and dangerous for public health.

The present research carried out in the Peloritani Mountains is devoted to: i) defining the actual geographical extent of the identified F- anomaly; ii) studying the water/rock interactions to ascertain if the leaching of F- from biotite mica, present in the high-grade metamorphic rocks and siliciclastic deposits, may be the natural phenomenon responsible for the ascertained fluoride contamination; iii) search for possible other causes of F- contamination as the salt wedge intrusion in the groundwaters of the coastal areas.

How to cite: Crea, F., Alessandrello, C., Parello, F., Somma, R., and Spoto, S. E.: Find the culprit, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5500, https://doi.org/10.5194/egusphere-egu23-5500, 2023.

vBG.5
|
EGU23-3869
Daniela Sapienza, Gennaro Baldino, Irene Lo Piccolo, Roberta Somma, Elvira Ventura Spagnolo, Cristina Mondello, Patrizia Gualniera, and Alessio Asmundo

The multidisciplinary approach in forensic science led to the development of geology and botany as predictive forensic applications (forensic geology – forensic botany) aimed at analyzing and studying the crime scene for the "solving" of the criminal hypothesis. Over the past fifteen years, the study of plant DNA has been used in forensics science to discriminate the place of origin of plant material found at a crime scene, to identify poisonous vegetable species, as a forensic marker in all cases where determining geographic origin is essential to investigative leads, missing person cases, and intelligence application (Bell et al., 2015), in the identification of Cannabis as support of law authorities in fighting drug abuse and global trafficking. These specific topics to date made it possible to: distinguish a primary crime scene from a secondary one, link a suspect to the crime scene, and determine the date of death. Findings of plant material can be examined through chemical analysis, morphological analysis, DNA analysis, PCR and electrophoresis. Comparative studies may be carried out among the plant remains collected from the victim and suspect and plant sampled on the event scene in order to trace the place where the plant transfer occurred. The analysis of the international literature presented through this review shows the importance of further developments in plant DNA analysis, growing and expanding a global database containing the plant DNA barcode, and implementing specific guidelines for the collection and sampling procedures of forensic samples.

How to cite: Sapienza, D., Baldino, G., Lo Piccolo, I., Somma, R., Ventura Spagnolo, E., Mondello, C., Gualniera, P., and Asmundo, A.: Overview in forensic purpose and application of plant DNA, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-3869, https://doi.org/10.5194/egusphere-egu23-3869, 2023.

vBG.6
|
EGU23-4457
|
ECS
|
Gennaro Baldino, Elvira Ventura Spagnolo, Stefano Vanin, Roberta Somma, Filippo Cucinotta, Cristina Mondello, Patrizia Gualniera, Michele Gaeta, Alessio Asmundo, and Daniela Sapienza

In a forensic context, the criminal case evaluation is often challenging, and the only autopsy may not be exhaustive to determine the cause and the time of death, mainly when the corpse is dismembered, charred, or putrefied. Moreover, the conditions of an altered corpse and the recovered places of the cadaver (countryside, forests, rivers, beaches, etc.), outdoors, or in burnt buildings and ruins, can raise challenges not only in terms of victim identification but also in terms of acquisition of additional information aimed at elucidating the dynamics of death, like the detection of the corpse transfer after the death, especially in cases of suspected homicides. In such complex cases, it is, therefore, of paramount importance to provide a multidisciplinary approach involving the collaboration of ultra-specialized forensic experts. In this context, experts in criminalistic disciplines, such as forensic geology, botany, and entomology, may provide their contribution, as well as the engineers applying to medicine new technologies for the 2D and 3D reconstructions of crime scenes and evidence. We consider helpful to report a court case that came to our attention, involving forensic pathology experts together with forensic biologists, geologists, botanists, naturalists, entomologists, veterinarians, physicists, computer scientists, and engineers whose collaboration based on a multidisciplinary approach contributed to the management and the solving of a suspect crime.

How to cite: Baldino, G., Ventura Spagnolo, E., Vanin, S., Somma, R., Cucinotta, F., Mondello, C., Gualniera, P., Gaeta, M., Asmundo, A., and Sapienza, D.: No chance for doubts: a multidisciplinary approach for solving a criminal case., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-4457, https://doi.org/10.5194/egusphere-egu23-4457, 2023.

vBG.7
|
EGU23-70
Jason Byrd, Daniela Sapienza, Michael Schaer, Adam Stern, Roberta Somma, Lerah Sutton, and Domenico Trombetta

Legal cases involving human and animal envenomizations may be encountered by the medicolegal investigator.  Such cases are often difficult due to lack of physical evidence and analytical difficulty.  The development and use of an interdisciplinary approach and standardized protocol involving experts in environmental and life sciences (toxicology, legal medicine, entomology, veterinary forensic science, biology, geography, geology, and meteorology) may improve the documentation, collection, and presentation of physical evidence in court.  This information can be utilized to develop and optimize new protocols for toxicological screenings for application in human and animal cases.  In such cases, the scientific background of coroners and police experts may not be sufficient to correctively delineate the environmental features of the territory that may be typical of certain species of venomous fauna present in the scene of the events. Therefore, protocols providing complete information concerning the environment of the scene and detail of the events together with exam protocols, sample collection, tissue preservation, and testing/analysis are needed. This holistic approach could enhance the ability to detect toxins involved in envenomizations to better manage forensic science and legal cases. 

 

How to cite: Byrd, J., Sapienza, D., Schaer, M., Stern, A., Somma, R., Sutton, L., and Trombetta, D.: Procedures for the documentation and collection of physical evidence from human and animal envenomization cases., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-70, https://doi.org/10.5194/egusphere-egu23-70, 2023.

vBG.8
|
EGU23-8685
|
ECS
|
Giulia Tagliabue, Cristina Cattaneo, and Luca Trombino

Many studies have shown how Environmental Sciences can contribute to the forensic and medico-legal investigations on murder and body concealment dynamics. Nonetheless, most of the research is generally limited to botanical, entomological and anthropological fields leaving out the observation of the active interaction between a decomposing body and the surrounding environment, such as soil. Indeed, a clandestine grave can destroy the valuable forensic evidence as well as prevent the identification of the offender or the victim itself and even the determination of the post-mortem interval (PMI), post-burial interval (PBI) and, overall, the dynamics of the crime act. Therefore, the present experiment, built on the basis of a previous pioneer project carried out in the same area between 2009 and 2011, will be based on the re-enactment of real cases of body disposal, consisting in a combination of multiple methods of concealment, all of them including the inhumation of the remains in a woodland setting. It will consist of the excavation of 32 burials, all dug on the same day, at a depth between 40 and 60 cm involving just as many piglet cadavers (Sus scrofa) weighing between 3 and 5 kg. They will be divided into four different groups, each of which will undergo peculiar treatments: eight will be buried naked; eight clothed; eight will be buried in quicklime and the last eight will be previously hurt. The experiment will be conducted for a total of 730 days and the exhumations of the specimens will be performed in eight increasing time intervals, to achieve different PBIs for each group of subjects (15, 30, 60, 120, 240, 365, 545 and 730 days). At the time of each exhumation biological material, commodities and soil will be sampled and investigated from a geochemical, microscopic (polarizing microscope) and ultramicroscopic (SEM-EDS) point of view, aiming to underline any evidence of mutual exchange of material between the different substrates, as well as any symptom of disturbance, both biochemical and mechanical. As focusing on a multidisciplinary approach, not only this study will allow to reach a standardization for the right reading of trace evidence in real cases of clandestine burials inquiry, but it also will contribute to draw up some guidelines for the exploitation of the parameters registered by the geopedological analytical techniques, which have been neglected for years in the forensic and medico-legal context.

How to cite: Tagliabue, G., Cattaneo, C., and Trombino, L.: The application of soil analysis in forensic taphonomy: using pigs as analogues for human corpses, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-8685, https://doi.org/10.5194/egusphere-egu23-8685, 2023.

vBG.9
|
EGU23-145
|
ECS
|
Giulia Tagliabue, Anna Masseroli, Mirko Mattia, Carlotta Sala, Elena Belgiovine, Daniele Capuzzo, Gaia Giordano, Paolo Maria Galimberti, Fabrizio Slavazzi, Cristina Cattaneo, and Luca Trombino

Soil is a dynamic matrix that can rapidly respond to disturbance events, such as the death and the subsequent deposition of an organism. Concurrently, it can be considered an archive of evidence due to its ability to record the signals of disturbance events. Such a condition turns the biogeochemical analysis of geopedological samples into a valuable tool for the study of decomposition processes, especially when they are flanked with the examination of the remains. The aim of the present research is to present the unique contextual situation of the Sepolcreto (i.e., burial ground) under the crypt of the ancient Ospedale Maggiore of Milan Ca’ Granda (Italy). The sepulchre hosted an estimated amount of 150000 buried individuals, 10000 of which are still buried in one of the underground chambers, named “chamber O”, and whose remains underwent various type of post-mortem transformative processes, both disruptive and preservative. In this study microscopic and ultramicroscopic analysis have been carried out in order to detect any evidence of material exchange between the bone tissue, from three skeletal remains collected from the “chamber O” of the Sepolcreto, and the surrounding pedosedimentary matrix. The specimens were analysed by the mean of a polarizing microscope and a SEM-EDS, which pointed out the presence of a mutual exchange of material between the two substrates, underlying the intensity of the interaction between organisms (even after their death) and the environment. Finally, this burial context permitted to observe an inedited type of soil, mainly composed of organic matter transformed by thanatological processes, bone tissue fragments and some other evidence of anthropic origin and/or activity. Therefore, it has been considered a new type of anthropogenic soil named “Thanatogenic soil”.

How to cite: Tagliabue, G., Masseroli, A., Mattia, M., Sala, C., Belgiovine, E., Capuzzo, D., Giordano, G., Galimberti, P. M., Slavazzi, F., Cattaneo, C., and Trombino, L.: The unique contextual situation of the Ca’ Granda burial ground: from taphonomic observations towards a new type of anthropogenic soil, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-145, https://doi.org/10.5194/egusphere-egu23-145, 2023.

Discussion