Utilization of Fluorescent Microspheres and a Green Fluorescent Protein-Marked Strain for Assessment of Microbiological Contamination of Permafrost and Ground Ice Core Samples from the Canadian High Arctic

Fluorescent microspheres were applied in a novel fashion during subsurface drilling of permafrost and ground ice in the Canadian High Arctic to monitor the exogenous microbiological contamination of core samples obtained during the drilling process. Prior to each drill run, a concentrated fluorescent microsphere (0.5-μm diameter) solution was applied to the interior surfaces of the drill bit, core catcher, and core tube and allowed to dry. Macroscopic examination in the field demonstrated reliable transfer of the microspheres to core samples, while detailed microscopic examination revealed penetration levels of less than 1 cm from the core exterior. To monitor for microbial contamination during downstream processing of the permafrost and ground ice cores, a Pseudomonas strain expressing the green fluorescent protein (GFP) was painted on the core exterior prior to processing. Contamination of the processed core interiors with the GFP-expressing strain was not detected by culturing the samples or by PCR to detect the gfp marker gene. These methodologies were quick, were easy to apply, and should help to monitor the exogenous microbiological contamination of pristine permafrost and ground ice samples for downstream culture-dependent and culture-independent microbial analyses.     

Molecular analysis of bacterial diversity in kerosene-based drilling fluid from the deep ice borehole at Vostok, East Antarctica

Decontamination of ice cores is a critical issue in phylogenetic studies of glacial ice and subglacial lakes. At the Vostok drill site, a total of 3650 m of ice core have now been obtained from the East Antarctic ice sheet. The ice core surface is coated with a hard-to-remove film of impure drilling fluid comprising a mixture of aliphatic and aromatic hydrocarbons and foranes. In the present study we used 16S rRNA gene sequencing to analyze the bacterial content of the Vostok drilling fluid sampled from four depths in the borehole. Six phylotypes were identified in three of four samples studied. The two dominant phylotypes recovered from the deepest (3400 and 3600 m) and comparatively warm (-10 degrees C and -6 degrees C, respectively) borehole horizons were from within the genus Sphingomonas, a well-known degrader of polyaromatic hydrocarbons. The remaining phylotypes encountered in all samples proved to be human- or soil-associated bacteria and were presumed to be drilling fluid contaminants of rare occurrence. The results obtained indicate the persistence of bacteria in extremely cold, hydrocarbon-rich environments. They show the potential for contamination of ice and subglacial water samples during lake exploration, and the need to develop a microbiological database of drilling fluid findings.     

Utilization of Drilling Fluid Base Oil Hydrocarbons by Microorganisms Isolated from Diesel-Polluted Soil

Hydrocarbon-degrading microorganisms identified as Pseudomonas luteola, Pseudomonas alcaligenes, Pseudomonas aeruginosa, and Actinomyces sp. were isolated from diesel oil-polluted soils using an enrichment culture technique. The isolates grew luxuriantly on hydrocarbons, including crude oil, diesel, kerosene, engine oil, cyclohexane, and dodecanol. Naphthalene and pyrene were poorly utilized, while there was no growth on benzene. The organisms utilized drilling fluid base oil as the sole source of carbon and energy, with rapid exponential growth at a rate ranging from 0.015 to 0.094 h^?1. The concomitant doubling time was between 7.4 and 45.5 h. Gas chromatographic analyses of the culture revealed reduction in the height of the n-alkane peaks, confirming biodegradation of the compounds. Among the isolates, P. alcaligenes had the highest (99.4%) percentage hydrocarbon degradation. Remarkable (99.2% and 98.7%) hydrocarbon removal was also noted for P. luteola and P. aeruginosa, while the lowest (92.3%) value was recorded in Actinomyces sp. These bacteria with high degradative capacity for hydrocarbons in oil-based drilling fluids would be useful in bioremediation of a tropical environment, polluted with spent drilling mud and drill cuttings.     

Penetration of fluorescent microspheres into the NEEM (North Eemian) Greenland ice core to assess the probability of microbial contamination

The validation of microbiological results from non-aseptically drilled deep ice cores is challenging because exogenous microbial cells can be transported into the core interior and compromise the existing microbial populations. The NEEM (North Eemian) ice core in Greenland provided a first-time opportunity to use fluorescent microspheres as tracers for assessing potential microbial contamination of glacial ice. We developed specific procedures to coat the surfaces of selected NEEM core samples representing bubbly (93–100 m), brittle (633–644 m) and clathrated (1,730 and 2,050 m) ice with melamine-based carboxylated fluorescent microspheres and tracked periodically their penetration into the core interior for 2.5 years using flow cytometry. Sufficient ice surface coating was achieved by immersing retrieved cores in plastic bags containing suspensions of pre-counted 1- and 10-μm microspheres or by down-hole microsphere deployment in plastic sleeves attached to the drill barrel and liberated during drilling. We examined the relationship between microspheres penetration and ice core depth, structure and time after coating. One consistent observation for all cores (except the brittle ice) was that removing a few millimeters of the outer layer drastically reduced microsphere counts, independent of timing, indicating that penetration was mostly limited to the surface layers. Any deeper penetration was found to be microsphere size dependent. The brittle ice showed significant microsphere penetration possibly due to microfractures. Overall, the use of fluorescent microspheres as tracers and microbial surrogates proved to be a sensitive approach for testing potential contamination during deep core projects.     

A Primer on the Offshore Contract Drilling Industry

Mobile offshore drilling units (MODUs) are specialized marine vessels used to drill subsea wells to find and produce hydrocarbons. The contract drilling industry is critical to the offshore oil and gas supply chain, and market dynamics are an important factor in the costs to drill an offshore well. In this article, an introduction to the industry is provided with an emphasis on the factors that influence rig day rates and market structure.     

Investigation of the potential for microbial contamination of deep granitic aquifers during drilling using 16S rRNA gene sequencing and culturing methods

Total number of bacteria, viable counts of aerobic and anaerobic heterotrophic bacteria and 16S rRNA gene diversity were investigated during drilling of three boreholes in the walls of the Äspö hard rock laboratory tunnel, at depths ranging from 380 to 446 m below sea level. Water samples were taken from the drill water source, the drilling equipment and from the drilled boreholes. The drill water was kept under nitrogen atmosphere and all equipment was steam cleaned before the start of a new drilling. Total and viable counts of bacteria in the drilled boreholes were several orders of magnitude lower than in the samples from the drilling equipment, except for sulphate reducing bacteria. A total of 158 16S rRNA genes that were cloned from the drill water source, the drilling equipment and the drilled boreholes were partially sequenced. The drilled boreholes generally had a 16S rRNA diversity that differed from what was found in samples from the drilling equipment. Several of the sequences obtained could be identified on genus level as one of the genera Acinetobacter, Methylophilus, Pseudomonas and Shewanella. In conclusion, the tubing used for drill water supply constituted a source of bacterial contamination to the rest of the drilling equipment and the boreholes. The results show, using molecular and culturing methods, that although large numbers of contaminating bacteria were introduced to the boreholes during drilling, they did not establish in the borehole groundwater at detectable levels.     

驯化复合微生物菌群处理废弃钻井泥浆活性研究

【背景】油田废弃钻井泥浆含油量高,污染物复杂,环境危害严重,现有技术无法满足日益发展的石油开采行业在废弃钻井泥浆处理方面的需求。生物法处理废弃钻井泥浆,工艺简单,成本低,但也存在局限,包括广谱性差、处理周期长、原油降解率低、泥浆性质波动冲击工艺稳定性等。【目的】构建一种高活性和高环境耐受能力的微生物菌群,分析遗传稳定性和综合性能,提高废弃钻井泥浆处理技术水平。【方法】通过定向富集、诱导驯化的方法,提高活性群落对石油烃乳化降解效率,降低共代谢底物反馈抑制和群体感应系统敏感度,分析群落结构和活性成员的种群类别,分析乳化降解石油烃的活性对应关系。【结果】从含油量超过12g/kg、芳烃-胶质沥青含量超过80%、含盐量超过8g/kg的钻井废弃泥浆中富集得到1个活性微生物菌群,主要成员包括假单胞菌属(Pseudomonas)、根瘤菌属(Rhizobium)、红细菌属(Rhodobacter)和嗜碱还原硫素杆菌(Dethiobacter alkaliphilus),比例分别达27.44%、20.73%、8.54%和7.93%。在超过22代的连续驯化过程中,假单胞菌(Pseudomonas)、类希瓦氏菌(Alishewanella)和盐单胞菌(Halomonas)数量达92.72%,菌群结构和活性趋于稳定。处理钻井废弃泥浆5 d,土壤含油率由处理前的12403 mg/kg降低到处理后的42 mg/kg,综合脱油效率99.67%,石油烃降解率68.9%。分析微生物群落作用前后石油饱和土壤中的石油含量变化,原始含油量261 g/kg,处理后含油量305 mg/kg,脱油率99.88%。【结论】菌群驯化后活性稳定,耐受高盐环境能力强,在钻井废弃泥浆、含油土壤及油泥污染物处理方面具有很强的工业应用潜力。     

Biodegradation of Petroleum Hydrocarbons in a Soil Polluted Sample by Oil-Based Drilling Cuttings

Microbial degradation of hydrocarbons in soils polluted by oil-based drilling mud and cuttings has been investigated by static methods such as composting or biopiling. Bioremediation of polluted soils by oil-based drilling cuttings through a slurry bioreactor has not previously been reported. The main aim of this work is to monitor hydrocarbon biodegradation in slurry of drilling cuttings and unpolluted soils and the effects of nutrients on it. Indigenous, bacterial-mixed culture isolated from a polluted soil by drilling cuttings adapted to drilling mud concentrations up to 15% (v/v) was done during a 15-month program. The total petroleum hydrocarbons’ (TPHs) removal efficiency in C/N/P 100/5/1 ratio was 90.5 and 79.85% under experimental and control conditions, respectively. The microbial count on the first day, 15 × 10⁷ CFUg^?1, reached 20 × 10⁹ CFUg^?1on the twenty-first day at experimental conditions. The TPH removal efficiency in C/N/P 100/10/2 was 92.5 and 82.25% at experiment and control, respectively. Increasing nitrogen and phosphorous amount couldn't increase microbial count in comparison with C/N/P ratio 100/5/1. The measured biomass contents and microbial counts in experiments were significantly higher than the control and confirmed hydrocarbons’ biodegradation during the time. Results showed that slurry bioreactors could accelerate the biodegradation of TPHs and reduce remediation time in soil polluted by oil-based drilling cuttings.     

Evaluation of deep subsurface sampling procedures using serendipitous microbial contaminants as tracer organisms

Surface microbiological investigations are critically dependent on the procedures used to collect samples for study. It can be difficult to distinguish between indigenous organisms and those encountered as contaminants during the drilling process. We found that coliform bacteria contaminated drilling mud slurries. These bacteria proved useful as tracer organisms in evaluating the degree of microbial contamination accidentally encountered while drilling for subterranean samples. While these organisms were found in high numbers in both the circulating muds and in the mud reservoir, few subsurface samples harbored conforms. Subsurface slurries did not inhibit the growth of a known coliform inoculum. These results indicate that the methods used to collect and field‐process cores from Atlantic coastal plain sediments were sufficient to prevent a large degree of bacterial contamination in most samples. The microflora in drilling fluids did not quantitatively or qualitatively account for the number and diversity of bacteria in subsurface samples. We conclude that a large and viable bacterial community is present in deep regions of the terrestrial subsurface.     

Microbiological Assessment of Circulation Mud Fluids During the First Operation of Riser Drilling by the Deep-Earth Research Vessel Chikyu

Quality assurance and control (QA/QC) is significant for the scientific drilling in order to accurately characterize physical, geochemical, and biological properties in the cored deep subseafloor materials. To explore the deep subseafloor life and its biosphere, identification and control of microbial contamination in drilling cores is critical for highly sensitive molecular analyses as well as cultivations, especially for the evaluation of low biomass and/or extremely harsh deep environments. Here we report some microbiological characteristics of circulation mud fluids before and after the first riser drilling operation by the newly constructed deep-earth research vessel Chikyu. During the Chikyu shakedown expedition CK06-06 in 2006, we used the riser system for drilling 547 to 647 meter below the seafloor into the sediments offshore the Shimokita Peninsula of Japan. Cultivation experiments showed that no microbial growth was observed in the precirculation mud fluid, while 4 × 10⁵ colonies per 1 ml were observed in the postcirculation mud fluid; all cultured bacterial isolates were found to be Halomonas. Using culture-independent molecular analysis, 16S rRNA gene sequences of Xanthomonas, which is used for industrial production of the mud fluid viscosifier “xanthan gum”, were predominantly detected in the precirculation mud fluid, while Halomonas sequences consistently dominated the clone library constructed from the postcirculation mud fluid. Archaeal 16S rRNA genes were amplified only from the postcirculation mud fluid; these archaeal clone sequences were affiliated to the Marine Crenarchaeota Group I (MGI), Marine Euryarchaeota Group II (MGII), Miscellaneous Crenarchaeotic Group (MCG), South African Gold Mine Euryarchaeotic Group (SAGMEG), Soil Group, and Methanococcus aeolicus. These results suggest that Halomonas contaminated and grew in the tank of circulation mud fluids, and other indigenous deep subseafloor microbial components, especially deep subsurface archaea, were also mixed into the post-circulation mud fluid.     

Force and torque modelling of drilling simulation for orthopaedic surgery

The advent of haptic simulation systems for orthopaedic surgery procedures has provided surgeons with an excellent tool for training and preoperative planning purposes. This is especially true for procedures involving the drilling of bone, which require a great amount of adroitness and experience due to difficulties arising from vibration and drill bit breakage. One of the potential difficulties with the drilling of bone is the lack of consistent material evacuation from the drill's flutes as the material tends to clog. This clogging leads to significant increases in force and torque experienced by the surgeon. Clogging was observed for feed rates greater than 0.5 mm/s and spindle speeds less than 2500 rpm. The drilling simulation systems that have been created to date do not address the issue of drill flute clogging. This paper presents force and torque prediction models that account for this phenomenon. The two coefficients of friction required by these models were determined via a set of calibration experiments. The accuracy of both models was evaluated by an additional set of validation experiments resulting in average R² regression correlation values of 0.9546 and 0.9209 for the force and torque prediction models, respectively. The resulting models can be adopted by haptic simulation systems to provide a more realistic tactile output.     

Effects of drill cuttings on biogeochemical fluxes and macrobenthos of marine sediments

Experimental work was performed on drill cuttings sampled from off-shore drilling operations. The cuttings contained remnants of two different types of drilling muds: a water-ilmenite based mud and an olefin-barite based mud. In a pilot experiment, a gradient of up to 65 mm thick layers of water-ilmenite based cuttings were added to 78 cm² core samples. In another set-up, 3 mm layers of water-ilmenite and olefin-barite based cuttings were added to replicate 1000 cm² box-core samples with natural benthic communities transferred from the Oslofjord, S.E. Norway. Boxes with no addition and addition of 3 mm “clean” sediment were used for control. Increased consumption of oxygen and nitrate indicated the presence of degradable organic phases in both mud systems. The release of silicate showed a general decrease with increasing thickness of the cuttings layer, but maximum rates in the 3.1 mm treatment indicated increased bioturbation at low and moderate doses. The initial (field) composition of the macrobenthic communities was maintained throughout the 3 months experimental period, and at community level, no significant difference was observed between the four treatments at the end of the exposure period. However, after grouping the treatments into “clean” (untreated control and 3 mm clean sediment) and “cuttings” (3 mm water-ilmenite and 3 mm olefin-barite based cuttings), multivariate statistical analyses revealed a significant difference in community composition between clean and cuttings treatments, and three taxa showed significantly reduced abundances in the cuttings treatments. Chemical toxicity of mud components is assumed to be small, and the observed effect was more likely a result of physical properties such as the size or shape of cuttings particles.     

Effects of sedimentation from water-based drill cuttings and natural sediment on benthic macrofaunal community structure and ecosystem processes

In this study, we aim at investigating the role of physical disturbance in effects of water-based drill cuttings on benthic ecosystems. Today, most of the cuttings discharged from oil and gas installations contain water-based drilling muds, rather than oil-based or synthetic muds. Drill cuttings with water-based muds are assumed to cause only marginal effects on the benthos, mainly resulting from sedimentation. However, this statement has not been experimentally tested, which is the purpose of the present work. Natural sediment particles and water-based drill cuttings were added to benthic communities in layer thicknesses of 3-24 mm in a mesocosm set-up. During the following 6 months, changes in benthic community structure and fluxes of oxygen and nutrients across the sediment water interface were studied. There was a significant reduction in number of taxa, abundance, biomass and diversity of macrofauna with increasing thickness of drill cuttings, which was not observed for the natural sediment particles. The drill cuttings also influenced oxygen consumption and oxygen penetration depth in the sediment, and it was concluded that an organic compound in the drill cuttings initiated a typical eutrophication response. Fluxes of phosphate and silicate were, however, similarly affected by the two types of particles, and maximum fluxes occurred in sediments treated with thin layers (3-6 mm) of particles. As the response of water-based drill cuttings in the present study was a result of factors other than physical disturbance, we recommend a reconsideration of the assumption that water-based drill cuttings only cause sedimentation (burial) effects.     

Operationally determined chemical speciation of barium and chromium in drilling fluid wastes by sequential extraction

ABSTRACT

A study has been conducted to determine the influence of pH on the speciation and distribution of barium and chromium in drilling mud. Samples in equilibrium under controlled conditions were subjected to sequential extraction procedure to fractionate the heavy metals into the designated forms of exchangeable, adsorbed, organically bound, carbonate and residual phases. This provides an insight into the potential availability of the heavy metals for possible release into groundwaters and/or surface waters. The major portion of both the metals studied was found in the carbonate and residual forms with the relative distribution depending on the pH. Generally, decreasing pH caused a shift from the residual form towards the carbonate or organic forms of metals. The occurrence of metals in more stable organic, carbonate and residual forms in drilling mud, coupled with no significant release to the aqueous phase upon varying the pH indicates the resistance of these metals to remobilisation from drilling mud.     

Response of Microorganisms to an Accidental Gasoline Spillage in an Arctic Freshwater Ecosystem

The response of microorganisms to an accidental spillage of 55,000 gallons of leaded gasoline into an Arctic freshwater lake was studied. Shifts in microbial populations were detected after the spillage, reflecting the migration pattern of the gasoline, enrichment for hydrocarbon utilizers, and selection for leaded-gasoline-tolerant microorganisms. Ratios of gasoline-tolerant/utilizing heterotrophs to “total” heterotrophs were found to be a sensitive indicator of the degree of hydrocarbon contamination. Respiration rates were elevated in the highly contaminated area, but did not reflect differences between moderately and lightly contaminated areas. Hydrocarbon biodegradation potential experiments showed that indigenous microorganisms could extensively convert hydrocarbons to CO₂. In situ measurement of gasoline degradation showed that, if untreated, sediment samples retained significant amounts of gasoline hydrocarbons including “volatile components” at the time the lake froze for the winter. Nutrient addition and bacterial inoculation resulted in enhanced biodegradative losses, significantly reducing the amount of residual hydrocarbons. Enhanced biodegradation, however, resulted in the appearance of compounds not detected in the gasoline. Since the contaminated lake serves as a drinking water supply, treatment to enhance microbial removal of much of the remaining gasoline still may be advisable.     

Paraformaldehyde-Resistant Starch-Fermenting Bacteria in “Starch-Base” Drilling Mud

Starch-fermenting bacteria were found in each of 12 samples of nonfermenting starch-base drilling mud examined. Of the 12 samples, 3 contained very active starch-fermenting gram-positive spore-bearing bacilli closely resembling Bacillus subtilis. Similar active starch-fermenting bacteria were found in fermenting starch-base drilling mud and in corn starch and slough water used to prepare such mud. The active starch-fermenting microorganisms completely hydrolyzed 1% (w/v) corn starch within 24 hr at 37.5 C. The active starch-fermenting bacteria isolated from fermenting drilling mud were capable of surviving 12 hr of continuous exposure to 0.1% (w/w) paraformaldehyde or 1 hr of continuous exposure to 0.5% (w/w) paraformaldehyde, with no diminution in starch-fermenting ability. The same organisms fermented starch after 3 hr of continuous exposure to 0.5% (w/w) paraformaldehyde, but not after 4 hr of exposure. The phenomenon of rapid disappearance of paraformaldehyde from fermenting drilling mud was observed in the laboratory using a modified sodium sulfite test. Paraformaldehyde, initially present in a concentration of 0.192 lb per barrel of mud, completely disappeared in 9 hr at 22 to 23 C. A significant decrease in paraformaldehyde concentration was detected 0.5 hr after preparation of the mud. It is suggested that the presence of relatively high concentrations of ammonia and chloride in the mud may facilitate the disappearance of paraformaldehyde. The failure of 0.1% (w/w) paraformaldehyde to inhibit the strong starch-fermenting microorganisms isolated from fermenting drilling mud, and the rapid disappearance of paraformaldehyde from the mud, explains the fermentation of starch which occurred in this mud, despite the addition of paraformaldehyde.     

颅骨自动钻孔技术探析

头骨钻孔为脑部微创手术的重要步骤,现有钻孔设备多采朋手动方式,钻孔设备没有任何判断钻穿的装置,钻穿骨头后停止钻进完全靠医生的经验来实现。介绍了国内外该领域的研究现状与存在问题,提出了一种颅骨钻穿自动停刀的判断方法,提出了颅骨自动钻孔技术未来发展的趋势。     

Hydrocarbons obtained by pyrolysis of some precambrian rocks of minnesota

Drill core samples of 42 Precambrian sedimentary, igneous, and metamorphic rocks were analyzed by heating under partial vacuum at 100°C and at 400°C to release hydrocarbons and other volatile products.The core samples yielded methane in amounts ranging from traces to 3 microliters per gram, but averaged much less. By way of comparison, samples of Middle Devonian Marcellus black shale, from Pennsylvania, yielded methane in amounts up to 7ul/g.Other straight chain hydrocarbons up to C₁₁ were found in the volatile products, especially those obtained at 400°C, and benzene was a common product, also mainly in the 400°C experiments. Carbon dioxide and nitrogen appear to form a large part of the nonhydrocarbon volatiles in at least some of the samples.Spectral data indicate that the straight chain pyrolysis products of the Precambrian rocks are mainly alkenes, whereas those of the Devonian rocks, referred to above, are a mixture of alkanes and alkenes. Alkanes were however, obtained from several algae-bearing Middle Precambrian argillites. Available evidence indicates, although not conclusively, that the alkenes were contained in the rock rather than being produced from alkanes during pyrolysis.The writers believe that surface contamination in most of the drill cores was minimal owing to the low permeability of the rocks studied, and that contamination by drilling was also minimal.There is a reasonable possibility that the volatiles, if not formed from kerogen residues by the pyrolysis experiments, are in part juvenile igneous gases or are substances that were distilled out of the deeperlying rocks during intervals of folding and metamorphism, and subsequently accumulated at higher levels.     

UAF radiorespirometric protocol for assessing hydrocarbon mineralization potential in environmental samples

Following the EXXOn Valdez oil spill, a radiorespirometric protocol was developed at the University of Alaska Fairbanks (UAF) to assess the potential for microorganisms in coastal waters and sediments to degrade hydrocarbons. The use of bioremediation to assist in oil spill cleanup operations required microbial bioassays to establish that addition of nitrogen and phosphorus would enhance biodegradation. A technique assessing 1-¹⁴C-n-hexadecane mineralization in seawater or nutrient rich sediment suspensions was used for both of these measurements. Hydrocarbon-degradation potentials were determined by measuring mineralization associated with sediment microorganisms in sediment suspended in sterilized seawater and/or marine Bushnell-Haas broth. Production of ¹⁴CO₂ and CO₂ was easily detectable during the first 48 hours with added hexadecane levels ranging from 10 to 500 mg/l of suspension and dependent on the biomass of hydrocarbon degraders, the hydrocarbon-oxidation potential of the biomass and nutrient availability. In addition to assessment of the hydrocarbon-degrading potential of environmental samples, the radiorespirometric procedure, and concomitant measurement of microbial biomass, has utility as an indicator of hydrocarbon contamination of soils, aqueous sediments and water, and can also be used to evaluate the effectiveness of bioremediation treatments.     

Trends in Basalt and Sediment Core Contamination During IODP Expedition 301

Perfluorocarbon tracers (PFTs) are used during cruises of the Ocean Drilling Program (ODP) and Integrated Ocean Program (IODP) to measure sample contamination with drilling fluid. Drilling fluid is supplied with a constant PFT concentration that can then be detected and quantified in sediment and basalt core samples. During IODP Expedition 301, we used washing (2×) and flaming to effectively remove PFT from the exterior of basalt rocks. Near-complete removal from the exterior allowed us to demonstrate that the interior of basalts was only minutely, if at all, contaminated with drilling fluid. We examined horizontal and vertical trends in sediment core contamination. Contamination decreased greatly between the core exterior to halfway along the core radius, and slightly from halfway to the center of cores, and was generally very low in halfway and center portions. Clay cores were, on average, more contaminated than cores with fine sand. Contamination was typically highest in the two uppermost sections (sections 1 and 2) and lower below (sections 3–5). There was no relationship between depth of core origin and contamination. To determine mechanisms of contamination in halfway and interior parts of cores, we estimated the diffusive flux of PFT from the core liner towards the core center. Based on conservative estimates, we concluded that diffusion did not account for any of the PFT measured in halfway and interior parts of cores in this study. Any measurable PFT concentrations in halfway and center parts of cores were caused by advection.