A Multi-Tracer Push-Pull Diagnostic Test for In Situ Air Sparging Systems

This document describes the development and initial application of a multi-tracer push-pull test designed to provide near real-time point-specific measures of contaminant volatilization and aerobic biodegrada-tion rates during in situ air sparging (IAS) operation. Measured biodegradation and volatilization rates are specific to the tracers used, so the results provide relative measures useful for identifying spatial differences in treatment performance and changes in performance with changes in system operation and design. The diagnostic test involves injecting a solution containing multiple tracer compounds into the target treatment zone through a monitoring well, piezometer, or drive point. The injected solution is initially deoxygenated and can contain: (a) a nondegradable, non-volatile conservative tracer, (b) one or more nondegradable, volatile chemicals, (c) an aerobically biodegradable, nonvolatile compound, and (d) a visible dye. After some predetermined hold time, an excess quantity of groundwater is extracted from the same injection point and the change in the concentrations of the tracer compounds is measured. Volatilization and oxygen utilization rates are then estimated from mass balances on the tracer components. The development of this diagnostic tool was conducted in a controlled physical model study and then initial field tests were conducted at the U.S. Navy Hydrocarbon National Test Site (HNTS) in Port Hueneme, California. Spatial variations in oxygenation and volatilization rates were observed, with oxygenation rates varying from 0 to 51 mg-O₂/L-water/d, and tracer volatilization rates varying from 0 to 47%/d. Acetate and sulfur hexafluoride (SF₆) were used as tracers in the initial testing, and it was discovered that these are not ideal choices due to the potential for anaerobic acetate biodegradation and SF₆ partitioning into trapped gas in the aquifer.     

Diagnostic Tools for Integrated In Situ Air Sparging Pilot Tests

In situ air sparging (IAS) pilot test procedures have been developed that provide rapid, on-site information about IAS performance. The standard pilot test consists of six activities conducted to look for indicators of infeasibility and to characterize the air distribution to the extent necessary to make design decisions about IAS well placement. In addition, safety hazards that need to be addressed prior to full-scale design are identified. Two additional pilot test activities are described in those cases where air distribution must be more precisely defined. The test activities include both chemical tests (tracking contaminant concentrations, dissolved oxygen and tracers) and physical tests (air flow rate and injection pressure, groundwater pressure response). Pilot test data from Eielson Air Force Base, Alaska illustrates implementation of the pilot test and interpretation of the data.     

Impact of liquid-to-gas hydrogen mass transfer on substrate conversion efficiency of an upflow anaerobic sludge bed and filter reactor

Efficient anaerobic degradation may be completed only under low levels of dissolved hydrogen in the liquid surrounding the microorganisms. This restraint can be intensified by the limitations of liquid-to-gas H₂ mass transfer, which results in H₂ accumulation in the bulk liquid of the reactor. Dissolved hydrogen proved to be an interesting parameter for reactor monitoring by showing a good correlation with short-chain volatile fatty acid concentration, namely propionate, which was not the case for the H₂ partial pressure. Biogas recycle was performed in a upflow anaerobic sludge bed and filter reactor. The effects of varying the ratio of recycled-to-produced gas from 2:1 (9 l/l reactor per day) to 8:1 (85 l/l reactor per day) were studied. By increasing the liquid—gas interface with biogas recycling, the dissolved hydrogen concentration could be lowered from 1.1 to 0.4 μ . Accordingly, the H₂ sursaturation factor was also reduced, leading to an important improvement of the H₂ mass transfer rate, which reached 20.86 h⁻¹ (±9.79) at a 8:1 gas recycling ratio, compared to 0.72 h⁻¹ (±0.24) for the control experiment. Gas recycling also lowered the propionate concentration from 655 to 288 mg l⁻¹ and improved the soluble chemical oxygen demand removal by 10–15%. The main problem encountered was the shorter solid retention time, which could lead to undesirable biomass washout at high gas recycling ratio. This could be circumvented by improving the reactor design to reduce the turbulence within the biomass bed.     

Selecting Remediation Goals by Assessing the Natural Attenuation Capacity of Groundwater Systems

Remediation goals for the source areas of a chlorinated ethene-contaminated groundwater plume were identified by assessing the natural attenuation capacity of the aquifer system. The redox chemistry of the site indicates that sulfate-reducing (H₂ ∼ 2 nanomoles [nM]) per liter conditions near the contaminant source grade to Fe(III)-reducing conditions (H₂ ∼ 0.5 nM) downgradient of the source. Sulfate-reducing conditions facilitate the initial reduction of perchloroethene (PCE) to trichloroethene (TCE), cis-dichloroethene (cis-DCE), and vinyl chloride (VC). Subsequently, the Fe(III)-reducing conditions drive the oxidation of cis-DCE and VC to carbon dioxide and chloride. This sequence gives the aquifer a substantial capacity for biodegrading chlorinated ethenes. Natural attenuation capacity (the slope of the steady-state contaminant concentration profile along a groundwater flowpath) is a function of biodegradation rates, aquifer dispersive characteristics, and groundwater flow velocity. The natural attenuation capacity at the Kings Bay, Georgia site was assessed by estimating groundwater flowrates (∼0.23±0.12 m/d) and aquifer dispersivity (∼1 m) from hydrologic and scale considerations. Apparent biodegradation rate constants (PCE and TCE ∼0.01 d^-1; cis-DCE and VC ∼0.025 d^-1) were estimated from observed contaminant concentration changes along aquifer flowpaths. A boundary-value problem approach was used to estimate levels to which contaminant concentrations in the source areas must be lowered (by engineered removal), or groundwater flow velocities lowered (by pumping) for the natural attenuation capacity to achieve maximum concentration limits (MCLs) prior to reaching a predetermined regulatory point of compliance.     

Enhancement of radiation-induced apoptosis by 6-formylpterin

Radiation-induced apoptosis and its possible enhancement in the presence of 6-formylpterin (6-FP), a metabolite of folic acid, were examined in human myelomonocytic lymphoma U937 cells. When cells were treated with 6-FP at a nontoxic concentration of 300 μM, and then exposed to X-rays at a dose of 10 Gy, significant enhancement of radiation-induced apoptosis as determined by nuclear morphological change, phosphatidylserine (PS) externalization and DNA fragmentation were observed. Flow cytometry for the detection of intracellular hydrogen peroxide (H₂O₂) revealed that 6-FP increased the formation of intracellular H₂O₂, which further increased when the cells were irradiated. Decrease of mitochondria trans-membrane potential (MMP), release of cytochrome c from mitochondria, and activation of caspase-3 were enhanced after the combined treatment. Remarkable activation of protein kinase C δ (PKC δ) and its translocation from cytosol to mitochondria were detected in combined treatment. Increase of intracellular Ca₂₊ concentrations ([Ca₂₊]i) was also observed, however, neither calpain I nor calpain II could inhibit the apoptosis. In addition, c-Jun NH₂-terminal kinase ( JNK) activation was not enhanced in the combined treatment. A protein involved in a caspase-independent apoptosis pathway, apoptosis inducing factor (AIF), remained unchanged even 3 h after treatment. These results indicate that intracellular H₂O₂ generated by 6-FP enhances radiation-induced apoptosis via the mitochondria-mediated caspase-dependent pathway, with the active involvement of PKC δ.     

Isolated respiring heart mitochondria release reactive oxygen species in states 4 and 3

Isolated mitochondria respiring on physiological substrates, both in state 4 and 3, are reported to be or not to be a source of reactive oxygen species (ROS). The cause of these discrepancies has been investigated. As protein concentration was raised in in vitro assays at 37°C, the rate of H₂O₂ release by rat heart mitochondria supplemented with pyruvate/malate or with succinate (plus rotenone) was shown to increase (0.03-0.15 mg protein/ml), to decrease (0.2-0.5 mg protein/ml) and to be negligible (over 0.5 mg protein/ml). The inhibition of mitochondrial respiration (with rotenone or antimycin A) or the increase in the oxygen concentration dissolved in the assay medium allowed an enhancement of ROS production rate throughout the studied range of protein concentrations. In mitochondria respiring in state 3 on pyruvate/malate or on succinate (plus rotenone), ROS release vanished for protein concentrations over 0.5 or 0.2 mg/ml, respectively. However, ROS production rates measured with low protein concentrations (below 0.1 mg/ml) or in oxygen-enriched media were similar or even slightly higher in the active respiratory state 3 than in the resting state 4 for both substrates. Consequently, these findings indicate that isolated mitochondria, respiring in vitro under conditions of forward electron transport, release ROS with Complex I- and II-linked substrates in the resting condition (state 4) and when energy demand is maximal (state 3), provided that there is sufficient oxygen dissolved in the medium.     

Effect of a nuclepolyhedrovirus of Autographa californica expressing the enhancin gene of Trichoplusia ni granulovirus on T. ni larvae

A recombinant Autographa californica nucleopolyhedrovirus (AcMNPV) strain showing higher virulence against Trichoplusia ni larvae than the wild-type virus was developed. The 'enhancin' (VEF) gene of T. ni granulovirus (TnGV) and the AcMNPV polyhedrin gene were cloned into the baculovirus transfer vector pAcUW31. This plasmid and AcMNPV BacPAK6 DNA were co-transfected into the BTI-Tn5B1-4 cell line. A recombinant AcMNPV strain (BacVEFPol) was purified, amplified, and bioassayed against T. ni first instar larvae. Its estimated LC₅₀ (0.184 OB/mm²) was 2.18 times lower than the LC₅₀ estimated for the wild-type AcMNPV (0.402 OB/mm²). Likewise, an LT₅₀ of 67.7 h was estimated for the recombinant AcMNPV strain while the LT₅₀ of wild-type AcMNPV was estimated at 81.9 h. This indicates a 17.4% reduction of the time required to kill the larvae. The higher virulence of the recombinant strain, evidenced by its LC₅₀ and LT₅₀ values being lower than those of the wild-type strain, indicates that the VEF protein is expressed properly and may be occluded in the OBs.     

Controlled Field Study on the Use of Nitrate and Oxygen for Bioremediation of a Gasoline Source Zone

Controlled releases of unleaded gasoline were used to evaluate the biotransformation of the soluble aromatic hydrocarbons (benzene, toluene, ethylbenzene, xylene isomers, trimethylbenzene isomers, and naphthalene) within a source zone using nitrate and oxygen as electron acceptors. Experiments were performed within two 2 m×2 m×3.5 m deep sheet-piling cells. A gasoline-contaminated zone was created below the water table in each treatment cell. Groundwater amended with electron acceptors was then flushed continuously through the cells for 174 d. One cell received approximately 100 mg/L nitrate and “microaerophilic” (i.e., 2 mg/L or less) dissolved oxygen (DO), a second cell received micro aerophilic DO only. Electron-acceptor utilization and hydrocarbon-metabolite formation were observed in both cells, suggesting that some microbial activity had been induced in response to flushing. However, nitrate utilization was slow relative to the cell residence time, and aromatic-hydrocarbon mass losses in response to microaerophilic DO addition were not apparent under these in situ conditions. Concentration trends in both cells suggested that there was relatively little biotransformation of the aromatic hydrocarbons over the 2-m flow path monitored in this experiment. Extraction-well concentration trends, for example, were consistent with abiotic gasoline dissolution. The results from the nitrate-amended cell suggest that a large denitrifying population capable of aromatic hydrocarbon biotransformation failed to develop within the gasoline source zone over a 14-month period of nitrate exposure. This study reinforces the need for detailed aquifer-specific testing prior to selecting bioremediation for full-scale cleanup, particularly for recent hydrocarbon spills.     

Long-Term Evolution of Biodegradation and Volatilization Rates in a Crude Oil-Contaminated Aquifer

Volatilization and subsequent biodegradation near the water Table make up a coupled natural attenuation pathway that results in significant mass loss of hydrocarbons. Rates of biodegradation and volatilization were documented twice 12 years apart at a crude-oil spill site near Bemidji, Minnesota. Biodegradation rates were determined by calibrating a gas transport model to O₂, CO₂, and CH₄ gas-concentration data in the unsaturated zone. Reaction stoichiometry was assumed in converting O₂ and CO₂ gas-flux estimates to rates of aerobic biodegradation and CH₄ gas-flux estimates to rates of methanogenesis. Model results indicate that the coupled pathway has resulted in significant hydrocarbon mass loss at the site, and it was estimated that approximately 10.52 kg/day were lost in 1985 and 1.99 kg/day in 1997. In 1985 3% of total volatile hydrocarbons diffusing from the floating oil were biodegraded in the lower 1 m of the unsaturated zone and increased to 52% by 1997. Rates of hydrocarbon biodegradation above the center of the floating oil were relatively stable from 1985 to 1997, as the primary metabolic pathway shifted from aerobic to methanogenic biodegradation. Model results indicate that in 1997 biodegradation under methanogenenic conditions represented approximately one-half of total hydrocarbon biodegradation in the lower 1 m of the unsaturated zone. Further downgradient, where substrate concentrations have greatly increased, total biodegradation rates increased by greater than an order of magnitude from 0.04 to 0.43 g/m²-day. It appears that volatilization is the primary mechanism for attenuation in early stages of plume evolution, while biodegradation dominates in later stages.     

Advances in In Situ Air Sparging/Biosparging

In situ air sparging (IAS) is a technology commonly used for treatment of submerged source zones and dissolved groundwater plumes. The acceptance of IAS by regulatory agencies, environmental consultants, and industry is remarkable considering the degree of skepticism initially surrounding the technology in the early 1990s. Much has been learned and reported in the literature since that time, but it appears that practice has changed little. In particular, conventional pilot testing, design, and operation practices reflect a lack of appreciation of the complex phenomena governing IAS performance and the unforgiving nature of this technology. Many systems are poorly monitored and likely to be inefficient or ineffective. Key lessons-learned since the early 1990s are reviewed and their implications for practice are discussed here. Of particular importance are issues related to: (a) the understanding of air flow distributions and the effects of geology and injection flowrate, (b) the need to characterize air flow distributions at the pilot- and field-scale, (c) how changes in operating conditions (e.g., pulsing) can affect performance improvements and reduce equipment costs, and (d) how conventional monitoring approaches are incapable of assessing if systems are performing as designed.     

The chemical microenvironment of the symbiotic planktonic foraminifer Orbulina universa

Microsensor measurements of CO₂, O₂, pH and Ca²⁺ in the vicinity of the symbiont-bearing planktonic foraminifer Orbulina universa showed major light-modulated changes in the chemical microenvironment due to symbiont photosynthesis, respiration of the holobiont, and precipitation of the calcite shell. Under saturating light conditions, microprofiles measured towards the shell surface showed an O₂ increase of up to 220% air saturation, a decrease in CO₂ concentration to 4.9 μM, and a pH increase to 8.8 due to symbiont photosynthesis. The Ca²⁺ concentration decreased to ∼9.6 mM in two specimens, while it increased to 10.2-10.8 mM in three other specimens kept in light. In darkness, the respiration of the community decreased the O₂ concentration to 82% of air saturation, CO₂ increased up to 15 μM, the pH decreased to 8.0, and the Ca²⁺ concentration increased up to 10.4 mM. These data, and derived calculations of the distribution of HCO₃^- and CO₃^2- near the shell, showed that the carbonate system in the vicinity of O. universa was significantly different from conditions in the surrounding seawater, both in light and darkness, due to the metabolism of the foraminifer and its associated algae. Experimental light-dark cycles indicated a sufficient CO₂ supply sustaining high carbon fixation rates of the symbiotic algae via conversion of HCO₃^- or via CO₂ release from calcification and host respiration. Our findings on irradiance-dependent CO₂ and pH changes in the vicinity of symbiont-bearing planktonic foraminifera give direct experimental evidence for the predictions of isotope fractionation models used in palaeoclimatology stating that metabolic processes affect the isotopic carbon signal (δ¹³C) in foraminifera.     

Development of a Microbial Consortium from a Contaminated Soil That Degrades Pentachlorophenol and Wood-Preserving Oil

An indigenous microbial consortium capable of degrading pentachlorophenol (PCP) and petroleum hydrocarbons (C₁₀-C₅₀) was produced from a soil contaminated with wood-preserving oil. Two 10-L stainless steel soil slurry (10% w/v) bioreactors were operated in fed-batch mode. To verify the growth and efficiency of PCP degraders in the presence of other contaminants, one bioreactor was fed with a PCP-based wood-preserving mixture (WPM) and a second reactor was fed with technical-grade NaPCP. During the 90-day period of activation, PCP, C₁₀-C₅₀, Cl^-, pH, and dissolved oxygen levels were monitored. The microbial community was monitored using specific most probably number (MPN) bacterial counts and mineralization tests. PCP degradation rates increased similarly in both reactors, from 19 to 132 mg/L-d in the NaPCP reactor, and from 41 to 112 mg/L-d in the WPM reactor. Contaminant loss calculations showed that 99.5% of PCP and 92.5% of C₁₀-C₅₀ added to the WPM reactor were biodegraded. It also revealed that 83% of polychlorinated dioxins and furans were removed. PCP-degrading bacteria increased from 7×10² to 1.6×10⁶ bacteria/mL in both reactors, and petroleum hydrocarbon degraders increased from 1.7×102 to 3.4×108 bacteria/mL in the WPM reactor, indicating that the activity of PCP degraders was not inhibited by the presence of microorganisms growing on petroleum hydrocarbons.     

Effect of oxygen transfer rate on β-carotene production from synthetic medium by Blakeslea trispora in shake flask culture

The effect of oxygen transfer rate (OTR) on β-carotene production by Blakelsea trispora in shake flask culture was investigated. The results indicated that the concentration of β-carotene (704.1 mg/l) was the highest in culture grown at maximum OTR of 20.5 mmol/(l h). In this case, the percentage of zygospores was over 50.0% of the biomass dry weight. On the other hand, OTR level higher than 20.5 mmol/(l h) was found to be detrimental to cell growth and pigment formation. To elucidate the effect of oxidative stress on β-carotene synthesis, the accumulation of hydrogen peroxide during fermentation under different OTRs was determined. A linear response of β-carotene synthesis to the level of H₂O₂ was observed, indicating that β-carotene synthesis is stimulated by H₂O₂. However, there was an optimal concentration of H₂O₂ (2400 μM) in enhancing β-carotene synthesis. At a higher concentration of H₂O₂, β-carotene decreased significantly due to its toxicity.     

EFFECT OF DISSOLVED OXYGEN PARTIAL PRESSURE ON THE ACCUMULATION OF ASTAXANTHIN IN CHEMOSTAT CULTURES OF HAEMATOCOCCUS LACUSTRIS (CHLOROPHYTA)

The effect of dissolved oxygen partial pressure on the accumulation of astaxanthin in the green alga Haematococcus lacustris ( Gir.) Rostaf (UTEX16) was studied in N-limited continuous chemostat cultures. The steady-state astaxanthin content measured against culture volume, cell number, and biomass dry weigh of Haematococcus cultures was proportional to the dissolved O₂ partial pressure in the culture medium, over the range of 0–50% O₂ The steady-state biomass dry weight concentrations remained at between 0.52 and 0.57 g. L^-1 over the range of dissolved O₂ partial pressure studied. Steady-state cell densities at dissolved O₂ partial pressures above the air saturation level (1.13–1.58 × 10⁵ cells.mL^-1) were about half of that measured at lower dissolved O₂ partial pressures (2.42–2.63 × 10⁵ cells.mL^-1). Both biflagellated zoospores and nonmotile aplanospores were found at steady state. The fraction of nonmotile cells was higher at dissolved O₂ partial pressures above the air saturation level (94.44–98.01%) than at dissolved O₂ partial pressure below the air level (79.64–86.12 and 91.75% ).     

Mitochondrial functions under hypoxic conditions: The steady states of cytochrome c reduction and of energy metabolism

1. The effect of low oxygen concentration on the oxidation-reduction states of cytochrome c and of pyridine nucleotide, on Ca²⁺ uptake, on the energy-linked reduction of pyridine nucleotide by succinate, and on the rate of oxygen consumption have been examined under various metabolic conditions, using pigeon heart mitochondria.

2. The oxygen concentration required to provide half-maximal reduction of cytochrome c (p50_c) ranges from 0.27 to 0.03 μM (0.2-0.02 Torr) depending upon the metabolic activity. There is a linear increase of the p50_c value with increasing respiratory rate.

3. The fraction of the normoxic respiration that is observed at p50_c is 70–90% under State 4 conditions, but is 30% under State 3 conditions.

4. The oxygen requirement for half-maximal reduction of pyridine nucleotide (p50_PN) varies less than p50_c, being 0.08 μM in State 3 and 0.06 μM in the uncoupled state.

5. The ability of the mitochondria to exhibit an energy-linked reduction of pyridine nucleotide by succinate disappears at an oxygen concentration of 0.09 μM (0.06 Torr). Below this oxygen concentration, endogenous Ca²⁺ begins to be released from the mitochondria. Thus, the critical oxygen concentration for bioenergetic function of mitochondria corresponds approximately to 50% reduction of pyridine nucleotide (p50_PN).     

American petroleum institute in situ air sparging database

An evaluation of data detailing in situ air sparging (IAS) systems at 59 sites has been assembled into an American Petroleum Institute in situ Air Sparging Database (API‐IAS Database). The database was developed to provide site managers insights concerning the state‐of‐the‐art of IAS system design, operation, and evaluation. The IAS radius of influence (ROI) is often evaluated based on changes in a number of physical, chemical, or biological monitoring parameters. Measurements of groundwater dissolved oxygen levels was the technique used most often to determine the ROI. Other parameters such as pressure changes in the vadose and saturated zones, groundwater mounding, air bubbling in wells and tracer gases were also used to aid in the determination of the IAS ROI. A review of 37 pilot studies revealed that the IAS ROI is generally between 10 to 26 ft. IAS technology is generally being applied in sandy soils. The application of IAS technology was deemed infeasible at seven sites where soils contained high levels of silts or clay. Analysis of design and operation data at 40 IAS sites revealed that a typical IAS well is 2 in. in diameter, with a 2‐ft screen, positioned 5 to 10 ft beneath the water table. The wells typically were operated at an overpressure (i.e., pressure in excess of that required to overcome the hydrostatic head) of less than 5 psi with a flow rate of less than 5 cfm. At several sites when IAS system pressures and flows were doubled, only slight increases in ROI resulted. Significant reductions of dissolved volatile organic hydrocarbon (VOCs) were observed at 12 sites as a result of IAS. However, long‐term water quality data following an IAS system shutdown was very limited.     

Absorption studies of Photosystem I photochemistry in the absence of vitamin K-1

Flash-induced absorption changes were studied on different timescales (nanosecond to millisecond) and at different temperatures (10 to 278 K) in highly enriched spinach PS I particles lacking vitamin K-1 and in which the electron transfer from the primary acceptor to the secondary acceptors was blocked. At all temperatures, the initial absorption change at 820 nm was followed by a fast decay (t_1/2 ≈ 47 ns at 278 K and ≈ 82 ns at 10 K) which is attributed to the decay of the primary radical pair (P-700⁺-A⁻₀). A slower phase of absorption decay is attributed to the P-700 triplet state, which was formed as a result of the biradical recombination, with a yield of about 30% at 278 K and about 75% at 10 K. Under air, the ³P-700 state decayed with a t_1/2 of about 50 μs at 278 K, whereas in the absence of oxygen it decayed with t_1/2 ≈ 560 μs. At 278 K, this yield was shown to depend on the presence of a magnetic field, with a maximum around 60 G. The ³P-700 decay halftime was nearly independent of temperature in the absence of oxygen (t_1/2 ≈ 1 ms at 10 K). The implications for the mechanisms involved in this decay are discussed. Addition of vitamin K-1 to these particles resulted in a decrease in the amplitude of the fast submicrosecond decay and a concomitant increase in the amplitude of a slow phase, indicating an efficient transfer from A⁻₀ to vitamin K-1. However, most functional properties of the acceptor A₁ were not reconstituted under these conditions.     

Biotransformation of glucose to gluconic acid by Aspergillus niger—study of mass transfer in an airlift bioreactor

A glucose–gluconic acid biotransformation system was suggested for the experimental study of oxygen transfer in bioreactors. This biosystem was used for the investigation of the effect of the flow rate and biomass concentration on the volumetric oxygen transfer coefficient k_La in a 10 dm³ internal-loop airlift bioreactor. For this purpose, the fermentation broth of the mycelial strain Aspergillus niger was employed, representing a three-phase system, where bubbles come into contact with dense rigid pellets. The results showed that the presented biotransformation system can be successfully utilised for the determination of the oxygen transfer rate in airlift bioreactors. The experiments showed a strong positive influence of the air flow rate on the rate (r_Glu), specific rate of gluconic acid production (k_Glu/X) as well as on the volumetric oxygen transfer coefficient (k_La). This confirmed an expected limitation of production rate by the oxygen transport from the gas to the liquid phase in the whole range of air flow rates applied. Moreover, consistent curves of the production rate r_Glu and k_La values vs. biomass concentration c_X (amount of enzymes) were observed. These exhibited a local maximum for c_X equal to 6.68 g dm⁻³. On the other hand, the specific production rate monotonously decreased with increasing biomass concentration. A decline of k_La values at higher c_X values was attributed to a bubble coalescence promoting effect of mycelial pellets.     

Photodynamic activity of a new sensitizer derived from porphyrin-C60 dyad and its biological consequences in a human carcinoma cell line

The photokilling activity of a porphyrin-C₆₀ (P-C₆₀) dyad was evaluated on a Hep-2 human larynx-carcinoma cell line. This study represents the first evaluation of a dyad, with high capacity to form a photoinduced charge-separated state, to act as agent to inactivate cells by photodynamic therapy (PDT). Cell treatment was carried out with 1 μM P-C₆₀ incorporated into liposomal vesicles. No dark cytotoxicity was observed using 1 μM P-C₆₀ concentration and during long incubation time (24 h). The uptake of sensitizer into Hep-2 was studied at different times of incubation. Under these conditions, a value of 1.5 nmol/10⁶ cells was found after 4 h of incubation showing practically no change even after 24 h. The cell survival after irradiation of the cells with visible light was dependent upon light exposure level. A high photocytotoxic effect was observed for P-C₆₀, which inactivated 80% of the cells after 54 J/cm² of irradiation. Moreover, the dyad kept a high photoactivity even under argon atmosphere. Thus, depending on the microenviroment where the sensitizer is localized, this compound could produce a biological photodamage through either a ¹O₂-mediated photoreaction process or a free radical mechanism under low oxygen concentration.

The mechanism of cell death was analyzed by Hoechst-33258, toluidine blue staining, TUNEL and DNA fragmentation. Cell cultures treated for 24 h with P-C₆₀ and irradiated with a dose of 54 J/cm² showed a great amount of apoptotic cells (58%). Moreover, changes in cell morphology were analyzed using fluorescence microscopy with Hoechst-33258 under low oxygen concentration. Under this anaerobic condition, necrotic cellular death predominated on apoptotic pathway. There were more apoptotic cells under air irradiation condition than under argon irradiation condition. To determine the apoptotic pathway, caspase-3 activation was studied by caspase-3 activity detection kits. The last results showed that P-C₆₀ induced apoptosis by caspase-3-dependent pathway. These results indicated that molecular dyad, which can form a photoinduced charge-separated state, is a promising model for phototherapeutic agents and they have potential application in cell inactivation by PDT.     

Monitoring Anaerobic Natural Attenuation of Petroleum Using a Novel In Situ Respiration Method in Low-Permeability Sediment

Assessing petroleum biodegradation rates is an important part of predicting natural attenuation in subsurface sediments. Monitoring carbon dioxide (CO₂) and methane (CH₄) produced in situ, and their radiocarbon ¹⁴C), stable carbon (¹³C) and deuterium (D). signature provide a novel method to assess anaerobic microbial processes. Our objectives were to: (1) estimate the rate of anaerobic petroleum hydrocarbon (PH) mineralization by monitoring the production of soil gas CH₄ and CO₂ in the vadose zone of low-permeability sediment, (2) evaluate the dominant microbial processes using δ¹³C and δD, and (3) determine the proportion of CH₄ and CO₂ attributable to anaerobic mineralization of PH using ¹⁴C analysis. Argon was sparged into the subsurface to dilute existing CO₂ and CH₄ concentrations. Vadose zone CO₂, CH₄, oxygen, total combustible hydrocarbons, and argon concentrations were measured for 75 days. CO₂ and CH₄ samples were collected on day 86 and analyzed for ¹⁴C, δ¹³C, and δD. Based on CH₄ soil gas production, the anaerobic biodegradation rate was estimated between 0.017 to 0.055 mg/kg soil-d. CH₄ ¹⁴C (2.6 pMC), δ¹³C (-45.64‰), and δD (-316‰) values indicated that fermentation of PH was the sale source of CH₄ in the vadose zone. CO₂ ¹⁴C (62 pMC) indicated that approximately 47% of the total CO₂ was from PH mineralization and 53% from plant root respiration. Although low-permeability sediment increases the difficulty of completely replacing in situ soil gas and assuring anaerobic conditions, this novel respiration method distinguished between anaerobic processes responsible for PH degradation.