Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) Bioremediation in Groundwater: Are Known RDX-Degrading Bacteria the Dominant Players?

Biodegradation of explosives in groundwater represents a promising remedial approach for these compounds. Although a range of bacteria capable of degrading the explosive hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) in pure culture have been described, the role of these known strains (and the genera they represent) during RDX degradation in groundwater has not been established. RDX-contaminated groundwater was collected from the Pueblo Chemical Depot (CO, USA) and the Picatinny Arsenal (NJ, USA) where bioremediation technologies are being tested. Soil columns and enrichment cultures were derived from Picatinny Arsenal groundwater. Bacteria-specific primers were used to amplify the 16S rRNA genes that were used for phylogenetic analysis. The species detected ranged across multiple genera, many of which have not been previously associated with RDX biodegradation. None of the retrieved sequences were exact matches to previously described RDX-degrading strains, although multiple sequences that grouped with known explosive-degrading strains of Clostridium and Pseudomonas were recovered. Genes previously reported to be associated with RDX degradation, including xplA, hydA, onr, xenA, and xenB, were not detected in any of the groundwater samples. These preliminary results indicate that the previously described RDX-degrading bacteria likely do not capture the microbial diversity associated with RDX bioremediation in groundwater, especially under the general biostimulation approaches used during most remediation efforts.     

Long-Term Explosive Contamination in Soil: Effects on Soil Microbial Community and Bioremediation

Explosive contamination in soil is a great concern for environmental health. Following 50 years of munitions manufacturing and loading, soils from two different sites contained ≥ 6,435 mg 2,4,6-trinitrotoluene (TNT), 2,933 mg hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) and 2,135 mg octahydrol-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) kg^{? 1} soil. Extractable nitrate-N was as high as 315 and ammonium-N reached 150 mg N kg^{? 1} soil. Water leachates in the highly contaminated soils showed near saturation levels of TNT and RDX, suggesting great risk to water quality. The long-term contamination resulted in undetectable fungal populations and as low as 180 bacterial colony forming units (CFU) g^–1 soil. In the most severely contaminated soil, dehydrogenase activity was undetectable and microbial biomass carbon was very low (< 3.4 mg C _mic kg^–1 soil). The diminished biological activity was a consequence of long-term contamination because short-term (14 d) contamination of TNT at up to 5000 mg TNT kg^–1 soil did not cause a decline in the culturable bacterial population. Natural attenuation may not be a feasible remediation strategy in soils with long-term contamination by high concentrations of explosives.     

Research on the Evaluation Method of Cr(VI) Migration Parameters in Topsoil and Its Application

Cr(VI) is a characteristic soil and groundwater contaminant in the chromite ore processing residue (COPR) disposal regions. Investigation of Cr(VI) adsorption and migration characteristics in topsoils has great significance for the supervision of contaminated sites. The methods of adsorption and soil column leaching experiments were used to study Cr(VI) migration characteristics in this research, and a Cr(VI) contaminated site in Hanqingba region of Baotou was chosen as the study area. Based on the adsorption experiment results, the soil adsorption properties of Cr(VI) were interpreted by the Langmuir and Freundlich adsorption isotherm, and the saturation adsorption capacity of the soil sample for Cr(VI) was 70.4 mg/kg. Cr(VI) migration characteristic in the soils was studied through the tracer and migration experiments. The permeability coefficient of the soil sample was 0.059 m/d, and the dispersion coefficient was 0.0371 cm²/s. The breakthrough curves of Br and Cr(VI) showed that the retardation effect of Cr(VI) in the soil was not obvious, and the computed retardation factor was 2.39. Under the circumstances of precipitation or irrigation, Cr(VI) in the COPR could be leached out, and the groundwater may be polluted for the weak soil adsorption capacity of Cr(VI). The research results could provide scientific support for the soil and groundwater pollution prevention and control plan of local government.     

Statistical and multivariate statistical techniques to trace the sources and affecting factors of groundwater pollution in a rapidly growing city on the Chinese Loess Plateau

Abstract

Groundwater quality is defined by various water quality parameters. The aims of the research are to understand the relationships among different groundwater quality parameters and to trace the sources and affecting factors of groundwater pollution via statistical and multivariate statistical techniques. The 36 shallow groundwater samples collected from shallow pumping wells in Yan’an City were analyzed for various water quality parameters. Correlation analysis, principal component analysis (PCA), hierarchical cluster analysis (HCA), and multivariable linear regressions (MLR) were jointly used in this study to explore the sources and affecting factors of groundwater pollution. The study reveals that the mineral dissolution/precipitation and anthropogenic input are the main sources of the physicochemical indices and trace elements in the groundwater. Groundwater chemistry is predominantly regulated by natural processes such as dissolution of carbonates, silicates, and evaporates and soil leaching, followed by human activities as the second factor. Climatic factors and land use types are also important in affecting groundwater chemistry. Cl^– is the greatest contributor to the overall groundwater quality revealed by the two regression models. The first model which has eight dependent variables is high in model reliability and stability, and is recommended for the overall groundwater quality prediction. The study is helpful for understanding groundwater quality variation in urban areas.     

Spatial distribution,exposure, and potential health risk assessment from nitrate in drinking water from semi-arid region of South India

Abstract

Elevated nitrate concentration in groundwater is a worldwide problem. Continuous exposure to high levels of nitrate in groundwater may cause adverse health effects among residents who use groundwater for consumption. Therefore, this study was conducted to identify the nitrate distribution and its potential health risk assessment from semi-arid region of Peddavagu in Central Telangana (PCT), South India. Groundwater samples were collected from thirty five locations and analyzed for nitrate and other water quality parameters. Nitrate (NO₃^-) in groundwater was observed to vary from 17 to 120?mg/L, with a mean of 58.74?mg/L. About 57% of samples exceeded the maximum acceptable limit of Indian drinking water standard. About, 40% of groundwater samples drinking water quality index (DWQI) is good, while 60% of groundwater falls in poor quality for drinking purposes. Health risk maps were created based on hazard quotient to quantify the potential health risk of the residents using US Environmental Protection Agency (US EPA) health risk assessment model. Health risk assessment revealed that mean total hazard index (HI_total) for men, women, and children were found as 1.42E?+?00, 1.67E?+?00, and 1.95E?+?00, respectively. Results exhibited that children are at high health risk than men and women in the PCT. Further, the human exposure to the NO₃^- contaminated water was above the critical limit of non-carcinogenic risk.     

Water sources accessed by arid zone riparian trees in highly saline environments,Australia

The flow regimes of arid zone rivers are often highly variable, and shallow groundwater in the alluvial aquifers can be very saline, thus constraining the availability and quality of the major water sources available to riparian trees—soil water, shallow groundwater and stream water. We have identified water sources and strategies used by riparian trees in more highly saline and arid conditions than previously studied for riparian trees of arid zone rivers. Our research focused on the riparian species Eucalyptus coolabah, one of the major riparian trees of ephemeral arid zone rivers in Australia. The water sources available to this riparian tree were examined using δ¹⁸O isotope data from xylem, soil water, groundwater and surface water. Additionally, soil chloride and matric potential data were used to infer zones of water availability for root uptake. Despite the saline conditions, the trees used a mixture of soil water and groundwater sources, but they did not use surface water directly. The study identified three strategies used to cope with typically high groundwater and soil water salinities. Firstly, the trees preferentially grow in zones of most frequent flushing by infiltrating streamflow, such as the bank-tops of channels. Secondly, the trees limit water use by having low transpiration rates. Thirdly, the trees are able to extract water at very low osmotic potentials, with water uptake continuing at chloride concentrations of at least 20,000–30,000 mg L⁻¹.     

Remediation of Explosive-Contaminated Soils: Alkaline Hydrolysis and Subcritical Water Degradation

Alkaline hydrolysis and subcritical water degradation were investigated as ex-situ remediation processes to treat explosive-contaminated soils from military training sites in South Korea. The addition of NaOH solution to the contaminated soils resulted in rapid degradation of the explosives. The degradation of explosives via alkaline hydrolysis was greatly enhanced at pH ≥12. Estimated pseudo-first-order rate constants for the alkaline hydrolysis of 2,4-dinitrotoluene (DNT), 2,4,6-trinitrotoluene (TNT) and hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) in contaminated soil at pH 13 were (9.6?±?0.1)×10^?2, (2.2?±?0.1)×10^?1, and (1.7?±?0.2)×10^?2 min^?1, respectively. In the case of subcritical water degradation, the three explosives were completely removed at 200–300°C due to oxidation at high temperatures and pressures. The degradation rate increased as temperature increased. The pseudo-first-order rate constants for DNT, TNT, and RDX at 300°C were (9.4?±?0.8)×10^?2, (22.8?±?0.3)×10^?2, and (16.4?±?1.0)×10^?2, respectively. When the soil-to-water ratio was more than 1:5, the extent of alkaline hydrolysis and subcritical water degradation was significantly inhibited.     

Using stable hydrogen and oxygen isotopes to study water movement in soil-plant-atmosphere continuum at Poyang Lake wetland,China

Water movement in the soil-plant-atmosphere continuum (SPAC) has a significant effect on the biogeochemical process in wetlands. This study investigated the water movement in the SPAC in Poyang Lake wetland, which is a protected area with an important ecological function within the Yangtze River basin, under different water-level conditions by analyzing the responses of river, groundwater, soil and plants to precipitation using stable hydrogen and oxygen isotopes. The results show that the stable hydrogen and oxygen isotopic compositions (δ¹⁸O and δD) of soil water decrease with increasing depth due to the near surface evaporation. During the dry season the water-level in Poyang Lake is low, when it rains the influencing depth of precipitation and evaporation on soil water isotopic signatures was 20 cm below the ground surface. The rain water infiltrates into the soil, recharges groundwater and flows to the river. When the water-level in Poyang Lake is low, the Xiu River is recharged by the groundwater, which recharges the soil water by capillary rise. During the flood season, the water-level is high and the water in Poyang Lake reaches or covers the meadows, recharges the groundwater and soil water. In the meantime, the water in Poyang Lake can be recharged by rain water when it rains. During the dry season when it doesn’t rain, plants mainly use groundwater, but soil water is preferred and plants don’t use rainwater directly when it rains. When the lake water-level is extremely low, the plants in Poyang Lake wetland may suffer from water stress, which is harmful for plant growth.     

Engineering plants for the phytodetoxification of explosives

Summary  Widespread contaimination of the environment by explosives resulting from the manufacture, disposal and testing of munitions is becoming a matter of increasing concern. Most explosives are considered to be a major hazard to biological systems due to their toxic and mutagenic effects. Interest on the bioremediation of land contaminated with explosives has recently been focused on phytoremediation. Unfortunately., whilst plants have many advantages for the remediation of contaminated land and water, they lack the catabolic versatility which enables microorganisms to mineralize such a wide diversity of xenobiotic compounds. This raised the interesting question as to whether the impressive biodegradative capabilities of soil bacteria could be combined with the high biomass and stability of plants to yield an optimal system for in situ bioremediation of explosive residues in soil. Our investigation into the degradation of explosive residues by soil bacteria resulted in the isolation of Enterobacter cloacae PB2, which is capable of utilizing nitrate ester explosives such as pentaerythritol tetranitrate (PETN) and nitroglycerin as the sole source of nitrogen for growth. We have successfully introduced PETN reductase, the enzyme initiating explosive degradation in this organism, into plants to create transgenic plants that degrade explosives. Since the bacterial degradative pathways for many classes of organic pollutant have been elucidated, this may be a generally applicable method of achieving bioremediation of contaminated soil in the environment.     

Effects of oil shale waste disposal on soil and water quality: hydrogeochemical aspects

Abstract

Environmental pollution from solid waste landfillings (SWLs) is of major concern to both the environmentalists and to individual citizens. The necessity for studying on contaminant generation and control is becoming more urgent in view of the risks associated with such sites.

An oil shale tailing at Maoming, South China, was chosen as our study case. Soil samples, water samples and oil shale tailings were collected from the site and analyzed for their compositions. The analytical results revealed that the soil and groundwater were contaminated to various degrees by several chemicals or pollutants from the oil shale tailings. The major environmental problems associated with the site were acidification of soil and groundwater, high content of heavy metals and sulfate in soil and groundwater and organic contamination of soil, in particular, finding of carcinogenous benzo[a] pyrene other PAHs.

Statistical and geochemical methods were applied to reveal the sources of contaminants. Soil and groundwater contamination were correlated obviously with the oil shale waste disposal. The nearer the sampling sites to the tailing, the heavier the soil and groundwater were contaminated. The different water samples composition had same chemical characteristics. The soil and water samples were analyzed for 16 PAHs (USEPA priority pollutants). It indicated that PAHs were retained mostly in the soil, which consisted of mainly naphthalene, fluorene, phenanthrene and anthracene. Analysis for PAHs source revealed that they were also from the oil shale tailing.     

Influx and efflux of arsenic in cotton fields irrigated with arsenic-contaminated groundwater

Abstract

Samples of rhizosphere soil, groundwater used for drip irrigation, and mature cotton plants were collected from farms at Kuitun, Xinjiang and analyzed for their arsenic (As) levels to account for the influx and efflux of arsenic in the field. The pH value and the soil-grain-size distribution were found to correlate with the different levels of arsenic accumulated by cotton plants and arable soil layers. The principal component analysis (PCA) indicates that the arsenic level in soil is influenced by the silt content and the arsenic level in groundwater, while the arsenic level in plant roots is affected mainly by the silt content and the arsenic level in soil. As estimated, about 64.6?±?2.7?μg of arsenic was extracted from soil by one cotton plant, and more than 44% of it was stored in husks. About 0.8-2.6 mg As/(m² yr) was extracted by plants from soil according to the average dry weight of the plant and the field planting density, while 2.4–28.0?mg As/(m² yr) entered the soil based on the irrigated groundwater volume and the arsenic level in groundwater. Taking account of the cotton residues left after harvest, up to 85.8% of arsenic in the plants returned to the soil. After calculation, about 0.7–2.2?mg As/(m² yr) returned to the soil, and thus the actual net arsenic input to the soil could reach 2.3–27.6?mg As/(m² yr). Because of an obvious rise of the soil arsenic level in Kuitun, Xinjiang, and certain preventive measures should be taken to prevent the propagation of arsenic in the agricultural field.     

Crepuscular activity of adult Sericesthis geminata (Coleoptera: Scarabaeidae): Influence of circadian rhythmicity and light intensity

Subterranean Sericesthis geminata (Boisduval) beetles emerge from the soil daily during the flight season. Emergence and flight are initiated within 15 min after sunset. The beetles are active above the soil surface as the intensity of illumination decreases from 240 lux to 0.7 lux.

If young adult beetles still in their pupal cells in the soil are placed under constant, low‐intensity illumination, they first emerge at any time of day, showing no cyclical diurnal activity pattern. When such beetles are exposed to diurnal fluctuations in illuminance, the first emergence and flight occur at dusk. These beetles subsequently show a diurnal rhythm in their activity, even when exposed to constant environmental conditions. This endogenous activity cycle has a period of about 22 h, and is synchronised with diurnal fluctuations in light intensity. It is reset in response to a change in the photoperiod.

The data suggest that, after initial emergence from the soil, daily crepuscular activity is initiated by an endogenously controlled activity rhythm which causes the beetles to burrow to the soil surface shortly before dusk. At the soil surface they are exposed to fluctuations in the duration and intensity of illumination which may reset the endogenous rhythm, affecting the time of subsequent emergence.     

Horizontal gene transfer (HGT) as a mechanism of disseminating RDX-degrading activity among Actinomycete bacteria

Aims: Hexahydro‐1,3,5‐trinitro‐1,3,5,‐triazine (RDX) is a cyclic nitramine explosive that is a major component in many high‐explosive formulations and has been found as a contaminant of soil and groundwater. The RDX‐degrading gene locus xplAB, located on pGKT2 in Gordonia sp. KTR9, is highly conserved among isolates from disparate geographical locations suggesting a horizontal gene transfer (HGT) event. It was our goal to determine whether Gordonia sp. KTR9 is capable of transferring pGKT2 and the associated RDX degradation ability to other bacteria. Methods and Results: We demonstrate the successful conjugal transfer of pGKT2 from Gordonia sp. KTR9 to Gordonia polyisoprenivorans, Rhodococcus jostii RHA1 and Nocardia sp. TW2. Through growth and RDX degradation studies, it was demonstrated that pGKT2 conferred to transconjugants the ability to degrade and utilize RDX as a nitrogen source. The inhibitory effect of exogenous inorganic nitrogen sources on RDX degradation in transconjugant strains was found to be strain specific. Conclusions: Plasmid pGKT2 can be transferred by conjugation, along with the ability to degrade RDX, to related bacteria, providing evidence of at least one mechanism for the dissemination and persistence of xplAB in the environment. Significance and Impact of Study: These results provide evidence of one mechanism for the environmental dissemination of xplAB and provide a framework for future field relevant bioremediation practices.     

基于植物-土壤反馈的不同绿肥驯化微生物对玉米生长的影响

【背景】在农田生态系统中,土壤微生物与植物互作的机制仍不清楚。【目的】进一步加强对植物-微生物互作的认识,筛选出引起不同反馈作用的关键微生物或微生物类群。【方法】采集豆科绿肥救荒野豌豆(Vicia sativa, V)、十字花科绿肥油菜(Brassica napus, N)和荒坡土壤(remnant prairie, R)驯化的田块土壤0-20 cm作为菌剂在温室进行植物-土壤反馈(plant-soil feedback,PSF)试验。土壤菌剂的接种量为10%,即有90%理化性质一致的灭菌土壤作为背景土,同时设置灭菌土壤菌剂作为对照(CK),种植玉米。每组土壤菌剂处理均分为50 mg/kg高磷(high phosphorus,HP)和5 mg/kg低磷(low phosphorus, LP)两个磷浓度处理。玉米收获后,测定产量和植株地上部磷含量,并取土壤样品进行高通量测序,解析不同养分供给情况下微生物对作物生长的反馈效应。【结果】高磷和土壤反馈效应均促进了玉米的生长。在低磷水平下,V、N和R处理的玉米地上部生物量均高于CK处理,但N处理的玉米地上部生物量增加最多(38%),且增幅显著高...     

Sampling for Explosives-Residues at Fort Greely,Alaska

Fort Greely, Alaska has an extensive complex of weapon training and testing areas located on lands withdrawn from the public domain under the Military Lands Withdrawal Act (PL106-65). The Army has pledged to implement a program to identify possible munitions contamination. Because of the large size (344,165,000 m²) of the high hazard impact areas, characterization of these constituents will be difficult. We used an authoritative sampling design to find locations most likely to contain explosives-residues on three impact areas. We focused our sampling on surface soils and collected multi-increment and discrete samples at locations of known firing events and from areas on the range that had craters, pieces of munitions, targets, or a designation as a firing point. In the two impact areas used primarily by the Army, RDX was the most frequently detected explosive. In the impact area that was also used by the Air Force, TNT was the most frequently detected explosive. Where detected, the explosives concentrations generally were low (<0.05 mg/kg) except in soils near low-order detonations, where the explosive-filler was in contact with the soil surface. These low-order detonations potentially can serve as localized sources for groundwater contamination if positioned in recharge areas.     

A New Design of Mental State Classification for Subject Independent BCI Systems

BackgroundBrain Computer Interface (BCI) systems have been widely used to develop sustainable assistive technology for people suffering from neurological impairments. A major limitation of current BCI systems is that they are based on Subject-dependent (SD) concept. The SD based BCI system is time consuming and inconvenient for physical or mental disables people and also not suitable for limited computer resources. In order to overcome these problems, recently subject-independent (SI) based BCI concept has been introduced to identify mental states of motor disabled people but the expected outcome of the SI based BCI has not been achieved yet. Hence this paper intends to present an efficient scheme for SI based BCI system. The goal of this research is to develop a method for classifying mental states which can be used by any user. For attaining this target, this study employs a supervised spatial filtering method with four types of feature extraction methods including Katz Fractal Dimension, Sub band Energy, Log Variance and Root Mean Square (RMS) and finally the obtained features are used as input to Linear Discriminant Analysis (LDA) classification model for identifying mental states for SI BCI system.ResultsThe performance of the proposed design is evaluated in several ways such as considering different time window length; different frequency bands; different number of channels. The mean classification accuracy using Katz feature is 84.35% which is the maximum output compare to other features that outperforms the existing methods.ConclusionsOur proposed design will help to make a new technology for development of real-time SI based BCI systems that can be more supportive for the motor disabled patients.     

艾比湖湿地芦苇根际土壤氨氧化古菌的多样性和群落结构

【目的】旨在揭示耐盐植物芦苇根际与非根际土壤AOA群落结构间的差异,为深入研究盐生植物根际土壤微生物与耐盐性之间的关系提供理论基础。【方法】应用高通量测序技术以氨单加氧酶基因(amoA)为分子标记,对新疆艾比湖湿地荒漠生态系统不同季节(春、夏、秋)芦苇根际与非根际土壤氨氧化古菌(AOA)的多样性和群落结构进行研究。【结果】结果表明,不同季节芦苇根际土壤AOA多样性和丰富度存在差异,相比非根际土壤,夏季和秋季芦苇根际土壤AOA多样性较低丰富度较高,春季多样性较高丰富度较低。芦苇根际土壤中AOA的多样性为春季夏季秋季。AOA群落组成分析表明,土壤样品中AOA群落主要集中在泉古菌门(Crenarchaeota)和奇古菌门(Thaumarchaeota),其中泉古菌门为主要优势菌门。RDA分析表明,含水量(SM)、有机质(SOM)、总氮(TN)和pH是影响芦苇根际土壤AOA群落多样性和丰富度的主要环境因子。【结论】不同季节芦苇根际土壤AOA多样性及丰富度存在差异,相比非根际土壤,芦苇根际土壤AOA更丰富。     

Understanding the relationships between molecule structure and imprinting effect of two acetyl‐nitrogen heterocyclic compounds

The molecularly imprinted polymers (MIPs) for two structural analogs, 1,3,5‐triacetyl‐1,3,5‐triazacyclohexane (TRAT) and 1,3,5,7‐tetraacetyl‐1,3,5,7‐tetraazacyclooctane (TAT), have been synthesized respectively under the same conditions. The TAT‐MIP showed excellent imprinting effect, whereas the TRAT‐MIP did not. To understand the different imprinting effects of the MIPs prepared from these two templates, the geometric structures and energetic properties of complexes formed around TAT and TRAT were studied computationally. The results indicate that in liquid phase, for the complexes formed with TAT and its nearest neighbor molecules, the magnitude of the binding energy increases with the number of surrounding TAT, methacrylic acid, and acetonitrile (ACT), whereas for the cases of TRAT, the magnitude of the binding energy increases with the number of surrounding TRAT and trimethylolpropane trimethacrylate. The studied systems form stronger and thus more stable networks encapsulating TAT than with TRAT. ACT may also play an important role in the polymerization phase in stabilizing the shapes of the cavities that TATs reside in. We propose these as the major factors that affect the different imprinting effects of the two MIPs. Copyright © 2016 John Wiley & Sons, Ltd.     

黑河下游柽柳根系水力提升对林分蒸散的贡献

准确量化植物根系水力提升(HL)及其生态-水文效应对于陆地生态系统水分循环和全球变化研究具有重要意义。基于2011—2012年黑河下游柽柳林地土壤含水量和涡度协方差观测资料,通过将土壤体积含水量分割为HL和水分损失量(WD),结合涡度协方差测定的潜热通量计算的蒸散量(ET),首次定量黑河下游柽柳根系HL及其对ET的贡献。据估算,柽柳根系HL主要发生在20—60 cm深度,生长季HL大小在0—1.4 mm/d之间变化,平均为0.22 mm/d,WD在0—0.76 mm/d之间变化,平均为0.23 mm/d,HL与WD的年内变化存在同步性,且HL与WD处于正平衡状态,表明HL通过将深层吸收的土壤水或地下水释放在根系吸收层以供植物蒸腾消耗外,还有剩余水分留存在该层内。生长季ET在0.31—5.38 mm/d之间变化,平均为2.82mm/d,但值得注意的是,HL与ET的年内变化存在时间滞后性,HL在5月最高,但ET在7月最大。HL对ET的贡献率在0.06%—108.25%之间变化,平均为19.25%,比例高于100%的时段主要在生长初期,也就是说在蒸散最大的夏季,HL是相对较小的,其原因可能有2个:一是HL受到夏季深层土壤干化的抑制,二是HL受到夏季夜间蒸腾的抑制,究竟是何种原因还有待进一步研究。