Organic Amendments to Enhance Atrazine and Metamitron Degradation in Two Contaminated Soils with Contrasting Textures

Among all types of xenobiotics, pesticides such as herbicides play a significant role in soil and water pollution due to their wide usage all over the world. This study addresses the ability of organic amendments to enhance atrazine and metamitron degradation in two herbicide-contaminated soils with contrasting textures under laboratory conditions. Soil samples were collected from surface soils with textures of sandy loam and silty clay, from northeastern Iran. Initial concentration of herbicides was 50 mg · kg^{? 1} soil. Contaminated soil samples were treated with manure, compost and vermicompost at rates of 0, 0.5, and 2% (w/w). Residual concentrations of atrazine and metamitron were determined by HPLC at the end of incubation periods of 20, 40, and 60 days. Residual concentrations of atrazine were 46.5, 38.9, and 36.2 mg · kg^{? 1} after 20, 40, and 60 days incubation, respectively. Residual metamitron concentrations were clearly lower than atrazine. After 20, 40, and 60 days, concentrations of metamitron were 2.9, 1.0, and 0.6 mg · kg^{? 1}, respectively. Organic amendments at the rates of 0.5 and 2% showed similar effects on the enhancement of herbicide degradation in soils. However, no statistically significant effect was observed among types of organic amendments (α = 0.05). Degradation was affected by soil textures. Residual concentrations of herbicides were higher in sandy loam than in silty clay soil.     

Mangrove soils as sinks for wastewater-borne pollutants

Soil column leaching experiments were conducted to assess the retention of nutrients and heavy metals in two types of mangrove soils receiving strong wastewater throughout a period of 5 months. NH₄ ⁺-N was the dominant form of nitrogen, nitrite and nitrate were in relatively low concentrations in all leachate collected. The concentrations of NH₄ ⁺-N in leachate collected from columns packed with Sai Keng of Hong Kong mangrove soil were higher than those packed with soils collected from Shenzhen of China. The leachate NH₄ ⁺-N contents of Shenzhen columns were significantly lower than that of the synthetic wastewater even at the end of the experimental period, indicating Shenzhen soils had very high capacity to bind nitrogen, and the amount of ammonium added from wastewater did not exceed the binding capacity of mangrove soil. The data also suggest that soils collected from Shenzhen mangrove swamp had higher capacity in retaining wastewater nitrogen than the Sai Keng soils. In contrast, leachate from Sai Keng columns had significantly lower ortho-P contents than those from Shenzhen columns. Actually, the leachate P concentrations of the Sai Keng columns treated with wastewater were similar to those receiving seawater (< 0.1 mg l^–). This finding implies Sai Keng soils were very effective in retaining wastewater P. Throughout the experiment, most heavy metals, including Cu, Zn, Cd, Ni and Cr were not detected in all leachate samples by flame atomic absorption spectrophotometry, indicating that both types of mangrove soils were capable of trapping wastewater-borne heavy metals. The study demonstrates that mangrove soils were good traps to immobilize wastewater-borne phosphorus and heavy metals but they were less efficient in retaining nitrogen from wastewater.     

Effects of wheat volunteers and blackgrass in set-aside following a winter wheat crop on soil infectivity and soil conduciveness to take-all

Two experiments were carried out in France in which disease indices were used to evaluate the effects of wheat volunteers and blackgrass (Alopecurus myosuroides) on soil infectivity and soil conduciveness to take-all caused by Gaeumannomyces graminis var. tritici. Soil infectivity was evaluated by measuring the disease index on susceptible wheat plants grown on soil samples collected from the field. Soil conduciveness to the disease was obtained by measuring disease indices on plants grown on soil samples to which different amounts of take-all fungus inoculum were added. One experiment (Expt. 1) was carried out using soils from farmers' fields (two fields in 1994 and two in 1995); soil infectivity and soil conduciveness were evaluated for three experimental situations: bare soil, soil with wheat volunteers and soil with blackgrass plants. In 1994 the soil infectivity was zero in bare soil, high with the wheat cover, and intermediate with the blackgrass cover. In 1995 the soil infectivity was uniformly low for all three conditions. Soils bearing wheat were less conducive than bare soil, soils bearing blackgrass and bare soils were similarly conducive. A second experiment (Expt. 2) carried out in 1995 compared the soil infectivity and soil conduciveness to take-all of soils planted with wheat or blackgrass in set-aside land after periods of wheat monoculture of 0–6 yr. The soil infectivity was low for all treatments. The soil was more conducive after blackgrass than after wheat. In both cases, the soil conduciveness was less when the monoculture had continued for more than 4 yr. The decline was less after blackgrass than after wheat. Thus, whenever set-aside is set up during the increase phase of the disease in fields with cereal successions, abundant wheat volunteers might hinder the expected positive effect of a break in cereal successions on take-all development. The presence of blackgrass in a set-aside field, with significant soil infectivity and high soil conduciveness, might increase the risks of take-all development in a wheat crop following set-aside.     

Isolation and Characterization of Atrazine Mineralizing Bacillus subtilis Strain HB-6

Atrazine is a widely used herbicide with great environmental concern due to its high potential to contaminate soil and waters. An atrazine-degrading bacterial strain HB-6 was isolated from industrial wastewater and the 16S rRNA gene sequencing identified HB-6 as a Bacillus subtilis. PCR assays indicated that HB-6 contained atrazine-degrading genes trzN, atzB and atzC. The strain HB-6 was capable of utilizing atrazine and cyanuric acid as a sole nitrogen source for growth and even cleaved the s-triazine ring and mineralized atrazine. The strain demonstrated a very high efficiency of atrazine biodegradation with a broad optimum pH and temperature ranges and could be enhanced by cooperating with other bacteria, suggesting its huge potential for remediation of atrazine-contaminated sites. To our knowledge, there are few Bacillus subtilis strains reported that can mineralize atrazine, therefore, the present work might provide some new insights on atrazine remediation.     

The potential of soil microorganisms to mineralize atrazine as predicted by MCH-PCR followed by nested PCR

The potential of soil microorganisms to mineralize atrazine was studied in soil samples collected from fields with various histories of atrazine application. In contrast to many previous studies, which showed no atrazine mineralization activity, all the tested soils mineralized atrazine regardless of their atrazine application history. However, the delay before mineralization and the variation in the subsequent mineralization rate were in agreement with the initial copy number of the atrazine dechlorinaze gene, and the proliferation rate of the degraders. Soils from corn fields, which had up to 100 copies of the atzA gene per gram of soil, had a lag period of 4-5 days before atrazine mineralization started, and final mineralization percentages ranged from 40% to 54%. However, soils from fields that were never amended with atrazine had much longer lag periods (more than 17 days), which decreased after enrichment of the degrader population with high concentrations of atrazine for 15 days. Generally the mineralization rate and the atzA gene copy number increased after the enrichment period. The atrazine mineralization potential was measured by PCR of genes from the atrazine mineralization pathway. Magnetic capture hybridization was the most efficient of the two tested methods for purifying target DNA of PCR inhibitors, without reducing the copy number of the required fragment. Nested PCR proved to be the most effective method for predicting the exact potential of the soil to mineralize the pollutant even without enrichment of a small population with the target genes. This method can complement microcosm studies and eliminate futile efforts when the potential to mineralize the pollutant does not exist in the soil.     

Field and soil microcosm studies on the survival and conjugation of a Pseudomonas putida strain bearing a recombinant plasmid, pADPTel

Pseudomonas putida CR30RNS (pADPTel) is an antibiotic-resistant strain with a recombinant plasmid that confers resistance to tellurite and the ability to catabolize atrazine. The survival of this strain as well as its ability to transfer genes for atrazine degradation and tellurite resistance to indigenous soil bacteria were tested in both fallow soil and canola (Brassica napus) rhizosphere by the use of parallel field and laboratory releases. Culturable CR30RNS (pADPTel) were enumerated in field and microcosm soils at 7- to 14-day intervals over 49 d. Strain CR30RNS (pADPTel) survived for up to 7 weeks in microcosm soils at a density of 10(4) CFU/g soil, whereas in field soils the population declined to 10(3) CFU/g soil by the fourth week. In contrast, when CR30RNS (pADPTel) was introduced into the soil as a seed coating of canola (B. napus 'Karoo'), the bacterium established at higher cell densities in the rhizosphere (10(6)-10(5) CFU/g fresh root mass), with no subsequent decrease in numbers. The presence of selective pressure (i.e., atrazine) had no significant effect on the survival of CR30RNS (pADPTel) in either field or microcosm soils. One year postinoculation field sites were examined for the presence of CR30RNS (pADPTel) and no evidence of culturable parental cells was observed when samples were plated onto selective media. However, the atzC and telAB gene segments were amplified from the field soils at that time. Under laboratory conditions, indigenous soil bacteria were capable of receiving and expressing the engineered plasmid construct at frequencies ranging from 1 to 10(-3) transconjugants per donor. However, no plasmid transfer to indigenous soil bacteria was detected in the field or microcosm soils regardless of the presence of canola rhizosphere and (or) the application of atrazine. Our results show that the survival and population size of P. putida CR30RNS (pADPTel) might be sufficient for degradation of environmental pollutants but that the transfer frequency was too low to be detected under the conditions of this study.     

Enzyme immunoassay determination of atrazine degradation in soil: Moisture,sterilization, and storage effects

Enzyme immunoassay (EIA) microtiter plate analysis was used to quantify atrazine (2‐chloro‐4‐ethylamino‐6‐isopropylamino‐1,3,5 triazine), fortified at 0, 50, and 500 or 549 ng/g, to Baxter and Maury silt loam soil sampled in 1965 and 1991. In the first experiment, aged soils (sampled in 1965 and stored air‐dried) were fortified with atrazine and then incubated in the dark at 0, 75, 150, 225 and 300 g/kg moisture for 15, 80, 154, and 289 d. In a second experiment, fresh soils were fortified with atrazine and incubated in the dark at 0, 150, and 300 g/kg moisture for 9, 15, 35, 55, 83, and 145 d. One half of the treatments in the second experiment were sterilized with 497 ng/g HgCl₂. Twenty milliliters of acetonitrile: water (9: 1) was used to extract 4 or 5 g of soil by vortex mixing at each sampling date. The soil extract was diluted, 80 μl incubated with antibody‐coated wells, and color development read using a microtiter plate reader. Recovery of atrazine from soil was 98% 5 d after fortification. Pesticide recoveries and first‐order degradation rates were dependent on the freshness and moisture content of the soil sample. Pesticide degradation was slower and recoveries higher in soil that had been air dried and stored since 1965, prior to fortification. More atrazine was extracted from soil maintained at 0 g/kg moisture than from soil maintained at 300 g/kg moisture over time.     

Ecological distribution of Spirillum lipoferum Beijerinck.

A survey in various countries revealed that the N2-fixing Spirillum lipoferum Beijerinck is a very common root and soil inhabitant in the tropics. More than half of the grass root and soil samples collected in tropical countries (four African countries and Brazil) contained abundant S. lipoferum populations, while less than 10% of the samples collected in temperate South Brazil, Kenya, and the U.S.A. contained the organism. There is a pronounced vegetation effect. Panicum maximum seems the most favorable among the forage grasses, while few positive samples were found under virgin tropical forest. Legume roots contained less S. lipoferum than adjacent soils. More than 80% of the samples from cereal roots (maize, sorghum, wheat, and rye) grown in fields fertilized with PK and Mo, in Rio de Janeiro State, were positive. Maize and sorghum grown under similar conditions in Wisconsin contained less than 10% of positive samples, but when maize fields were inoculated 90% of the root samples contained S. lipoferum. Alluvial soils were more favorable than eroded hill soils. Occurrence in soil was strongly pH-dependent with a pH around 7, being optimal (correlation coefficient r = 0.90). Sporadic occurrence was observed even in soils with pH 4.8. Surface-sterilized P. maximum roots collected from soils with pH ranging from 4.8 to 7.2 contained high S. lipoferum numbers which did not correlate with soil pH (r = 0.41). Amendment with malate of acid soils was not very effective in increasing nitrogenase (N2-ase) activity, but in two soils with pH above 6.4, high N2-ase activity was obtained after 16 to 48 h of incubation. In two soils from a temperate climate region, inoculation with S. lipoferum increased N2-ase activity produced through malate amendment.     

Mineralization Potential of Atrazine and Degradation Intermediates from Clustered Characteristics in Inoculated Soils

Soil properties impact pesticide persistence. Because these characteristics operate together in situ, identification of their clustered associations can help explain pesticide fate. Factor analysis was used to reduce the dimensionality of soil characteristics by grouping them into clustered independent factors, which were then related to the mineralization of atrazine and selected degradation intermediates. A Sharpsburg silty clay loam, Ortello sandy loam, and Hord silt loam were inoculated with a Hord soil that had a high capacity for atrazine mineralization. The soils were spiked with ¹⁴C-radiolabeled atrazine, deethylatrazine, hydroxyatrazine, N-isopropylammeline, N-isopropylammelide or cyanuric acid and sampled during incubation for 80 d (atrazine) or 40 d (degradation intermediates) at 22°C. Low mineralization in uninoculated soils demonstrated that the absence of atrazine-mineralizing microorganisms was most limiting. In inoculated soils, regression analysis indicated mineralization of atrazine (R² = 0.88) and its degradation intermediates (R² ≥ 0.89) was related to factors associated with bioavailability and microbial activity. For atrazine, this relationship indicated mineralization may be positively influenced by higher pH and available phosphorus, lower NO₃-N, organic carbon and clay contents, and lower adsorption. Our results show how factor analysis can be used in conjunction with multiple regression to determine mineralization potential and thus help identify soils with limited degradation capacities and possible long-term persistence.     

Biodegradation of Atrazine by Agrobacterium radiobacter J14a and Use of This Strain in Bioremediation of Contaminated Soil

We examined the ability of a soil bacterium, Agrobacterium radiobacter J14a, to degrade the herbicide atrazine under a variety of cultural conditions, and we used this bacterium to increase the biodegradation of atrazine in soils from agricultural chemical distribution sites. J14a cells grown in nitrogen-free medium with citrate and sucrose as carbon sources mineralized 94% of 50 μg of [¹⁴C-U-ring]atrazine ml⁻¹ in 72 h with a concurrent increase in the population size from 7.9 × 10⁵ to 5.0 × 10⁷ cells ml⁻¹. Under these conditions cells mineralized the [ethyl-¹⁴C]atrazine and incorporated approximately 30% of the ¹⁴C into the J14a biomass. Cells grown in medium without additional carbon and nitrogen sources degraded atrazine, but the cell numbers did not increase. Metabolites produced by J14a during atrazine degradation include hydroxyatrazine, deethylatrazine, and deethyl-hydroxyatrazine. The addition of 10⁵ J14a cells g⁻¹ into soil with a low indigenous population of atrazine degraders treated with 50 and 200 μg of atrazine g⁻¹ soil resulted in two to five times higher mineralization than in the noninoculated soil. Sucrose addition did not result in significantly faster mineralization rates or shorten degradation lag times. However, J14a introduction (10⁵ cells g⁻¹) into another soil with a larger indigenous atrazine-mineralizing population reduced the atrazine degradation lag times below those in noninoculated treatments but did not generally increase total atrazine mineralization.     

Extracellular Enzyme Activity in a Willow Sewage Treatment System

This paper presents the results of studies on the activity of extra-cellular enzymes in soil-willow vegetation filter soil which is used in the post-treatment of household sewage in an onsite wastewater treatment system located in central Poland. Wastewater is discharged from the detached house by gravity into the onsite wastewater treatment system. It flows through a connecting pipe into a single-chamber septic tank and is directed by the connecting pipe to a control well to be further channelled in the soil-willow filter by means of a subsurface leaching system. Soil samples for the studies were collected from two depths of 5?cm and 1?m from three plots: close to the wastewater inflow, at mid-length of the plot and close to its terminal part. Soil samples were collected from May to October 2009. The activity of the extra-cellular enzymes was assayed by the fluorometric method using 4-methylumbelliferyl and 7-amido-4-methylcoumarin substrate. The ranking of potential activity of the assayed enzymes was the same at 5?cm and 1?m soil depths, i.e. esterase?>?phosphmomoesterase?>?leucine-aminopeptidase?>?β-glucosidase?>?α-glucosidase. The highest values of enzymatic activity were recorded in the surface layer of the soil at the wastewater inflow and decreased with increasing distance from that point.     

Microbiological Comparison of Surface Soil and Unsaturated Subsurface Soil from a Semiarid High Desert

Thirty-two chemoheterotrophic bacteria were isolated from unsaturated subsurface soil samples obtained from ca. 70 m below land surface in a high desert in southeastern Idaho. Most isolates were gram positive (84%) and strict aerobes (79%). Acridine orange direct counts of microbes in one subsurface sample showed lower numbers than similar counts performed on surface soils from the same location (ca. 5 × 10⁵ versus 2 × 10⁶ cells per g [dry weight] of soil), but higher numbers than those from plate counts performed on the subsurface material. Another sample taken from the same depth at another location showed no evidence of colonies under identical conditions. Soil analyses indicated that subsurface sediments versus surface soils were slightly alkaline (pH 7.9 versus 7.4), had a higher water content (25.7 versus 6.3%), and had lower organic carbon concentrations (0.05 to 0.17 versus 0.25% of soil dry weight). Analyses of biologically relevant gases from the unsaturated subsurface indicated an aerobic environment. As in other unsaturated soil environments, either a high proportion of bacteria in these subsurface sediments are not viable or they are incapable of growth on conventional media under aerobic conditions. The presence and numbers of bacteria in these deep sediments may be influenced by colonization opportunities afforded by periodic percolation of surface water through fractures in overlying strata.     

Persistence of Perchlorate and the Relative Numbers of Perchlorate- and Chlorate-Respiring Microorganisms in Natural Waters, Soils, and Wastewater

Cell numbers of perchlorate (PRM)- and chlorate (CRM)-reducing microorganisms and the persistence of perchlorate were determined in samples of soils, natural waters, and wastewater incubated under laboratory conditions. Complete perchlorate reduction in raw wastewater and creek water was achieved in 4 to 7 days and 8 to 29 days, respectively, depending on the individual growth substrate (acetate, lactate, citric acid, or molasses) employed. Perchlorate persisted in most mixed cultures developed with 2 g of “pristine” soil, but declined in mixed cultures developed with 100 g of soil. Less than seven days were required to completely reduce perchlorate in cultures started with 10 g of a perchlorate-contaminated soil obtained from a site in Texas. The concentration of PRM was estimated using a 5-tube most probable number (MPN) procedure. To account for discrepancies due to differences in the total number of bacteria (per mass of sample) in the samples, difficulty in removing bacteria from soil samples, and the lack of an unequivocal method to measure total viable cells in these different systems, we normalized our MPN results on the basis of 10⁶ or 10⁹ total bacteria counted using acridine orange direct counts (AODC). There were more PRM in wastewater samples on a per-cell basis (15 to 350 PRM/10⁶-AODC) than in water samples (0.02 to 0.4 PRM/10⁶-AODC). There were also more PRM in soils from sites exhibiting direct evidence of perchlorate contamination (100 to 200 PRM/10⁹-AODC) than from other sites (nondetectable to 0.77 PRM/10⁹-AODC). These results demonstrate that perchlorate-reducing bacteria are present at perchlorate-contaminated sites, and that perchlorate can be degraded by these microorganisms through the addition of different electron donors, such as acetate and lactate.     

Effects of biochar amendment on the sorption and degradation of atrazine in different soils

ABSTRACT

Sugarcane top-derived biochar was added to an alluvial soil, a moist soil and a paddy soil at the rate of 0.2% and 0.5% (w/w). After the addition of 0.2% and 0.5% biochar, the sorption coefficients (K_d) of atrazine (Ce = 10 mg L^?1) were increased by 26.97% and 79.58%, respectively, in the moist soil with a low level of total organic carbon (TOC), while it increased by 31.43% and 60.06%, respectively, in the paddy soil with a high TOC content. The half-time persistence values of atrazine in the alluvial soil, moist soil and paddy soil were 28.18, 23.74 and 39.84 d, respectively. In the 0.2% biochar amended soils, the corresponding half-times of atrazine for the alluvial soil, moist soil and paddy soil were extended by 10.33, 11.81 and 1.42 d, and they were prolonged by 16.83, 17.52 and 14.74 d, respectively, in the 0.5% biochar amended soils. Atrazine degradation products (deisopropylatrazine and desethylatrazine) decreased after they accumulated to 3.2 and 1 mg kg^?1, respectively. Generally, increasing sorption was accompanied by decreasing degradation of atrazine which is found in biochar-amended soils.     

Impact of Polyacrylamide Treatment on Sorptive Dynamics and Degradation of 2,4-D and Atrazine in Agricultural Soil

High-molecular-weight, anionic polyacrylamide (PAM) is added to irrigation water to reduce soil erosion during furrow irrigation of crops. The chemical nature of PAM, together with the observation that the polymer can be biotransformed by soil bacteria, led us to question the impact of PAM treatment on the fate of coapplied agrochemicals. The herbicides, atrazine (nonionic) and 2,4-D (anionic), were tested for pesticide sorption, desorption, and degradation in PAM-treated and untreated soils. Sorption of atrazine and 2,4-D in soil was unaffected by PAMtreatment, as was atrazine desorption. However, 2,4-D desorbedmore readily from the PAM-treated soil than from untreated soil. With respect to pesticide degradation, mineralization of the 2,4-D aromatic ring was not impacted by PAM treatment, but decarboxylation of the 2,4-D carboxylic acid side chain was significantly reduced in the PAM-treated soil. Limited mineralization (7 to 10%) of atrazine was observed in both soils. However, in PAM-treated soils atrazine conversion to ¹⁴CO₂ and bound residue components was significantly reduced, and there was an increase in the level of methanol extractable metabolites. These results may indicate that PAM application can alter the environmental fate of some pesticides in soils, especially under the high dose treatment conditions examined in this study.     

小兴安岭两种森林类型土壤有机碳库及周转

采用室内培养法测定了不同温度下(8、18、28 ℃)小兴安岭原始阔叶红松林和阔叶次生林土壤有机碳的矿化速率和矿化量,并用三库一级动力学模型对有机碳各库进行拟合.结果表明： 基于单位干土质量的阔叶次生林土壤有机碳矿化速率和累计矿化量均大于原始红松林,但有机碳累计矿化量占总有机碳的比率小于原始红松林.2种森林类型土壤活性碳库和缓效碳库随土层加深而减小,其占总有机碳的比例增加.尽管阔叶次生林土壤活性和缓效碳库均大于原始红松林,但其占总有机碳的比例却小于原始红松林,而土壤惰性碳库及其比例均大于原始红松林,表明阔叶次生林土壤有机碳整体上更稳定.土壤活性碳库平均驻留时间(MRT)为9～24 d,且随土层加深而缩短,而缓效碳库MRT为7～42 a,且随土层加深而延长.土壤活性碳库及其占总有机碳的比例随温度升高而线性增加,缓效碳库则降低;原始红松林土壤活性碳随温度的增速大于阔叶次生林,表明原始红松林土壤有机碳库对温度变化反应更敏感.     

长期施肥对红壤水稻土磷脂脂肪酸特性和酶活性的影响

对中国科学院红壤生态实验站长期定位试验中不同施肥处理红壤水稻土磷脂脂肪酸(PLFA)特性及酶活性进行了分析.结果表明:不同施肥处理的土壤酶活性、养分、微生物生物量及微生物群落多样性差异较大;施肥处理增加了PLFA的种类和微生物量;施肥土壤的真菌PLFA量大于不施肥土壤,细菌PLFA量小于不施肥土壤,说明真菌较细菌更能适应养分贫瘠的条件.NPK平衡施肥和施有机肥处理的PLFA总量均高于施无机氮肥和未施肥处理,两者分别比未施肥处理高222%和79%,表明NPK平衡施肥和施有机肥更有利于作物生长.施肥还可增加土壤酶活性,其中,土壤脲酶和磷酸酶活性可以作为衡量土壤肥力水平的指标.     

盐城海滨湿地盐沼植被对土壤碳氮分布特征的影响

在盐城海滨湿地不同植被带下采集土壤样品,研究了土壤有机碳和全氮的空间分布特征,分析了盐沼植物对湿地土壤碳、氮分布的影响.结果表明：在盐城海滨湿地,表层土壤中有机碳和全氮含量分别介于1.71～7.92 g·kg^-1和0.17～0.36 g·kg^-1之间,变幅较大,不同植被带之间存在显著差异,且各植被带表层土壤中有机碳、全氮含量均高于光滩.垂直方向上,各植被带土壤中有机碳、全氮的分布均呈自表向下逐渐降低的趋势,15 cm以下其含量基本保持稳定.土壤有机碳与全氮、碳氮比呈显著正相关,但全氮与碳氮比无显著相关性.     

Monitoring of bacterial community in a coniferous forest soil after a wildfire

Changes in the soil bacterial community of a coniferous forest were analyzed to assess microbial responses to wildfire. Soil samples were collected from three different depths in lightly and severely burned areas, as well as a nearby unburned control area. Direct bacterial counts ranged from 3.3-22.6 x 10(8) cells/(g.soil). In surface soil, direct bacterial counts of unburned soil exhibited a great degree of fluctuation. Those in lightly burned soil changed less, but no significant variation was observed in the severely burned soil. The fluctuations of direct bacterial count were less in the middle and deep soil layers. The structure of the bacterial community was analyzed via the fluorescent in situ hybridization method. The number of bacteria detected with the eubacteria-targeted probe out of the direct bacterial count varied from 30.3 to 84.7%, and these ratios were generally higher in the burned soils than in the unburned control soils. In the surface unburned soil, the ratios of alpha-, beta- and gamma-proteobacteria, Cytophaga-Flavobacterium group, and other eubacteria groups to total eubacteria were 9.9, 10.6, 15.5, 9.0, and 55.0%, respectively, and these ratios were relatively stable. The ratios of alpha-, beta- and gamma-proteobacteria, and Cytophaga-Flavobacterium group to total eubacteria increased immediately after the wildfire, and the other eubacterial proportions decreased in the surface and middle layer soils. By way of contrast, the composition of the 5 groups of eubacteria in the subsurface soil exhibited no significant fluctuations during the entire period. The total bacterial population and bacterial community structure disturbed by wildfire soon began to recover, and original levels seemed to be restored 3 months after the wildfire.     

atz gene expressions during atrazine degradation in the soil drilosphere

One of the various ecosystemic services sustained by soil is pollutant degradation mediated by adapted soil bacteria. The pathways of atrazine biodegradation have been elucidated but in situ expression of the genes involved in atrazine degradation has yet to be demonstrated in soil. Expression of the atzA and atzD genes involved in atrazine dechlorination and s‐triazine ring cleavage, respectively, was investigated during in situ degradation of atrazine in the soil drilosphere and bulked samples from two agricultural soils that differed in their ability to mineralize atrazine. Interestingly, expression of the atzA gene, although present in both soils, was not detected. Atrazine mineralization was greatest in Epoisses soil, where a larger pool of atzD mRNA was consistently measured 7 days after atrazine treatment, compared with Vezin soil (146 vs. 49 mRNA per 10 ⁶ 16S rRNA, respectively). Expression of the atzD gene varied along the degradation time course and was profoundly modified in soil bioturbated by earthworms. The atzD mRNA pool was the highest in the soil drilosphere (casts and burrow‐linings) and it was significantly different in burrow‐linings compared with bulk soil (e.g. 363 vs. 146 mRNA per 10 ⁶ 16S rRNA, 7 days after atrazine treatment in Epoisses soil). Thus, consistent differences in atrazine mineralization were demonstrated between the soil drilosphere and bulk soil. However, the impact of bioturbation on atrazine mineralization depended on soil type. Mineralization was enhanced in casts, compared with bulk soil, from Epoisses soil but in burrow‐linings from Vezin soil. This study is the first to report the effects of soil bioturbation by earthworms on s‐triazine ring cleavage and its spatial variability in soil.