Persistence of Denitrifying Enzyme Activity in Dried Soils

The effects of air drying soil on denitrifying enzyme activity, denitrifier numbers, and rates of N gas loss from soil cores were measured. Only 29 and 16% of the initial denitrifying enzyme activity in fresh, near field capacity samples of Maury and Donerail soils, respectively, were lost after 7 days of air drying. The denitrifying activity of bacteria added to soil and activity recently formed in situ were not stable during drying. When dried and moist soil cores were irrigated, evolution of N gas began, and it maximized sooner in the dried cores. This suggests that the persistence of denitrifying enzymes permits accelerated denitrification when dried soils are remoistened. Enzyme activity increased significantly in these waterlogged cores, but fluctuations in enzyme activity were small compared with fluctuations in actual denitrification rate, and enzyme activities were always greater than denitrification rates. Apparent numbers of isolatable denitrifiers (most-probable-number counts) decreased more than enzyme activity as the soils were dried, but after the soils were rewetted, the extent of apparent growth was not consistently related to the magnitude of N loss. We hypothesize that activation-inactivation of existing enzymes by soil O₂ is of greater significance in transient denitrification events than is growth of denitrifiers or synthesis of new enzymes.     

The Effects of the Gamma Isomer of Benzene Hexachloride (Hexachlorocyclohexane) on Plant Growth and on Mitosis

Three experiments have been carried out on the effects of thegamma isomer of benzene hexachloride (hexachlorocyclohexane),applied in the form of a china clay dust containing appropriateamounts of the pure compound. The first experiment showed that root-growth of cress was unaffectedby gamma-BHC, but that in wheat, growth was significantly reduced. The effect of the compound on mitosis in rye was shown by thesecond erperiment to resemble that of colchicine and other mitoticpoisons in inducing polycentric mitosis or polyploidy by inhibitingspindle action and in causing enlarged nuclei of irregular shapewhich contained increased amounts of nucleolar material. In the third experiment the threshold concentrations for root-growthinhibition and for the production of abnormal cytological effectswere found to be the same. It is considered that the growth-regulatory and mitotic effectsof gamma-BHC are causally related.     

Seasonal Fluctuations and Long-Term Persistence of Pathogenic Populations of Agrobacterium spp. in Soils

Short- and long-term persistence of pathogenic (i.e., tumor forming) agrobacteria in soil was investigated in six nursery plots with a history of high crown gall incidence. No pathogenic Agrobacterium strains were isolated in soil samples taken in fall and winter in any plots, but such strains were isolated from both bulk soils and weed rhizospheres (over 0.5 × 10⁵ pathogenic CFU/g of bulk soil or rhizosphere) in three out of six plots in spring and summer. PCR amplifications of a vir sequence from DNA extracted from soil confirmed the presence of Ti plasmids in summer and their absence in fall and winter. The results indicate that strains that harbor a Ti plasmid had an unforeseen positive fitness versus Ti plasmid-free strains in soil and rhizosphere in spring and summer in spite of the apparent absence of tumor, and hence of opines. The gain of fitness occurred during a bloom of all cultivable agrobacteria observed only in conducive soils. An evolution of the pathogenic population was recorded during a 4-year period in one particularly conducive soil. In 1990, the pathogenic population in this soil consisted of only biovar 1 strains harboring both octopine- and nopaline-type Ti plasmids. In 1994, it consisted of only nopaline-type Ti plasmids equally distributed among biovar 1 and 2 strains. These results suggest that nopaline-type Ti plasmids conferred a better survival ability than octopine-type Ti plasmids to biovar 2 agrobacteria under the present field conditions.     

Long-Term Persistence and Leaching of Escherichia coli in Temperate Maritime Soils

Enteropathogen contamination of groundwater, including potable water sources, is a global concern. The spreading on land of animal slurries and manures, which can contain a broad range of pathogenic microorganisms, is considered a major contributor to this contamination. Some of the pathogenic microorganisms applied to soil have been observed to leach through the soil into groundwater, which poses a risk to public health. There is a critical need, therefore, for characterization of pathogen movement through the vadose zone for assessment of the risk to groundwater quality due to agricultural activities. A lysimeter experiment was performed to investigate the effect of soil type and condition on the fate and transport of potential bacterial pathogens, using Escherichia coli as a marker, in four Irish soils (n = 9). Cattle slurry (34 tonnes per ha) was spread on intact soil monoliths (depth, 1 m; diameter, 0.6 m) in the spring and summer. No effect of treatment or the initial soil moisture on the E. coli that leached from the soil was observed. Leaching of E. coli was observed predominantly from one soil type (average, 1.11 ± 0.77 CFU ml⁻¹), a poorly drained Luvic Stagnosol, under natural rainfall conditions, and preferential flow was an important transport mechanism. E. coli was found to have persisted in control soils for more than 9 years, indicating that autochthonous E. coli populations are capable of becoming naturalized in the low-temperature environments of temperate maritime soils and that they can move through soil. This may compromise the use of E. coli as an indicator of fecal pollution of waters in these regions.The contamination of groundwater, including potable water supplies, with microbial pathogens continues to be a global concern (52, 59). Of particular importance in developed countries are the high levels of contamination associated with small-scale and very-small-scale drinking water supplies (5, 19, 57), often groundwater, which serve an estimated 10% of the total population in the European Union (13). The high numbers of these water supplies found to be contaminated with fecal bacteria and thus considered to be unfit for human consumption are worrying because the water from them is often untreated or inadequately treated prior to consumption. Microbial pathogens are known to survive for considerable periods of time in groundwater (29), which increases the health risk due to utilization of contaminated supplies. There are various sources of contamination, but evidence suggests that contamination from the spreading of animal slurries and manures on land can be a significant contributor (3, 33, 53). Spreading of agricultural slurries and manures on land is used by the agricultural sector as a means of nutrient recycling. The health risks associated with the spreading of animal and human wastes containing enteric pathogens have been recognized for a long time (10, 18). Animal manure and wastewaters may contain a broad range of pathogenic microorganisms, including Escherichia coli O157:H7, Campylobacter, Cryptosporidium, Salmonella spp., and pathogenic viruses, which are released into the environment during spreading (15, 22, 55). The levels and incidence of pathogens present in animal manures and slurries are influenced by a number of factors, including herd health, age demographics, stress factors, diet, season, and manure management and storage (37, 39).Soils (and subsoils) often act as a zone for mitigating microbial contamination of groundwater associated with the spreading of animal slurries and manures on land. Some of the pathogenic microorganisms applied to agricultural soils have, however, been observed to leach through the soil into groundwater, which can affect drinking water quality and pose a risk to public health (16, 26, 28, 42, 50), confirming that soil is not always a sufficient obstruction for protection of groundwater (16, 53). Consequently, characterization of the movement of pathogens through the unsaturated soil and subsoil zone (vadose zone) has become critical for assessment of the risk to groundwater posed by agricultural activities (8, 14, 42). The soil and subsoil type is believed to be a major factor influencing the potential transfer of pathogens through soil to groundwater (3, 34, 41, 50). The preapplication moisture status of a soil, which may be influenced by the season, also impacts pathogen survival, fate, and transport (2, 11, 43, 54).E. coli is widely used as an indicator of fecal contamination of water, and certain strains are known to be pathogenic (12). Thus, characterizing this organism''s transport through soil is important because of the health risk posed by the organism itself and with regard to its validity as an indicator of the fate of enteropathogens in the environment. E. coli strains have diverse properties and capabilities that affect their survival and transport in soils (9, 36, 56, 60). Consequently, data obtained by using total E. coli rather than individual surrogate strains can be more representative of the fate and transport of E. coli present in animal slurries. E. coli O157 die-off in soils has been reported to be the same as or quicker than total E. coli die-off, suggesting that data for total E. coli provide a conservative estimate of the survival potential (38, 56). Although many field and laboratory studies have investigated E. coli transport through soil columns (4, 6, 16, 43, 46, 47, 50, 51), most studies have investigated transport through soil to a depth of less than 30 cm. For assessment of the risk of transport to groundwater, such studies may not take into account the variation in soil physical and chemical characteristics with depth (e.g., the frequency and continuity of macropores, organic matter, and moisture contents) that affect bacterial transport. Furthermore, rainfall was often simulated in previous studies, which allows experimental conditions to be controlled but may not be representative of the risk due to variable natural rainfall events over time. In this study, we used intact soil monoliths that were 1 m deep to assess the risk of leaching of total E. coli in four representative Irish soil types under natural rainfall and environmental conditions.The objective of this study was to quantitatively investigate the impact of soil type and season (soil moisture content) on the fate and transport of E. coli spread on four different temperate maritime soil types under natural rainfall conditions. We hypothesized that there would be a greater microbial risk to underlying groundwater with better-drained soil types than with relatively poorly drained soil types following the application of animal slurry. In addition, we hypothesized that E. coli cells spread on wetter spring soils would be transported in greater numbers than E. coli cells spread on drier soils in the summer.     

Mobility and Persistence of Petroleum Hydrocarbons in Peat Soils of Southeastern Mexico

Spilled crude petroleum from oil wells contains numerous hydrocarbons, some of which are toxic and threaten life. We have studied the mobility and persistence of hydrocarbons in waterlogged soils that contain large proportions of fermented organic matter (Histosols) and large concentrations of dissolved organic carbon (DOC) in the State of Tabasco, Mexico. We sampled soil and phreatic water at sites polluted by oil spills for several decades, as well as at sites that had only recently (few weeks) been polluted, and compared their hydrocarbon contents with those of unaffected sites in the same area. Samples were analyzed for 16 non-alkylated polyaromatic hydrocarbons (PAHs) and n-alkanes from nC9 to nC34. The spilled hydrocarbons had remained predominantly in the organic surface horizons of the soil where spillage occurred; there was little evidence of movement within the soil. The fraction of low molecular weight compounds was larger at sites of recent spills than where spills happened several decades ago. Nevertheless, sites of old spills still contained large concentrations of hydrocarbons, among which those of low molecular weight represented from 30 to 49% of total PAHs and from 50 to 84% of total n-alkanes, indicating that volatilization or microbial degradation is slow in these soils. In the peat horizons the measured organic carbon partition coefficients (K _oc ) for the higher molecular weight PAHs were consistently smaller than those estimated by empirical equations by up to two orders of magnitude. The dissolved organic carbon of these peat soils seems to influence this behavior. At sites of old spills, partition coefficients for the PAHs were larger than at sites of recent spills.