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PubMedDate not supplied

Soil mixing to decrease surface stratification of phosphorus in manured soils.

Continual applications of fertilizer and manure to permanent grassland or no-till soils can lead to an accumulation of P at the surface, which in turn increases the potential for P loss in overland flow. To investigate the feasibility of redistributing surface stratified P within the soil profile by plowing, Mehlich-3 P rich surface soils (128-961 mg kg(-) in 0-5 cm) were incubated with lower-P subsoil (16-119 mg kg(-1) in 5-20 cm) for 18 manured soils from Oklahoma and Pennsylvania that had received long-term manure applications (60-150 kg P ha(-1) yr(-1) as dairy, poultry, or swine manure for up to 20 yr). After incubating a mixture of 5 g surface soil (0- to 5-cm depth) and 15 g subsoil (5- to 20-cm depth) for 28 d, Mehlich-3 P decreased 66 to 90% as a function of the weighted mean Mehlich-3 P of surface and subsoil (i.e.. 1:3 ratio) (r2 = 0.87). At Klingerstown, Northumberland County, south central Pennsylvania, a P-stratified Berks soil (Typic Dystrochrept) (495 mg kg(-1) Mehlich-3 P in 0- to 5-cm depth) was chisel plowed to about 25 cm and orchardgrass (Dactylis glomerata L.) planted. Once grass was established and erosion minimized (about 20 wk after plowing and planting), total P concentration in overland flow during a 30-min rainfall (6.5 cm h(-1)) was 1.79 mg L(-1) compared with 3.4 mg L(-1) before plowing, with dissolved P reduced from 2.9 to 0.3 mg L(-1). Plowing P-stratified soils has the potential to decrease P loss in overland flow, as long as plowing-induced erosion is minimized.

Agriculture↗
PubMed2006

The survival of pathogens in soil treated with wastewater sludge and in potatoes grown in such soil.

The prevalence of pathogens on potatoes (Solanum tuberosum) grown in soil amended with a pathogen rich wastewater sludge was investigated. Bacteria of the family Enterobacteriaceae are important pathogens causing intestinal and systemic illness of humans and other animals. Type B sludge was used. Sludges investigated are the high metal and the low metal sludges. Microorganisms in the sludge-amended soil were using culture-based technique. Salmonella and E. coli were observed in tested soil samples. No microorganisms were isolated from control samples taken throughout the process of the experiment. At harvest time, some of the potato samples from LMS soil were contaminated. These potatoes were subjected to further investigation using molecular techniques (polymerase chain reaction) with fD1 and rP2 as primers. Organisms identified from the sequenced potato peel samples with the BLAST search tool included Enterobacter agglomerans (Pantoea agglomerans), several Buttiauxella spp., Pectobacterium spp., Erwinia spp. and a few Pantoea spp. Other than the E. agglomerans, which is commonly found in the gut and upper respiratory tract of humans and in the environment, all the other species identified were found to be mainly either plant or soil pathogens. The E. agglomerans are not primary pathogens but secondary opportunistic pathogens particularly in immunocompromised individuals. These results suggest that growing high risk crops using wastewater sludge contaminated soil may lead to limited infestation of produce with primary pathogens. It appears that the use of HMS due to early pathogen die-off provides less risk of infection than the LMS. However, proper treatment of wastewater sludge to reduce pathogen load is essential prior to its use as soil conditioner.

Escherichia coli↗
PubMedDate not supplied

[The analysis of coefficient of 137Cs transfer from soil into potato in relationship with 137Cs content in soil and plant mineral feed].

The soil-potato transfer factor for 137Cs (TF) was estimated by using results of 137Cs activity concentration measurements in 214 samples of soil and potato taken at fields with various level of contamination with 137Cs. The relationships between the coefficient TF and soil characteristics (acidity pH (KCl), content of K2O, P2O5, CaO and MgO in soil) and soil contamination with 137Cs have been analysed. The results show that the TF values tend to decrease with increasing concentration of 137Cs, K2O, P2O5, and CaO in considered sod-podsolic sandyloam soil. The regression function describing the TF dependence of 137Cs, K2O, P2O5, and CaO content in soil has been derived.

Biological Transport↗
PubMed2003

[Relationship among soil enzyme activities, vegetation state, and soil chemical properties of coal cinder yard].

From field investigation and laboratory analysis, the relationships among soil enzyme activities, vegetation state and soil chemical properties of coal cinder yard in thermal power station were studied. The results showed that vegetation on coal cinder yard was distributed in scattered patch mainly with single species of plant, and herbs were the dominant species. At the same time, the activity of three soil enzymes had a stronger relativity to environment conditions, such as vegetation state and soil chemical properties. The sensitivity of three soil enzymes to environmental stress was in order of urease > sucrase > catalase. The relativity of three soil enzymes to environmental factor was in order of sucrase > urease > catalase. Because of urease being the most susceptible enzyme to environmental conditions, and it was marked or utmost marked interrelated with vegetation state and soil chemical properties, urease activity could be used as an indicator for the reclamation of wasteland.

Cadmium↗
PubMed2003

[Quantitative simulation on the vertical distribution of soil organic matters in mountainous soil profiles in the subtropical area, south China].

Quantitative descriptions of soil organic matter (SOM) dynamics, i.e., their distribution, turnover and movement, are essential for the running of the simulation of terrestrial ecosystem organic matter models. In this study, based on utilizing SOM diffusion-translation-decomposition model, two soil profiles were selected in different vegetation zones at Dinghushan Mountain for quantitative studies on SOM dynamics and their controlling factors. SOM were divided into three kinds of compartments: rapid compartment with turnover rate of 0.1-1.yr-1, slow compartment with turnover rate of 0.002-0.02.yr-1, and stable compartment with turnover rate of 0.0001-0.001.yr-1. The numerical results suggested that SOM distribution in soil profile in subtropical mountainous areas of south China obeyed the law of diffusion motion, translation motion and decomposition. The turnover rate of SOM rapid compartment was 0.483.yr-1 in the forest vegetation zone, and was 0.694.yr-1 in the shrub vegetation zone. The turnover rates of SOM slow compartment in the two kinds of vegetation zones were both 0.02.yr-1, and the turnover rates of SOM stable compartment in the two kinds of vegetation zones were both 0.001.yr-1. SOM diffusion rate and translation rate for the forest vegetation zone was 4 cm2.yr-1 and 0.2 mm.yr-1, respectively, and the two rates of the shrub vegetation zone were 1 cm2.yr-1 and 0.5 mm.yr-1, respectively. The obvious discrepancy between numerical values and measuring values for SOM content occurred in the 0-10 cm sections of the profiles, which might be due to the fact that the upper sections were at the interface between lithosphere and atmosphere, and were influenced directly by changes of climatic and environmental factors. The two kinds of values for SOM content were identical below the upper section of the profiles, and it indicated stable pedogenesis environments. Diffusion motion had obvious influences on SOM vertical distribution, and translation motion had clear impacts on SOM distribution only in the upper 0-10 cm section. Comparison analysis suggested that SOM dynamics were controlled mainly by soil profile qualities such as SOM content, clay content, soil fabric, void types and their developments, soil fauna and microorganism activities, etc. With the increasing of primary production of aboveground vegetation, the turnover rate of SOM rapid compartment decreased and SOM content increased, which provided scientific basis for increasing soil carbon sink through anthropogenic effects.

Diffusion↗
PubMed2004

[Microbial characteristics of straw-amended degraded soils in central Tibet and its effect on soil fertility].

This paper studied the dynamics of microbial communities in degraded soils of central Tibet under straw amendment and its effect on soil fertility. The results showed that straw amendment, and soil covering with spring highland barley (Hordeum vulgare var. nudum) straw in particular, could supply a beneficial soil environment for the relatively balanced growth of soil microbes, e.g., reduced water evaporation, appropriate temperature, and increased content of organic matter and nutrients. All the results demonstrated the possibility of straw amendment in recovering soil fertility and in reconstructing of soil structure in a relatively short period.

Carbon↗
PubMed1986

[Calcium, phosphorus and magnesium levels in the soil, grass and the body of bulls after irrigation of the soil with sewage water].

The aim of the studies was determination of the influence of irrigation with the water of the river Ner on the content of calcium, phosphorus and magnesium in soil, plants and organism of bulls fed on the hay grown on the irrigated soil. The soil irrigated with waste water, its vegetation and 30 bulls of the Black and White breed used in this experiment. The bulls were divided into three groups. The experiment was repeated twice and lasted 93 days each time. The animals from group I and II were given the hay from the meadows irrigated with waste water. The second group of bulls received the hay from the soil which was irrigated more intensively. The animals from group III received the hay from non-irrigated soils. The daily ration of food consisted of 5 kilograms of hay and 3 kilograms of dry beet pulp. Calcium, phosphorus and magnesium were found in the soil, in hay and in the bulls blood serum. Magnesium was found in the bull's hair. The irrigation with the Ner's water increased the amount of calcium and magnesium in the soil and its vegetation. No influence of the irrigation with waste water on the content of phosphorus in hay was observed. No definite relationship between the levels of Ca, P and Mg in food and in the bull's blood serum was observed; however, a relation between the amount of magnesium in food and in the bull's hair was found.

Animal Feed↗
PubMed2002

Effects of soil amendment on gas depth profiles in soil monoliths using direct mass spectrometric measurement.

Land use and agricultural practices are known to influence the source and sink concentrations of various gases, including greenhouse gases (NOx CH4 and CO2). in soils. With everincreasing production of domestic sewage sludge and the prohibition of disposal at sea, pressure on waste disposal increases. Anaerobically digested domestic sewage sludge and/or lime were applied to an upland. Scottish soil and their effects on gas depth profiles monitored as indicators of microbial processes of the soil ecosystem. The concentrations of various gases (Ar, O2. CO2, CH4, N2, NOx) were measured simultaneously at each depth using membrane inlet mass spectrometry (MIMS). This technique enables the direct measurement of multiple gas species throughout soil cores with minimal disturbance. Intact soil monoliths were collected from the sample site, following amendment, and maintained in a constant temperature, environmental growth chambers. Statistical analyses (one-way ANOVA and LSD tests) were conducted to identify the depths at which gas concentrations in amended cores were significantly different from those in control (un-amended) cores. Significant effects were observed on the concentration of CO2, CH4, NOx and N2 at certain depths. Average CH4 concentration was consistently higher (>1 microM) in the upper horizon following application of sludge and sludge and lime together. N2 and NOx concentrations were elevated in cores treated with lime by approximately 100 and 32 microM. respectively, in much of the upper horizon. CO2 concentration increased above control mean values, at certain depths, following application of either sludge or lime. Some explanation for the changes in soil gas concentration was provided by reference to the microorganism assemblages and the gases associated with biochemistry of nitrification, denitrification, methane oxidation and methanogenesis.

Argon↗
PubMed2006

Collection and storage of CO2 for 13C analysis: An application to separate soil CO2 efflux into root- and soil-derived components.

Soil surface CO2 efflux is comprised of CO2 from (i) root respiration and rhizosphere microbes and (ii) heterotrophic respiration from the breakdown of soil organic matter (SOM). This efflux may be partitioned between these sources using delta13C measurements. To achieve this, continuous flow isotope ratio mass spectrometry can be used and, in conjunction with 10 mL septum-capped vials, large numbers of samples may be analysed using a Finnigan MAT Delta(plus)XP interfaced to a Gas Bench II. Here we describe a number of advances to facilitate such work, including: (i) a technique for monitoring mass spectrometer performance, (ii) improvements to sample storage, and (iii) a gas-handling system for incubating and sampling the CO2 derived from roots and soils. Mass spectrometer performance was monitored using an automated refillable vial. Compressed air analysed with this system had mean delta13C of -9.61 +/- 0.16 per thousand (+/- 1sigma, n = 28) collected over four runs. Heating the butyl rubber septa used to seal the vials at 105 degrees C for 12 h improved the sample storage. After air transportation over 12 days, the isotope composition of the CO2 at ambient concentrations was unchanged (before: -35.2 +/- 0.10 per thousand, n = 4; after: -35.3 +/- 0.10 per thousand, n = 15); without heat treatment of the septa the CO2 became slightly enriched (-35.0 +/- 0.14 per thousand, n = 15). The linearity of the Gas Bench II was found to decline above 8000 micromol CO2 mol(-1). To stay within a linear range and to allow the incubation of soil and root material we describe a gas-handling system based around a peristaltic pump. Finally, we demonstrate these methods by growing a C-4 grass (Guinea grass, Panicum maximum Jacq.) in a C-3 soil. Root respiration was found to contribute between 5 and 22% to the soil surface CO2 efflux. These methodologies will facilitate experiments aimed at measuring the isotopic composition of soil-derived CO2 across a range of ecological applications.

Journal Article↗
PubMed1992

Soil water content, soil strength and the growth of elm root suckers.

The elongation rate of root suckers of Dutch elm (Ulmus x hollandica Mill.) increased with increasing age of the sucker, soil water content and net growth pressure (the excess of turgor pressure over soil restraining pressure) and it decreased with increasing soil strength. The increase in the rate of sucker elongation with age was probably the result of a decrease in osmotic potential causing an increase in the turgor pressure. Increasing soil strength increased the rate of osmotic adjustment. The increase in the rate of sucker elongation with increasing soil water content was probably due to an increase in the water potential of the sucker and a decrease in soil strength associated with increasing soil water content.

Journal Article↗
PubMed1989

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 x 10 versus 2 x 10 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.

Journal Article↗
PubMed1990

New method for extraction of streptomycete spores from soil and application to the study of lysogeny in sterile amended and nonsterile soil.

A new method for the isolation and enumeration of streptomycete spores from soil was developed. This method makes use of a cation-exchange resin to disperse soil particles. It allowed the detection of 10 spores in 100 g of sterile soil, while ca. 10 could be accurately enumerated in 100 g. This method was applied to studying the fate of a marked actinophage in soil. In sterile amended and nonsterile soil, relatively high numbers of actinophages were only found during the first few days of the experiment when the host streptomycete was in the mycelial form. Later, after sporulation, lysogens could be detected in sterile amended soil and could still be found 60 days after inoculation. Although no lysogens were found in nonsterile soil, the introduced phage could still be detected in the free state after 60 days, albeit at a low titer.

Journal Article↗
PubMed1996

Importance of Preferential Flow and Soil Management in Vertical Transport of a Biocontrol Strain of Pseudomonas fluorescens in Structured Field Soil.

The large-scale release of wild-type or genetically modified bacteria into the environment for control of plant diseases or for bioremediation entails the potential risk of groundwater contamination by these microorganisms. For a model study on patterns of vertical transport of bacteria under field conditions, the biocontrol strain Pseudomonas fluorescens CHA0, marked with a spontaneous resistance to rifampin (CHA0-Rif), was applied to a grass-clover ley plot (rotation grassland) and a wheat plot. Immediately after bacterial application, heavy precipitation was simulated by sprinkling, over a period of 8 h, 40 mm of water containing the mobile tracer potassium bromide and the dye Brilliant Blue FCF to identify channels of preferential flow. One day later, a 150-cm-deep soil trench was dug and soil profiles were prepared. Soil samples were extracted at different depths of the profiles and analyzed for the number of CHA0-Rif cells and the concentration of bromide and Brilliant Blue FCF. Dye coverage in the soil profiles was estimated by image analysis. CHA0 was present at 10(sup8) CFU/g in the surface soil, and 10(sup6) to 10(sup7) CFU/g of CHA0 was detected along macropores between 10 and 150 cm deep. Similarly, the concentration of the tracer bromide along the macropores remained at the same level below 20 cm deep. Dye coverage in lower soil layers was higher in the ley than in the wheat plot. In nonstained parts of the profiles, the number of CHA0-Rif cells was substantially smaller and the bromide concentration was below the detection limit in most samples. We conclude that after heavy rainfall, released bacteria are rapidly transported in large numbers through the channels of preferential flow to deeper soil layers. Under these conditions, the transport of CHA0-Rif is similar to that of the conservative tracer bromide and is affected by cultural practice.

Journal Article↗
PubMed2006

Evaluation of the bioavailability of the herbicide prosulfocarb through adsorption on soils and model soil colloids, and through a simple bioassay.

Adsorption isotherms of prosulfocarb were determined on soils with different physicochemical properties. The extent of adsorption increased with the organic carbon content, but the results also suggested the involvement of some inorganic soil surfaces. In order better to understand the role of each soil surface, adsorption-desorption isotherms were determined on model soil colloids consisting of a soil humic acid, a montmorillonite, a synthetic aluminium hydroxide and their associations. The highest adsorption was observed on the humic acid, but it was also confirmed that the montmorillonite interacted with prosulfocarb. In contrast, the aluminium hydroxide was not active and its association with montmorillonite provoked a decrease in adsorption compared with montmorillonite alone. Except for humic acid, the highest adsorption took place on the ternary association montmorillonite-aluminium hydroxide-humic acid. On each surface tested, the adsorption was largely reversible and decreased at increasing pH. The herbicidal activity of prosulfocarb was tested by the determination of the germination and growth of a typical weed, Lolium multiflorum Lam, in contact with prosulfocarb solutions at different concentrations. The herbicide did not prevent the germination of the seeds but inhibited the growth of the roots and leaves. The same test was performed in the presence of the ternary system to evaluate the influence of adsorption on the plant bioavailability. It was concluded that the presence of an adsorptive surface reduced the herbicidal activity and that the simple bioassay proposed could be useful in predicting the extent of adsorption in a given soil.

Adsorption↗
PubMed2006

Root controls on soil microbial community structure in forest soils.

We assessed microbial community composition as a function of altered above- and belowground inputs to soil in forest ecosystems of Oregon, Pennsylvania, and Hungary as part of a larger Detritus Input and Removal Treatment (DIRT) experiment. DIRT plots, which include root trenching, aboveground litter exclusion, and doubling of litter inputs, have been established in forested ecosystems in the US and Europe that vary with respect to dominant tree species, soil C content, N deposition rate, and soil type. This study used phospholipid fatty-acid (PLFA) analysis to examine changes in the soil microbial community size and composition in the mineral soil (0-10 cm) as a result of the DIRT treatments. At all sites, the PLFA profiles from the plots without roots were significantly different from all other treatments. PLFA analysis showed that the rootless plots generally contained larger quantities of actinomycete biomarkers and lower amounts of fungal biomarkers. At one of the sites in an old-growth coniferous forest, seasonal changes in PLFA profiles were also examined. Seasonal differences in soil microbial community composition were greater than treatment differences. Throughout the year, treatments without roots continued to have a different microbial community composition than the treatments with roots, although the specific PLFA biomarkers responsible for these differences varied by season. These data provide direct evidence that root C inputs exert a large control on microbial community composition in the three forested ecosystems studied.

Plant Roots↗
PubMed2006

The role of indigenous bacterial and fungal soil populations in the biodegradation of crude oil in a desert soil.

The biodegradation capacity of indigenous microbial populations was examined in a desert soil contaminated with crude oil. To evaluate biodegradation, soil samples supplemented with 5, 10 or 20% (w/w) of crude oil were incubated for 90 days at 30 degrees C. The effect of augmentation of the soil with vermiculite (50% v/v) as a bulking agent providing increased surface/volume ratio and improved soil aeration was also tested. Maximal biodegradation (91%) was obtained in soil containing the highest concentration of crude oil (20%) and supplemented with vermiculite; only 74% of the oil was degraded in samples containing the same level of crude oil but lacking vermiculite. Gas chromatograms of distilled fractions of crude oil extracted from the soil before and after incubation demonstrated that most of the light and part of the intermediate weight fractions initially present in the oil extracts could not be detected after incubation. Monitoring of microbial population densities revealed an initial decline in bacterial viable counts after exposure to oil, presumably as a result of the crude oil's toxicity. This decline was followed by a steep recovery in microbial population density, then by a moderate increase that persisted until the end of incubation. By contrast, the inhibitory effect of crude oil on the fungal population was minimal. Furthermore, the overall increased growth response of the fungal population, at all three levels of contamination, was about one order of magnitude higher than that of the bacterial population.

Aluminum Silicates↗
PubMed2005

Effects of a soil conditioner on some physical and biological features of soils: results from a greenhouse study.

A soil amendment substance-organic bio-stimulator, Terralyt Plus (TP), was used to observe its impact on the properties of clay loam (CL), sandy clay loam (SCL) and sandy loam (SL) soils and the growth of corn (Zea mays indentata L.) and wheat (Triticum aestivum ssp./vulgare Vill. v. lutescens) under greenhouse conditions. The diluted TP solutions (1:500, 1:1000 and 1:2000) were sprayed onto the soil surfaces. The wheat growth increased for CL and SCL with the application of TP at 1:1000. The highest dry weights were detected with 1:500 TP and corn in all the soils. Penetration resistance of CL containing corn increased with increasing TP concentration. TP was also effective in improving the aggregate stability for CL but not for the other soils. Catalase enzyme activity (CEA), soil evolution (SE) and the total aerobic bacterial population (TABP) were significantly increased (P<0.05) by spraying TP at 1:1000 onto CL.

Agriculture↗
PubMed2005

Photo-Fenton treatment of TNT contaminated soil extract solutions obtained by soil flushing with cyclodextrin.

The technical feasibility and performances of coupling flushing abilities of cyclodextrin solutions for 2,4,6-trinitrotoluene (TNT) removal from contaminated soil and the ability of Photo-Fenton treatment for final disposal of soil extract solutions containing high TNT loads have been investigated at laboratory scale. Methylated-beta-cyclodextrin (MCD) has shown better ability than hydroxypropyl-beta-cyclodextrin (HPCD) to complex TNT. The MCD solution increased the aqueous concentration of TNT in soil extract effluents as much as 2.1 times the concentrations obtained during the water flush of the soil. TNT in soil extract solution has been treated by Photo-Fenton. Our results indicate that MCD has a beneficial effect on the degradation rates of TNT. This relative improvement of TNT degradation rate (1.3 time) in presence of high amounts of hydroxyl radical scavengers can be ascribed to the formation of a ternary complex (TNT-cyclodextrin-iron) which can direct hydroxyl radical reaction toward TNT. Complete mineralization of soil extraction solutions was not achieved and TNT degradation pathway has been elucidated in order to ensure that no potential toxic intermediate is left at the end of the treatment time. After successive TNT hydroxylations, oxidative opening of the TNT aromatic ring quickly occurred, leading to the accumulation of short chain carboxylic acids such as oxalic acid and formic acid.

Cyclodextrins↗