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Seasonal and annual changes in soil respiration in relation to soil temperature, water potential and trenching.

Soil respiration (rs), soil temperature (Ts) and volumetric soil water content were measured in a balsam fir (Abies balsamea (L.) Mill.) ecosystem from 1998 to 2001. Seasonal variation in root and microbial respiration, and covariation in abiotic factors confounded interpretation of the effects of Ts and soil water potential (Psis) on rs. To minimize the confounding effect of temperature, we analyzed the effect of Psis on rs during the summers of 1998-2000 when changes in Ts were slight. Soil respiration declined 25-50% in response to modest water stress (minimum Psis of -0.6 to -0.2 MPa), and between years, there was substantial variation in the relationship between rs and Psis. In the summer of 2000, 2-m2 plots were subjected to drought for 1 month and other plots were irrigated. The relationship between summertime rs and Psis in the experimental plots was similar to that estimated from the survey data obtained during the same summer. In late spring and early autumn of 2001, 2-m2 trenched and untrenched plots were subjected to drought or exposed to rainfall. It was dry in the early autumn and there was severe soil drying (Psis of -10 MPa in untrenched plots and -2 MPa in trenched plots). In spring, rs in untrenched plots responded more to modest water stress than rs in trenched plots, indicating that root respiration is more sensitive than microbial respiration to water stress at this time of year. The response to abiotic factors differed significantly between spring and autumn in untrenched plots but not in trenched plots, indicating that root activity was greater in early autumn than in late spring, and that roots acclimated to the sustained, severe water stress experienced before and during the autumn.

Abies↗

Effects of brash removal after clear felling on soil and soil-solution chemistry and field-layer biomass in an experimental nitrogen gradient.

Biofuels, such as brash from forest fellings, have been proposed as an alternative energy source. Brash removal may affect the sustainability of forest production, e.g., through a change in the availability of cations and N in the soil. We report initial effects of brash removal on inorganic N content in humus and mineral soil, soil-solution chemistry, and field-layer biomass after clear felling an N-fertilisation experiment in central Sweden. The experiment comprised six different fertiliser levels, ranging from 0 to 600 kg N ha(-1). Urea was given every 5th year during 1967 to 1982 to replicated plots, giving total doses of 0 to 2400 kg N ha(-1). Clear felling took place in 1995, 13 years after the last fertilisation. The removal of brash decreased the NO3- content in the humus layer after clear felling. A decrease in the NO3- concentration of the soil solution was indicated during most of the study period as well. No effect of the previous N fertilisation was found in the humus layer, but in the mineral soil there was an increase in NO3- content for the highest N dose after clear felling ( p = 0.06). The soil-solution chemistry and the field-layer biomass showed an irregular pattern with no consistent effects of brash removal or previous fertilisation.

Agriculture↗

Intact soil-core microcosms compared with multi-site field releases for pre-release testing of microbes in diverse soils and climates.

Intact soil-core microcosms were used to compare persistence of Pseudomonas chlororaphis 3732RN-L11 in fallow soil and on wheat roots with field releases at diverse sites. Parallel field and microcosm releases at four sites in 1996 were repeated with addition of one site in 1997. Microcosms were obtained fresh and maintained at 60% soil water holding capacity in a growth chamber at 70% relative humidity, a 12-hour photoperiod, and constant temperature. Persistence of 3732RN-L11 was measured at each site in field plots and microcosms at 7-21 day intervals, and in duplicate microcosms sampled at an independent laboratory. Linear regression slopes of field plot and microcosm persistence were compared for each site, and between identical microcosms sampled at different sites, using log10 transformed plate counts. Microcosm persistence closely matched field plots for wheat roots, but persistence in fallow soil differed significantly in several instances where persistence in field plots was lower than in microcosms. Analysis of weather variations at each site indicated that rainfall events of 30-40 mm caused decreased persistence in fallow soil. Cooler temperatures enhanced persistence in field plots at later time points. Inter-laboratory comparison of regression slopes showed good agreement for data generated at different sites, though in two instances, longer sampling periods at one site caused significant differences between the sites. Soil characteristics were compared and it was found that fertility, namely the carbon to nitrogen ratio, and the presence of expanding clays, were related to persistence. These microcosm protocols produced reliable data at low cost, and were useable for pre-release risk analyses for microorganisms.

Agriculture↗

Effects and risk assessment of linear alkylbenzene sulfonates in agricultural soil. 3. Sublethal effects on soil invertebrates.

Sewage sludge applied to agricultural soils often contains considerable amounts of linear alkylbenzene sulfonates (LAS). Toxic effects of LAS on soil organisms should, therefore. be evaluated to ensure safe use of sewage sludge as a fertilizer. In this study, dose-response relationships for the toxicity of Na-LAS to six species of soil invertebrates (survival, reproduction, and growth) were established using a sandy, agricultural soil as test substrate. In general, toxic effects on reproduction and growth appeared when the concentration in soil exceeded 40 to 60 mg/kg. Reproduction was approximately fourfold more sensitive in earthworms and enchytracids than in springtails and mites. It is argued that this difference in sensitivity is related to the dependency of soil pore water, which is high in the annelids but comparatively low in the arthropods.

Agriculture↗

Determination of the As(III)/As(V) ratio in soil by X-ray absorption near-edge structure (XANES) and its application to the arsenic distribution between soil and water.

The details of a method used to determine the As(III)/As(V) ratio in soil by arsenic K-edge XANES spectroscopy are described. The spectra of mixtures of NaAs(III)O2 and NaH2As(V)O4, conducted for an As(III)/As(V) calibration, were well-fitted by combining normalized spectra of NaAsO2 and Na2HAsO4, where the coefficients multiplied by the normalized spectra were identical to the molar ratio of As(III) and As(V) in the mixtures. XANES spectra of arsenic in soil samples could also be fitted by a linear combination of the spectra of NaAsO2 and Na2HAsO4, which enabled us to estimate the As(III)/As(V) in a soil containing 10.2 mg/kg arsenic. The As(III)/As(V) ratio in the soil was compared with that of a soil solution contacted with the soil determined by HPLC-ICP-MS, showing that As(III) is distributed to water more readily than As(V). The application of the XANES method is important for a better understanding of the behavior of As(III) and As(V) independently in a natural aquifer.

Arsenic↗

Hurricane-loaded soil: effects on nitric oxide emissions from soil.

The nitric oxide (NO) flux from eastern North Carolina soils subjected to flooding from hurricanes were studied in laboratory experiments. Three sites along the Neuse River basin in eastern North Carolina that sustained different intensities of flooding in September 1999 from Hurricane Floyd were examined. Hurricane Floyd impacted the Neuse River basin by inducing flooding that damaged and disabled hog (Sus scrofa) lagoons and municipal wastewater treatment plants. Between approximately 53 and 325 million liters (14 and 86 million gallons) of untreated hog waste and between approximately 5.7 and 34.4 billion liters (1.5 and 9.1 billion gallons) of untreated municipal wastewater are projected to have entered the Neuse River basin, increasing the concentrations of nitrogen (N), phosphorus (P), and total solids. Phosphorus and total solids are projected to have increased 3.2 and 199.2 mg/L, respectively. Total N was projected to have increased by 9.8 mg/L, which is posited to have increased the NO flux from flooded soils for months after the hurricane. Nitric oxide emissions from soil can adversely affect ozone levels in the lower troposphere. Minimization of NO flux from soil is advantageous, protecting air quality as well as conserving valued nitrogen fertilizers. Hurricane-loaded soils were found to produce more than 30 times greater NO emissions than nonflooded soils with NO fluxes ranging from 0.1 to 102.5 ng N/(m2 s).

Disasters↗

Prediction of soil organic partition coefficients by a soil leaching column chromatographic method.

The soil organic partition coefficient (Koc) is one of the most important parameters to depict the transfer and fate of a chemical in the soil-water system. Predicting Koc by using a chromatographic technique has been developing into a convenient and low-cost method. In this paper, a soil leaching column chromatograpy (SLCC) method employing the soil column packed with reference soil GSE 17201 (obtained from Bayer Landwirtschaftszentrum, Monheim, Germany) and methanol-water eluents was developed to predict the Koc of hydrophobic organic chemicals (HOCs), over a log Koc range of 4.8 orders of magnitude, from their capacity factors. The capacity factor with water as an eluent (k'w) could be obtained by linearly extrapolating capacity factors in methanol-water eluents (k'w) with various volume fractions of methanol (symbol in text). The important effects of solute activity coefficients in water on k'w and Koc were illustrated. Hence, the correlation between log Koc and log k'w (and log k') exists in the soil. The correlation coefficient (r) of the log Koc vs. log k'w correlation for 58 apolar and polar compounds could reach 0.987, while the correlation coefficients of the log Koc -log k' correlations were no less than 0.968, with (symbol in text)ranging from 0 to 0.50. The smaller the (symbol in text), the higher the r. Therefore, it is recommended that the eluent of smaller (symbol in text), such as water, be used for accurately estimating Koc. Correspondingly, the r value of the log Koc -log k'w correlation on a reversed-phase Hypersil ODS (Thermo Hypersil, Kleinostheim, Germany) column was less than 0.940 for the same solutes. The SLCC method could provide a more reliable route to predict Koc indirectly from a correlation with k'w than the reversed-phase liquid chromatographic (RPLC) one.

Chromatography, Liquid↗

Survival of Salmonella on tomatoes stored at high relative humidity, in soil, and on tomatoes in contact with soil.

Salmonellosis has been linked to the consumption of several types of raw fruits and vegetables, some of which may have been contaminated with Salmonella before harvesting. The objectives of this study were to investigate water and soil as reservoirs of Salmonella for the contamination of mature green tomato fruits. Salmonella survived for at least 45 days in inoculated moist soil. The population of Salmonella on tomatoes in contact with soil increased by 2.5 log10 CFU per tomato during storage for 4 days at 20 degrees C and remained constant for an additional 10 days. The number of cells inoculated on tomatoes decreased by approximately 4 log10 CFU per tomato during storage for 14 days at 20 degrees C and 70% relative humidity. Fruits in contact with inoculated soil for 1 day at 20 degrees C harbored Salmonella only near or on the skin surface. More Salmonella cells were observed in stem scar and subsurface areas of tomatoes as the time of storage increased. PCR fingerprinting revealed that among five Salmonella serotypes in the inoculum, Salmonella Montevideo was the most persistent on tomatoes in contact with inoculated soil and on spot-inoculated tomatoes, followed by Salmonella Poona and Salmonella Michigan. The results of this study demonstrate that an enhanced green fluorescent protein marker can be used to detect cells and monitor the growth of Salmonella in the presence of other microorganisms. Observations on the infiltration of Salmonella into tomato tissues support the contention that preharvest contact of produce with contaminated water or soil exacerbates problems associated with the postharvest removal of pathogens or their accessibility to treatment with sanitizers.

Bacterial Typing Techniques↗

Soil contamination and infections by soil-transmitted helminths in an endemic village in southern Thailand.

The aim of this study was to test the association between soil contamination and infection of the household members by soil-transmitted helminths in dry and rainy seasons. A lake-side community in southern Thailand with a population of 2,340 was studied twice, in the dry season and rainy season of 1995. Fifty households were randomly selected. Soil samples near the latrine, in the yard, at the foot-washing area and under the trees were taken and analysed for presence of helminthic eggs. All members of the selected household were interviewed and stool samples obtained. Age-adjusted odds ratios of presence of Ascaris and Trichuris eggs in the household soil for ascariasis and trichuriasis were 10.5 (95% CI 1.5-77.1) and 5.5 (95% CI 2.4-12.7) in dry season and 10.4 (95% CI 2.5-43.8) and 8.3 (95% CI 3.4-20.0) in rainy season. The levels of hookworm eggs detected in the soil were too low to test the association. Soil analysis for eggs of Ascaris and Trichuris may be used to predict infections among the household members but not that for hookworm.

Ascariasis↗

[Evaluation on soil anti-erodibility of soil and water conservation forest].

Indexes including organic matter content, water stable aggregate content, mean weight diameter of water stable aggregate, aggregate degree and disperse coefficient were selected to evaluate soil anti-erodibility of soil and water conservation forests component of different tree species at different ages. The results showed that soil and water conservation forest played an important role in improving soil anti-erodibility, especially to the topsoil. Compared with that of Chinese pine pure forests, Chinese pine-broadleaved mixed forests had higher soil organic matter content, and water stable aggregate content increased by 1.71%-38.53%, and soil anti-erodibility was also increased with increasing stand age.

China↗

[Transformation characteristics of sulfur forms in acid sulfate soils under different soil water conditions].

Aimed to detect the quantitative impact of soil water condition on the transformation of sulfur forms in acid sulfate soils (ASS), a simulation test was made with 8 treatments. The results indicated that water was an important factor affecting the transformation processes. Wet but not inundated or over dried condition was benefit to the oxidation of pyrite S and the formation of water soluble S (WS-S) and exchangeable S (Ex-S) in ASS. In the three treatments with different inundated and drained off cycles, soil pyrite S content averagely decreased 1.29-3.20 g x kg(-1) during a single drained off period, while soil WS-S and Ex-S contents averagely increased 0.90-1.63 and 0.58-1.47 g x kg(-1), respectively. During inundated period, soil pyrite S content was relatively stable, but soil WS-S and Ex-S contents were decreased significantly due to the dilution of water. It was suggested that the total S (mainly WS-S) of ASS was discharged in drainage process, and the accumulative amount of the discharge and the transformation of the S forms were associated with the length of the inundated and drained off cycles. The dynamics of Jarosite S, organic S and element S in all treatments were also discussed here.

Iron↗

[Variation of soil temperature before and after cultivation of marsh and its effect on soil thermal regime].

Marsh has important ecological and environmental functions and is sensitive to the global climate change, while the variation of soil temperature could better indicate the climate fluctuation. Our study showed that the annual and seasonal dynamic changes of soil temperature in marsh showed distinctly "sinusoid" character curve, whereas the mean annual temperature of different soil depths showed "U" feature. From May to September, the mean temperature at the topsoil (10 cm) of uncultivated marsh was 11.69 +/- 3.04 degrees C, while that of cultivated marsh was 15.80 +/- 3.41 degrees C. The soil respiration rate of uncultivated marsh in August and September was 156.41 +/- 76.91 mg x m(-2) x h(-1) and 116.75 +/- 57.43 mg x m(-2) x h(-1), accounted for 14.6% and 13.1% of that of cultivated marsh, respectively. The soil temperature was significantly positively correlated with soil respiration.

Crops, Agricultural↗

[The potassium metabolism of typical northern Algerian soils. I. Global evaluation of the potassium supply of soils].

In samples from 87 and 39 profiles, respectively, of typical Northern Algerian soils the following parameters were determined of the K content: total K, exchangeable and water soluble K, K saturation degree, and potassium replenishment capacity. The latter was carried out by four methods (N HCl 50 degrees C, HNO3 boiling, 0.05 and 0.2 N NaTPB). The results obtained were used to check the widespread view that Algerian soils are well supplied with K. The following grouping is suggested from the results of the investigation: --soils with high to very high values for all forms of K (50% of the samples), --soils with lower and medium values for exchangeable K, which require K fertilization actually or in the near future if K uptake by crops increases (30 to 35% of the samples), --soils with TPB values indicating a high binding strength of Ki in which a very limited replenishment power can be expected despite partly high or very high values of acid soluble K (more than 25% of the samples). These results indicate that it is necessary to differentiate the assessment of the K content of Algerian soils.

Algeria↗

[Public health evaluation of (hazardous) substances in soil--concept of the AGU and Department of "Tolerable (Hazardous) Substance Concentrations in Soil" for metals].

Up to now no uniform procedure and no generally accepted values exist for health evaluation of pollutants in soil. Aim of the working group for environmental hygiene (AGU) of the Bavarian Ministry of Labour and Social Order, Family, Women and Health is to propose health-based procedures and values for assessment, in consideration of existing concepts and regulations. Basis for health evaluation is the existence of appropriate soil investigations. This refers to the sampling scheme (sampling depth, sampling site and manner, number and representativity of samples) as well as sample preparation and analysis. The "still tolerable pollutant concentration in soil" (TSKB) is supposed to mark a threshold which separates a range of tolerable pollutant concentration from a range where soil-related measures are indicated. Basis for determination of a TSKB-value is the estimation of the average uptake of the respective substance via air, drinking water and food. From this the average level of a tolerable dosis without health risk by regular long-term uptake by humans is calculated. From the remaining portion of tolerable uptake the TSKB-value for the additional pathway of uptake by soil is derived. The estimations are representatively performed for 3-year old children, because small children are especially endangered by uptake of polluted soil. TSKB-values were determined by this procedure for the metals As, Cd, Cr, Cu, Hg, Ni, Pb, Zn and compared with assessment criteria and values of other working groups.

Adult↗

Application of solid phase microextraction for the determination of soil fumigants in water and soil samples.

The potential of solid phase microextraction (SPME) for the determination of the soil fumigants 1,3-dichloropropene (1,3-DCP) and methyl isothiocyanate (MITC) in environmental samples such as soil and water samples has been investigated. Direct immersion SPME followed by GC/ECD/NPD analysis allowed the rapid determination of the two fumigants in water samples, with very little sample manipulation, giving an LOD of 0.5 microg L(-1). Precision, calculated as relative standard deviation (RSD) for six replicates at three concentration levels, was found to be lower than 20% at the concentration levels tested. For the analysis of soil samples, headspace (HS)-SPME combined with GC/ECD/NPD analysis has been applied. Quantification using matrix-matched calibration curves allowed determination of both analytes (MITC and 1-3-DCP) with a LOD of 0.1 microg kg(-1) (RSD < 10%) for the two concentration levels assayed (0.02 and 0.2 mg kg(-1)). The HS-SPME procedure developed in this paper was applied to soil samples from experimental green house plots treated with metham-Na, a soil disinfestation agent that decomposes in soil to MITC. The absence of sample manipulation as well as the low solvent consumption in SPME methodology are among the main advantages of this analytical approach.

Journal Article↗

Mobility of aniline, benzoic acid, and toluene in four soils and correlation with soil properties.

Soil properties and retention mechanisms affecting the relative mobility of aniline, benzoic acid, and toluene in Cecil sandy loam (clayey, kaolinitic, thermic Typic Hapludults), Holdredge silt loam (fine-silty, mixed, mesic Typic Argiustolls), Sharpsburg silty clay loam (fine, montmorillonitic, mesic Typic Argiudolls), and Valentine fine sand (mixed, mesic Typic Ustipsamments) were delineated in laboratory studies. The effect of the synthetic organic compounds (SOCs) was also determined on effective organic campounds (SOCs) was also determined on effective cation exchange capacity (ECEC) of the soils. Benzoic acid was most mobile of the SOCs but was retained in the Cecil soil by hydrogen bonds to Fe oxides. Toluene was least mobile and probably was hydrophobically sorbed to all soils. Aniline was electrostatically retained in protonated form to organic and inorganic exchange sites of the soils and reduced the ECEC of aniline-treated Holdredge and Sharpsburg soils.

Journal Article↗

Changes in sulphate retention, soil chemistry and drainage water quality along an upland soil transect.

Soils sampled along an altitudinal transect in an upland area of North East Scotland have been used to investigate downslope changes in the capacity of soils to retain sulphate. Simulated laboratory experiments involving the leaching of reconstituted cores with 'rainfall' containing low (1.85 mg litre(-1) and high (51.90 mg litre(-1) concentrations of sulphate indicate that soils developed on upper slopes have a limited capacity to adsorb sulphate, whereas soils on lower slopes have a much greater sulphate adsorption capacity. Soil drainage water, produced from 'sensitive' upper slope soils may therefore be significantly modified by physico-chemical reactions in lower slopes before reaching watercourses.

Journal Article↗