Enumeration of sulfur-oxidizing populations in Saskatchewan agricultural soils

1991 ◽  
Vol 71 (1) ◽  
pp. 127-136 ◽  
Author(s):  
J. R. Lawrence ◽  
J.J. Germida
Keyword(s):  
Soil Properties ◽  
Soil Ph ◽  
Oxidation Rate ◽  
Elemental Sulfur ◽  
Agricultural Soils ◽  
Clay Content ◽  
Sulfur Oxidation ◽  
Sand Content ◽  
Sulfur Oxidizing ◽  
S Oxidation

Heterotrophic and autotrophic sulfur-oxidizing populations in 35 Saskatchewan agricultural soils were enumerated. These populations included heterotrophs that produce thiosulfate and or sulfate during elemental sulfur (S°) oxidation, heterotrophic thiosulfate oxidizers, and autotrophic thiosulfate oxidizers. Populations of Thiobacillus thiooxidans and T. ferrooxidans were not detected in any of the soils tested. Heterotrophs that oxidized S° to thiosulfate as the major oxyanion were the most abundant oxidizers enumerated (107–108 cells g−1) and were found in all soils. Autotrophic thiosulfate-oxidizers were detected in 10 of the soils surveyed. Heterotrophic S° and thiosulfate-oxidizing populations exhibited positive trends with soil pH, total-S, hydriodic reducible-S, and clay content, whereas populations of autotrophic thiosulfate oxidizers were negatively correlated with these factors and positively related to sand content and increasing C:S ratios. In soils containing autotrophic thiosulfate oxidizers the amount of thiosulfate relative to sulfate detected was reduced although no effect on S° oxidation rate was detected. Amendment of 15 selected agricultural soils with 0.5% S° significantly reduced total heterotrophic populations, whereas autotrophic thiosulfate oxidizers increased from undetectable levels to 104 cells g−1. Therefore most Saskatchewan soils contain abundant populations of heterotrophic S° oxidizers, and populations of autotrophs that respond to S° applications. Key words: Sulfur oxidation, autotrophic sulfur oxidizers, heterotrophic sulfur oxidizers, soil properties

ELEMENTAL SULFUR OXIDATION AS INFLUENCED BY PLANT GROWTH AND DEGREE OF DISPERSION WITHIN SOIL

1990 ◽  
Vol 70 (3) ◽  
pp. 499-502 ◽  
Author(s):  
H. H. JANZEN
Keyword(s):  
Plant Growth ◽  
Key Words ◽  
Oxidation Rate ◽  
Elemental Sulfur ◽  
Sulfur Oxidation ◽  
Particle Dispersion ◽  
Controlled Environment ◽  
Oxidation Rates ◽  
S Oxidation ◽  
Elemental Sulfur Oxidation

Controlled environment studies were conducted to characterize the effects of cropping treatment and degree of particle dispersion on S oxidation rate. In two soils (a Chernozem and a Luvisol), S oxidation rates were not greatly affected by cropping treatment (barley, beans, canola, or fallow). In a second experiment, S oxidation was shown to approach maximum rates at a dispersion level of 1000 g soil g−1 S. Key words: Sulfur, placement, rhizosphere, fertilizer, elementals

Effect of nutrients and elemental sulfur particle size on elemental sulfur oxidation and the growth of Thiobacillus thiooxidans

1997 ◽  
Vol 48 (4) ◽  
pp. 497 ◽  
Author(s):  
Sholeh ◽  
Rod D. B. Lefroy ◽  
Graeme J. Blair
Keyword(s):  
Particle Size ◽  
Elemental Sulfur ◽  
Sulfur Oxidation ◽  
Thiobacillus Thiooxidans ◽  
Oxidation Rates ◽  
South Wales ◽  
Incubation Experiments ◽  
P Rate ◽  
Oxidation Model ◽  
S Oxidation

Elemental sulfur (S) has many attractions as a fertiliser but it must be oxidised to sulfate before it is plant available. Two laboratory incubation experiments with a high S sorbing basaltic soil (Haplohumult) from Walcha, New South Wales, are reported here. The first experiment was conducted to study the effect of ? P and other nutrients on the oxidation of elemental S and the growth of Thiobacillus thiooxidans. The second experiment studied the effect of phosphorus (P) rate, elemental S particle size, and elemental S form on the oxidation of elemental S at different times. There were significant differences between treatments in the percentage and amount of elemental S oxidised, with the lowest oxidation occurring during the 6-week incubation in the P treatment, which represented 1�8% of the applied S compared with 16�0% when all nutrients were supplied. There was a significant linear relationship between T. thiooxidans population at the end of the incubation period and the amount of elemental S oxidised. The oxidation of elemental S was higher when fine (50?150 �m) particle size elemental S was used, compared with coarse (150?250 �m) elemental S. There was no clear difference in oxidation rate between ground and recrystallised elemental S. The S oxidation rates recorded in these experiments were compared with those predicted by an S oxidation model and found to be in close agreement.

SULFUR ISOTOPE FRACTIONATION DURING THE OXIDATION OF ELEMENTAL SULFUR BY THIOBACILLI IN A SOLONETZIC SOIL

1982 ◽  
Vol 62 (1) ◽  
pp. 105-110 ◽  
Author(s):  
R. G. L. McCREADY ◽  
H. R. KROUSE
Keyword(s):  
Soil Profile ◽  
Oxidation Rate ◽  
Isotope Fractionation ◽  
Sulfur Isotope ◽  
Elemental Sulfur ◽  
Isotopic Analysis ◽  
Thiobacillus Thioparus ◽  
Sulfur Isotope Fractionation ◽  
Solonetzic Soil ◽  
S Oxidation

The oxidation rate of elemental S added to a Solonetzic soil was compared between an uninoculated soil and soils inoculated with two species of thiobacilli. Twelve weeks after S was added, 24% was oxidized to soluble S anions in the uninoculated soil, 34% in soil inoculated with Thiobacillus thiooxidans, and 84% in soil inoculated with Thiobacillus thioparus. The SO42− produced during S oxidation by thiobacilli was enriched in the lighter isotope by an average of 1‰ in comparison with the substrate S. Therefore, 34S-enriched S could be applied to Solonetzic soils and the migration of biologically produced H2SO4 into the soil profile may be followed by isotopic analysis of the soil sulfate.

scholarly journals Effect on Chemical and Physical Properties of Soil Each Peat Moss, Elemental Sulfur, and Sulfur-Oxidizing Bacteria

Plants ◽  
2021 ◽  
Vol 10 (9) ◽  
pp. 1901
Author(s):  
So-Young Lee ◽  
Eun-Gyeong Kim ◽  
Jae-Ryoung Park ◽  
Young-Hyun Ryu ◽  
Won Moon ◽  
...  
Keyword(s):  
Soil Ph ◽  
Elemental Sulfur ◽  
Organic Matter Content ◽  
Matter Content ◽  
Peat Moss ◽  
Soil Environment ◽  
Biological Factors ◽  
Sulfur Oxidizing ◽  
Properties Of Soil ◽  
Sulfur Oxidizing Bacteria

Peat moss is an organic substance corroded by sphagnum moss and has a pH of 3.0–4.0. Elemental sulfur is sulfated and oxidized by the action of bacteria to become sulfuric acid. These biological factors can alter the soil environment. Blueberries require soil with a pH of 4.5–5.2 and high organic matter content. In this experiment, we investigated whether different treatment rates of peat moss, elemental sulfur, and sulfur-oxidizing bacteria affect changes in soil pH, physicochemical properties, and electrical conductivity. We detected strong changes in soil pH as a reaction to the supply of peat moss, elemental sulfur, and sulfur-oxidizing bacteria. The pH of the soil when peat moss and elemental sulfur each were supplied was reduced. In addition, the pH decreased faster when elemental sulfur and sulfur-oxidizing bacteria were supplied together than elemental sulfur alone, satisfying an acidic soil environment suitable for blueberry cultivation. In this experiment, it is shown that peat moss, elemental sulfur, and sulfur-oxidizing bacteria are suitable for lowering soil pH. It was demonstrated that when elemental sulfur and sulfur-oxidizing bacteria were treated together, the pH decreased faster than when treated with peat moss. It could be economically beneficial to farmers to use elemental sulfur and sulfur-oxidizing bacteria, which are cheaper than peat moss, to reduce the pH of the soil.

scholarly journals Bioavailability of Sulfur from Waste Obtained during Biogas Desulfurization and the Effect of Sulfur on Soil Acidity and Biological Activity

Processes ◽  
2020 ◽  
Vol 8 (7) ◽  
pp. 863 ◽  
Author(s):  
Monika Tabak ◽  
Aneta Lisowska ◽  
Barbara Filipek-Mazur
Keyword(s):  
Soil Ph ◽  
Crop Production ◽  
Soil Acidity ◽  
Elemental Sulfur ◽  
Sulfur Oxidation ◽  
Soil Samples ◽  
Limiting Factor ◽  
Alternative Source ◽  
Soil Enzymatic Activity ◽  
Waste Reuse

Sulfur deficiency has been recognized as a limiting factor for crop production in many regions of the world. A 120-day incubation experiment was conducted to assess the effect of the applied waste elemental sulfur on sulfur bioavailability in soil. Four doses of sulfur were applied: 10, 20, 30 and 60 mg S kg−1 dry matter (d.m.) of soil. In order to assess the effect of soil pH adjustment on sulfur oxidation, the research was conducted on two sets of soil samples: one set of soil samples had natural pH, and the second one was limed before sulfur application. Application of waste sulfur slightly affected the soil pH, and increased the content of available sulfur in soil proportionally to sulfur dose. A beneficial effect of waste sulfur application on soil dehydrogenase and catalase activity was found. Liming reduced soil acidity, and significantly increased sulfate content and soil enzymatic activity. Waste elemental sulfur may be an alternative source of sulfur, supplementing the deficiencies of this element in soils. The described way of sulfur waste reuse corresponds with the increasingly common approach to create waste-free technologies in all economy.

The Distribution and Abundance of Vesicular Arbuscular Endophytes in Some Western Australian Soils

1977 ◽  
Vol 25 (5) ◽  
pp. 515 ◽  
Author(s):  
LK Abbott ◽  
AD Robson
Keyword(s):  
Soil Properties ◽  
Soil Ph ◽  
Western Australia ◽  
Agricultural Soils ◽  
Soil Samples ◽  
Root Infection ◽  
Spore Type ◽  
Va Mycorrhizas ◽  
Vesicular Arbuscular ◽  
Western Australian

The distribution and abundance of large-spored vesicular arbuscular (VA) endophytes was examined at three localities in Western Australia. Within each locality, soil samples were collected from sites with a range of soil properties and superphosphate histories. Vesicular arbuscular endophytes were widespread. Spores were found in all but five of 104 samples. In two of the samples where spores were not found, plants grown in the soils formed VA mycorrhizas. Root infection by a fine endophyte resembling Rhizophagus tenuis was also frequently observed. Five spore types were found. Honey-coloured sessile spores were present in 85% of the samples. The yellow vacuolate spore type was the second most common endophyte, but its distribution was mostly limited to cultivated and fertilized soils. Endophytes other than the yellow vacuolate spore type occurred on both virgin and agricultural soils. The distribution of honey-coloured sessile and yellow vacuolate spores in cultivated soils appeared to be associated with variation in soil pH. The total numbers of spores collected on a 106 μm sieve were not correlated with soil pH, NaHCO3-extractable phosphorus or superphosphate history.

scholarly journals Mimicking the Microbial Oxidation of Elemental Sulfur with a Biphasic Electrochemical Cell

2021 ◽  
Author(s):  
Marco F. Suárez-Herrera ◽  
Jose Solla-Gullon ◽  
Micheal D. Scanlon
Keyword(s):  
Driving Force ◽  
Elemental Sulfur ◽  
Electrochemical Cell ◽  
Sulfur Oxidation ◽  
Sulfur Cycle ◽  
Ambient Conditions ◽  
Microbial Oxidation ◽  
Artificial System ◽  
Sulfur Oxidizing ◽  
Aqueous Anions

<p>The lack of an artificial system that mimics elemental sulfur (S<sub>8</sub>) oxidation by microorganisms inhibits a deep mechanistic understanding of the sulfur cycle in the biosphere and the metabolism of sulfur-oxidizing microorganisms. In this article, we present a biphasic system that mimics biochemical sulfur oxidation under ambient conditions using a liquid|liquid (L|L) electrochemical cell and gold nanoparticles (AuNPs) as an interfacial catalyst. The interface between two solvents of very different polarity is an ideal environment to oxidise S<sub>8</sub>, overcoming the <a>incompatible solubilities </a>of the hydrophobic reactants (O<sub>2</sub> and S<sub>8</sub>) and hydrophilic products (H<sup>+</sup>, SO<sub>3</sub><sup>2–</sup>, SO<sub>4</sub><sup>2–</sup>, <i>etc.</i>). The interfacial AuNPs provide a catalytic surface onto which O<sub>2</sub> and S<sub>8</sub> can adsorb. Control over the driving force for the reaction is provided by polarizing the L|L interface externally and tuning the Fermi level of the interfacial AuNPs by the adsorption of aqueous anions.</p>

scholarly journals Determining the variation of soil properties in the Batumi Delta

2016 ◽  
Author(s):  
Bülent Turgut ◽  
Merve Ateş
Keyword(s):  
Organic Matter ◽  
Correlation Analysis ◽  
Moisture Content ◽  
Soil Properties ◽  
Aggregate Stability ◽  
Clay Content ◽  
Soil Samples ◽  
Sand Content ◽  
Delta Plain ◽  
Mean Weight Diameter

Abstract. The aim of this study was to determine certain basic properties of soils in the Batumi delta, to determine the relationships of studied properties, and to identify differences with regards to these properties between different sampling sites in the delta that were selected based on the delta morphology. In this context, a total of 125 soil samples were collected from five different sampling sites, and the clay, silt and sand content of the samples were determined along with their mean weight diameter (MWD) values, aggregate stability (AS) values, amount of water retained under −33 kPa (FC) and −1500 kPa (WP) pressure and organic matter (OM) content. Correlation analysis indicated that clay content and OM were positively correlated with MWD, and OM was positively correlated with AS. However, the sand content was found to be negatively correlated with MWD. In addition, clay, silt and OM content were positive correlated with FC and WP. Variance analysis results determined statistically significant differences between the sampling sites with respect to all of the evaluated properties. The active delta section of the study area was characterized by high sand content, while the lower delta plain was characterized by high OM and AS values, and the upper delta plain was characterized by high WMD values, high FC and WP moisture content levels and high clay and silt content. In conclusion, it was demonstrated that the examined properties were significantly affected by the different morphological positions and usages of these different areas. These results may help with the management of agricultural lands in the Batumi delta, which has never been studied before.

Extractable Fe in the surface horizons of a range of soils from Queensland

Soil Research ◽  
1990 ◽  
Vol 28 (2) ◽  
pp. 259 ◽  
Author(s):  
JO Skjemstad ◽  
HVA Bushby ◽  
RW Hansen
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Soil Ph ◽  
Clay Content ◽  
Surface Soils ◽  
Soil Weathering ◽  
Extraction Procedures ◽  
Weathering Processes ◽  
Mobile Component ◽  
Extractable Iron

The levels of iron and aluminium extracted from 36 surface soils by pyrophosphate, oxalate and dithionite are compared with a number of other soil properties. Correlations suggest that aluminium released by these extraction procedures is largely associated with organic matter while only a small fraction of the iron released is in this form. Significant correlations between soil pH and the negative logarithms of both oxalate (r = 0.715) and pyrophosphate (r = 0.959) extractable iron in soils with >20% clay content indicate that pH is the most significant factor in determining the level of ferrihydrite and iron/organic matter complexes in surface soils. The significance of these relationships in terms of soil weathering processes is discussed. Further, the data suggest that pyrophosphate extractable iron is a useful indicator of the most active, mobile component of iron in surface soils.

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