1988
DOI: 10.1080/00288233.1988.10417943
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Effect of particle size on the oxidation of elemental sulphur, thiobacilli numbers, soil sulphate, and its availability to pasture

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Cited by 28 publications
(13 citation statements)
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“…Mass transfer was expected to be an important rate-limiting factor in the overall process. Rates of aerobic S 0 oxidation soils is known to be dependent on surface area (Germida and Janzen, 1993;Lee et al, 1988;Sholeh et al, 1997). Increasing S 0 concentration would provide an increased surface area for colonization and dissolution, thus, it is expected that the greater S 0 concentrations would support more rapid kinetics.…”
Section: Role Of S 0 Concentrationmentioning
confidence: 99%
“…Mass transfer was expected to be an important rate-limiting factor in the overall process. Rates of aerobic S 0 oxidation soils is known to be dependent on surface area (Germida and Janzen, 1993;Lee et al, 1988;Sholeh et al, 1997). Increasing S 0 concentration would provide an increased surface area for colonization and dissolution, thus, it is expected that the greater S 0 concentrations would support more rapid kinetics.…”
Section: Role Of S 0 Concentrationmentioning
confidence: 99%
“…2c and C). There are a number of reasons for this result in high plant uptake and accumulation of these heavy metals; however, the main reason is most probably that the increase of solubility of Zn and Cd leads to an improvement in metal bioavailability with a decrease of soil pH by application of S. There are certain groups of acidophilic soil bacteria in the soil, predominantly the genus Thiobacillus, that can oxidize S and change it to SO 4 2 À when soil pH has decreased (Lee et al, 1988;Tichý et al, 1997;Kayser et al, 2000). McLaughlin et al (1998) reported that increasing SO 4 2 À in soil could increase shoot Cd concentration, in the present experiment, the increasing SO 4 2 À in soil (data were not given) may be another cause that increased the shoot Cd content.…”
Section: Accumulation Of Pb and Zn In Plant Shoots And Rootsmentioning
confidence: 99%
“…One important fact is the oxidation of S by certain groups of acidophilic bacteria, notably Thiobacillus spp. in the soil (Lee et al, 1988;Seidel et al, 1998;Tichý et al, 1997;Kayser et al, 2000). Tichý et al (1997) reported that 156 mmol of different types of elemental sulphur per kilogram of soil were added to a gleyic cambisol with an initial soil pH between 5 and 5.5, the soil pH decreased to 3.3 within 80 days.…”
Section: Soil Phmentioning
confidence: 99%
“…The soil acidifying effect of S 0 may be explained by the activities of certain groups of acidophilic soil bacteria, particularly the genus Thiobacillus, which can metabolize S 0 in the presence of O 2 and generate H þ and SO 2À 4 , leading to soil acidification. [11][12][13][14] …”
Section: Soil Phmentioning
confidence: 99%