Transfer of sulphur to the digestive tract of sheep.

The transfer of sulphate from plasma to digestive tract and from digestive tract to plasma in crossbred sheep was estimated by the use of isotope dilution techniques with Na235SO4. The passage of 35S along the digestive tract was simultaneously measured by reference to two inert radioactive markers infused intraruminally. In the first experiment, three sheep given a roughage-based diet containing 174 +/- 7 mg S/day received an intravenous infusion of Na235SO4 for 7 days before collections were made of plasma and of digesta from the rumen, abomasum and terminal ileum. Similar collections were made in the second experiment in which four sheep received intraruminal infusions of Na235SO4. From estimates of infusion rate of 35S, specific radioactivity of 35S in plasma and digesta and rate of flow of sulphur in the digestive tract the following calculations were made: The transfer of sulphate from the plasma to the rumen was calculated as 29 mg S/day. Of this only 12 mg S/day passed as organic sulphur in digesta from the stomach. As the net gain of sulphur in the stomach in this experiment was 153 mg/day, sulphate transferred from the plasma contributed only a small amount of sulphur derived from endogenous sources in the stomach. In contrast, the substantial passage of 35S into the intestinal lumen during intravenous infusion of 35SO4 suggested that 38 and 41 mg S/day of the 236 and 145 mg organic S/day flowing from the small and large intestine respectively was derived from plasma sulphate, corresponding to about 26% of the dose.     

Sulphate recycling and metabolism in sheep and cattle.

Merino wethers and Brahman x Shorthorn steers, offered lucerne or spear grass hay, were used to study the movements of sulphate through pools in plasma and ruminal liquor. The irreversible loss of sulphate from ruminal liquor was 60 and 76% of sulphur ingested for both species fed lucerne and spear grass respectively. The irreversible loss of sulphate from the plasma averaged 67 and 56% of sulphur ingested for animals fed lucerne and spear grass respectively. Daily recycling of sulphate to the rumen of sheep was 98 mg sulphur on the lucerne diet and 3.9 mg sulphur on the spear grass diet. Sulphate recycling in cattle fed lucerne was 533 mg sulphur; in cattle fed spear grass the value was 234 mg sulphur. Over 6 days following an intravenous injection of [35S]sulphate into sheep and cattle fed lucerne, 5-10% of the dose was excreted in the faeces and c. 10% was retained. Corresponding values for animals fed spear grass were 23-31% in faeces and 40-51% of the dose retained. After intraruminal injections of [35S]sulphate, animals fed lucerne excreted 15-18% of the dose in the faeces and retained 25-30% of the dose over 6 days. Values for animals fed spear grass were 22-26% in faeces and 62-70% retained. It was concluded that sulphate recycling to the rumen is a limiting factor in microbial synthesis for sheep fed low-quality roughage, and that secretion of endogenous sulphur into the postruminal tract of ruminants is of importance in the metabolism of sulphate.     

Effect of high rates of sulphur on the CaCO3 and CaSO4 content of calcareous soils

Samples of two calcareous soils from central Iraq were amended with 2, 6 and 10 mg g⁻¹ soil of agriculturegrade sulphur and incubated for 4, 8 and 12 weeks at 30°C and 70% water-holding capacity. At the end of each incubation period, soils were analyzed for sulphate, CaCO₃ and CaSO₄. The sulphate content of the soils increased, whereas the CaCO₃ content decreased, with increasing S levels and incubation time. The gypsum formed was in proportion to the sulphur oxidised and the calcium released from CaCO₃.     

The role of soil microbes in plant sulphur nutrition

Chemical and spectroscopic studies have shown that in agricultural soils most of the soil sulphur (>95%) is present as sulphate esters or as carbon-bonded sulphur (sulphonates or amino acid sulphur), rather than inorganic sulphate. Plant sulphur nutrition depends primarily on the uptake of inorganic sulphate. However, recent research has demonstrated that the sulphate ester and sulphonate-pools of soil sulphur are also plant-bioavailable, probably due to interconversion of carbon-bonded sulphur and sulphate ester-sulphur to inorganic sulphate by soil microbes. In addition to this mineralization of bound forms of sulphur, soil microbes are also responsible for the rapid immobilization of sulphate, first to sulphate esters and subsequently to carbon-bound sulphur. The rate of sulphur cycling depends on the microbial community present, and on its metabolic activity, though it is not yet known if specific microbial species or genera control this process. The genes involved in the mobilization of sulphonate- and sulphate ester-sulphur by one common rhizosphere bacterium, Pseudomonas putida, have been investigated. Mutants of this species that are unable to transform sulphate esters show reduced survival in the soil, indicating that sulphate esters are important for bacterial S-nutrition in this environment. P. putida S-313 mutants that cannot metabolize sulphonate-sulphur do not promote the growth of tomato plants as the wild-type strain does, suggesting that the ability to mobilize bound sulphur for plant nutrition is an important role of this species.     

Effects of organic matter on sulphur oxidation in soil and influence of sulphur oxidation on soil nitrification

Summary The effects of wheat straw and pressed sugar beet pulp on sulphur oxidation were determined in a loam soil amended with 1% (w/w) elemental sulphur. Wheat straw stimulated the oxidation of elemental sulphur over the first 2 to 3 weeks of the incubation period, resulting in an increase in LiCl-extractable sulphate. After 4 to 7 weeks incubation however, the only significant increase in soil sulphate followed the 1% straw addition, while at week 7 sulphate concentrations in the 0.25% and 5.0% straw amended soils were lower than the control. Pressed sugar beet pulp (1% w/w) initially stimulated the oxidation of elemental sulphur in the soil, but by weeks 3 to 7 of the incubation period rates of oxidation in pulp-amended soils were lower than the control. Towards the end of the incubation period however, sulphate concentrations in the amended soils exceeded the control values, significantly so by week 11. The concentration of thiosulphate and tetrathionate also increased in soils receiving sugar beet pulp. Nitrification was inhibited in soils in which sulphur oxidation was actively occurring. Although possible alternatives are mentioned, such inhibition appears to result from a decrease in soil pH brought about by the oxidation of elemental sulphur to sulphuric acid.     

The evaluation of plant-available sulphur in soils. II

Summary The availability to oats of adsorbed sulphate in soils and of sulphate impurity in calcium carbonate was studied in pot-culture experiments.When calcium carbonate was added to soils with pH values ranging from 5.7 to 7.4 the uptake of sulphur by oats was increased, due probably to enhanced mineralization of soil organic sulphur. When the calcium carbonate contained sulphate impurity the uptake of sulphur was further increased by an amount comparable with the release of sulphate which could be expected from a reaction of the calcium carbonate with the exchangeable hydrogen of the soil. Sulphate in excess of this amount appeared to be largely unavailable. Uptake of sulphur by oats from calcareous sands containing large amounts of insoluble sulphate associated with calcium carbonate also suggested that soil sulphur in this form had very low availability to plants.Substantial increases in the amounts of sulphur extracted by reagents commonly used for the determination of adsorbed sulphate in soils occurred when soils were airdried at about 20°C. Decreases in adsorbed sulphate in soils following the growth of oats in pot culture confirmed that adsorbed sulphate is readily available to plants.     

Nutritive value of lupin-seed protein and leaf-protein concentrates supplemented with various sulphur sources

The effect of DL methionine, methionine hydroxyanalogue (MHA) and sodium sulphate on the nutritive value of lupin-seed protein and leaf-protein concentrate (LPC) from lucerne for rats and chicks was evaluated. Methionine and MHA markedly improved the biological value of both lupin- and LPC-proteins, but the effect of sodium sulphate was not significant.The supplement of organic sulphur-compounds improved the performance of chicks fed on lupin-seed meal, but the effect of sodium sulphate was negligible. There was no significant response to any of the organic and inorganic sulphur compounds in chicks fed on LPC diets. These results suggest that some factor other than methionine defiency is limiting the nutritive value of LPC for these animals.     

Biogeochemical cycling of sulphur in karst and transfer into speleothem archives at Grotta di Ernesto, Italy

Trace amounts of sulphur in speleothems suggest that stalagmites may act as archives of sulphur deposition, thereby recording aspects of atmospheric variability in sulphur content. Accurate interpretation of this novel sulphur archive depends upon understanding how biogeochemical cycling in the soil and epikarst above the cave may modify the precursor atmospheric values of sulphur concentration and isotopic composition prior to incorporation into the speleothem record. Dual isotope analysis of δ³⁴S-SO₄ and δ¹⁸O-SO₄ is used to trace biogeochemical transformations of atmospheric sulphur through the cave system at Grotta di Ernesto in the Italian Alps and builds towards a framework for interpretation of speleothem sulphur archives which depends on overlying ecosystem dynamics and karst hydrological properties. A three component model of atmospheric sulphate signal modification is proposed to be driven by (1). vegetation and soil cycling, (2). the degree of groundwater mixing in the karst aquifer; and (3). redox status. The relative influence of each process is specific to individual drip flow sites and associated stalagmites, rendering each sulphur archive a unique signal of environmental conditions. Under conditions found in the soil and epikarst above Grotta di Ernesto, the dual isotope signatures of sulphate sulphur and oxygen incorporated into speleothem carbonate, closely reflect past conditions of industrial sulphur loading to the atmosphere and the extent of signal modification through biogeochemical cycling and aquifer mixing.     

Impact of pedospheric and atmospheric sulphur nutrition on sulphur metabolism of Allium cepa L., a species with a potential sink capacity for secondary sulphur compounds

Onion (Allium cepa L.) was able to use atmospheric H(2)S as sole sulphur source for growth. The foliarly absorbed H(2)S was rapidly metabolized into water-soluble, non-protein thiol compounds, including cysteine, and subsequently into other sulphur compounds in the shoots. In H(2)S-exposed plants, the accumulation of sulphur compounds in the shoots was nearly linear with the concentration (0.15-0.6 microl l(-1)) and duration of the exposure. Exposure of onion to H(2)S for up to 1 week did not affect the sulphur content of the roots. Secondary sulphur compounds formed a sink for the foliarly absorbed sulphide, and the sulphur accumulation upon H(2)S exposure could, for a great part, be ascribed to enhancement of the content of gamma-glutamyl peptides and/or alliins. Furthermore, there was a substantial increase in the sulphate content in the shoots upon H(2)S exposure. The accumulation of sulphate originated both from the pedosphere and from the oxidation of absorbed atmospheric sulphide, and/or from the degradation of accumulated secondary sulphur compounds. From studies on the interaction between atmospheric and pedospheric sulphur nutrition it was evident that H(2)S exposure did not result in a down-regulation of the sulphate uptake by the roots.     

Novel sulphur-oxidizing bacteria consummate sulphur deficiency in oil seed crop

Archives of Microbiology - Plants absorb sulphate, the oxidized form of elemental sulphur (S°), from soil. Sulphur-oxidizing bacteria play a key role in transformation of sulphur in soil. Oil...     

Some factors affecting the mineralization of organic sulphur in soils

Summary Factors affecting the release of sulphate from a number of eastern Australian soils were studied.All of the soils released sulphate when dried. The amounts released were influenced by the manner in which the soil was dried. Air-drying in the laboratory at 20°C released least sulphate.Sulphate was mineralized in all soils by incubation at 30°C but the amounts mineralized could not be related to soil type or any single soil property. The ratio of nitrogen mineralized: sulphur mineralized varied widely between soils and was generally appreciably greater than the ratio of total nitrogen: organic sulphur in the soils.A rapid flush of mineralization of both sulphur and nitrogen took place when some of the soils were rewetted and incubated after they had been dried in the laboratory and stored for 4 to 5 months. Following this, the rate of mineralization was similar to that in the original undried soil. During this flush, the enhancement of sulphur mineralization was relatively greater than that of nitrogen so that the ratio of nitrogen mineralized: sulphur mineralized was considerably smaller than that during later phases of the incubation or that of the original moist soil. Soils collected after they had remained dry in the field for a similar period of time did not show this type of mineralization although they had initially done so when collected moist and air-dried in the laboratory.The effects of temperature, soil moisture, toluene and formaldehyde, and the addition of calcium carbonate to soils on the mineralization of sulphur were similar to their effects on the mineralization of nitrogen.     

Growth of Lucerne (Medicago sativa L.) Exposed to Sulphur Dioxide

The effect of exposure to sulphur dioxide (0 or 96 µgm^–3 SO₂) on the growth and sulphur content of lucerne(Medicago sativa L.) was examined in a period of 135 d duringwhich the plants were harvested four times. The lucerne wasgrown in pots of soil with and without the addition of sulphateand of nitrate. Evidence of sulphur deficiency, including areduction in the weight, the number and the sulphur contentof shoots, was found in plants grown without added sulphate.Deficiency was alleviated through exposure of plants to SO₂.Apart from reducing shoot weight at one harvest and generallyincreasimg the concentration of sulphur in the shoots, exposureto SO₂ had no significant effect on plants grown with addedsulphate. The yield of shoots was greater, and was reduced toa lesser extent with sulphur deficiency, in plants grown withadded nitrate than in those dependent on rhizobia. Whilst thetranspiration coefficient increased greatly in sulphur-deficientplants, it was reduced where otherwise similarly treated plantswere exposed to SO₂; this treatment did not alter the coefficientin plants with an adequate supply of sulphur from the soil.     

The evaluation of plant-available sulphur in soils

Summary Examination of a range of naturally occurring calcium carbonates and calcareous soils has shown that insoluble sulphate associated with calcium carbonate may comprise an important fraction of soil sulphur. One soil contained as much as 93 per cent of its sulphur in this form. It seems likely that this sulphate occurs as a co-precipitated or co-crystallized impurity in the calcium carbonate.Most surface soils had only low capacity to adsorb sulphate and contained only small amounts of sulphur in this form. Two acid surface soils and many acid subsoils, however, adsorbed sulphate quite strongly and in some acid subsoil clays adsorbed sulphate made up an important fractions of the total sulphur.Sulphate adsorption was found to be negligible above pH 6.5 and adsorbed sulphate may be determined by aqueous extraction after increasing the pH above this value by addition of solid calcium carbonate. Adsorption of sulphate during acid extraction of soils can lead to low values in the determination of acid-soluble sulphates. Sulphate so adsorbed can be determined by a second extraction with water after the addition of solid calcium carbonate to increase the pH to a value greater than 6.5.     

Catalytic and regulatory properties of sulphur metabolizing enzymes in cyanobacterium Synechococcus elongatus PCC 7942

Synechococcus elongatus PCC 7942 was able to grow with several S sources. The sulphur metabolizing enzymes viz. ATP sulphurylase, cysteine synthase, thiosulphate reductase and L- and D-cysteine desulphydrases were regulated by sulphur sources, particularly by sulphur amino acids and organic sulphate esters. Sulphur starvation reduced ATP sulphurylase and cysteine synthase whereas reduced glutathione appreciated Cys degradation activity. With partially purified enzymes apparent Km values for sulphate, ATP, D- and L-Cys, thiosulphate, sulphide and O-acetyl serine were in a range of 12-50 microM. p-Nitrophenyl sulphate inhibited ATP sulphurylase competitively. Met was a feedback inhibitor of several key enzymes.     

Organic sulphur sources for the growth of the dermatophyte microsporum gypseum

The suitability of 30 organic compounds (of them 19 sulphur-containing amino acids) at a concentration of 1mm as sulphur sources for the growth of the dermatophyteMicrosporum gypseum was investigated. The dry mass of the mycelium after an 11-d growth served as a measure of utilizability. Of sulphur amino acids cystine, cysteine, reduced and oxidized glutathione, cysteic and cysteinesulphinic acids, S-sulphocysteine, lanthionine, taurine and serine sulphate were the best sources. Methionine and methionine-sulphone were utilized slightly less effectively. Other compounds were medium to poor sources and only S-carboxymethylcysteine was not utilized at all. All organic compounds that are not of amino acid type were poor sulphur sources or were utilized at all. Sodium dodecyl sulphate inhibited germination and growth completely.     

Microbial oxidation of elemental sulphur in brown soil

Plant and Soil - Brown soil formed from loamy clay was examined for its ability to produce sulphate from added elemental suphur. At higher rates of sulphur applications the pH of a slightly acid...     

Effect of sulphur inoculated with Thiobacillus on soil salinity and growth of tropical tree legumes.

A greenhouse experiment was carried out with the objective of evaluating the effects of the elementary sulphur inoculated with Thiobacillus, compared with gypsum, in the amendment of a alluvial sodic saline soil from the Brazilian semiarid region, irrigated with saline water and grown with the tropical legumes leucena and mimosa. The treatments consisted of levels of sulphur (0; 300 and 600 kg/ha) and gypsum (1,200 and 2,400 kg/ha), irrigation using different waters containing the salts NaHCO3, MgCl2, CaCl2, NaCl and KCl, with different electrical conductivities (ECs: 0.2. 6.1 and 8.2 dS/m at 25 degrees C). Based on the results it appears that saline water increased exchangeable Na+, K+, Ca2+, Mg2+, and soil pH. Sulphur inoculated with Thiobacillus was more efficient than gypsum in the reduction of the exchangeable sodium of the soil and promoting leaching of salts, especially sodium. Sulphur inoculated with Thiobacillus reduced the EC of the soil saturation extract to levels below that adopted in soil classification of sodic or saline sodic. Leucena was more tolerant to salinity and mimosa more resistant to acidity promoted by sulphur inoculated with Thiobacillus.     

The effect of sodium chloride and sulphate on sulphur oxidation in soil

Summary The effect of sodium chloride on sulphur oxidation in Terra Rossa and Rendzina soils was studied by incubation and perfusion techniques. Sulphur oxidation was observed at concentrations up to 8 per cent NaCl, but was completely arrested at 10 per cent sodium chloride. Sodium chloride caused a delay in the onset of sulphur oxidation, its rate being only slightly affected. A relationship between sulphate appearance and decrease in pH was observed only in sulphur-amended Terra Rossa soil. Under optimal conditions, 53 and 54 per cent of added sulphur (5000 ppm) was recovered as SO₄-S from the Terra Rossa and Rendzina soils, respectively. This maximal level of sulphate production was only slightly affected by the addition of sulphate up to 3000 ppm S.It was concluded that inhibition in further sulphur oxidation was not caused by sulphate accumulation.     

Sulphur uptake by ryegrass and its relationship to inorganic and organic sulphur levels and sulphatase activity in soil

Summary Yield of perennial ryegrass and uptake of S at 10, 18 and 25°C were studied in a pot trial using 12 soils with different levels of adsorbed sulphate, total organic S, ester-S, C-bonded S and sulphatase activity.Adsorbed sulphate gave the best correlations with yield and S-uptake at each temperature. At the end of the trial appreciable levels of adsorbed sulphate remained in all the soils. For a given soil, the amount remaining was the same irrespective of the growth temperature employed. This adsorbed sulphate was considered to be unavailable for plant growth.Sulphur uptake was greater in all cases (except at 10°C for one soil) than the decrease in adsorbed sulphate during the trial. This additional sulphur was presumed to have come from organic sources and was significantly correlated (0.1%) with organic S, ester-S, C-bonded S and sulphatase activity at each temperature. These correlations were, however, markedly influenced by one organic S rich soil. When this was omitted the significance of the organic S, ester-S and sulphatase activity correlations fell to 5% and the C-bonded S correlations became non-significant. In this latter instance the absence of significant relationships with C-bonded S was taken to indicate that in this trial the fraction was of less importance in S mineralisation than ester-S.Although sulphatase activity is implicated in the mineralisation process by its significant correlations with the uptake of organic S, other factors are discussed which suggest that the correlations may not be conclusive.     

Biotic conversion of sulphate to sulphide and abiotic conversion of sulphide to sulphur in a microbial fuel cell using cobalt oxide octahedrons as cathode catalyst

Varying chemical oxygen demand (COD) and sulphate concentrations in substrate were used to determine reaction kinetics and mass balance of organic matter and sulphate transformation in a microbial fuel cell (MFC). MFC with anodic chamber volume of 1 L, fed with wastewater having COD of 500 mg/L and sulphate of 200 mg/L, could harvest power of 54.4 mW/m², at a Coulombic efficiency of 14%, with respective COD and sulphate removals of 90 and 95%. Sulphide concentration, even up to 1500 mg/L, did not inhibit anodic biochemical reactions, due to instantaneous abiotic oxidation to sulphur, at high inlet sulphate. Experiments on abiotic oxidation of sulphide to sulphur revealed maximum oxidation taking place at an anodic potential of −200 mV. More than 99% sulphate removal could be achieved in a MFC with inlet COD/sulphate of 0.75, giving around 1.33 kg/m³ day COD removal. Bioelectrochemical conversion of sulphate facilitating sulphur recovery in a MFC makes it an interesting pollution abatement technique.