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From Elemental Sulfur to Hydrogen Sulfide in Agricultural Soils and Plants

机译:农业土壤和植物中从元素硫到硫化氢

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摘要

Sulfur is an essential element in determining the productivity and quality of agricultural products. It is also an element associated with tolerance to biotic and abiotic stress in plants. In agricultural practice, sulfur has broad use in the form of sulfate fertilizers and, to a lesser extent, as sulfite biostimulants. When used in the form of bulk elemental sulfur, or micro- or nano-sulfur, applied both to the soil and to the canopy, the element undergoes a series of changes in its oxidation state, produced by various intermediaries that apparently act as biostimulants and promoters of stress tolerance. The final result is sulfate S+6, which is the source of sulfur that all soil organisms assimilate and that plants absorb by their root cells. The changes in the oxidation states of sulfur S0 to S+6 depend on the action of specific groups of edaphic bacteria. In plant cells, S+6 sulfate is reduced to S−2 and incorporated into biological molecules. S−2 is also absorbed by stomata from H2S, COS, and other atmospheric sources. S−2 is the precursor of inorganic polysulfides, organic polysulfanes, and H2S, the action of which has been described in cell signaling and biostimulation in plants. S−2 is also the basis of essential biological molecules in signaling, metabolism, and stress tolerance, such as reactive sulfur species (RSS), SAM, glutathione, and phytochelatins. The present review describes the dynamics of sulfur in soil and plants, considering elemental sulfur as the starting point, and, as a final point, the sulfur accumulated as S−2 in biological structures. The factors that modify the behavior of the different components of the sulfur cycle in the soil–plant–atmosphere system, and how these influences the productivity, quality, and stress tolerance of crops, are described. The internal and external factors that influence the cellular production of S−2 and polysulfides vs. other S species are also described. The impact of elemental sulfur is compared with that of sulfates, in the context of proper soil management. The conclusion is that the use of elemental sulfur is recommended over that of sulfates, since it is beneficial for the soil microbiome, for productivity and nutritional quality of crops, and also allows the increased tolerance of plants to environmental stresses.
机译:硫是决定农产品生产率和质量的重要元素。它也是与植物对生物和非生物胁迫的耐受性相关的元素。在农业实践中,硫以硫酸盐肥料的形式被广泛使用,并在较小程度上用作亚硫酸盐生物刺激剂。当以散装元素硫或微硫或纳硫的形式使用时,该元素同时应用于土壤和冠层时,其氧化态会发生一系列变化,这些变化显然是由各种中间物产生的,这些中间物显然起着生物刺激剂的作用。耐压力的促进者。最终结果是硫酸盐S +6 ,它是所有土壤生物同化和植物通过其根细胞吸收的硫的来源。硫S 0 变成S +6 的氧化态的变化取决于特定细菌的作用。在植物细胞中,硫酸盐S +6 还原为S -2 并掺入生物分子中。 S −2 也被H2S,COS和其他大气源的气孔吸收。 S −2 是无机多硫化物,有机多硫化物和H2S的前体,其作用已在植物的细胞信号传导和生物刺激中得到描述。 S −2 还是信号,代谢和胁迫耐受性中必不可少的生物分子的基础,例如活性硫(RSS),SAM,谷胱甘肽和植物螯合素。本文以元素硫为起点,以生物结构中S −2 积累的硫为终点,描述了土壤和植物中硫的动态变化。描述了改变土壤-植物-大气系统中硫循环不同组成部分的行为的因素,以及这些因素如何影响农作物的生产力,质量和胁迫耐受性。还描述了影响S −2 和多硫化物与其他S物种的细胞产生的内在和外在因素。在适当的土壤管理下,将元素硫的影响与硫酸盐的影响进行了比较。结论是,与硫酸盐相比,建议使用元素硫,因为它对土壤微生物组,作物的生产力和营养质量均有益,还可以提高植物对环境胁迫的耐受性。

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