Max Planck Institute for Marine Microbiology, Bremen, Germany.
FEMS Microbiol Ecol. 2010 Jun;72(3):476-84. doi: 10.1111/j.1574-6941.2010.00865.x. Epub 2010 Mar 19.
The effect of NO(3)(-) addition on dissimilatory SO(4)(2-) reduction and sulfide conversion in organic-rich sludge from the digestion basin of a recirculating marine aquaculture system was studied. SO(4)(2-) reduction could only explain a minor fraction (up to 4-9%) of the observed total sulfide production (up to 35 mmol L(-1) day(-1)), indicating that the main source of sulfide in the sludge was not SO(4)(2-) reduction, but desulfuration during the decomposition of organic matter. Although NO(3)(-) inhibited SO(4)(2-) reduction, but not desulfuration, the primary NO(3)(-) mitigation effect was the onset of NO(3)(-)-mediated sulfide oxidation (up to 75 mmol L(-1) day(-1)), partially to elemental sulfur (S(0)). Above NO(3)(-) concentrations of 0.6 mM in the bulk water, the net sulfide production and oxidation zones were moved deeper into flocs and sludge cores, which effectively prevented sulfide from entering the water column. However, the sulfide efflux from the sludge instantly recovered after NO(3)(-) depletion. Thus, the NO(3)(-) level in the water column controls the zonation and magnitude of sulfur transformations in the sludge. The effect of NO(3)(-) relies therefore on its sustained presence in the water column, which in turn depends on a well-functioning nitrification in the mariculture system.
研究了添加硝酸盐(NO3-)对循环海水养殖系统消化池富含有机物污泥中异化 SO42-还原和硫化物转化的影响。SO42-还原只能解释观察到的总硫化物生成量(高达 35mmol L-1 day-1)的一小部分(最高 4-9%),这表明污泥中硫化物的主要来源不是 SO42-还原,而是有机物分解过程中的脱硫作用。尽管 NO3-抑制 SO42-还原,但不抑制脱硫作用,NO3-的主要缓解作用是引发由 NO3-介导的硫化物氧化(高达 75mmol L-1 day-1),部分氧化为元素硫(S0)。在 bulk water 中硝酸盐浓度超过 0.6mM 时,净硫化物生成和氧化区更深地进入絮体和污泥核心,有效地阻止了硫化物进入水柱。然而,NO3-耗尽后,污泥中的硫化物渗出量会立即恢复。因此,水柱中的 NO3-水平控制了污泥中硫转化的分区和幅度。NO3-的作用取决于其在水柱中的持续存在,而这又取决于海水养殖系统中硝化作用的良好运行。