Thiobazillen im Wasser und Sediment der Saar

Maria Schneider, Ulrich Zaiss , Heinrich Kaltwasser
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引用次数: 2

Abstract

The number of thiobacilli and the thiosulfate oxidation potency were determined in the water and in the sediment of the river Saar in order to study the aerobic part of the sulfur cycle. Samples were taken along the entire course of the river between summer 1978 and spring 1981, i.e. before the lower part of the river was canalized.

In the water samples, a close correlation was observed between the total number of thiobacilli and the thiosulfate oxidation potency. In the sediment of the middle part of the river, which is canalized, the observed concentration and metabolic activity of the thiobacilli, the presence of sulfide and the diminished concentration of sulfate indicated that both oxidation and reduction of sulfur occurred in this reach.

Highest concentrations (numbers) and activities of thiobacilli, both in the water and in the sediment, were observed at low waters in August 1978; 103 cells/ml water and 105 cells/g sediment were detected. Lowest concentrations and activities were measured during high waters in February 1980. In a longitudinal study of the river the following species were enumerated in water and sediment by means of selective media: T. thioparus, T. neapolitanus, T. denitrificans, T. thiooxidans and T. ferrooxidans.

Downstream from the source, the number of all these species increased, but in case of T. thioparus and T. neapolitanus maximum concentrations were already observed in the upper part of the river, which is not canalized and not polluted by industrial wastes. The remaining three species increased in number along the entire river. The concentrations of the individual species were considerably higher in the sediments than in the overlaying water. In general, the detected numbers were about 103-times higher in the sediment samples, regardless whether selective or non-selective media were used.

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沙土里的黄铁矿,黄铁矿
为了研究硫循环的好氧部分,测定了萨尔河水体和沉积物中硫杆菌的数量和硫代硫酸盐的氧化力。样本是在1978年夏至1981年春期间沿整条河流采集的,即在河流下游开凿运河之前。在水样中,硫杆菌总数与硫代硫酸盐氧化力密切相关。在河道中游泥沙中,硫杆菌的浓度和代谢活性、硫化物的存在和硫酸盐浓度的降低表明,该河段发生了硫的氧化和还原。1978年8月低潮时观察到水和沉积物中硫杆菌的最高浓度(数量)和活性;检测到103个细胞/ml水,105个细胞/g沉积物。1980年2月的高水位测得最低浓度和活动。在对河流的纵向研究中,通过选择媒介在水和沉积物中列举了以下物种:T. thiioparus, T. neapolitanus, T.反硝化,T. thioooxidans和T. ferrooxidans。在源头下游,所有这些物种的数量都有所增加,但以T. thiioparus和T. neapolitanus的最高浓度已经出现在河流上游,这是没有运河和没有受到工业废物污染的地区。剩下的三种在整个河流的数量都在增加。沉积物中单个物种的浓度明显高于上覆水体。总的来说,无论使用选择性介质还是非选择性介质,沉积物样品中检测到的数量都高出约103倍。
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