Scholten J C, Stams A J
Department of Microbiology, Wageningen Agricultural University, Netherlands.
Antonie Van Leeuwenhoek. 1995 Nov;68(4):309-15. doi: 10.1007/BF00874141.
A freshwater sediment from a ditch of a peat grassland near Zegveld (Province of Utrecht, The Netherlands) was investigated for its potential methanogenic and syntrophic activity and the influence of sulfate and nitrate on these potential activities. Methanogenesis started after a 10 days lagphase. After 35-40 days aceticlastic methanogens were sufficiently enriched to cause a net decrease of acetate. In the presence of sulfate methane formation was only slightly affected. The addition of nitrate led to an outcompetition of aceticlastic methanogens by nitrate reducers. When inorganic electron acceptors were absent, substrates like propionate and butyrate were converted by syntrophic methanogenic consortia. Addition of inorganic electron acceptors resulted in an outcompetition of the syntrophic propionate and butyrate degrading consortia by the sulfate and nitrate reducers.
对荷兰乌得勒支省泽格维尔德附近泥炭草地沟渠中的淡水沉积物进行了研究,以探究其产甲烷和互营活性以及硫酸盐和硝酸盐对这些潜在活性的影响。产甲烷作用在10天的滞后期后开始。35 - 40天后,乙酸裂解产甲烷菌充分富集,导致乙酸盐净减少。在有硫酸盐存在的情况下,甲烷生成仅受到轻微影响。添加硝酸盐导致硝酸盐还原菌取代了乙酸裂解产甲烷菌。当不存在无机电子受体时,丙酸盐和丁酸盐等底物由互营产甲烷菌群落转化。添加无机电子受体导致硫酸盐和硝酸盐还原菌取代了互营降解丙酸盐和丁酸盐的菌群落。