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Effects of Metals on Methanogenesis Sulfate Reduction Carbon Dioxide Evolution and Microbial Biomass in Anoxic Salt Marsh Sediments

机译:金属对缺氧盐沼沉积物甲烷化硫酸盐还原二氧化碳生成和微生物生物量的影响

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摘要

The effects of several metals on microbial methane, carbon dioxide, and sulfide production and microbial ATP were examined in sediments from Spartina alterniflora communities. Anaerobically homogenized sediments were amended with 1,000 ppm (ratio of weight of metal to dry weight of sediment) of various metals. Time courses in controls were similar for CH4, H2S, and CO2, with short initial lags (0 to 4 h) followed by periods of constant gas production (1 to 2 days) and declining rates thereafter. Comparisons were made between control and experimental assays with respect to initial rates of production (after lag) and overall production. Methane evolution was inhibited both initially and overall by CH3HgCl, HgS, and NaAsO2. A period of initial inhibition was followed by a period of overall stimulation with Hg, Pb, Ni, Cd, and Cu, all as chlorides, and with ZnSO4, K2CrO4, and K2Cr2O7. Production of CO2 was generally less affected by the addition of metals. Inhibition was noted with NaAsO2, CH3HgCl, and Na2MoO4. Minor stimulation of CO2 production occurred over the long term with chlorides of Hg, Pb, and Fe. Sulfate reduction was inhibited in the short term by all metals tested and over the long term by all but FeCl2 and NiCl2. Microbial biomass was decreased by FeCl2, K2Cr2O7, ZnSO4, CdCl2, and CuCl2 but remained generally unaffected by PbCl2, HgCl2, and NiCl2. Although the majority of metals produced an immediate inhibition of methanogenesis, for several metals this was only a transient phenomenon followed by an overall stimulation. The initial suppression of methanogenesis may be relieved by precipitation, complexation, or transformation of the metal (possibly by methylation), with the subsequent stimulation resulting from a sustained inhibition of competing organisms (e.g., sulfate-reducing bacteria). For several environmentally significant metals, severe metal pollution may substantially alter the flow of carbon in sediments.
机译:在互花米草群落的沉积物中检测了几种金属对微生物甲烷,二氧化碳,硫化物产生和微生物ATP的影响。将厌氧均质的沉积物修改为1000 ppm(金属重量与沉积物干重之比)的各种金属。对照中CH4,H2S和CO2的时间过程相似,最初的滞后时间短(0到4小时),随后是稳定的产气时间段(1-2天),此后速率下降。在对照和实验分析之间就初始生产率(滞后)和总体生产率进行了比较。 CH3HgCl,HgS和NaAsO2最初和全部抑制了甲烷的释放。在最初的抑制期之后,是全部以氯化物形式的Hg,Pb,Ni,Cd和Cu以及ZnSO4,K2CrO4和K2Cr2O7进行总体刺激。通常,添加金属对二氧化碳的生产影响较小。 NaAsO2,CH3HgCl和Na2MoO4表现出抑制作用。长期以来,Hg,Pb和Fe的氯化物对CO 2 产生的刺激较小。硫酸盐的还原在短期内受所有测试金属的抑制,而长期而言,除FeCl 2 和NiCl 2 以外的所有金属均被抑制。 FeCl 2 ,K 2 Cr 2 O 7 ,ZnSO 4 ,CdCl 2 和CuCl 2 ,但通常不受PbCl 2 ,HgCl 2 和NiCl的影响 2 。尽管大多数金属会立即抑制甲烷生成,但对于几种金属来说,这只是短暂的现象,随后是整体刺激。甲烷生成的最初抑制可以通过金属的沉淀,络合或转化(可能通过甲基化)来缓解,而随后的刺激则是由于竞争生物(例如硫酸盐还原菌)的持续抑制而产生的。对于几种对环境重要的金属,严重的金属污染可能会大大改变沉积物中碳的流量。

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