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IN SITU NEUTRALIZATION OF ACIDIC PIT LAKES: PROCESSES IN THE SEDIMENT AND LIMITING FACTORS

机译:原位中和酸性坑湖泊:沉积物中的过程和限制因素

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A strategy to neutralize acidic pit lakes was tested in a field mesocosm of 4500 m~3 volume in the Acidic Pit Mine Lake 111 in Germany. After addition of the substrates Carbokalk and straw a neutral sediment layer formed, in which microbial sulphate and iron reduction as well as sulphide precipitation occurred. The neutralisation rate was limited by the precipitation of iron sulphides rather than by microbial reactions. Oxidation of H_2S by ferric iron in the anoxic sediment lowered the net sulphate reduction rate. During the experiment precipitation of ferric minerals formed an acidic sediment layer at the sediment surface. In that layer sulphides did not precipitate, but H_2S diffused into the overlying water where it was oxidised.
机译:在德国酸性矿井湖111中,在4500m〜3体积的田间核科中和酸性坑湖中和酸性坑湖的策略。在加入底物叉子和秸秆中形成中性沉积物层,其中发生微生物硫酸盐和铁还原以及硫化物沉淀。中和速率受硫化铁沉淀而不是通过微生物反应的限制。通过铁铁在缺氧沉积物中对H_2S的氧化降低了硫酸盐还原率。在实验期间,矿物质的沉淀在沉积物表面形成酸性沉积物。在那层硫化物没有沉淀,但是H_2s扩散到其被氧化的上覆水中。

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