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Sulfate and organic matter concentration in relation to hydrogen sulfide generation at inert solid waste landfill site – Limit value for gypsum

机译:惰性固体废物填埋场硫化氢和有机物浓度与硫化氢生成的关系 - 石膏的极限值

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摘要

In order to suggest a limit value for gypsum (CaSO4) for the suppression of hydrogen sulfide (H2S) generation at an inert solid waste landfill site, the relationship between raw material (SO4 and organic matter) for H2S generation and generated H2S concentration, and the balance of raw material (SO4) and product (H2S) considering generation and outflow were investigated. SO4 concentration should be less than approximately 100mg-SO4/L in order to suppress H2S generation to below 2000ppm. Total organic carbon (TOC) concentration should be less than approximately 200mg-C/L assuming a high SO4 concentration. The limit value for SO4 in the ground is 60mg-SO4/kg with 0.011wt% as gypsum dihydrate, i.e., approximately 1/10 of the limit value in inert waste as defined by the EU Council Decision (560mg-SO4/kg-waste). The limit value for SO4 in inert waste as defined by the EU Council Decision is high and TOC is strictly excluded. The cumulative amount of SO4 outflow through the liquid phase is much larger than that through the gas phase. SO4 concentration in pore water decreases with time, reaching half the initial concentration around day 100. SO4 reduction by rainfall can be expected in the long term.
机译:为了建议用于抑制惰性固体垃圾填埋场中硫化氢(H2S)生成的石膏(CaSO4)的限值,生成H2S的原料(SO4和有机物)与生成的H2S浓度之间的关系,以及研究了考虑产生和流出的原料(SO4)和产品(H2S)的平衡。为了将H2S的产生抑制到2000ppm以下,SO4的浓度应小于约100mg-SO4 / L。假设高SO4浓度,总有机碳(TOC)浓度应小于约200mg-C / L。地面中SO4的限值为60mg-SO4 / kg,其中0.011wt%为二水合石膏,即欧盟理事会决定所定义的惰性废物限值的约1/10(560mg-SO4 / kg-废物)。根据欧盟理事会决定,惰性废物中SO4的限值很高,并且严格禁止使用TOC。通过液相流出的SO4累积量比通过气相流出的累积量大得多。孔隙水中的SO4浓度随时间降低,在第100天左右达到初始浓度的一半。从长期来看,降雨会导致SO4浓度降低。

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    Asakura Hiroshi;

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  • 年度 2015
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  • 正文语种 en
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