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Emissions of porewater compounds and gases from the subaquatic sediment disposal site 'Rodewischhafen', Hamburg harbour

机译:来自汉堡港的亚水底沉积物处置场“ Rodewischhafen”的孔隙水化合物和气体的排放

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In the year 1993 a confined and unused harbour basin was used to store 290,000 m3 of fine-grained dredged material from Hamburg harbour. About 70% of the deposit surface was water covered. The edge areas were above the water table and covered with reed. Emissions of dissolved compounds into the groundwater, as well as surface gas emissions were measured from 1994 to 1996. As indicators for water fluxes from the deposit we used NH4+ and HCO3- because of their high concentrations in mud porewater in comparison to groundwater, The average concentrations of NH4+ and HCO3- in the porewater increased during 2 years from 85 to 250 mg NH4+ 1(-1) and from 2.0 to 3.1 g HCO3- 1(-1), while the groundwater samples showed constant values of 8 mg NH4+ 1-(1) and 0.7 g HCO3- 1(-1). Furthermore, the average gas emissions over the water surface were 3.2 g CH4 m(-2) d(-1) and 0.8 g CO2 m(-2) d(-1). In contrast, no methane and 3.0 g CO2 m(-2) d(-1) were emitted from land areas. The results indicated, that there were no significant emissions of mud porewater compounds into the groundwater but high CH4-emissions over the water covered surface of the mud deposit. (C) 1998 IAWQ. Published by Elsevier Science Ltd. [References: 6]
机译:在1993年,一个狭窄且未使用的港口盆地被用来储存290,000立方米汉堡港的细颗粒疏dr物料。大约70%的沉积物表面被水覆盖。边缘区域在地下水位上方,并覆盖着芦苇。从1994年到1996年测量了溶解的化合物向地下水的排放以及地表气体的排放。作为沉积物水通量的指标,我们使用了NH4 +和HCO3-,因为它们在泥浆孔隙水中的浓度比地下水高,平均两年内,孔隙水中的NH4 +和HCO3-浓度从85上升到250 mg NH4 + 1(-1)和从2.0上升到3.1 g HCO3-1(-1),而地下水样品显示的恒定值为8 mg NH4 + 1 -(1)和0.7克HCO3-1(-1)。此外,水面上的平均气体排放量为3.2 g CH4 m(-2)d(-1)和0.8 g CO2 m(-2)d(-1)。相反,没有甲烷和3.0 g CO2 m(-2)d(-1)从陆地区域排放。结果表明,没有明显的泥浆孔隙水化合物排放到地下水中,但是在泥浆沉积物的水覆盖表面上有较高的CH4排放量。 (C)1998 IAWQ。由Elsevier Science Ltd.发布[参考:6]

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