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Accumulation of phosphorus in coastal marine sediments: relationship to benthic and diffusive fluxes

机译:沿海海洋沉积物中磷的积累:与底栖和扩散通量的关系

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Sedimentary phosphorus was characterized in sediment cores from 3 coastal ecosystems of the Gulf of Cadiz High spatial variability was observed in total phosphorus (from 445 to 20291 mu g g sed (1)) and in the other phosphorus phases studied This variability correlates with the proximity of the 10 sampling stations to sources of urban and/or industrial effluent in the zone The benthic and diffusive fluxes were measured concurrently with sediment collection at these stations The measured values of benthic fluxes range between -14 and 6 mmol m (2) d (1) Generally stations that showed increased interstitial phosphate concentrations with increasing depth were characterized by positive values in phosphate benthic fluxes and by high percent ages of reactive forms of sedimentary phosphorus Negative benthic fluxes were associated with stations receiving more anthropogenic matter which showed progressively decreasing phosphate concentrations in the interstitial water with depth In these anthropogenic areas the non reactive forms of phosphorus (those associated with ferric oxyhydroxide and authigenic carbonate fluorapatite) are abundant and reach values exceeding 75% of total phosphorus in sediment
机译:在加的斯湾的3个沿海生态系统的沉积物核心中表征了沉积磷,在总磷(从445到20291 mg sed sed(1))和其他研究的磷相中观察到了高度的空间变异性。该区域内城市和/或工业废水来源的10个采样站底流和扩散通量与这些站的沉积物收集同时进行测量。底流通量的测量值介于-14和6 mmol m(2)d(1 )通常,随着深度的增加,间隙磷酸盐浓度升高的站的特征是磷酸盐底栖通量的正值和沉积磷的活性形式的高年龄年龄。在这些人类中具有深度的间隙水磷的非生成型区域(与氢氧化铁和自生碳酸盐氟磷灰石相关的磷)的非活性形式丰富,其值超过沉积物中总磷的75%

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