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Cadmium transport in sediments by tubificid bioturbation: An assessment of model complexity

机译:镉通过生物扰动在沉积物中的迁移:对模型复杂性的评估

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摘要

Biogeochemistry of metals in aquatic sediments is strongly influenced by bioturbation. To determine the effects of biological transport on cadmium distribution in freshwater sediments, a bioturbation model is explored that describes the conveyor-belt feeding of tubificid oligochaetes. A stepwise modelling strategy was adopted to constrain the many parameters of the model: (i) the tubificid transport model was first calibrated on four sets of microspheres (inert solid tracer) profiles to constrain tubificid transport; (ii) the resulting transport coefficients were subsequently applied to simulate the distribution of both particulate and dissolved cadmium. Firstly, these simulations provide quantitative insight into the mechanism of tubificid bioturbation. Values of transport coefficients compare very well with the literature, and based on this, a generic model of tubificid bioturbation is proposed. Secondly, the application of the model to cadmium dataset sheds a light on the behaviour of cadmium under tubificid bioturbation. Cadmium enters the sediment in two ways. In one pathway, cadmium enters the sediment in the dissolved phase, is rapidly absorbed onto solid particles, which are then rapidly transported to depth by the tubificids. In the other pathway, cadmium is adsorbed to particles in suspension in the overlying water, which then settle on the sediment surface, and are transported downwards by bioturbation. In a final step, we assessed the optimal model complexity for the present dataset. To this end, the two-phase conveyor-belt model was compared to two simplified versions. A solid phase-only conveyorbelt model also provides good results: the dissolved phase should not be explicitly incorporated because cadmium adsorption is fast and bioirrigation is weak. Yet, a solid phase-only biodiffusive model does not perform adequately, as it does not mechanistically capture the conveyor-belt transport at short time-scales.
机译:水生沉积物中金属的生物地球化学受到生物扰动的强烈影响。为了确定生物运输对淡水沉积物中镉分布的影响,研究了一种生物扰动模型,该模型描述了输送管带进给的小卵寡壳类动物。采用逐步建模策略来约束模型的许多参数:(i)首先在四组微球(惰性固体示踪剂)剖面上校准微管输运模型,以约束微管输运; (ii)随后将得到的传输系数应用于模拟颗粒和溶解镉的分布。首先,这些模拟提供了对管状生物扰动机理的定量见解。输运系数的值与文献有很好的比较,在此基础上,提出了微管生物扰动的通用模型。其次,该模型在镉数据集上的应用揭示了在微管生物扰动下镉的行为。镉以两种方式进入沉积物。在一种途径中,镉以溶解相进入沉积物中,被吸收到固体颗粒上,然后被微管迅速输送到深处。在另一种途径中,镉被吸附到上层水中的悬浮颗粒中,然后沉积在沉积物表面,并通过生物扰动向下运输。在最后一步,我们评估了当前数据集的最佳模型复杂度。为此,将两阶段传送带模型与两个简化版本进行了比较。仅固相的输送带模型也提供了良好的结果:溶解的相不应明确纳入,因为镉的吸附速度快且生物灌溉能力弱。然而,仅固相生物扩散模型不能充分发挥作用,因为它不能在短时间内以机械方式捕获传送带的运输。

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