Williams J R, Giering S L C
National Oceanography Centre Southampton UK.
Geophys Res Lett. 2022 Nov 16;49(21):e2022GL099563. doi: 10.1029/2022GL099563. Epub 2022 Nov 2.
Sinking particles are important in delivering carbon to the deep ocean where it may be stored out of contact with the atmosphere. Whilst particle sinking velocities are known to be influenced by a multitude of factors, size-based parameterizations remain common in biogeochemical models and in the methods used to determine particulate fluxes from autonomous platforms. Here we carried out an extensive literature review (62 data sets) into the size-sinking velocity relationship, and find the relationship is much weaker for studies examining particles in situ (median = 0.09) compared with ex situ studies (median = 0.35). This discrepancy may be because particles examined in the laboratory have more uniform properties than those studied in situ. Our review highlights the shortcomings of using a simple relationship between size and sinking velocity to calculate sinking particulate fluxes in the ocean; considering additional particle characteristics will enable more accurate calculations of particulate fluxes.
下沉颗粒对于将碳输送到深海至关重要,在深海中碳可能会被储存起来,与大气隔绝。虽然已知颗粒下沉速度受多种因素影响,但基于大小的参数化方法在生物地球化学模型以及用于确定自主平台颗粒通量的方法中仍然很常见。在此,我们对大小与下沉速度的关系进行了广泛的文献综述(62个数据集),发现与非原位研究(中位数 = 0.35)相比,原位研究颗粒的大小与下沉速度关系要弱得多(中位数 = 0.09)。这种差异可能是因为实验室中研究的颗粒性质比原位研究的颗粒更均匀。我们的综述突出了使用大小与下沉速度之间的简单关系来计算海洋中下沉颗粒通量的缺点;考虑颗粒的其他特征将能更准确地计算颗粒通量。