将如下段落用规范英语翻译图3的散点图以及图4的泰勒图表明控制组与敏感实验组模拟的全球海洋POC通量的优劣程度没有显著差异尽管河流源岩性物质的浓度及向外海方向的扩散距离发生改变。这说明考虑RLM的压舱作用后尽管对全球海洋POC通量的模拟效果没有明显提升但也未造成不利影响；这并不意味着敏感实验组中边缘海的模拟效果没有改变只是可能由于收集到的位于边缘海的沉积物捕集器数据较少它们对整体的相关性和回归斜率有

The scatter plot in Figure 3 and the Taylor diagram in Figure 4 indicate that there is no significant difference in the quality of simulated global ocean POC flux between the control group and the sensitive experimental group, despite changes in the concentration of riverine source rock materials and their diffusion distance towards the open ocean. This suggests that, although the addition of the RLM effect did not significantly improve the simulation of global ocean POC flux, it also did not have any adverse effects. This does not necessarily mean that the simulation of the marginal seas in the sensitive experimental group was not affected, but rather that the limited sediment trap data collected from these regions may have had a small impact on the overall correlation and regression slope. It is worth noting that although the changes in simulation performance were small, the addition of riverine source rock material pressure effect enhanced the correlation coefficient between simulated and observed POC flux results slightly, from 0.58 in the control group to a maximum of 0.68 in the sensitive experimental group, particularly in the sensitive experiment of riverine source rock materials migrating from the continental shelf and slope towards the ocean, without performing logarithmic transformation