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但就全球而言几组模拟的效果相似。这说明考虑河流源岩性物质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

The scatter plot in Figure 3 and the Taylor diagram in Figure 4 indicate that there is no significant difference in the performance of simulating global ocean POC flux between the control group and the sensitive experimental group, despite changes in the concentration of riverine source rock material and the distance of diffusion towards the open ocean. Several simulations show similar effects globally, indicating that the inclusion of the effect of riverine source rock material on POC flux simulation did not significantly improve or adversely affect global ocean modeling. This does not necessarily mean that the modeling effect in the sensitive experimental group in the marginal seas has not changed, but rather that the limited sediment trap data collected in the marginal seas may have a smaller impact on the overall correlation and regression slope. It is worth mentioning that although the change in modeling effect is not significant, the inclusion of the effect of riverine source rock material on POC flux simulation without logarithmic transformation has slightly increased the correlation coefficient between the simulated results and the observed values, from 0.58 in the control group to the highest value of 0.68 in the sensitive experimental group, especially in the sensitive experiment of riverine source rock material transporting towards the ocean along the continental shelf and slope