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生物聚合物对海底沉积物流变特性和海底碎屑流运移行为的影响。

Influence of biopolymers on the rheological properties of seafloor sediments and the runout behavior of submarine debris flows.

机构信息

Department of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University, N10W8, Kita-ku, Sapporo, 060-0810, Japan.

Kochi Institute for Core Sample Research (KOCHII), Institute for Extra-cutting-edge Science and Technology Avant-garde Research (X-star), Agency for Marine-Earth Science and Technology, Nankoku, 783-8502, Japan.

出版信息

Sci Rep. 2021 Jan 15;11(1):1493. doi: 10.1038/s41598-021-81186-8.

Abstract

Submarine debris flows are mass movement processes on the seafloor, and are geohazards for seafloor infrastructure such as pipelines, communication cables, and submarine structures. Understanding the generation and run-out behavior of submarine debris flows is thus critical for assessing the risk of such geohazards. The rheological properties of seafloor sediments are governed by factors including sediment composition, grain size, water content, and physico-chemical conditions. In addition, extracellular polymeric substances (EPS) generated by microorganisms can affect rheological properties in natural systems. Here we show that a small quantity of EPS (~ 0.1 wt%) can potentially increase slope stability and decrease the mobility of submarine debris flows by increasing the internal cohesion of seafloor sediment. Our experiments demonstrated that the flow behavior of sediment suspensions mixed with an analogue material of EPS (xanthan gum) can be described by a Herschel-Bulkley model, with the rheological parameters being modified progressively, but not monotonously, with increasing EPS content. Numerical modeling of debris flows demonstrated that the run-out distance markedly decreases if even 0.1 wt% of EPS is added. The addition of EPS can also enhance the resistivity of sediment to fluidization triggered by cyclic loading, by means of formation of an EPS network that binds sediment particles. These findings suggest that the presence of EPS in natural environments reduces the likelihood of submarine geohazards.

摘要

海底碎屑流是海底的一种物质运动过程,对海底管道、通讯电缆和海底结构等海底基础设施构成地质灾害。因此,了解海底碎屑流的产生和流动行为对于评估此类地质灾害的风险至关重要。海底沉积物的流变特性受多种因素控制,包括沉积物成分、粒径、含水量和物理化学条件。此外,微生物产生的胞外聚合物(EPS)也会影响自然系统中的流变特性。本文研究表明,少量 EPS(约 0.1wt%)可以通过增加海底沉积物的内聚力,潜在地增加边坡稳定性并降低海底碎屑流的流动性。实验表明,添加 EPS 类似物(黄原胶)的沉积物悬浮液的流动行为可以用赫谢尔-布尔克利模型来描述,流变参数随 EPS 含量的增加而逐渐但非单调地变化。碎屑流的数值模拟表明,即使添加 0.1wt%的 EPS,碎屑流的流动距离也会明显缩短。EPS 的添加还可以通过形成束缚沉积物颗粒的 EPS 网络,增强沉积物对循环荷载引发的流态化的阻力。这些发现表明,自然环境中 EPS 的存在降低了海底地质灾害发生的可能性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e7df/7810891/af14f0b41e17/41598_2021_81186_Fig1_HTML.jpg

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