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集水区泥沙在大堡礁大陆架上的模拟归宿。

Simulated fate of catchment-derived sediment on the Great Barrier Reef shelf.

机构信息

CSIRO Ocean and Atmosphere, GPO Box 1538, Hobart, Tasmania 7001, Australia.

CSIRO Ocean and Atmosphere, GPO Box 1538, Hobart, Tasmania 7001, Australia.

出版信息

Mar Pollut Bull. 2018 Oct;135:954-962. doi: 10.1016/j.marpolbul.2018.08.018. Epub 2018 Aug 17.

DOI:10.1016/j.marpolbul.2018.08.018
PMID:30301121
Abstract

Numerical experiments using a 3D model of fine sediment transport in the Great Barrier Reef region indicate deposition of the bulk mass of catchment sediments from river plumes within a few tens of kilometres from river mouths. A very fine fraction of easily resuspended catchment sediment has a capacity to propagate over much greater distances reaching out into the mid-shelf and outer-shelf regions. The model suggests such particles, instrumental to the development of low density flocs in the marine environment, can play a critical role in altering optical properties of water masses over the shelf during wet years. The mid-term (4 year) impact of Great Barrier Reef catchments on the probability of suspended sediment concentration exceeding the ecologically significant trigger value of 2 mg/L is confined to inshore regions adjacent to river mouth locations.

摘要

数值实验表明,大堡礁地区细颗粒泥沙输运的三维模型中,大部分流域泥沙在距河口几十公里范围内发生沉积。而流域中很细的一部分易于再悬浮的泥沙颗粒,其传播距离更远,可以到达中陆架和外陆架区域。该模型表明,这些颗粒对于在海洋环境中形成低密度絮体至关重要,它们在湿润年份可能会对陆架区水体的光学性质产生重大影响。在大堡礁流域的中期(4 年)影响下,悬浮泥沙浓度超过 2mg/L 这一具有生态意义的触发值的概率仅限于紧邻河口的近岸区域。

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