首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Processes of physical change to the seabed and bivalve recruitment over a 10-year period following experimental hydraulic clam dredging on Banquereau, Scotian Shelf
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Processes of physical change to the seabed and bivalve recruitment over a 10-year period following experimental hydraulic clam dredging on Banquereau, Scotian Shelf

机译:在斯科科陆架Banquereau进行水力蛤lam疏following后的10年中,海床和双壳类动物的物理变化过程

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A previous study on the effects of experimental hydraulic clam dredging on seabed habitat and commercial bivalve populations revealed a lack of recovery after a 3-year post-dredging period (1998-2001) on a deep (65-75 m) offshore sandy bank on the Scotian Shelf, Canada. Follow-up sidescan sonar surveys were carried out 5 and 10 years after dredging (2003,2008) in order to identify long-term processes of seabed recovery. Grab sampling was carried out 10 years after dredging to identify post-dredging commercial bivalve recruitment. Changes in the seafloor, including dredge tracks, were documented with a series of 7 sidescan sonar surveys between 1998 and 2008. A sediment mobility model was constructed based on modeled tidal current and hindcast wave data over this time period to quantify natural seabed disturbance and interpret changes to the dredge tracks mapped by sidescan sonar surveys. The model indicated that tidal currents had minimal effect on sediment mobilization. The main driving force associated with re-working of surficial sediments as evidenced by deterioration of dredge tracks in sonograms was annual fall/winter storms. While the annual frequency of storms and associated wave heights was variable, the observations and sediment mobility calculations suggest that the most influential variable is the magnitude of individual large storms, specifically storms with a significant wave height of similar to 11 m. These storms are capable of generating mobile sediment layers of 20-30 cm thickness, equivalent to the dredge blade cutting depth. It appears that, with minor exceptions, sediment properties have returned to pre-dredging conditions 10 years after dredging in this habitat Based on known age-length relationships, the four commercial bivalve species showed very low recruitment at the experimental site over the 10-year post-dredging period. However, this is unlikely due to a dredging effect since a similar pattern was observed in non-dredged areas. Crown Copyright (C) 2014 Published by Elsevier Ltd. All rights reserved.
机译:先前的一项实验性水力蛤lam疏on对海底栖息地和商业双壳类种群的影响的研究表明,在深水区(65-75 m)的海底沙质河道进行了三年的疏post期(1998-2001年)后,缺乏恢复。加拿大的斯科蒂货架。为了确定海床恢复的长期过程,在挖泥后(2003、2008)进行了5年和10年的后续侧扫声纳调查。挖泥后10年进行了抓斗采样,以确定挖泥后的商业双壳类动物招募。 1998年至2008年期间,通过一系列7次侧扫声纳调查,记录了海底的变化,包括挖泥船的航迹。基于这段时间内的潮流和后向波数据,建立了沉积物迁移模型,以量化自然海床扰动并解释侧扫声纳勘测所映射的挖泥机航迹的变化。该模型表明,潮流对泥沙动员影响最小。声像图上的挖泥机轨迹恶化表明,与表层沉积物再造有关的主要驱动力是每年的秋季/冬季风暴。尽管每年的暴风雨频率和相关的波高是可变的,但观测和沉积物迁移率计算表明,最具影响力的变量是单个大型暴风的强度,特别是波高接近11 m的暴风。这些风暴能够产生厚度为20-30厘米的可移动沉积物层,相当于疏the刀片的切割深度。看来,除少数例外,在该生境中挖泥后10年,沉积物特性已恢复到挖泥前的状态。根据已知的年龄长度关系,四种商业双壳类在过去的十年中在实验点的招募量非常低后挖期。但是,由于挖泥效果不太可能,因为在非挖泥区域观察到了类似的图案。官方版权(C)2014,由Elsevier Ltd.发行。保留所有权利。

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