首页 > 最新文献

Deep-Sea Research Part I-Oceanographic Research Papers最新文献

英文 中文
High genetic connectivity of the two main cold-water scleractinian framework engineers from the Southwestern Atlantic 来自西南大西洋的两种主要的冷水硬核框架工程师的高遗传连通性
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-10-16 DOI: 10.1016/j.dsr.2025.104606
Kátia Cristina Cruz Capel , Pedro Leocorny , Raphael de Mello Carpes , Marcelo Visentini Kitahara , Carla Zilberberg
Cold-water coral reefs (>150 m) are highly biodiverse ecosystems mainly engineered by few scleractinian and Porifera species. Due to the low number of framework building scleractinian species combined with their low growth rates, cold-water reefs are considered vulnerable marine ecosystems susceptible to human impacts such as demersal fisheries. Apart from their occurrence, a seminal information that subsidizes best practices for their conservation is related to gene flow/population genetics. However, research on the latter is hampered by the expensive sampling logistics and, to date, most studies have focused on the North Atlantic. Here we use microsatellite markers to understand the genetic diversity and population structure of the most important cold-water framework builders in the Southwestern Atlantic, Desmophyllum pertusum and Solenosmilia variabilis. The genotyping of 285 specimens belonging to both species showed low clonality rates, high levels of genetic diversity with no evidence of inbreeding, and no population structure along a latitudinal gradient of nearly 700 km, similar to what has been previously observed for the sympatric species Madrepora oculata and M. piresae. The recurrent absence of population structure for cold-water corals in the Southwestern Atlantic along latitudinal and depth ranges, suggests that oceanographic factors, such as the direction and speed of the Western South Atlantic Central Water and of the Antarctic Intermediate Water, combined with the spawning "window" and the pelagic larval duration (PLD) of these species play crucial roles in their dispersion and connectivity patterns.
冷水珊瑚礁(水深150米)是一种高度生物多样性的生态系统,主要由少数硬核虫和多孔虫组成。由于构建框架的硬核物种数量少,加上它们的生长速度低,冷水珊瑚礁被认为是脆弱的海洋生态系统,容易受到人类的影响,如底栖渔业。除了它们的发生之外,与基因流动/群体遗传学有关的一个重要信息补贴了它们保护的最佳实践。然而,对后者的研究受到昂贵的采样物流的阻碍,迄今为止,大多数研究都集中在北大西洋。本研究利用微卫星标记研究了西南大西洋最重要的冷水框架构建者Desmophyllum pertusum和Solenosmilia variabilis的遗传多样性和群体结构。这两个物种的285个标本的基因分型结果显示,它们的克隆率低,遗传多样性水平高,没有近亲繁殖的证据,在近700 km的纬度梯度上没有种群结构,与之前对同域物种Madrepora culata和M. piresae的观察结果相似。西南大西洋冷水珊瑚在纬度和深度范围内的种群结构反复缺失,表明海洋因素,如南大西洋西部中部水域和南极中间水域的方向和速度,结合这些物种的产卵“窗口”和远洋幼虫期(PLD),对它们的分散和连通性模式起着至关重要的作用。
{"title":"High genetic connectivity of the two main cold-water scleractinian framework engineers from the Southwestern Atlantic","authors":"Kátia Cristina Cruz Capel ,&nbsp;Pedro Leocorny ,&nbsp;Raphael de Mello Carpes ,&nbsp;Marcelo Visentini Kitahara ,&nbsp;Carla Zilberberg","doi":"10.1016/j.dsr.2025.104606","DOIUrl":"10.1016/j.dsr.2025.104606","url":null,"abstract":"<div><div>Cold-water coral reefs (&gt;150 m) are highly biodiverse ecosystems mainly engineered by few scleractinian and Porifera species. Due to the low number of framework building scleractinian species combined with their low growth rates, cold-water reefs are considered vulnerable marine ecosystems susceptible to human impacts such as demersal fisheries. Apart from their occurrence, a seminal information that subsidizes best practices for their conservation is related to gene flow/population genetics. However, research on the latter is hampered by the expensive sampling logistics and, to date, most studies have focused on the North Atlantic. Here we use microsatellite markers to understand the genetic diversity and population structure of the most important cold-water framework builders in the Southwestern Atlantic, <em>Desmophyllum pertusum</em> and <em>Solenosmilia variabilis</em>. The genotyping of 285 specimens belonging to both species showed low clonality rates, high levels of genetic diversity with no evidence of inbreeding, and no population structure along a latitudinal gradient of nearly 700 km, similar to what has been previously observed for the sympatric species <em>Madrepora oculata</em> and <em>M. piresae</em>. The recurrent absence of population structure for cold-water corals in the Southwestern Atlantic along latitudinal and depth ranges, suggests that oceanographic factors, such as the direction and speed of the Western South Atlantic Central Water and of the Antarctic Intermediate Water, combined with the spawning \"window\" and the pelagic larval duration (PLD) of these species play crucial roles in their dispersion and connectivity patterns.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"226 ","pages":"Article 104606"},"PeriodicalIF":2.1,"publicationDate":"2025-10-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145365509","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Deep-sea biotope classification using opportunistic sampling: insights for future management 利用机会取样的深海生物群落分类:对未来管理的见解
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-10-08 DOI: 10.1016/j.dsr.2025.104604
Heidy Q. Dias , Kerstin Kröger , Andrew J. Wheeler , Riccardo Arosio , Audrey Recouvreur , Tim P. Le Bas , Isobel A. Yeo , Patrick C. Collins
An iterative approach to optimise deep-sea biotope classification using a combination of acoustic data and Remotely Operated Vehicle (ROV) video footage was developed and tested at the Tropic Seamount site in the Northeast Atlantic. Two methods for biotope classification were compared: a top-down approach based on acoustic substrate classification followed by biological characterisation, and a bottom-up approach using multivariate analysis of biological assemblages only. Video transects were analysed at two spatial resolutions (200 m and 50 m segments) to assess scale effects on biotope delineation. Biotopes were classified using a combination of geological and biological data with each biotope representing a distinct combination of substrate types and their associated benthic assemblages. The bottom-up approach using 50 m segments identified 12 distinct biotopes with stronger environmental correlations compared to broader classifications at 200 m scale. This study demonstrates that shorter transects (50 m) combined with bottom-up sampling approaches are preferable for capturing the ecological heterogeneity characteristic of deep-sea seamount environments, with important implications for vulnerable marine ecosystem identification and spatial management.
研究人员在东北大西洋的Tropic Seamount海域开发并测试了一种利用声学数据和遥控潜水器(ROV)视频片段相结合的优化深海生物群落分类的迭代方法。比较了两种生物群落分类方法:基于声学基底分类的自上而下方法和基于生物特征的自下而上方法,以及仅使用生物组合的多变量分析的自下而上方法。以两种空间分辨率(200米和50米片段)对视频样带进行分析,以评估尺度效应对生物群落圈定的影响。利用地质和生物数据的组合对生物群落进行分类,每个生物群落代表了基质类型及其相关底栖生物组合的独特组合。与在200米尺度上进行更广泛的分类相比,自下而上的方法在50米尺度上确定了12种不同的生物群落,它们具有更强的环境相关性。该研究表明,较短的样带(50 m)结合自下而上的采样方法可以更好地捕捉深海海山环境的生态异质性特征,对海洋脆弱生态系统的识别和空间管理具有重要意义。
{"title":"Deep-sea biotope classification using opportunistic sampling: insights for future management","authors":"Heidy Q. Dias ,&nbsp;Kerstin Kröger ,&nbsp;Andrew J. Wheeler ,&nbsp;Riccardo Arosio ,&nbsp;Audrey Recouvreur ,&nbsp;Tim P. Le Bas ,&nbsp;Isobel A. Yeo ,&nbsp;Patrick C. Collins","doi":"10.1016/j.dsr.2025.104604","DOIUrl":"10.1016/j.dsr.2025.104604","url":null,"abstract":"<div><div>An iterative approach to optimise deep-sea biotope classification using a combination of acoustic data and Remotely Operated Vehicle (ROV) video footage was developed and tested at the Tropic Seamount site in the Northeast Atlantic. Two methods for biotope classification were compared: a top-down approach based on acoustic substrate classification followed by biological characterisation, and a bottom-up approach using multivariate analysis of biological assemblages only. Video transects were analysed at two spatial resolutions (200 m and 50 m segments) to assess scale effects on biotope delineation. Biotopes were classified using a combination of geological and biological data with each biotope representing a distinct combination of substrate types and their associated benthic assemblages. The bottom-up approach using 50 m segments identified 12 distinct biotopes with stronger environmental correlations compared to broader classifications at 200 m scale. This study demonstrates that shorter transects (50 m) combined with bottom-up sampling approaches are preferable for capturing the ecological heterogeneity characteristic of deep-sea seamount environments, with important implications for vulnerable marine ecosystem identification and spatial management.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104604"},"PeriodicalIF":2.1,"publicationDate":"2025-10-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145266257","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Integrated optical and acoustic monitoring of deep-sea bubble plume – A case study in Haima cold seep 深海气泡羽流的光声综合监测——以海马冷渗为例
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-10-08 DOI: 10.1016/j.dsr.2025.104603
Shuduo Liu , Ben Liu , Mengran Du , Chenguang Yang , Wen Xu
Monitoring underwater bubble plumes plays a vital role in understanding the plumes’ impacts on marine ecosystems. In this study, an integrated optical and acoustic deep-sea bubble plume observation system was designed and presented. The system was deployed in the Haima cold seep at a depth of 1,386 m, where a total of 4.5 h of optical and acoustic recordings were collected. Customized methods for processing both optical and acoustic data were also developed: a convolutional neural network (CNN) was used to identify individual bubbles from optical data stream, a passive acoustic bubble detection method integrating cell averaging constant false alarm rate (CA-CFAR) detector was applied to address human-induced interferences, and parabolic interpolation was employed to improve the resolution of time delay estimation for active acoustic observation. All the collected data were comprehensively processed and analyzed. The quantitative analysis of the video data yielded a mean bubble radius of 2.35 mm, and a gas flux ranging from 0.052 L/min to 0.086 L/min. The frequency-dependent sound speed variations obtained from the active acoustic data align well with existing theory on linear pressure wave propagation in bubbly liquid, suggesting the deep-sea bubbles influence the sound speed in predictable ways. This study represents an important early development of an integrated optical and acoustic system for in-situ deep-sea bubble plume monitoring, offering valuable insights and practical considerations for future iterations of related instrumentation and data analysis algorithms.
监测水下气泡羽流对了解其对海洋生态系统的影响起着至关重要的作用。本文设计并实现了一种光学与声学相结合的深海气泡羽观测系统。该系统部署在海马冷渗1386 m深度,共收集了4.5 h的光学和声学记录。此外,还开发了针对光学和声学数据的定制化处理方法:利用卷积神经网络(CNN)识别光学数据流中的单个气泡,利用集成单元平均恒定虚警率(CA-CFAR)检测器的被动声学气泡检测方法解决人为干扰,利用抛物线插值提高主动声学观测时延估计的分辨率。所有收集到的数据都进行了全面的处理和分析。视频数据的定量分析得出平均气泡半径为2.35 mm,气体通量为0.052 L/min ~ 0.086 L/min。从主动声波数据中获得的声速随频率的变化与现有的气泡液体线性压力波传播理论很好地吻合,表明深海气泡以可预测的方式影响声速。该研究代表了用于深海气泡羽流原位监测的光学和声学集成系统的重要早期发展,为未来相关仪器和数据分析算法的迭代提供了有价值的见解和实际考虑。
{"title":"Integrated optical and acoustic monitoring of deep-sea bubble plume – A case study in Haima cold seep","authors":"Shuduo Liu ,&nbsp;Ben Liu ,&nbsp;Mengran Du ,&nbsp;Chenguang Yang ,&nbsp;Wen Xu","doi":"10.1016/j.dsr.2025.104603","DOIUrl":"10.1016/j.dsr.2025.104603","url":null,"abstract":"<div><div>Monitoring underwater bubble plumes plays a vital role in understanding the plumes’ impacts on marine ecosystems. In this study, an integrated optical and acoustic deep-sea bubble plume observation system was designed and presented. The system was deployed in the Haima cold seep at a depth of 1,386 m, where a total of 4.5 h of optical and acoustic recordings were collected. Customized methods for processing both optical and acoustic data were also developed: a convolutional neural network (CNN) was used to identify individual bubbles from optical data stream, a passive acoustic bubble detection method integrating cell averaging constant false alarm rate (CA-CFAR) detector was applied to address human-induced interferences, and parabolic interpolation was employed to improve the resolution of time delay estimation for active acoustic observation. All the collected data were comprehensively processed and analyzed. The quantitative analysis of the video data yielded a mean bubble radius of 2.35 mm, and a gas flux ranging from 0.052 L/min to 0.086 L/min. The frequency-dependent sound speed variations obtained from the active acoustic data align well with existing theory on linear pressure wave propagation in bubbly liquid, suggesting the deep-sea bubbles influence the sound speed in predictable ways. This study represents an important early development of an integrated optical and acoustic system for in-situ deep-sea bubble plume monitoring, offering valuable insights and practical considerations for future iterations of related instrumentation and data analysis algorithms.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"226 ","pages":"Article 104603"},"PeriodicalIF":2.1,"publicationDate":"2025-10-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145324080","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Trophic ecology of the deep-sea skate Dipturus oxyrinchus (Linnaeus, 1758) in the bathyal food web of the central Mediterranean Sea 地中海中部深海食物网中深海冰鱼Dipturus oxyrinchus (Linnaeus, 1758)的营养生态学
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-10-04 DOI: 10.1016/j.dsr.2025.104602
Martina Arcioni , Isabella D'Ambra , Salvatrice Vizzini , Danilo Scannella , Monica Calabrò , Fabio Falsone , Michele Luca Geraci , Marco Oliverio , Sergio Vitale , Germana Garofalo , Gioacchino Bono , Francesco Colloca
The Mediterranean Sea is a biodiversity hotspot where most elasmobranchs are severely threatened, and there is limited knowledge regarding life history traits and trophic ecology. In this context, our study focuses on the trophic ecology of the longnose skate (Dipturus oxyrinchus) in the Strait of Sicily (central Mediterranean), which is designated as an Important Shark and Ray Area. The objectives of the present study were to investigate the main changes in the feeding habits of the species according to ontogeny and bathymetric distribution. We collected 152 specimens at depths between 200 and 700 m from 2016 to 2019. The combination of stomach content and stable isotope analyses allowed to classify the longnose skate as a generalist feeder, with a diet dominated by crustaceans, and smaller contributions of bony fish and cephalopods. The most consumed crustaceans were decapods (including Parapenaeus longirostris, Iridonida speciosa, Chlorotocus crassicornis) and mysids (Lophogaster typicus). Multivariate analyses indicated that predator total length and collection depth had a significant effect on the prey consumption patterns, which was corroborated by General Additive Models (GAM), allowing determination of the most commonly consumed prey. Significant ontogenetic changes were observed, with smaller individuals primarily preying upon benthic organisms and larger individuals adopting a more benthopelagic diet, reflected by a slight increase in trophic position. This study highlights the role of the longnose skate within the bathyal food web of the Strait of Sicily, providing useful information for ecosystem modelling, which will support effective conservation strategies.
地中海是一个生物多样性的热点地区,大多数板鳃动物受到严重威胁,但对其生活史特征和营养生态学的认识有限。在此背景下,我们的研究重点是长鼻鳐(Dipturus oxyrinchus)在西西里岛海峡(地中海中部)的营养生态学,该海峡被指定为鲨鱼和鳐鱼的重要区域。本研究的目的是根据个体发育和水深分布,探讨该物种摄食习性的主要变化。2016年至2019年,我们在200至700米的深度收集了152个标本。结合胃内容物和稳定同位素分析,可以将长鼻鳐归类为一种多面手的捕食者,以甲壳类动物为主,硬骨鱼和头足类动物的贡献较小。食用最多的甲壳类动物是十足类(包括长尾拟虾、绿齿虾、长角绿齿虾)和粘虫类(典型Lophogaster typicus)。多变量分析表明,捕食者的总长度和采集深度对猎物的消费模式有显著影响,并通过通用加性模型(GAM)证实了这一点,从而确定了最常消耗的猎物。观察到显著的个体发生变化,较小的个体主要捕食底栖生物,而较大的个体采用更底栖的饮食,这反映在营养地位的轻微增加上。这项研究强调了长鼻鳐在西西里岛海峡深海食物网中的作用,为生态系统建模提供了有用的信息,这将支持有效的保护策略。
{"title":"Trophic ecology of the deep-sea skate Dipturus oxyrinchus (Linnaeus, 1758) in the bathyal food web of the central Mediterranean Sea","authors":"Martina Arcioni ,&nbsp;Isabella D'Ambra ,&nbsp;Salvatrice Vizzini ,&nbsp;Danilo Scannella ,&nbsp;Monica Calabrò ,&nbsp;Fabio Falsone ,&nbsp;Michele Luca Geraci ,&nbsp;Marco Oliverio ,&nbsp;Sergio Vitale ,&nbsp;Germana Garofalo ,&nbsp;Gioacchino Bono ,&nbsp;Francesco Colloca","doi":"10.1016/j.dsr.2025.104602","DOIUrl":"10.1016/j.dsr.2025.104602","url":null,"abstract":"<div><div>The Mediterranean Sea is a biodiversity hotspot where most elasmobranchs are severely threatened, and there is limited knowledge regarding life history traits and trophic ecology. In this context, our study focuses on the trophic ecology of the longnose skate (<em>Dipturus oxyrinchus</em>) in the Strait of Sicily (central Mediterranean), which is designated as an Important Shark and Ray Area. The objectives of the present study were to investigate the main changes in the feeding habits of the species according to ontogeny and bathymetric distribution. We collected 152 specimens at depths between 200 and 700 m from 2016 to 2019. The combination of stomach content and stable isotope analyses allowed to classify the longnose skate as a generalist feeder, with a diet dominated by crustaceans, and smaller contributions of bony fish and cephalopods. The most consumed crustaceans were decapods (including <em>Parapenaeus longirostris, Iridonida speciosa</em>, <em>Chlorotocus crassicornis</em>) and mysids (<em>Lophogaster typicus</em>). Multivariate analyses indicated that predator total length and collection depth had a significant effect on the prey consumption patterns, which was corroborated by General Additive Models (GAM), allowing determination of the most commonly consumed prey. Significant ontogenetic changes were observed, with smaller individuals primarily preying upon benthic organisms and larger individuals adopting a more benthopelagic diet, reflected by a slight increase in trophic position. This study highlights the role of the longnose skate within the bathyal food web of the Strait of Sicily, providing useful information for ecosystem modelling, which will support effective conservation strategies.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104602"},"PeriodicalIF":2.1,"publicationDate":"2025-10-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145266096","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Spatial variation of diapycnal mixing estimated from high-resolution seismic images of subsurface eddies, Bering Sea 白令海地下涡旋高分辨率地震图像估算的地表旋流混合的空间变化
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-27 DOI: 10.1016/j.dsr.2025.104601
Linghan Meng, Kun Zhang, Haibin Song, Shun Yang
Turbulent mixing is a primary physical process responsible for vertical exchange of materials, heat, momentum, and energy in the ocean, and plays a key role in maintaining the overturning circulation. There are many ways to enhance ocean mixing, one of which is through oceanic eddies. However, sparse in-situ observations cannot accurately describe the structural characteristics of eddies and their contribution to turbulent mixing in the Bering Sea. In this study, we observed numerous subsurface eddies in the deep-sea region of the Bering Sea using high-resolution seismic images. These anticyclonic eddies are primarily oval-shaped or bowl-shaped, with horizontal scales of 7–65 km. The majority fall within the submesoscale range, suggesting they are mainly submesoscale eddies. They generally develop in waters shallower than 250 m, with only a few found below 300 m. Submesoscale filaments are observed on the flanks of these eddies, some of which extend downward from the eddy sides, appearing as inclined filamentous reflections. Using seismic data, we estimated diapycnal mixing and obtained its spatial distribution. The results reveal that diffusivity is significantly enhanced at the edges of eddies, especially along their sides and upper boundaries, with values reaching up to 10−3 m2 s−1. The enhanced diapycnal mixing may be related to submesoscale processes generated during eddy stirring and shear instability caused by eddy-induced velocities. Turbulent mixing induced by eddies promotes the vertical transport of heat, nutrients, and other substances in the ocean, thereby influencing primary productivity in the Bering Sea and significantly impacting the marine environment and ecosystem.
湍流混合是海洋中物质、热量、动量和能量垂直交换的主要物理过程,在维持倾覆环流中起着关键作用。增强海洋混合的方法有很多,其中之一就是通过海洋涡流。然而,稀疏的原位观测不能准确描述白令海涡旋的结构特征及其对湍流混合的贡献。在这项研究中,我们使用高分辨率地震图像观察了白令海深海地区的许多地下漩涡。这些反气旋涡旋主要呈椭圆形或碗形,水平尺度为7-65公里。大多数在亚中尺度范围内,表明它们主要是亚中尺度涡旋。它们一般生长在250米以下的水域,只有少数生长在300米以下。在这些涡旋的侧面观察到亚中尺度细丝,其中一些从涡旋侧面向下延伸,表现为倾斜的丝状反射。利用地震资料,估计了河床混合作用,得到了其空间分布。结果表明,涡旋边缘的扩散系数显著增强,特别是沿涡旋边缘和上边界的扩散系数可达10−3 m2 s−1。湍流混合的增强可能与涡旋搅拌过程中产生的亚中尺度过程和涡旋诱导速度引起的剪切不稳定有关。涡流引起的湍流混合促进了海洋中热量、营养物质和其他物质的垂直输送,从而影响了白令海的初级生产力,对海洋环境和生态系统产生了重大影响。
{"title":"Spatial variation of diapycnal mixing estimated from high-resolution seismic images of subsurface eddies, Bering Sea","authors":"Linghan Meng,&nbsp;Kun Zhang,&nbsp;Haibin Song,&nbsp;Shun Yang","doi":"10.1016/j.dsr.2025.104601","DOIUrl":"10.1016/j.dsr.2025.104601","url":null,"abstract":"<div><div>Turbulent mixing is a primary physical process responsible for vertical exchange of materials, heat, momentum, and energy in the ocean, and plays a key role in maintaining the overturning circulation. There are many ways to enhance ocean mixing, one of which is through oceanic eddies. However, sparse in-situ observations cannot accurately describe the structural characteristics of eddies and their contribution to turbulent mixing in the Bering Sea. In this study, we observed numerous subsurface eddies in the deep-sea region of the Bering Sea using high-resolution seismic images. These anticyclonic eddies are primarily oval-shaped or bowl-shaped, with horizontal scales of 7–65 km. The majority fall within the submesoscale range, suggesting they are mainly submesoscale eddies. They generally develop in waters shallower than 250 m, with only a few found below 300 m. Submesoscale filaments are observed on the flanks of these eddies, some of which extend downward from the eddy sides, appearing as inclined filamentous reflections. Using seismic data, we estimated diapycnal mixing and obtained its spatial distribution. The results reveal that diffusivity is significantly enhanced at the edges of eddies, especially along their sides and upper boundaries, with values reaching up to 10<sup>−3</sup> m<sup>2</sup> s<sup>−1</sup>. The enhanced diapycnal mixing may be related to submesoscale processes generated during eddy stirring and shear instability caused by eddy-induced velocities. Turbulent mixing induced by eddies promotes the vertical transport of heat, nutrients, and other substances in the ocean, thereby influencing primary productivity in the Bering Sea and significantly impacting the marine environment and ecosystem.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104601"},"PeriodicalIF":2.1,"publicationDate":"2025-09-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145219856","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Variability of the Weddell Sea deep waters in GLORYS12v1 reanalysis 在GLORYS12v1再分析中威德尔海深水的变率
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-26 DOI: 10.1016/j.dsr.2025.104599
Marina Noro , Tiago S. Dotto , Marcos Tonelli , Ilana Wainer
Understanding deep-water variability in the Weddell Sea remains a challenge, given the limited observational coverage and the difficulties ocean models face in representing fine-scale processes, particularly along the Antarctic margin. Recent high-resolution oceanic products offer a valuable opportunity to advance understanding of this region. Nevertheless, it is crucial to critically evaluate their reliability before relying on them for scientific analysis. Here, we assess the representation and variability of Warm Deep Water (WDW), Weddell Sea Deep Water (WSDW), and Weddell Sea Bottom Water (WSBW) in the 1/12° Global Ocean Physics Reanalysis (GLORYS12v1) between 1993 and 2020. GLORYS12v1 reproduces key hydrographic features and vertical stratification below 500 m, despite persistent biases in the upper ocean. WDW shows a spurious freshening trend and a cool bias in Section SR4, diverging from the observed neutral salinity and warming trend. Moreover, WSDW and WSBW exhibit overestimated warming and salinification trends. These discrepancies are primarily linked to (i) a weakening of the Weddell Gyre, which limits inflow and renewal of deep waters; (ii) stronger westerlies enhancing Ekman transport and upwelling; and (iii) changes in sea ice concentration affecting deep convection. A complex maximum covariance analysis reveals strong decadal-scale covariability between the Weddell Gyre barotropic circulation and the thermohaline structure of deep water masses, especially WSDW and WSBW. Although GLORYS12v1 resolves many relevant processes, its overestimation of trends and underrepresentation of coastal dynamics highlight the need for improved vertical coordinate schemes, refined mixing parameterizations, and enhanced observational coverage to better capture the variability of deep waters in polar regions.
考虑到有限的观测覆盖范围和海洋模式在代表精细尺度过程方面面临的困难,特别是在南极边缘,了解威德尔海的深水变化仍然是一个挑战。最近的高分辨率海洋产品为进一步了解该地区提供了宝贵的机会。然而,在依靠它们进行科学分析之前,批判性地评估它们的可靠性是至关重要的。在此,我们评估了1993 - 2020年1/12°全球海洋物理再分析(GLORYS12v1)中暖深水(WDW)、威德尔海深水(WSDW)和威德尔海底水(WSBW)的代表性和变率。GLORYS12v1再现了500米以下的关键水文特征和垂直分层,尽管在上层海洋中存在持续的偏差。在SR4剖面中,WDW表现出虚假的变冷趋势和偏冷趋势,偏离了观测到的中性盐度和变暖趋势。此外,WSDW和WSBW表现出高估的变暖和盐化趋势。这些差异主要与(1)威德尔环流的减弱有关,这限制了深水的流入和更新;(ii)较强西风带加强艾克曼运输及上升流;(三)影响深层对流的海冰浓度变化。复最大协方差分析表明,威德尔环流正压环流与深水团温盐结构,特别是与wsw和WSBW的温盐结构之间具有较强的年代际协变性。虽然GLORYS12v1解决了许多相关过程,但其对趋势的高估和对沿海动态的代表性不足,突出表明需要改进垂直坐标方案,改进混合参数化,并扩大观测覆盖范围,以便更好地捕捉极地深水的变率。
{"title":"Variability of the Weddell Sea deep waters in GLORYS12v1 reanalysis","authors":"Marina Noro ,&nbsp;Tiago S. Dotto ,&nbsp;Marcos Tonelli ,&nbsp;Ilana Wainer","doi":"10.1016/j.dsr.2025.104599","DOIUrl":"10.1016/j.dsr.2025.104599","url":null,"abstract":"<div><div>Understanding deep-water variability in the Weddell Sea remains a challenge, given the limited observational coverage and the difficulties ocean models face in representing fine-scale processes, particularly along the Antarctic margin. Recent high-resolution oceanic products offer a valuable opportunity to advance understanding of this region. Nevertheless, it is crucial to critically evaluate their reliability before relying on them for scientific analysis. Here, we assess the representation and variability of Warm Deep Water (WDW), Weddell Sea Deep Water (WSDW), and Weddell Sea Bottom Water (WSBW) in the 1/12° Global Ocean Physics Reanalysis (GLORYS12v1) between 1993 and 2020. GLORYS12v1 reproduces key hydrographic features and vertical stratification below 500 m, despite persistent biases in the upper ocean. WDW shows a spurious freshening trend and a cool bias in Section SR4, diverging from the observed neutral salinity and warming trend. Moreover, WSDW and WSBW exhibit overestimated warming and salinification trends. These discrepancies are primarily linked to (i) a weakening of the Weddell Gyre, which limits inflow and renewal of deep waters; (ii) stronger westerlies enhancing Ekman transport and upwelling; and (iii) changes in sea ice concentration affecting deep convection. A complex maximum covariance analysis reveals strong decadal-scale covariability between the Weddell Gyre barotropic circulation and the thermohaline structure of deep water masses, especially WSDW and WSBW. Although GLORYS12v1 resolves many relevant processes, its overestimation of trends and underrepresentation of coastal dynamics highlight the need for improved vertical coordinate schemes, refined mixing parameterizations, and enhanced observational coverage to better capture the variability of deep waters in polar regions.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104599"},"PeriodicalIF":2.1,"publicationDate":"2025-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145219855","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A near field study of sediment plumes for a pre-prototype nodule collector trial in the abyssal Pacific Ocean 太平洋深海结核收集器试验原型前期沉积物羽流的近场研究
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-25 DOI: 10.1016/j.dsr.2025.104595
Raphael Ouillon, Carlos Muñoz-Royo, Souha El Mousadik, Thomas Peacock
Observations from multi-platform monitoring of the sediment plume created during a pre-prototype deep-seabed nodule mining collector trial in the Pacific Ocean are presented and discussed. A combination of fundamental and geophysical fluid dynamics theory, as well as built-for-purpose numerical modeling, is used to interpret the observations. In turn, the implications of the interpreted observations for both monitoring and modeling of deep-seabed mining sediment plumes are considered. The observations occurred over a wide range of spatial and temporal scales, obtained through collector-mounted instruments within the mining area, instrumented moorings hundreds of meters away from the mining activity, and instrumented AUV operations at distances of hundreds to thousands of meters away from the test site. At each scale, interpreting plume observations is non-trivial because of the complexity of plume dynamics. Through interpretation of the observations, we exemplify the challenge of using plume monitoring or modeling alone in order to create a complete, non-ambiguous representation of the plume that is spatio-temporally resolved. Our analysis shows that an effective strategy that encompasses monitoring technology, deployment configuration, data interpretation, modeling approach, model parametrization, and model validation must be informed by plume physics at all levels. Furthermore, non-hydrostatic physics are instrumental to the evolution of plumes, and thus plume modeling for deep-sea mining sediment plumes needs to resolve non-hydrostatic processes.
本文介绍并讨论了对太平洋深海结核采矿收集器试验中产生的沉积物羽流的多平台监测结果。基础和地球物理流体动力学理论的结合,以及专门的数值模拟,被用来解释观测结果。反过来,解释观测对深海底采矿沉积物羽流的监测和建模的影响也被考虑。观测发生在广泛的空间和时间尺度上,通过采矿区内安装的采集器仪器,距离采矿活动数百米的仪器系泊,以及距离试验场数百至数千米的仪器AUV操作获得。在每个尺度上,由于羽流动力学的复杂性,解释羽流观测是非平凡的。通过对观测结果的解释,我们举例说明了单独使用羽流监测或建模的挑战,以便创建一个完整的、无歧义的羽流时空解析表示。我们的分析表明,一个有效的策略,包括监测技术、部署配置、数据解释、建模方法、模型参数化和模型验证,必须从各个层面上了解羽流物理。此外,非流体静力物理对羽流演化具有重要意义,因此深海采矿沉积物羽流模拟需要解决非流体静力过程。
{"title":"A near field study of sediment plumes for a pre-prototype nodule collector trial in the abyssal Pacific Ocean","authors":"Raphael Ouillon,&nbsp;Carlos Muñoz-Royo,&nbsp;Souha El Mousadik,&nbsp;Thomas Peacock","doi":"10.1016/j.dsr.2025.104595","DOIUrl":"10.1016/j.dsr.2025.104595","url":null,"abstract":"<div><div>Observations from multi-platform monitoring of the sediment plume created during a pre-prototype deep-seabed nodule mining collector trial in the Pacific Ocean are presented and discussed. A combination of fundamental and geophysical fluid dynamics theory, as well as built-for-purpose numerical modeling, is used to interpret the observations. In turn, the implications of the interpreted observations for both monitoring and modeling of deep-seabed mining sediment plumes are considered. The observations occurred over a wide range of spatial and temporal scales, obtained through collector-mounted instruments within the mining area, instrumented moorings hundreds of meters away from the mining activity, and instrumented AUV operations at distances of hundreds to thousands of meters away from the test site. At each scale, interpreting plume observations is non-trivial because of the complexity of plume dynamics. Through interpretation of the observations, we exemplify the challenge of using plume monitoring or modeling alone in order to create a complete, non-ambiguous representation of the plume that is spatio-temporally resolved. Our analysis shows that an effective strategy that encompasses monitoring technology, deployment configuration, data interpretation, modeling approach, model parametrization, and model validation must be informed by plume physics at all levels. Furthermore, non-hydrostatic physics are instrumental to the evolution of plumes, and thus plume modeling for deep-sea mining sediment plumes needs to resolve non-hydrostatic processes.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104595"},"PeriodicalIF":2.1,"publicationDate":"2025-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145320709","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Crustacean assemblage structure over the Charlie-Gibbs Fracture Zone of the Mid-Atlantic Ridge collected during the 2009 Henry B. Bigelow expedition 2009年Henry B. Bigelow探险队收集的大西洋中脊查理-吉布斯断裂带上的甲壳类动物组合结构
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-24 DOI: 10.1016/j.dsr.2025.104596
Kathryn E. Medina, Rosanna J. Milligan, Tracey T. Sutton, Tamara Frank
The Charlie Gibbs Fracture Zone (CGFZ) consists of two nearly parallel fracture transform faults that intersect the Mid-Atlantic Ridge (MAR) axis. This area has high primary productivity and biomass levels due to the topography and water. A predominant hydrographic feature of the MAR is the Sub-Polar Front (SPF) which runs along the southern edge of the CGFZ and is known as a biogeographical boundary for multiple species. As part of The Census of Marine Life project Patterns and Processes of the Ecosystem of the northern Mid-Atlantic (MAR-ECO), the abundance and distribution patterns of the CGFZ crustacean community (primarily Decapoda) surveyed during the 2009 H B. Bigelow voyage were analyzed. Specimens were collected from five discrete depths, ranging between 0 and 3500 m deep, using a Norwegian microzooplankton trawl equipped with a multi-sampler. Analyses indicate that geographic location relative to the CGFZ is correlated to pelagic crustacean distribution, but the surrounding water masses are likely the primary drivers of abundance and diversity variations. The abundance of pelagic crustaceans was higher in the cold waters to the northwest of the CGFZ. A higher diversity was found in the warmer southeastern waters presumably due to stable influx of nutrients and food supply, and dominating mesoscale eddies located in the southeast of the study area. Benthic crustaceans in the northwest had an increased abundance and diversity compared the southeast region. This suggests that at depth, the MAR may act as a biogeographic barrier separating the two geographic regions and reducing connectivity.
查理吉布斯断裂带(CGFZ)由两条几乎平行的断裂转换断层组成,它们与大西洋中脊(MAR)轴线相交。由于地形和水,该地区具有较高的初级生产力和生物量水平。南海的一个主要水文特征是亚极锋(SPF),它沿着CGFZ的南部边缘,被称为多种物种的生物地理边界。作为中大西洋北部海洋生物生态系统模式和过程普查项目(MAR-ECO)的一部分,分析了2009年毕格罗航次期间调查的CGFZ甲壳类(主要是十足类)群落的丰度和分布格局。使用配备多采样器的挪威微型浮游动物拖网,从0至3500米深的五个不同深度收集标本。分析表明,相对于CGFZ的地理位置与上层甲壳类的分布有关,但周围的水体可能是甲壳类丰度和多样性变化的主要驱动因素。中上层甲壳类动物的丰度在冻土带西北部的冷水区较高。在温暖的东南海域,由于营养物质和食物供应的稳定流入,以及研究区东南部的中尺度涡流占主导地位,发现了更高的多样性。西北地区底栖甲壳类动物的丰度和多样性均高于东南地区。这表明,在深度上,MAR可能是分隔两个地理区域并降低连通性的生物地理屏障。
{"title":"Crustacean assemblage structure over the Charlie-Gibbs Fracture Zone of the Mid-Atlantic Ridge collected during the 2009 Henry B. Bigelow expedition","authors":"Kathryn E. Medina,&nbsp;Rosanna J. Milligan,&nbsp;Tracey T. Sutton,&nbsp;Tamara Frank","doi":"10.1016/j.dsr.2025.104596","DOIUrl":"10.1016/j.dsr.2025.104596","url":null,"abstract":"<div><div>The Charlie Gibbs Fracture Zone (CGFZ) consists of two nearly parallel fracture transform faults that intersect the Mid-Atlantic Ridge (MAR) axis. This area has high primary productivity and biomass levels due to the topography and water. A predominant hydrographic feature of the MAR is the Sub-Polar Front (SPF) which runs along the southern edge of the CGFZ and is known as a biogeographical boundary for multiple species. As part of The Census of Marine Life project Patterns and Processes of the Ecosystem of the northern Mid-Atlantic (MAR-ECO), the abundance and distribution patterns of the CGFZ crustacean community (primarily Decapoda) surveyed during the 2009 H B. Bigelow voyage were analyzed. Specimens were collected from five discrete depths, ranging between 0 and 3500 m deep, using a Norwegian microzooplankton trawl equipped with a multi-sampler. Analyses indicate that geographic location relative to the CGFZ is correlated to pelagic crustacean distribution, but the surrounding water masses are likely the primary drivers of abundance and diversity variations. The abundance of pelagic crustaceans was higher in the cold waters to the northwest of the CGFZ. A higher diversity was found in the warmer southeastern waters presumably due to stable influx of nutrients and food supply, and dominating mesoscale eddies located in the southeast of the study area. Benthic crustaceans in the northwest had an increased abundance and diversity compared the southeast region. This suggests that at depth, the MAR may act as a biogeographic barrier separating the two geographic regions and reducing connectivity.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104596"},"PeriodicalIF":2.1,"publicationDate":"2025-09-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145266256","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Transformations of particulate organic matter from the surface to the abyssal plain in the North Pacific as inferred from compound-specific stable isotope and microbial community analyses 从特定化合物稳定同位素和微生物群落分析推断的北太平洋深海平原表层颗粒有机质向深海平原的转化
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-23 DOI: 10.1016/j.dsr.2025.104597
Lee C. Miller , Hilary G. Close , Kalina C. Grabb , Christine L. Huffard , Fuyan Li , David M. Karl , Kenneth L. Smith , Edward F. DeLong , Claudia R. Benitez-Nelson , Jeffrey C. Drazen , Brian N. Popp
Particulate organic matter (POM) produced in surface waters undergoes extensive reworking and breakdown by microbial and metazoan communities as it sinks to the abyssal seafloor and serves as the base of benthic and pelagic food webs. Here, we examined how various size classes of POM in the oligotrophic North Pacific Subtropical Gyre (Station ALOHA) and in the eutrophic California Current System (Station M) undergo microbial alteration throughout the water column. Compound-specific stable isotope analysis showed that sampling method strongly impacts the type of POM quantified as export to the deep sea. Moored abyssal sediment traps captured material that matched the isotopic composition of surface POM, indicating they collected large, fast-sinking particles, in contrast to the more heavily reworked particles collected with in situ filtration at the same depths. Extending δ15N analyses of amino acids to bathypelagic and abyssopelagic depths for the first time, we confirmed that most particle remineralization and reworking occurs within the upper ∼400 m of the water column regardless of initial surface productivity. At Station ALOHA, we further used 16S rRNA barcoding to characterize the microbial communities associated with the POM. We found that chemolithoautotrophic ammonia-oxidizing archaea are abundant in the upper water column at Station ALOHA and that their abundance corresponded to regions of high heterotrophic reworking as indicated by amino acid isotope analysis.
在地表水中产生的颗粒有机物质(POM)在下沉到深海海底并作为底栖生物和远洋食物网的基础时,经过微生物和后生动物群落的广泛改造和分解。在这里,我们研究了贫营养北太平洋副热带环流(ALOHA站)和富营养加利福尼亚洋流系统(M站)中不同大小类别的POM如何在整个水柱中经历微生物改变。化合物特异性稳定同位素分析表明,采样方法对定量输出到深海的POM类型有强烈影响。系泊的深海沉积物捕集器捕获的物质与表面POM的同位素组成相匹配,表明它们收集了大而快速下沉的颗粒,与在相同深度通过原位过滤收集的更重加工的颗粒形成对比。我们首次将氨基酸的δ15N分析扩展到深海和深海,证实了大多数颗粒再矿化和再加工发生在水柱的上部~ 400 m,而不管初始表面生产力如何。在ALOHA站点,我们进一步使用16S rRNA条形码来表征与POM相关的微生物群落。研究发现,在ALOHA站的上层水柱中存在丰富的化化岩自养氨氧化古菌,氨基酸同位素分析表明,它们的丰度与高异养重工区相对应。
{"title":"Transformations of particulate organic matter from the surface to the abyssal plain in the North Pacific as inferred from compound-specific stable isotope and microbial community analyses","authors":"Lee C. Miller ,&nbsp;Hilary G. Close ,&nbsp;Kalina C. Grabb ,&nbsp;Christine L. Huffard ,&nbsp;Fuyan Li ,&nbsp;David M. Karl ,&nbsp;Kenneth L. Smith ,&nbsp;Edward F. DeLong ,&nbsp;Claudia R. Benitez-Nelson ,&nbsp;Jeffrey C. Drazen ,&nbsp;Brian N. Popp","doi":"10.1016/j.dsr.2025.104597","DOIUrl":"10.1016/j.dsr.2025.104597","url":null,"abstract":"<div><div>Particulate organic matter (POM) produced in surface waters undergoes extensive reworking and breakdown by microbial and metazoan communities as it sinks to the abyssal seafloor and serves as the base of benthic and pelagic food webs. Here, we examined how various size classes of POM in the oligotrophic North Pacific Subtropical Gyre (Station ALOHA) and in the eutrophic California Current System (Station M) undergo microbial alteration throughout the water column. Compound-specific stable isotope analysis showed that sampling method strongly impacts the type of POM quantified as export to the deep sea. Moored abyssal sediment traps captured material that matched the isotopic composition of surface POM, indicating they collected large, fast-sinking particles, in contrast to the more heavily reworked particles collected with <em>in situ</em> filtration at the same depths. Extending δ<sup>15</sup>N analyses of amino acids to bathypelagic and abyssopelagic depths for the first time, we confirmed that most particle remineralization and reworking occurs within the upper ∼400 m of the water column regardless of initial surface productivity. At Station ALOHA, we further used 16S rRNA barcoding to characterize the microbial communities associated with the POM. We found that chemolithoautotrophic ammonia-oxidizing archaea are abundant in the upper water column at Station ALOHA and that their abundance corresponded to regions of high heterotrophic reworking as indicated by amino acid isotope analysis.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104597"},"PeriodicalIF":2.1,"publicationDate":"2025-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145157709","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Design and experimentation of self-contained digital cone for deep sea 深海独立式数字锥的设计与实验
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-09-23 DOI: 10.1016/j.dsr.2025.104600
Zhangyong Jin , Jin Guo , Jiawang Chen , Bijin Liu , Zhonghui Zhou , Feng Gao , Ziqiang Ren
Seabed soil properties play an essential role in a wide range of marine engineering applications. This study presents the design of a distinctive self-contained cone that is in line with international standards and suitable for deep-sea operations. This design aims to address and overcome the current limitations faced by cone penetration testing probes, such as problems related to rod connections and signal attenuation. An inclination-based posture correction algorithm was introduced to obtain vertical penetration displacement. Additionally, a calibration curve was established between applied load on the probe and the recorded strain gauge signal. Based on theoretical calculations and finite element simulation experiments, an analysis and research were carried out on the impact of deep-sea environmental factors, such as high-pressure environments and seal ring friction, on penetration survey results. Simultaneously, a tidal flat test was performed. By comparing the data collected by the probe with that of the vane shear test, the accuracy of the probe was verified. In the final implementation stage, the cone was introduced to a specially designed CPT station in the South China Sea. The obtained geotechnical parameters largely corresponded with the previously examined strata characteristics, confirming the cone's reliability and effectiveness for in-situ survey work in deep-sea environments.
海底土壤特性在海洋工程中有着广泛的应用。本研究提出了一种独特的、符合国际标准的、适合深海作业的独立锥体设计。该设计旨在解决和克服锥体穿透测试探头目前面临的局限性,例如与杆连接和信号衰减有关的问题。提出了一种基于倾斜的姿态校正算法来获取垂直侵彻位移。此外,在探头上施加的载荷与记录的应变片信号之间建立了校准曲线。基于理论计算和有限元模拟实验,分析研究了深海高压环境、密封圈摩擦等环境因素对侵彻测量结果的影响。同时进行了潮平试验。通过将探头采集的数据与叶片剪切试验数据进行对比,验证了探头的准确性。在最后实施阶段,该锥被引入中国南海一个特别设计的CPT站。获得的岩土参数与之前检测的地层特征基本吻合,证实了锥筒在深海环境中进行原位测量工作的可靠性和有效性。
{"title":"Design and experimentation of self-contained digital cone for deep sea","authors":"Zhangyong Jin ,&nbsp;Jin Guo ,&nbsp;Jiawang Chen ,&nbsp;Bijin Liu ,&nbsp;Zhonghui Zhou ,&nbsp;Feng Gao ,&nbsp;Ziqiang Ren","doi":"10.1016/j.dsr.2025.104600","DOIUrl":"10.1016/j.dsr.2025.104600","url":null,"abstract":"<div><div>Seabed soil properties play an essential role in a wide range of marine engineering applications. This study presents the design of a distinctive self-contained cone that is in line with international standards and suitable for deep-sea operations. This design aims to address and overcome the current limitations faced by cone penetration testing probes, such as problems related to rod connections and signal attenuation. An inclination-based posture correction algorithm was introduced to obtain vertical penetration displacement. Additionally, a calibration curve was established between applied load on the probe and the recorded strain gauge signal. Based on theoretical calculations and finite element simulation experiments, an analysis and research were carried out on the impact of deep-sea environmental factors, such as high-pressure environments and seal ring friction, on penetration survey results. Simultaneously, a tidal flat test was performed. By comparing the data collected by the probe with that of the vane shear test, the accuracy of the probe was verified. In the final implementation stage, the cone was introduced to a specially designed CPT station in the South China Sea. The obtained geotechnical parameters largely corresponded with the previously examined strata characteristics, confirming the cone's reliability and effectiveness for in-situ survey work in deep-sea environments.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"225 ","pages":"Article 104600"},"PeriodicalIF":2.1,"publicationDate":"2025-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145219854","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
期刊
Deep-Sea Research Part I-Oceanographic Research Papers
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1