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Open AccessDOI: 10.1016/j.ijmst.2025.06.001Original Research

Mechanism of low-disturbance and high-pressure-retaining sampling of seafloor sediments at 10000-meter depth and its laboratory experiment and on-site sea trials

Guangping Liu¹,Shanqiang Jiang¹,Yongping Jin¹,Buyan Wan¹,Liang Liu¹,Youduo Peng¹

National-Local Joint Engineering Laboratory of Marine Mineral Resources Exploration Equipment and Safety Technology, Hunan University of Science and Technology, Xiangtan 411201, China

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Mechanism of low-disturbance and high-pressure-retaining sampling of seafloor sediments at 10000-meter depth and its laboratory experiment and on-site sea trials
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Published In
Academic Research Journal
Published:January 15, 2025Edition:Vol. 32, Issue 6 • pp. 100-112Citation:Guangping Liu et al. (2025), Academic Research Journal
Impact FactorPeer-Reviewed Core
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Key Takeaways & Executive Findings

  • • A novel deep-sea sediment pressure-retaining sampler achieves pressure preservation rates of 94.21% and 92.02% at depths of 9298.4 m and 9142.8 m, significantly exceeding the current 80% technical indicator. • A radial disturbance model based on spherical cavity expansion theory was developed to quantify sediment disturbance, using the plastic deformation radius as an evaluation index. • Indoor experiments with embedded sensors validated the theoretical model, confirming the accuracy of predicted radial stress and pore water pressure distributions. • On-site sea trials in the Kuril-Kamchatka Trench retrieved sediment samples with clear stratification and minimal disturbance, demonstrating the sampler's effectiveness for deep-sea geological research.
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Abstract

Obtaining high-quality 10000-meter-deep seafloor sediment samples is the prerequisite and foundation for conducting deep-sea geological and environmental scientific research. The bottom structure of the deep seafloor is complex, and the physical and mechanical properties and disturbance resistance of sediments of different lithologies vary greatly, so the sediment sampler inevitably disturbs the sediments during the sampling process and affects the quality of the sediment samples. A new type of deep-sea sediment pressure retaining sampler is introduced, the force state and elastic–plastic state of the sampler destroying sediments are analyzed, the radial disturbance model of sediment coring based on the spherical cavity expansion theory is established, and the radius of sediments undergoing plastic deformation around the spherical holes is used as an index for evaluating the radial disturbance of sediments. The distribution of stress and strain fields in the sediments during the expansion of the spherical cavity and the influencing factors of the radius of the radially disturbed region (plastic region) are analyzed using an arithmetic example, and the influence law is analyzed. A sediment disturbance experimental platform was built indoors to simulate the sediment coring process. The radial stress field and pore water pressure of the sediment during the coring process were monitored by sensors arranged inside the sediment, and the results of indoor tests verified the correctness of the perturbation theory model. The sampler was carried aboard the deep-sea manned submersible FENDOUZHE and conducted on-site tests at depths of 9298.4 and 9142.8 m in the Kuril-Kamchatka Trench. Pressure-preserved sediment samples were retrieved, with preservation rates of 94.21% and 92.02%, respectively, which are much higher than the current technical indicator of 80% of pressure-holding ratio for deep-sea sediments. The retrieved sediments have obvious stratification characteristics and little disturbance.

1. Introduction

The seafloor is rich in hydrocarbons, minerals, organisms, sediments, and other resources [1], and the acquisition of these seafloor resources is entirely dependent on advanced seafloor collection methods and technical equipment [2]. As the stratigraphic structure of the deep seabed is very complex, and the physical and mechanical properties of sediments of different lithologies and their resistance to disturbance vary greatly [3,4], sampling equipment inevitably disturbs the sediments during the sampling process, which affects the quality of the sediment samples and even prevents the retrieval of the sediment samples. In addition to not reflecting its basic composition, the disturbed samples cannot effectively reflect its engineering properties and in-situ characteristics, and it is inaccurate to use them as the basis for seafloor scientific research and resource development, especially as the basis for seafloor engineering and construction, which is extremely dangerous [5,6]. Therefore, it is of great significance to obtain in-situ low-disturbance sediment samples.

At present, the basis of sediment disturbance discrimination includes three ways...

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Cite This Research Paper
Guangping Liu, Shanqiang Jiang, Yongping Jin, Buyan Wan, Liang Liu, Youduo Peng (2025). Mechanism of low-disturbance and high-pressure-retaining sampling of seafloor sediments at 10000-meter depth and its laboratory experiment and on-site sea trials. SinoTechIntel Verified Research. https://doi.org/10.1016/j.ijmst.2025.06.001
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Frequently Asked Questions

What is the significance of obtaining high-quality deep-sea sediment samples?

High-quality deep-sea sediment samples are essential for accurate geological and environmental research, as disturbed samples fail to reflect in-situ properties and can lead to dangerous engineering decisions.

How does the new sampler achieve high pressure retention?

The sampler is designed to maintain pressure during retrieval, achieving preservation rates of 94.21% and 92.02% in sea trials, far exceeding the 80% standard, through advanced mechanical design and pressure-retaining mechanisms.

What is the spherical cavity expansion theory used for?

It is used to model the radial disturbance of sediments during coring, providing a quantitative index (plastic deformation radius) to evaluate and minimize disturbance.

How were the theoretical models validated?

Indoor experiments with embedded sensors monitored radial stress and pore water pressure, and the results matched the theoretical predictions, confirming the model's correctness.

What were the results of the on-site sea trials?

The sampler was tested at depths of 9298.4 m and 9142.8 m in the Kuril-Kamchatka Trench, retrieving pressure-preserved sediment samples with high pressure retention and minimal disturbance, showing clear stratification.

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