Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (5): 119-132.DOI: 10.13745/j.esf.sf.2021.5.2

Previous Articles     Next Articles

Effects of biocomponent on the geotechnical properties of seafloor surface sediments in the Western Pacific Warm Pool

ZHOU Shang1,2(), XU Jishang1,2,3, LIU Yong1,2,*(), LI Guangxue1,2,3, LI Anlong1,2,3, CAO Lihua1,2,3, ZHAI Ke4, XU Jizheng3, QUAN Yongzheng1,2   

  1. 1. Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Ocean University of China, Qingdao 266100, China
    2. College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
    3. Engineering Research Center of Marine Petroleum Development and Security Safeguard, MOE, Ocean University of China, Qingdao 266100, China
    4. Qingdao Haida Ocean Energy Engineering Technology Co. Ltd,Qingdao 266073, China
  • Received:2021-02-17 Revised:2021-04-22 Online:2022-09-25 Published:2022-08-24
  • Contact: LIU Yong

Abstract:

The Western Pacific Warm Pool (WPWP) is located in the tropical western Pacific and the eastern Indian Ocean with an average annual surface water temperature of over 28 ℃. Due to the varying depositional environments under different tectonic settings, the biocomponent contents in pelagic sediments of the WPWP differ greatly. Biocomponents have a significant impact on the geotechnical properties of deep-see sediments, however, the correlation between the two has not been studied previously. To fill this gap, we investigated the geotechnical properties of surface sediments in the core of the WPWP and identified the sediment components under microscope. As results show, the natural moisture content ranges from 61.1% to 435.1%, natural density from 1.04 to 1.76 g/cm3, penetration resistance from 0 to 100 kPa, and vane shear strength from 0 to 8.6 kPa. The high natural moisture content, low natural density, and low shear strength are consistent with the characteristics of typical geotechnical properties of deep-sea sediment. Calcareous sediments of the Western Carolingian ridge, seamounts and other areas with water depths less than the CCD (Carbonate Compensation Depth) generally contain more than 50% calcareous biocomponents, and the same proportion of siliceous biocomponents is likely found in siliceous sediments of the southwestern Western Carolingian trough and surrounding deep trench areas; whereas clay sediments mainly distribute in the Western Carolingian basin. With decreasing calcareous and increasing siliceous biocomponents, the surface sediment varies from calcareous to clay to siliceous and its natural moisture content increases while its natural density, penetration resistance and vane shear strength decrease. It suggests that the geotechnical properties of deep-sea surface sediment are correlated with the contents of biocomponents—specifically, its penetration resistance, vane shear strength and natural density are positively influenced by calcareous biocomponents and negatively influenced by siliceous biocomponents, while the opposite holds true for natural moisture content. This paper establishes the relationship between biocomponent and geotechnical properties of abyssal sediments, and proposes a fitting formula between the biocomponent content and geotechnical properties, which is useful for evaluating the geotechnical properties of deep-sea sediments.

Key words: deep-sea surface sediment, biocomponent, natural moisture content, natural density, penetration resistance, vane shear strength

CLC Number: