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Pore pressures in marine sediments: An overview of measurement techniques and some geological and engineering applications

  • Part II: Sampling Technique
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Abstract

Pore pressures in the seabed are extremely sensitive to any imposed stress because of the low permeabilities commonly exhibited by marine sediments. Consequently, the measurement of sediment pore pressures can be used to infer either the nature of the imposed stress (if the sediment properties are known) or the physical properties of the sediment (if the imposed stresses are known). Stresses of many different types may be exerted on the seabed either through hydrostatic forces (e.g. tidal and wave effects), or directly by lithospheric forces (e.g. tectonic and thermal forces). Several techniques for measuring in situ pore pressures in the upper few metres of sediments have been developed, and one instrument, the PUPPI, will operate autonomously in water depths up to 6000 m. Basic sediment properties and processes can already be inferred from pore pressure responses using this technique. However, further application and development could greatly enhance its capability, especially for long-term monitoring of sediment conditions. In this Chapter, pore pressure measurement techniques are briefly reviewed and problems are highlighted. An outline is given of some of the many ways in which pore pressure measurements could be used to gain further insight into geological processes and to determine some of the pertinent sediment properties more accurately for engineering applications.

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  1. P. J. Schultheiss

    Present address: Deacon Laboratory, Institute of Oceanographic Sciences, Wormley, GU8 5UB, Godalming, Surrey, UK

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  1. Schultheiss Geotek, Fern Cottage, Marley Lane, GU27 3RF, Haslemere, Surrey, UK

    P. J. Schultheiss

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Schultheiss, P.J. Pore pressures in marine sediments: An overview of measurement techniques and some geological and engineering applications. Marine Geophysical Researches 12, 153–168 (1990). https://doi.org/10.1007/BF00310570

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  • DOI: https://doi.org/10.1007/BF00310570

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