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HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
Citation: HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.

Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors

  • Received Date: 2000-06-09
  • Rev Recd Date: 2000-11-23
  • Spatio-temporal variation of subsurface porosity and permeability is controlled by various factors during sedimentation and diagcncsis.The dcpositional environments and the types of sediment basin control the original composition before hurial, texture and porosity of sediments.The sedimentary factors to control the porosity and permeability are mainly sedimentary facics, stratigraphy sequences and so on.The process of sedimentation was much shorter than the diagcncsis, and relatively easy to study.Recently, some traditional mechanism of secondary porosity formation for subsurface sediment is challenged by new theories.The formation of secondary porosity from the aluminium-silicate solution by organic acid is the most important mechanism.However it will result in the increase of pH value precipitation of carbonate and kaolinitc.The dissolulion by carbonic water to form the secondary porosity in subsurface is also limited.Ncw mechanism such as dissolution of sediment by the meteoric water by the deep cooling formation water proves effective and hydrolysis of the silicates is also accepted universally.In addition, the precipitation and material sources of some diagcnctic authigcnic minerals related to the secondary porosity also have new mode.These are several essentials to understand the formation of secondary porosity and estimate the porosity and the permeability of the reservoir. For the carbonate rocks the oil/gas reservoir related to the palco-carst nearby the unconformitv have got more attention. During the deep burial diagenesis, the temperature and prcssure control the difference of the habit of dissolution and precipitation for different carbonate minerals leading to the differcncc of porosity and permeability distribution in subsurface carbonate rocks, which is very important for prediction of carhonate reservoir.
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  • Received:  2000-06-09
  • Revised:  2000-11-23

Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors

Abstract: Spatio-temporal variation of subsurface porosity and permeability is controlled by various factors during sedimentation and diagcncsis.The dcpositional environments and the types of sediment basin control the original composition before hurial, texture and porosity of sediments.The sedimentary factors to control the porosity and permeability are mainly sedimentary facics, stratigraphy sequences and so on.The process of sedimentation was much shorter than the diagcncsis, and relatively easy to study.Recently, some traditional mechanism of secondary porosity formation for subsurface sediment is challenged by new theories.The formation of secondary porosity from the aluminium-silicate solution by organic acid is the most important mechanism.However it will result in the increase of pH value precipitation of carbonate and kaolinitc.The dissolulion by carbonic water to form the secondary porosity in subsurface is also limited.Ncw mechanism such as dissolution of sediment by the meteoric water by the deep cooling formation water proves effective and hydrolysis of the silicates is also accepted universally.In addition, the precipitation and material sources of some diagcnctic authigcnic minerals related to the secondary porosity also have new mode.These are several essentials to understand the formation of secondary porosity and estimate the porosity and the permeability of the reservoir. For the carbonate rocks the oil/gas reservoir related to the palco-carst nearby the unconformitv have got more attention. During the deep burial diagenesis, the temperature and prcssure control the difference of the habit of dissolution and precipitation for different carbonate minerals leading to the differcncc of porosity and permeability distribution in subsurface carbonate rocks, which is very important for prediction of carhonate reservoir.

HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
Citation: HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
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