{"title":"纳帕里马山地层泥岩在高压下的 P 波和 S 波速度及衰减情况","authors":"K.T. Ramjarrie , O.O. Blake , U.C. Iyare","doi":"10.1016/j.jappgeo.2024.105450","DOIUrl":null,"url":null,"abstract":"<div><p>Velocity and attenuation (the inverse of the Q factor, Q<sup>−1</sup>) are fundamental elastic wave attributes used to understand subsurface physical properties and characterize unconventional reservoirs. Mudstone, an abundant sedimentary rock, is commonly regarded as a source rock with great promise for unconventional exploration. Despite this, velocity and attenuation studies are lacking on mudstones and have failed to address the link between these elastic wave attributes and physical rock properties. In this study, we measured the P- and S-wave velocities (Vp and Vs) and Q factors (Qp and Qs) of the Naparima Hill organic-rich mudstone at effective pressures up to 130 MPa. The main aims are to investigate the effects of mineralogy, bulk density, porosity, and saturation on these elastic wave attributes and to evaluate if a relationship exists between velocity and attenuation. Vp and Vs were obtained using the trough transmission method, while the spectral-ratio and rise-time techniques were used to determine Qp and Qs in the frequency range of 0.8 to 1.7 MHz. The results show that the velocities and Q factors rose with increasing carbonate, bulk density, and effective pressure, and decreasing clay, silica, and porosity. The saturated mudstones have lower velocities and Q factors than the dry specimens. Strong, linear relationships (R<sup>2</sup> > 0.85) were established between Vp and Vs under both dry and saturated conditions. Moderate to strong linear relationships (R<sup>2</sup> > 0.5) were established between Qs and Qp, Qp and Vp, Qs and Vs, and Qs and Vp under saturated conditions. These relationships create a framework for predicting the elastic wave attributes (Vs, Qp, and Qs), from the readily extractable Vp in mudstones.</p></div>","PeriodicalId":54882,"journal":{"name":"Journal of Applied Geophysics","volume":"228 ","pages":"Article 105450"},"PeriodicalIF":2.2000,"publicationDate":"2024-07-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"P- and S-wave velocities and attenuations of Naparima Hill Formation mudstones at elevated pressures\",\"authors\":\"K.T. Ramjarrie , O.O. Blake , U.C. Iyare\",\"doi\":\"10.1016/j.jappgeo.2024.105450\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Velocity and attenuation (the inverse of the Q factor, Q<sup>−1</sup>) are fundamental elastic wave attributes used to understand subsurface physical properties and characterize unconventional reservoirs. Mudstone, an abundant sedimentary rock, is commonly regarded as a source rock with great promise for unconventional exploration. Despite this, velocity and attenuation studies are lacking on mudstones and have failed to address the link between these elastic wave attributes and physical rock properties. In this study, we measured the P- and S-wave velocities (Vp and Vs) and Q factors (Qp and Qs) of the Naparima Hill organic-rich mudstone at effective pressures up to 130 MPa. The main aims are to investigate the effects of mineralogy, bulk density, porosity, and saturation on these elastic wave attributes and to evaluate if a relationship exists between velocity and attenuation. Vp and Vs were obtained using the trough transmission method, while the spectral-ratio and rise-time techniques were used to determine Qp and Qs in the frequency range of 0.8 to 1.7 MHz. The results show that the velocities and Q factors rose with increasing carbonate, bulk density, and effective pressure, and decreasing clay, silica, and porosity. The saturated mudstones have lower velocities and Q factors than the dry specimens. Strong, linear relationships (R<sup>2</sup> > 0.85) were established between Vp and Vs under both dry and saturated conditions. Moderate to strong linear relationships (R<sup>2</sup> > 0.5) were established between Qs and Qp, Qp and Vp, Qs and Vs, and Qs and Vp under saturated conditions. These relationships create a framework for predicting the elastic wave attributes (Vs, Qp, and Qs), from the readily extractable Vp in mudstones.</p></div>\",\"PeriodicalId\":54882,\"journal\":{\"name\":\"Journal of Applied Geophysics\",\"volume\":\"228 \",\"pages\":\"Article 105450\"},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2024-07-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Applied Geophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0926985124001666\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Applied Geophysics","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0926985124001666","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
P- and S-wave velocities and attenuations of Naparima Hill Formation mudstones at elevated pressures
Velocity and attenuation (the inverse of the Q factor, Q−1) are fundamental elastic wave attributes used to understand subsurface physical properties and characterize unconventional reservoirs. Mudstone, an abundant sedimentary rock, is commonly regarded as a source rock with great promise for unconventional exploration. Despite this, velocity and attenuation studies are lacking on mudstones and have failed to address the link between these elastic wave attributes and physical rock properties. In this study, we measured the P- and S-wave velocities (Vp and Vs) and Q factors (Qp and Qs) of the Naparima Hill organic-rich mudstone at effective pressures up to 130 MPa. The main aims are to investigate the effects of mineralogy, bulk density, porosity, and saturation on these elastic wave attributes and to evaluate if a relationship exists between velocity and attenuation. Vp and Vs were obtained using the trough transmission method, while the spectral-ratio and rise-time techniques were used to determine Qp and Qs in the frequency range of 0.8 to 1.7 MHz. The results show that the velocities and Q factors rose with increasing carbonate, bulk density, and effective pressure, and decreasing clay, silica, and porosity. The saturated mudstones have lower velocities and Q factors than the dry specimens. Strong, linear relationships (R2 > 0.85) were established between Vp and Vs under both dry and saturated conditions. Moderate to strong linear relationships (R2 > 0.5) were established between Qs and Qp, Qp and Vp, Qs and Vs, and Qs and Vp under saturated conditions. These relationships create a framework for predicting the elastic wave attributes (Vs, Qp, and Qs), from the readily extractable Vp in mudstones.
期刊介绍:
The Journal of Applied Geophysics with its key objective of responding to pertinent and timely needs, places particular emphasis on methodological developments and innovative applications of geophysical techniques for addressing environmental, engineering, and hydrological problems. Related topical research in exploration geophysics and in soil and rock physics is also covered by the Journal of Applied Geophysics.