1995
DOI: 10.1190/1.1443782
|View full text |Cite
|
Sign up to set email alerts
|

Attenuation of P‐ and S‐waves as a method of distinguishing gas and condensate from oil and water

Abstract: Compressional-and shear-wave attenuation data were calculated from sonic waveforms in three wells. The results show that at similar porosities and at in-situ conditions, gas and condensate sandstone reservoirs exhibit higher P-wave attenuation (lower P-wave quality factor, Qp) than either fully-water or partially "oil + water" saturated sandstones. However, S -wave attenuation and quality factor Qs do not show such a strong dependence on pore fluids. Furthermore, Qp/Qs < 1 indicates presence of gas or condensa… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

9
68
2
1

Year Published

2002
2002
2024
2024

Publication Types

Select...
5
1
1
1

Relationship

0
8

Authors

Journals

citations
Cited by 154 publications
(84 citation statements)
references
References 30 publications
(41 reference statements)
9
68
2
1
Order By: Relevance
“…In out attenuation coefficient calculations we assumed that the acquisition frequency was 5 kHz. If instead 10 kHz was selected, the attenuation coefficient values would be twice those shown in Figure 6 and closer to those reported by Klimentos (1995).…”
Section: Attenuation At Partial Saturation -Synthetic Examplessupporting
confidence: 49%
See 2 more Smart Citations
“…In out attenuation coefficient calculations we assumed that the acquisition frequency was 5 kHz. If instead 10 kHz was selected, the attenuation coefficient values would be twice those shown in Figure 6 and closer to those reported by Klimentos (1995).…”
Section: Attenuation At Partial Saturation -Synthetic Examplessupporting
confidence: 49%
“…The attenuation coefficient values shown in Figure 6b are smaller than those reported by Klimentos (1995) for a gas sandstone interval at about 30% water saturation ( α between 13 and 16 dB/m). One problem in matching the Klimentos (1995) measurements is that the exact parameters of his acquisition and rock properties have not been reported. In out attenuation coefficient calculations we assumed that the acquisition frequency was 5 kHz.…”
Section: Attenuation At Partial Saturation -Synthetic Examplescontrasting
confidence: 46%
See 1 more Smart Citation
“…Waves induced by fluid flow can lead to stratum absorption, which is the main causation of attenuation of seismic waves [10,11]. When seismic waves propagate through reservoirs, high-frequency energy waves decay more rapidly than low-frequency waves, which may lead to high-frequency energy loss and only conserve strong low-frequency energy [9,[12][13][14]. Some theoretical and practical studies have been carried out to verify this phenomenon by many scholars [9,[15][16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…Basically, this algorithm is applied to clastic rocks, where the aim is to differentiate the water-bearing zone from the hydrocarbon-bearing zone. Klimentos (1995) used three well data to gauge the P-and S-wave attenuation from sonic data using the spectral peak method. Due to P-and S-wave attenuation, a gas condensate in clean sandstone was marked with the Sw ranging from 25 to 30%.…”
Section: Introductionmentioning
confidence: 99%