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首页> 外文期刊>Journal of Seismic Exploration >ESTIMATION OF WATER/GAS SATURATION AND EFFECTIVE PRESSURE FROM SEISMIC VELOCITIES AND QUALITY FACTORS AS FUNCTIONS OF FREQUENCY: PREDICTIONS OF AN EMPIRICAL MODEL
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ESTIMATION OF WATER/GAS SATURATION AND EFFECTIVE PRESSURE FROM SEISMIC VELOCITIES AND QUALITY FACTORS AS FUNCTIONS OF FREQUENCY: PREDICTIONS OF AN EMPIRICAL MODEL

机译:从地震速度和质量因子作为频率函数估算水/天然气饱和度和有效压力:经验模型的预测

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摘要

The two main reservoir parameters that change during hydrocarbon production are water saturation (S_w) and effective pressure (P_c), The predictions of an empirical model to estimate S_w and P_e. from seismic quality factors and velocities in partially saturated water-gas systems are investigated. The predictions include the following. Compressional velocity (V_p) is insensitive to frequency below~100 Hz. Shear velocity (V_S) is insensitive to frequency but sensitive to S_w suggesting that high frequency lab V_S measurements can be used for modeling at seismic frequencies. The P-wave quality factor (Q_P) shows diagnostic behavior as a function of S_w for frequencies greater than 500 Hz and S_w > 50%. At low frequencies (< 1 KHz) and S_w < 85%, Q_S~(-1) decreases with S_w; at frequencies > 1 KHz, Q_S~(-1) increases with S_w. The Q_S/Q_P ratio is predicted to be independent of frequency for water saturation greater than 90%. The dependence of predicted V_P and V_S on P_e is non-linear at all frequencies (30 Hz - 5 KHz). Q_S~(-1) is maximum at full saturation whereas Q_P~(-1) is maximum at partial saturation (~80%). V_P, V_S, Q_P and Q_S are relatively insensitive to P_e at P_e > 10 Mpa. Q_S/Q_P is independent of P_e but shows nearly linear dependence on S_W at S_W < 70%. The predicted Q_S/Q_P values are shifted downward and the V_P/V_S vs. S_w curves are flatter for tight sandstones, compared to porous sandstones. V_P/V_S and Q_S/Q_P ratios together are potentially diagnostic of P_e and S_w at frequencies from 30 Hz to 5 KHz. The results of this paper are empirical predictions that are testable.
机译:在油气生产过程中变化的两个主要储层参数是水饱和度(S_w)和有效压力(P_c)。估算S_w和P_e的经验模型的预测。从地震质量因子和部分饱和水煤气系统中的速度进行了研究。这些预测包括以下内容。压缩速度(V_p)对低于100 Hz的频率不敏感。剪切速度(V_S)对频率不敏感,但对S_w敏感,这表明可以将高频实验室V_S测量值用于地震频率建模。对于大于500 Hz的频率和S_w> 50%,P波品质因数(Q_P)将诊断行为作为S_w的函数。在低频(<1 KHz)和S_w <85%时,Q_S〜(-1)随着S_w减小;在频率> 1 KHz时,Q_S〜(-1)随着S_w增加。对于大于90%的水饱和度,预计Q_S / Q_P比与频率无关。在所有频率(30 Hz-5 KHz)下,预测的V_P和V_S对P_e的依赖性都是非线性的。 Q_S〜(-1)在完全饱和时最大,而Q_P〜(-1)在部分饱和时(〜80%)最大。在P_e> 10 Mpa时,V_P,V_S,Q_P和Q_S对P_e相对不敏感。 Q_S / Q_P独立于P_e,但在S_W <70%时显示出几乎与S_W线性相关。与多孔砂岩相比,致密砂岩的预测Q_S / Q_P值向下移动,V_P / V_S与S_w的曲线更平坦。 V_P / V_S和Q_S / Q_P比率一起可能在30 Hz至5 KHz的频率下诊断P_e和S_w。本文的结果是可检验的经验预测。

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