地层水矿化度对补偿中子测井影响的自动校正方法研究
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李鹏举, 李勇勇, 徐茂河, 付勇路, 田甜
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A study of automatic correction method for the influence of formation water salinity on compensating neutron logging
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Peng-Ju LI, Yong-Yong LI, Mao-He XU, Yong-Lu FU, Tian TIAN
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表1 不同矿化度、孔隙度地层的近远探测器计数率比值
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Table 1 Near-to-far detector counting ratio for different salinity and porosity formations
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K 103 mg/L | R ?=5% | R ?=10% | R ?=15% | R ?=20% | R ?=25% | R ?=30% | R ?=35% | R ?=40% | 2 | 5.5358 | 7.3936 | 9.2141 | 11.6282 | 14.1128 | 17.0609 | 18.9479 | 21.6945 | 4 | 5.5444 | 7.4277 | 9.2462 | 11.6992 | 14.2696 | 17.1051 | 19.0131 | 21.9471 | 6 | 5.5572 | 7.4825 | 9.3373 | 11.7815 | 14.3485 | 17.2619 | 19.0914 | 22.1562 | 8 | 5.5731 | 7.5638 | 9.3841 | 11.9180 | 14.3956 | 17.4312 | 19.2609 | 22.3781 | 10 | 5.5901 | 7.5894 | 9.4568 | 12.0523 | 14.5766 | 17.6433 | 19.4910 | 22.3431 | 20 | 5.6567 | 7.7037 | 9.7060 | 12.5078 | 14.9819 | 18.0859 | 20.3406 | 22.7827 | 40 | 5.8027 | 8.0302 | 10.1818 | 13.3278 | 15.9587 | 19.0758 | 21.2311 | 23.7184 | 60 | 5.8788 | 8.2548 | 10.6310 | 14.0790 | 16.5734 | 19.9398 | 22.2737 | 24.8705 | 80 | 5.9763 | 8.5090 | 10.9372 | 14.5618 | 17.0692 | 20.9989 | 23.0968 | 25.8535 | 100 | 6.0386 | 8.7159 | 11.3617 | 14.8231 | 17.7682 | 21.5449 | 23.8259 | 26.0628 | 120 | 6.2177 | 8.9431 | 11.8504 | 15.3939 | 18.1720 | 21.3842 | 24.1710 | 26.2046 | 140 | 6.3345 | 9.1501 | 12.1744 | 15.8193 | 18.4743 | 22.1051 | 23.8934 | 26.5727 | 160 | 6.4960 | 9.3850 | 12.5665 | 16.2511 | 18.8303 | 22.3568 | 24.3982 | 26.9084 | 180 | 6.6368 | 9.5602 | 12.7814 | 16.7247 | 19.1785 | 21.9225 | 24.2472 | 26.7856 | 200 | 6.7386 | 9.8133 | 12.9987 | 16.7941 | 19.3919 | 22.4329 | 24.9869 | 27.5232 |
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