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COMPENSATED NEUTRON LOG RESPONSE ISSUES – A TUTORIAL

机译:补偿中子对数响应问题-补习

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Compensated neutron logs have been around for manyyears, and have been used successfully for manypetrophysical applications. Although the basic designand general response characteristics of theseinstruments have remained relatively constant over theyears, service companies have refined the responsecharacterizations and have updated their hardware,providing evolutionary improvements. Unfortunately,the general understanding among petrophysicists ofhow compensated neutron instruments work and howbest to make use of the log data appears to have laggedor perhaps even worsened in recent years. This paperdiscusses several obstacles to understanding andinterpreting neutron logs and proposes some techniquesfor avoiding problems.One obstacle is a tendency to oversimplify the physicsof the measurement. Hydrogen plays a very importantrole in slowing fast neutrons to the epithermal orthermal levels at which compensated neutroninstruments detect them, and a hydrogen index (HI) hashistorically been used as an aid in discussing neutrontool responses and in interpreting neutron log data. Inmany cases, hydrogen plays a dominant role in neutronlogging, but it is not the only element that interacts withneutrons. Thinking of neutron log responses strictly interms of HI can lead to a misunderstanding of theresponse and to errors in log interpretation. A betterway to deal with neutron log responses is in terms ofthe neutron slowing, diffusion, and absorptionproperties of the formation.Another obstacle is a tendency to think of allcompensated neutron measurements as being the same.Although most compensated neutron instruments aresimilar in design, their response characteristics are notthe same. The differences show up most readily in themineralogy and environmental corrections for differentinstruments. A careful comparison of the correctioncharts for different tools shows this. Attempting tocorrect a neutron log using the charts or the underlyingalgorithms intended for a different tool can be a seriousmistake.Another issue is that different curve names may meandifferent things. It is very important to understand whatthe mnemonics mean and which curve to use for aspecific application.The issues of statistical precision, resolution, and datasampling rate are strongly interrelated for compensatedneutron tools. These issues are not difficult toovercome, but it is necessary to be aware of them andtake each into consideration when using the data.One final obstacle is a lack of understanding of theresponse differences in wireline and LWD instruments.Differences in detailed design parameters can result inresponse differences, but there are also basicdifferences in the way wireline and LWD data arerecorded and processed. These, too, can cause responsedifferences, some of which can be quite significant.Some of these basic differences will be consideredalong with the discussion of other issues.Although this paper is not an exhaustive treatment ofcompensated neutron logging issues, some of the moreimportant ones are discussed. Alternative ways oflooking at the data are presented, as are some ideas forfurther work.
机译:补偿中子测井仪已经出现了很多 年,并已成功用于许多领域 岩石物理应用。虽然基本设计 和这些的一般反应特征 在过去的十年中,工具一直保持相对稳定 多年以来,服务公司不断完善应对措施 特性并更新了其硬件, 提供进化上的改进。很遗憾, 岩石物理学家的普遍理解 补偿中子仪器如何工作以及如何工作 最好利用日志数据似乎已滞后 甚至在最近几年恶化。这篇报告 讨论了理解和理解的几个障碍 解释中子测井并提出一些技术 为了避免出现问题。 一个障碍是过度简化物理学的趋势 测量的氢起着非常重要的作用 在使快中子减速到超热或 补偿中子的热能级 仪器检测到它们,并且氢指数(HI)达到 历史上曾被用作讨论中子的辅助手段 工具响应和解释中子测井数据。在 在许多情况下,氢在中子中起主导作用 日志记录,但这不是与之交互的唯一元素 中子。对中子测井响应的严格思考 HI条款可能会导致对 响应以及日志解释中的错误。一个更好的 处理中子测井响应的方法是 中子减速,扩散和吸收 地层的性质。 另一个障碍是倾向于思考所有问题 补偿的中子测量值是相同的。 尽管大多数补偿中子仪器是 在设计上相似,它们的响应特性不一样 相同。差异最容易显示在 不同矿物学和环境校正 仪器。仔细比较校正 不同工具的图表显示了这一点。试图 使用图表或底层校正中子测井 用于其他工具的算法可能很严重 错误。 另一个问题是,不同的曲线名称可能意味着 不同的东西。了解什么是非常重要的 助记符的平均值,以及用于哪条曲线 具体的应用。 统计精度,分辨率和数据问题 采样率与补偿有很强的相关性 中子工具。这些问题并不难 克服,但有必要意识到它们, 使用数据时要考虑到每个因素。 最后一个障碍是缺乏对 有线和随钻测井仪器的响应差异。 详细设计参数的差异可能导致 回应差异,但也有基本的 有线和随钻测井数据的方式差异 记录和处理。这些也会引起回应 差异,其中一些可能非常重要。 其中一些基本差异将被考虑 以及其他问题的讨论。 尽管本文并未详尽地论述 补偿中子测井问题,还有更多 重要的讨论。替代方式 介绍了查看数据以及一些想法 进一步的工作。

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