ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Language
Years
  • 1
    facet.materialart.
    Unknown
    In:  Protokoll über das 28. Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung : Haltern am See, 23.-27. September 2019
    Publication Date: 2020-04-05
    Description: Electromagnetic (EM) method, especially Controlled Source Electromagnetic (CSEM) are a unique way of observing fluid movement at depth from the surface. The depth range of interest for hydrocarbon and geothermal applications is from about 500m to 5-7 km. For hydrocarbon reservoirs monitoring we focus to improve the recovery factors and understand fluid movement resulting in lower carbon footprint per produced barrel of oil. For geothermal applications, we can observe magma movements as aid for volcano eruption prediction or monitor producing geothermal field to improve production efficiency and to observe (in correlation with microseismic) reservoir damage and potential induced seismicity. To see percentage level variations, more detailed attention is required at all data handling stages. During acquisition, more effort is required to obtain long term stable transmitter and receiver sites including not only daily monitoring of contact resistance but also controlling them during the acquisition process to better than 1% variations. Because of the large dynamic range of the signal, a highly accurate reference level with active adjustment before the transmitted signal is necessary. While processing the data, a feedback loop between filter selection and noise suppression in the reservoir signal band allows you to optimize the filter and to reduce their effect on the anomaly itself. For a sedimentary environment, anisotropy is the biggest cause for error and misinterpretation. It is derived before the survey from existing logs using end members derived from the resistivity log based on the interaction of the layers on reservoir scale. Another serious issue is the image focus. In principle, we assume the information comes from underneath the receiver but for different measurements it comes from various volume between transmitter and receiver. As with focusing of laterologs, we use a focusing method either by differential measurements or additional borehole receivers. We are using real field measurements as example for potential misinterpretation to illustrate the severance of these issues.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...