Optimisation of temperature observational well selection

Israel M. Kutasov, Lev V. Eppelbaum

Research output: Contribution to journalArticlepeer-review


In wellbore climatology the method of temperature inversion to determine the trends in ground surface temperature history (GSTH) assumes that the process of a well's thermal recovery is practically completed. However, for deep wells (>100-300m) the drilling process, due to the lengthy period of drilling fluid circulation, greatly alters the temperature of formation immediately surrounding the well. As a result, the determination of the formation temperature (with a specified absolute accuracy) at any depth requires a lengthy period of shut-in time. The objective of this study is to determine how long it takes before the error caused by mud circulation is small compared to the change arising from the change in surface temperature. In this paper we suggest two techniques, Slider's method and utilisation of the γ-function, which enable us to estimate the rate of temperature decline and the difference between the formation and shut-in temperatures.

Original languageEnglish
Pages (from-to)192-198
Number of pages7
JournalExploration Geophysics
Issue number3
StatePublished - 2013


  • Slider's method
  • climate
  • formation temperature
  • observational well

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geology


Dive into the research topics of 'Optimisation of temperature observational well selection'. Together they form a unique fingerprint.

Cite this