Conference Papers Database New search

Cementing of Geothermal Wells – Radius of Thermal Influence

Izzy KUTASOV, Lev EPPELBAUM

Key words
downhole temperature, cement setting, radial heat flow
Conference
Stanford Geothermal Workshop
Year
2012
Session
Reservoir Engineering
Language
English
Paper number
Kutasov

Full text

192 KB, opens in a new tab

Abstract

Temperature and pressure are two basic influences on the downhole performance of cement slurries. They affect how long the slurry will pump and how develops the strength necessary to support the pipe. Temperature has the more pronounced influence. The downhole temperature controls the pace of chemical reactions during cement hydration resulting in cement setting and strength development. The shut-in temperature affects how long the slurry will pump and how well will develop. Assessment of the temperature development during hydration is necessary to determine how fast the cement will reach an acceptable compressive strength before the casing could be released. Cementing of casing of geothermal wells is conducted at high downhole temperatures. For this reason the cement hydration retards is often used. Thus, it is very important to predict the temperature increase during the cement setting. This will permit to determine the optimal time lapse between the cementing and temperature survey. A semi-analytical formula which allow one to estimate the temperature increase versus setting time is used to describe the transient temperature at the cylinder’s wall, while at the surface of the cylinder the radial heat flow rate (into formations) is a quadratic function of time. In order to more closely test the mechanical properties of cement under well conditions, the cement must typically be cured or hydrated for the appropriate amount of time under the temperature and pressure conditions as close as possible to downhole conditions in the well. At laboratory tests of cement slurries is important to specify the radius of thermal influence. This will allow to determining the distance from the axis of the wellbore’s model where a constant temperature should be maintained. The abovementioned formula is also used to estimate the radius of thermal influence. An example of the calculations is presented.

Copyright 2012, Stanford Geothermal Program. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

Attend the next Stanford Geothermal Workshop. Workshop details
You have opened 0 records today from 216.73.216.139 (216.73.216.139).
Viewed 30 September 2026, 11:21 pm.