Estimation of geothermal temperature and gradient using inversion of transient wellbore temperature measurements

被引:1
作者
Chekhonin, E. M. [1 ]
Akchurin, R. Z. [2 ]
Ramazanov, A. Sh. [2 ]
Popov, Y. A. [1 ]
Valiullin, R. A. [2 ]
机构
[1] Skolkovo Inst Sci & Technol, 30-1 Bolshoy Blvd, Moscow 121205, Russia
[2] Ufa Univ Sci & Technol, 32 Zaki Validi Str, Ufa 450076, Russia
关键词
Equilibrium formation temperature; Temperature logging; Drilling schedule; Circulation; Shut-in; Transient heat transfer; Rock thermal properties; HEAT-TRANSFER; CIRCULATION; MUD; PREDICTION; MODEL; WELLS;
D O I
10.1016/j.applthermaleng.2024.125309
中图分类号
O414.1 [热力学];
学科分类号
摘要
This paper describes the development, validation, and application of a simulator for estimating geothermal temperature and its gradient from disturbed temperature measurements along a section of a vertical or subvertical wellbore. The simulator is based on a mathematical model including transient heat transfer during drilling, circulation, cementing, and shut-in conditions in and around a wellbore. It considers the actual schedule and parameters of the well construction stages in a layered formation. Along with a critical review of existing analogue-solutions, the paper addresses the issue of completeness of the tests for such kinds of simulators, as well as the volume and the quality of the initial data required for modeling. The developed simulator was successfully tested against several known analytical and numerical solutions and applied to real field data. Parametric studies on synthetic cases allowed us to quantitatively evaluate the impact of uncertainty in drilling schedule and formation thermal properties on the reconstructed geothermal temperature and its gradient. The uncertainty in the input time-depth curve for the wellbore when the average relative difference in day-by-day drilling depth is about 11% leads to errors up to 3% and 20% in geothermal temperature and its gradient, respectively. The typical uncertainty of +/- 30% in rock thermal properties, primarily thermal conductivity, results in errors up to 2.5% and 9.3% in geothermal temperature and its gradients, respectively. It was also shown that the noise in the recorded temperature data may result in errors in geothermal temperature gradient estimation up to several percent. Developed simulator is a useful tool for the determination of geothermal temperature and its gradient, as it is important in solving fundamental and applied problems in the geothermal and petroleum industries.
引用
收藏
页数:14
相关论文
共 87 条
[61]   TEMPERATURE DISTRIBUTION IN A CIRCULATING DRILLING FLUID [J].
RAYMOND, LR .
JOURNAL OF PETROLEUM TECHNOLOGY, 1969, 21 (MAR) :333-&
[62]  
Roadifer R.D., 1987, 62 SPE ANN TECHN C E
[63]  
Romero J., 1998, 1997 SPE ANN TECHN C, DOI [10.2118/49056-MS, DOI 10.2118/49056-MS]
[64]  
Roux B., 1980, 50 ANN CAL REG M SOC
[65]  
Samarskii A.A., 1977, The Theory of Difference Schemes
[66]  
Santoyo-Gutierrez E.R., 1997, PhD thesis,
[67]  
Schoeppel R.J., 1971, FALL M SOC PETR ENG, DOI [10.2118/3364-MS, DOI 10.2118/3364-MS]
[68]  
Schon JH, 2011, HDBK PETR EXPLORAT, V8, P1
[69]  
Semenova A. P., 2006, Theoretical study of heat transfer in a borehole and a rock mass as applied to geothermal problems
[70]   Heat transfer and pressure drop of liquids in tubes [J].
Sieder, EN ;
Tate, GE .
INDUSTRIAL AND ENGINEERING CHEMISTRY, 1936, 28 :1429-1435