Temperature Transient Modeling and Analysis for Hydraulically Fractured Wells

M. Onur, Kiymet Gizem Gul
{"title":"Temperature Transient Modeling and Analysis for Hydraulically Fractured Wells","authors":"M. Onur, Kiymet Gizem Gul","doi":"10.2118/209653-ms","DOIUrl":null,"url":null,"abstract":"\n In this work, new analytical sandface temperature solutions are developed for linear flow towards an infinite-conductivity hydraulically fractured well producing under specified constant-rate or constant- bottomhole pressure (BHP) production. The solutions apply for slightly compressible, single-phase undersaturated oil reservoirs with irreducible water saturation or liquid-dominated geothermal reservoirs. They include the effects of conduction, convection, the Joule-Thomson expansion of fluids and adiabatic expansion of the total rock and fluid system, and fluid loss fracture damage. They neglect the variation of rock and fluid properties with pressure and temperature so that pressure diffusivity and thermal energy balance equations are decoupled to obtain the analytical linear-flow temperature solutions using Laplace (for constant-rate) and Boltzmann (for constant-BHP) transformations. To validate the analytical solutions, a numerical solution is developed to solve the mass and thermal energy balance equations simultaneously and account for the variation of rock and fluid properties with pressure and temperature. We proposed a correction to fluid viscosity variation as input for the analytic solutions. The numerical and analytical solutions have been compared and verified with a commercial thermal reservoir simulator. Results indicate that the fracture surface temperature is decreasing with a square of time for constant-rate production but is constant for constant BHP production. The temperature responses for both modes of production are controlled by the adiabatic expansion of the rock and fluid properties and the thermal diffusivity of the rock. The effect of thermal conductivity plays a significant role for both production modes as the matrix permeability decreases. The fracture damage has different signatures on temperature transients at early and late times for both modes of production. The approximate analytical solutions show the information content of temperature transient data acquired from an infinitely conductive hydraulically fractured well under matrix linear flow. They are simple and can be used to perform matrix linear flow analysis jointly with pressure and rate transient data to estimate the thermal and mechanical properties of the rock and fluids. The numerical solution can be used for a more general analysis procedure based on automated history matching for constant as well as variable rate and pressure production test sequences.","PeriodicalId":332644,"journal":{"name":"Day 2 Tue, June 07, 2022","volume":"43 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-06-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Day 2 Tue, June 07, 2022","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2118/209653-ms","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

In this work, new analytical sandface temperature solutions are developed for linear flow towards an infinite-conductivity hydraulically fractured well producing under specified constant-rate or constant- bottomhole pressure (BHP) production. The solutions apply for slightly compressible, single-phase undersaturated oil reservoirs with irreducible water saturation or liquid-dominated geothermal reservoirs. They include the effects of conduction, convection, the Joule-Thomson expansion of fluids and adiabatic expansion of the total rock and fluid system, and fluid loss fracture damage. They neglect the variation of rock and fluid properties with pressure and temperature so that pressure diffusivity and thermal energy balance equations are decoupled to obtain the analytical linear-flow temperature solutions using Laplace (for constant-rate) and Boltzmann (for constant-BHP) transformations. To validate the analytical solutions, a numerical solution is developed to solve the mass and thermal energy balance equations simultaneously and account for the variation of rock and fluid properties with pressure and temperature. We proposed a correction to fluid viscosity variation as input for the analytic solutions. The numerical and analytical solutions have been compared and verified with a commercial thermal reservoir simulator. Results indicate that the fracture surface temperature is decreasing with a square of time for constant-rate production but is constant for constant BHP production. The temperature responses for both modes of production are controlled by the adiabatic expansion of the rock and fluid properties and the thermal diffusivity of the rock. The effect of thermal conductivity plays a significant role for both production modes as the matrix permeability decreases. The fracture damage has different signatures on temperature transients at early and late times for both modes of production. The approximate analytical solutions show the information content of temperature transient data acquired from an infinitely conductive hydraulically fractured well under matrix linear flow. They are simple and can be used to perform matrix linear flow analysis jointly with pressure and rate transient data to estimate the thermal and mechanical properties of the rock and fluids. The numerical solution can be used for a more general analysis procedure based on automated history matching for constant as well as variable rate and pressure production test sequences.
水力压裂井温度瞬态建模与分析
在这项工作中,开发了新的解析式地表温度解,用于在规定的恒速率或恒井底压力(BHP)下生产无限导流水力压裂井的线性流动。该解决方案适用于轻度可压缩、含水饱和度不可还原的单相欠饱和油藏或以液体为主的地热油藏。它们包括传导效应、对流效应、流体的焦耳-汤姆逊膨胀效应和整个岩石和流体系统的绝热膨胀效应,以及流体损失破裂损伤效应。他们忽略了岩石和流体性质随压力和温度的变化,因此压力扩散率和热能平衡方程解耦,使用拉普拉斯(恒速率)和玻尔兹曼(恒bhp)变换获得线性流动温度的解析解。为了验证解析解,建立了同时求解质量和热能平衡方程的数值解,并考虑了岩石和流体性质随压力和温度的变化。我们提出了对流体粘度变化的修正作为解析解的输入。数值解和解析解在商业热油藏模拟器上进行了比较和验证。结果表明,在恒速生产条件下,裂缝表面温度随时间的平方而降低,而在恒压生产条件下,裂缝表面温度不变。两种生产方式的温度响应都受岩石的绝热膨胀和流体性质以及岩石的热扩散率控制。随着基质渗透率的降低,导热系数对两种生产方式的影响都很显著。对于两种生产方式,裂缝损伤在早期和后期的温度瞬态特征不同。近似解析解显示了矩阵线性渗流下无限导流水力压裂井温度瞬态数据的信息量。它们简单,可用于结合压力和速率瞬态数据进行矩阵线性流动分析,以估计岩石和流体的热力学性质。数值解可用于基于自动历史匹配的更一般的分析程序,用于恒定和可变速率和压力生产测试序列。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信