ImageVerifierCode 换一换
格式:PDF , 页数:7 ,大小:187.28KB ,
资源ID:176057      下载积分:12 积分
快捷下载
登录下载
邮箱/手机:
温馨提示:
快捷下载时,用户名和密码都是您填写的邮箱或者手机号,方便查询和重复下载(系统自动生成)。 如填写123,账号就是123,密码也是123。
特别说明:
请自助下载,系统不会自动发送文件的哦; 如果您已付费,想二次下载,请登录后访问:我的下载记录
支付方式: 支付宝扫码支付 微信扫码支付   
验证码:   换一换

加入VIP,免费下载
 

温馨提示:由于个人手机设置不同,如果发现不能下载,请复制以下地址【https://www.wnwk.com/docdown/176057.html】到电脑端继续下载(重复下载不扣费)。

已注册用户请登录:
账号:
密码:
验证码:   换一换
  忘记密码?
三方登录: QQ登录  

下载须知

1: 本站所有资源如无特殊说明,都需要本地电脑安装OFFICE2007和PDF阅读器。
2: 试题试卷类文档,如果标题没有明确说明有答案则都视为没有答案,请知晓。
3: 文件的所有权益归上传用户所有。
4. 未经权益所有人同意不得将文件中的内容挪作商业或盈利用途。
5. 本站仅提供交流平台,并不能对任何下载内容负责。
6. 下载文件中如有侵权或不适当内容,请与我们联系,我们立即纠正。
7. 本站不保证下载资源的准确性、安全性和完整性, 同时也不承担用户因使用这些下载资源对自己和他人造成任何形式的伤害或损失。

版权提示 | 免责声明

本文(ASTM_D_4645_-_08.pdf)为本站会员(益****师)主动上传,蜗牛文库仅提供信息存储空间,仅对用户上传内容的表现方式做保护处理,对上载内容本身不做任何修改或编辑。 若此文所含内容侵犯了您的版权或隐私,请立即通知蜗牛文库(发送邮件至admin@wnwk.com或直接QQ联系客服),我们立即给予删除!

ASTM_D_4645_-_08.pdf

1、Designation:D464508Standard Test Method forDetermination of In-Situ Stress in Rock Using HydraulicFracturing Method1This standard is issued under the fixed designation D4645;the number immediately following the designation indicates the year oforiginal adoption or,in the case of revision,the year of

2、 last revision.A number in parentheses indicates the year of last reapproval.Asuperscript epsilon()indicates an editorial change since the last revision or reapproval.1.Scope*1.1 This test method covers the determination of the in-situstate of stress in rock by hydraulic fracturing.NOTE1Hydraulic fr

3、acturing for stress determination is also referredto as hydrofracturing,and sometimes as minifracing.Hydraulic fracturingand hydrofracturing may also refer to fracturing of the rock by fluidpressure for the purpose of altering rock properties,such as permeabilityand porosity.1.2 Hydraulic fracturing

4、 is the widely accepted field methodavailable for in situ stress measurements at depths greater than50 m.It can be used in drill holes of any diameter.1.3 Hydraulic fracturing can also be used in short holes forwhich other stress measuring methods,such as overcoring,arealso available.The advantage o

5、f hydraulic fracturing is that ityields stresses averaged over a few square metres(the size ofthe induced hydraulic fracture)rather than over grain sizeareas,as in the case of overcoring techniques.1.4 All observed and calculated values shall conform to theguidelines for significant digits and round

6、ing established inPractice D6026.1.4.1 The method used to specifiy how data are collected,calculated,or recorded in this standard is not directly related tothe accuracy to which the data can be applied in design or otheruses,or both.How one applies the results obtained using thisstandard is beyond i

7、ts scope.1.5 The values stated in SI units are to be regarded asstandard.No other units of measurement are included in thisstandard.1.6 This standard does not purport to address all of thesafety problems,if any,associated with its use.It is theresponsibility of the user of this standard to establish

8、 appro-priate safety and health practices and determine the applica-bility of regulatory limitations prior to use.2.Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to Soil,Rock,and ContainedFluidsD2113 Practice for Rock Core Drilling and Sampling ofRock for Site ExplorationD3740 Pr

9、actice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD5079 Practices for Preserving and Transporting Rock CoreSamplesD6026 Practice for Using Significant Digits in GeotechnicalData3.Terminology3.1 For terminolo

10、gy used in this test method,refer toTerminology D653.3.2 Definitions of Terms Specific to This Standard:3.2.1 breakdown pressurethe pressure required to inducea hydraulic fracture in a previously intact test interval.3.2.2 in-situ stressrock stress measured in situ(as op-posed to by remote sensing).

11、3.2.3 secondary breakdown(or fracture reopening,or re-frac)pressure the pressure required to reopen a closed,previously induced hydrofracture after the test interval pressurehas been allowed to return to its initial condition.3.2.4 shut-in pressure(or ISIP(instantaneous shut-inpressure)the pressure

12、reached when the induced hydrofrac-ture closes back after pumping is stopped.3.2.5 vertical and horizontal principal stresses the threeprincipal stresses in situ are generally assumed to act one in thevertical direction and the other two in the horizontal plane.4.Summary of Test Method4.1 Asection o

13、f the borehole is isolated by pressurizing twoinflatable rubber packers.The fluid pressure in the sealed-off1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.12 on Rock Mechanics.Current edition approved July 1,2008.

14、Published July 2008.Originally approvedin 1987.Last previous edition approved in 2004 as D4645 041.DOI:10.1520/D4645-08.2For referenced ASTM standards,visit the ASTM website,www.astm.org,orcontact ASTM Customer Service at serviceastm.org.For Annual Book of ASTMStandards volume information,refer to t

15、he standards Document Summary page onthe ASTM website.*A Summary of Changes section appears at the end of this standardCopyright ASTM International,100 Barr Harbor Drive,PO Box C700,West Conshohocken,PA 19428-2959.United States1 interval between the two packers is raised by pumping fluidinto it at a

16、 controlled rate until a fracture occurs in the boreholewall.Pumping is stopped and the pressure in the interval isallowed to stabilize.The pressure is then reduced to the porepressure level of the rock formation,and the pressurizationprocess is repeated several times maintaining the same flowrate.Additional pressure cycles can be conducted at differentflow rates.The magnitudes of the principal stresses arecalculated from the various pressure readings.The orientationof the fracture is detected i

copyright@ 2008-2023 wnwk.com网站版权所有

经营许可证编号:浙ICP备2024059924号-2