2012
年第
36
卷
第
3
期
文章编号:
1673-5005
(2012)
03-0014
-0
6
中国石油大学学报(自然科学版)
Journal of China University of Petroleum
Vo
1.
36
No.3
Jun.2012
砂泥岩间互地层破裂准则选取及在裂缝穿透性
评价中的应用
卢虎胜张俊峰
2
李世银
3
邹
军
4
刘爱武
5
(1中国石油大学地球科学与技术学院,山东青岛
266580;
2.
中石油青海油田边远油田开发公司,青海海西
ì'l'j
816400;
3.
中国石油塔里木油田分公司勘探开发研究院,新疆库尔勒
841000;
4
中国石油川庆钻探工程有限公司
对外合作和市场开发处,四川成都
610051;
5.
中石化江汉油田分公司勘探开发研究院,湖北武汉
430223
)
摘要:针对目前存在的多种岩石破裂准则,以某油气回裂缝性砂泥岩储层为例,在岩心裂缝观察和岩石力学试验的基
础上,通过数理统计和公式推导的方法,建立适用于地下低渗透砂岩和泥岩间互地层的破裂判断准则,并基于构造应力
场与裂缝参数之间的定量关系模型,实现砂泥互层时裂缝穿透程度定量评价。结果表明:在压缩状态下,砂泥岩间五地
层破裂判据适用两段式莫尔-库仑准则,但在拉张应力状态下,莫尔-库仑准则不适用,改用格里菲斯准则;砂、泥岩力
学参数存在差异,同样受力变形条件下,裂缝先在砂岩中产生,再向泥岩中垂向延伸扩展,并发生一定产状的变化;泥岩
厚度为
5m
是裂缝能否穿透的
11
伍界值,多数裂缝会终止于砂泥岩界面处;相同的受力条件下砂岩越薄越容易产生裂缝,
泥岩厚度达到
20
m
时砂岩厚度的变化对砂岩裂缝延伸进泥岩中的发育程度和裂缝密度影响很小。
关键词:砂泥岩间互层;构造应力;裂缝密度;破裂准则
中图分类号
:TE
122.2
文献标志码
:A
doi: 10.
3969/j.
issn.
1673-5005.2012.03.003
Best selection among
crack
criterions to sandstone-mudstone formation
and
its application to
fracture
penetration ability evaluation
LU
Hu-sheng
I
,
ZHANG
Jun-feng
2
,
LI
Shi-yin
3
,
ZOU
Jun
4
,
LIU
Ai-wu
5
(
1.
School
of
Ge
osciences in
Chin
α
University
of
Petroleum , Qingdao 266580 , China;
2.
Outling Oiifìeld Developing Company
of
Qinghai
Oi
1j
ìeld ,
PetroChin
日
,
H
,
α
ixizhou
816400 , China;
3. Communication
Comp
α ny
of
Tarim Basin Oiifìeld
of
Xinjiang ,
Korl
α841000
,
China;
4. External
Cooperation
α nd
Marketing Department
of
Chuanqing Drilling Engineering
Comp
α
ny
Limited ,
PetroChin
日
,
Chengdu 610051 , China;
5.
Exploration and Development Research Institute
of
liangh
α n
Oiifìeld Company , SINOPEC , Wuhan 430223 , China)
Abstract:
Based on the present rock crack criterions , cores observation and rock mechanic tests , a new effective rock failure
criterion for interbedded sand and mud stone formation in a certain fractured oil and gas field was developed through the
method of mathematical deduction. The penetration degree of fractures in mudstone was evaluated based on the quantitative
model between tectonic stress and fracture parameters. The results show that for the compressed conditions
, multibowl Kou
lomb-Mohr criterion will be selected
to
study the formation , but for the tensile conditions , Griffith criterion should be select-
ed. With obvious difference in mechanical properties of sandstone
and
mudstone , fractures will form in
sandston
巳
firstly
,
then
extend into mudstone in vertical direction with variable occurrence. The critical thickness of mudstone is 5 m whether fracture
could penetrate the mudstone
, and most of fractures will end at the lithologic interface. For the same conditions , the thinner
sandstone is easy
to
generate fractures. When the sandstone thickness reaches
20
m, the thickness variation of sandstone has
little influence on fracture's development and penetration degree among mudstone.
Key
words:
interbedded sand and mud stone formation; tectonic
stress;
fracture density; crack criterions
收稿日期,
2011-10-26
基金项目.国家科技重大专项课题
(2008ZX05001
)
作者简介·卢虎胜
(1970
一)
,男(汉族)
,甘肃甘谷人,博七研究生,主要从事储层地质及开发地质研究
c