中国石油大学学报(自然科学版)
中國石油大學學報(自然科學版)
중국석유대학학보(자연과학판)
JOURNAL OF CHINA UNIVERSITY OF PETROLEUM(EDITION OF NATURAL SCIENCE)
2010年
1期
24-28
,共5页
季宗镇%戴俊生%汪必峰%刘洪柯
季宗鎮%戴俊生%汪必峰%劉洪柯
계종진%대준생%왕필봉%류홍가
裂缝预测%孔隙度%渗透率%应变能%表面能%地应力
裂縫預測%孔隙度%滲透率%應變能%錶麵能%地應力
렬봉예측%공극도%삼투솔%응변능%표면능%지응력
fracture prediction%porosity%permeability%strain energy%surface energy%earth stress
以裂缝在古应力场中产生、在现今应力场被改造为研究路线,以应变能、表面能理论为基础,选用库伦-莫尔准则及格里菲斯准则分别作为岩石剪性及张性破裂判据,建立造缝期古应力场及现今应力场三向挤压应力状态及有张应力存在情况下裂缝参数计算模型,并用此模型进行实例分析计算.结果表明:现今应力场中难以产生裂缝,裂缝体积密度、线密度与古裂缝相同,现今裂缝开度及渗流性能受作用在裂缝面上的正应力及剪应力影响,相比古裂缝参数有明显变化;石港油田阜二段断层附近为储层裂缝发育密集区,裂缝开度、孔隙度及渗透率等参数高值区主要位于靠近断层的构造高部位.
以裂縫在古應力場中產生、在現今應力場被改造為研究路線,以應變能、錶麵能理論為基礎,選用庫倫-莫爾準則及格裏菲斯準則分彆作為巖石剪性及張性破裂判據,建立造縫期古應力場及現今應力場三嚮擠壓應力狀態及有張應力存在情況下裂縫參數計算模型,併用此模型進行實例分析計算.結果錶明:現今應力場中難以產生裂縫,裂縫體積密度、線密度與古裂縫相同,現今裂縫開度及滲流性能受作用在裂縫麵上的正應力及剪應力影響,相比古裂縫參數有明顯變化;石港油田阜二段斷層附近為儲層裂縫髮育密集區,裂縫開度、孔隙度及滲透率等參數高值區主要位于靠近斷層的構造高部位.
이렬봉재고응력장중산생、재현금응력장피개조위연구로선,이응변능、표면능이론위기출,선용고륜-막이준칙급격리비사준칙분별작위암석전성급장성파렬판거,건립조봉기고응력장급현금응력장삼향제압응력상태급유장응력존재정황하렬봉삼수계산모형,병용차모형진행실례분석계산.결과표명:현금응력장중난이산생렬봉,렬봉체적밀도、선밀도여고렬봉상동,현금렬봉개도급삼류성능수작용재렬봉면상적정응력급전응력영향,상비고렬봉삼수유명현변화;석항유전부이단단층부근위저층렬봉발육밀집구,렬봉개도、공극도급삼투솔등삼수고치구주요위우고근단층적구조고부위.
Tectonic fracture occurred in palaeostress field and was modified in current stress field. The calculation model of fracture parameter in fracture building stage, palaeostress field and current stress field in triaxial compression state and extension stage, was developed based on strain energy and surface energy theory. The Coulumb-Mohr principle was applied to examination of shear fracture, while Griffith principle was applied to examination of tension fracture. The results show that the rocks hardly burst in current stress field. The volume density and linear density of current fracture are same with those of palaeofracture, while the aperture and seepage of fracture change significantly. The current fracture parameters are affected by positive stress and shear stress on the fracture surface. The Fuer segment reservoir fractures in Shigang Oilfield mainly distribute near the faults. The high value area of aperture, porosity and permeability of fractures is in the structural high situs near the faults.