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The Brittleness Evaluation of Sand and Shale based on the Stress‐Strain Curve in Fifth Member of Xujiahe Formation, Xinchang Gas Field, Sichuan Province
Author(s) -
ZHANG Haotian,
ZHOU Wen,
ZHAO Cheng
Publication year - 2015
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12307_10
Subject(s) - oil shale , china , resource (disambiguation) , shale gas , zhàng , engineering , mining engineering , geology , library science , geography , archaeology , computer science , waste management , computer network
for horizontal well drilling, hydraulic fracturing and production prediction of gas shale. The evaluation methods for rock’s brittleness through testing are as follows: 1the characteristics of stress-strain curve, such as the ratio of reversible strain to total strain; 2the result of rock intensity testing, such as the function of compressive strength and tensile strength; 3the ratio of brittle minerals to total minerals; 4the characteristics of burial history of rock. However, Brittleness index that evaluates the rock’s brittleness is not always reliable which is concluded by Altindag (2002). In this study, the relations between the brittleness and mechanical parameters for sand and shale are analyzed basing on the stress strain test. Rock can be classified into 4 categories, namely high brittleness sand (I), low brittleness sand (II), high brittleness shale (III) and high plastic shale (IV) (Fig1B). Comparing the mechanical characteristics of these 4 categories, high brittle sand is great different from high plastic shale with greater yield strength, greater compressive strength, greater Young’s modulus, greater ratio of reversible strain to total strain and lower Poisson’s ratio and so on. But some of these mechanical properties are similar between the high brittle shale (III) and the high plastic shale (IV). By analyzing the correlations of the brittle categories and mechanical parameters, it can be assumed that the high brittle rock with high Young’s modulus, low Poisson’s ratio, high ratio of yield strength to compressive strength, high ratio of reversible strain to total strain, and the four brittleness factors are defined as follows: BYm=(Ym-Ymmin)/(Ymmax-Ymmin) 1 Bμ=(μ-μmax)/( μmin -μmax) 2 BRε=(Rε-Rεmin)/(Rεmax-Rεmin ) 3 BRσ=(Rσ-Rσmin)/(Rσmax-Rσmin ) 4 Where, Rε=εel/εtot; Rσ=σy/σc; εel-elastic strain; εtot-total strain; σy-yield strength; σc-compressive strength; YmYoung’s modulus; μ-Poisson’s ratio. So a comprehensive brittleness index could be defined with the four brittleness factors above, Bn=(αBYm+βBμ+γBRε+δBRσ)×100% 5 Correlation analysis shows that the four brittleness factors are all good relations with the brittleness of rock. Multiple regression analysis show that BYm and BRε are significant compared with Bn, while Bμ and BRσ are not. Based on analysis above, a new brittleness index is defined with Young’s modulus and the ratio of reversible strain to total strain, which shows that the higher Young’s modulus and the ratio of reversible strain to total strain are, the greater brittleness of rock is (equation 6). It is considered to be reliable and practical through the study of the relativity between mechanical characterizes, hydraulic fracturing effect with the new brittleness index. Bn=(0.477•BYm+0.622•BRε)×100% 6 ZHANG Haotian, ZHOU Wen and ZHAO Cheng, 2015. The Brittleness Evaluation of Sand and Shale based on the Stress-Strain Curve in Fifth Member of Xujiahe Formation, Xinchang Gas Field, Sichuan Province . Acta Geologica Sinica (English Edition), 89(supp.): 433.