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《Petroleum Exploration and Development》 2002-04
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An approach to the generating mechanism of secondary pores and pore evolution model of He 8 gas layer in Suligemiao gas field

LIU Rui e 1,2 , SUN Fen jin 2, BAI Wen hua 2,3 , MA Cheng hua 2, HUANG Yue ming 2 (1.Northwest University, Shaanxi 710069, P. R. China; 2.The langfang Branch of RIPED, PetroChina, Hebei 065007, P. R. China; 3.China University of Geoscie  
Suligemiao gas field is another significant discovery followed the discovery of Yulin gas field in Ordos basin, however porosity genesis type between He 8 gas layer in Suligemiao gas field and that of Shan 2 layer in Yulin gas field has greater diversity. Through digenetic research, the sandstones of He 8 interval are of B period of the late diagenesis. According to systematic petro mineral appraisal, environmental scan electron microscope analysis, and energy spectrum, it is found that tuffaceous, unstable debris and unstable fillings are very excessive. Different types of secondary porosity are extensive. In order to study the origin of the secondary pores, acidolysis simulating experiment, under simulating stratigraphic conditions, has been developed. By the means of environmental scan electron microscope analysis and energy spectrum analysis, the sample's variety before and after acidolysis corrasion has been contrasted. By the means of plasma emission spectrum analysis, the water sample's components after the acidolysis corrasion also have been tested. The results indicate that the tuffaceous sandstone's corrasion is very obvious, and the corrasion become serious as the acidity of acetic acid increased. The tuffaceous sandstone's corrosion capacity is 7.0 11.0 times that of the quartz sandstones. The felspathic corrosion lagged that of alter tuffaceous matrix. Through analy sis and research the author indicates that the main origin of the secondary pore is the corrosion of tuffaceous sandstone, and puts forward the new pore evolvement model of the tuffaceous sandstone.
【CateGory Index】: P618.13
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