Combining rate-controlled porosimetry and NMR to probe full-range pore throat structures and their evolution features in tight sands: A case study in the Songliao Basin, China. (May 2017)

• Record Type: Journal Article
• Authors: Xiao, Dianshi; Jiang, Shu; Thul, David; Huang, Wenbiao; Lu, Zhengyuan; Lu, Shuangfang
• Is Part Of: Marine and petroleum geology. Volume 83(2017)
• Page Start: 111
• Page End: 123
• Publication Date: 2017-05
• Subjects: Pore throat structure -- Pore throat evolution -- Fluid mobility -- Porosimetry -- NMR -- Tight sands; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2017.03.003
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: To better understand reservoir quality and to produce accurate petrophysical interpretations, it is necessary to understand complex and heterogeneous pore throat structures in tight sands and to develop a technique to reveal the full range of pore and throat distributions. In this study, in order to characterize the features and evolutions of pore throat structures, nine samples from the Lower Cretaceous tight gas sandstone in the Songliao Basin of China are measured by nuclear magnetic resonance (NMR), rate-controlled porosimetry (RCP) and scanning electron microscopy (SEM). Throats with bifractal structures are found in these tight sands and can be divided into a backbone formation (BF) region and a percolation region using RCP data. Because (i) throats in the percolation region record treelike pore structures and are predominant in small pore spaces and (ii) a good correlation exists between NMR-derived T2 relaxation times and the RCP-derived radius of throats, the throat distribution obtained via RCP can be used to calibrate the NMR PSD and then to partition the PSD into distributions of pore bodies and throats. These data indicate that (i) throats are more common than pore bodies in pore spaces of tight sands with lower permeability, (ii) pore bodies are connected to throats from both the BF and percolation regions, in which the fluid mobility in pore bodies is mainly controlled by the pore to throat ratio (PTR), which is related to the intersection throat of these two regions, and (iii) compaction, dissolution, clay cementation and sediment properties (e.g., rock compositions) have different impacts on the evolutions of pore bodies and throats, in which larger PTR values in tight sands are mainly produced by compaction and pore-bridging clay cementation, and lower contents of pore bodies are commonly related to abundant plastic compositions and pore-bridging clay cementation. Highlights: Throats in tight sands are divided into two regions related to different pore structure. Combining of NMR and RCP reveals the full-range distribution of pore and throat. The fluid mobility of pore bodies is mainly affected by pore to throat ratio. The impacts of dominant diagenesis on pore-throat structure evolution are studied.