New NMR-Based Methodology for Inferring the Presence of Movable Heavy Oil in Reservoir Layers* Pedro A. Romero1, Nestor Acosta2, and Hiran Serrano3 Search and Discovery Article #40519 (2010) Posted March 18, 2010 *Adapted from expanded abstract and slides prepared for oral presentation at AAPG International Conference and Exhibition, Rio de Janeiro, Brazil, November 15-18, 2009 1 Baker Hughes Inc., Rio de Janeiro, Brazil (pedro.romero@bakerhughes.com) Baker Hughes Inc., Comodoro Rivadavia, Argentina 3 YPF S.A., Comodoro Rivadavia, Argentina 2 Abstract The present contribution is the result of the authors’ several experiences in the NMR analysis of sandstone reservoirs with argillaceous-tuffaceous matrix belonging to geological formations of Cretaceous age. It is intended to highlight the advantages and synthetically show the main aspects of the use of NMR tools for characterization of movable heavy oil in continental clastic reservoirs of the Gulf of San Jorge Basin in Argentina. The methodology presented is for inferring the presence of movable heavy oil in reservoir layers of a fluvial environment. It is based on six main principal indicators: reservoir pressure development of spontaneous potential increase of the resistivity response of the layer the slope of the T2 log mean of the furthest right hand side lobe of the T2 distribution when plotted in depth the presence of water-based mud filtrate in the DT2 maps the NMR permeability When these indicators are considered, the prediction of the layer can be forecast with high probability. This work specially describes how NMR derived properties improve the fluid typing in these reservoirs. The present approach has been validated with measured data from production tests. Copyright © AAPG. Serial rights given by author. For all other rights contact author directly. References Acosta, N., 2008, Analysis of Nuclear Magnetic Resonance for characterization of continental clastic reservoirs, San Jorge Basin, Argentina: Naturalia Patagonic Science Magazine. Acosta, N., P. Romero, G. Magenta, G. Potas, C. Cabrera, C. Coccia, L. Di Benedetto, and L. Ferreira, 2007, Methodology for characterization of a clastic reservoir based on correlations between electrofacies, NMR and image logs, A case study from San Jorge Basin: 10th. International Congress of the Brazilian Geophysical Society and EXPOGEF, Rio de Janeiro, Brazil, Acosta, N., E. Estrada, and B. Saavedra, 2007, Porosity variations by diagenesis in reservoirs of the Bajo Barreal Formation, San Jorge Basin: Methodology of evaluation with logs: X Latin American and Caribbean Petroleum Engineering Conference, SPE # 108065, Buenos Aires, Argentina. Breda, E., and M. Lucero (Repsol-YPF), 2005, Caracterización de los reservorios de la Formación Bajo Barreal Inferior Arenas y Tobas (Sección Tobácea), VI Congreso de Exploración y Desarrollo de Hidrocarburos, 1, p. 197-214. Mar del Plata, Argentina. Chen, S., G. Hursan, D. Beard, and D. Georgi, SPE 84481: G.TE Correction for Processing Multigradient, Multiple –TE NMR Log Data. SPE, Texas, USA. Domínguez, H., B. Saavedra, A. Corbelleri, and L. Sliwinsky, 2005, Uso de resonancia magnética nuclear para la caracterización de reservorios y fluidos en yacimientos de la Cuenca del Golfo San Jorge, Patagonia, Argentina: VI Congreso de Exploración y Desarrollo de Hidrocarburos, Mar del Plata, 1, p. 59-71. Pedro A. Romero Nestor Acosta Hiran Serrano NMR Petrophysics NMR Behavior Of Heavy Oil Detection Of Heavy Oil – Field Example Summary NMR porosity measurement ◦ Calibrated to 100% water tank ◦ Amplitude of measured signal as % of calibrated signal is NMR total porosity 100 pu ↔ Mcal M log Calibration Tank M cal Mlog NMR Time 100 Echo Train Amplitude Amplitude RF Pulses 90°x 180°y 180°y Echo Signals 180°y 180°y 180°y TE Time Echo Train TW Time TE : inter-echo spacing time TW : wait time ( ≥ 3 x T1 for full recovery) NMR logging measures: Amount of Magnetization of 1H present in the rock sample independently of the lithology Slow relaxation times in large pores Fast relaxation times in small pores Pore Geometry: Surface, Volume 1 / T2s = * S / V Fluid typing: Viscosity 1 / T2b = 1200 Field Gradient: Diffusion 1 / T2d = [(* G * TE)2 ]*D / 12 NMR Porosity is defined by the equation A = HI * T * (1 - e - TW / T1) ◦ HI - Hydrogen Index of fluid filling the pore space Low hydrogen index of gas and light oil results in porosity undercall ◦ T1 - Longitudinal relaxation time ◦ TW - Time between measurements at the same frequency – TW ≥ 3*T1 for full recovery MR Depth of Investigation ∆B0,A ∆ℓA ∆B0,A = GA (Gauss/cm) 4 3 2 ∆ℓA f B0 Depth of Investigation (inches) 5 1 0 1000 ∆B0,B fA, B0,A ∆ℓB ∆B0,B fB, B0,B 900 800 700 600 Frequency (kHz) = GB (Gauss/cm) ∆ℓB fC, B0,C ∆B0,C ∆B0,C ∆ℓC ∆ℓC ℓA ℓB ℓC Efficiency….Data accuracy….People-oriented service D.O.I. = GC (Gauss/cm) 500 400 High Gradient 3 2 1 0 4 T2 cutoffs Partial Porosity Partial Porosity 4 Low Gradient 0.1 1 100 10 T2 (ms) Diffusion Effect Efficiency….Data accuracy….People-oriented service 1000 T2 cutoffs 3 2 1 0 0.1 1 100 10 1000 T2 (ms) No Diffusion Effect NMR Petrophysics NMR Behavior Of Heavy Oil Detection Of Heavy Oil – Field Example Summary Tar Clay Bound Water Heavy Oil Capillary Bound Water Moveable Water Water-based Mud-Filtrate Incremental Porosity (pu) T2 Cut-off 0.01 0.1 1 10 100 1000 0.01 0.1 1 10 100 1000 Detected NMR Spectrum 0.01 0.1 1 10 100 1000 T2 (ms) • What do we know about the model independently of any NMR data? Gas Light oil Heavy oil Free water Capillary-bound water Clay-bound water ◦ T1>=T2,i -> T1/T2,i is used instead of T1 ◦ T1/T2,i < 10 In most cases it remains under 3. ◦ 0.3 <= T2,i <= 10000 ms ◦ 10-12 <= D <= 10-7 m2/s” NMR Petrophysics NMR Behavior Of Heavy Oil Detection Of Heavy Oil – Field Example Summary Located in the heart of Patagonia, and extending from the Atlantic Ocean to the Andean foothills Accounts for around one third of the hydrocarbon production in Argentina. The origin and subsequent geological evolution of the basin are caused by the rift process responsible for the opening of the Atlantic Ocean in early Jurassic times. Accumulation of terrigeneous sediments continued well into early Cretaceous times Lab Log Permeability : Timur-Coates K = · · (BVM/BVI)χ NMR Petrophysics NMR Behavior Of Heavy Oil Detection Of Heavy Oil – Field Example Summary In oil-wet reservoirs, T2 intrinsic from water-based mud filtrate is a very significant indicator of the presence of movable heavy oil. The relaxation time of the water-based mud filtrate is around 1024 ms -a Bulk relaxation phenomenon. The T2 apparent spectra, when displayed for different GTE values, reflect mostly the enhanced relaxation of water-based mud filtrate displacing oil. The negative slope in depth of the log mean value of the higher T2 apparent spectral window may also indicate the presence of heavy oil. From Isolated to Integrated Data Analysis 26 Thank you Obrigado Gracias
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