Petromod Introduction

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Transcript of Petromod Introduction

Application to 1-D Basin Modeling

PetroModSchlumberger

• Simulation of basin evolution: tracking hydrocarbon generation and expulsion

• Estimate volume hydrocarbon entrapment, flow and accumulation

• Spatial scale: 10s to 100s of Kms.

• Time scale: 100s to Mas

• Dynamic reservoir geometry

• 1D model: examines burial history at a point location.

• 2-D model: either in map or cross section, can be used to reconstruct oil and gas generation, migration and accumulation along a cross section.

• 3-D model: reconstructs petroleum systems at reservoir and basin scales and has the ability to display the output in 1D, 2D or 3D, and through time

• Al-Hajeri and Al Saeed et al. (2009)

PurposeBasin and Petroleum System Modeling

Create New Project

New model folders

New model folders

2-D and 3-D Petromod Tools

PetroMod 1-D

Create new model

Conceptual Model Building Steps

1. Structural and Stratigraphic Model

2. Present day petroleum system analysis

•Al-Hajeri and Al Saeed et al. (2009)

Generic EventsIn

put

Out

put

•Al-Hajeri and Al Saeed et al. (2009)

Materials

Main Input• Sediment deposition (Stratigraphy)• Erosion• Lithology• Petroleum System Elements (PSE)• Total Organic Carbon (TOC)• Kinetics • Hydrogen Index

Boundary Conditions• Paleo-Water Depth (PWD)• Sediment Water Interface Temperature (SWI-Temperature)• Heat Flow

• Al-Hajeri and Al Saeed et al. (2009)

Basin and Petroleum System Modeling

Main Input

TOC: Quantity of organic carbon in source rock, both kerogen and bitumen.

HI: (S2/TOC) x 100An estimate of hydrogen richness in source rock. It help estimating maturity if kerogen content is known. HI-OI plot can give a rough assessment of petroleum generative potential of a source rock

http://www.dcnr.state.pa.us/topogeo/econresource/oilandgas/marcellus/sourcerock_index/sourcerock_quanity/index.htm

Main Input

Main Input

Kinetics

Reaction tabs

Well Assignment

Well Assignment

• Paleo-Water Depth (PWD) is an important parameter which controls the rate of sedimentation, erosion, and the volume of water controls pressure load on top of a system.

• Temperature controls transformation of kerogen into petroleum

• Paleo-Heat flow

• Sediment-Water Interface Temperature (SWIT)

Boundary Conditions

•Al-Hajeri and Al Saeed et al. (2009)

Boundary Conditions McKenzie Model for Heat Flow during Rifting

Boundary Conditions: Heat flow (McKenzie Model)

Petroleum System Element Edit

Burial History Preview

• Checking Geometric evolution of the model• This is not simulated data (No compaction added)

Simulation

Results: Time Plots

Results: Burial History Plot with HC Potential Overlay

Results: Burial History Plot with Paleo-Temp Overlay