Condensate
/Gas Ratio Variability and Prediction in the Obaiyed Field, Western Desert, Egypt: Integrated Technology for Effective Near-field Exploration
By
Erdem Idiz1, J. Westrich1, P. van Laer1, O. Podlaha1, M. Nour-el-din2, J. Schreurs2, B. Bell3, P. Boerrigter3
(1) Shell International E&P B.V, 2280 AB Rijswijk, Netherlands (2) SENV, (3) Bapetco, Cairo, Egypt
The development and application of reliable methods for predicting
condensate
-to-gas ratio (CGR) in the area of Obaiyed field in the western desert
of Egypt, is a critical issue for both near-field exploration activities and
ongoing redevelopment efforts within the field. As is commonly the case for
gas/
condensate
assets, liquid production in Obaiyed has a significant impact on
overall financial performance. CGR prediction is best approached from an
integrated perspective that combines aspects of reservoir engineering,
geochemistry, and petroleum systems
analysis
. The current study comprised the
following elements: (a) a comprehensive evaluation of CGR variability based on
PVT analyses and production test results (b) detailed investigation of
condensate
and gas geochemistry data aimed at establishing the underlying
controls of CGR variability and (c) a 3-D basin modeling study to provide a
regional understanding of source and migration factors impacting CGR. The
results of the study showed:
- Gases and
oil
/condensates in the Obaiyed field and satellites are all from
a common Khataba source, but multiple kitchen areas have contributed to the
accumulations.
- The bulk of the ‘condensates’ are oils dissolved in the gases. Gases, in particular, show a large variation in maturity and vary systematically across the field. CGR values show a strong correlation with the gas maturities.
- Lateral and column height variations in all geochemical parameters dominate over stratigraphic variability at any one location.
- The CGR variability in Obaiyed is caused by incomplete mixing of several
phases of charge that have entered the trap over time (i.e.,
oil
, wet gas and
dry gas). The gradients in fluid properties are likely due to (1) insufficient
time for homogenization and/or (2) the presence of barriers/baffles in the Lower
Safa Fm.
The key control on CGR in Obaiyed and surrounding prospects is whether there is charge access to highly mature dry gas coming out of the Matruh trough.
