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The AAPG/Datapages Combined Publications Database

West Texas Geological Society

Abstract


WTGS Fall Symposium: A Decade of Shale, 2018
Pages 68-69

Abstract: Reducing Risk and Mitigating Cost by Understanding the Source of H2S. Examples from Texas

Richard Drozd,1 P. F. DuBois,2 Derrick Whiting3

Abstract

No operator wants to have a sour gas problem in their well. Even worse, “Surprise, we detected 10, 1000 or > 10,000 ppm H2S in your well!”

The presence of H2S in the production stream is a well-known problem from a safety and commercial perspective. Understanding the H2S source is critical to estimating potential production quantities over time as well as identification of H2S trends. Source identification allows critical cost and associated risk reduction decisions such as evaluating chemical treatment vs sour facility to be made early in the life of the field.

Sulfur is incorporated into organic matter shortly after deposition, generally within the first few meters of the subsurface, via reduction of seawater sulfate by bacteria. If there are abundant metals available, the sulfur will preferentially form metal sulfides. There are three main sources of H2S in petroleum

Bacterial reduction of sulfate to H2S through dissimilatory reactions. The biological creation of H2S requires conditions in the subsurface compatible with bacterial growth, the most important of which is reservoir temperatures <80°C.

Thermochemical sulfate reduction = TSR. TSR is a reaction of sulfate minerals (primarily anhydrite) and petroleum to form H2S and carbonates. This reaction is thought to begin only a subsurface temperatures > 120°C or more.

Previous HitThermalNext Hit decomposition of sulfides in kerogen in clay-poor sulfur rich source rocks. The reactions are high temperature at the late stages of Previous HitthermalNext Hit Previous HitmaturationTop in carbonate dominated source rocks. Associated oils are high in sulfur and can provide a source for the H2S in addition to the primary kerogen.

Determining the origin of H2S found in any particular accumulation requires analysis of the H2S itself, as well as the other components of the natural gas, the water, and possibly any produced liquids. Examples from Texas will include thermochemical H2S that migrated from deep reservoirs, biological H2S generated in situ and a combination of both types.

Once the source has been identified informed economic decisions with respect to treatment, facility types and even where to market (sour or sweet) can be made early in field development.


 

Acknowledgments and Associated Footnotes

1 Richard Drozd: Weatherford Laboratories

2 P. F. DuBois: Weatherford Laboratories

3 Derrick Whiting: Weatherford Laboratories

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