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Record W2791874717 · doi:10.2118/184880-pa

Far-Field Proppant Detection Using Electromagnetic Methods: Latest Field Results

2018· article· en· W2791874717 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueSPE Production & Operations · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeophysical and Geoelectrical Methods
Canadian institutionsConocoPhillips (Canada)
FundersSandia National Laboratories
KeywordsField (mathematics)Electromagnetic fieldPetroleum engineeringGeologyPhysicsMathematics

Abstract

fetched live from OpenAlex

Summary More than 100 billion lbm of proppant are placed annually in wells across the globe, with the majority in unconventional reservoirs. The location of the proppant in these horizontal wells and formations is critical to understanding reservoir drainage, well spacing, and stage spacing. However, for many years proppant detection has primarily been limited to near-wellbore measurements. A novel method to detect proppant in the far field has been developed and is the subject of this paper. The proppant-detection method developed uses electromagnetic (EM) methods. This technology entails using a transmitter source and an array of electric- and magnetic-field sensors at the surface. A current signal with a unique wave form and frequency is transmitted to the bottom of the wellbore via a standard electric-line (E-line) unit. In addition, an electrically conductive proppant is pumped into the stage(s) of interest. The electric and magnetic fields are measured both before and after the detectable proppant stages, and a novel analysis method is then used to process and invert these differenced data to create an image of the propped reservoir volume (PRV). This technology is the product of years of development of computer models capable of forward modeling this technique. Once this modeling was completed, an initial field test was performed in west Texas (WTX), with a preliminary analysis of this work presented in a previous paper (Palisch et al. 2016). Since that paper, however, additional processing of the data has yielded a much-more-detailed image of the proppant location in this Bone Springs well. In addition, a subsequent field application has been performed in a major basin in the northeastern US. Multiple stages received detectable proppant of varying stage volumes, and the analysis has also shown a detailed image of the proppant location in that wellbore. Furthermore, the initial field test in WTX used only electric-field sensors, whereas this latest test used both electric- and magnetic-field receivers. The authors’ numerical simulations coupled with the field results indicate the percentage difference between prefracture and post-fracture results is two times higher using magnetic- vs. electric-field sensors. This paper will review the technology development and methods, will present the latest imaging from the initial WTX test, and will describe the latest learnings from the most-recent field test. This paper should be beneficial to all completions and development personnel who are interested in knowing where proppant is in their fractures. This technology has the potential to assist in understanding well drainage and spacing, stage and perforation-cluster spacing, vertical fracture coverage, and the effect of fracture-design changes.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Other design · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.872
Threshold uncertainty score0.967

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.033
GPT teacher head0.312
Teacher spread0.279 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it