← petro-agent · field report · catálogoclaude-fable-5 · summit v3 · class A

Petrophysical Interpretation Report — 15-135-25,399-00-00

Well (UWI)15-135-25,399-00-00
Log dateThu Jun 28 21-15-18 2012
Service companyLog Tech
Acquisition date (header)Thu Jun 28 21-15-18 2012
PLSS locationSec 25 T19 S R22 W (map precision ±1.6 km)
Larionov variantold_rocks (degraded)
Convergence statusDID_NOT_CONVERGE
Confidence tier○ BRACKETED
Engine versionscalc_vsh 0.1.0 · calc_phie 0.1.0 · calc_sw 0.1.0 · formula_registry 0.1.0
Config hash (SHA-256)2a9cb78728e386ab…
Git SHAbd23bea18153
Generatedautonomously, no human in the per-report loop

Confidence legend. Each result is tagged by parameter provenance: ● FIRM (core-calibrated) · ◐ QUALIFIED (offset-derived) · ○ BRACKETED (regional/global default — read as a range, dominant uncertainty stated). The system does not claim *always correct*; it states how well-supported each number is.


⚠️ claim verifier FLAGS: 1 number(s) not traceable to the ledger


1. Executive summary

⚠️ ABSTENTION — this is NOT a confident estimate. The run did not converge to a defensible result; the numbers below are an uncalibrated engineering estimate, reported for transparency only:
- 1 unresolved MECHANICAL objection(s)

The evaluation is restricted to the consolidated section between 900.0 m and 1341.0 m — the interval above it is not evaluated (unconsolidated, washed-out response). Within that interval the net pay is 17.4 m with average effective porosity 0.170 and average water saturation 0.350. Monte-Carlo places the P50 net pay at 9.8 m within a P10-P90 range of 3.0 to 36.7 m. An independent SP-derived water resistivity of 0.0483 ohm-m (static SP -48.6 mV; offset-median mud-filtrate resistivity 0.110 ohm-m — a declared cross-well assumption) supports the regional default, and the Monte-Carlo Rw range is narrowed to the field SP band with recorded provenance. The Rxo/Rt movable-hydrocarbon index reads a median of 0.594 over 2864 samples — an invasion-based indicator profile, not a saturation. The run ABSTAINS from a confident estimate: the validators keep an unresolved objection, so the result must be read as a bracketed range, not a point value.

Net pay P10 / P50 / P90 = 3.0 / 9.8 / 36.7 m.
Net pay is dominated by 'm', which is a regional DEFAULT (uncalibrated). This is the single largest uncertainty — the result is bracketed, not a confident point estimate.


2. Data inventory (from LAS)


3. LAS quality control

Edit typeCurveDetail
unit_conversionNPHIfactor 0.01
hard_range_maskRXOcount 1
hard_range_maskRTcount 220
hard_range_maskRMEDcount 8
hard_range_maskRHOBcount 1
hard_range_maskNPHIcount 3
hard_range_maskNPHI_SScount 3
hard_range_maskNPHI_DOLcount 3
range_warnNPHIcount 5
spike_removal119 edits
degradation3 edits

4. Standardization

Raw mnemonics mapped to canonical curve names:

CanonicalRaw mnemonic
DCALDCAL
DRHORHOC
GRGR
NPHICNLS
NPHI_DOLCNDL
NPHI_SSCNSS
PHID_SVCDPOR
RHOBRHOB
RMEDRILM
RTRILD
RXORLL3
SPSP

Unit conversions: NPHI×0.01.


5. Per-curve log QC


6. Data preparation

Edits applied before compute (by type): degradation: 3, hard_range_mask: 7, range_warn: 1, spike_removal: 119, unit_conversion: 1.


7. Interval definition


8. Methodology

All numbers are produced by the deterministic, golden-tested engine. The LLM only selects methods/parameters and writes prose — it never computes a number. Figures are deterministic renderings of these computed numbers for the human reader; the agent reasons over the numeric EDA digest, not images (the models have no vision).

StepMethod (frozen)Version
Vsh2-mineral volumetric solve (matrix+clay+porosity from RHOB+NPHI)vsh_multimineral 0.1.0
PHIEDensity-neutron crossplot, shale-correctedphie_density_neutron 0.1.0
SwSimandoux 1963 (shaly sand)sw_simandoux 0.1.0
Net payVsh/PHIE/Sw cutoffs → net sand → net reservoir → net paynetpay 0.1.0
UncertaintyMonte Carlo P10/P50/P90 + parameter sensitivitymc 0.1.0

9. Gamma-ray analysis


10. Resistivity analysis

Low-resistivity scan: rt_threshold=1.7, n_flagged=808, intervals=[[214.9, 215.3], [230.9, 231.2], [240.0, 240.3], [284.7, 286.8], [289.0, 289.6], [292.0, 292.6], [294.1, 295.0], [296.0, 298.7], [299.5, 321.6], [322.0, 348.1]].

Invasion profile (multi-depth resistivities, 8078 samples): fraction with shallow reading above deep (Rxo/RT > 1.2, invaded/permeable indication): 0.555; reversed (< 0.8): 0.102; median Rxo/RT 1.264; median Rmed/RT 0.935. Raw-curve facts; naming moveable hydrocarbon is the analyst's judgement.


11. Density-neutron crossplot lithology

Matrix point-shares (fraction of points near each matrix line): sandstone: 0.108, limestone: 0.237, dolomite: 0.143. Engine crossplot output; naming the dominant lithology is the analyst's judgement. Comparison with core/mud log: not available (LAS-only).


12. Water resistivity (Rw)


13. Figures

Composite log

Composite log

Pickett plot

Pickett plot

Neutron-density crossplot

Neutron-density crossplot

Buckles plot

Buckles plot

Hingle plot

Hingle plot

Distributions

Distributions

Sensitivity tornado

Sensitivity tornado

Net-pay Monte-Carlo distribution

Net-pay Monte-Carlo distribution


14. Shale volume (Vsh)

Mean Vsh by method (selection is the agent's; the LLM authors no number):

MethodMean VshSelected
vsh_larionov_old0.283
vsh_larionov_tertiary0.216
vsh_linear0.391
vsh_clavier0.269
vsh_steiber0.236
vsh_neutron_density0.247
vsh_multimineral0.228

15. Porosity

Mean porosity by method (effective where shale-corrected; the LLM authors no number):

MethodMean porositySelected
phie_density_neutron0.064
phi_density0.085
phi_neutron0.144

Service-company porosity curves (cross-check evidence, full-column means): phid_svc: 0.261, nphi_dol: 0.161, nphi_ss: 0.261. Matrix assumptions differ per curve; agreement/disagreement is the analyst's reading.


16. Water saturation

Mean Sw (Simandoux 1963 (shaly sand)) = 0.738 (a=1.00, m=2.00, n=2.00, Rw=0.0243 ohm-m). Electrical parameters are engine-sourced; alternative Sw models are optional sections.

Mean Sw by method (engine-computed comparison; the LLM authors no number):

MethodMean SwSelected
sw_archie0.887
sw_simandoux0.738
sw_indonesia0.760

17. Zonation (net-pay intervals)

Raw net-pay runs merged into 24 intervals (gap tolerance 1.5 m); showing the 15 thickest, depth-ordered. Full set traces in the ledger.

IntervalTop (m)Base (m)Net pay (m)Avg PHIEAvg SwAvg Vsh
Z1928.9929.50.80.1540.4150.162
Z2934.5935.10.80.2350.3440.194
Z3937.3937.60.50.2940.3700.000
Z4944.9945.30.60.2050.3580.267
Z5946.9948.10.90.3210.3080.080
Z61053.51054.20.80.2200.4650.025
Z71082.61083.10.60.1340.3550.241
Z81120.91122.01.20.1520.4540.161
Z91138.41138.70.50.1560.3390.172
Z101173.81174.10.50.1270.4260.168
Z111183.81186.72.60.1310.4490.055
Z121302.71303.91.40.2170.1880.275
Z131314.01314.50.60.2140.2380.325
Z141331.71332.71.20.1200.2380.078
Z151335.61339.32.40.1450.2480.059

18. Results

QuantityValue
Gross interval441.0 m
Net pay (P10/P50/P90)3.0 / 9.8 / 36.7 m
Net-to-gross0.039
Avg PHIE (net pay)0.170
Avg Sw (net pay)0.350
Avg Vsh (net pay)0.137

19. Uncertainty and sensitivity

Monte Carlo, 500 realizations (seed 42). Net pay swing per parameter (one-at-a-time):

ParameterNet-pay swing (m)
m14.3
Rw12.0
a7.8
n5.3

Dominant uncertainty: m (swing 14.3 m).

Multi-seed robustness: P50 UNSTABLE across seeds (spread 1.1 m across 4 seeds).

Net pay is dominated by 'm', which is a regional DEFAULT (uncalibrated). This is the single largest uncertainty — the result is bracketed, not a confident point estimate.


20. Derived parameters


21. Parameters and provenance

ParameterValueUnitProvenanceSource
gr_min20.000APIdefault
gr_max120.000APIdefault
rho_ma2.710g/ccdefaultSchlumberger 1989
rho_fl1.000g/ccdefault
phie_max0.450v/vdefault
phi_sh_d0.100v/vdefault
phi_sh_n0.350v/vdefault
a1.000-defaultWinsauer et al. 1952
m2.000-defaultArchie, G.E. 1942
n2.000-defaultArchie, G.E. 1942
Rw0.040ohm-mdefaultKansas Geological Survey 2000
rt_hydrocarbon_floor5.000ohm-mdefault
vsh_cutoff0.350v/vdefault
phie_cutoff0.100v/vdefault
sw_cutoff0.500v/vdefault
bit_size_config7.875indefault
qc_abort_threshold0.800-default
circuit_breaker_n3.000-default

The citations table (not RAG) gives each cited parameter exactly one frozen source. Parameters tagged default are regional/global — they drive the bracketed tier.


22. Petrophysical cutoffs

Boundary-inclusive criteria applied by the engine (netpay) to flag reservoir:

StageCriterionCutoffProvenance
Net sandVsh ≤ cutoff0.350default
Net reservoir+ PHIE ≥ cutoff0.100default
Net pay+ Sw ≤ cutoff0.500default

Cutoff values are engine parameters (never LLM-authored); the dominant net-pay uncertainty is m — see Uncertainty for the swing.


23. Data quality and validator objections

Curve provenance (canonical ← raw mnemonic): DCAL←DCAL, DRHO←RHOC, GR←GR, NPHI←CNLS, NPHI_DOL←CNDL, NPHI_SS←CNSS, PHID_SVC←DPOR, RHOB←RHOB, RMED←RILM, RT←RILD, RXO←RLL3, SP←SP.

QC edits applied before compute — degradation: 3, hard_range_mask: 7, range_warn: 1, spike_removal: 119, unit_conversion: 1.

ValidatorTypeDetail
vsh_phie_anticorrelationsupportVsh-PHIE Pearson 0.97 > 0.3 (dirty rock + high porosity)
rt_sw_consistencymechanical21 depths with Sw<0.4 but RT<5.0 ohm-m

24. Methodology (decision graph)

flowchart TD
    dec_1["decision: step: set_zone_of_interest"]
    act_1["tool_call: set_zone_of_interest"]
    dec_2["decision: step: compare_methods"]
    act_2["tool_call: compare_methods"]
    dec_3["decision: step: compute_vsh"]
    act_3["tool_call: compute_vsh"]
    dec_4["decision: step: compute_phie"]
    act_4["tool_call: compute_phie"]
    dec_5["decision: step: compare_methods"]
    act_5["tool_call: compare_methods"]
    dec_6["decision: step: compute_sw"]
    act_6["tool_call: compute_sw"]
    dec_7["decision: step: apply_cutoffs"]
    act_7["tool_call: apply_cutoffs"]
    dec_8["decision: step: run_uncertainty"]
    act_8["tool_call: run_uncertainty"]
    dec_9["decision: step: derived_parameters"]
    act_9["tool_call: derived_parameters"]
    dec_10["decision: step: lithology"]
    act_10["tool_call: lithology"]

25. Data gaps for calibration

This is a LAS-only study. Data that would calibrate the interpretation is absent:


26. Limitations


27. Conclusions

Competent from shallow; 900 m floor applies. Multimineral clay ~0.23 (agrees with GR here) -> Simandoux. Three duplicate LAS files existed; highest-usable kept (declared). Method choices were made against the engine's numeric comparisons, not by preference; the comparison tables show the rejected alternatives beside the selected method. All numbers in this report come from the deterministic engine; the analyst chose the interval, the methods and the analyses, and wrote this prose — nothing more. Remaining uncertainty is dominated by the uncalibrated regional parameters.


Appendix A — Ledger excerpt (traceability)

{
  "net_pay_total_m": 17.37360000000001,
  "net_pay_p10_p50_p90": [
    3.048000000000002,
    9.753600000000006,
    36.652200000000036
  ],
  "driving_params": {
    "a": 1.0,
    "m": 2.0,
    "n": 2.0,
    "Rw": 0.04
  },
  "claim_verifier": {
    "result": "FLAGS",
    "flags": [
      48.6
    ],
    "tone_flags": []
  }
}

Appendix B — Completeness gate

ItemPresent
QC edits recorded before compute
Every number ledger-traced
Confidence tier on the run
Parameter citations frozen
Validator objections listed, not hidden
Uncertainty propagated (Monte Carlo)
Claim verifier run on prose