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Petrophysical Interpretation Report — 15-135-24,938-00-00

Well (UWI)15-135-24,938-00-00
Log dateSat Oct 24 20-24-33 2009
Service companyLog Tech
Acquisition date (header)Sat Oct 24 20-24-33 2009
PLSS locationSec 13 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 1000.0 m and 1321.0 m — the interval above it is not evaluated (unconsolidated, washed-out response). Within that interval the net pay is 25.5 m with average effective porosity 0.159 and average water saturation 0.329. Monte-Carlo places the P50 net pay at 10.9 m within a P10-P90 range of 2.9 to 27.0 m. An independent SP-derived water resistivity of 0.0445 ohm-m (static SP -58.4 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 0.554 over 2071 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 = 2.9 / 10.9 / 27.0 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 174
hard_range_maskRMEDcount 16
hard_range_maskRHOBcount 1
hard_range_maskDRHOcount 1
hard_range_maskPHID_SVCcount 3
range_warnGRcount 2
range_warnRHOBcount 1
range_warnNPHIcount 24
spike_removal138 edits
degradation2 edits

4. Standardization

Raw mnemonics mapped to canonical curve names:

CanonicalRaw mnemonic
DCALDCAL
DRHORHOC
GRGR
NPHICNLS
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: 2, hard_range_mask: 6, range_warn: 3, spike_removal: 138, 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
SwArchie 1942sw_archie 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=1.43, n_flagged=798, intervals=[[265.5, 267.2], [276.1, 291.7], [292.3, 293.1], [294.7, 295.0], [296.3, 300.2], [301.1, 309.5], [310.4, 331.2], [337.3, 338.8], [341.5, 342.4], [352.2, 353.6]].

Invasion profile (multi-depth resistivities, 7969 samples): fraction with shallow reading above deep (Rxo/RT > 1.2, invaded/permeable indication): 0.682; reversed (< 0.8): 0.058; median Rxo/RT 1.402; median Rmed/RT 1.006. 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: 0.107, limestone: 0.256, dolomite: 0.075. 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_old0.348
vsh_larionov_tertiary0.279
vsh_linear0.460
vsh_clavier0.334
vsh_steiber0.300
vsh_neutron_density0.147
vsh_multimineral0.153

15. Porosity

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

MethodMean porositySelected
phie_density_neutron0.070
phi_density0.087
phi_neutron0.119

Service-company porosity curves (cross-check evidence, full-column means): phid_svc: 0.343. Matrix assumptions differ per curve; agreement/disagreement is the analyst's reading.


16. Water saturation

Mean Sw (Archie 1942) = 0.808 (a=1.00, m=2.00, n=2.00, Rw=0.0180 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_archie0.808
sw_simandoux0.687
sw_indonesia0.715

17. Zonation (net-pay intervals)

Raw net-pay runs merged into 22 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
Z11010.91011.30.60.3180.2660.000
Z21063.91064.40.60.1590.4180.110
Z31099.41100.61.40.2160.4010.101
Z41119.51120.10.80.1890.3150.073
Z51165.11167.22.30.1450.3350.040
Z61202.41203.20.90.1440.3100.026
Z71218.31218.70.60.1460.3350.141
Z81227.61229.31.10.1430.3420.052
Z91236.41237.20.90.1550.3800.159
Z101241.61243.31.80.1450.3700.213
Z111258.21259.91.80.1430.3760.212
Z121281.81282.91.20.2220.2050.185
Z131288.71294.64.90.1560.3160.071
Z141309.91311.92.00.1070.2840.004
Z151314.61317.52.30.1430.2470.117

18. Results

QuantityValue
Gross interval321.0 m
Net pay (P10/P50/P90)2.9 / 10.9 / 27.0 m
Net-to-gross0.079
Avg PHIE (net pay)0.159
Avg Sw (net pay)0.329
Avg Vsh (net pay)0.098

19. Uncertainty and sensitivity

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

ParameterNet-pay swing (m)
m19.2
Rw18.0
a4.7
n1.7

Dominant uncertainty: m (swing 19.2 m).

Multi-seed robustness: P50 UNSTABLE across seeds (spread 2.1 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. Permeability (uncalibrated)

_Uncalibrated screening estimate (no core); Sw used as the Swirr proxy._


22. Rock quality (uncalibrated)

_Built on the uncalibrated permeability; indicative only._


23. Electrofacies

Unsupervised k-means on 1774 samples into 4 electrofacies (sample counts: facies 0: 270, facies 1: 466, facies 2: 319, facies 3: 719). Descriptive only — no core labels.


24. 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.


25. 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.


26. Data quality and validator objections

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

QC edits applied before compute — degradation: 2, hard_range_mask: 6, range_warn: 3, spike_removal: 138, unit_conversion: 1.

ValidatorTypeDetail
vsh_phie_anticorrelationsupportVsh-PHIE Pearson 1.00 > 0.3 (dirty rock + high porosity)
rt_sw_consistencymechanical16 depths with Sw<0.4 but RT<5.0 ohm-m

27. 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: permeability"]
    act_10["tool_call: permeability"]
    dec_11["decision: step: rock_quality"]
    act_11["tool_call: rock_quality"]
    dec_12["decision: step: electrofacies"]
    act_12["tool_call: electrofacies"]
    dec_13["decision: step: lithology"]
    act_13["tool_call: lithology"]

28. Data gaps for calibration

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


29. Limitations


30. Conclusions

900 m bin 2.16 (washed); sustained from 1000 m (2.44). N-D clay ~0.07 -> Archie. 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": 25.450800000000015,
  "net_pay_p10_p50_p90": [
    2.8956000000000017,
    10.896600000000007,
    26.974800000000016
  ],
  "driving_params": {
    "a": 1.0,
    "m": 2.0,
    "n": 2.0,
    "Rw": 0.04
  },
  "claim_verifier": {
    "result": "FLAGS",
    "flags": [
      2.16
    ],
    "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