| Well (UWI) | 15-135-24,938-00-00 |
| Log date | Sat Oct 24 20-24-33 2009 |
| Service company | Log Tech |
| Acquisition date (header) | Sat Oct 24 20-24-33 2009 |
| PLSS location | Sec 13 T19 S R22 W (map precision ±1.6 km) |
| Larionov variant | old_rocks (degraded) |
| Convergence status | DID_NOT_CONVERGE |
| Confidence tier | ○ BRACKETED |
| Engine versions | calc_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 SHA | bd23bea18153 |
| Generated | autonomously, 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
⚠️ 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.
| Edit type | Curve | Detail |
|---|---|---|
| unit_conversion | NPHI | factor 0.01 |
| hard_range_mask | RXO | count 1 |
| hard_range_mask | RT | count 174 |
| hard_range_mask | RMED | count 16 |
| hard_range_mask | RHOB | count 1 |
| hard_range_mask | DRHO | count 1 |
| hard_range_mask | PHID_SVC | count 3 |
| range_warn | GR | count 2 |
| range_warn | RHOB | count 1 |
| range_warn | NPHI | count 24 |
| spike_removal | — | 138 edits |
| degradation | — | 2 edits |
Raw mnemonics mapped to canonical curve names:
| Canonical | Raw mnemonic |
|---|---|
| DCAL | DCAL |
| DRHO | RHOC |
| GR | GR |
| NPHI | CNLS |
| PHID_SVC | DPOR |
| RHOB | RHOB |
| RMED | RILM |
| RT | RILD |
| RXO | RLL3 |
| SP | SP |
Unit conversions: NPHI×0.01.
Edits applied before compute (by type): degradation: 2, hard_range_mask: 6, range_warn: 3, spike_removal: 138, unit_conversion: 1.
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).
| Step | Method (frozen) | Version |
|---|---|---|
| Vsh | 2-mineral volumetric solve (matrix+clay+porosity from RHOB+NPHI) | vsh_multimineral 0.1.0 |
| PHIE | Density-neutron crossplot, shale-corrected | phie_density_neutron 0.1.0 |
| Sw | Archie 1942 | sw_archie 0.1.0 |
| Net pay | Vsh/PHIE/Sw cutoffs → net sand → net reservoir → net pay | netpay 0.1.0 |
| Uncertainty | Monte Carlo P10/P50/P90 + parameter sensitivity | mc 0.1.0 |
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.
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).
Composite log

Pickett plot

Neutron-density crossplot

Buckles plot

Hingle plot

Distributions

Sensitivity tornado

Net-pay Monte-Carlo distribution

Mean Vsh by method (selection is the agent's; the LLM authors no number):
| Method | Mean Vsh | Selected |
|---|---|---|
| vsh_larionov_old | 0.348 | |
| vsh_larionov_tertiary | 0.279 | |
| vsh_linear | 0.460 | |
| vsh_clavier | 0.334 | |
| vsh_steiber | 0.300 | |
| vsh_neutron_density | 0.147 | |
| vsh_multimineral | 0.153 | ✓ |
Mean porosity by method (effective where shale-corrected; the LLM authors no number):
| Method | Mean porosity | Selected |
|---|---|---|
| phie_density_neutron | 0.070 | ✓ |
| phi_density | 0.087 | |
| phi_neutron | 0.119 |
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.
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):
| Method | Mean Sw | Selected |
|---|---|---|
| sw_archie | 0.808 | ✓ |
| sw_simandoux | 0.687 | |
| sw_indonesia | 0.715 |
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.
| Interval | Top (m) | Base (m) | Net pay (m) | Avg PHIE | Avg Sw | Avg Vsh |
|---|---|---|---|---|---|---|
| Z1 | 1010.9 | 1011.3 | 0.6 | 0.318 | 0.266 | 0.000 |
| Z2 | 1063.9 | 1064.4 | 0.6 | 0.159 | 0.418 | 0.110 |
| Z3 | 1099.4 | 1100.6 | 1.4 | 0.216 | 0.401 | 0.101 |
| Z4 | 1119.5 | 1120.1 | 0.8 | 0.189 | 0.315 | 0.073 |
| Z5 | 1165.1 | 1167.2 | 2.3 | 0.145 | 0.335 | 0.040 |
| Z6 | 1202.4 | 1203.2 | 0.9 | 0.144 | 0.310 | 0.026 |
| Z7 | 1218.3 | 1218.7 | 0.6 | 0.146 | 0.335 | 0.141 |
| Z8 | 1227.6 | 1229.3 | 1.1 | 0.143 | 0.342 | 0.052 |
| Z9 | 1236.4 | 1237.2 | 0.9 | 0.155 | 0.380 | 0.159 |
| Z10 | 1241.6 | 1243.3 | 1.8 | 0.145 | 0.370 | 0.213 |
| Z11 | 1258.2 | 1259.9 | 1.8 | 0.143 | 0.376 | 0.212 |
| Z12 | 1281.8 | 1282.9 | 1.2 | 0.222 | 0.205 | 0.185 |
| Z13 | 1288.7 | 1294.6 | 4.9 | 0.156 | 0.316 | 0.071 |
| Z14 | 1309.9 | 1311.9 | 2.0 | 0.107 | 0.284 | 0.004 |
| Z15 | 1314.6 | 1317.5 | 2.3 | 0.143 | 0.247 | 0.117 |
| Quantity | Value |
|---|---|
| Gross interval | 321.0 m |
| Net pay (P10/P50/P90) | 2.9 / 10.9 / 27.0 m |
| Net-to-gross | 0.079 |
| Avg PHIE (net pay) | 0.159 |
| Avg Sw (net pay) | 0.329 |
| Avg Vsh (net pay) | 0.098 |
Monte Carlo, 500 realizations (seed 42). Net pay swing per parameter (one-at-a-time):
| Parameter | Net-pay swing (m) |
|---|---|
| m | 19.2 |
| Rw | 18.0 |
| a | 4.7 |
| n | 1.7 |
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.
_Uncalibrated screening estimate (no core); Sw used as the Swirr proxy._
_Built on the uncalibrated permeability; indicative only._
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.
| Parameter | Value | Unit | Provenance | Source |
|---|---|---|---|---|
| gr_min | 20.000 | API | default | — |
| gr_max | 120.000 | API | default | — |
| rho_ma | 2.710 | g/cc | default | Schlumberger 1989 |
| rho_fl | 1.000 | g/cc | default | — |
| phie_max | 0.450 | v/v | default | — |
| phi_sh_d | 0.100 | v/v | default | — |
| phi_sh_n | 0.350 | v/v | default | — |
| a | 1.000 | - | default | Winsauer et al. 1952 |
| m | 2.000 | - | default | Archie, G.E. 1942 |
| n | 2.000 | - | default | Archie, G.E. 1942 |
| Rw | 0.040 | ohm-m | default | Kansas Geological Survey 2000 |
| rt_hydrocarbon_floor | 5.000 | ohm-m | default | — |
| vsh_cutoff | 0.350 | v/v | default | — |
| phie_cutoff | 0.100 | v/v | default | — |
| sw_cutoff | 0.500 | v/v | default | — |
| bit_size_config | 7.875 | in | default | — |
| qc_abort_threshold | 0.800 | - | default | — |
| circuit_breaker_n | 3.000 | - | default | — |
The citations table (not RAG) gives each cited parameter exactly one frozen source. Parameters tagged
defaultare regional/global — they drive the bracketed tier.
Boundary-inclusive criteria applied by the engine (netpay) to flag reservoir:
| Stage | Criterion | Cutoff | Provenance |
|---|---|---|---|
| Net sand | Vsh ≤ cutoff | 0.350 | default |
| Net reservoir | + PHIE ≥ cutoff | 0.100 | default |
| Net pay | + Sw ≤ cutoff | 0.500 | default |
Cutoff values are engine parameters (never LLM-authored); the dominant net-pay uncertainty is m — see Uncertainty for the swing.
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.
| Validator | Type | Detail |
|---|---|---|
| vsh_phie_anticorrelation | support | Vsh-PHIE Pearson 1.00 > 0.3 (dirty rock + high porosity) |
| rt_sw_consistency | mechanical | 16 depths with Sw<0.4 but RT<5.0 ohm-m |
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"]
This is a LAS-only study. Data that would calibrate the interpretation is absent:
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.
{
"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": []
}
}
| Item | Present |
|---|---|
| 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 | ✓ |