| Well (UWI) | 15-135-25872-00-00 |
| Log date | Wed Jun 24 02-11-28 2015 |
| Service company | Pioneer Energy Services |
| Acquisition date (header) | Wed Jun 24 02-11-28 2015 |
| PLSS location | Sec 23 T19S R22W (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: 2 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 1333.5 m — the interval above it is not evaluated (unconsolidated, washed-out response). Within that interval the net pay is 26.1 m with average effective porosity 0.196 and average water saturation 0.313. Monte-Carlo places the P50 net pay at 13.0 m within a P10-P90 range of 2.3 to 29.1 m. An independent SP-derived water resistivity of 0.0481 ohm-m (static SP -49.0 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 0.628 over 2145 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 = 2.3 / 13.0 / 29.1 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 | RT | count 164 |
| hard_range_mask | RMED | count 83 |
| range_warn | GR | count 4 |
| range_warn | NPHI | count 3 |
| spike_removal | — | 125 edits |
| degradation | — | 3 edits |
Raw mnemonics mapped to canonical curve names:
| 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 |
Unit conversions: NPHI×0.01.
Edits applied before compute (by type): degradation: 3, hard_range_mask: 2, range_warn: 2, spike_removal: 125, 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=1.61, n_flagged=809, intervals=[[192.3, 194.2], [211.4, 212.4], [227.8, 228.3], [236.8, 237.7], [281.0, 283.0], [292.8, 293.1], [293.8, 298.6], [300.1, 303.0], [304.0, 305.7], [307.1, 309.2]].
Invasion profile (multi-depth resistivities, 8073 samples): fraction with shallow reading above deep (Rxo/RT > 1.2, invaded/permeable indication): 0.584; reversed (< 0.8): 0.085; median Rxo/RT 1.301; median Rmed/RT 0.960. Raw-curve facts; naming moveable hydrocarbon is the analyst's judgement.
Matrix point-shares (fraction of points near each matrix line): sandstone: 0.094, limestone: 0.176, dolomite: 0.068. 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 | 0.351 | |
| vsh_larionov_tertiary | 0.278 | |
| vsh_linear | 0.467 | |
| vsh_clavier | 0.337 | |
| vsh_steiber | 0.300 | |
| vsh_neutron_density | 0.166 | |
| vsh_multimineral | 0.167 | ✓ |
Mean porosity by method (effective where shale-corrected; the LLM authors no number):
| Method | Mean porosity | Selected |
|---|---|---|
| phie_density_neutron | 0.077 | ✓ |
| phi_density | 0.097 | |
| phi_neutron | 0.129 |
Service-company porosity curves (cross-check evidence, full-column means): phid_svc: 0.377, nphi_dol: 0.169, nphi_ss: 0.268. Matrix assumptions differ per curve; agreement/disagreement is the analyst's reading.
Mean Sw (Archie 1942) = 0.792 (a=1.00, m=2.00, n=2.00, Rw=0.0221 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 | 0.792 | ✓ |
| sw_simandoux | 0.649 | |
| sw_indonesia | 0.680 |
Raw net-pay runs merged into 23 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 | 1041.8 | 1044.2 | 1.7 | 0.221 | 0.417 | 0.000 |
| Z2 | 1067.6 | 1068.0 | 0.6 | 0.136 | 0.465 | 0.000 |
| Z3 | 1073.4 | 1076.1 | 2.9 | 0.375 | 0.190 | 0.000 |
| Z4 | 1081.0 | 1082.2 | 1.4 | 0.289 | 0.252 | 0.000 |
| Z5 | 1094.2 | 1094.7 | 0.6 | 0.133 | 0.416 | 0.002 |
| Z6 | 1127.9 | 1128.7 | 0.9 | 0.176 | 0.342 | 0.082 |
| Z7 | 1236.7 | 1238.2 | 0.8 | 0.116 | 0.422 | 0.132 |
| Z8 | 1247.2 | 1248.9 | 1.5 | 0.148 | 0.407 | 0.270 |
| Z9 | 1253.6 | 1254.3 | 0.8 | 0.188 | 0.349 | 0.252 |
| Z10 | 1258.2 | 1258.8 | 0.8 | 0.127 | 0.367 | 0.000 |
| Z11 | 1262.6 | 1263.4 | 0.9 | 0.147 | 0.352 | 0.124 |
| Z12 | 1270.4 | 1271.0 | 0.8 | 0.134 | 0.357 | 0.054 |
| Z13 | 1294.0 | 1294.9 | 0.9 | 0.224 | 0.226 | 0.305 |
| Z14 | 1301.2 | 1309.1 | 6.1 | 0.172 | 0.307 | 0.046 |
| Z15 | 1326.6 | 1329.8 | 3.4 | 0.171 | 0.204 | 0.042 |
| Quantity | Value |
|---|---|
| Gross interval | 333.5 m |
| Net pay (P10/P50/P90) | 2.3 / 13.0 / 29.1 m |
| Net-to-gross | 0.078 |
| Avg PHIE (net pay) | 0.196 |
| Avg Sw (net pay) | 0.313 |
| Avg Vsh (net pay) | 0.072 |
Monte Carlo, 500 realizations (seed 42). Net pay swing per parameter (one-at-a-time):
| Parameter | Net-pay swing (m) |
|---|---|
| m | 18.9 |
| Rw | 16.0 |
| a | 7.8 |
| n | 4.4 |
Dominant uncertainty: m (swing 18.9 m).
Multi-seed robustness: P50 UNSTABLE across seeds (spread 1.9 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.
| 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, 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: 2, range_warn: 2, spike_removal: 125, unit_conversion: 1.
| Validator | Type | Detail |
|---|---|---|
| vsh_phie_anticorrelation | support | Vsh-PHIE Pearson 0.91 > 0.3 (dirty rock + high porosity) |
| rt_sw_consistency | mechanical | 28 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: lithology"]
act_10["tool_call: lithology"]
This is a LAS-only study. Data that would calibrate the interpretation is absent:
From 1000 m (2.42). N-D clay ~0.08 -> 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": 26.060400000000016,
"net_pay_p10_p50_p90": [
2.2860000000000014,
12.954000000000008,
29.12364000000002
],
"driving_params": {
"a": 1.0,
"m": 2.0,
"n": 2.0,
"Rw": 0.04
},
"claim_verifier": {
"result": "FLAGS",
"flags": [
49.0,
2.42
],
"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 | ✓ |