Isometric Permanence Pathways 200y and 1000y

Parent hub: Isometric Biochar Protocol
Modules: Isometric Modules Soil Built Burial
Science: Permanence Science for Credits · models soil GHG from biochar · inertinite permanence benchmark · Permanence
Compare: Verra VM0044 Permanence and Quantification · Puro CORC200+ · CSI Global Biochar C-Sink

Primary source for soil equations: Biochar Storage in Soil Environments v1.3. Protocol framing: Biochar Production and Storage v1.3. Launch rationale: Isometric science article (2024-10-10).


Two soil crediting options

OptionDurability labelCore inputsConservatism
1200 yearsH/Corg + mean annual soil temperature~17th percentile Woolf fit; (F) capped at 0.95; soil T floor 7 °C
21,000 yearsRandom reflectance R₀ ≥ 2% on non-reactive CMean − 1 SD on both fractions; (F) capped at 0.95

Stored carbon:

[ CO_2e_{stored} = C_{biochar} \times m_{biochar} \times F_{durable} \times \frac{44.01}{12.01} ]

where (C_{biochar} =) Total C − (C_{inorg}) (only organic C credited).

Projects may combine both tiers under one validation if production batches are temporally and spatially separated with chain-of-custody — each batch under exactly one tier (soil module).


Eligibility chemistry before either option

ParameterThresholdSource
Molar H/Corg< 0.5Soil module Table 2
Molar O/Corg< 0.2Soil module Table 2
Heavy metals / PAH / PCDD/F / PCBWBC upper bounds (module tables)Soil module
LabsISO 17025 or Isometric-agreed equivalentSoil module
SamplesPrefer ≥ 3 per measured batchProtocol §8.3 / module

Contrast Verra soil gate H:Corg ≤ 0.7 (Verra VM0044 Permanence and Quantification).


Option 1 — 200-year (Woolf-conservative)

[ F_{durable,200} = \min\Bigl(0.95,; 1 - \bigl[c + (a + b \cdot \ln(T_{soil})) \cdot H/C_{org}\bigr]\Bigr) ]

CoefficientValue
(a)-0.383
(b)0.350
(c)-0.048

Fit uses the 17th percentile of the Woolf et al. (2021) durability distribution (~ one SD below the mean under normality assumptions) (soil module Table 4; Woolf DOI).

Soil temperature rules

  • Prefer project-specific annual soil T baselining (ISO 4974 or equivalent); ≥ 10 measurements per site-month average narrative in module
  • Or justified value from global soil T datasets (e.g., Lembrechts et al. 2022)
  • Air temperature may not proxy soil T (module notes soil often 2–4 °C warmer)
  • If within-boundary soil T varies by > 1 °C, split project or use highest (most conservative) T

EU alignment note

Isometric’s science article links the 200-year option to the EU Carbon Removal Certification Framework “permanent removal” framing (article). Policy detail: vault EU CRCF references in Carbon Markets Hub / research report — do not invent delegated-act thresholds here.


Option 2 — 1000-year (Ro / inertinite)

Science basis: inertinite permanence benchmark (DOI) — biochars with mean R₀ ≥ 2% structurally akin to inertinite macerals with geological persistence.

Measurement requirements

RequirementDetail
MethodRandom reflectance, e.g. ISO 7404-5:2009
Density≥ 500 maceral-level R₀ measurements per sample
Replication≥ 3 samples; submit R₀ histogram at verification
Non-reactive CThermogravimetric residual organic C (Hawk / Rock-Eval-style re-pyrolysis then combustion)
Crediting math((\bar{R}{pass} - s{R}) \times (\bar{C}{non\text{-}reactive} - s{C})) then min(0.95, max(0, ·))

Only the fraction passing the 2% benchmark, applied to the non-reactive pool, is credited — reactive C is discounted.

Comparison to CSI upper class

CSI Global Biochar C-Sink upper class uses higher Ro (≥ 3.8%) or HyPy ≥ 90% for 90% GPC — different threshold and pool logic (CSI Global Biochar C-Sink). Isometric’s 2% inertinite benchmark is the Sanei et al. framing, not CSI’s 3.8% upper class.


Buffer philosophy (soil)

Soil module projects are typically No Observable Risk → 0% buffer pool, because labile decay is already discounted in (F_{durable}). Risk reassessed at crediting-period renewal (soil module).

Built-environment module uses a 2% buffer under Very Low Risk framing (Isometric Modules Soil Built Burial).


Non-soil horizons (pointer)

ModuleHorizonPermanence approach
Low-oxygen burial≥ 1000yRo paths ± incubation safety factor 3
Built environment> 1000yInertinite + labile × (1 − 3×F_reversal); asphalt labile 100% abraded

Detail: Isometric Modules Soil Built Burial.


Intellectual map across standards

CampProgramsInputs
Decay-model / centuriesIsometric 200y; Puro CORC200+; Verra 100y Table 3H/Corg and/or temperature class, soil T
Inertinite / Ro millennialIsometric 1000y; CSI upper GPCR₀, HyPy, non-reactive C

Puro explicitly encourages Ro reporting but does not yet quantify with it (Puro CORC200+).